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Table T23. Results from APCT-3 temperature profiles, Site U1386.

Core Original
depth
(mbsf)
Tidal sea
level height*
(m)
Corrected
depth
(mbsf)
Minimum
temperature
(°C)
Minimum
temperature
prior to
mudline
(°C)
Average
temperature at
mudline
(°C)
In situ
temperature
(°C)
Thermal
resistance
(m2K/W)
339-U1386A-
4H 32.2 –0.2 33.3 12.93 13.19 13.54 14.20 22.6
7H 60.8 0.5 61.2 12.85 13.85 14.11 15.19 43.6
10H 89.3 0.8 89.4 13.01 13.51 14.30 16.14 67.4
13H 117.8 –0.3 119.0 12.82 14.03 14.20 17.05 93.8
16H 144.0 –0.8 145.7 12.59 13.99 14.20 18.09 114.4
19H 167.2 –0.3 168.4 12.54 13.64 14.01 18.88 131.2
Average: 12.79 13.70 14.06    
339-U1386B-
2H 16.8 0.4 17.3 13.44 13.50 13.59 13.56 11.7
5H 45.3 –0.4 46.6 13.34 13.34 13.56 14.85 32.0
8H 73.8 –0.75 75.45 13.84 13.84 14.04 15.75 55.6
11H 102.3 –0.45 103.65 13.92 13.92 14.20 16.67 80.1
14H 130.5 0.25 131.15 13.68 14.06 14.20 17.64 103.5
17H 157.6 0.5 158 13.67 14.05 14.40 18.46 123.6
Average: 13.65 13.78 14.00    

* = –0.9 m tidal height when mudline Core 339-U1386-1H 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, 2013b]).

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