Biebow, Nicole; Kulinich, R; Baranov, Boris V (2003): Physical properties of sediment core LV29-56-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.126598, In: Biebow, N et al. (2011): Hydrography and documentation of sediment profiles from expedition KOMEX II [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.769906
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Biebow, Nicole; Kulinich, R; Baranov, Boris V (2002): KOMEX II (Kurile Okhotsk Sea Marine Experiment): Cruise report RV Akademik M.A. Lavrentyev cruise 29, leg 1 and leg 2; Vladivostok-Pusan-Okhotsk Sea-Pusan-Vladivostok; May 25-August 05, 2002. GEOMAR Report, 110, 190 pp, https://doi.org/10.3289/geomar_rep_110_2002
Project(s):
Coverage:
Latitude: 54.012433 * Longitude: 146.265783
Date/Time Start: 2002-06-18T21:38:00 * Date/Time End: 2002-06-18T22:19:00
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 5.900 m
Event(s):
LV29-56-1 * Latitude: 54.012433 * Longitude: 146.265783 * Date/Time Start: 2002-06-18T21:38:00 * Date/Time End: 2002-06-18T22:19:00 * Elevation: -1470.0 m * Recovery: 5 m * Location: Derugin Basin * Campaign: LV29-1 (KOMEX II) * Basis: Akademik M.A. Lavrentiev * Method/Device: Gravity corer (Russian type) (RGC) * Comment: Strong degassing (plastic film bursted).
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Magnetic susceptibility, volume | kappa | 10-6 SI | Biebow, Nicole | ||
3 | Temperature, in rock/sediment | t | °C | Biebow, Nicole | ||
4 | Conductivity, thermal | k | W/m/K | Biebow, Nicole |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
131 data points
Data
1 Depth sed [m] | 2 kappa [10-6 SI] | 3 t [°C] | 4 k [W/m/K] |
---|---|---|---|
0.000 | 56.0 | 2.23 | |
0.050 | 32.0 | ||
0.100 | 35.0 | ||
0.150 | 347.0 | ||
0.200 | 45.0 | ||
0.250 | 46.0 | ||
0.300 | 36.0 | ||
0.350 | 34.0 | ||
0.400 | 21.0 | 2.39 | |
0.450 | 13.0 | ||
0.500 | 17.0 | ||
0.550 | 18.0 | ||
0.600 | 20.0 | ||
0.650 | 5.0 | ||
0.700 | 33.0 | ||
0.750 | 26.0 | ||
0.800 | 27.0 | ||
0.850 | 26.0 | ||
0.900 | 18.0 | ||
0.950 | 15.0 | ||
1.000 | 24.0 | 2.77 | 0.875 |
1.050 | 28.0 | ||
1.100 | 13.0 | ||
1.150 | 26.0 | ||
1.200 | 20.0 | ||
1.250 | 14.0 | ||
1.300 | 4.0 | ||
1.350 | 11.0 | ||
1.400 | 10.0 | ||
1.450 | 4.0 | ||
1.500 | 7.0 | ||
1.550 | 7.0 | ||
1.600 | 10.0 | ||
1.650 | 9.0 | ||
1.700 | 10.0 | ||
1.750 | 8.0 | ||
1.800 | 11.0 | ||
1.850 | 8.0 | 0.540 | |
1.900 | 7.0 | ||
1.950 | 12.0 | ||
2.000 | 15.0 | 2.62 | |
2.050 | 12.0 | ||
2.100 | 12.0 | ||
2.150 | 14.0 | ||
2.200 | 12.0 | ||
2.250 | 62.0 | ||
2.300 | 10.0 | ||
2.350 | 9.0 | ||
2.400 | 7.0 | ||
2.450 | 10.0 | ||
2.500 | 11.0 | ||
2.550 | 11.0 | ||
2.600 | 10.0 | ||
2.650 | 9.0 | ||
2.700 | 24.0 | ||
2.750 | 29.0 | ||
2.800 | 24.0 | 2.86 | |
2.850 | 24.0 | ||
2.900 | 23.0 | ||
2.950 | 24.0 | ||
2.970 | 0.661 | ||
3.000 | 26.0 | ||
3.050 | 25.0 | ||
3.100 | 27.0 | ||
3.150 | 24.0 | ||
3.200 | 22.0 | ||
3.250 | 20.0 | ||
3.300 | 24.0 | ||
3.350 | 26.0 | ||
3.400 | 23.0 | ||
3.450 | 27.0 | ||
3.500 | 27.0 | ||
3.550 | 23.0 | ||
3.600 | 22.0 | ||
3.650 | 23.0 | ||
3.700 | 16.0 | ||
3.750 | 17.0 | ||
3.800 | 20.0 | ||
3.850 | 24.0 | ||
3.900 | 22.0 | ||
3.950 | 18.0 | ||
4.000 | 18.0 | ||
4.050 | 19.0 | ||
4.100 | 22.0 | ||
4.150 | 21.0 | ||
4.200 | 10.0 | ||
4.250 | 25.0 | ||
4.300 | 34.0 | ||
4.350 | 25.0 | ||
4.400 | 20.0 | ||
4.450 | 24.0 | ||
4.500 | 29.0 | 2.88 | |
4.550 | 29.0 | ||
4.600 | 21.0 | ||
4.650 | 17.0 | ||
4.700 | 23.0 | ||
4.750 | 23.0 | ||
4.800 | 25.0 | ||
4.850 | 25.0 | ||
4.900 | 25.0 | ||
4.950 | 25.0 | ||
5.000 | 25.0 | ||
5.050 | 30.0 | ||
5.100 | 48.0 | ||
5.150 | 27.0 | ||
5.200 | 22.0 | ||
5.250 | 36.0 | ||
5.300 | 47.0 | ||
5.350 | 23.0 | ||
5.400 | 16.0 | ||
5.450 | 34.0 | ||
5.500 | 380.0 | ||
5.550 | 23.0 | ||
5.600 | 35.0 | 3.13 | 0.737 |
5.600 | 2.98 | ||
5.650 | 32.0 | ||
5.700 | 28.0 | ||
5.750 | 33.0 | ||
5.800 | 31.0 | ||
5.850 | 26.0 | ||
5.900 | 28.0 |