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hygroscopic coefficient |
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hygroscopic coefficient [¦hī·grə¦skäp·ik ‚kō·i′fish·ənt] (hydrology) The percentage of water that a soil will absorb and hold in equilibrium in a saturated atmosphere. How to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit webmaster's page for free fun content. |
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