Table T19. Results from APCT-3 temperature profiles, Site U1390.
| Hole, core |
Original depth (mbsf) |
Tidal sea level height* (m) |
Corrected depth (mbsf) |
In situ temperature (°C) |
Thermal resistance (m2K/W) |
|---|---|---|---|---|---|
| 339-U1390A- | |||||
| 4H | 32.1 | 0.3 | 31.55 | 14.2 | 26.0 |
| 7H | 60.6 | 0.5 | 59.85 | 15.12 | 46.8 |
| 339-U1390B- | |||||
| 2H | 18.6 | –0.7 | 19.05 | 13.56 | 15.7 |
| 5H | 47.1 | 0 | 46.85 | 14.51 | 38.3 |
| 8H | 75.6 | 0.6 | 74.75 | 15.34 | 57.8 |
| 339-U1390C- | |||||
| 3H | 23.4 | –0.8 | 23.95 | 13.6 | 19.2 |
| 6H | 51.9 | 0.4 | 51.25 | 14.86 | 41.4 |
| 9H | 80.4 | 0.8 | 79.35 | 15.42 | 60.8 |
| 12H | 108.9 | 0.1 | 108.55 | 16.5 | 83.9 |
* = –0.25 m tidal height when mudline Core 339-U1390A-1H was taken. In situ temperatures were determined using TP-Fit software by Martin Heesemann. Thermal resistance was calculated from thermal conductivity data (see “Physical properties”) corrected for in situ conditions (see “Downhole measurements” in the “Methods” chapter [Expedition 339 Scientists, 2012b]).
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