Field investigations for sustainable groundwater utilization in the Konan basin

• Published in: Water resources management Vol. 13; no. 6; pp. 443 - 470
• Main Authors: JHA, M. K, CHIKAMORI, K, KAMII, Y, YAMASAKI, Y
• Format: Journal Article
• Language: English
• Published: Dordrecht Springer 01.12.1999; Springer Nature B.V
• Subjects: Aquifers; Earth sciences; Earth, ocean, space; Exact sciences and technology; Field tests; Gravel; Groundwater; Groundwater basins; Groundwater flow; Groundwater recharge; Hydrogeology; Hydrology. Hydrogeology; Japan, Kochi Prefect., Konan Basin; Japan, Monobe R; Sand & gravel; Stream discharge; Stream flow; Surface-groundwater relations; Water resources; Winter; Far East; Shikoku; Kochi Japan; Japan; Japan, Kochi Prefect., Konan Basin; Japan, Monobe R; changes of level; pump tests; ground water; ground-water recharge; water supply; consumption; demand; pumping; gravel; sand; hydraulic conductivity; aquifers; Asia; fluctuations; water resource management; unconfined aquifers; fresh water; streamflow
• ISSN: 0920-4741; 1573-1650
• DOI: 10.1023/A:1008184010262

The Konan groundwater basin of Kochi Prefecture, Japan, is experiencing freshwater shortages for the past few years, particularly during the winter season. The present study aimed at analyzing the problem and exploring increased groundwater withdrawals to meet burgeoning freshwater demands in various sectors. The trend analysis of waterconsumption indicates that the groundwater demandwould increase by 43 and 52% by the years 2010 and2025, respectively, compared to 32 100 m^sup 3^ d^sup -1^ at present.The streamflow of the Monobe River reduces to a minimumin winter and it shows a decreasing trend in recentyears. The geologic investigation results indicatethat unconfined (phreatic) aquifers comprisingalluvial sand and gravel and/or diluvial silty sandand gravel are dominant, and that the northwestern andwestern portions of the basin have greater potentialfor groundwater. Groundwater flows essentially fromnorth to south into the ocean. Groundwater levelfluctuations over the basin vary appreciably in spaceand time, indicating a wide variation of naturalrecharge. Field observations confirm the hypothesisthat stream-aquifer interaction also significantlycontributes to groundwater recharge, besides therainfall infiltration. Further, the pumping testsresults demonstrate that though the aquifers arelow-yielding, enhanced groundwater withdrawals couldbe possible. The aquifer hydraulic conductivity ischaracterized as high and ranges from 65 to 804 m d^sup -1^(mean = 229 m d^sup -1^), thereby suggesting great aquiferheterogeneity. Finally, it is concluded that thelong-term sustainability of the scarce groundwaterresource of the Konan basin is doubtful, and that acomprehensive analysis of the groundwater system isessential prior to formulating plans for the futuregroundwater development and management.[PUBLICATION ABSTRACT]