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  • 1
    Publication Date: 2017-04-03
    Description: (extended abstract)
    Description: INGV, Regione Sicilia, Ministero Sviluppo Economico
    Description: Published
    Description: Ettore Majorana Foundation and Centre for Scientific Culture, Erice, Sicily
    Description: 5.9. Formazione e informazione
    Description: open
    Keywords: Inertia ; Physics ; Fluid Dynamics ; 05. General::05.03. Educational, History of Science, Public Issues::05.03.99. General or miscellaneous ; 05. General::05.05. Mathematical geophysics::05.05.99. General or miscellaneous ; 05. General::05.09. Miscellaneous::05.09.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Extended abstract
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  • 2
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-25
    Description: The second half of CHAIN Cruise #11, 22 February until 22 March, 1960, is detailed as to type of measurements made with their specific locations. The cruise areas were in the St. Croix region, the Puerto' Rico Trench and the tracks from the Bahamas to Bermuda to Woods Hole. Camera lowerings, lowerings of the thermal probe and accompanying cores, dredging, sound velocimeter lowerings, and acoustic studies of the scattering layer were the special events undertaken while precision bathymetry and towing of the Continuous Temperature Recording Chain were on a watch standing basis.
    Description: Undersea Warfare Branch, Office of Naval Research Under Contract Nonr- 1367(00) (NR- 261-10 2)
    Keywords: Underwater photography ; Submarine topography ; Marine sediments
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 3
    Publication Date: 2022-05-25
    Description: The purpose of this data file, which has been modelled after Hathaway (1971), is to make available most of the basic data that was collected as part of Woods Hole Oceanographic Institution's study of New Bedford Harbor. The New Bedford Harbor project, which was jointly funded by the Office of Sea Grant and Woods Hole, was designed to examine the past and present patterns of dispersal and accumulation of fine-grained sediments and waste materials in New Bedford Harbor and its approaches.
    Description: Prepared for the Department of Commerce, National Oceanic and Atmospheric Administration, Office of Sea Grant under Contract 04-6-158-44016 and 04-6-158-44106.
    Keywords: Estuarine sediments ; Estuarine pollution ; Marine sediments ; Sedimentation analysis ; Factory and trade waste ; Sewage disposal ; Water quality
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 4
    Publication Date: 2022-05-26
    Description: Originally issued as Reference No. 68-4, series later renamed WHOI-.
    Description: In February-March 1965, a series of piston cores were taken aboard ATLANTIS II off the coast of Arabia, Pakistan, and India (Figure 1) in water depths of about 3,000 meters. The principal objectives of this program were (a ) to obtain information on the change in petrology of the sediments as a function of geography and depth (b) to study the microfauna in the sediment profiles, and (c) to apply geochemical tools for the elucidation of the diagenetic fate of the organic matter and the history of the sediments. This article presents data on the geochemical part of the project. Principally, we are concerned with the oxygen and carbon isotope distribution in carbonates, the carbon isotope composition of sedimentary organic matter, and the amino acid composition of the sediment material. These studies represent a part of a larger program at our Institute which is concerned with the distribution of (a) stable isotopes and (b) organic compounds such as amino acids, carbohydrates, or hydrocarbons in recent and ancient sediments, natural waters, and marine organisms.
    Description: National Science Foundation under Grant GP-4904
    Keywords: International Indian Ocean Expedition (1960-1965) ; Atlantis II (Ship : 1963-) Cruise AII15 ; Marine sediments ; Amino acids
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 5
    Publication Date: 2022-05-26
    Keywords: Marine sediments ; Corrosion and anti-corrosives
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 6
    Publication Date: 2022-05-26
    Description: The objective of this investigation was to measure bottom loss in normal incident reflection of pulses of twelve kcps sound and to study its geological significance. To this end a semi-automatic instrument system was developed which is capable of making continuous measurements of the peak pressure and the time integral of the square of the pressure of the sea floor echo, from a vessel underway. Observations were taken in both deep and shallow water areas in the Western North Atlantic. The early cruises were conducted in deep water to investigate the range and variability of bottom loss values. Geological control consisted mainly of a precise bathymetric record. The later cruises were conducted in shall ow water, in areas where the geology has been well studied previously by investigators using techniques of classical geology. In these latter cruises the acoustic measurements were correlated with a schedule of sediment dredging and underwater photography. Thirty-one thousand acoustic measurements were made. Median bottom loss values and standard deviations were computed and the results summarized in eleven hundred sets, each set corresponding to a location at sea. Seventy-seven sediment stations were occupied. A complete particle size analysis and a water content analysis were performed on these sediments to determine their size and mass characteristics . The size characteristics included the median grain size, the sorting coefficient, and the percentages of gravel, sand, silt, and clay. A sediment class name was determined from the gravel, sand, silt, and clay percentages according to the Shepard system of classification. The mass characteristics included porosity, bulk density, sound velocity, acoustic impedance, Rayleigh reflection coefficient, and theoretical bottom loss. The combined results show a good correlation between measurements of bottom loss and both mass and size characteristics of the sediment. The measured bottom loss increases as the porosity increases. The measured bottom loss also increases as the silt-clay percentage increases since the porosity of sediments generally increases as this fraction increases. It seems that the Rayleigh reflection coefficient can be used to predict acoustic bottom loss at normal incidence. Conversely, normally-incident bottom loss can be used under the assumption of a Rayleigh reflection process to determine the nature of the bottom sediment. The acoustical and geological results have been made available in tabulations, scatter diagrams, and as geographical plots. Except for the initial measurements, all operations, including the final displays, were accomplished through automatic digital processing machines.
    Description: The Office of Naval Research under Contract Nonr-4029 ~ Nonr-13 67~ Nonr-1841 (74) ~ NR 083 -15 7~ and the Bureau of Ships under Contracts NObsr-72521 and NObsr-89464.
    Keywords: Marine sediments ; Ocean bottom ; Underwater acoustics--Instruments
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 7
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: Submitted in partial fulfillment of the requirements for the degree of Doctor of Science at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution.
    Description: The first of two sets of data reported here, measured over two-dimensional immobile current ripples, comprises skin-friction time series at four streamwise positions and velocity profiles measured to within a few mm of the bed. The velocity profiles cannot be linked to the local mean skin friction through the law of the wall, so they do not represent an internal boundary layer growing downstream of reattachment. Rather the velocity field is the sum of a spatially averaged rotational profile and a locally inviscid perturbation. Normalized skin-friction spectra are independent of position, but skin-friction probabilty density functions show strong increases in skewness and kurtosis near reattachment. The second set of data comprises measurements of the skin-friction vector field around isolated hemispheres with and without model sedimentary tails, and skinfriction and velocity measurements on arrays of hemispheres with and without tails. The skin-friction field around an isolated hemisphere is not consistent with formation of growth of a sedimentary tail more than about two obstacle heights long. The skin-friction field in a hemisphere array of areal density 0.02 is significantly distorted from the isolated-element case, and the roughness length in arrays of two areal densities is not altered by addition of tails.
    Description: Funding was provided by the National Science Foundation under Grant aCE 77-20437 and by the Office of Naval Research under Contract N00014-80-C-0273.
    Keywords: Current ripples ; Skin-friction patterns ; Sedimentary tails ; Roughness length ; Rough turbulent boundary layers ; Ocean bottom ; Marine sediments ; Frictional resistance (Hydrodynamics)
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report , Thesis
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  • 8
    Publication Date: 2022-05-26
    Description: An investigation of the release of Ni-63, Co-60, and Fe-55 from Inconel 600 and 347SS stainless steel specimens implanted in marine sediment for one year is described. Radiochemical analysis of the sediment from overcores of the metal specimens permits estimation of integrated activities, release rates, and diffusion coefficients of the three radionuclides. Disturbance of the sediment upon recovery limits the values to order of magnitude estimates. The redox chemistry of the sediments is characterized by measurement of several naturally occurring oxidizing agents and is correlated with the behavior of the radionuclides. Details of the deployment, sampling and analytical procedures are also given.
    Keywords: Marine sediments ; Corrosion and anti-corrosives ; Metals
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 9
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: A listing of high southern latitude (〉30° S) pre-Pleistocene sediment cores is given for samples obtained by the coring and drilling programs of the Lamont-Doherty Geological Observatory, the Antarctic Program of the Florida State University, the French Museum national d'Histoire naturelle, and the Deep Sea Drilling Program. Information on geologic age, core length, lithology, bathymetry, and geographic location are given for each sediment sample. Ages of cores are given whenever possible to the nearest sub-epoch (middle Miocene, etc), together with (when known) the fossils used to determine the age, and the source of the age determination. Many core ages are from previously unpublished sources. The listing provides information on approximately 500 different cores. A computer-searchable version of the database may be obtained by writing to the senior author. A brief analysis of latitudinal and bathymetric patterns of sedimentation is also given for the Paleogene, Miocene, and Pliocene of the Southern Ocean. Throughout the Neogene, an essentially modern pattern of sedimentation is seen, with carbonate ooze predominating north of the present-day position of the polar front, siliceous ooze between the polar front and approximately 65° S, and clay near the Antarctic continent and in water depths 〉4 km. Paleogene and Cretaceous patterns of sedimentation appear to be different, but are difficult to distinguish due to plate motion and subsidence, and also because of the relatively small number of available pre-Neogene sediment cores.
    Description: Funding was provided by the National Science Foundation under grant Nos. OCE 79-19092 and DPP83-17087.
    Keywords: Marine sediments
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 10
    Publication Date: 2022-05-26
    Description: The deep western boundary current (DWBC) of the Indian Ocean flows northward along the western margin of the Mascarene Basin, and is funneled through a narrow passage (near 09°S, 52°E) prior to entering the Somali Basin to the north. Recently completed geological and geophysical operations within this passage reveal the presence of fields of well-developed abyssal sediment waves, with amplitudes of 10 to 50 meters and wavelengths of hundreds of meters to ~1 km. The two principal fields of sediment waves are confined to the flanks of the passages, and are restricted to a narrow depth interval (~3950 to 4150 meters). Individual waves appear to be elongated parallel to the passage axis and the presumed flow direction of the DWBC. The waves are relatively transparent to low-frequency echo sounding (3.5 kHz) and seismic profiling (17-70Hz), although weak internal reflectors are present within individual waves. These reflectors are conformable with the overlying sea floor, thereby suggesting neither upslope nor downslope migration of the waves. The sediment comprising the waves is a well-sorted calcareous ooze dominated by fine silt components (principally coccoliths), in marked contrast to the heterogeneous biogenic ooze on the adjacent channel floor. The lithology and local distribution pattern of the waves suggest that they are constructional bedforms associated with the flow of the DWBC, and not slump structures. A deep hydrocast at the sill of the channel indicates a near-bottom layer of Antarctic Bottom Water (Θ 〈0.9°C) approximately 200 meters thick, whose depth range corresponds with that of the sediment waves. Interpretations of the origin of the sediment waves in terms of the local flow regime will require (1) a more precise description of the physiography and structure of individual sediment waves; and (2) closely-spaced measurements of the nearbottom velocity structure of the DWBC within regions of the passage where sediment waves are apparently forming.
    Description: Prepared for the National Science Foundation under Grant OCE76-21522
    Keywords: Marine sediments ; Waves ; Atlantis II (Ship : 1963-) Cruise AII93-7
    Repository Name: Woods Hole Open Access Server
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  • 11
    Publication Date: 2022-05-26
    Description: A time series vertical flux assessment of pelagic diatoms was conducted during September, 1982 through September, 1983 at subarctic Pacific Station PAPA (50°N, 145°W; water depth 4200 m) using PARFLUX sediment traps deployed at 1000 and 38000 m. The time series sediment trap samples were collected for 11 to 16-day periods during the year; a total of 24 samples represent a full year's record of flux. Eighteen taxonomic groups of diatoms were enumerated, based on a census of four wet-sieved size fractions: 250-1000μm, 125-250μm, 63-125μm, and 〈 63μm. In order to study the sinking processes of diatoms, detailed information on frustule integrity was acquired. For example , counts of single valves were separated from frustules. Size-fractioned fluxes of all the counting groups are graphically presented, which provides a data base for further investigations.
    Description: Prepared for the National Science Foundation under Grant OCE 85-02472.
    Keywords: Diatoms ; Marine sediments
    Repository Name: Woods Hole Open Access Server
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  • 12
    Publication Date: 2022-05-26
    Description: In 2001, the Geophysical Fluid Dynamics Summer Study Program grappled with Conceptual Models of the Climate. Eli Tziperman (Weizman Institute), Paola Cessi (Scripps Institution of Oceanography) and Ray Pierre- Humbert (University of Chicago) provided the principal lectures. This introduction gave us all a glimpse into the complex problem of the climate, both in the present, past and future, and even on other planets. As always, the next weeks of the program were filled with many seminars from the visitors, and culminated in the fellow's reports.
    Keywords: Climatic changes ; Physics
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 13
    Publication Date: 2022-05-26
    Description: Supplement to Reference No. 57-5. Originally issued as Reference No. 57-19.
    Description: During R/V CARYN Cruise No. 108 to the New York Bight samples of the bottom were obtained with an orange peel dredge at 23 stations and additional bottom samples were obtained by aqualung divers. These samples have been returned to the Woods Hole Oceanographic Institution where they have been analyzed for their iron content.
    Description: National Lead Company
    Keywords: Iron ; Waste disposal in the ocean ; Marine sediments ; New York Bight ; Caryn (Ship : 1948-1958) Cruise 108
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 14
    Publication Date: 2022-05-26
    Description: Originally issued as Reference No. 57-5.
    Description: During the period 19-24 October, 1956, the W.H.O .I. Research Vessel CARYN was employed by the National Lead Company of New York to make a self-contained diving and bottom sampling survey in their present industrial waste disposal area in the New York Bight.
    Description: National Lead Company
    Keywords: Iron ; Waste disposal in the ocean ; Marine sediments ; Caryn (Ship : 1948-1958) Cruise 108
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 15
    Publication Date: 2022-05-26
    Description: CTD and acoustic Doppler current profiler (ADCP) observations were made on the North Brazil shelf adjacent to the mouth of the Amazon River during R/V Iselin cruise I8909 August 3-14, 1989 as part of A Multidisciplinary Amazon Shelf SEDiment Study (AMASSEDS). These observations were obtained during a large-scale survey in support of geological and geochemical sampling, an anchored time series station consisting of 26 hourly CTD casts, and one transect which was repeated off the mouth of the Amazon River. The maximum sampling depth at each station was within two meters of the bottom. The primary objectives of the AMASSEDS hydrographic measurement program were to (a) observe and characterize the temperature, salinity, density, oxygen, fluorescence and light transmission fields and their spatial variability on the north Brazilian shelf directly influenced by the Amazon River discharge, (b) resolve the seaward extent and vertical structure of the surface plume of low salinity Amazon River water during different stages of river discharge, (c) describe the spatial structure of the turbidity and associated suspended sediment distributions across the shelf, (d) characterize the properties of the Amazon shelf water beneath the surface plume and their seasonal variability, and (e) describe the landward penetration of the North Brazil Current (NBC) with respect to water properties and shelf currents. This report represents a summary in graphic and tabular form of the hydrographic observations made during the first AMASSEDS cruise (I8909) on the R/V Iselin.
    Description: Funding was provided by the National Science Foundation through Grant Number OCE 88-12917
    Keywords: Amazon Shelf Sediment Study ; Hydrography ; Marine sediments ; Columbus Iselin (Ship) Cruise CI8909
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 16
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: The theory of oblique-angle seismic reflectivity, as applied to oceanographic research, is presented. An experiment has been developed in which continuous oblique reflection profiles were made by towing an acoustic source behind a ship and listening with a hydrophone suspended beneath a free-floating radio buoy. Information received at the hydrophone was transmitted to the ship and recorded on magnetic tape. Energies of the bottom-reflected signals have been calculated for varying angles of incidence and the corresponding reflectivities produced. Results from the Tyrrhenian Sea and from north of Puerto Rico indicate the possibility that the sound velocity in the first-layer sediments is less than the sound velocity of the bottom water.
    Description: The Bureau of Ships Under Contract NObsr-89464
    Keywords: Marine sediments
    Repository Name: Woods Hole Open Access Server
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  • 17
    Publication Date: 2022-05-26
    Description: Also published as: Biological Bulletin 159 (1980): 459-460
    Description: Last year we reported on time-of-transit experiments in which magnetically orienting bacteria crossed a 1-mm stretch in the direction of a uniform magnetic field. The bacteria were found to behave as tiny self-propelled compass needles subject both to magnetic field alignment and to the randomizing effect of thermal agitation. In strong fields, magnetic bacteria are held in tight aligment; in weaker fields, their swimming paths meander more and transit times are greater. Paul Langevin derived an expression for the distribution of orientation in an ensemble of free-moving dipole particles as a function of ambient field strength. His theory becomes applicable to our experiments when bacterial migration is analyzed as a sequence of short steps during each of which the cell swims in a direction randomly selected from the Langevin distribution . The duration of each step, Δt, is actually a time constant of the cell's loss of directionality due to thermal agitation. By thus treating the migration as a process of random walk with drift, we are able to predict the mean and variance of the time of transit across a 1-mm stretch.
    Description: Prepared for the Office of Naval Research under Contract N00014-79-C-0071.
    Keywords: Marine sediments ; Statistical mechanics
    Repository Name: Woods Hole Open Access Server
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  • 18
    Publication Date: 2022-05-26
    Description: Also published as: Journal of the Acoustical Society of America 69 (1981): 84-94
    Description: The results of a deep-ocean bottom interaction experiment are presented in which the effects of both bottom refraction and subbottom reflection were observed. Data were obtained in the Hatteras Abyssal Plain using a deep towed 220-Hz pulsed cw source and two receivers anchored near the bottom. For ranges between 1 and 6 km, corresponding to bottom grazing angles less than 13°, the quadrature components of the received signals were recorded digitally. The observed amplitude shows a strong spatial interference pattern which is composed of the direct and bottom interacting arrivals. It is shown that for small source-receiver separations, the bottom return is dominated by a strong subbollom reflection. With increasing separation, this arrival evolves into a refracted arrival due to the presence of a positive sound-speed gradient in the sediment overlying the subbottom. Because of the gradient, a caustic is formed, and corresponding high intensity regions are observed in the data at the expected ranges. Values of sediment layer thickness, sound-speed gradient, and sound-speed drop at the water-bollom interface are obtained from best fits to the data using ray theory, normal mode theory, and the parabolic equation method. These values are consistent with those obtained in nearby locations by other workers. The success of the parabolic equation method indicates that at small grazing angles, the bottom interaction process may be modeled as a propagation process combined with the effect of a perfect, soft subbollom reflector. A value of sediment attenuation, 0.0015 dB/mat 220Hz, is also inferred from the data and is among the lowest values reported to date in the literature.
    Description: Prepared for the Office of Naval Research under Contract N00014-77-C-0196 administered through NORDA
    Keywords: Marine sediments ; Acoustical engineering
    Repository Name: Woods Hole Open Access Server
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  • 19
    Publication Date: 2022-05-26
    Description: A deep operating self-contained high-frequency echo sounder known as Deep Probe was recently developed at W.H.O.I. under ERDA and Sea Grant contracts for the purpose of resolving fine details of bottom and sub-bottom sediment layering in the deep ocean. In August 1975 this system was mounted on R.V. KNORR for a coring expedition (KNORR #51) to the Rockall Trough area east of the United Kingdom under the direction of Dr. Charles Hollister. The purpose of this exercise was to determine the correlation between the high frequency acoustic sounding records and the stratification of several Giant Piston Cores (GPC) taken in the same area. Three of these cores, GPC-13, 17 and 19, have been analyzed and compared graphically with the acoustic survey of each core location, using Deep Probe, near-bottom, both as a 12 kHz echo-sounder, and as a deep receiver for detecting returns from a 3.5 kHz pinger mounted on the surface vessel. The acoustic traces for both frequencies were then compared for detail and depth of penetration with respect to the cores. Good to excellent correlation with core stratigraphy is indicated at 12 kHz. Resolution ranged from fair to poor at 3.5 kHz although transmission losses through the core were lower at this frequency. The general conclusion is that deep echo-sounding at 12 kHz is an excellent technique for delineation of shallow bottom and sub-bottom sediments in high detail, and that deep sounders having characteristics similar to Deep Probe could therefore prove valuable for detailed surveys of small areas preliminary to coring, or in deep-towed fish form, for general seismic profiling of shallow sediments over longer tracts in the deep ocean.
    Description: Prepared for the Sandia Laboratories under contract number 07-7923.
    Keywords: Echo sounding ; Marine sediments ; Knorr (Ship : 1970-) Cruise KN51
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  • 20
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: This report presents data obtained from cored sediments collected during numerous cruises in the Northwest Atlantic area. The cores were obtained by SCUBA, gravity cores and DSRV ALVIN. The sediments were sampled with 6 centimeter diameter plastic core liners and ranged in length from 9 to 63 centimeters. Analyses conducted on sediment material include organic carbon, organic nitrogen, percent sand-silt-clay, percent calcium carbonate and pore water concentrations of ammonia, nitrite, nitrate, silicate and phosphate.
    Description: This work was supported by ONR Contract N00014-74-C0262 and NSF Grant OCE 76-21878.
    Keywords: Marine sediments ; Sedimentation and deposition ; Oceanus (Ship : 1975-) Cruise OC6 ; Knorr (Ship : 1970-) Cruise KN68
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  • 21
    Publication Date: 2022-05-26
    Description: Includes Errata dated May 2, 1979
    Description: The experimental benthic chamber was designed to conduct both laboratory and in situ investigations on the transport and degradation of petroleum type hydrocarbons at the sediment water interface, and to investigate the sediment/ water/organism interactions. In its basic form, it consists of a rectangular flume constructed of stainless steel tube, a windowed observation chamber, a variable velocity pumping system and its associated controls, battery packs, and interconnecting cables. The base of the observation chamber is a removable assembly, allowing the user to select either a closed rectangular box for laboratory use, or a mud grab bottom sampler configuration for in situ evaluation. For in situ use, the mud grab doors are opened, the device lowered until it contacts and settles into the bottom. The side walls of the mud grab, its jaws, and the observation chamber walls effectively seal the assembly into a closed recirculating sea water system that uses the bottom sediment as the controlled sample. Hydrocarbon, oxygen, or other materials may be used to spike the recirculating sea water or bottom sediment. Several instrumentation ports have been provided to allow monitoring of the internal system chemistry. The self-contained power pack is pressure compensated with gaseous carbon dioxide, providing a non-explosive atmosphere within the battery box compartment as well as the pump drive motor package. A five day, on-the-bottom, operational test indicated that the battery system would provide sufficient reserve power to operate the device for an extrapolated minimum of 10 days without serious degradation of the internal water flow within the system. On completion of the bottom program, the mud grab doors are pneumatically closed, retaining the sea water and sediment sample as a complete ecological test system that can be returned to the surface for additional evaluation.
    Description: Prepared For : U.S. Department of Energy Division of Biomedical and Environmental Programs Contract: EE-77-S-02-4256 and U.S. Department of Interior Bureau of Land Management Interagency Agreement: IA 7-20
    Keywords: Hydrocarbons ; Marine sediments
    Repository Name: Woods Hole Open Access Server
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  • 22
    Publication Date: 2022-05-26
    Description: Also published as: Journal of the Acoustical Society of America 68 (1980): 1376-1390
    Description: Seventeen piston cores up to 13 m long were recovered from representative acoustic and lithologic environments of the Hatteras and Nares Abyssal Plains in the western North Atlantic. Compressional-wave velocities (corrected to in situ conditions) and bulk physical properties measured on the cores are used to characterize the acoustic framework of these areas. For correlation with conventional seismic data, wholecore averages of properties are a better index to the acoustic nature of abyssal plain sediments than properties of the upper few centimeters of the seafloor because (I) strong changes in lithofacies (and acoustic properties) occur over depth scales of tens of centimeters to meters in the sediment column, and (2) conventional seismic frequencies of 3.5 kHz or less sample these variations to subbottom depths of tens of meters and more. Wholecore properties are a function of the thickness and distribution of high-velocity silt and sand layers in the core; they vary in a complex fashion with proximity to the source of turbidity currents, distance from axial paths of turbidity-current flows, local and regional basin geometry, and seafloor slope. Thus strongly reflective seabed regions with numerous high-velocity layers are not restricted simply to near-source areas nor are weakly reflective seabed regions (clay sediments only) limited to "distal" areas. Whole-core properties show a good qualitative correlation to variations in 3.5-kHz reflection profiles, and 3.5-kHz echo character therefore provides a useful means of mapping general acoustic properties over large regions of abyssal plains.
    Description: Prepared for the Office of Naval Research under Contracts N00014-75-C-0210 and N00014-79-C-0071; NR 083-004.
    Keywords: Underwater acoustics ; Marine sediments
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  • 23
    Publication Date: 2022-05-26
    Description: Particulate matter samples were collected using free-drifting sediment traps in the Peru upwelling area in 1978 to assess the vertical flux and organic composition of lipids associated with particles sinking out of the euphotic zone. Samples have been analyzed for a variety of lipids, including hydrocarbons, fatty acids, wax esters, steryl esters, triacylglycerols, alkyldiacylglycerols, fatty alcohols, sterols, and steroid ketones. The purpose of this report is to collate the fatty acid and fatty acid ester (wax ester, steryl ester, triacylglycerol, and alkyldiacylglycerol) for the 20 floating sediment traps which were deployed.
    Description: Funding was provided by the Office of Naval Research under Contracts N00014-74-C-0262, N00014-79-C-0071, and by the National Science Foundation under Grants OCE 77-26084 and OCE 80-18436.
    Keywords: Fatty acids ; Marine sediments ; Knorr (Ship : 1970-) Cruise KN73
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  • 24
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: The location of sediment samples from the northern and equatorial portions of the western African continental shelf and upper slope are presented, along with a discussion of analytical techniques and some preliminary results.
    Description: Supported by the National Science Foundation under Grant No. GX-28193.
    Keywords: Marine sediments ; International Decade of Ocean Exploration, 1970-1980
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  • 25
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: This report supplements Volumes 1-6 of the core descriptions published previously in this sequence (Johnson and Driscoll, 1975; 1977; Broda, Franks, and Keith, 1981). It contains visual descriptions and smear slide analyses for all cores received in the geological samples collection of the Woods Hole Oceanographic Institution between mid-1980 and mid~l984. Approximately 240 sample localities from the North Atlantic, South Atlantic, Mediterranean and Pacific Oceans are represented. Charts of ships' tracks and updated computer listings of all cores in the W.H.O.I. collection are also included.
    Description: Prepared for the National Science Foundation Under Grant OCE82-00119.
    Keywords: Marine sediments ; Drill cores
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 26
    Publication Date: 2022-05-26
    Description: With the support of the National Science Foundation, we have completed the first cruise devoted to the GOFS and JGOFS program for the North Atlantic Bloom studies between March 28 and April 6 on board R/V Atlantis II. The major task of this cruise, to deploy bottom-tethered mooring arrays with time-series sediment traps along with current meters at two critical stations, 34°N and 47°N along 20°W, was accomplished. All 6 sediment traps, 3 on each array, were set at 14-day intervals for 13 periods from April 3 to September 26, 1989. Their opening and closing times were synchronized throughout the period of deployment. The arrays and instruments will be recovered and redeployed in September/October, 1989. Ancillary water column data, such as CTD, fluorometry, pigments, and major nutrient distribution, were also successfully completed (except for transmissometry profiling at the 47°N station) in order to understand the prebloom setting at JGOFS 34°N, 47°N, and 60°N stations. At the 47°N station on April 2, the mixed layer depth was 248m.
    Description: Funding was provided by the National Science Foundation through grant Number OCE 88-14228.
    Keywords: Joint Global Ocean Flux Study ; Marine sediments ; Atlantis II (Ship : 1963-) Cruise AII119-2
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 27
    Publication Date: 2022-05-26
    Description: Originally issued as Reference No. 60-35, series later renamed WHOI-.
    Description: The Woods Hole Oceanographic Institution contracted to make a survey of the bathymetry and sediments at the Navy Torpedo Testing Range in Cape Cod Bay at the request of the Project Engineer at the U. S Naval Underwater Ordnance Station, Newport, Rhode Island- Contract Number N298(122)16639. The area studies is approximately 35 miles SE from Boston and 15 miles NW from Provincetown in the southern part of .Massachusetts Bay.
    Description: Submitted to the u. S. Naval Underwater Ordnance Station, Newport, Rhode Island Under Contract N298(122)16639 and Reqn. No. 122/5271/60
    Keywords: Marine sediments ; Submarine topography ; Underwater photography
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 28
    Publication Date: 2022-05-26
    Description: The Sea Duct Ocean-Bottom Laboratory is a computer controlled recirculating inverted flume for the in-situ study of sediment transport. It is designed to measure the sea floor response to controlled currents analogous to those generated by surface waves, tidal, or deep ocean storms. The external support frame is an equilateral triangle with sixteen foot sides. It is 12 feet high, has an air weight of 12,500 lbs., and a 2800 lb. submerged weight. Three lead acid battery packs located at the vertex of the triangle legs provide power for the recirculating water pumps, hydraulic power, and ancillary equipment. The inner rotatable structure consists of a 4 foot long by 2 foot wide open bottom windowed test section that is 9 inches high. It is connected to 30 feet of 8 inch tube configured as an elongated toroid. Above the test section is a traverse carriage with stereo camera, flash, and a laser Doppler velocimeter to measure fluid stresses. Internal flow velocities are controlled and can be ramped up to approximately 2 ft/sec providing shear stress sufficient to scour sand, silts, and fine clays. Water and sediment sampling devices obtain specimens from inside and outside the test section. This report consists of three sections. The first subdivision discusses the electro-mechanical systems and deployment- recovery techniques, while the second portion covers the microprocessor controller and its support equipment. The third section contains the appendices, which consists of program listings, schematics, system and deployment check-list, etc.
    Description: Office of Naval Research, Environmental Sciences Directorate, under Contracts N00014-85-C-0001 and N00014-87-K-007
    Keywords: Marine sediments ; Sediment transport ; Ocean bottom ; Ocean currents ; Data processing
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 29
    Publication Date: 2022-05-26
    Description: Nordic Seas sedimentation data file, v. 1
    Description: Seventy-nine particle. flux samples were collected from 1983 to 1986 using 7 automated time-series sediment traps at 6 stations distributed in the northern and eastern portion of the Nordic Seas as part of a German/U.S. joint program on arctic sedimentation studies. Each sample represents either one month or two weeks of sedimentation at approximately 400 m above the sea floor. In this data file the results of laboratory analysis conducted at the Woods Hole Oceanographic Institution, U.S.A. of the main sedimentological criteria: total mass, carbonate, opal, combustible, organic carbon, nitrogen, and lithogenic mass are presented in both tabular and histogram form. Results from the southern and western portion of the Nordic Seas will be published as they become available.
    Description: Funding was provided by the Office of Naval Research under Grant Number N00014--85-C-0001.
    Keywords: Marine sediments
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 30
    Publication Date: 2022-05-26
    Description: A method has been developed to measure rare-earth elements (REE) in gram-sized marine sediment samples. A strong acid digestion technique followed by ion-exchange chromatography is used to solubilize, separate, and purify the REE from other matrix components. Instrumental detection is by inductively coupled plasma-atomic emission spectrometry (ICP-AES). Excellent precision and accuracy were proved by analyses of unknown sediment replicates and standard reference rock samples. Blanks and empirically determined detection limits are discussed in relation to measured REE concentrations in sediments. Direct evidence is given for the co-precipitation and fractionation of the REE by precipitates formed as a result of the acid digestion with HF. A technique for dissolving these is then presented.
    Description: Funding was provided by the National Science Foundation under grant Number OCE 84-17910; and the United States Department of Energy under grant Number DE-AC02-76EV03566.
    Keywords: Marine sediments ; Rare earth metals
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 31
    Publication Date: 2022-05-26
    Description: A seasonal flux study of silicoflagellates and Actiniscus was conducted at subarctic Pacific Station PAPA (50°N, 145°W; water depth 4200 m) during September, 1982 through August, 1984 using PARFLUX time series sediment traps deployed at 1000 m and 3800 m depths. The time series sediment trap samples were collected for 4 to 16-day periods depending on the samples; most of the samples were collected for 14 to 16-day periods. A total of 47 continuous samples represents nearly a two-year record of the fluxes of silicoflagellate and Actiniscus taxa at 3800 m depth. An additional 12 samples from 1000 m represent a continuous 6-month period which provides a pair of samples from two depths of each time series. Analysis of the paired samples is essential to understand particle sinking processes. Seven silicoflagellate taxa, several additional variants of silicoflagellat.es, and Actiniscus pentasterias group were enumerated, based on a census of four wet sieved size fractions: 250-1000μm, 125-250μm, 63-125μm, and 〈63μm. A total of more than 32x103 specimens were identified to species level and counted in this study. Statistics of the counts are given. The fluxes of silicoflagellate taxa of all four size fractions are graphically presented. This report provides a detailed data base for further investigations of seasonal silicoflagellate fluxes in the area.
    Description: Prepared for the National Science Foundation under Grant OCE 85- 02472.
    Keywords: Silicoflagellates ; Actiniscus pentasterias ; Marine sediments
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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