Investigation of Water Erosion and Soil Loss Values with using the Measured Data from Cs-137 Method and Experimental Plots in Iran

Message:
Abstract:
Soil erosion is a serious issue in Iran. Determining the rate of soil erosion in various regions could help for better understanding of the erosion condition and soil conservation planning as well. In accordance with this constraint, more than 840 measured values derived from Cs-137 method and experimental plots in 31 research sites countrywide were collected, and analyzed related to different land uses, climates and slope classes. The existence of a few hundred times difference between cesium- 137 derived soil erosion and experimental plot's soil loss prevent us to combine these two sets of data. Comparison of the soil erosion and soil loss value in different land uses characterized the forest with minimum rate followed with ranges and dry farming respectively. Nevertheless, soil loss from poor ranges on marly formations was analyzed in a separate class due to nearly ten-fold differences with other ranges. Surface cover, tillage, and land sensitivity to the erosion are some factors that affect these differences. Comparison of two measured data sets in different climates indicated that the highest rates are generally matched to the Mediterranean climate. Lower soil loss in other regions could be related to the dense vegetation cover in humid area and low rainfall in arid climates correspondingly. Also, it is noted that apart from exceptional cases, the highest rate of soil erosion and soil loss are measured on gentle slopes between 1.5-12 percent which reduces by an increase in slope degree. The reduction of erosion rate in steeper slopes most probably relates to the abundance of surface gravel cover.
Language:
Persian
Published:
Journal of Watershed Management Research, Volume:6 Issue: 11, 2015
Pages:
137 to 151
https://www.magiran.com/p1423501  
سامانه نویسندگان
  • Arabkhedri، Mahmood
    Author (2)
    Arabkhedri, Mahmood
    Professor Water and soil conservation,
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