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Abstract
This paper is written to analyse the variation of water production due to compaction in a field in Venezuela. The producing water, after being analysed, was suspected not from aquifer. So where does the water come from? The results shows that pore structures of reservoir changed, and producing water is due to volume changes of immobile water and mobile water as the result of compaction. It means that relative permeability curves have changed when rock deforms.
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Article Details
Issue: Vol 14 No 2 (2011)
Page No.: 38-53
Published: Jun 30, 2011
Section: Sciences of Earth and Environment - Research article
DOI: https://doi.org/10.32508/stdj.v14i2.1916
Copyright Info
Copyright: The Authors. This is an open access article distributed under the terms of the Creative Commons Attribution License CC-BY 4.0., which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
How to Cite
Ta, D., & Behrenbruch, P. (2011). ESTIMATION OF NEW RELATIVE PERMEABILITY CURVES DUE TO COMPACTION CASE STUDY AT BACHAQUERO FIELD – VENEZUELA. Science and Technology Development Journal, 14(2), 38-53. https://doi.org/https://doi.org/10.32508/stdj.v14i2.1916
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