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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Journal of materials science 18 (1999), S. 1547-1549 
    ISSN: 1573-4811
    Source: Springer Online Journal Archives 1860-2000
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1573-4803
    Source: Springer Online Journal Archives 1860-2000
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Notes: Abstract The structure and crystallographic orientation of mineral phase in the oblique prismatic layer of Mytilus edulis shell were studied by SEM, XRD and TEM with selected area electron diffraction (SAED). A crystallographic orientation regulation, i.e. the adjacent 1–5 calcite prisms with the same three-dimensional orientation in the oblique prismatic layer, was found for the first time. It is observed that the calcite prisms in the oblique prismatic layer were grown with their (104) parallel to the shell surface.
    Type of Medium: Electronic Resource
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  • 3
  • 4
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    PANGAEA
    In:  Supplement to: McGann, Mary L; Erikson, Li H; Wan, Elmira; Powell, Charles; Maddocks, Rosalie F (2013): Distribution of biologic, anthropogenic, and volcanic constituents as a proxy for sediment transport in the San Francisco Bay Coastal System. Marine Geology, 345, 113-142, https://doi.org/10.1016/j.margeo.2013.05.006
    Publication Date: 2023-05-12
    Description: Although conventional sediment parameters (mean grain size, sorting, and skewness) and provenance have typically been used to infer sediment transport pathways, most freshwater, brackish, and marine environments are also characterized by abundant sediment constituents of biological, and possibly anthropogenic and volcanic, origin that can provide additional insight into local sedimentary processes. The biota will be spatially distributed according to its response to environmental parameters such as water temperature, salinity, dissolved oxygen, organic carbon content, grain size, and intensity of currents and tidal flow, whereas the presence of anthropogenic and volcanic constituents will reflect proximity to source areas and whether they are fluvially- or aerially-transported. Because each of these constituents have a unique environmental signature, they are a more precise proxy for that source area than the conventional sedimentary process indicators. This San Francisco Bay Coastal System study demonstrates that by applying a multi-proxy approach, the primary sites of sediment transport can be identified. Many of these sites are far from where the constituents originated, showing that sediment transport is widespread in the region. Although not often used, identifying and interpreting the distribution of naturally-occurring and allochthonous biologic, anthropogenic, and volcanic sediment constituents is a powerful tool to aid in the investigation of sediment transport pathways in other coastal systems.
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 5
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    PANGAEA
    In:  Supplement to: Barnard, Patrick L; Erikson, Li H; Elias, Edwin; Dartnell, Peter (2012): Sediment transport patterns in the San Francisco Bay Coastal System from cross-validation of bedform asymmetry and modeled residual flux. Marine Geology, 345, 72-95, https://doi.org/10.1016/j.margeo.2012.10.011
    Publication Date: 2023-01-13
    Description: The morphology of ~45,000 bedforms from 13 multibeam bathymetry surveys was used as a proxy for identifying net bedload sediment transport directions and pathways throughout the San Francisco Bay estuary and adjacent outer coast. The spatially-averaged shape asymmetry of the bedforms reveals distinct pathways of ebb and flood transport. Additionally, the region-wide, ebb-oriented asymmetry of 5% suggests net seaward-directed transport within the estuarine-coastal system, with significant seaward asymmetry at the mouth of San Francisco Bay (11%), through the northern reaches of the Bay (7-8%), and among the largest bedforms (21% for lambda 〉 50 m). This general indication for the net transport of sand to the open coast strongly suggests that anthropogenic removal of sediment from the estuary, particularly along clearly defined seaward transport pathways, will limit the supply of sand to chronically eroding, open-coast beaches. The bedform asymmetry measurements significantly agree (up to ~ 76%) with modeled annual residual transport directions derived from a hydrodynamically-calibrated numerical model, and the orientation of adjacent, flow-sculpted seafloor features such as mega-flute structures, providing a comprehensive validation of the technique. The methods described in this paper to determine well-defined, cross-validated sediment transport pathways can be applied to estuarine-coastal systems globally where bedforms are present. The results can inform and improve regional sediment management practices to more efficiently utilize often limited sediment resources and mitigate current and future sediment supply-related impacts.
    Keywords: MB; Multibeam; San Francisco Bay, California; SF_bays
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 6
    Publication Date: 2023-01-13
    Keywords: Area/locality; Asymmetry; Bedform height; Depth, relative; MB; Multibeam; Multibeam bathymetry; Number; San Francisco Bay, California; SF_bays; Slope; UTM Easting, Universal Transverse Mercator; UTM Northing, Universal Transverse Mercator; Wavelength, bedform
    Type: Dataset
    Format: text/tab-separated-values, 254498 data points
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  • 7
    Publication Date: 2023-01-13
    Keywords: Area/locality; Asymmetry; Bedform height; Crest location, UTM Easting, Universal Transverse Mercator; Crest location, UTM Northing, Universal Transverse Mercator; Depth, relative; MB; Multibeam; Multibeam bathymetry; Sample ID; San Francisco Bay, California; SF_bays; Trough location, UTM Easting, Universal Transverse Mercator; Trough location, UTM Northing, Universal Transverse Mercator; Wavelength, bedform
    Type: Dataset
    Format: text/tab-separated-values, 673919 data points
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  • 8
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    PANGAEA
    In:  Supplement to: Hegermiller, Christie A; Rueda, Ana; Erikson, Li H; Barnard, Patrick L; Antolinez, Jose A A; Mendez, Fernando J (2017): Controls of Multimodal Wave Conditions in a Complex Coastal Setting. Geophysical Research Letters, 44(24), 12,315-12,323, https://doi.org/10.1002/2017GL075272
    Publication Date: 2023-01-13
    Description: The lookup tables relate deep-water significant wave height, peak wave period, and peak wave direction with nearshore significant wave height, peak wave period, mean wave period, peak wave direction, and directional spreading at 4,802 stations spaced ~100 m apart along the 10 m bathymetric contour and 20 intermediate-water stations coincident with CDIP buoys within the Southern California Bight from Point Conception to the Mexican border. Deep-water significant wave height bin size = 0.25 m. Deep-water peak wave period bin size = 3 s. Deep-water peak wave direction bin size = 8 deg. Station file = socal.loc is a text file with 4822 lat,lon coordinates for stations starting from 1 to 4822. Lookup table files = LUT_STN*toSTN*.mat Each lookup table file is a mat file containing the lookup table for 600 stations, as noted in the filename. Structures of input/deep-water significant wave height, peak wave period, and peak wave direction and output/nearshore significant wave height, peak wave period, mean wave period, peak wave direction, and directional spreading allow for easy indexing of deep-water wave conditions to find nearshore conditions at a station of interest. These lookup tables were generated with Simulating WAves Nearshore model. Detailed modeling information can be found in: Hegermiller et al., submitted. Controls of multimodal wave conditions in a complex coastal setting. Please email chegermiller@usgs.gov for more information.
    Keywords: Southern_California
    Type: Dataset
    Format: application/zip, 735.9 MBytes
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  • 9
    Publication Date: 2023-05-12
    Keywords: Aluminium; Antimony; Arsenic; Baker_Beach_West; Barium; Beryllium; Bismuth; Bonita_Cove_Central; Cadmium; Caesium; Calcium; Cerium; Chromium; Cobalt; Copper; Date/Time of event; DEPTH, sediment/rock; Description; Event label; Gallium; Grab; GRAB; Hand trowel; Inductively coupled plasma - mass spectrometry (ICP-MS); Iron; Lanthanum; Latitude of event; Lead; Lithium; Longitude of event; Magnesium; Manganese; Molybdenum; MSF37-2005; Nickel; Niobium; North_Ocean_Beach; OB23-2005; Phosphorus; Potassium; Pt_Bonita_1; Rodeo_Beach_2; Rubidium; Sand Wave Field; San Francisco Bay, California; Scandium; Silver; Sodium; South_Ocean_Beach; South Ocean Beach Offshore; Strontium; Thallium; Thorium; Titanium; TROW; Uranium; Vanadium; Yttrium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 304 data points
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  • 10
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    PANGAEA
    In:  Supplement to: Barnard, Patrick L; Foxgrover, Amy C; Elias, Edwin; Erikson, Li H; Hein, James R; McGann, Mary L; Mizell, Kira; Rosenbauer, Robert J; Swarzenski, Peter W; Takesue, Renee K; Wong, Florence L; Woodrow, Donald L (2013): Integration of bed characteristics, geochemical tracers, current measurements, and numerical modeling for assessing the provenance of beach sand in the San Francisco Bay Coastal System. Marine Geology, 336, 120-145, https://doi.org/10.1016/j.margeo.2012.11.008
    Publication Date: 2023-05-12
    Description: Over 150 million cubic meter of sand-sized sediment has disappeared from the central region of the San Francisco Bay Coastal System during the last half century. This enormous loss may reflect numerous anthropogenic influences, such as watershed damming, bay-fill development, aggregate mining, and dredging. The reduction in Bay sediment also appears to be linked to a reduction in sediment supply and recent widespread erosion of adjacent beaches, wetlands, and submarine environments. A unique, multi-faceted provenance study was performed to definitively establish the primary sources, sinks, and transport pathways of beach sized-sand in the region, thereby identifying the activities and processes that directly limit supply to the outer coast. This integrative program is based on comprehensive surficial sediment sampling of the San Francisco Bay Coastal System, including the seabed, Bay floor, area beaches, adjacent rock units, and major drainages. Analyses of sample morphometrics and biological composition (e.g., Foraminifera) were then integrated with a suite of tracers including 87Sr/86Sr and 143Nd/144Nd isotopes, rare earth elements, semi-quantitative X-ray diffraction mineralogy, and heavy minerals, and with process-based numerical modeling, in situ current measurements, and bedform asymmetry to robustly determine the provenance of beach-sized sand in the region.
    Type: Dataset
    Format: application/zip, 5 datasets
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