toyoovoS l\vC i^lt-^°°'/o62. A Quantitative Comparison of some Mechanisms Generating Overpressure in Sedimentary Basins Institutt for energiteknikk Institute for Energy Technology A quantitative comparison of some mechanisms generating overpressure sedimentary basins Magnus Wangen Institute for Energy Technology Box 40 N-2007 Kjeller NORWAY e-mail:
[email protected] tel: +47-6380-6259 fax: +47-6381-5553 Submitted October 30, 2000 Revised Mars 7, 2001 DISCLAIMER Portions of this document may be illegible in electronic image products. Images are produced from the best available original document. Performing Organisation Document no.: Date Institutt for energiteknikk IFE/KR/E-2001/002 2001-05-18 Kjeller Project/Contract no. and name Client/Sponsor Organisation and reference: Title and subtitle A Quantitative Comparison of some Mechanisms Generating Overpressure in Sedimentary Basins Authors) l\/j. 1 \ Reviewed >0 Approved Magnus Wan^cnj (j Tom Pedersen Tor Bjdmstad Abstract Expulsion of fluids in low permeable rock generate overpressure. Several mechanisms are suggested for fluid expulsion and overpressure build-up, and some of them have here been studied and compared. These are mechanical compaction, aquathermal pressuring, dehydration of clays, hydrocarbon generation and cementation of the pore space. A single pressure equation for these fluid expulsion processes has been studied. In particular, the source term in this pressure equation is studied carefully, because the source term consists of separate terms representing each mechanism for pressure build-up. The amount of fluid expelled from each mechanism is obtained from these individual contributions to the source term. It is shown that the rate of change of porosity can be expressed in at least two different ways for dehydration reactions and oil generation.