Pecher, Ingo A; Villinger, Heinrich; Kaul, Norbert; Crutchley, Gareth J; Mountjoy, Joshu J; Huhn, Katrin; Kukowski, Nina; Henrys, Stuart A; Rose, Paula S; Coffin, Richard C (2017): Heat flow data at station SO247_55-13 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.878095, In supplement to: Pecher, Ingo A; Villinger, Heinrich; Kaul, Norbert; Crutchley, Gareth J; Mountjoy, Joshu J; Huhn, Katrin; Kukowski, Nina; Henrys, Stuart A; Rose, Paula S; Coffin, R B (2017): A Fluid Pulse on the Hikurangi Subduction Margin: Evidence From a Heat Flux Transect Across the Upper Limit of Gas Hydrate Stability. Geophysical Research Letters, 44(24), 12,385-12,395, https://doi.org/10.1002/2017GL076368
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Coverage:
Latitude: -38.647530 * Longitude: 178.670120
Date/Time Start: 2016-04-13T14:40:15 * Date/Time End: 2016-04-13T14:40:15
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 5.199 m
Event(s):
SO247_55-13 (GeoB20837-13) * Latitude: -38.647530 * Longitude: 178.670120 * Date/Time: 2016-04-13T14:40:15 * Elevation: -668.0 m * Location: South Pacific Ocean * Campaign: SO247 (SLAMZ) * Basis: Sonne_2 * Method/Device: Heat-Flow probe (HF) * Comment: HF1625P13
Comment:
Depth, sediment = Penetration depth
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Kaul, Norbert | Geocode | |
2 | Sample code/label | Sample label | Kaul, Norbert | Sensor | ||
3 | Depth, relative | Depth rel | m | Kaul, Norbert | relative to top of heat flow probe | |
4 | Temperature, in rock/sediment | t | °C | Kaul, Norbert | Heat flow probe | |
5 | Conductivity, thermal | k | W/m/K | Kaul, Norbert | ||
6 | Conductivity, thermal | k | W/m/K | Kaul, Norbert | assumed | |
7 | Integrated thermal resistance | ITR | m2 K/W | Kaul, Norbert | Calculated | Bullarad depth |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
117 data points
Data
1 Depth sed [m] | 2 Sample label (Sensor) | 3 Depth rel [m] (relative to top of heat flow ...) | 4 t [°C] (Heat flow probe) | 5 k [W/m/K] | 6 k [W/m/K] (assumed) | 7 ITR [m2 K/W] (Bullarad depth, Calculated) |
---|---|---|---|---|---|---|
0.000 | 21 | -1.62 | 5.8595 | 1.1 | -1.623 | |
0.260 | 20 | -1.36 | 5.8687 | 1.1 | -1.363 | |
0.520 | 19 | -1.10 | 5.8594 | 1.1 | -1.103 | |
0.780 | 18 | -0.84 | 5.8630 | 1.1 | -0.844 | |
1.040 | 17 | -0.58 | 5.8572 | 1.1 | -0.584 | |
1.300 | 16 | -0.32 | 5.8606 | 1.1 | -0.324 | |
1.560 | 15 | -0.06 | 5.8492 | 1.1 | -0.064 | |
1.820 | 14 | 0.20 | 5.7597 | 1.1 | 0.183 | |
2.079 | 13 | 0.46 | 5.7755 | 1.07 | 1.1 | 0.427 |
2.339 | 12 | 0.72 | 5.8102 | 1.03 | 1.1 | 0.675 |
2.599 | 11 | 0.98 | 5.8472 | 1.1 | 0.925 | |
2.859 | 10 | 1.24 | 5.8715 | 1.12 | 1.1 | 1.158 |
3.119 | 9 | 1.50 | 5.8826 | 1.17 | 1.1 | 1.385 |
3.379 | 8 | 1.76 | 5.8760 | 1.17 | 1.1 | 1.607 |
3.639 | 7 | 2.02 | 5.8895 | 1.20 | 1.1 | 1.825 |
3.899 | 6 | 2.28 | 5.8917 | 1.22 | 1.1 | 2.040 |
4.159 | 5 | 2.54 | 5.8966 | 1.27 | 1.1 | 2.249 |
4.419 | 4 | 2.80 | 5.9097 | 1.31 | 1.1 | 2.452 |
4.679 | 3 | 3.06 | 5.9129 | 1.27 | 1.1 | 2.652 |
4.939 | 2 | 3.32 | 5.9288 | 1.43 | 1.1 | 2.845 |
5.199 | 1 | 3.58 | 5.9268 | 1.37 | 1.1 | 3.031 |