uncertainty of the soil erodibility factor (k), estimated using the usle nomograph in calcareous soils of hashtrood, (north-west of iran)

نویسندگان

علیرضا واعظی

حسینعلی بهرامی

سیدحمیدرضا صادقی

محمدحسین مهدیان

چکیده

in the universal soil loss equation (usle), soil erodibility factor (k) is estimated through nomograph. using the nomograph in calcareous soils may lead to uncertainty in estimating the erodibility factor. this study was conducted in hashtrud, (north west of iran) from march 2005 to march 2006. field measurements were carried out in an agricultural area of 30 km × 30 km. thirty six land grids were considered in the study area and three standard plots installed in a dry-farming land of each grid. k value was assessed based on soil loss per unit of the rainfall erosivity factor (r) and estimated using the usle nomograph. results indicated that the measured k value (0.0042 t h mj-1 mm-1) was on the average 10.98 times lower than the estimated value (0.0360 t h mj-1 mm-1). mean percentage error of the estimation was 974.6. these results reveal that using the nomograph leads to uncertainty of the soil erodibility factor in the study area. regression analysis showed that the soil erodibility factor is affected by mineral soil particles, organic matter, lime, and gravel (r2=0.85, p

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منابع مشابه

spatial variability of soil erodibility factor (k) of the usle in north west of iran

the soil erodibility factor varies spatially according to variations of some soil properties on the surface. this study was carried out to compare spatial variability of the soil erodibility factor as estimated and measured using the usle. the study was conducted in an agricultural zone with an area of in 900 km2 in hashtrood, northwestern iran. in the study area, 36 square grids with a dimensi...

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