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Information Journal Paper

Title

INVESTIGATING SPATIAL DISTRIBUTION CHARACTERISTICS OF RAINFALL EROSIVITY OVER HORMOZGAN PROVINCE, IRAN

Pages

  94-109

Abstract

 Introduction: Water and wind erosion are the two main causes of land degradation. The extent of water erosion is greater, and its outcomes are much more complicated, than the other types of erosion in Iran (Sadeghi et al.2011). Rainfall erosivity is one of the key parameters for SOIL EROSION risk assessment under future landuse and climate change (Meusburger et al.2012). Rainfall erosivity is the potential ability for rainfall to cause soil loss. Erosivity can be quantified by means of the R factor calculation of the universal soil loss equation (USLE). The universal soil loss equation (USLE) is a mathematical model to predict soil loss. Therefore, the awareness of its level and variation is critical to improve the management of the land. Thus, one can note that ISOERODENT MAPS are essential in evaluating the potential of SOIL EROSION over specific region. The objective of this study was to investigate the spatial pattern of R factor using the modified FOURNIER INDEX (MFI) over HORMOZGAN province…

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    APA: Copy

    ADELI, BEHZAD, GHOLAMI, H., & NAFARZADEGAN, A.R.. (2016). INVESTIGATING SPATIAL DISTRIBUTION CHARACTERISTICS OF RAINFALL EROSIVITY OVER HORMOZGAN PROVINCE, IRAN. QUANTITATIVE GEOMORPHOLOGICAL RESEARCHES, 5(2 ), 94-109. SID. https://sid.ir/paper/248975/en

    Vancouver: Copy

    ADELI BEHZAD, GHOLAMI H., NAFARZADEGAN A.R.. INVESTIGATING SPATIAL DISTRIBUTION CHARACTERISTICS OF RAINFALL EROSIVITY OVER HORMOZGAN PROVINCE, IRAN. QUANTITATIVE GEOMORPHOLOGICAL RESEARCHES[Internet]. 2016;5(2 ):94-109. Available from: https://sid.ir/paper/248975/en

    IEEE: Copy

    BEHZAD ADELI, H. GHOLAMI, and A.R. NAFARZADEGAN, “INVESTIGATING SPATIAL DISTRIBUTION CHARACTERISTICS OF RAINFALL EROSIVITY OVER HORMOZGAN PROVINCE, IRAN,” QUANTITATIVE GEOMORPHOLOGICAL RESEARCHES, vol. 5, no. 2 , pp. 94–109, 2016, [Online]. Available: https://sid.ir/paper/248975/en

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