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Soil salinity on Tulelake lands

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Authors

James N. Luthin, University of California, Davis.
Kenneth Baghott, Modoc-Siskiyou Counties, University of California.

Publication Information

California Agriculture 14(3):12-12.

Published March 01, 1960

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Abstract

Water moves upward from the water table level by capillary action to the soil surface and evaporates, leaving the salts in the soil. However, the water table must be close to the soil surface for long periods of time for the upward movement and evaporation of the water to take place. Poor soil drainage and inadequate control of irrigation water contribute to the salinity problem.

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Soil salinity on Tulelake lands

James N. Luthin, Kenneth Baghott
Webmaster Email: bjnoel@ucanr.edu

Soil salinity on Tulelake lands

Share using any of the popular social networks Share by sending an email Print article
Share using any of the popular social networks Share by sending an email Print article

Authors

James N. Luthin, University of California, Davis.
Kenneth Baghott, Modoc-Siskiyou Counties, University of California.

Publication Information

California Agriculture 14(3):12-12.

Published March 01, 1960

PDF  |  Citation  |  Permissions

Author Affiliations show

Abstract

Water moves upward from the water table level by capillary action to the soil surface and evaporates, leaving the salts in the soil. However, the water table must be close to the soil surface for long periods of time for the upward movement and evaporation of the water to take place. Poor soil drainage and inadequate control of irrigation water contribute to the salinity problem.

Full text

Full text is available in PDF.

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