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Disposal of Flashed Brine Dosed with CaCO3 Scale Inhibitor: What Happens when the Inhibitor is Exhausted

D.E. Michels

Location
East Mesa, California; Imperial Valley
Conference
Stanford Geothermal Workshop
Year
1983
Session
Injection
Language
English

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Abstract

A freshly flashed geothermal liquid, previously dosed wlth inhibitor and supersaturated with calcite was injected into another well where It displaced an unflashed counterpart of itself around the wellbore. Back-production of the injectate, and subsequently the natlve fluid, has yielded data for the rate that a scale inhibitor is degraded after injection. The circumstance also dlsplays a novel mechanism whereby two fluids that do not physically mix nevertheless react wlth one another through the reservoir rock's serving a role of intermediary. The results have been further interpreted to conclude that in some circumstances a short lifetime for the scale inhibitor is not necessarily a problem for long-term lnjection.

Copyright 1983, 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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