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ABSTRACT
The absorbance at 1.94µ by a soil-methanol extract was used for measuring the soil water contents of three different textured soils. A linear relation between absorbance and soil water content was adequate for moisture determinations ranging from air dry to the moisture equivalent. For Quincy loamy sand and Barnes loam soils, calibration based only on laboratory standards was sufficient. For Houston Black clay, calibration against oven-dry samples was necessary. Determination time was approximately 1 hour.
1 Contribution from the Southern Plains Branch, Soil and Water Conservation Research Division, ARS, USDA.
2 Soil Scientists, US Agr. Water Quality Management Lab., Durant, Oklahoma 74701.
Received for publication May 24, 1972. Accepted for publication August 9, 1972.
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