1965Journal of Soil ScienceRequires access

THE INFLUENCE OF TEXTURE ON THE MOISTURE CHARACTERISTICS OF SOILS

P. J. Salter, J. B. WILLIAMS

Open publisher page 87 citations

Abstract

Summary The available‐water capacity of the top 2 ft of twenty‐seven soils of different texture has been determined, together with the moisture release characteristics of twenty of the soils. The moisture contents at field capacity and at the permanent wilting point increased as the soils became finer in texture but the medium‐textured soils held the greatest volume of available‐water. The available‐water capacities of the soils ranged from 0.77 in./ft depth in a sand to 3.12 in./ft in a silt loam and 3.13 in./ft in a peat. Clay soils held approximately 1.95 in./ft. The effects of soil texture and other factors affecting the available‐water capacities and moisture release characteristics of soils are discussed.

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Summary The available‐water capacity of the top 2 ft of twenty‐seven soils of different texture has been determined, together with the moisture release characteristics of twenty of the soils. The moisture contents at field capacity and at the permanent wilting point increased as the soils became finer in texture but the medium‐textured soils held the greatest volume of available‐water. The available‐water capacities of the soils ranged from 0.77 in./ft depth in a sand to 3.12 in./ft in a silt loam and 3.13 in./ft in a peat. Clay soils held approximately 1.95 in./ft. The effects of soil texture and other factors affecting the available‐water capacities and moisture release characteristics of soils are discussed.

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Available abstract

Summary The available‐water capacity of the top 2 ft of twenty‐seven soils of different texture has been determined, together with the moisture release characteristics of twenty of the soils. The moisture contents at field capacity and at the permanent wilting point increased as the soils became finer in texture but the medium‐textured soils held the greatest volume of available‐water. The available‐water capacities of the soils ranged from 0.77 in./ft depth in a sand to 3.12 in./ft in a silt loam and 3.13 in./ft in a peat. Clay soils held approximately 1.95 in./ft. The effects of soil texture and other factors affecting the available‐water capacities and moisture release characteristics of soils are discussed.

Key concepts: Soil water, Loam, Permanent wilting point, Soil texture, Moisture, Water content, Field capacity, Environmental science

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