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  • Cambridge University Press  (1,146)
  • PANGAEA
  • 1985-1989
  • 1980-1984
  • 1965-1969  (1,202)
  • 1967  (1,202)
Collection
Keywords
Years
  • 1985-1989
  • 1980-1984
  • 1965-1969  (1,202)
Year
  • 1
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    PANGAEA
    In:  Supplement to: Bonatti, Enrico (1967): Mechanisms of deep-sea volcanism in the South Pacific. In: Abelson, P (Ed.) Researches in Geochemistry, Wiley, New York, 2, 453-491, hdl:10013/epic.45968.d001
    Publication Date: 2023-08-28
    Description: It is stressed that the main difference between quiet and hyaloclastic activity is that in the former the interaction between hot lava and seawater during the eruption is minimal, whereas it is very extensive in the latter. This strong interaction is the cause of the processes which accompany hyaloclastic eruptions, processes which, in their turn, influence the chemistry and mineralogy of wide areas of the Pacific Ocean floor. Admittedly they are not well known yet, but their extensive study seems worthwhile. Two suggestions based on data presented here may be pointed out : 1) Deep-sea basaltic rocks showing breccia and/or ash-like features must not necessarily have erupted under shallow water or above sea level, as is commonly believed. 2) The "altered" or "fresh" appearance of submarine basalts is not necessarily to be ascribed to the relative age or youth of the rock. In fact extensive "alteration" of submarine lavas may commonly take place rapidly at high temperature during the eruption, rather than gradually after emplacement as is generally the case in subaerial formations. Deep-sea waters of the Pacific normally have a pH close to 7 and a rather constant low temperature, close to 0°C. Alteration of igneous minerals after emplacement under such conditions must be exceedingly slow, and concepts of "weathering" as learned in surface geology cannot be applied.
    Keywords: Aluminium oxide; AMPH-001D; AMPH-002D; AMPH-005D; AMPH01AR; AMPH01AR-001D; AMPH01AR-002D; AMPH01AR-005D; AMPHITRITE; Argo; Calcium oxide; Chromium; Cobalt; Copper; DEPTH, sediment/rock; Description; Dredge; DRG; Event label; Iron; Magnesium oxide; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Optical spectrographic analysis; Pacific Ocean; Potassium oxide; Sample ID; Silicon dioxide; Titanium dioxide
    Type: Dataset
    Format: text/tab-separated-values, 64 data points
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  • 2
    Publication Date: 2023-08-28
    Keywords: Aluminium; Atomic emission spectroscopy (AES); Barium; Blake Plateau, Atlantic Ocean; Calcium; Cobalt; Copper; Date/Time of event; Deposit type; DEPTH, sediment/rock; Dredge; Dredge, rock; DRG; DRG_R; Elevation of event; Event label; GOS74; GOS74-2340; GOS74-2387; Gosnold; Horizon; Iron; Latitude of event; Lead; Longitude of event; Magnesium; Manganese; MDPC02HO-MP-026A-3; Method/Device of event; MIDPAC; Molybdenum; MPC-26A-3; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Phosphorus; Piston corer; Potassium; Sample ID; Silicon; Sodium; Strontium; Titanium; V03; V03-157; Vema; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 81 data points
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  • 3
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    PANGAEA
    In:  Supplement to: Gibson, T G; Schlee, John S (1967): Sediments and fossiliferous rocks from the eastern side of the Tongue of the Ocean, Bahamas. Deep Sea Research and Oceanographic Abstracts, 14(6), 691-702, https://doi.org/10.1016/S0011-7471(67)80007-X
    Publication Date: 2023-08-28
    Description: In August 1966, two dives were made with the deep-diving submersible Alvin along the eastern side of the Tongue of the Ocean to sample the rock and sediment. Physiographically, the area is marked by steep slopes of silty carbonate sediment and precipitous rock cliffs dusted by carbonate debris. Three rocks, obtained from the lower and middle side of the canyon (914–1676 m depth), are late Miocene-early Pliocene to late Pleistocene-Recent in age; all are deep-water pelagic limestones. They show (i) that the Tongue of the Ocean has been a deep-water area at least back into the Miocene, and (ii) that much shallow-water detritus has been swept off neighbouring banks to be incorporated with the deep-water fauna in the sediment.
    Keywords: 2684; AL50000; AL50200; AL50300; AL50400; ALV166; ALV-166; ALV500; ALV-500; ALV502; ALV-502; ALV-503; ALV-504; Alvin; Comment; Deposit type; DEPTH, sediment/rock; Description; Event label; File name; Grab; GRAB; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Substrate type; Tongue of the Ocean; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 42 data points
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  • 4
    Publication Date: 2023-08-28
    Description: This collection includes data on the chemical composition of ocean manganese nodules from the Pacific Ocean obtained with different methods.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 5
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    PANGAEA
    In:  Supplement to: Barnes, Steven S (1967): The formation of oceanic ferromanganese nodules (Ph.D. dissertation). University of California, San Diego, 118 pp
    Publication Date: 2023-08-28
    Description: Mineralogical and chemical analyses performed on 67 ferromanganese nodules from widely varying locations and depths within the marine environment of the Pacific Ocean indicate that the minor element composition is controlled by the mineralogy and that the formation of the mineral phases is depth dependent. The pressure effect upon the thermodynamics or kinetics of mineral formation is suggested as the governing agent in the depth dependence of the mineralogy. The minor elements, Pb and Co, appear concentrated in the dMnO2 phase, whereas Cu and Ni are more or less excluded from this phase. In the manganites, Pb and Co are relatively low in concentration, whereas Cu and Ni are spread over a wide range of values. The oxidation of Pb and Co from divalent forms in sea water to higher states can explain their concentration in the dMnO2 phase.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 6 datasets
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  • 6
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    PANGAEA
    In:  Supplement to: Newell, IM (1967): Abyssal Halacaridae (Acari) from the southeast Pacific. Pacific Insects, 9(4), 693-708, https://download.pangaea.de/reference/80730/attachments/9_4_-693.pdf
    Publication Date: 2023-08-28
    Description: Station 678E (29°22'S. latitude, 80WW. longitude) is roughly midway between San Felix and Juan Fernandez Islands, and approximately 700 km west of the coast of Chile. The sample at Station 678E was collected in a Riedl Dredge with a finer net sewn into the cod end of the 500 JJ mesh bag. The change in depth during the dredging operation indicated a rather rapid shelving. The bottom was a red clay with some volcanic ash. Manganese nodules were present (rock dredge sample).
    Keywords: ABR_Cruise17; ABR17_678E; Anton Bruun; Comment; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample ID; Sediment type; South Pacific Ocean
    Type: Dataset
    Format: text/tab-separated-values, 7 data points
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  • 7
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    PANGAEA
    In:  Supplement to: Ahrens, L H; Willis, J P; Oosthuizen, CO (1967): Further observations on the composition of manganese nodules, with particular reference to some of the rarer elements. Geochimica et Cosmochimica Acta, 31(11), 2169-2180, https://doi.org/10.1016/0016-7037(67)90059-2
    Publication Date: 2023-08-28
    Description: Mn, Fe, Ca, Co, Ni, Cu, Zn, Cd, Sn, Tl, Pb and Bi have been estimated in thirty-two nodules from the Pacific, Atlantic and Indian oceans. Various features about the composition of manganese nodules are discussed: element abundances, degrees of enrichment, inter-element relationships (notably between Ni and Cu, and between Zn and Cd), regional variations and some aspects of statistical distribution.
    Keywords: A-266/R-45; AFII-A1254; AFII-A316; AFII-A322; ALB-13; ALB-173; Albatross (1882-1921); Albatross1899-1900; Albatross1904-1905; ALBTR-13; ALBTR-173; ALBTR-4676; AT26601; AT266-45; Atlantic Ocean; Atlantis (1931); Banda Sea; Bismuth; Cadmium; Calcium; CASC-5D; CASCADIA; Cobalt; Copper; Core; CORE; Date/Time of event; DEPTH, sediment/rock; Description; Direct current (DC) arc spectrochemistry; DOWNWIND-H; Dredge; Dredge, chain bag; DRG; DRG_C; DWHD72; Elevation of event; Epce; Event label; FANB01BD; FANBD-20D; FANFARE-B; GAL_1950-1952_Denmark; Galathea; GALT-179; GALT-182; GALT-469; GALT-494; GALT-574; GALT-658; GALT-724; GC; Gravity corer; Horizon; Indian Ocean; Iron; Latitude of event; Lead; Longitude of event; Manganese; Nickel; NIOE-135; NIOE-42; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North-East Pacific Ocean; Northern_Holiday; North-West Pacific Ocean; NTHL02HO-010PH; NTHL-10; Pacific Ocean; PC; Piston corer; Sample ID; Spencer F. Baird; Tasman Sea; Thallium; Tin; V19; V19-232; Vema; Wired profile sonde; WP; X-ray fluorescence (XRF); Zinc
    Type: Dataset
    Format: text/tab-separated-values, 434 data points
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  • 8
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    PANGAEA
    In:  Supplement to: Cronan, David S (1967): The geochemistry of some manganese nodules and associated pelagic deposits (Ph. D. Dissertation). Dept. of Geochemistry, Imperial College of Science and Technology, London, United Kingdom, 728 pp
    Publication Date: 2023-08-28
    Description: The first part of this thesis includes some topics of a non-geochemical nature but which are of importance in interpreting the geochemistry of nodules. The points covered include their distribution, petrography, structure, mineralogy and internal compositional variations. Part Two includes the geochemistry of both nodules and that of their surrounding sediments, This geochemical study has been divided into firstly, a general geochemical study of both nodules and sediments using a statistical approach to the interpretation of the data, secondly, the regional geochemistry of Pacific and Indian Ocean nodules and sediments, the latter entirely uninvestigated in the past, and thirdly, local variations in the composition of nodules. Throughout, emphasis has been placed on the geochemistry of nodules in terms of their environment of formation.
    Keywords: AMPH01AR; AMPH03AR-084G; AMPH-084G; AMPHITRITE; Argo; Atlantic Ocean; Barium; CHA-297; Challenger1872; Chromium; Cobalt; Copper; Core; CORE; D2; D4; D5133; D5175; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Discovery (1962); DNWB0ABD; DNWB0ABD-018G; DODO; DODO-232D; DOWNWIND-B1; DOWNWIND-H; Dredge; Dredge, rock; DRG; DRG_R; DWBG18; DWHD47; Elevation of event; Event label; GC; Grab; GRAB; Gravity corer; H.M.S. Challenger (1872); Horizon; Indian Ocean; Iron; JAPANYON; JPYN04BD-011G; JPYN05BD-029G; JYN4-011G; JYN5-029G; Latitude of event; Lead; Loch_Fyne_B; Loch Fyne, Scotland; Longitude of event; Loss on ignition; LSDA; LSDA-219D; LUSIAD-A; Manganese; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Optical spectrographic analysis; Pacific Ocean; PC; Piston corer; PROA; PROA-105G; PROA-113PG; RISEPAC; RISP-111PG; RISP-111V; Sample comment; Sample ID; Sediment type; Size; Spencer F. Baird; Strontium; SYM_1872; SY Mallard; TC; Titanium; Trigger corer; Vanadium; Volumetric; WAH-2P; WAHI01BD; WAHINE; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 354 data points
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  • 9
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    PANGAEA
    In:  Supplement to: Pratt, Richard M (1967): Photography of seamounts (Chapter 13). In: Hersey, JB (Ed.): Deep Sea Photography, The Johns Hopkins Oceanographic Studies. John Hopkins University Press, 145-148, https://www.vliz.be/en/imis?module=ref&refid=11063
    Publication Date: 2023-08-28
    Description: Seamounts are very effectively studied by deep-sea photography. Each photograph can be considered as a sample point when used in connection with bathymetric surveys, dredge samples, and cores, thus making it possible to delineate and map geologic and biologic zones on a seamount. Seamounts transcend through a great depth range and are characterized by minimal sedimentation which results in exciting and photogenic differences of environment over a short distance, as typified by our studies of Great Meteor and the New England Seamounts.
    Keywords: AT260-8D; Bermuda Rise; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample ID; Sediment type; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 7 data points
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  • 10
    Publication Date: 2023-08-28
    Keywords: Cobalt; Copper; Description; Indian Ocean; Iron; John_Murray_Expedition; MABAH-166; Mabahiss (1933); Molybdenum; Monegasque Trawl; MTRW; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Sample code/label; Silicon; Spectrographic analysis; Titanium; X-ray fluorescence (XRF)
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
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  • 11
    Publication Date: 2023-08-28
    Keywords: Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; Indian Ocean; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; Vit 5186; Vit 5200; Vit 5202; Vit 5270; Vit 5272; Vityaz (ex-Mars); Vityaz-35; VITYAZ5186; VITYAZ5193; VITYAZ5200; VITYAZ5201; VITYAZ5202; VITYAZ5270; VITYAZ5272
    Type: Dataset
    Format: text/tab-separated-values, 116 data points
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  • 12
    Publication Date: 2023-08-28
    Keywords: Aluminium oxide; Barium oxide; Calcium oxide; Carbon, organic, total; Carbon dioxide; Chromium(III) oxide; Cobalt oxide; Copper(II) oxide; Description; Dredge; DRG; Elevation of event; Event label; Identification; Indian Ocean; Iron oxide, Fe2O3; Latitude of event; Longitude of event; Loss on ignition; Magnesium oxide; Manganese oxide; Molybdenum trioxide; Nickel oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Oxygen, gas; PC; Phosphorus pentoxide; Piston corer; Sample ID; Silicon dioxide; Sulfur trioxide; Titanium dioxide; Tungsten trioxide; Vanadium oxide; Vit 5186; Vit 5200; Vit 5202; Vit 5270; Vit 5272; Vityaz (ex-Mars); Vityaz-35; VITYAZ5186; VITYAZ5193; VITYAZ5200; VITYAZ5201; VITYAZ5202; VITYAZ5270; VITYAZ5272; Wet chemistry; Zirconium dioxide
    Type: Dataset
    Format: text/tab-separated-values, 275 data points
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  • 13
    Publication Date: 2023-08-28
    Keywords: Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; ENDV; ENDV_D169; ENDV_D5; ENDV_F116; ENDV_F127; ENDV_F129; ENDV_F132; ENDV_F133; Event label; HMNZS Endeavour (1944); Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Size; South Pacific Ocean; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 54 data points
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  • 14
    Publication Date: 2023-08-28
    Keywords: Aluminium; Barium; Beryllium; Boron; Chromium; Cobalt; DEPTH, sediment/rock; Dredge; DRG; ENDV; ENDV_D169; ENDV_D5; ENDV_F116; ENDV_F127; ENDV_F129; ENDV_F132; ENDV_F133; Event label; HMNZS Endeavour (1944); Identification; Iron; Lanthanum; Lead; Magnesium; Manganese; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Phosphorus; Sodium; South Pacific Ocean; Spectrographic analysis; Strontium; Tin; Titanium; Vanadium; Ytterbium; Yttrium; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 113 data points
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  • 15
    Publication Date: 2023-08-28
    Keywords: 2P-50; 2P-51; Barium; Calcium; Chromium; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Dredge; DRG; Elevation of event; Event label; Iron; Latitude of event; Longitude of event; Manganese; Microprobe; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Potassium; Prospector; Prospector-63; Sample ID; Scandium; Shape; Strontium; Thorium; Titanium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 41 data points
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  • 16
    Publication Date: 2023-08-28
    Keywords: 2P-50; 2P-51; Atomic absorption spectrometry (AAS); Cerium; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Europium; Event label; Iron; Lanthanum; Latitude of event; Longitude of event; Lutetium; Manganese; Molybdenum; Neodymium; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Prospector; Prospector-63; Samarium; Sample ID; Scandium; Shape; Size; Terbium; Titanium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 55 data points
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  • 17
    Publication Date: 2023-08-28
    Keywords: 2P-50; Calcium; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Iron; Latitude of event; Lead; Longitude of event; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Prospector; Prospector-63; Sample ID; Shape; Size; X-ray emission spectroscopy (XES); Zinc
    Type: Dataset
    Format: text/tab-separated-values, 26 data points
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  • 18
    Publication Date: 2023-08-28
    Keywords: Argo; Calcium; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Description; DODO; DODO-006D; DODO-008D; DODO-014D; DODO-015D-2; Dredge; DRG; Elevation of event; Event label; Iron; Latitude of event; Lead; Longitude of event; Manganese; Method/Device of event; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Sample ID; Shape; X-ray emission spectroscopy (XES); Zinc
    Type: Dataset
    Format: text/tab-separated-values, 69 data points
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  • 19
    Publication Date: 2023-08-28
    Keywords: Age, dated; Age, dated standard deviation; Argon-40; Atomic absorption spectrometry (AAS); Comment; Deposit type; DEPTH, sediment/rock; Description; DISTANCE; DOWNWIND-H; Dredge; Dredge, chain bag; DRG; DRG_C; DWHD47; Event label; FANB01BD; FANBD-20D; FANFARE-B; Horizon; Mass spectrometry; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northern_Holiday; North-West Pacific Ocean; NTHL02HO-010PH; NTHL-10; Pacific Ocean; Potassium; Sample ID; Spencer F. Baird; Substrate type; Wired profile sonde; WP
    Type: Dataset
    Format: text/tab-separated-values, 40 data points
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  • 20
    Publication Date: 2023-08-28
    Keywords: Alpha spectrometry; Argo; Atlantic Ocean; CARR-5; D4; Deposit type; DEPTH, sediment/rock; DISTANCE; Distance, maximum; Distance, minimum; DOWNWIND-H; Dredge; Dredge, rock; DRG; DRG_R; DWHD47; DWHD72; Event label; Horizon; LSDA; LSDA-219D; LUSIAD-A; MDPC02HO-MP-026A-3; MIDPAC; MPC-26A-3; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Sample ID; Thorium-230/Thorium-232 ratio; Thorium-232; Uranium-234/Uranium-238 activity ratio; Uranium-234/Uranium-238 activity ratio, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 228 data points
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  • 21
    Publication Date: 2023-08-28
    Keywords: Aluminium; Argo; Arsenic; Atlantic Ocean; Barium; Boron; Calcium; Carbon, total; CARR2_2D; CARR2_9D; CARR-5; CARROUSEL2; CHA-299; Challenger1872; Chromium; Cobalt; Copper; D3; D4; Deposit type; DEPTH, sediment/rock; Description; DNWB0ABD; DNWB0BBD; DODO; DODO-006D; DODO-011D; DODO-014D; DODO-015D-2; DODO-113D; DOWNWIND-B1; DOWNWIND-B2; DOWNWIND-H; Dredge; Dredge, rock; DRG; DRG_R; DWBD2; DWBD5; DWBD7; DWHD15; DWHD47; Elevation of event; Event label; F1HE-9; Gallium; Grab; GRAB; H.M.S. Challenger (1872); Horizon; Indian Ocean; Iron; JasperSeamount; JSPSMT-1; Latitude of event; Lead; Longitude of event; LSDA; LSDA-199D; LSDA-219D; LUSIAD-A; Magnesium; Manganese; MDPC02HO-MP-025F-2; MDPC02HO-MP-033K; MDPC02HO-MP-037C; MDPC03HO-MP-043B; MDPC03HO-MP-043C; MDPC03HO-MP-043D; Mercury; Method/Device of event; MIDPAC; Molybdenum; MPC-25F-2; MPC-33K; MPC-37C; MPC-43B; MPC-43C; MPC-43D; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North-East Pacific Ocean; Pacific Ocean; PC; Phosphorus; Piston corer; Potassium; PROA; PROA-072D; Rubidium; Sample ID; Scandium; Shape; Silicon; Size; SOB; SOB-013D; SOBO03BD-013D; Sodium; Southern Borderland; Spencer F. Baird; Strontium; Titanium; V15; V15-136; Vanadium; Vema; Water in rock; Wet chemistry; X-ray fluorescence (XRF); Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 487 data points
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  • 22
    Publication Date: 2023-07-10
    Keywords: Acari; Actinonema longicaudatum; Bathylaimus depressus; Batillipes; Cephalobus sp.; Chromadora nudicapitata; Coleoptera; Copepoda; DEPTH, sediment/rock; Desmodera ditlevseni; Desmodora bipapillata; Diptera; Distance, relative; Dolicholaimus oceanus; Gastrotricha; Halalaimus florescens; Halalaimus gracilis; Halalaimus relatus; Halalaimus sarsi; Haliplectus bickneri; Haliplectus caudopapillatus; Haliplectus minimus; HAND; IIOE - International Indian Ocean Expedition; Indeterminata; Kinorhyncha; Latronema orcinum; Lauratonema spiculifer; Leptokoenenia gerlachi; M1; Mesacanthion hirsutum; Metachromadora clavata; Meteor (1964); Microcerberus; Nematoda; Nygmatonchus minutus; Oligochaeta; Oncholaimellus meteori; Oncholaimus flagellatus; Oxystomina circulosa; Paracyatholaimus saradi; Parajapyx gerlachi; Polychaeta; Procamacolaimus tubifer; Protodrilus; Red Sea; Rhabditis sp.; Sample code/label; Sampling by hand; Sarso_beach; Sarsonia murphyi; Steineria parapolychaeta; Synonchium obtusum; Thalassoalaimus brasiliensis; Theristus flevensis; Theristus pertenuis; Triletium sp.; Turbellaria
    Type: Dataset
    Format: text/tab-separated-values, 556 data points
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  • 23
    Publication Date: 2023-07-10
    Keywords: Chromadora nudicapitata; Coleoptera; DEPTH, sediment/rock; Desmodora bipapillata; Distance, relative; Draconema cephalatum; Eurystomina mammillata; Halalaimus gracilis; Halalaimus sarsi; Haliplectus bickneri; Haliplectus caudopapillatus; HAND; IIOE - International Indian Ocean Expedition; Indeterminata; Lauratonema spiculifer; Leptokoenenia gerlachi; M1; Mesacanthion hirsutum; Mesacanthion monhystera; Metachromadora clavata; Meteor (1964); Microcerberus; Nematoda; Nygmatonchus minutus; Oligochaeta; Oncholaimellus meteori; Oxystomina circulosa; Platycoma africanum; Red Sea; Rhabditis sp.; Sample code/label; Sampling by hand; Sarso_beach; Steineria aegyptica; Synonchium obtusum; Theristus flevensis; Theristus pertenuis; Triletium sp.
    Type: Dataset
    Format: text/tab-separated-values, 170 data points
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  • 24
    Publication Date: 2023-07-11
    Keywords: Aragonite; Aragonite/Strontianite ratio; Calcite; Calcite/Dolomite ratio; Cross_Bank; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Magnesium-Calcite; PC; Piston corer; Size fraction
    Type: Dataset
    Format: text/tab-separated-values, 56 data points
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  • 25
    Publication Date: 2023-11-01
    Keywords: Abies; Acer; Alnus; Artemisia; Azolla glochidia; Azolla massulae; Azolla microspores; Betula; Botryococcus; Calluna; Campanulaceae; Carpinus; Caryophyllaceae; Centaurea montana-type; Centaurea sp.; cf. Syringa sect. Ligustrina; Chara; Chenopodiaceae; Compositae; Convolvulus; Corylus; Counting, palynology; Cruciferae; Cyperaceae; DEPTH, sediment/rock; EDEA; Edelman auger; Epilobium; Equisetum; Ericaceae; Eucommia; Euphorbia; Eu-Potamogeton-type; Filipendula; Fraxinus; Gramineae; Hippophae; Juniperus-type; Lower Saxony, Northern Germany; Lycopodium annotinum; Lycopodium clavatum; Lycopodium sp.; Lythrum; Mercurialis cf. annua; Myrica; Myriophyllum spicatum/verticillatum; Nuphar; Nymphaea; Oenotheraceae; Onobrychis; Osmunda; Osterholz; Picea; Pinus; Plantago major/media-type; Pollen and spore preservation; Pollen indeterminata; Polygonum persicaria-type; Polypodiaceae; Polypodium vulgare; Populus; Pteridium; Quercus; Ranunculaceae; Ranunculus; Rhamnus frangula; Rosaceae; Rosa-type; Rubiaceae; Salix; Sparganium-type; Sphagnum; Thalictrum; Tilia; Trifolium-type; Tsuga; Typha latifolia-type; Ulmus; Umbelliferae; Valeriana; Varia; Viburnum opulus
    Type: Dataset
    Format: text/tab-separated-values, 5688 data points
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  • 26
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    Publication Date: 2023-11-01
    Keywords: Acer; Alnus; Artemisia; Betula; Campanula; Caryophyllaceae; Chenopodiaceae; Compositae; Corylus; Counting, palynology; Cruciferae; Cyperaceae; DEPTH, sediment/rock; EDEA; Edelman auger; Elm_C; Eu-Potamogeton-type; Filipendula; Fraxinus; Gramineae; Liliaceae; Lower Saxony, Northern Germany; Nuphar; Nymphaea; Papilionaceae; Picea; Pinus; Pollen indeterminata; Pollen zone; Polypodiaceae; Quercus; Ranunculus; Rosaceae; Rubiaceae; Sparganium-type; Tilia; Ulmus; Umbelliferae; Varia; Viburnum opulus
    Type: Dataset
    Format: text/tab-separated-values, 272 data points
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  • 27
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    Publication Date: 2023-11-01
    Keywords: Abies; Acer; Alnus; Artemisia; Betula; Carpinus; Caryophyllaceae; Chenopodiaceae; Compositae; Corylus; Counting, palynology; Cruciferae; Cyperaceae; DEPTH, sediment/rock; Dryopteris austriaca; Dryopteris thelypteris; EDEA; Edelman auger; Elm_A; Epilobium; Equisetum; Eu-Potamogeton-type; Fagus; Filipendula; Fraxinus; Gramineae; Hedera; Helianthemum; Hystrichosphaerids; Ilex; Juglans; Juniperus-type; Lemna; Liquidambar; Lower Saxony, Northern Germany; Lycopodium annotinum; Lycopodium clavatum; Matteuccia struthiopteris; Myriophyllum spicatum/verticillatum; Nuphar; Nymphaea; Osmunda; Picea; Pinus; Plantago major/media-type; Pollen indeterminata; Pollen zone; Polypodiaceae; Polypodium; Pre-Quaternary sporomorphs; Pteridium; Quercus; Ranunculaceae; Ranunculus; Rhamnus frangula; Rhus; Rubiaceae; Rumex; Salix; Saxifraga-type; Sciadopitys; Scrophulariaceae; Sparganium-type; Taxus; Thalictrum; Tilia; Tsuga; Typha latifolia-type; Ulmus; Umbelliferae; Varia; Viburnum opulus
    Type: Dataset
    Format: text/tab-separated-values, 1320 data points
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  • 28
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    Publication Date: 2023-11-01
    Keywords: Abies; Alnus; Artemisia; Betula; Blechnum spicant; Botrychium; Campanula; Carya; Caryophyllaceae; Castanea; Chenopodiaceae; Comment; Compositae; Corylus; Counting, palynology; Cruciferae; Cryptomeria; Cyperaceae; DEPTH, sediment/rock; Dryopteris austriaca; Dryopteris thelypteris; EDEA; Edelman auger; Elm_B; Equisetum; Ericaceae; Eu-Potamogeton-type; Fagus; Filipendula; Fraxinus; Gramineae; Hedera; Hystrichosphaerids; Ilex; Juniperus-type; Labiatae; Lower Saxony, Northern Germany; Lycopodium annotinum; Menyanthes; Nuphar; Nymphaea; Papilionaceae; Picea; Pinus; Pollen, tertiary, other; Pollen indeterminata; Pollen zone; Polypodiaceae; Polypodium; Pre-Quaternary sporomorphs; Pteridium; Quercus; Rhamnus frangula; Rosaceae; Rubiaceae; Rumex; Salix; Taxus; Thalictrum; Tilia; Typha latifolia-type; Ulmus; Umbelliferae; Urticaceae; Valeriana; Varia; Viburnum opulus; Viscum
    Type: Dataset
    Format: text/tab-separated-values, 1830 data points
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  • 29
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    Publication Date: 2023-11-01
    Keywords: 1b; Abies; Acer; Alnus; Anemone-type; Artemisia; Betula; Botryococcus; Calluna; Carpinus; Carya; Caryophyllaceae; Celtis; cf. Athyrium; cf. Brasenia; cf. Eucommia; cf. Syringa sect. Ligustrina; cf. Viburnum opulus; Chara; Chenopodiaceae; Compositae; Corylus; Counting, palynology; Cruciferae; Cryptomeria; Cyperaceae; DEPTH, sediment/rock; Dryopteris thelypteris; EDEA; Edelman auger; Elm_K; Engelhardtia; Equisetum; Ericaceae; Eu-Potamogeton-type; Fagus; Filipendula; Fraxinus; Gentianaceae; Geum-type; Gramineae; Hedera; Humulus-type; Hystrichosphaerids; Ilex; Impatiens noli-tangere; Juglandaceae; Juniperus-type; Keteleeria; Liquidambar; Lower Saxony, Northern Germany; Lycopodium annotinum; Lycopodium clavatum; Lycopodium sp.; Lysimachia; Matteuccia struthiopteris; Mentha-type; Menyanthes; Myriophyllum alterniflorum; Myriophyllum spicatum/verticillatum; Nuphar; Nymphaea; Nyssa; Osmunda; Papilionaceae; Pediastrum; Picea; Pinus; Plantago lanceolata; Plantago major/media-type; Platycarya; Pollen, tertiary, other; Pollen indeterminata; Pollen zone; Polygonum persicaria-type; Polypodiaceae; Populus; Pre-Quaternary sporomorphs; Pteridium; Pterocarya; Quercus; Ranunculaceae; Ranunculus; Rhamnus frangula; Rhus; Rosaceae; Rosa-type; Rubiaceae; Rumex; Sagittaria; Salix; Saxifragaceae; Sciadopitys; Scrophulariaceae; Sparganium-type; Sphagnum; Taxus; Thalictrum; Tilia; Trollius; Tsuga; Typha latifolia-type; Ulmus; Umbelliferae; Utricularia; Valeriana; Varia; Viburnum opulus; Viscum; Vitis
    Type: Dataset
    Format: text/tab-separated-values, 6489 data points
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  • 30
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    Publication Date: 2023-11-01
    Keywords: 25; Abies; Acer; Alnus; Artemisia; Betula; Campanula; Caryophyllaceae; Chenopodiaceae; Compositae; Corylus; Counting, palynology; Cruciferae; Cyperaceae; DEPTH, sediment/rock; Dryopteris filix-mas; Dryopteris thelypteris; EDEA; Edelman auger; Elm_D; Equisetum; Ericaceae; Eu-Potamogeton-type; Fagus; Filipendula; Fraxinus; Geum-type; Gramineae; Hystrichosphaerids; Juniperus-type; Lower Saxony, Northern Germany; Nuphar; Nymphaea; Papilionaceae; Picea; Pinus; Pollen, tertiary, other; Pollen indeterminata; Pollen zone; Polypodiaceae; Polypodium; Potentilla-type; Pteridium; Quercus; Ranunculaceae; Rhamnus frangula; Rosaceae; Rosaceae-type; Rubiaceae; Rumex; Salix; Sparganium-type; Sphagnum; Taxus; Tilia; Typha latifolia-type; Ulmus; Umbelliferae; Utricularia; Varia; Viburnum opulus; Viscum
    Type: Dataset
    Format: text/tab-separated-values, 1815 data points
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  • 31
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    In:  Supplement to: Isaeva, Alexandra B (1967): Chemical composition of ferromanganese nodules of the Indian ocean (in Russian). Lithology and Mineral Resources, 3, 43-56, hdl:10013/epic.46141.d001
    Publication Date: 2023-08-28
    Description: This paper presents data on the chemical composition of iron-manganese nodules and associated sediments collected during the 35th voyage of the R/V "Vityaz" in 1962. The samples were made available to the author by Prof, P. L. Bezrukov. Data on the general distribution of manganese nodules at the bottom of the Indian Ocean were already given by P. L. Bezrukov (1962, 1963). Here the author analyzed the geochemistry of nodules samples from seven stations and four samples from the associated sediments. The analysis separates the outer layer of nodules from their apparent internal core.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 32
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    In:  Supplement to: Summerhayes, Colin P (1967): Manganese nodules from the South-Western Pacific. New Zealand Journal of Geology and Geophysics, 10(6), 1372-1381, https://doi.org/10.1080/00288306.1967.10423222
    Publication Date: 2023-08-28
    Description: Manganese nodules from the Campbell Plateau and Macquarie Ridge have been chemically analysed and their compositions compared with other Pacific nodules. No significant differences in composition are apparent. Foraminifera from nodule nucleii are late Tertiary or Quaternary, indicating the late geological formation of manganese nodules in this region. Nodule formation may be related to late Tertiary or Quaternary submarine volcanism.
    Keywords: Dredge; DRG; ENDV; ENDV_D169; ENDV_D5; ENDV_F116; ENDV_F127; ENDV_F129; ENDV_F132; ENDV_F133; HMNZS Endeavour (1944); NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; South Pacific Ocean
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 33
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    In:  Supplement to: Laughton, Anthony S (1967): RRS "Discovery" Cruise 16, 20 January - 6 May 1967. Geology and geophysics in the Red Sea, Gulf of Aden and N.W. Indian Ocean. Institute of Oceanographic Sciences Cruise Report, Wormley, UK, 16, 15 pp, https://eprints.soton.ac.uk/id/eprint/392182
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken on Cruise 16 of the R.R.S. "Discovery" from January until May 1967 by the National Institute of Oceanography, Wormley, United Kingdom. A total of 73 cores and dredges were recovered and are available through the British Oceanographic Data Centre for sampling and study.
    Keywords: Carlsberg Ridge; Comment; Core; CORE; D16; D6224; D6243; D6249; D6252; D6253; D6254; D6256; D6257; D6263; D6264; D6267; D6269; D6271; D6273; D6274; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Discovery (1962); Dredge, rock; DRG_R; Elevation of event; Event label; Grab; GRAB; Gulf of Aden; Indian Ocean, Carlsberg Ridge; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Photo/Video; Position; PV; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 149 data points
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  • 34
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    In:  Supplement to: Barnes, Steven S; Dymond, Jack R (1967): Rates of accumulation of ferro-manganese nodules. Nature, 213(5082), 1218-1219, https://doi.org/10.1038/2131218a0
    Publication Date: 2023-08-28
    Description: Although various models have been proposed to explain the origin of manganese nodules (see Goldberg and Arrhenius), two major hypotheses have received extensive attention. One concept suggests that manganese nodules form as the result of interaction between submarine volcanic products and sea water. The common association of manganese nodules with volcanic materials constitutes the main evidence for this theory. The second theory involves a direct inorganic precipitation of manganese from sea water. Goldberg and Arrhenius view this process as the oxidation of divalent manganese to tetravalent manganese by oxygen under the catalytic action of particulate iron hydroxides. Manganese accumulation by the Goldberg and Arrhenius theory would be a relatively slow and comparatively steady process, whereas Bonatti and Nayudu believe manganese nodule formation takes place subsequent to the eruption of submarine volcanoes by the acidic leaching of lava.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 35
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    In:  Supplement to: Cronan, David S; Tooms, J S (1967): Geochemistry of manganese nodules from the N.W. Indian Ocean. Deep Sea Research and Oceanographic Abstracts, 14(2), 239-249, https://doi.org/10.1016/0011-7471(67)90009-5
    Publication Date: 2023-08-28
    Description: Manganese nodules collected from four sites in the N.W. Indian Ocean by R.R.S. Discovery have been analysed for a range of elements. At two of the sites, samples were collected from two morphological populations, at one of these sites each population being a distinct chemical population also. In addition, considerable differences have been observed in the composition of morphologically similar modules from sites a few miles apart. The information obtained is of significance in any consideration of the genesis of the nodules and could have practical implications in the event that manganese nodules become a potential source of manganese and other metallic elements.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 36
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    In:  Supplement to: Winterhalter, Boris; Siivola, Jaakko (1967): An electron microprobe study of the distribution of iron, manganese, and phosphorus in concretions from the Gulf of Bothnia, northern Baltic Sea. Comptes Rendus de la Société Géologique de Finlande, 39, 161-172, https://www.geologinenseura.fi/sites/geologinenseura.fi/files/bt_229.pdf
    Publication Date: 2023-08-28
    Description: Fe-Mn-concretions of a spheroidal type were found according to electron probe determinations to consist of alternating iron- and manganese-rich layers. This pattern was ascribed to seasonal variations in the physico-chemical conditions governing the precipitation of the hydrous oxides of iron and manganese. Calculations based on the rhythmic growth of the concretions investigated gave a mean accumulation rate of 0.15-0.20 mm/yr. The rather high phosphorus content (average 3.5 % P2O5) of the concretions was found to be concentrated in the iron-rich layers, probably as a result of the scavenging effect of ferric hydroxide.
    Keywords: Analyst; Baltic Sea; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; Grab; GRAB; Iron oxide, Fe2O3; Latitude of event; Longitude of event; Manganese oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Phosphorus pentoxide; Sample ID; Wet chemistry; WNT-A3; WNT-BII; WNT-BIII; WNT-KA4; WNT-P20; WNT-P9; WNT-RR5; WNT-SM2; WNT-US4
    Type: Dataset
    Format: text/tab-separated-values, 60 data points
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  • 37
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    In:  Woods Hole Oceanographic Institution | Supplement to: Milliman, John; Manheim, Frank T; Pratt, Richard M; Zarudzki, E F K (1967): ALVIN dives on the continental margin off the southeastern United States, July 2-13, 1967. Woods Hole Oceanographic Institution, Woods Hole, MA, Technical Report, 67-80, 48, https://doi.org/10.1575/1912/1521
    Publication Date: 2023-08-28
    Description: In late June and July, 1967, the Deep Submergence Research Vehicle (DSRV) ALVIN, aboard its mother ship, LULU, proceeded from the spring base of operations, Nassau, to its home port of Woods Hole. During this trip, from July 2 to July 14, a series of five dives were made by ALVIN on the Blake Plateau off Georgia and South Carolina, and on the continental slope north of Cape Hatteras. One of the objectives of the dive was to investigate the manganese and phosphate deposits of the Blake Plateau.
    Keywords: ALV-200; ALV-201; ALVIN; Blake Plateau, Atlantic Ocean; Comment; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; Event label; Latitude of event; Longitude of event; Lulu; Lulu0767; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample ID; Sediment type; Size; Submersible Alvin
    Type: Dataset
    Format: text/tab-separated-values, 22 data points
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  • 38
    Publication Date: 2023-08-28
    Keywords: Barium; Chromium; Cobalt; Copper; D2; D5133; D5136; D5138; D5179; Description; Discovery (1962); Dredge, rock; DRG_R; Event label; Indian Ocean; Iron; Lead; Loss on drying; Loss on ignition; Manganese; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Sample ID; Silicon; Titanium
    Type: Dataset
    Format: text/tab-separated-values, 435 data points
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  • 39
    Publication Date: 2023-08-28
    Keywords: Aluminium; Argo; Atlantic Ocean; Atomic absorption spectrometry (AAS); Barium; Beryllium; Boron; Cadmium; Calcium; CARR2_9D; CARROUSEL2; Cerium; Chromium; Cobalt; Copper; D3; D4; Deposit type; DEPTH, sediment/rock; Description; DODO; DODO-006D; DODO-008D; DODO-014D; DODO-015D-2; DODO-113D; DOWNWIND-H; Dredge; Dredge, rock; DRG; DRG_R; DWHD15; DWHD47; Elevation of event; Europium; Event label; Horizon; Indian Ocean; Iron; JasperSeamount; JSPSMT-1; Lanthanum; Latitude of event; Lead; Longitude of event; LSDA; LSDA-199D; LSDA-219D; LUSIAD-A; Lutetium; Magnesium; Manganese; MDPC02HO-MP-025F-2; MDPC02HO-MP-033K; MDPC02HO-MP-037C; Method/Device of event; MIDPAC; Molybdenum; MPC-25F-2; MPC-33K; MPC-37C; Neodymium; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Phosphorus; Potassium; PROA; PROA-072D; Samarium; Sample ID; Scandium; Shape; Silicon; Size; Sodium; Spencer F. Baird; Strontium; Terbium; Thallium; Thorium; Titanium; Vanadium; Ytterbium; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 283 data points
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  • 40
    Publication Date: 2023-08-28
    Keywords: Argo; Barium; Cadmium; Chromium; Deposit type; DEPTH, sediment/rock; DODO; DODO-011D; DODO-015D-2; DODO-113D; DOWNWIND-H; Dredge; DRG; DWHD47; Element analysis, neutron activation (NAA); Elevation of event; Event label; Horizon; Indian Ocean; Latitude of event; Longitude of event; Magnesium; Method/Device of event; Molybdenum; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Phosphorus; Potassium; PROA; PROA-072D; Sample ID; Shape; Sodium; Spencer F. Baird; Strontium; Thallium; Tin; Titanium; Vanadium; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 38 data points
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  • 41
    Publication Date: 2023-08-28
    Keywords: Aluminium; Barium; Beryllium; Boron; Calcium; Carbon, total; CHA-299; Challenger1872; Chromium; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Description; DOWNWIND-H; Dredge; Dredge, rock; DRG; DRG_R; DWHD15; DWHD47; Elevation of event; Event label; Grab; GRAB; H.M.S. Challenger (1872); Horizon; Iron; Latitude of event; Lead; Longitude of event; Magnesium; Manganese; MDPC03HO-MP-043B; Method/Device of event; MIDPAC; Molybdenum; MPC-43B; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Potassium; Sample ID; Scandium; Shape; Silicon; Size; Sodium; Strontium; Sulfur, total; Titanium; Vanadium; Water in rock; Wet chemistry
    Type: Dataset
    Format: text/tab-separated-values, 94 data points
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  • 42
    Publication Date: 2023-08-28
    Keywords: Aluminium; Argo; Barium; Bismuth; Boron; Cadmium; Calcium; Carbon, total; Cerium; CHA-299; Challenger1872; Chromium; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Description; DNWB0ABD; DNWB0BBD; DODO; DODO-113D; DOWNWIND-B1; DOWNWIND-B2; DOWNWIND-H; Dredge; Dredge, rock; DRG; DRG_R; DWBD2; DWBD5; DWBD7; DWHD15; DWHD47; Elevation of event; Event label; Gallium; Grab; GRAB; H.M.S. Challenger (1872); Horizon; Indian Ocean; Iron; Lanthanum; Latitude of event; Lead; Lithium; Longitude of event; Magnesium; Manganese; MDPC02HO-MP-025F-2; MDPC02HO-MP-033K; MDPC03HO-MP-043B; MDPC03HO-MP-043C; Method/Device of event; MIDPAC; Molybdenum; MPC-25F-2; MPC-33K; MPC-43B; MPC-43C; Neodymium; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North-East Pacific Ocean; Pacific Ocean; PC; Phosphorus; Piston corer; Potassium; Quantum emission spectrography; Sample ID; Scandium; Shape; Silicon; SOB; SOB-013D; SOBO03BD-013D; Sodium; Southern Borderland; Spencer F. Baird; Strontium; Sulfur, total; Thallium; Thorium; Titanium; V15; V15-136; Vanadium; Vema; Water in rock; Wet chemistry; Ytterbium; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 353 data points
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  • 43
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    In:  Scripps Institution of Oceanography, UC San Diego
    Publication Date: 2023-09-25
    Keywords: Argo; Comment; Deposit type; DEPTH, sediment/rock; Description; Dredge; Dredge, rock; DRG; DRG_R; Event label; GC; Gravity corer; Horizon; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; NOVA01AR-005G; NOVA01AR-007G; NOVA01AR-011G; NOVA03HO-016D; NOVA04HO-022D; NOVA04HO-027D; NOVA04HO-031D; NOVA04HO-061D; NOVA04HO-062D; NOVA04HO-063D; NOVA04HO-064D; NOVA05AR-041D; NOVA05AR-043D; NOVA05AR-045D; NOVA05AR-053P; NOVA05AR-057D; NOVA05HO-01D; NOVA05HO-03D; NOVA05HO-03GO; NOVA08AR-113G; NOVA08AR-115G; NOVA08AR-118D; NOVA08AR-122G; NOVA-A; NOVA-A113G; NOVA-A115G; NOVA-A118D; NOVA-A11G; NOVA-A122G; NOVA-A41D; NOVA-A43D; NOVA-A45D; NOVA-A53; NOVA-A57D; NOVA-A5G; NOVA-A7G; NOVA-H; NOVA-H16D; NOVA-H1D; NOVA-H22D; NOVA-H27D; NOVA-H31D; NOVA-H3D; NOVA-H3GO; NOVA-H61D; NOVA-H62D; NOVA-H63D; NOVA-H64D; Pacific Ocean; PC; Piston corer; Position; Quantity of deposit; Sediment type; Size; Southwest Pacific Ocean; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 180 data points
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  • 44
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    In:  Supplement to: Grant, John Bruce (1967): A comparison of the chemistry and mineralogy with the distribution and physical aspects of marine manganese concretions of the Southern Oceans. Contributions of the Sedimentology Research Laboratory, Florida State University, 19, 99 pp, https://ntrl.ntis.gov/NTRL/dashboard/searchResults/titleDetail/PB177287.xhtml
    Publication Date: 2023-10-04
    Description: An extensive deposit of ferromanganese concretions has been investigated in the Southern Ocean around Antarctica, a region of particular interest in that it contains most of the parameters thought to be of importance in concretion formation. The physical and chemical properties of 93 concretions from 62 stations have been analyzed for possible interpretations as to the elemental source and the distributional characteristics as possible responses to respective parameters. It was found that four classes of concretionary types best represent the physical characteristics of concretions recovered within this area and that their morphology may be representative of the rate of formation and the proximity to the source of elemental constituents. It is suggested that the major source of concentrated elements in Southern Ocean ferromanganese concretions is submarine volcanism, with the dominant volcanism occurring along the Pacific-Antarctic Ridge. There is some evidence that connects periodic concretion growth and distribution characteristics to possible glacial and inter-glacial periods.
    Keywords: AFII-A451; Alpha spectrometry; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Description; Dredge; Dredge, rock; DRG; DRG_R; Elevation of event; ELT05; ELT05.015-RD; ELT05.017-RD; ELT06; ELT06.005-RD; ELT06.010-RD; ELT06.011-B; ELT07; ELT07.001-RD; ELT10; ELT10.002-RD; ELT10.013-RD; ELT10.021A-RD; ELT11; ELT11-001-BT; ELT11-003-BT; ELT13; ELT13.007-BT; ELT13.008-BT; ELT14; ELT14.007-RD; ELT15; ELT15.006-RD; ELT16; ELT16.006-BT; ELT17; ELT17.001-RD; Eltanin; Event label; Identification; Iron; Latitude of event; Longitude of event; Manganese; Method/Device of event; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Southern Ocean; South Pacific Ocean; South Tasman Sea; Thorium-232; TRAWL; Trawl net; Uranium-238; X-ray fluorescence (XRF)
    Type: Dataset
    Format: text/tab-separated-values, 248 data points
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  • 45
    facet.materialart.
    Unknown
    PANGAEA
    Publication Date: 2024-03-06
    Keywords: Betula sp., fruits; Betula sp., fruit scales; Calluna vulgaris; Carex sect. Eucarex; Carex sect. Vignea; Caryophyllaceae; Ceratophyllum demersum; Chara, oogonia; Counting, palynology; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; EDEA; Edelman auger; Elm_B; Juncus; Lower Saxony, Northern Germany; Menyanthes; Najas minor; Nuphar; Nymphaea; Pinus, seeds; Pollen zone; Polygonum lapathifolium; Potamogeton cf. lucens; Potamogeton fluitans; Potamogeton friesii; Potamogeton natans; Potamogeton perfoliatus; Potamogeton praelongus; Potamogeton pusillus; Potamogeton sp.; Potamogeton trichoides; Ranunculus sceleratus; Rubus idaeus; Rumex maritimus; Rumex sp.; Umbelliferae
    Type: Dataset
    Format: text/tab-separated-values, 798 data points
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  • 46
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    Unknown
    PANGAEA
    Publication Date: 2024-03-06
    Keywords: 1b; Betula nana, fruits; Betula nana, fruit scales; Betula sp., fruits; Betula sp., fruit scales; Brasenia; Calluna vulgaris; Carex sect. Eucarex; Carex sect. Vignea; Caryophyllaceae; Ceratophyllum demersum; Chara, oogonia; Counting, palynology; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; EDEA; Edelman auger; Elm_K; Juncus; Lower Saxony, Northern Germany; Menyanthes; Najas minor; Nuphar; Nymphaea; Nymphaea: hairs; Pinus, seeds; Pollen zone; Polygonum lapathifolium; Polygonum sp.; Potamogeton cf. lucens; Potamogeton natans; Potamogeton praelongus; Potamogeton sp.; Potamogeton trichoides; Ranunculus sceleratus; Rubus idaeus; Rumex maritimus; Rumex sp.; Sagittaria sagittifolia; Umbelliferae
    Type: Dataset
    Format: text/tab-separated-values, 1773 data points
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  • 47
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    Unknown
    PANGAEA
    In:  Supplement to: Traganza, Eugene D (1967): Dynamics of the carbon dioxide system on the Great Bahama Bank. Bulletin of Marine Science, 17(2), 348-366, https://www.ingentaconnect.com/content/umrsmas/bullmar/1967/00000017/00000002/art00010
    Publication Date: 2024-03-15
    Description: Carbon dioxide is lost from the ocean by calcium carbonate precipitation (-p), photosynthesis (-b) and gas evasion at the sea surface (-g). Among the most active sites are warm shallow seas. In this paper seasonal studies on the Great Bahama Bank relate these processes in an equation which takes into account the indirect effects of advection (a), evaporation (e), and eddy diffusion (d). Calcium carbonate precipitation is very seasonal and accounts for about half of the total losses. The delta sum CO2/deltaCa ratio is always about 1.87 on the bank. A high summer carbonate loss is inversely correlated with summer increases of chlorinity and temperature suggesting that CaCO3 is precipitated inorganically or biogenic production of CaCO3 is regulated by these parameters or both.
    Keywords: Alkalinity, total; Aragonite saturation state; Bicarbonate; Bicarbonate ion; Calcification/Dissolution; Calcification rate of calcium carbonate; Calcite saturation state; Calculated; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Carbon dioxide, total; Chloride; Coast and continental shelf; Date; Entire community; EPOCA; EUR-OCEANS; European network of excellence for Ocean Ecosystems Analysis; European Project on Ocean Acidification; Field observation; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); North Atlantic; OA-ICC; OCE; Ocean Acidification International Coordination Centre; Oceanography; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Pelagos; pH; Salinity; Temperate; Temperature, water; Traganza_Great_Bahama_Bank
    Type: Dataset
    Format: text/tab-separated-values, 279 data points
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  • 48
    Publication Date: 1967-01-01
    Description: The C14 dates given below are a continuation of the work presented in our previous list (RIKEN II), and have been obtained by counting CO2 at ca. 2 atm pressure in a 2.7 L stainless steel counter. Results obtained during 1966 are described.
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  • 49
    Publication Date: 1967-01-01
    Description: Most of these analyses we obtained during 1966 with equipment and techniques previously employed. Methane from the higher numbered samples was produced in a bomb reactor at pressures up to 1000 psi. Also, many smaller samples were counted in a 700-ml vol counter at 2 atm pressure, which has a background of 1.76 = .02 counts/min.
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  • 50
    Publication Date: 1967-01-01
    Description: The following list of dates is compiled from samples prepared since publication of our last date list (OWU II) and includes determinations through November, 1966. Equipment and operating procedures are the same, except that the sample conversion system has been altered to include a second vacuum pumping system and a separate oxygen/nitrogen combustion train.
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  • 51
    Publication Date: 1967-01-01
    Description: The measurements reported in this list were made in the Louvain C14 dating laboratory in 1966. Sample preparation, counting procedure and calculation method are described in the previous lists. Ages are calculated on the basis of a C14 half life of 5570 yr (Godwin, 1962). Errors, including the experimental standard deviation of the counting rate of the background, of the modern standard and of the unknown sample, are expressed by 1σ (Crèvecoeur and others, 1959).
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  • 52
    Publication Date: 1967-01-01
    Description: This date list includes those series of samples completed in this laboratory as of November, 1966. The B.P. ages are based upon A.D. 1950, and are calculated with a half-life value of 5568 yr. All samples were counted at least twice for periods of not less than 1000 min each. Errors quoted are derived from measurements of sample, background, and modern-age calibration, but do not include any half-life error. All samples were pretreated with 3N HCl, and some, where noted, received additional pretreatment with 2% NaOH for the removal of possible humic contaminants.
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  • 53
    Publication Date: 1967-01-01
    Description: The Radiocarbon Dating Laboratory of the Oak Ridge Institute of Nuclear Studies (ORINS) was developed as a teaching and research facility in the Special Training Division. This facility is available to participants enrolled in various courses held at ORINS, research groups associated with the 41 universities that make up the Oak Ridge Associated Universities (ORAU), and other colleges, unversities or institutions interested in this lab for teaching or research.
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  • 54
    Publication Date: 1967-01-01
    Description: In all measurements reported in La Jolla I through IV and for the first of those herein reported (LJ-994 to LJ-1025 and LJ-GAP-1 to LJGAP-15), we followed the procedure designed by Suess (1954) in producing acetylene (C2H2) for radiocarbon counting. For the subsequent samples, however, the following reaction for C2H2 synthesis was used:
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  • 55
    Publication Date: 1967-01-01
    Description: Most of the measurements reported here have been obtained with the 4.5-L CO2 counter previously described (Kiel I; Erlenkeuser, 1965). A few samples have been dated with a 3-L proportional counter. The copper counter is surrounded by 28 GM counters in the form of a double ring. The total assembly is shielded by 10 cm of old lead. Neither an inner lead shield between counter and anticoincidence ring nor screening of sensitive volume by a quartz tube-as in the 4.5-L counter-has been used. Background of the small counter is 17.20 cpm or The 0.95 x NBS value is 9.5 cpm at 400 torr. Within statistical error background does not depend on atmospheric pressure. The 3-L counter is placed under a concrete wall, 2.5 m in length and 9.4 m in height.
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  • 56
    Publication Date: 1967-01-01
    Description: The following list covers measurements of bomb-produced C14 in series of cereals and grasses collected on the northern hemisphere from 1956 through 1966. Samples were measured in order to determine the yearly addition of bomb produced C14 at a single locality, and to detect possible geographic variations in the distribution and uptake of bomb-generated C14 in terrestrial plant material during years with greatly varying additions of bomb C14. Measurements are given in the ∆ scale (Lamont VIII), i.e. per mil deviations from 0.95 times the activity of the NBS oxalic-acid standard (the natural C14 level).
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  • 57
    Publication Date: 1967-01-01
    Description: Both the 2-L counter, described in GSC I, and the 5-L counter (GSC IV) were operated routinely during the past year. Approximately half of the determinations reported here were obtained from each counter. The 5-L counter was operated mainly at 1 atm.
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  • 58
    Publication Date: 1967-01-01
    Description: This date list contains a selection of C14 dates of geological samples obtained from March 1963 until July 1966. The preceding date lists (Hannover I, III, IV) give a description of preparation and measuring methods.
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  • 59
    Publication Date: 1967-01-01
    Description: This report summarizes the radiocarbon dates obtained at the University of Wisconsin since November, 1965; the procedures followed and equipment used have been described previously (Wisconsin II).The dates reported have been calculated on the assumption of a half-life of 5568 yr for C14, 1950 as the reference year. Samples have normally been run at 3 atm pressure for a minimum of 15,000 counts. The standard deviation quoted includes only the 1σ of the counting statistics of background, sample, and standard counts.
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  • 60
    Publication Date: 1967-01-01
    Description: The measurements reported have been carried out during 1966 in the Isotope Laboratory of the Institute of Geophysics and Planetary Physics as a continuation of the UCLA date lists I through V. Samples were analyzed as CO2-gas at one atm in a 7.5 L proportional counter with three energy channels. The all-solid-state unit is supplied with high voltage from a remarkably stable and interference-free battery source. Radiocarbon ages have been calculated on the basis of a 5568-yr half-life as was recommended by the Sixth International C14 and H3 Dating Conference, June 1965, in Pullman, Washington. The standard for the contemporary biosphere remains as 95% of the count rate of NBS oxalic acid for radiocarbon laboratories. Background determinations have been based on CO2 obtained from marble. The error listed is always at least a one-sigma statistical counting error. In critical cases C13/C12 isotope ratio measurements were made to correct the dates. All samples were subjected to accepted pretreatments differing in the individual cases to exclude contamination.
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  • 61
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    Unknown
    Cambridge University Press
    Publication Date: 1967-01-01
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  • 62
    Publication Date: 1967-01-01
    Description: The following list covers some old measurements not included in previous lists and most of the samples measured at the Uppsala C14 laboratory since the last list (Uppsala V) except for all of the samples utilized for determining the increase of the C14/G12 ratio due to explosion of nuclear devices, and except for more than twenty samples measured for testing, storing, and pretreatment of Foraminifera
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  • 63
    Publication Date: 1967-01-01
    Description: This list reports routine measurements made at this laboratory since the preparation of Texas IV. Samples numbered through Tx-309 were counted under the supervision of Pearson, who left the laboratory early in 1966. Valastro, Associate Director since August, 1966, is responsible for samples beginning with Tx-310. Laboratory administration and sample screening have been handled by Davis, M. A. Tamers, formerly Director, resigned in 1966.
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  • 64
    Publication Date: 1967-01-01
    Description: This paper is a direct continuation of Stockholm VI. The bone samples analyzed and published in this list are treated according to a method, modified (Sellstedt, Engstrand and Gejvall, 1966) and described by Berger, Horney and Libby (1964).
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  • 65
    Publication Date: 1967-01-01
    Description: The following list of dates has been obtained since the compilation of List II in December 1965. Procedures of measurement are essentially unchanged from those reported previously (SR I and SR II).
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  • 66
    Publication Date: 1967-01-01
    Description: A radiocarbon laboratory has been set up to assist with the Pleistocene research undertaken in the Geology Department at Birmingham and has been designed for the measurement of ages of geological material up to at least 50,000 yr old. Construction began in May, 1965 and routine dating commenced in October, 1966. This is carried out using a CH4 proportional counter.
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  • 67
    Publication Date: 1967-01-01
    Description: The dates reported here represent a portion of those determined in 1966, The Radiocarbon Dating Laboratory of the Instituto Venezolano de Investigaciones Científicas carries out a synthesis of benzene for each sample and detects the activity with a liquid scintillation spectrometer. For routine measurements, 3 cc synthesized benzene and 1 cc commercial toluene, with PPO and dimethyl-POPOP scintillators, are used in a special small counting vial. The modern standard is 95% of the NBS oxalic acid, which gives a net modern count rate of 23.9 cpm. The background is now 8.5 cpm.
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  • 68
    Publication Date: 1967-01-01
    Description: This date list covers a selection of C14 results of archaeologic, hydrologic and speleologic samples that have been investigated in the period from March 1963 until July 1966. Dates of geologic samples will be presented in the following list.
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  • 69
    Publication Date: 1967-01-01
    Description: The C14 measurements reported here were made in this laboratory between November 15, 1965 and June 15, 1966. Sample descriptions are classified as follows: I.Geochemical SamplesII.Geologic-Paleoclimatic SamplesIII.Early Man-Alluvial Stratigraphy SamplesIV.Archaeologic Samples
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  • 70
    Publication Date: 1967-01-01
    Description: This list is a compilation of samples dated since September, 1965. It includes a continuation of several series begun in FSU I as well as new series undertaken since that time.
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  • 71
    Publication Date: 1967-01-01
    Description: This date list consists of some of the samples measured since summer 1965. For the routine measurements the same technique and equipment as described earlier was used (Bern IV).
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  • 72
    Publication Date: 1967-01-01
    Description: This list of dates is a continuation of Gakushuin V. Instruments and techniques are essentially the same as those used for Gakushuin III, IV and V.
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  • 73
    Publication Date: 1967-01-01
    Description: In late 1962 the old radiocarbon laboratory in Groningen was demolished and new dating equipment was erected in an underground cellar specially built for the purpose.
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  • 74
    Publication Date: 1967-11-09
    Description: Townsend's (1961) hypothesis that the turbulent motion in the inner region of a boundary layer consists of (i) an ‘active’ part which produces the shear stress τ and whose statistical properties are universal functions of τ and y, and (ii) an ‘inactive’ and effectively irrotational part determined by the turbulence in the outer layer, is supported in the present paper by measurements of frequency spectra in a strongly retarded boundary layer, in which the ‘inactive’ motion is particularly intense. The only noticeable effect of the inactive motion is an increased dissipation of kinetic energy into heat in the viscous sublayer, supplied by turbulent energy diffusion from the outer layer towards the surface. The required diffusion is of the right order of magnitude to explain the non-universal values of the triple products measured near the surface, which can therefore be reconciled with universality of the ‘active’ motion.Dimensional analysis shows that the contribution of the ‘active’ inner layer motion to the one-dimensional wave-number spectrum of the surface pressure fluctuations varies as τ2w/k1 up to a wave-number inversely proportional to the thickness of the viscous sublayer. This result is strongly supported by the recent measurements of Hodgson (1967), made with a much smaller ratio of microphone diameter to boundary-layer thickness than has been achieved previously. The disagreement of the result with most other measurements is attributed to inadequate transducer resolution in the other experiments.
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  • 75
    Publication Date: 1967-11-09
    Description: The fluid is assumed to be inviscid and to be confined within two parallel planes, each perpendicular to the axis of rotation. A sphere is set moving, relative to the rotating fluid, in a straight line with uniform velocity and the temporal development of the flow structure examined. It is found that ultimately the flow has different properties inside and outside the cylinder [Cscr ], circumscribing the sphere and having its generators parallel to the axis of rotation. Inside [Cscr ] the fluid moves with the sphere as if solid; in early experiments of Taylor (1923) this phenomenon was observed. Outside [Cscr ] the motion is a two-dimensional potential flow past [Cscr ] as if it were solid. Then the asymmetry observed by Taylor and predicted in an earlier theory of the author for an unbounded fluid (1953) is not borne out. A partial explanation is offered.
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  • 76
    Publication Date: 1967-11-09
    Description: An analysis is described for convection from a circular cylinder subjected to transverse oscillations relative to the fluid in which it is immersed. The analysis is based upon use of the acoustic streaming flow field. It is assumed that the frequency involved is sufficiently small that the acoustic wavelength in the fluid is much larger than the cylinder diameter, and that there is no externally imposed mean flow across or along the cylinder. Solutions are presented which are appropriate for a wide range of Prandtl number, and the cases of small and of large streaming Reynolds number are distinguished. The analysis compares favourably with experiments when the influence of natural convection is small.
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  • 77
    Publication Date: 1967-11-09
    Description: The two-dimensional internal wave pattern produced by a small disturbance moving with constant velocity along a line of arbitrary inclination in an inviscid, density stratified liquid is studied. It is shown how the far field wave pattern evolves as the inclination changes from the extreme of horizontal motion to that of vertical motion. It is found that, in general, waves propagate ahead of the disturbance.
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  • 78
    Publication Date: 1967-11-09
    Description: The paper deals with the regular refraction of a plane shock at a gas interface for the particular case where the reflected wave is an expansion fan. Numerical results are presented for the air–CH4 and air–CO2 gas combinations which are respectively examples of ‘slow–fast’ and ‘fast–slow’ refractions. It is found that a previously unreported condition exists in which the reflected wave solutions may be multi-valued. The hodograph mapping theory predicts a new type of regular–irregular transition for a refraction in this condition. The continuous expansion wave type of irregular refraction is also examined. The existence of this wave system is found to depend on the flow being self-similar. By contrast the expansion wave becomes centred when the flow becomes steady. Transitions within the ordered set of regular solutions are examined and it is shown that they may be either continuous or discontinuous. The continuous types appear to be associated with fixed boundaries and the discontinuous types with movable boundaries. Finally, a number of almost linear relations between the wave strengths are noted.
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  • 79
    Publication Date: 1967-10-17
    Description: A largely qualitative experimental investigation has been made of cellular convection patterns produced by the instability of a horizontal layer of fluid heated uniformly throughout its body and cooled from above. The fluid was aqueous zinc sulphate solution, and the heating was produced by an electrolytic current. The flow was visualized and photographed using polystyrene beads which, because of a differential expansion, came out of suspension in regions where the fluid was hotter or colder than average.The development of the cellular patterns as the Rayleigh number (a modified form) was varied was in many respects similar to that for Bénard convection. There were, however, two striking differences. First, the fluid descended in the centres of the cells and ascended at the peripheries; this was probably associated with the asymmetry between the heating and cooling. Secondly, and more surprisingly, the horizontal scale of the convection patterns was unusually large (except at the lowest Rayleigh numbers); the distance between rising and falling currents was observed to reach typically five times the depth of the layer.This last observation may be relevant to theories of convection within the Earth's mantle, to mesoscale convection in the atmosphere, and to patterns formed in ice.
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  • 80
    Publication Date: 1967-12-22
    Description: The acoustic streaming of an idealized elastico-viscous fluid near a cylindrical obstacle is considered using the boundary-layer type of approximation. It is shown that this streaming phenomena can be greatly influenced by the presence of elasticity in the fluid.
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  • 81
    Publication Date: 1967-10-17
    Description: The one-dimensional problem of shock-wave reflexion with relaxation is treated numerically by combining the shock-wave, characteristic, and Rayleigh-line equations. The theoretical results are compared with pressure and density measurements in CO2, and the agreement is found to be excellent.
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  • 82
    Publication Date: 1967-11-29
    Description: In a rotating system, the vertical transport of angular momentum by internal gravity waves is independent of height, except at critical levels where the Doppler-shifted wave frequency is equal to plus or minus the Coriolis frequency. If slow rotation is ignored in studying the propagation of internal gravity waves through shear flows, the resulting solutions are in error only at levels where the Doppler-shifted and Coriolis frequencies are comparable.
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  • 83
    Publication Date: 1967-11-29
    Description: Most suspensions exhibit a rheological behaviour which cannot be represented by either Bingham's or Ostwald–De Waele's law. In studying such cases a very simple expression with only three parameters may be used. Starting with an intermediate law of this sort, this paper gives velocity profiles and head losses in laminar flow, which have been computed and plotted on diagrams in non-dimensional co-ordinates.It has been found that transition flow rates in circular tubes for data taken from the literature and from experiments conducted on drilling muds at the Institut Français du Pétrole, are efficiently predicted by an empirical criterion (Ryan & Johnson 1959) which establishes a relation between a generalized Reynolds number and a generalized Hedström number.
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  • 84
    Publication Date: 1967-11-29
    Description: The velocities and the associated pressure gradients of infinitely long liquid-borne cylinders flowing freely in pipes are related analytically to their radial positions. These velocities and pressure gradients are compared with those of liquids in cylinder-free pipes and expressed as ratios. A digital computer was used to evaluate the resultant equations for values of the cylinder/pipe diameter ratio between 0·25 and 0·97, with radial positions varying from the fully eccentric to the fully concentric position. As the clearance between the pipe and the bottom of the cylinder increases, the pressure ratio (RP) decreases and the velocity ratio (RV) increases. The relationship between RP and RV is independent of liquid viscosity and density, capsule density and pipe diameter, and is shown to be nearly linear for the larger diameter ratios. The R, R relationships are compared with data from three experimental capsule pipelines with pipe diameters from ½ to 4 in., involving a variety of diameter ratios, cylinder lengths and densities, and oil viscosities. The experimental results for single capsules of finite length are shown to be in close agreement with the predictions for infinitely long cylinders.The relevance of the analysis to capsule pipelining is indicated by relating experimental values of capsule velocity over a wide range of densities to the theoretical clearance of the capsules. A general relationship of this type would permit the optimization of the power requirements of any particular throughput of a given commodity.
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  • 85
    Publication Date: 1967-11-29
    Description: The linear stability of a quiescent, three-dimensional rectangular box of fluid heated from below is considered. It is found that finite rolls (cells with two non-zero velocity components dependent on all three spatial variables) with axes parallel to the shorter side are predicted. When the depth is the shortest dimension, the cross-sections of these finite rolls are near-square, but otherwise (in wafer-shaped boxes) narrower cells appear. The value of the critical Rayleigh number and preferred wave-number (number of finite rolls) for a given size box is determined for boxes with horizontal dimensions h, ¼ ≤ h/d ≤ 6, where d is the depth.
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  • 86
    Publication Date: 1967-08-11
    Description: A theory is developed to determine the shape of water-bells. The motion of the gas induced by the moving walls is taken into account in this analysis. A rapidly converging iterative procedure leads to a theoretical shape which agrees well with the experimental shape of the water-bell.
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  • 87
    Publication Date: 1967-08-11
    Description: A theoretical study is made of a simple design for an underwater shock gun, which consists of a chamber in the form of a hollow circular cone, with a spherical sector of explosive charge fitted into the apex. When the explosive is initiated at the apex, the resulting sector of a spherical blast wave will be diffracted by expansion waves moving inwards after the leading shock has emerged from the rim of the cone.The progress of the expansion wave-fronts is calculated, and the results show a surprising inability of the diffraction process to ‘eat into’ the full-strength sector of spherical blast. It is found to be possible to design such a gun so that it is capable of projecting a high intensity shock-pressure beam over a considerable range, using only a very small explosive charge.
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  • 88
    Publication Date: 1967-08-11
    Description: We consider, in this paper, boundary-layer flows which are induced when an isothermal rigid-body rotation is disturbed by heating the fluid. The basic rigid-body rotation is sustained by one or more rotating planes at which the temperature differences are initiated. Conditions of both uniform and unsteady heating are discussed.
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  • 89
    Publication Date: 1967-07-18
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  • 90
    Publication Date: 1967-07-18
    Description: We consider here the higher order effect of moderate longitudinal surface curvature on steady, two-dimensional, incompressible laminar boundary layers. The basic partial differential equations for the problem, derived by the method of matched asymptotic expansions, are found to possess similarity solutions for a family of surface curvatures and pressure gradients. The similarity equations obtained by this anaylsis have been solved numerically on a computer, and show a definite decrease in skin friction when the surface has convex curvature in all cases including zero pressure gradient. Typical velocity profiles and some relevant boundary-layer characteristics are tabulated, and a critical comparison with previous work is given.
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  • 91
    Publication Date: 1967-07-18
    Description: A homogeneous fluid of viscosityvis confined between two co-axial disks (vertical separationH) which rotate relative to a rotating system (angular velocity Ω). The resulting velocity field is studied for values of the parameterv/2ΩH2in the range 1·6 × 10−2to 1·8 × 10−3. The Rossby number, defined as the ratio of the relative angular velocity of the disks to the angular velocity of the system, ranged from 0·038 to 0·0041. The dependence of the resulting velocity field (interior and boundary-layer flow) on geometrical parameters, imposed surface and bottom velocities, and Ω, is in good agreement with the calculations of Stewartson and Carrier. In particular, when the two disks rotate with the same angular velocity, the width of the vertical shear layer at the edge of the disks is found to be proportional to Ω−0·25±0·02. When the disks rotate in opposite senses, a shear layer in the vertical velocity is observed which transports fluid from one disk to the other and whose width is proportional to Ω−0·40±0·10. The magnitude and shape of the observed vertical velocity is in fair agreement with a numerical integration of the theoretical results.
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  • 92
    Publication Date: 1967-10-17
    Description: A shallow layer of silicone oil on a plane, circular copper plate was uniformly heated from below. The air on its surface was kept at constant temperature by a uniformly cooled glass plate close to the oil, which at the same time inhibited air motions. Motions began with concentric circular rolls which, after the centre ring had formed, broke down into a hexagonal pattern. A rather accurate determination of the wavelength of the motions was possible. The wavelength was found to be variable with the depth of the fluid layer in qualitative accordance with the theory of Nield. Supercritical motions are briefly discussed.
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  • 93
    Publication Date: 1967-10-17
    Description: Helmholtz stated and Korteweg proved that of all divergenceless velocity fields in a domain, with prescribed values on the boundary, the solution of the Stokes equation minimizes the rate of viscous energy dissipation. Hill & Power and also Kearsley proved the corresponding reciprocal maximum principle involving the stress tensor. We prove generalizations of both these principles to the flow of a liquid containing one or more solid bodies and drops of another liquid. The essential point in doing this is to take account of the motion of the solids or drops, which must be determined along with the flow. We illustrate the use of these principles by deducing several consequences from them. In particular we obtain upper and lower bounds on the effective coefficient of viscosity and a lower bound on the sedimentation velocity of suspensions of any concentration. The results involve the statistical properties of the distribution of suspended particles or drops. Graphs of the bounds are shown for special cases. For very low concentrations of spheres, both bounds on the effective viscosity coefficient are the same, and agree with the results of Einstein and Taylor.
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  • 94
    Publication Date: 1967-11-09
    Description: Drag reduction caused by dilute, distilled water solutions of five polyethylene oxides, molecular weights from 80,000 to 6,000,000, in turbulent pipe flow was studied experimentally in 0·292 and 3·21 cm ID pipes. It was found that the onset of drag reduction occurs at a well-defined wall shear stress related to the random-coiling effective diameter of the polymer. Laminar to turbulent transition is not, in general, delayed. The extent of drag reduction induced by a homologous series of polymers in a given pipe is a universal function of concentration, flow rate, and molecular weight. The maximum drag reduction possible is limited by an asymptote that is independent of polymer and pipe diameter. Flow structure measurements in a single polymer solution, 1000 ppm of molecular weight 690,000, showed that the mean flow follows an ‘effective slip’ model. In this, the mean velocity profile consists of a ‘Newtonian plug’ convected along at an additional, ‘effective slip’ velocity. The turbulent flow structure follows the ‘effective slip’ model towards the pipe wall, but is significantly different from Newtonian towards the pipe axis; in particular, the inertial subrange observed in isotropic Newtonian turbulence was absent in an energy spectrum taken on the pipe axis in the polymer solution.
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  • 95
    Publication Date: 1967-06-22
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  • 96
    Publication Date: 1967-06-22
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  • 97
    Publication Date: 1967-06-22
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  • 98
    Publication Date: 1967-05-01
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  • 99
    Publication Date: 1967-05-01
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  • 100
    Publication Date: 1967-08-11
    Description: The boundary-layer equations for the steady laminar flow of a vertical jet, including a buoyancy term caused by temperature differences, are solved by similarity methods. Two-dimensional and axisymmetric jets are treated. Exact solutions in closed form are found for certain values of the Prandtl number, and the velocity and temperature distribution for other Prandtl numbers are found by numerical integration.
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