Integrated Geospatial and Analytical Hierarchy Process Approach for Assessing Sustainable Management of Groundwater Recharge Potential in Barind Tract

被引:6
作者
Hossain, Md. Zahed [1 ,2 ]
Adhikary, Sajal Kumar [2 ]
Nath, Hrithik [2 ,3 ]
Kafy, Abdulla Al [4 ]
Altuwaijri, Hamad Ahmed [5 ]
Rahman, Muhammad Tauhidur [6 ]
机构
[1] Bangladesh Univ Business & Technol BUBT, Dept Text Engn, Dhaka 1216, Bangladesh
[2] Khulna Univ Engn & Technol KUET, Dept Civil Engn, Khulna 9203, Bangladesh
[3] Univ Creat Technol Chittagong UCTC, Dept Civil Engn, Chattogram 4212, Bangladesh
[4] Univ Texas Austin, Dept Geog & Environm, 1 Univ Stn A3100, Austin, TX 78712 USA
[5] King Saud Univ, Coll Humanities & Social Sci, Dept Geog, Riyadh 11451, Saudi Arabia
[6] Univ Texas Dallas, Sch Econ Polit & Policy Sci, Geospatial Informat Sci Program, 800 Campbell Rd, Richardson, TX 75080 USA
关键词
groundwater recharge; sustainable development; analytical hierarchical process; GIS; Barind tract; SOIL-WATER CONTENT; RAINFALL INTENSITY; LAND-USE; INFORMATION-SYSTEM; GIS; ZONES; BASIN; SURFACE; IDENTIFICATION; VARIABILITY;
D O I
10.3390/w16202918
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Groundwater depletion in Bangladesh's Barind tract poses significant challenges for sustainable water management. This study aims to delineate groundwater recharge potential zones in this region using an integrated geospatial and Analytical Hierarchy Process (AHP) approach. The methodology combines remote-sensing data with GIS analysis, considering seven factors influencing groundwater recharge: rainfall, soil type, geology, slope, lineament density, land use/land cover, and drainage density. The AHP method was employed to assess the variability of groundwater recharge potential within the 7586 km2 study area. Thematic maps of relevant factors were processed using ArcGIS software. Results indicate that 9.23% (700.22 km2), 47.68% (3617.13 km2), 37.12% (2816.13 km2), and 5.97% (452.70 km2) of the study area exhibit poor, moderate, good, and very good recharge potential, respectively. The annual recharge volume is estimated at 2554 x 106 m3/year, constituting 22.7% of the total precipitation volume (11,227 x 106 m3/year). Analysis of individual factors revealed that geology has the highest influence (33.57%) on recharge potential, followed by land use/land cover (17.74%), soil type (17.25%), and rainfall (12.25%). The consistency ratio of the pairwise comparison matrix was 0.0904, indicating acceptable reliability of the AHP results. The spatial distribution of recharge zones shows a concentration of poor recharge potential in areas with low rainfall (1200-1400 mm/year) and high slope (6-40%). Conversely, very good recharge potential is associated with high rainfall zones (1800-2200 mm/year) and areas with favorable geology (sedimentary deposits). This study provides a quantitative framework for assessing groundwater recharge potential in the Barind tract. The resulting maps and data offer valuable insights for policymakers and water resource managers to develop targeted groundwater management strategies. These findings have significant implications for sustainable water resource management in the region, particularly in addressing challenges related to agricultural water demand and climate change adaptation.
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页数:21
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