无承压含水层水平衡评价(卡尔巴拉-伊拉克)

S. A. Majeed, Fatin A. Alnasrawi, Muthanna M. A. Al-Shammari
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摘要

地下水被认为是研究区内唯一的灌溉资源。该地区的无承压Dibdibba含水层被认为是一个生产水文地质单元,延伸到伊拉克中部和南部的大片地区。本研究对含水层系统的水文地质特征及含水层流向进行了研究。AQTESOLV 4.5版抽水试验结果分析表明,研究区Dibdibba含水层的渗透率为(129 ~ 161)m2/day,导水率为(3.6 ~ 5.3)m/day。水流网显示水流方向由西南向东北和向东,流向幼发拉底河流域的泄流区。利用卡尔巴拉地区气象站的气象资料对水量平衡进行了评价。水平衡计算的主要目的是预测封闭系统中水分含量的时间变化,并估计研究区地下水储量的变化。综合计算水量平衡分量可知,研究区流入水量为6317.57 m3/d,流出水量为6931.93 m3/d。因此,地下水储量(ΔS)的变化将为(−6317.57 m3/天)。这一结果是研究区地下水消耗增加和过度开采的危险信号。
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Water Balance Assessment of Unconfined Aquifer (Karbala-Iraq)
Groundwater is consider as a sole resource for irrigation in the study area. The unconfined Dibdibba aquifer in this area is considered as a producing hydrogeological unit that extend over large areas in the central and southern part of Iraq.In this study, hydrogeological characteristics of the aquifer system as well as aquifer flow direction were investigated. The pumping test results analysis by AQTESOLV Version 4.5 reveals that transmissibility and hydraulic conductivity of Dibdibba Aquifer in the study area ranged from (129–161) m2/day and (3.6–5.3) m/day respectively.The flow net showed that flow direction is from the southwest to the northeast and east, towards the discharge zone along the Euphrates River.Water balance was evaluated using meteorological data of Karbala meteorological stations. The main purpose of a water balance calculation is to predict temporal variations of water content in a closed system and to estimate change in groundwater storage in the study area. Overall calculations of the water balance components shows that the inflow water that reach the study area is (6,317.57 m3/day) while the amount of outflow water is (6931.93 m3/day). Therefore the change in the groundwater storage (ΔS) will be (−6,317.57 m3/day). This result is dangerous sign of increasing of groundwater consumption and overexploitation in the study area.
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