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Tan, Brian; Germaine, John T; Flemings, Peter B (2006): Consolidation properties and strength characteristics of ODP Site 204-1244 sediments [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.775119, Supplement to: Tan, B et al. (2006): Data report: Consolidation and strength characteristics of sediments from ODP Site 1244, Hydrate Ridge, Cascadia continental margin. In: Tréhu, AM; Bohrmann, G; Torres, ME; Colwell, FS (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 204, 1-148, https://doi.org/10.2973/odp.proc.sr.204.102.2006

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Abstract:
Eight whole-core samples from Ocean Drilling Program Site 1244, Hydrate Ridge, Cascadia continental margin, were provided to Massachusetts Institute of Technology (Cambridge, Massachusetts, USA) for geotechnical characterization. The samples were collected from depths ranging from 5 to 136 meters below seafloor (mbsf). Seven of the eight whole-core samples were located within the gas hydrate stability zone, whereas the eighth sample was located in the free gas zone. Atterberg limits testing showed that the average liquid limit of the soil is 81% and the average plastic limit is 38%, giving an average plasticity index of 43%. The liquid limit is sensitive to oven drying, shown by a drop in liquid limit to 64% when tests were performed on an oven-dried sample. Loss on ignition averages 5.45 wt%. Constant rate of strain consolidation (CRSC) tests were performed to obtain the compression characteristics of the soil, as well as to determine the stress history of the site. CRSC tests also provided hydraulic conductivity and coefficient of consolidation characteristics for these sediments. The compression ratio (Cc) ranges from 0.340 to 0.704 (average = 0.568). Cc is fairly constant to a depth of 79 mbsf, after which Cc decreases downhole. The recompression ratio (Cr) ranges from 0.035 to 0.064 (average = 0.052). Cr is constant throughout the depth range. In situ hydraulic conductivity varies between 1.5 x 10**-7 and 3 x 10**-8 cm/s and shows no trend with depth. Ko-consolidated undrained compression/extension (CKoUC/E) tests were also performed to determine the peak undrained shear strength, stress-strain curve, and friction angle. The normalized undrained strength ranges from 0.29 to 0.35. The friction angle ranges from 27 to 37. Because of the limited amount of soil, CRSC and CKoUC/E tests were also conducted on resedimented specimens.
Project(s):
Coverage:
Median Latitude: 44.586231 * Median Longitude: -125.119816 * South-bound Latitude: 44.586160 * West-bound Longitude: -125.119860 * North-bound Latitude: 44.586300 * East-bound Longitude: -125.119750
Date/Time Start: 2002-07-12T00:00:00 * Date/Time End: 2002-08-22T00:00:00
Event(s):
204-1244 * Latitude: 44.586233 * Longitude: -125.119750 * Date/Time Start: 2002-07-12T00:00:00 * Date/Time End: 2002-08-22T00:00:00 * Elevation: -895.4 m * Penetration: 1051.2 m * Recovery: 545 m * Location: North Pacific Ocean * Campaign: Leg204 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 69 cores; 555.5 m cored; 495.7 m drilled; 98.1 % recovery
204-1244B * Latitude: 44.586160 * Longitude: -125.119860 * Date/Time Start: 2002-07-13T01:00:00 * Date/Time End: 2002-07-13T12:45:00 * Elevation: -896.0 m * Penetration: 54.1 m * Recovery: 56.85 m * Location: North Pacific Ocean * Campaign: Leg204 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 6 cores; 54.1 m cored; 0 m drilled; 105.1 % recovery
204-1244C * Latitude: 44.586300 * Longitude: -125.119830 * Date/Time Start: 2002-07-13T12:45:00 * Date/Time End: 2002-07-16T05:30:00 * Elevation: -895.1 m * Penetration: 333.5 m * Recovery: 315.5 m * Location: North Pacific Ocean * Campaign: Leg204 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 39 cores; 332 m cored; 1.5 m drilled; 95 % recovery
Size:
10 datasets

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Datasets listed in this publication series

  1. Tan, B; Germaine, JT; Flemings, PB (2006): (Table T4) Atterberg limits, organic matter content, and calcite content of ODP Site 204-1244 sediments. https://doi.org/10.1594/PANGAEA.775105
  2. Tan, B; Germaine, JT; Flemings, PB (2006): (Tables T8-T13) Soil mineralogy of calcite treated random powder samples of ODP Site 204-1244 sediments. https://doi.org/10.1594/PANGAEA.775107
  3. Tan, B; Germaine, JT; Flemings, PB (2006): (Tables T38,T40,T44,T46,T50,T52) Ko-consolidated undrained test results and consolidation properties of ODP Site 204-1244 sediments. https://doi.org/10.1594/PANGAEA.775117
  4. Tan, B; Germaine, JT; Flemings, PB (2006): (Tables T39,T41,T45,T47,T51,T53) Ko-consolidated undrained test results and properties of undrained shearing stage of ODP Site 204-1244 sediments. https://doi.org/10.1594/PANGAEA.775118
  5. Tan, B; Germaine, JT; Flemings, PB (2006): (Table T36) Ko-consolidated undrained test conditions and consolidation properties of ODP Site 204-1244 sediments. https://doi.org/10.1594/PANGAEA.775115
  6. Tan, B; Germaine, JT; Flemings, PB (2006): (Table T37) Ko-consolidated undrained test conditions and properties of undrained shearing stage of ODP Site 204-1244 sediments. https://doi.org/10.1594/PANGAEA.775116
  7. Tan, B; Germaine, JT; Flemings, PB (2006): (Tables T14-T16) Soil mineralogy of clay-fraction random powder samples of ODP Site 204-1244 sediments. https://doi.org/10.1594/PANGAEA.775108
  8. Tan, B; Germaine, JT; Flemings, PB (2006): (Tables T18-T35) Constant rate of strain consolidation properties of ODP Site 204-1244 sediments. https://doi.org/10.1594/PANGAEA.775111
  9. Tan, B; Germaine, JT; Flemings, PB (2006): (Table T17) Constant rate of strain consolidation test conditions and consolidation properties of ODP Site 204-1244 sediments. https://doi.org/10.1594/PANGAEA.775109
  10. Tan, B; Germaine, JT; Flemings, PB (2006): (Tables T5-T7) Soil mineralogy of random powder samples of ODP Site 204-1244 sediments. https://doi.org/10.1594/PANGAEA.775106