CAJ | 학술논문

为研究山西省洪山泉流量衰减的原因，对天然状态下（1955-1983年）、人类活动影响较小阶段（1984-1998年）和人类活动影响较大阶段（1999-2008年）三个阶段的水均衡情况进行了分析。结果表明：岩溶水的过量开采是导致泉水流量减少的主导因素，人类活动影响下泉流量处于负均衡，各均衡期内泉流量与均衡结果具有密切的联系，泉流量随着负均衡值的增大快速减小。
위연구산서성홍산천류량쇠감적원인，대천연상태하（1955-1983년）、인류활동영향교소계단（1984-1998년）화인류활동영향교대계단（1999-2008년）삼개계단적수균형정황진행료분석。결과표명：암용수적과량개채시도치천수류량감소적주도인소，인류활동영향하천류량처우부균형，각균형기내천류량여균형결과구유밀절적련계，천류량수착부균형치적증대쾌속감소。
In order to study the relationship between discharge and water balance in Hongshan Spring of Shanxi Province,this paper adopted water balance method to analyze the water balance under natural conditions(1955 - 1983),the conditions of low impact of human activities(1984 -1998)and high impact of human activities(1999 - 2008),respectively. The results show that the over-exploitation of karst groundwater is the pri-mary reason of leading to decrease of spring discharge;the spring discharge represents a negative-balance condition under human activities;spring discharge shows close relationship with water balance and the increasing negative balance in decreasing spring discharge.