Udic moisture regime
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Wikipedia
The udic moisture regime is common to soils of humid climates which have well-distributed rainfall, or which have enough rain in summer so that the amount of stored moisture plus rainfall is approximately equal to, or exceeds, the amount of evapotranspiration. Water moves down through the soil at some time in most years.
Some soil suborders, like udalf (alfisol) and udept (inceptisol), have a udic moisture regime.
See also
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Last updated on Monday April 28, 2008 at 18:52:56 PDT (GMT -0700)
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This article is licensed under the GNU Free Documentation License.
Last updated on Monday April 28, 2008 at 18:52:56 PDT (GMT -0700)
View this article at Wikipedia.org - Edit this article at Wikipedia.org - Donate to the Wikimedia Foundation
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