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(B) Bulk thermal conductivity measured for core samples.
Significant clay content ranging from 8%to28%8% has been measured for core retrieved from the site, depending on locations and depth; illite and smectite are among the major clay minerals identified [40, 41].
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We compare the result of this model against experimental data measured for special core analysis of six different cores of carbonate rocks.
Cores were transferred to the laboratory within 2 h of collection and soil moisture was measured for each core using a soil moisture sensor (Dynamax ML2 ThetaProbe).
Inorganic element composition was measured for selected core profiles (LEF 44, 45, 47 and 50) using a NITON XL3t 900 GOLDD X-ray fluorescence (XRF) hand-held elemental analyzer (Thermo Scientific).
MPB production was measured for submerged core samples (collected from Daebu mudflat, Korea) at a fixed irradiance and temperature in the laboratory under the conditions of (1) constant light (data-I), (2) light dark incubation (data-II), and (3) in situ reflected (data-III).
NGR was not measured for these cores (Tada et al. 2015).
The quantity ℓ B /D cannot be measured for planetary cores, however.
The permeability measurements obtained here range between 3.5 and 6 microDarcy, which may appear higher than what is typically measured for shale cores (Tinni et al. 2012) and may correspond with a higher permeability zone.
Thermal conductivity values were measured for whole-round core samples (red circles), half-core samples (blue squares), and rock-chips samples (green triangles) retrieved from JFAST borehole C0019E.
Biocrust cover was measured for each 22 corecore using the point-intercept method.
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