1,721,230 research outputs found
Heat flow data at station HF1620 during RV SONNE cruise SO247
No full textWe used the 6 m long Bremen heat flow probe also called Giant Heat Flow Probe (GHF). The heat probe is constructed in the classical “violin bow” design (Hyndman et al., 1979; Hartmann and Villinger, 2002, Villinger et al., 2010), with 21 thermistors distributed over an active length of 5.2 m in 0.26 m intervals mounted inside an oil filled hydraulic tube (O.D. 14 mm) which is attached to the strength member (O.D. 130 mm). The sensor tube also contains a heater wire for the generation of high energy heat pulses of typically on the order of 800 J/m for in situ thermal conductivity measurements according to the pulsed needle probe method (Lister, 1979). A calibrated PT-100 seawater sensor on top of the weight stand allows to measure the absolute bottom water temperature and to check the calibration of the sensor string in deep water with high accuracy. Inclination and acceleration of the probe is measured to monitor the penetration process into the sediments and potential disturbances during the actual measurement period
M162 GLORIA-FLOW, Heat flow data at station HF2003
No full textHeat flow data, taken with the 6 m Bremen heat probe during M162 in the Gulf of Cadiz. Heat flow data were measured across fault zones to support the idea of fluid transport along leaking faults
Heat flow data at station HF2021 during RV SONNE cruise SO278
No full textStation HF2021 pentration 1 - 11 temperature-time raw data in ASCII Format. Temperature in Milli Kelvin (mK) and time in GMT, 1 second sample interval. Results of heat flow station HF2021, penetrations 1 - 13, results of in-situ temperatures and thermal conductivities in depth dependent order. Temperature is in Degree Celsius (°C), thermal conductivity in (W/m*K). Thermal conductivity can be measured or set
Marine heat flow data at station HF2211 sampled during RV METEOR cruise M183
No full textHeat flow data, sampled during M183 within the RIFLOR project. Locations are along the Mid Atlantic ridge between 57° 29'N and 58° 18'N, mainly within the denominated Squid Pond. We used the 6 m Bremen heat probe with 21 channels. In-situ temperatures and thermal conductivities were derived using MHFRED, according to the inversion method of Villinger and Davis (2007)
Marine heat flow data at station HF2221 sampled during RV METEOR cruise M183
No full textHeat flow data, sampled during M183 within the RIFLOR project. Locations are along the Mid Atlantic ridge between 57° 29'N and 58° 18'N, mainly within the denominated Squid Pond. We used the 6 m Bremen heat probe with 21 channels. In-situ temperatures and thermal conductivities were derived using MHFRED, according to the inversion method of Villinger and Davis (2007)
Marine heat flow data at station HF2217 sampled during RV METEOR cruise M183
No full textHeat flow data, sampled during M183 within the RIFLOR project. Locations are along the Mid Atlantic ridge between 57° 29'N and 58° 18'N, mainly within the denominated Squid Pond. We used the 6 m Bremen heat probe with 21 channels. In-situ temperatures and thermal conductivities were derived using MHFRED, according to the inversion method of Villinger and Davis (2007)
Marine heat flow data at station HF2213 sampled during RV METEOR cruise M183
No full textHeat flow data, sampled during M183 within the RIFLOR project. Locations are along the Mid Atlantic ridge between 57° 29'N and 58° 18'N, mainly within the denominated Squid Pond. We used the 6 m Bremen heat probe with 21 channels. In-situ temperatures and thermal conductivities were derived using MHFRED, according to the inversion method of Villinger and Davis (2007)
Marine heat flow data at station HF2218 sampled during RV METEOR cruise M183
No full textHeat flow data, sampled during M183 within the RIFLOR project. Locations are along the Mid Atlantic ridge between 57° 29'N and 58° 18'N, mainly within the denominated Squid Pond. We used the 6 m Bremen heat probe with 21 channels. In-situ temperatures and thermal conductivities were derived using MHFRED, according to the inversion method of Villinger and Davis (2007)
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