吉林大学学报(地球科学版) ›› 2019, Vol. 49 ›› Issue (3): 762-772.doi: 10.13278/j.cnki.jjuese.20170322
苏小四1,2, 高睿敏1, 袁文真3, 鹿帅1, 苏东1, 张丽华4, 孟祥菲4, 左恩德1
Su Xiaosi1,2, Gao Ruimin1, Yuan Wenzhen3, Lu Shuai1, Su Dong1, Zhang Lihua4, Meng Xiangfei4, Zuo Ende1
摘要: 河水入渗补给是傍河水源地的主要补给来源,确定河水补给强度对于促进水源地长期安全的开采具有十分重要的意义。以沈阳黄家水源地为研究区,通过对比研究区河水、地下水的水化学及氢氧稳定同位素特征,分析了水源地地下水的补给来源及强度。结果表明:傍河水源地地下水主要接受河水的入渗补给和区域地下水的侧向补给;受河床沉积物和含水介质的岩性及结构在空间上的差异影响,河水入渗补给后在向地下水位漏斗中心流动的过程中具有浅层和深层两条地下水流路径,深层地下水与河水的水力联系更为紧密;河水对地下水的补给强度具有明显的时空变化特点,表现为雨季河水入渗强度明显大于旱季,并且随着与辽河距离的增加,水源地地下水获得的河水补给量呈逐渐减小的趋势。
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