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Effect of sand shape on evaporation from soil surface

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Summary

Loss of water through evaporation for different types of soils was examined. Soils were prepared from a clay soil and multiangular or platy sand in different proportions. The evaporation curves are of the type z=a+bx+cx2 but with different slopes. Both soils had the same percentage of clay and sand but platy-sand soils behaved as if they had a finer texture.

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References

  1. Alijai U H and Hulbert C 1970 Soil Sci. 110, 328–332.

    Google Scholar 

  2. Banin A and Amiel A 1969 Geoderma 3, 185–198.

    Google Scholar 

  3. Puech J et al. 1974 Comt. Rend. 284 Ser. D, 1045–1048.

    Google Scholar 

  4. Ritchie T J and Adams E J 1974 Soil Sci. Soc. Am. Pr. 38, 131–134.

    Google Scholar 

  5. Salter P J et al. 1966 J Soil Sci. 17, 93–98.

    Google Scholar 

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Misopolinos, N.D., Kalovoulos, J.M. Effect of sand shape on evaporation from soil surface. Plant Soil 80, 151–154 (1984). https://doi.org/10.1007/BF02232951

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  • DOI: https://doi.org/10.1007/BF02232951

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