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- W2024957051 abstract "Leaching studies showed that shallow glacial soils that have become saline-sodic can be reclaimed with tile drains installed at a depth of 30 inches with a 30-foot spacing. The glacial till at the experimental site occurred at a depth of 2 to 3 feet below the surface and was slowly permeable. Only after the application of 71 inches of water was the saline-sodic soil sufficiently reclaimed to allow normal plant growth. Some decrease in salt concentration was found below the tile drains. There was no difference in salt movement with respect to proximity to the tile lines. The development of non-saline-sodic soils was not evident during the trial. Most of the gypsum applied during the trial remained in the surface 6 inches after the final water application." @default.
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- W2024957051 date "1962-02-01" @default.
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- W2024957051 title "RECLAMATION OF A SALINE-SODIC SOIL WITH SHALLOW TILE DRAINAGE" @default.
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- W2024957051 doi "https://doi.org/10.4141/cjss62-007" @default.
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