Journal of the Korean Society of Groundwater Environment (대한지하수환경학회지)
- Volume 1 Issue 1
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- Pages.33-50
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- 1994
Sustainable Yield of Groundwater Resources of the Cheju Island
제주도 지하수자원의 최적 개발가능량
- Published : 1994.09.01
Abstract
The Hydrogeologic data of 455 water wells comprising geologic log and aquifer test were analyzed to determine hydrogeologic characteristics of the Cheju island. The groundwater. of the Cheju island is occurred in unconsolidated pyroclastic deposits and crinker interbedded in highly jointed basaltic and andesic rocks as high level, basal and parabasal types under unconfined condition. The average transmissivity and specific yield of the aquifer are at about 29,300㎡/day and 0.12 respectively, The total storage of groundwater is estimated about 44 billion cubic meters. Average annual precipitation is about 3,390 million ㎥ among which average recharge is estimated for 1,494 million ㎥ being equivalent 44.1% of total annual precipitation with 638 million ㎥ of runoff and 1,256 million ㎥ of evapotranspiration. Based on groundwater budget analysis, the sustainable yield is about 620 million ㎥(41% of annual recharge)and rest is discharging into the sea. The geologic logs of recently drilled thermal water wells indicate that very low-permeable marine sediments(Sehwa-ri formation) composed of loosely cemented sandy silt derived from mainly volcanic ashes at the 1st stage volcanic activity of the area is situated at the 120
제주도 지하수자원의 산출특성을 규명키 위하여 총 455개 기존관정의 자료를 전산처리하여 지역별 대수성 수리특성을 규명하였다. 제주도는 주로 현무암내에 협재된 화산쇄설층, crinker층과 현무암의 1 및 2차 유효공극이 주 대수대의 역할을 하며 이들은 기저, 준기저 및 상위대수층으로 구성되어 있다. 본도 대수층의 평균 투수량계수는 29,300
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