Transmissivity Estimation and Mapping of the Dammam Karst Aquifer in Central Iraq

Q3 Earth and Planetary Sciences
Sumayah Majeed, Nassrin Al-Mansori, Saif Alquzweeni
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引用次数: 0

Abstract

The most reliable method to determine an aquifer's transmissivity is pumping tests; however, these studies are time-consuming and costly. An alternative approach to estimating transmissivity is to use the well's specific capacity. The aim of this research is to improve our knowledge of the transmissivity of the Dammam karst aquifer in central Iraq to support sustainable management strategies. The specific capacity and transmissivity data of 39 wells were collected. The normality tests showed that transmissivity and specific capacity are log-normally distributed. A simple linear regression with R2 = 0.84 relates transmissivity to the specific capacity. Subsequently, the resulting relationship was used to estimate transmissivity from the 135 specific capacities. The measured and estimated transmissivity data (174 data points) were used for geostatistical analysis. Using the kriging technique, an interpolated distribution map of transmissivity was developed. The cross-validation reveals that the geostatistical method gives a good estimate of the transmissivity of the Dammam aquifer.
伊拉克中部达曼岩溶含水层的渗透率估算和绘图
确定含水层渗透性最可靠的方法是抽水试验,但这些研究耗时费钱。估算渗透率的另一种方法是使用水井的比容。这项研究的目的是增进我们对伊拉克中部达曼岩溶含水层渗透性的了解,为可持续管理战略提供支持。研究收集了 39 口水井的比容和透射率数据。正态性检验表明,透射率和比容呈对数正态分布。R2 = 0.84 的简单线性回归将透射率与比容联系起来。随后,根据 135 个比容估算出透射率。测量和估算的透射率数据(174 个数据点)被用于地质统计分析。利用克里金技术,绘制了透射率插值分布图。交叉验证结果表明,地质统计方法很好地估算了达曼含水层的透射率。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Iraqi Geological Journal
Iraqi Geological Journal Earth and Planetary Sciences-Geology
CiteScore
1.80
自引率
0.00%
发文量
152
审稿时长
7 weeks
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