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Cites:

1

Information Journal Paper

Title

PARTICLE SIZE DISTRIBUTION OF SURFACE-ERODED SOIL IN DIFFERENT RAINFALL INTENSITIES AND SLOPE GRADIENTS

Pages

  216-229

Abstract

 Introduction: Soil water erosion on the slope lands involves detachment, transport and deposition of soil materials due to erosive forces of raindrops and surface RUNOFF. Surface RUNOFF can produce relatively high soil loss and is often the dominant hillslope erosion process. The rate of surface RUNOFF which controls surface erosion on the uniform areas in the hillsolpes, is dependent on rainfall intensity and slope steepness. In various studies, the relationships between rainfall characteristics and surface RUNOFF were well known. Many studies have been performed on the relationship between RUNOFF and rainfall characteristics and soil loss. …

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  • Cite

    APA: Copy

    VAEZI, A.R., & EBADI, M.. (2017). PARTICLE SIZE DISTRIBUTION OF SURFACE-ERODED SOIL IN DIFFERENT RAINFALL INTENSITIES AND SLOPE GRADIENTS. JOURNAL OF WATER AND SOIL (AGRICULTURAL SCIENCES AND TECHNOLOGY), 31(1 ), 216-229. SID. https://sid.ir/paper/141694/en

    Vancouver: Copy

    VAEZI A.R., EBADI M.. PARTICLE SIZE DISTRIBUTION OF SURFACE-ERODED SOIL IN DIFFERENT RAINFALL INTENSITIES AND SLOPE GRADIENTS. JOURNAL OF WATER AND SOIL (AGRICULTURAL SCIENCES AND TECHNOLOGY)[Internet]. 2017;31(1 ):216-229. Available from: https://sid.ir/paper/141694/en

    IEEE: Copy

    A.R. VAEZI, and M. EBADI, “PARTICLE SIZE DISTRIBUTION OF SURFACE-ERODED SOIL IN DIFFERENT RAINFALL INTENSITIES AND SLOPE GRADIENTS,” JOURNAL OF WATER AND SOIL (AGRICULTURAL SCIENCES AND TECHNOLOGY), vol. 31, no. 1 , pp. 216–229, 2017, [Online]. Available: https://sid.ir/paper/141694/en

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