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The Effect of Aeration on Silica Scaling

Brown, K.L., McDowell, G.D.

Conference
New Zealand Geothermal Workshop
Year
1982
Session
Scaling
Language
English

Full text

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Abstract

Silica scaling rates have been measured for separated water at Ohaaki BR22 well. oxygen into separated water streams of differing temperatures has no effect on the rate of silica deposition, because the silica present has not polymerised. observed a silica scaling rate of 0.42 for a supersaturation level of 1.92 at of 8.9. The mechanism of silica scale formation probably involves cementation of preformed colloid particles onto the walls of the pipes. polymerisation of monomeric silica has been measured at three different temperatures and no induction period has been observed.

Copyright 1982, University of Auckland. 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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