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Nature of soil water

  • Paul R. Day*
  • , G.H. Bolt
  • , D.M. Anderson
  • *Corresponding author for this work

    Research output: Chapter in Book/Report/Conference proceedingChapterAcademicpeer-review

    Abstract

    This chapter deals with the properties of soil water which should be considered in any comprehensive theory of its behavior. The water present in the soil in its various stages of wetting has been described functionally by the terms hygroscopic, capillary, and gravitational water, and geometrically by the terms pendular and funicular water. It has been found that there are functional relationships between the water content and physical variables such as vapor pressure, matric suction and capillary or hydraulic conductivity. The forces acting on the soil water can be classified, for convenience, into matric forces (those which result from the presence of the solid phase), osmotic forces (those caused by dissolved solutes), and body forces (inertial forces and gravitational force). Calculations of energy relationships and potential distributions in the soil furnish the best means yet devised for explaining and predicting by a single theory most of the phenomena relating to soil water.

    Original languageEnglish
    Title of host publicationIrrigation of Agricultural Lands
    EditorsR.M. Hagan, H.R. Haise, T.W. Edminster
    PublisherWiley
    Chapter12
    Pages193-208
    Number of pages16
    Volume11
    ISBN (Electronic)9780891182061
    ISBN (Print)9780891180128
    DOIs
    Publication statusPublished - 1 Jan 1967

    Keywords

    • Body forces
    • Matric forces
    • Osmotic forces
    • Physical variables
    • Soil water suction
    • Soil-water relations
    • Water content

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