Stock, Oliver; Melles, Martin (2006): Water content of sediment core PG1127-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.399025
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Stock, Oliver (1997): Rekonstruktion der holozänen Entwicklungsgeschichte des Pjassinosees mit Hilfe von Seesedimenten. Diploma Thesis, University Potsdam, 67 pp
Project(s):
Funding:
Fourth Framework Programme (FP4), grant/award no. MAS3980185: Quaternary Environment of the Eurasian North
Coverage:
Latitude: 70.028330 * Longitude: 87.811660
Minimum DEPTH, sediment/rock: 0.010 m * Maximum DEPTH, sediment/rock: 0.480 m
Event(s):
PG1127-1 * Latitude: 70.028330 * Longitude: 87.811660 * Lake water depth: 10.9 m * Penetration: 0.57 m * Recovery: 0.57 m * Campaign: RU-Land_1993_Norilsk_Taymyr (Norilsk/Taymyr93) * Basis: AWI Arctic Land Expedition * Method/Device: Gravity corer Potsdam (SL_P)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Water content, wet mass | Water wm | % | Melles, Martin |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
48 data points
Data
1 Depth sed [m] | 2 Water wm [%] |
---|---|
0.010 | 56.20 |
0.020 | 57.60 |
0.030 | 46.38 |
0.040 | 47.03 |
0.050 | 51.78 |
0.060 | 52.65 |
0.070 | 52.94 |
0.080 | 52.92 |
0.090 | 46.88 |
0.100 | 49.49 |
0.110 | 50.87 |
0.120 | 51.39 |
0.130 | 49.22 |
0.140 | 47.97 |
0.150 | 48.81 |
0.160 | 49.20 |
0.170 | 47.59 |
0.180 | 46.25 |
0.190 | 44.93 |
0.200 | 44.83 |
0.210 | 43.48 |
0.220 | 43.64 |
0.230 | 45.49 |
0.240 | 42.11 |
0.250 | 41.04 |
0.260 | 44.43 |
0.270 | 44.55 |
0.280 | 42.01 |
0.290 | 43.75 |
0.300 | 43.60 |
0.310 | 43.91 |
0.320 | 42.21 |
0.330 | 41.23 |
0.340 | 40.36 |
0.350 | 40.36 |
0.360 | 38.16 |
0.370 | 38.64 |
0.380 | 40.17 |
0.390 | 42.53 |
0.400 | 40.27 |
0.410 | 40.57 |
0.420 | 40.22 |
0.430 | 40.01 |
0.440 | 41.16 |
0.450 | 39.27 |
0.460 | 38.27 |
0.470 | 37.66 |
0.480 | 38.82 |