Published on 29 September 2010

Porosity of Mini Cores (Plugs) of the KTB Main Hole HB1d

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KTB, WG Geophysics

Description

The porosity was determined using the most common Archimedian method (Schopper, 1982). It is based on the following three weight determinations of the sample: (1) The samples were dried for approximately 100 hours at 80 °C in an oven until the sample weight remains constant. The pore space is filled with air. (2) The samples were saturated, i.e. the pore space was completely filled with destilled water. Therefore, at room temperature and under vacuum the samples were submerged in destilled water for at least 24 hours. Afterwards atmospheric pressure was applied for at least 24 hours to let the water invade into the sample. The sample was taken from the water and the fluid film on the sample surface was removed. (3) At least, the saturated samples were submerged again in destilled water and the third measurement was done. An apparent mass due to buoyancy was determined.

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Metrics

Dataset Index

0.3

FAIR Score

15%

Citations

0

Mentions

0

Metrics Over Time

Publication Details

DOI

Publisher

Deutsches GeoForschungsZentrum GFZ

Assigned Domain

Subfield

Pharmacology

Field

Medicine

Domain

Health Sciences

Confidence Score

86%

Source

Open Alex

Keywords

German Continental Deep Drilling ProgramLand basedcalculationDate of SamplingDensityMatrix DensityPorosity

Normalization Factors

FT

15.38

CTw

1.00

MTw

1.00