Identification of Groundwater Potential Recharge Zones in Flinders Ranges, South Australia Using Remote Sensing, GIS, and MIF Techniques

被引:21
|
作者
Ahmed, Alaa [1 ,2 ]
Alrajhi, Abdullah [3 ]
Alquwaizany, Abdulaziz S. [3 ]
机构
[1] Univ South Australia, UniSA STEM, Ctr Scarce Resources & Circular Econ ScaRCE, Adelaide, SA 5095, Australia
[2] Desert Res Ctr, Geol Dept, Div Water Resource, Mathaf El Matariya St, Cairo 11753, Egypt
[3] King Abdulaziz City Sci & Technol, King Abdullah Rd, Riyadh 11442, Saudi Arabia
关键词
remote sensing; geographic information system; multi-influencing factors technique; groundwater potential recharge zones; Flinders Ranges; South Australia; FREQUENCY RATIO MODEL; REGION; LAND; LINEAMENTS; GEOMETRY; DISTRICT;
D O I
10.3390/w13182571
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In Australia, water resource management is a major environmental, biological, and socio-economic issue, and will be an essential component of future development. The Hawker Area of the central Flinders Ranges, South Australia suffers from a lack of reliable data to help with water resource management and decision making. The present study aimed to delineate and assess groundwater recharge potential (GWRP) zones using an integration between the remote sensing (RS), geographic information system (GIS), and multi-influencing factors (MIF) approaches in the Hawker Area of the Flinders Ranges, South Australia. Many thematic layers such as lithology, drainage density, slope, and lineament density were established in a GIS environment for the purpose of identifying groundwater recharge potential zones. A knowledge base ranking from 1 to 5 was assigned to each individual thematic layer and its categories, depending on each layer's importance to groundwater recharge potential zones. All of the thematic layers were integrated to create a combined groundwater potential map of the study area using weighting analysis in ArcGIS software. The groundwater potential zones were categorized into three classes, good, moderate, and low. The resulting zones were verified using available water data and showed a relative consistency with the interpretations. The findings of this study indicated that the most effective groundwater potential recharge zones are located where the lineament density is high, the drainage density is low, and the slope is gentle. The least effective areas for groundwater recharge are underlain by shale and siltstone. The results indicated that there were interrelationships between the groundwater recharge potential factors and the general hydrology characteristics scores of the catchment. MIF analysis using GIS mapping techniques proved to be a very useful tool in the evaluation of hydrogeological systems and could enable decision makers to evaluate, better manage, and protect a hydrogeological system using a single platform.
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页数:18
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