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That is why, the flux detection probe (FDP) ended up being designed that employs electrogeophysical dimensions to estimate in situ sediment porosity, that can easily be used to convert pore water velocity to Darcy flux. Dynamic pore water velocity is acquired by monitoring fluid conductivity and temperature along the FDP probe. Stress sensors deployed at the top and bottom for the probe give you the additional information required to estimate vertical permeability. This study
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