Fisher, Andrew T; Foucher, Jean Paul; Yamano, Makoto; Hyndman, Roy D (1993): (Table 1) Thermal conductivity of ODP Site 131-808. PANGAEA, https://doi.org/10.1594/PANGAEA.785421, Supplement to: Fisher, AT et al. (1993): Data report: Corrected thermal conductivity data, Leg 131. In: Hill, IA; Taira, A; Firth, JV; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 131, 451-456, https://doi.org/10.2973/odp.proc.sr.131.138.1993
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Measurements of thermal conductivity made during Ocean Drilling Program (ODP) Leg 131 were corrected during the cruise using the following set of standards: fresh water, fused silica, Macor ceramic, and basalt. The true thermal conductivity of the basalt standard was not known during Leg 131. In this report, we use a corrected conductivity value for the basalt standard to calibrate measurements made during the leg.
Latitude: 32.352150 * Longitude: 134.944367
Date/Time Start: 1990-04-04T00:00:00 * Date/Time End: 1990-05-31T00:00:00
Minimum DEPTH, sediment/rock: 0.55 m * Maximum DEPTH, sediment/rock: 1309.16 m
131-808 * Latitude: 32.352150 * Longitude: 134.944367 * Date/Time Start: 1990-04-04T00:00:00 * Date/Time End: 1990-05-31T00:00:00 * Elevation: -4685.1 m * Penetration: 4130.2 m * Recovery: 732.1 m * Location: Philippine Sea * Campaign: Leg131 * Basis: Joides Resolution * Device: Composite Core (COMPCORE) * Comment: 163 cores; 1463.3 m cored; 1980 m drilled; 50% recovery
|#||Name||Short Name||Unit||Principal Investigator||Method||Comment|
|1||Sample code/label||Sample label||Fisher, Andrew T||ODP sample designation|
|2||DEPTH, sediment/rock||Depth||m||Geocode – mbsf|
|3||Conductivity, thermal||k||W/m/K||Fisher, Andrew T||full-space, uncorrected for in-situ conditions (unchanged from Taira, Hill, Firth et al., 1991)|
|4||Conductivity, thermal||k||W/m/K||Fisher, Andrew T||half-space, uncorrected for in-situ conditions (corrected from Taira, Hill, Firth et al., 1991, using new basalt standard)|
|5||Conductivity, thermal||k||W/m/K||Fisher, Andrew T||either full-space or half-space, corrected to in-situ conditions (Ratcliffe, 1960; Clark, 1966), as described in Taira, Hill, Firth, et al. (1991)|
1359 data points