Spelling suggestions: "subject:"soilmoisture"" "subject:"highmoisture""
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A STUDY OF PARTIALLY SATURATED FLOW IN SAND-EPOXY RESIN COLUMNSCarney, John Bryan, 1921- January 1968 (has links)
No description available.
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Some effects of soil moisture on the growth of wheat (Triticum aestivum L. em Thell.)Intalap, Suhbawatr, 1937- January 1968 (has links)
No description available.
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The effects of three moisture levels applied to Lehman lovegrass grown on a fertilized desert grassland soilBentley, Russell Gordon, 1939- January 1964 (has links)
No description available.
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The penetration of moisture into soils as affected by chemical composition and physical properties of irrigation watersAyers, Alvin Dearing, 1909- January 1934 (has links)
No description available.
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The effect of mesquite control on the soil moisture content of mesquite-infested range land in Southern ArizonaMartin, S. Clark (Samuel Clark), 1916- January 1947 (has links)
No description available.
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Comparative analysis of the effect of a closed-loop irrigation system on crop yieldMatthews, John Homer 05 1900 (has links)
No description available.
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Soil moisture deficits and surpluses in south western Quebec.Lake, Edwin Berthrand. January 1968 (has links)
No description available.
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Observations of soil moisture changes in flat land soils in Quebec.Shrivastava, Naresh Chandra. January 1968 (has links)
No description available.
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Lightning polarity over soil moisture boundaries during three tornadic outbreaks (1990-95)Berry, Douglas P. January 2005 (has links)
This study presents an overview of lightning formation and the correlations seen with soil moisture slope along with potential of tornadic thunderstorms. Three moisture classes (large, marginal, small) were created using soil moisture observed during three tornado outbreaks (June-02-1990, April-26-1994, May-13-1995) over the Midwest. Chi-square, Nearest Neighbor, and Point Density calculations were performed and suggest that lightning polarity/frequency shift between soil moisture classes at a = .01. Using lightning characteristics in the thunderstorm lifecycle, one is able to evaluate relative tornadogenesis areas within moisture classes some 8-10 hours in advance. Tornadogenesis points fell within expected areas indicating that borders between marginal and small moisture classes are approximate locations of stage change (mature to dissipation) of the thunderstorm lifecycle. Results are intended to be used as a tool that helps verify situations that are more likely to be tornadic when observing real-time lightning data from thunderstorms crossing significant soil moisture boundaries. / Department of Geography
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Infiltration and water availability in the major soil series of Nevis, W. I.Hinds, Robert P. January 1971 (has links)
No description available.
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