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Modelling of Chemical and Thermal Changes in Well PN-26, Palinpinon Philippines

R.C.M. Malate and M.J. OĆ­Sullivan

Location
Palinpinon, Philippines; Negros
Conference
Stanford Geothermal Workshop
Year
1990
Session
Geochemistry/Modeling
Language
English

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Abstract

Significant chloride changes in well PN-26 during its period of exploitation have been mainly attributed to reinjection fluid returns. Here fluid returns are modelled by a simple time-dependent production-reinjection lumped parameter model. Analytic solutions are derived for the cases of constant and variable production rates. The variable production rate model adequately described the chloride changes in well PN-26. The early return of reinjection fluid has also resulted in a substantial decline in the measured temperam in the well. This change in temperature is modelied by coupling the mass balance model to a frslcture flow modeLThe simple heat advection model satisfactorily represents the thermal decline observed in the well.

Copyright 1990, Stanford Geothermal Program. Readers who download papers from this site should honour the copyright of the original authors, and may not copy or distribute the work further without the permission of the original publisher.

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