IMPACT OF CONTROLLED AND FREE DRAINAGE ON SOIL SALINITY IN MARDAN SCARP, THROUGH LONG TERM SIMULATION OF SOLUTE TRANSPORT MODEL ( LEACHC)

G. Khan, Daulat Khan, K. A. Khan, Akhtar Ali, M. Nazeer
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Abstract

Field study was conducted to determine the impact of controlled and free drainage on soil salinity from September 2004 to September 2005 in drainage unit 106 for long term simulation of solute transport of Mardan Salinity Control and Reclamation Project (SCARP) NWFP Pakistan. Leaching Estimation and Chemistry (LEACHC) model was calibrated for 44 days. The model was simulated for one, two and five years respectively, under controlled and free drainage at one meter water table depth. Simulation indicated different patterns of salinity related to water table depths under each condition. In controlled condition, the salt trend to accumulate at the upper part of root zone mainly due to evaporation. While the salinity under free condition showed fluctuation according to the actual field condition. Result indicated that at controlled drainage of 1.0m watertable depth, soil electrical conductivity (EC) increased to 2.42 dS/ m, 3.97 dS/ m and 6.14 dS/ m after 1, 2 and 5 years of simulation at 12.5 cm depth, while 1.78, 1.92 and 2.27 dS/m at depth of 62.5 cm respectively. At 2.0 m watertable depth EC increased to 1.9 dS/ m, 2.2 and 3.8 dS/m at a depth of 12.5 cm, while at a depth of 62.5 cm EC reached to 1.8, 1.98 and 3.8 dS/m respectively. For free drainage EC decreased from 0.94 dS/m to 1.13 dS/m at depths of 12.5 and 62.5 cm respectively. The soil salinity was increased with rising of water table under controlled drainage and it decreased in case of free drainage. It is concluded that LEACHC is a valid model for simulation of solute transport and it is applicable to soil salinity status of Mardan SCARP.
控制和自由排水对马尔丹陡坡土壤盐分的影响——基于溶质运移模型(淋滤)的长期模拟
2004年9月至2005年9月,在巴基斯坦西北边境省马尔丹盐渍化控制和复垦工程(SCARP)的106排水单元进行了控制排水和自由排水对土壤盐分的影响。浸出估计和化学(LEACHC)模型校准44天。模型分别模拟了1年、2年和5年的控制排水和1米地下水位下的自由排水。模拟表明,在每种条件下,与地下深度相关的盐度模式不同。在控制条件下,盐主要由于蒸发作用而向根区上部积累。而自由条件下的矿化度则根据现场实际情况出现波动。结果表明:在地下水位1.0m控制排水条件下,12.5 cm土壤电导率(EC)在模拟1、2和5年后分别增加到2.42、3.97和6.14 dS/m, 62.5 cm土壤电导率(EC)分别增加到1.78、1.92和2.27 dS/m。在水深2.0 m处,12.5 cm处EC分别增加到1.9、2.2和3.8 dS/m, 62.5 cm处EC分别达到1.8、1.98和3.8 dS/m。自由排水时,在12.5 cm和62.5 cm深度,EC分别从0.94 dS/m下降到1.13 dS/m。控制排水条件下土壤盐分随地下水位升高而升高,自由排水条件下土壤盐分随地下水位升高而降低。结果表明,LEACHC是一个有效的溶质运移模拟模型,适用于马尔丹SCARP土壤盐分状况。
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