水资源保护2018，Vol.34Issue(1)：31-35,5.DOI:10.3880/j.issn.10046933.2018.01.06
河道再生水入渗的水岩相互作用机理研究
Interaction mechanism experiment of water and rocks in infiltration of reclaimed water
摘要
Abstract
Based on the water diversion project from Wenyu River to Chaobai River , the leaching experiment was carried out to study the cation exchange adsorption mechanism and TN and NO 3--N removal effect of riverbed medium in the process of the reclaimed water passing through riverbed .According to the groundwater quality monitoring data , the interaction mechanism of water and rocks between the reclaimed water and riverbed medium was verified .The results show that the salinity in groundwater increases for nine years of using the reclaimed water . Though the infiltration of reclaimed water causes the exchange between K +in water and Ca2+in soil, the total hardness of groundwater decreases .The concentration of NO 3--N is very low in groundwater due to the significant removal effect of riverbed medium .For inorganic components , the reclaimed water has no negative effect .关键词
再生水/地下水/阳离子交换吸附/NO3--NKey words
reclaimed water/groundwater/cation exchange adsorption/NO3--N分类
天文与地球科学引用本文复制引用
刘立才,单悦,黄俊雄,李炳华,杨勇..河道再生水入渗的水岩相互作用机理研究[J].水资源保护,2018,34(1):31-35,5.基金项目
国家水体污染控制与治理科技重大专项(2014ZX07203-010) （2014ZX07203-010）
