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Water movement through Panoche clay loam soil

Author

Listed:
  • Nielsen, V
  • Davidson, J. M.
  • Biggar, J. W.
  • Miller, R. J.

Abstract

Water movement through Panoche clay loam is explained on the basis of the soil-water properties within the profile. Laboratory-determined soil water content-tension relations from 3-inch cores taken from the field every 6 inches to 5 feet were shown to provide reliable estimates of soil water behavior. Water management practices relative to favorable plant-available soil water and favorable salt balance within the profile are discussed.

Suggested Citation

  • Nielsen, V & Davidson, J. M. & Biggar, J. W. & Miller, R. J., 1964. "Water movement through Panoche clay loam soil," Hilgardia, California Agricultural Experiment Station, vol. 35(17).
    • Handle: RePEc:ags:hilgar:381904
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    File URL: https://ageconsearch.umn.edu/record/381904/files/v35n17p491.pdf
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