A well‐known parameter in electrical bore‐hole logging is the formation factor (formation resistivity/pore‐water resistivity) and its relationship to formation porosity (or void ratio). This in turn can be used to give an assessment of the foundation characteristics of a saturated sand. To use this relationship in marine sediment investigation's, a device has been constructed which measures the resistivity of a seafloor sand by passing a focused current into the sediment from a superior position, rather than by physically penetrating the sediment with an electrode array which would inevitably produce a mechanical disturbance. At present, the investigated depth (which is a function of the size of the electrode array) relates to a zone within 0.5 m of the water‐sediment interface. Knowing the sediment resistivity, the formation factor can be determined from a separate assessment of the pore‐water resistivity. The formation factor is empirically related to the porosity of the sand by means of a graph prepared from measurements made in a formation factor‐porosity cell, which allows both parameters to be determined simultaneously throughout a range of packing conditions. From the determination of in‐situ porosity the relative density of the sand can be subsequently calculated.
No takes yet. Share an insight, caveat, or question.
Peter D. Jackson (1975) studied this question.
Synapse has enriched 4 closely related papers on similar clinical questions. Consider them for comparative context: