伊拉克东北部阿尔金山科普里盆地含水层水文地质特征评估

Q3 Earth and Planetary Sciences Iraqi Geological Journal Pub Date : 2024-01-31 DOI:10.46717/igj.57.1a.12ms-2024-1-23
Mustafa Akbar, Aysar Al-Shama’a
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引用次数: 0

摘要

本次研究旨在评估研究区域含水层的水文地质特征。由于抽水井附近没有观测井,因此在分布于研究区域的 GW1、GW2、GW8、GW9、GW11、GW13 和 GW16 七口井进行了单次抽水试验。抽水试验记录使用含水层测试 2016.1 软件进行分析,该软件基于四种方法:Theis、Hantush、Cooper-Jacob 和 Theis 恢复法。研究区域上部含水层的渗透率平均值介于 13.4 平方米/天和 279 平方米/天之间,水力传导率介于 0.162 米/天和 4.14 米/天之间,贮存率介于 0.166 和 0.826 之间。下含水层的透水率介于 11.4 平方米/天和 177 平方米/天之间,导水性为 0.214 米/天和 1.17 米/天,蓄水率为 0.0791 和 0.99。
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Evaluation of Hydrogeological Characteristics of Aquifers in Altun Kopri Basin, Northeastern Iraq
The current research aims to evaluate the hydrogeological characteristics of the water-bearing layers in the study area. Because of the absence of observation wells near the pumping wells, the single pumping test experiment was achieved at seven wells, GW1, GW2, GW8, GW9, GW11, GW13, and GW16, distributed in the study area. The pumping test records were analyzed using Aquifer Test 2016.1 software, which is based on four methods: Theis, Hantush, Cooper-Jacob, and Theis recovery. The average values of transmissivity for the upper aquifer in the study area ranged between 13.4 m2/ day and 279 m2/ day, while the hydraulic conductivity ranged between 0.162 m/day and 4.14 m/day, and the storativity was 0.166 and 0.826. For the lower aquifer, the transmissivity ranges between 11.4 m2/ day and 177 m2/ day, the hydraulic conductivity is 0.214 m/ day and 1.17 m/ day, and the storativity is 0.0791 and 0.99.
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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
期刊最新文献
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