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  • Wiley-Blackwell  (21,185)
  • PANGAEA
  • 1960-1964  (21,272)
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  • 1
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    PANGAEA
    In:  EPIC3Manchester Literay and Philosophical Society, Bremerhaven, PANGAEA, 106, pp. 22-45
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 2
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    PANGAEA
    In:  EPIC3Transactions of the Dumfriesshire ..., Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 3
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    PANGAEA
    In:  EPIC3Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 4
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    PANGAEA
    In:  EPIC3Ergänzungsheft Reihe A (8°), Nr. 5 zur Deutschen Hydrographischen Zeitschrift, Deutsches Hydrographisches Institut, Hamburg., Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 5
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    PANGAEA
    In:  EPIC3LUNDS UNIVERSITETS ÄRSSKRIFT. N.F. Avd. 2. Bd 59. Nr 7., Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 6
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    PANGAEA
    In:  Supplement to: Goodell, H G (1964): Eltanin Cruise 05 - Descriptions of cores, submarine photography and dredges. in Goodell, H.G., 1964. Marine geology of the Drake Passage, Scotia Sea, and South Sandwich Trench; USNS Eltanin marine geology cruises 1-8. Sedimentology Research Laboratory Contribution. Department of Geology, Florida State University, Tallahassee, Florida
    Publication Date: 2023-08-28
    Description: Cores, submarine photography and dredges described in this report were taken during the R/V Eltanin Cruise 5 in 1962 by the Department of Geology, Florida State University. Cores and dredges were recovered for 31 stations and are available at the Antarctic Research Facility, Florida State University for sampling and study.
    Keywords: Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge, rock; DRG_R; Elevation of event; ELT05; ELT05.001-MT; ELT05.001-TC; ELT05.002-PG; ELT05.004SS-RD; ELT05.005-PG; ELT05.009-PC; ELT05.009-TC; ELT05.010-TC; ELT05.011-PC; ELT05.012-PC; ELT05.014-PC; ELT05.015-RD; ELT05.016-RD; ELT05.017-RD; ELT05.028-PC; ELT05.029-PC; ELT05.031-PC; ELT05.10-C; ELT05.11-C; ELT05.17-C; ELT05.18-C; ELT05.20-C; ELT05.25-C; ELT05.27-C; ELT05.28-C; ELT05.29-C; ELT05.30-C; ELT05.9-C; Eltanin; Event label; GC; Grab; GRAB; Gravity corer; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Photo/Video; Piston corer; Position; PV; Quantity of deposit; Sample ID; Sediment type; Size; South Pacific Ocean; Substrate type; TRAWL; Trawl net; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 396 data points
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  • 7
    Publication Date: 2023-08-28
    Description: In May 1964 the Institute of Marine Science (University of Miami), Scripps Institution of Oceanography (University of California), Woods Hole Oceanographic Institution, and Lamont Geological Observatory (Columbia University) joined in the establishment of the JOINT OCEANOGRAPHIC INSTITUTIONS DEEP EARTH SAMPLING (JOIDES) program. The long range purpose of this organization is to obtain continuous core samples of the entire sedimentary column from the floors of the oceans. It was decided that initial efforts would be limited to water depths of less than 1000 fathoms (6000 feet), and tentative locations were selected for drilling operations off the eastern, western and Gulf coasts of the United States. Near the end of December 1964 it was found that the M/V Caldrill I, a drilling vessel capable of working to depths of 6000 feet, was to engage in drilling operations on the Grand Banks of Newfoundland during the summer of 1965 for the Pan American Petroleum Corporation. Thus it was agreed to organize a drilling program along the track of Caldrill between California and the Grand Banks. Selection was made of an area on the continental shelf and the Blake Plateau off Jacksonville, Florida. Based upon many previous geological and geophysical investigations by the participating laboratories, a considerable body of knowledge had been gained about this region of the continental-oceanic border. For this initial program of JOIDES, the Lamont Geological Observatory was chosen as the operating institution with J. L. Worzel as principal investigator, and C. L. Drake and H. A. Gibbon as program planners.
    Keywords: Blake Plateau, Atlantic Ocean; Caldrill I; Comment; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; JOID-6; JOIDES_prelim; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sample ID; Sediment type; Size; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 10 data points
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  • 8
    Publication Date: 2023-08-28
    Description: Cores, submarine photography and dredges described in this report were taken during the R/V Eltanin Cruise 6 in 1963 by the Department of Geology, Florida State University. Cores and dredges were recovered for 32 stations along with bottom photography and are available at the Antarctic Research Facility, Florida State University for sampling and study.
    Keywords: Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge, rock; DRG_R; ELT06; ELT06.003-BT; ELT06.003-MT; ELT06.004-BT; ELT06.005-RD; ELT06.006-PC; ELT06.006-RD; ELT06.007-BT; ELT06.007-MT; ELT06.007-PC; ELT06.007-RD; ELT06.007-TC; ELT06.009-B; ELT06.009-RD; ELT06.010-RD; ELT06.011-B; ELT06.011-PC; ELT06.012A-RD; ELT06.012-PC; ELT06.013-PC; ELT06.013-RD; ELT06.014-BT; ELT06.015-BT; ELT06.015-PC; ELT06.016-PC; ELT06.019-PH; ELT06.041-PH; ELT06.10-13C; ELT06.11-13C; ELT06.12-13C; ELT06.13-14C; ELT06.19-12C; ELT06.36-20C; ELT06.41-22C; ELT06.42-23C; ELT06.43-23C; ELT06.44-23C; Eltanin; Event label; File name; GC; Gravity corer; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Photo/Video; Piston corer; Position; PV; Quantity of deposit; Sediment type; Size; Southern Ocean; Substrate type; TC; TRAWL; Trawl net; Trigger corer; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 757 data points
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  • 9
    Publication Date: 2023-08-28
    Keywords: Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge, rock; DRG_R; ELT07; ELT07.001-RD; ELT07.002-MT; ELT07.007-BT; ELT07.008-BT; ELT07.014-PG; ELT07.016-PC; ELT07.016-RD; ELT07.017-PC; ELT07.017-RD; ELT07.018-PC; ELT07-12C; ELT07-13C; ELT07-14C; ELT07-16C; ELT07-20C; ELT07-22C; ELT07-3C; ELT07-5C; Eltanin; Event label; File name; Grab; GRAB; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Photo/Video; Piston corer; Position; PV; Quantity of deposit; Sediment type; Size; Southern Ocean; Substrate type; TRAWL; Trawl net; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 319 data points
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  • 10
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    PANGAEA
    In:  Antarctic Research Facility, Florida State University
    Publication Date: 2023-08-28
    Keywords: Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Elevation of event; ELT08; ELT08.007-PC; ELT08.011-PH; ELT08.012-PH; ELT08.013-PH; ELT08.015-PH; ELT08.016-PH; ELT08-12C; ELT08-14C; ELT08-19C; ELT08-1C; ELT08-2C; ELT08-4C; Eltanin; Event label; File name; GC; Gravity corer; Identification; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Photo/Video; Piston corer; Position; PV; Quantity of deposit; Sediment type; Size; Southern Ocean; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 144 data points
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  • 11
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    PANGAEA
    In:  Supplement to: Bouma, Arnold H; Marshall, N F (1964): A method for obtaining and analysing undisturbed oceanic sediment samples. Marine Geology, 2(1), 81-99, https://doi.org/10.1016/0025-3227(64)90028-3
    Publication Date: 2023-08-28
    Description: A German coring device (Reineck, 1958) has been improved to obtain oriented, undisturbed cores at any depth of water. The samples are rectangular in shape, 8 × 12 inches in plan and a maximum of 18 inches high. Good cores have been obtained from clayey material as well as from gravelly sand. No disturbances due to coring were observed on the collected samples. These large samples make it possible to conduct many varieties of investigations, such as study of living organisms and shear strength measurements, as soon as the sample is on deck of a ship; radiography on slices, peeling and impregnation techniques, granulometry, mineralogy, porosity, fossil content, etc. Construction and use of the box corer and applications of some of these analytical techniques are described.
    Keywords: BCR; Box corer (Reineck); Comment; Deposit type; DEPTH, sediment/rock; Description; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; SAN_JUAN_1963; Sediment type; SNJ-C8; Spencer F. Baird; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 7 data points
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  • 12
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    PANGAEA
    In:  Supplement to: Murata, K J; Erd, R C (1964): Composition of sediments from the experimental Mohole Project (Guadalupe Site). Journal of Sedimentary Research, 34(3), 633-655, https://doi.org/10.1306/74D7110E-2B21-11D7-8648000102C1865D
    Publication Date: 2023-08-28
    Description: Based on chemical, spectrographic and X-ray analyses, 34 samples from the experimental Mohole consist of variable proportions of calcite (0-60 percent), biogenic opal (0-50 percent), and normal lithogenous matter (14-97 percent) with an average of 20, 32, and 48 percent, respectively. Contamination with trachytic ash, rhyolitic ash, and saponite and dolomite occurring as alteration products of basaltic material affects the composition of a few samples. Magnesium, manganese, and phosphorus seem to have been derived from basaltic material also. The amounts of barium in the samples seems to be inversely related to sedimentation rates.
    Keywords: Comment; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Drillship_CUSS-I; Elevation of event; GC; Gravity corer; Latitude of event; Longitude of event; MOHO-1; MOHOLE_phase-1; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sample ID; Sampling/drilling; Sediment type
    Type: Dataset
    Format: text/tab-separated-values, 7 data points
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  • 13
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken on the DODO Expedition in May 1964 until December 1964 by the Scripps Institution of Oceanography from the R/V Argo. A total of 290 cores and dredges were recovered and are available at Scripps for sampling and study.
    Keywords: Argo; Comment; Core; CORE; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; DODO; DODO-006D; DODO-007D; DODO-008D; DODO-009D-1; DODO-009D-2; DODO-011D; DODO-012D; DODO-013D; DODO-014D; DODO-015D-1; DODO-015D-2; DODO-017PG; DODO-020C; DODO-025PG; DODO-026P; DODO-027P; DODO-027PG; DODO-031PG; DODO-048D; DODO-057P; DODO-060P; DODO-062D; DODO-065P; DODO-065PG; DODO-066DA; DODO-067P; DODO-070C; DODO-072P; DODO-075P; DODO-077G; DODO-084G; DODO-110P; DODO-112P; DODO-113D; DODO-114D; DODO-116D; DODO-123D; DODO-125D; DODO-127D; DODO-128D; DODO-129V; DODO-130G; DODO-132P; DODO-143D; DODO-232D; Dredge; DRG; Elevation of event; Event label; GC; Gravity corer; Indian Ocean; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Piston corer; Position; Quantity of deposit; Sample ID; Sediment type; Size; Solomon Sea; Substrate type; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 475 data points
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  • 14
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    PANGAEA
    In:  National Institute of Oceanography, Wormely | Supplement to: National Institute of Oceanography, Wormley (1964): International Indian Ocean Expedition, RRS Discovery Cruise 2 Report. Geology and Geophysics in N.W. Indian Ocean, 23 August to 4 December 1963. The Royal Society, London, 35 pp, https://www.bodc.ac.uk/resources/inventories/cruise_inventory/reports/d2.pdf
    Publication Date: 2023-08-28
    Description: This report gives a comprehensive general description of the scientific activities of Cruise 2 of R. R. S. 'Discovery'. These were largely geological and geophysical and were part of the British contribution to the International Indian Ocean Expedition. In addition to the thirteen geophysicists and geologists on board, there were five scientists involved in ocean chemistry, temperature measurements and ornithology making continuous observations - their accounts are also included. The report of a geological expediton ashore in the Seychelles is given in section 6.
    Keywords: D2; D5106; D5111; D5113; D5123; D5127; D5128; D5132; D5133; D5136; D5137; D5138; D5172; D5173; D5175; D5179; Deposit type; DEPTH, sediment/rock; Description; Discovery (1962); Dredge, rock; DRG_R; Elevation of event; Event label; Identification; Indian Ocean; 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; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 91 data points
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  • 15
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    PANGAEA
    In:  Supplement to: Arrhenius, Gustaf; Mero, John L; Korkisch, J (1964): Origin of oceanic manganese minerals. Science, 144(3615), 170-173, https://doi.org/10.1126/science.144.3615.170
    Publication Date: 2023-08-28
    Description: A criterion is suggested for discrimination between ferromanganese oxide minerals, deposited after the introduction of manganese and associated elements in sea water solution at submarine vulcanism, and minerals which are slowly formed from dilute solution, largely of continental origin. The simlultaneous injection of thorium into the ocean by submarine vulcanism is indicated, and its differentiation from continental thorium introduced into the ocean by runoff is discussed.
    Keywords: ALB-13; ALB-2; Albatross (1882-1921); Albatross1899-1900; Albatross1904-1905; ALBTR-13; ALBTR-2; ALBTR-4711; ALBTR-4721; Cobalt; Colorimetry; DEPTH, sediment/rock; DNWB0ABD; DOWNWIND-B1; DOWNWIND-H; Dredge; DRG; DWBD4; DWHD72; Event label; Horizon; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Optical spectrographic analysis; Pacific Ocean; Spencer F. Baird; Thorium
    Type: Dataset
    Format: text/tab-separated-values, 18 data points
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  • 16
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    PANGAEA
    In:  Supplement to: Menard, H William (1964): Manganese nodules (Chapter 8). In: Marine Geology of the Pacific. McGraw-Hill, New York, U.S.A., 171-190
    Publication Date: 2023-08-28
    Description: Prof. H. H. W. Menard has brought together nearly all that was known of the Pacific geology in the early 1960s. His book contains a particular chapter on manganese nodules giving a stimulating review of the features and processes known to govern their distribution and chemical composition.
    Keywords: Comment; Deposit type; DEPTH, sediment/rock; Description; Eastern Basin, Pacific Ocean; Eastern Mariana Basin, Pacific Ocean; Elevation of event; Event label; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northwestern Basin, Pacific Ocean; Pacific Ocean; Photo/Video; Position; PV; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; VITYAZ; Vityaz (ex-Mars); Vityaz-29; VITYAZ3630-PH; VITYAZ3632-PH; VITYAZ3644-PH; VITYAZ3844-PH; VITYAZ3846-PH; VITYAZ4239-PH; VITYAZ4249-PH; VITYAZ4261-PH; VITYAZ4265-PH; VITYAZ4273-PH; VITYAZ4279-PH; VITYAZ4285-PH
    Type: Dataset
    Format: text/tab-separated-values, 131 data points
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  • 17
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    PANGAEA
    In:  Institute of Oceanographic Sciences, Wormley
    Publication Date: 2023-08-28
    Description: This report gives a comprehensive general description of the scientific activities of Cruise 2 of R. R. S. 'Discovery'. These were largely geological and geophysical and were part of the British contribution to the International Indian Ocean Expedition. In addition to the thirteen geophysicists and geologists on board, there were five scientists involved in ocean chemistry, temperature measurements and ornithology making continuous observations - their accounts are also included. The report of a geological expediton ashore in the Seychelles is given in section 6.
    Keywords: D2; D5106; D5111; D5113; D5123; D5127; D5128; D5132; D5133; D5136; D5137; D5138; D5172; D5173; D5175; D5179; Deposit type; DEPTH, sediment/rock; Description; Discovery (1962); Dredge, rock; DRG_R; Event label; Identification; Indian Ocean; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Photo/Video; Position; PV; Quantity of deposit; Sediment type; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 95 data points
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  • 18
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    PANGAEA
    In:  Supplement to: Kaneps, A; Lair, C; Morgenstein, M (1964): R/V Robert Conrad Cruise 8 - Preliminary Megascopic Descriptions of Split Cores. Lamont Geological Observatory, Columbia University, New York, unpublished, 208
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken during the Robert Conrad Cruise 8 from November 1963 until August 1964 by the Lamont Geological Observatory, Columbia University from the R/V Robert Conrad. A total of 140 cores and dredges were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Keywords: Atlantic Ocean; Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge, rock; DRG_R; Elevation of event; Event label; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Quantity of deposit; RC08; RC08-100; RC08-102; RC08-103; RC08-106; RC08-107; RC08-109; RC08-11; RC08-110; RC08-112; RC08-113; RC08-114; RC08-116; RC08-12; RC08-120; RC08-125; RC08-126; RC08-128; RC08-129; RC08-12RD; RC08-130; RC08-135; RC08-137; RC08-14; RC08-140; RC08-141; RC08-143; RC08-144; RC08-145; RC08-147; RC08-148; RC08-15; RC08-16; RC08-19; RC08-20; RC08-21; RC08-25; RC08-26; RC08-27; RC08-31; RC08-32; RC08-34; RC08-35; RC08-36; RC08-37; RC08-38; RC08-39; RC08-42; RC08-43; RC08-44; RC08-45; RC08-48; RC08-49; RC08-4RD; RC08-5; RC08-50; RC08-53; RC08-55; RC08-6; RC08-63; RC08-67; RC08-69; RC08-70; RC08-71; RC08-72; RC08-73; RC08-75; RC08-7RD; RC08-8; RC08-80; RC08-81; RC08-82; RC08-83; RC08-84; RC08-85; RC08-86; RC08-87; RC08-88; RC08-89; RC08-8RD; RC08-90; RC08-94; RC08-97; RC08-98; RC08-99; RC08-9RD; Robert Conrad; Sample ID; Sediment type; Size; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 1616 data points
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  • 19
    Publication Date: 2023-08-28
    Keywords: Comment; Deposit type; DEPTH, sediment/rock; Description; Event label; GC; Gravity corer; Identification; Mariana Basin, Pacific Ocean; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northwestern Basin, Pacific Ocean; OKEAN; Okean Grab; Position; Quantity of deposit; Sediment type; Size; Substrate type; TRAWL; Trawl net; Visual description; VITYAZ; Vityaz (ex-Mars); Vityaz-25; Vityaz-29; VITYAZ3150-TR; VITYAZ3631-GR-1; VITYAZ3729-GC-1; VITYAZ3802-TR; VITYAZ3899-GR-1; VITYAZ3996-TR; VITYAZ4074-TR; VITYAZ4084-GR-1; VITYAZ4090-TR; VITYAZ4104-TR; VITYAZ4191-TR; VITYAZ4217-TR; VITYAZ4265-TR; VITYAZ4281-TR; VITYAZ4331-GR-1; VITYAZ4351-GR; VITYAZ4359-GR-1; VITYAZ4362-GR-1; VITYAZ4370-TR
    Type: Dataset
    Format: text/tab-separated-values, 149 data points
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  • 20
    Publication Date: 2023-08-28
    Keywords: Aluminium oxide; Calcium oxide; Cobalt oxide; DEPTH, sediment/rock; Description; DNWB0ABD; DOWNWIND-B1; Dredge; DRG; DWBD15; DWBD4; Event label; Identification; Iron oxide, Fe2O3; Loss on ignition; Magnesium oxide; Manganese oxide; Mariana Basin, Pacific Ocean; Nickel oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northwestern Basin, Pacific Ocean; OKEAN; Okean Grab; Oxygen; Pacific Ocean; Phosphorus pentoxide; Silicon dioxide; Spencer F. Baird; Titanium dioxide; TRAWL; Trawl net; VITYAZ; Vityaz (ex-Mars); Vityaz-29; VITYAZ3631-GR-1; VITYAZ3802-TR; VITYAZ3899-GR-1; VITYAZ3996-TR; VITYAZ4084-GR-1; VITYAZ4090-TR; VITYAZ4104-TR; VITYAZ4191-TR; VITYAZ4281-TR; VITYAZ4351-GR; VITYAZ4370-TR; Wet chemistry
    Type: Dataset
    Format: text/tab-separated-values, 252 data points
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  • 21
    Publication Date: 2023-08-28
    Keywords: Aluminium oxide; Barium oxide; Calcium oxide; Carbon dioxide; Cobalt oxide; Copper(II) oxide; DEPTH, sediment/rock; Description; DOWNWIND-H; Dredge; DRG; DWHD47; DWHD72; Event label; GC; Gravity corer; Horizon; Identification; Iron oxide, Fe2O3; Lead oxide; Magnesium oxide; Manganese dioxide; Manganese oxide; Nickel oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northwestern Basin, Pacific Ocean; OKEAN; Okean Grab; Pacific Ocean; Potassium oxide; Silicon dioxide; Sodium oxide; Titanium dioxide; TRAWL; Trawl net; VITYAZ; Vityaz (ex-Mars); Vityaz-25; Vityaz-29; VITYAZ3150-TR; VITYAZ3729-GC-1; VITYAZ4074-TR; VITYAZ4217-TR; VITYAZ4265-TR; VITYAZ4331-GR-1; VITYAZ4359-GR-1; VITYAZ4362-GR-1; Water in rock; Wet chemistry
    Type: Dataset
    Format: text/tab-separated-values, 212 data points
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  • 22
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    In:  Supplement to: Nayudu, Y Rammohanroy (1964): Palagonite tuffs (hyaloclastites) and the products of post-eruptive processes. Bulletin of Volcanology, 27(1), 391-410, https://doi.org/10.1007/BF02597539
    Publication Date: 2023-08-28
    Description: A synoptic review of the studies of well-known occurrences of palagonite tuffs is presented. Included are palagonite tuffs from Iceland, and pillow-lava palagonite complexes from Columbia River basalts and from the central Oregon coast. Additional petrologic and x-ray defraction data for selected samples are presented. Petrologic evidence shows that basaltic glass of aqueous tuffs and breccias consists of sideromelane, which is susceptible to palagonitization. It is shown that palagonitization is a selective alteration process, involving hydration, oxidation and zeolitization. Some of the manganese nodules dredged from the Pacific Ocean floor contain nucleus of palagonite-tuff breccias or of zeolite. A brief megascopic and microscopic description of nodules from the south Pacific, the Mendocino ridge and the 'Horizon' Nodule from the north Pacific is presented. Petrographic studies of palagonite-tuff breccias of manganese nodules and other palagonites suggest that migration and segregation of metallic elements occur during and subsequent to palagonitization. During the palagonitization of sideromelane, nearly 30 percent of sea water is absorbed. The hydration of sideromelane is also accompanied by oxidation of iron and other elements. These oxides may be released either in colloidal form or in true solution and tend to precipitate first from the unstable palagonite.
    Keywords: CHIN02BD; CHIN0ABD-002G; CHINOOK; CHNK-2G; Date/Time of event; DEPTH, sediment/rock; Description; DOWNWIND-H; Dredge; Dredge, chain bag; DRG; DRG_C; DWHD72; Elevation of event; Event label; FANB01BD; FANBD-25D; FANFARE-B; GC; Gravity corer; Horizon; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northern_Holiday; North-West Pacific Ocean; NTHL02HO-010PH; NTHL-10; Pacific Ocean; Sample code/label; Sample ID; Spencer F. Baird; Uniform resource locator/link to image; Wired profile sonde; WP
    Type: Dataset
    Format: text/tab-separated-values, 16 data points
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  • 23
    Publication Date: 2023-08-28
    Description: This collection of data on manganese nodules on the floor of the Pacific Ocean represents all the information that was available to the authors in May, 1964. It is compiled from both published references and original data. No attempt is made here to generalize or to speculate on the origin of the manganese or associated elements further discussion of these aspects of the subject may be had by reference to the literature.
    Keywords: ALB-13; ALB-173; ALB-31; Albatross (1882-1921); Albatross1899-1900; Albatross1904-1905; ALBTR-13; ALBTR-173; ALBTR-31; ALBTR-4660; ALBTR-4662; ALBTR-4676; ALBTR-4681; ALBTR-4685; ALBTR-4701; ALBTR-4711; ALBTR-4721; CARN_Revelle_46; CARN_Revelle_78; CARN7-150; CARN7-86; CARN-Cruise7; Carnegie; CASC-5D; CASCADIA; CHA-299; CHA-302; Challenger1872; CHIN02BD; CHIN02BD-016G; CHINOOK; CHNK-16G; CHUB01BD; CHUB01BD-002G; CHUB01BD-034G; CHUB-2; CHUB-34; CHUB5; CHUBASCO; Core; CORE; DNWB0ABD; DNWB0ABD-016G; DNWB0ABD-017G; DNWB0ABD-019G; DNWB0BBD; DNWB0BBD-037G; DNWB0BBD-040G; DNWB0BBD-043G; DNWB0BBD-048G; DNWB0BBD-052G; DNWB0BBD-054G; DNWB0BBD-055G; DNWB0BBD-056G; DNWB0DBD; DNWB0DBD-147GB; DNWH0AHO-004H; DNWH0BHO-034G; DNWH0DHO-092H; DOWNWIND-B1; DOWNWIND-B2; DOWNWIND-B4; DOWNWIND-H; Dredge; Dredge, rock; DRG; DRG_R; DWBD1; DWBD2; DWBD4; DWBD5; DWBD7; DWBG147B; DWBG16; DWBG17; DWBG19; DWBG37; DWBG40; DWBG43; DWBG48; DWBG52; DWBG54; DWBG55; DWBG56; DWBG78; DWHD15; DWHD16; DWHD47; DWHD55; DWHD72; DWHG34; DWHH4; DWHH92; Eastern Basin, Pacific Ocean; Epce; GC; Grab; GRAB; Gravity corer; H.M.S. Challenger (1872); Horizon; MDPC02HO-MP-025F-1; MDPC02HO-MP-033D; MDPC03HO-MP-043A; MIDPAC; MPC-25F-1; MPC-33D; MPC-43A; NAGA; NAGA8C; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North-East Pacific Ocean; Pacific Ocean; SIO-DX-1; Spencer F. Baird; Stranger; TRAWL; Trawl net; V15; V15-126; Vema; Vityaz (ex-Mars); Vityaz-29; VITYAZ4239-TR; VITYAZ4289-TR
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 24
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Skornyakova, Nadezhda S; Andrushchenko, Polina F; Fomina, Lidiya S (1964): Chemical composition of the Pacific ocean's iron-manganese concretions. Deep Sea Research and Oceanographic Abstracts, 11(1), 93-104, https://doi.org/10.1016/0011-7471(64)91086-1
    Publication Date: 2023-08-28
    Description: One the most interesting features of ocean sedimentation is the manganese formations on the surface of the ocean floor in some areas. These are especially widespread in the Pacific Ocean as concretions, grains, and crusts on rock fragments and bedrock outcrops. Iron-manganese concretions are the most abundant as they completely cover about 10% of the bottom of the Pacific Ocean where there are ore concentrations. The concretions occupy from 20-50% of the bottom and up to 80-90% on separate submarine rises. Such concretions are found in different types of bottom deposits, from abyssal red clays to terrigenous muds, but they occur most widely in red clays and quite often in carbonate muds. Their shape and their dimensions are very diverse and change from place to place, from station to station, varying from 0.5-20 cm. They may be oval, globular, reniform, or slaggy and often they are fiat or isometric concretions of an indefinite shape. The concretions generally have nuclei of pumice, basalt fragments, clayey and tuffaceous material, sharks' teeth, whale ossicles, and fossil sponges. Most concretions have concentric layers, combined with dendritic ramifications of iron and manganese oxides.
    Keywords: DNWB0ABD; DOWNWIND-B1; DOWNWIND-H; Dredge; DRG; DWBD15; DWBD4; DWHD47; DWHD72; GC; Gravity corer; Horizon; Mariana Basin, Pacific Ocean; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northwestern Basin, Pacific Ocean; OKEAN; Okean Grab; Pacific Ocean; Spencer F. Baird; TRAWL; Trawl net; VITYAZ; Vityaz (ex-Mars); Vityaz-25; Vityaz-29; VITYAZ3150-TR; VITYAZ3631-GR-1; VITYAZ3729-GC-1; VITYAZ3802-TR; VITYAZ3899-GR-1; VITYAZ3996-TR; VITYAZ4074-TR; VITYAZ4084-GR-1; VITYAZ4090-TR; VITYAZ4104-TR; VITYAZ4191-TR; VITYAZ4217-TR; VITYAZ4265-TR; VITYAZ4281-TR; VITYAZ4331-GR-1; VITYAZ4351-GR; VITYAZ4359-GR-1; VITYAZ4362-GR-1; VITYAZ4370-TR
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 25
    Publication Date: 2023-08-28
    Keywords: ALB-31; Albatross (1882-1921); Albatross1899-1900; ALBTR-31; Aluminium; Barium; Boron; Calcium; Calculated from weight/volume; CARN_Revelle_46; CARN_Revelle_78; CARN7-150; CARN7-86; CARN-Cruise7; Carnegie; CASC-5D; CASCADIA; Chromium; Cobalt; Copper; Core; CORE; DEPTH, sediment/rock; Description; DNWB0BBD; DNWB0BBD-037G; DNWH0AHO-004H; DOWNWIND-B2; DOWNWIND-H; Dredge; DRG; DWBG37; DWBG78; DWHD55; DWHH4; Epce; Event label; Gallium; GC; Gravity corer; Horizon; Identification; Iron; Lead; Magnesium; Manganese; Molybdenum; NAGA; NAGA8C; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North-East Pacific Ocean; Pacific Ocean; Phosphorus; Potassium; Sediment type; Shape; Silicon; SIO-DX-1; Size; Sodium; Spencer F. Baird; Stranger; Strontium; Sulfur, total; Thallium; Tin; Titanium; TRAWL; Trawl net; V15; V15-126; Vanadium; Vema; Vityaz (ex-Mars); Vityaz-29; VITYAZ4239-TR; Water content, wet mass; X-ray fluorescence (XRF); Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 257 data points
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  • 26
    Publication Date: 2023-08-28
    Keywords: ALB-13; ALB-173; ALB-31; Albatross (1882-1921); Albatross1899-1900; Albatross1904-1905; ALBTR-13; ALBTR-173; ALBTR-31; ALBTR-4660; ALBTR-4662; ALBTR-4676; ALBTR-4681; ALBTR-4685; ALBTR-4701; ALBTR-4711; ALBTR-4721; Aluminium; Atomic emission spectroscopy (AES); Barium; Bismuth; Boron; Cadmium; Calcium; Calculated from weight/volume; Calculated from weight loss after ignition at 450 °C; CARN_Revelle_46; CARN_Revelle_78; CARN7-150; CARN7-86; CARN-Cruise7; Carnegie; CASC-5D; CASCADIA; CHA-299; CHA-302; Challenger1872; CHIN02BD; CHIN02BD-016G; CHINOOK; CHNK-16G; Chromium; CHUB01BD; CHUB01BD-002G; CHUB01BD-034G; CHUB-2; CHUB-34; CHUB5; CHUBASCO; Cobalt; Copper; Core; CORE; DEPTH, sediment/rock; Description; DNWB0ABD; DNWB0ABD-016G; DNWB0ABD-017G; DNWB0ABD-019G; DNWB0BBD; DNWB0BBD-037G; DNWB0BBD-040G; DNWB0BBD-043G; DNWB0BBD-048G; DNWB0BBD-052G; DNWB0BBD-054G; DNWB0BBD-055G; DNWB0BBD-056G; DNWB0DBD; DNWB0DBD-147GB; DNWH0AHO-004H; DNWH0BHO-034G; DNWH0DHO-092H; DOWNWIND-B1; DOWNWIND-B2; DOWNWIND-B4; DOWNWIND-H; Dredge; Dredge, rock; DRG; DRG_R; DWBD1; DWBD2; DWBD4; DWBD5; DWBD7; DWBG147B; DWBG16; DWBG17; DWBG19; DWBG37; DWBG40; DWBG43; DWBG48; DWBG52; DWBG54; DWBG55; DWBG56; DWBG78; DWHD15; DWHD16; DWHD47; DWHD55; DWHD72; DWHG34; DWHH4; DWHH92; Eastern Basin, Pacific Ocean; Epce; Event label; Gallium; GC; Grab; GRAB; Gravity corer; H.M.S. Challenger (1872); Horizon; Identification; Iron; Lanthanum; Lead; Loss on ignition; Magnesium; Manganese; MDPC02HO-MP-025F-1; MDPC02HO-MP-033D; MDPC03HO-MP-043A; MIDPAC; Molybdenum; MPC-25F-1; MPC-33D; MPC-43A; NAGA; NAGA8C; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North-East Pacific Ocean; Pacific Ocean; Page(s); Phosphorus; Potassium; Sample code/label; Scandium; Sediment type; Shape; Silicon; Silver; SIO-DX-1; Size; Sodium; Spencer F. Baird; Stranger; Strontium; Thallium; Thorium; Titanium; TRAWL; Trawl net; Uranium; Vanadium; Vityaz (ex-Mars); Vityaz-29; VITYAZ4239-TR; VITYAZ4289-TR; Water content, wet mass; Ytterbium; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 1930 data points
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  • 27
    facet.materialart.
    Unknown
    PANGAEA
    In:  Scripps Institution of Oceanography, UC San Diego
    Publication Date: 2023-09-25
    Keywords: CARR2_2D; CARR2_4D; CARR2_5G; CARR2_6D; CARR2_9D; CARROUSEL2; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Event label; GC; Gravity corer; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sediment type; Spencer F. Baird; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 31 data points
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  • 28
    Publication Date: 2024-04-16
    Keywords: Aluminium; Barium; Calcium; Calculated from weight/volume; Cobalt; Copper; DEPTH, sediment/rock; Description; Dredge, rock; DRG_R; Event label; Horizon; Identification; Inductively coupled plasma atomic emission spectroscope (ICP-AES); Iron; Lead; Magnesium; Manganese; MDPC02HO-MP-025F-1; MDPC03HO-MP-043A; MIDPAC; Molybdenum; MPC-25F-1; MPC-43A; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Phosphorus; Potassium; Sediment type; Shape; Silicon; Sodium; Strontium; Titanium; TRAWL; Trawl net; Vityaz (ex-Mars); Vityaz-29; VITYAZ4239-TR; Water content, wet mass; X-ray fluorescence (XRF); Zinc
    Type: Dataset
    Format: text/tab-separated-values, 49 data points
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  • 29
    Electronic Resource
    Electronic Resource
    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964), S. 147-147 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
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  • 30
    Electronic Resource
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    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964), S. 149-154 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
    Notes: A method is presented for using an adiabatic reactor to study the kinetics of reactions of gases on solid catalysts. The method is based on measurement of the steady state axial profile of temperature or composition in a specially designed adiabatic packed bed reactor. Reaction rates are calculated from these measured profiles by graphical differentitation. The method is applicable for multireaction systems and for any type of kinetic behavior.The method was demonstrated by an experimental study of cumene cracking an silica-alumina catalyst at 420° to 480°C. The measured reaction rates are in satisfactory agreement with results obtained by other investigators who used isothermal reactors. Areas of application of the adiabatic method are suggested.
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  • 31
    Electronic Resource
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    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964), S. 290-425 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
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  • 32
    Electronic Resource
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    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964), S. 291-291 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
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  • 33
    Electronic Resource
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    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964), S. 430-430 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
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  • 34
    Electronic Resource
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    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964) 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
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  • 35
    Electronic Resource
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    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964), S. 595-597 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
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  • 36
    Electronic Resource
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    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964), S. 435-435 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
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  • 37
    Electronic Resource
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    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964), S. 445-447 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
    Additional Material: 5 Ill.
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  • 38
    Electronic Resource
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    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964), S. 460-465 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
    Notes: Solutions to the equations of multicomponent mass transfer may be written as matrix generalizations of the solution to the equivalent binary mass transfer equation when intial and boundary concentrations are constant, there are no homogeneous reactions, and all physical properties including the diffusion coefficient matrix are concentration independent.The analogue of the binary mass transfer coefficient is a multicomponent mass transfer coefficient matrix which depends only upon the mass transfer coefficients of the equivalent binary system and the diffusion coefficient matrix of the multicomponent system.When interphase transfer takes place, the inverse multicomponent mass transfer coefficient matrices of each phase are additive. Their sum yields an overall resistance to mass transfer which is the inverse of the overall multicomponent mass transfer coefficient matrix.
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  • 39
    Electronic Resource
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    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964), S. 135-137 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
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  • 40
    Electronic Resource
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    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964), S. 3-3 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
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  • 41
    Electronic Resource
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    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964), S. 26-30 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
    Additional Material: 2 Ill.
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  • 42
    Electronic Resource
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    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964), S. 30-34 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
    Additional Material: 12 Ill.
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  • 43
    Electronic Resource
    Electronic Resource
    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964) 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
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  • 44
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    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964), S. 785-785 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
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  • 45
    Electronic Resource
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    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964), S. 491-496 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
    Notes: An experimental investigation of the effects of various physical properties on the dispersedphase mass transfer coefficient was carried out for both nonoscillating and oscillating liquid droplets falling in a single stream through stationary continuous liquid phases. The Colburn and Welsh two-component technique was used to isolate and measure the disperesed-phase resistance to mass transfer. This technique limited the experimental study to systems with low interfacial tensions, between 2.5 and 5.8 dynes/cm. Solute was transferred into the droplets, and the droplet concentration was measured after droplet-fall heights ranging from about 2 cm. to 103 cm. Precautions were taken to minimize end effects.The experimental mass transfer rates on nonoscillating droplets in general were greater than that predicted by the Kronig and Brink model for nonoscillating circulating droplets. Experimental Sherwood numbers for four liquid systems were correlated in terms of a relationship involving the dispersed-phase Schmidt number, the Weber number, and the time group, 4DLtc/d2e, which allows for the time dependency of the transfer mechanism. The data were correlated with an average absolute deviation of 34%. The Kronig and Brink and Newman relations fitted the experimental data for nonoscillating droplets with an average absolute deviation of 46 and 54%, respectively. The experimental results for the oscillating droplets were correlated by two relationships with an average absolute deviation of 10.5%. The Handlos and Baron model fitted the experimental results for oscillating droplets with an average absolute deviation of 38%.
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  • 46
    Electronic Resource
    Electronic Resource
    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964), S. 502-508 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
    Notes: The inherent uncertainty of the critical heat flux in saturated pool boiling has been inconclusively debated for some time. In an effort to ascertain this uncertainty a series of 234 tests was conducted at atmospheric pressure with saturated water outside horizontal, a.c. heated, 0.234-in. O.D., A-nickel tubes in an open 6 × 6 × 9-in. deep pool. Approximately fifty tests were conducted with each of four test sections which were protected from physical burnout by a detector circuit which terminated the applied current before the wall temperature exceeded approximately 450°F. The maximum relative uncertainty in the derived values of critical heat flux was ±3%.For all the tests the minimum, average, and maximum critical fluxes were 0.201 × 106, 0.436 × 106, and 0.596 × 106 B.t.u./hr. sq. ft., respectively, and the average critical wall superheat was 41°F. The surface roughness of the test sections remained essentially unchanged during the program. The data show that there is an inherent uncertainty or scatter band in the critical heat flux under conditions of minimum surface variability, and that solely hydrodynamic theories of burnout do not fully represent the phenomenon, since surface condition can constitute a significant influence.
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  • 47
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    AIChE Journal 10 (1964), S. 530-534 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
    Additional Material: 5 Ill.
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  • 48
    Electronic Resource
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    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964), S. 968-981 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
    Additional Material: 10 Ill.
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  • 49
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    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964), S. 83-88 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
    Additional Material: 8 Ill.
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  • 50
    Electronic Resource
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    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964), S. 548-550 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
    Additional Material: 1 Tab.
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  • 51
    Electronic Resource
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    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964), S. 115-124 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
    Notes: Experimental studies were made of fog formation in free jets containing glycerine and dibutyl phthalate. Visual and photographic observations showed that condensation took place near the nozzle in the mixing zone between the jet and the ambient air. Fog formation began at a well-defined location downstream from the nozzle depending on the initial velocity, temperature, and concentration of vapor. The location could be changed by inserting solid bodies or by adding foreign nuclei to the mixing zone. Measurements were made of mean temperature and concentration profiles in the mixing zone with noncondensable gases. These compared well with the predictions of turbulent boundary-layer theory. Calculations were made of the supersaturation to be expected in the case of glycerine. Downstream of the point where condensation first occurred fog filled most of the region where the calculated supersaturation was above unity. Based on the experimental evidence a mechanism is proposed for condensation in a free jet.
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    AIChE Journal 10 (1964), S. 132-133 
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    AIChE Journal 10 (1964) 
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    AIChE Journal 10 (1964), S. 146-283 
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    AIChE Journal 10 (1964), S. 155-159 
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    AIChE Journal 10 (1964), S. 785-789 
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    AIChE Journal 10 (1964), S. 605-611 
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    Notes: This investigation was undertaken to obtain an analytical solution to the problem of predicting particle-to-fluid heat and mass transfer rates in multiparticle systems at low Reynolds numbers. The energy equation based on the free surface model was solved by expanding the fluid temperature distribution in even powers of the spherical angle and by assuming that the fluid properties remain relatively constant with temperature. Solutions were obtained for Peclet numbers between 0.1 and 100 and fractional void volumes between 0.4 and 1.0. They show that the average Nusselt or Sherwood number in a bed of particles is a function of both the fractional void volume and the Peclet number, the effect of Peclet number decreasing as the bed becomes more concentrated in the low Peclet number range. A plot of the results in terms of the j factor vs. the Reynolds number shows good agreement with published experimental mass and heat transfer data and indicates that the j factor is not independent of the Schmidt or Prandtl numbers at low Reynolds number, low Peclet number flow.
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    AIChE Journal 10 (1964), S. 617-620 
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    AIChE Journal 10 (1964), S. 625-631 
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    Notes: Generalized virial coefficients B*, C*, D*, and their derivatives have been established to satisfy experimental compressibility and Δuo, Δho data for spherically-symmetrical, nonpolar gases.
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    AIChE Journal 10 (1964), S. 631-639 
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    AIChE Journal 10 (1964), S. 645-651 
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    AIChE Journal 10 (1964), S. 656-660 
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    Notes: By using a special surface thermocouple Moore and Mesler have measured large temperature fluctuations during nucleate boiling of water on chromel P surface. They found that the temperature dropped 20° to 30°F. in about 2 msec. but required 10 to 20 msec. to recover. They have postulated that the surface was cooled during initial bubble growth by evaporation of a microlayer into the bubble. To test this hypothesis a technique was developed to photograph a bubble growing from an artificial site as the surface temperature was measured.Temperature fluctuations were recorded on an oscilloscope which automatically triggered the bubble photographs by means of a time delay unit and flash tube. Photographs of bubbles were taken at 1 μsec. exposure time and ranged from about 10 μsec. after the start of the temperature drop to about 1 msec. before the start of another cycle. The photographs show that the surface cools during bubble growth and recovers during bubble departure.
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    AIChE Journal 10 (1964), S. 804-809 
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    AIChE Journal 10 (1964), S. 260-265 
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    Notes: The point of inversion of a water-in-oil type of dispersion to an oil-in-water type is investigated for several water-oil systems by studying the volume ratios of the phases in relation to their physical properties. The point of inversion for each system of an immiscible organic liquid and water and organic liquid mixture and water is obtained by varying the phase-volume ratios and determining the type of dispersion after complete mixing. The effects of temprature, interfacial tension, and density are found to have no correlation generally applicable to the systems studied. A volume-viscosity relationship is found to exist within limits. This correlation is that the phase-volume ratio at the point of inversion is equal to the square root of the ratio of teh viscosities of the respective phases at the interface. The theoretical aspects of this relationship are studied along with its limitations.
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    AIChE Journal 10 (1964), S. 274-275 
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    AIChE Journal 10 (1964), S. 275-277 
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    AIChE Journal 10 (1964), S. 277-281 
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    AIChE Journal 10 (1964), S. 278-288 
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    AIChE Journal 10 (1964), S. 278-284 
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    Notes: Outline below is a method for simplification of the solution of diffusion problems involving irreversible first-order reactions. It permits writing the concentration profiles for reactive systems in terms of those for nonreactive systems of the same geometry and similar boundary conditions. The method is valid where fluid flow patterns and concentration boundary conditions are time independent and where the assumptions of constant density and mass diffusivity are acceptable. The useful results of this development are summarized in Equations (31) through (33) and represent a generalization of an earlier development by P. V. Danckwerts (1).
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    AIChE Journal 10 (1964), S. 293-297 
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    Notes: Constant pressure diffusion rates of hydrogen through Vycor porous glass were measured in nitrogen and neon systems. The experimental diffusivities are less than those predicted by the random pore model indicating that this model may not be satisfactory for a low porosity material such as Vycor. Interpreted in terms of an assembly of parallel pores the data suggest a tortuosity factor of approximately 2.4.Rate data for the ortho-para hydrogen reaction were also measured at -196°C. and 1 atm. The catalyst 2% nickel/Vycor was found to have pore properties (area, mean pore size, pore volume) similar to that of plain Vycor. Predicted effectiveness factors using the experimental diffusion data were in good agreement with values determined experimentally. The latter were evaluated from rate measurements on both pellet and particles (58 μ mean diameter).
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    AIChE Journal 10 (1964), S. 303-308 
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    Notes: Four different flow regimes may be identified during transport of dilute suspensions of solid particles through horizontal pipes by liquids in turbulent flow as the velocity is varied. The regimes may be characterized by the distribution of solids in the channel. In two of the regimes the bulk of the material is immediately adjacent to the bottom of the channel and is clumped up either into transverse waves (dunes or islands) with a reproducible periodicity or into longitudinal waves (long stria). The definition of the other two regimes is somewhat more arbitrary but may qualitatively be described as heterogeneous or homogeneous flow. Extensive studies of the conditions under which transverse and longitudinal waves occurred, when combined with results of previous studies, showed that all four of these flow regimes may be conveniently represented on a single diagram in which the terminal-settling velocity divided by the friction velocity and the Reynolds number on particle diameter and friction velocity are the coordinates. Because the particle Reynolds number based on the terminal-settling velocity can be uniquely defined as an additional parametre on such a diagram the particular flow behavior for any given combination of system and particle characteristics can be readily determined.
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    AIChE Journal 10 (1964), S. 309-315 
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    Notes: A computational method has been developed for obtaining the solution to a class of optimization problems by the combined use of the maximum principle and a maximum (or minimum) seeking technique on the analogue computer. Various maximum seeking techniques can be used for this method. However if the random search technique is used, this computational method has the advantage of being able to investigate a large number of operating (or controlling) variables.The calculation procedure is essentially a trial-and-error procedure which is alternately integration and maximum seeking operations. The variables over which the system is to be optimized are approximated by a finite number of straight line segments n. Thus the maximum (or minimum) of the Hamiltonian function which is obtained by the maximum principle need only be obtained at n + 1 points along the optimization path (or trajectory).To illustrate the use of the method the optimum operating variable profiles (or gradients) in a tubular chemical reactor were computed.The present method, in addition to making it easier to investigate systems with a moderate number of state variables, can be used to solve problems with almost any kind of constraints and performance index encountered in ordinary optimum design problems. It offers some possibilities for on-line optimizing control of a process. A special purpose analogue computer could be built for this use.
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    AIChE Journal 10 (1964), S. 323-329 
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    Notes: Velocity distributions, pressure gradients, and overall pressure drops are presented. A definite concavity was found in the velocity profile near the entrance for case I. In case II, which is more realistic physically, very definite effects are transmitted upstream, and the velocity distributions downstream show little concavity.
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    AIChE Journal 10 (1964), S. 330-339 
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    Notes: Significant changes in heat and momentum transfer rates can be caused by finite interfacial velocities and external field forces. This study considers the nonlinear problem of combined free and forced convection in vertical and horizontal two-dimensional conduits with finite transverse velocity.Similarity transformations for the temperature function have been found which reduce the energy, momentum, continuity, and state equations for these configurations to nonlinear systems of two coupled ordianary differential euqations. These equations are solved by approximate methods to give Nusselt numbers and friction factors as well as velocity and temperature profiles.Stream to wall temperature differences increase with suction and decrease with injection. The effects of interfacial velocity on temperature profiles and heat transfer increase dramatically with Prandtl number. Because blowing and suction strongly affect temperature profiles they substantially modify natural convection effects in vertical flows. Suction creates steeper transverse temperature gradients and accentuates buoyancy effects in vertical flows. Conversely injection flattens temperature profiles and thus decreases the influence of buoyancy on the velocity field.
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    AIChE Journal 10 (1964), S. 357-364 
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    AIChE Journal 10 (1964), S. 369-373 
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    AIChE Journal 10 (1964), S. 67-67 
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    AIChE Journal 10 (1964), S. 61-67 
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    Notes: The definition of filtration resistance is re-examined in view of the new theory (12) of the variation of flow rate with respect to distance through a filter cake. In the new definition it is shown that the filtration resistance depends upon slurry concentration as well as applied pressure. A correction factor modifying the specific filtration resistance previously defined by Ruth (5, 6) is developed.Where the hydraulic pressure variation within a cake is known, methods are presented for calculating the variation of flow rate with respect to distance and the change of filtration resistance in relation to slurry concentration.
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    AIChE Journal 10 (1964), S. 79-82 
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    AIChE Journal 10 (1964), S. 89-91 
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    AIChE Journal 10 (1964), S. 98-105 
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    AIChE Journal 10 (1964), S. 110-114 
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    AIChE Journal 10 (1964), S. 130-144 
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    AIChE Journal 10 (1964), S. 144-144 
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    AIChE Journal 10 (1964), S. 166-173 
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    AIChE Journal 10 (1964), S. 180-186 
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    Notes: Unusual heat transfer phenomena have been observed between solid surfaces and fluids near their thermodynamic critical point. To understand better these phenomena temperature and velocity profiles and local heat transfer coefficients were measured for turbulent flow of carbon dioxide in a tube at 1,075 lb/sq. in. abs. (pc = 1,071). The results indicate a severe flattening of the radial temperature profiles, a maximum in the velocity profile between the wall and the tube axis, and a maximum in h' when the bulk fluid temperature passes through the transposed critical temperature.The results can be explained qualitatively by considering the variation with temperature of thermal conductivity near the tube wall and specific heat in the turbulent core.
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    AIChE Journal 10 (1964), S. 194-197 
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    AIChE Journal 10 (1964), S. 202-205 
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    AIChE Journal 10 (1964), S. 220-221 
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    AIChE Journal 10 (1964), S. 238-245 
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    AIChE Journal 10 (1964), S. 266-269 
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    AIChE Journal 10 (1964), S. 274-274 
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    AIChE Journal 10 (1964), S. 269-273 
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    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
    Notes: A method is presented for solving the basic energy expression for the temperature distribution for turbulent heat transfer in a circular conduit with a digital computer. The method assumes a knowledge of the velocity distribution, the eddy conductivity term as a function of the radial position, and a constant wall temperature. For illustrative purposes only a dimensionless expression is derived from Reichardt's relationship which gives the eddy conductivity term as a function of radial position with Reynolds and Prandtl numbers as parameters.Incorporated in the computer program is Richardson's three-point extrapolation formula which permits the determination of a more accurate eigenvalue from three previously computed values which were obtained by using three different values of the reduced radial increment. Agreement with the Crank-Nicholson method is quite good, although the method with eigenvalues is considered to be superior. Eigenvalues determined from the analytical solution of the energy expression for the laminar flow case and those computed by the numerical method are in excellent agreement. This is indicative of the accuracy and reliability of the proposed numerical method.
    Additional Material: 5 Ill.
    Type of Medium: Electronic Resource
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  • 97
    Electronic Resource
    Electronic Resource
    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964) 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
    Type of Medium: Electronic Resource
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  • 98
    Electronic Resource
    Electronic Resource
    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964), S. 298-302 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
    Additional Material: 5 Ill.
    Type of Medium: Electronic Resource
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  • 99
    Electronic Resource
    Electronic Resource
    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964), S. 517-523 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
    Notes: In the absence of turbulent fluctuations the main effect of a velocity gradient on the floc properties is a rearrangement of particles within the floc producing a more dense floc structure. When the suspension is sufficiently dilute that floc-floc collisions are negligible, the limits on the floc diameter are (1 + α)5/3 〈 (Df/Dp) ≤ (1 + α)2, where α is the ratio of the volume of fluid immobilized in the floc structure to volume of solids in the floc structure as determined from hindred-settling measurements. These results set an upper limit on the floc size.Under turbulent flow conditions the principle mechanism leading to floc rupture is pressure differences on opposite sides of the floc which cause bulgy deformation and rupture. The breakup of the floc is resisted by the yield stress τy and is promoted by an increase in the energy dissipation per unit mass of fluid ∊. Because the energy dissipation per unit mass is at a maximum near the pipe wall, the floc size is at a minimum in this same region.By application of the concepts of local isotropy, the floc size is found to be proportional to (τy9/∊5)1/2once the turbulent intensity is sufficient to overcome the yield stress. In the wall region the floc diameter is proportional to (du/dr)3 (τy9/∊8)1/2.
    Additional Material: 4 Ill.
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  • 100
    Electronic Resource
    Electronic Resource
    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 10 (1964), S. 524-529 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
    Notes: The purpose of this study was to develop the use of semibatch operation of a recirculation reactor in kinetic studies. Ethylene hydrogenation over a supported copper catalyst was studied experimentally. In semibatch operation one of the reactants is fed at the rate necessary to hold the total pressure in the reactor constant. In ethvlene hydrogenation the reaction rate is directly equal to the feed rate, and the kinetics can be studied at constant partial pressure of either of the reactants. Since ethane is inert, this technique permitted the study of reaction rate as a function of one variable at a time.Although ethylene hydrogenation has been studied extensively, there is not general agreement regarding the kinetics over a copper catalyst. The results are themselves of interest because they indicate the reasons for the apparently conflicting data in the literature.
    Additional Material: 6 Ill.
    Type of Medium: Electronic Resource
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