在伊拉克东北部基尔库克使用层次分析法、RS 和 GIS 技术对 Shewasoor 子盆地的地下水潜力区进行建模和绘图

Q3 Earth and Planetary Sciences
Madyan Al-Gburi, Mohmmed Hasan, R. Habala
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引用次数: 0

摘要

地下水被认为是维持生命最重要的自然资源之一。由于人口剧增和人类活动的发展,Shewasoor 小流域对水的需求不断增加。此外,由于干旱和半干旱地区的气候变化,地下水稀缺。本研究旨在确定 Shewasoor 小盆地地下水潜力的空间分布。本研究利用地理信息系统和遥感技术,在通过多标准决策分析确定每个参数的权重后,采用层次分析法(analytical hierarchy process method)对七个图层(地质、坡度、海拔、线型、排水密度、土壤和土地利用/土地覆盖)进行建模,绘制了 Shewasoor 子流域的地下水潜势图。结果显示,地下水潜力图分为五个区域。该次盆地的大部分(61.8 平方公里)属于极高地下水潜势区,分布在海拔、排水密度和白哈桑地层低坡度的区域;从次盆地中心向北延伸。中度地下水潜势区(47.6 平方公里)主要包括白哈珊地层海拔和坡度中等的区域。约 49.6 平方公里为极低至低地下水潜势区,主要分布在该次盆地东部 Mukdadiyah 地层内海拔和坡度较高的区域;此外,由于海拔和坡度较高,该次盆地南部、西部和中部部分地区 Bai-Hassan 地层内的地下水潜势较低。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Modeling and Mapping of Groundwater Potential Zones of the Shewasoor Sub-Basin Using Analytical Hierarchy Process, RS and GIS Techniques in Kirkuk, Northeastern Iraq
Groundwater is considered one of the most vital natural resources for sustaining life. The demand for water in the Shewasoor sub-basin is constantly increasing due to formidable population growth and the development of human activities. Besides, groundwater is scarce due to climatic changes in arid and semi-arid. This study aims to determine spatial distribution of groundwater potential in the Shewasoor sub-basin. This study relied on seven layers (geology, slope, elevation, lineament, drainage density, soil, and land use/land covers) using geographic information systems, remote sensing, and applying the analytical hierarchy process method after determining the weights for each parameter by a multi-criteria decision analysis; to model the groundwater potential map in the Shewasoor sub-basin. The result appeared as a map of groundwater potential categorized into five zones. The majority of the sub-basin (61.8 km2) falls under a very high-high groundwater potential zone, which distributes over an area of elevations, drainage density, and slopes low of the Bai-Hassan Formation; from the center towards the north of the sub-basin. The moderate groundwater potential zone (47.6 km2) mainly encompasses an area of elevations and slopes moderate to the Bai-Hassan formation. About 49.6 km2 is a very low to low groundwater potential zone, mainly found over the area of the elevations and slopes high within the Mukdadiyah Formation east of the sub-basin; in addition to, low groundwater potential within the Bai-Hassan Formation in the south, west, and some part center of the sub-basin due of the elevations and slopes high.
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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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