Effect of Climate Changes and Coefficient of Surface Roughness on Soil Loss by Wind Erosion in Some Central and Southern Iraq

M. Al-Rawi
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Abstract

"act Woodruff and siddoway, 1965, established an equation for the estimation of soil Loss by wind erosion called Wind Erosion Equation (WEQ); solution of this equation gives the maximum amount of wind erosion under certain field conditions and is considered evidence in identifying the necessary methods for treating wind erosion in those conditions (Eltaif et al.,1991). This study aims to find out the extent to which climate change in the Samawah region of southern Iraq and Baghdad in central Iraq over a period of 34 years has affected values of soil losing by wind erosion using equation of (woodruff and siddoway, 1965) and effectiveness of this changes in soil surface roughness factor in reducing or increasing these loss. Two sites were selected located within central and southern regions of Iraq, one in Al-Jadiriya area in Baghdad governorate and the other in Samawah area in Al-Muthanna governorate. The results showed that estimated soil losing for years (1980-2013) in Al-Jadiriya decrease annually by 10-30 kg.hec.-1.year-1, while samawah increase by 240-760 kg.hec.-1.year-1. The effect of surface roughness factor was significant in reducing soil loss during period of study. Roughness factor for ridge (0.5) has reduced soil losing by 2.6 times compared to non-ridge soils (1).The ratio in semi-bridge soil (0.75) was 65%. This is due to the impact of bridge in reducing wind speed and reducing its erosivity. The general direction of soil loss indicates decrease in Al-Jadiriya area and increase in Samawah area with the case of fluctuation in soil loss between high and low of general direction line due to climate factor (C) in general equation of soil loss and it reflects ability of wind erosion, so decreased when wet conditions improved, by increased rainfall, reduced evaporation and increasing when dry conditions dominate Corresponding author: E-mail( mohammed.alrawi@coagri.uobaghdad.edu.iq ) All rights reserved AlMuthanna University"
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气候变化和地表粗糙度系数对伊拉克中部和南部部分地区风蚀土壤流失的影响
act Woodruff和siddoway(1965)建立了估算风蚀土壤流失量的方程,称为风蚀方程(wind erosion equation, WEQ);该方程的解给出了在某些野外条件下的最大风蚀量,并被认为是确定在这些条件下处理风蚀的必要方法的证据(Eltaif et al.,1991)。本研究旨在利用(woodruff and siddoway, 1965)方程,找出伊拉克南部Samawah地区和伊拉克中部巴格达34年间气候变化对土壤风蚀损失量的影响程度,以及土壤表面粗糙度因子的变化对减少或增加土壤风蚀损失量的有效性。选定的两个地点位于伊拉克中部和南部地区,一个在巴格达省的Al-Jadiriya地区,另一个在Al-Muthanna省的Samawah地区。结果表明,Al-Jadiriya地区1980-2013年土壤流失量每年减少10-30 kg.hec. 1。而samawah每年增加240-760公斤。研究期间,地表粗糙度因子对减少土壤流失量的作用显著。与非垄土相比,垄土的粗糙度系数(0.5)减少了2.6倍的土壤流失量(1),半桥土的粗糙度系数(0.75)为65%。这是由于桥梁在降低风速和降低其侵蚀力方面的作用。土壤流失量的总方向为Al-Jadiriya地区减少,Samawah地区增加,在土壤流失量的总方向线上下波动的情况下,受土壤流失量总方程中的气候因子(C)的影响,土壤流失量反映风蚀能力,湿润条件改善时土壤流失量减少,降雨增加,蒸发减少,干燥条件下土壤流失量增加。E-mail(mohammed.alrawi@coagri.uobaghdad.edu.iq)版权所有
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