5. Compute the equivalent mud density in the annulus if the mud density entering the well is 9 Ibm/gal and the ROP is 100 ft/hr. Assume a vertical wellbore and a flow rate of 600 gal/min, a bit size of 9.875 in., a pipe OD of 7 in., and a rock bulk density of 2.2 g/ cm3 (HINT: compute cuttings concentration first).

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Principles of Seepage

In hydrology, when water flows down in a pore or crack of unsaturated soil due to gravity, the deep layer of soil is called seepage. It is the slow movement of water in the soil layer. Seepage is mainly found near hydraulic structures and is responsible for the stability of earthen-type hydraulic structures.