No abstract

With the expansion of irrigated agriculture throughout the world, much land now saline or alkaline must be reclaimed. Reported herein are the results of both flushing and leaching salts from a saline-alkali soil in the Coachella Valley of California's Colorado Desert. The paper presents a quantitative evaluation of the effectiveness of removing a salt crust by flushing, and it compares the removal of the usual salts with the re moval of a high concentration of boron. Flushing as a reclamation procedure was found to be ineffective. Leaching was found to remove 80 per cent of the initially high salts with the application of one foot of water for each foot depth of soil considered. Equal leaching of boron required three times as much water.

Tile drainage effluent from systems on irrigated land in the San Joaquin Valley of California was analyzed for nitrogen and phosphorus and the quantity of each element found was correlated with the quantity of N and P applied for four different cropping patterns. Large percentages of applied N were found to be lost in tile drainage effluent. Phosphorus losses were not significant.

A four‐year study of drainage effluent obtained from 15 tile drainage systems located in the arid San Joaquin Valley of California showed that the concentration of salts and the various ions discharged in the tile effluent decreased, logarithmically, from the time that the tile systems were installed. Regression equations and correlation coefficients are presented for total salts, boron, sodium, calcium plus magnesium, chloride and sulfate ions, versus time from 0 to 12 years of tile drainage system age. The relationships presented could change with more intensive drainage and more liberal use of irrigation water, providing a more rapid trend toward equilibrium.