Talk:Capillary fringe

WikiProject class rating
This article was automatically assessed because at least one WikiProject had rated the article as stub, and the rating on other projects was brought up to Stub class. BetacommandBot 09:45, 10 November 2007 (UTC)

External links modified
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 * Added archive https://web.archive.org/web/20051112143423/http://wlapwww.gov.bc.ca:80/wat/gws/gwbc/C02_origin.html to http://wlapwww.gov.bc.ca/wat/gws/gwbc/C02_origin.html

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Definition
As I was expanding the references, I decided to temporarily organize by which of three definitions the reference adheres to]. Unsaturated capillary flow is very important to understanding salinization of soils, b/c sometimes capillary action delivers salts several feet vertically to accumulate evaporation on the soil surface. If you went by a saturated-only definition, the article might not appreciate that behavior in groundwater. Yet I can see how unsaturated capillary flow would not be at all important to a geologist for understanding groundwater flow, contamination, plumes and such. -- Paleorthid (talk) 23:46, 12 January 2019 (UTC)