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As a result, the Atchafalaya River was running high, soils were saturated and pools and other potential water storage areas were full.
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High soil aluminum and low soil calcium concentrations resulting from acid deposition have been implicated in this decline.
High soil-moisture levels favour development of destructive water mold fungi, such as species of Aphanomyces, Pythium, and Phytophthora.
This quantity is defined as the maximum annual rate of soil loss by erosion that will permit high soil productivity for an indefinite period of time.
The high soil compaction around the piospheres resulted in high soil bulk density and reduced soil porosity.
High soil erosion upstream from Gemesho is also attributed to the topography, high rainfall and comparatively high soil erodibility.
Plants use different strategies to deal with high soil salinity.
Our findings indicate a potential high soil erosion risk.
A high soil organic matter content strongly correlates with high nitrogen content.
Even with the SWC measures there are areas that will continue to have high soil erosion.
However, the relationship between termites' mounds and high soil moisture is scientifically well accepted.
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