珲春盆地地下水补径排条件及其影响因素
The Recharge, Runoff and Discharge Characteristics of Groundwater in Hunchun Basin and the Influencing Factors
作者: 石旭飞 * , 赵海卿 , 郭晓东 ：中国地质调查局沈阳地质调查中心/沈阳地质矿产研究所，辽宁 沈阳;
关键词: 地下水； 补径排条件； 水循环； 珲春盆地； Groundwater； The Recharge； Runoff and Discharge Characteristics； Water Cycle； Hunchun Basin
摘要:Abstract: The groundwater level of Hunchun Basin was measured, and the recharge, runoff and discharge characteristics of groundwater in Hunchun Basin and the influencing factors are analyzed by using the measured data. Generally, the groundwater level in the Hunchun Basin is high in the east and low in the west. It flows from the piedmont belt to the Hunchun River valley which is from northeast to southwest. The groundwater flows from north to south in the northern piedmont area; the groundwater in the eastern piedmont area flows from east to west; the groundwater in the southern piedmont area flows from southeast to northwest. The hydraulic gradient gradually decreases from the piedmont to the plain. The groundwater is recharged from the bedrock area in Qihudong village, Heping village, Xinhua village, Hongxing village, Zhibian village etc. The Zhonghua village, Chunjing village, Donggang village, Nanqinmeng village are groundwater runoff areas. The groundwater is discharged to Tumen River in Bajiazi village, Shatuozi village, Xiwaizi village etc.
文章引用: 石旭飞 , 赵海卿 , 郭晓东 (2017) 珲春盆地地下水补径排条件及其影响因素。 矿山工程， 5， 95-99. doi: 10.12677/ME.2017.53014
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