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摘要:
By sampling the undercurrent belts of riverfront, shoal and riverbed at Xianyang, Xi’an, Lintong and Huaxian in Weihe basin of Shaanxi province in the summer and winter of 2014 and analyzed the water chemical character through Piper trilinear chart, This thesis has come to the following conclusions: (1) PH in shoal range from 7.42 to 7.98, and in riverfront, the average is 7.58, present alkaline. The TDS in riverfront is higher than that of river water, it range from 506.5 to 824, 616.06 mg?L?1 in average. (2) All of the water at riverfront, shoal and riverbed under the influence of carbonate. The concentration of ionic concentration at shoal is between riverbed and riverfront, by contrast, it close to riverfront. This result means the shoal recharged by both surface and river water, and the groundwater recharge is more conspicuous than surface water. Besides, from upstream to downstream, the two kinds of main ions ( and Ca2+) have little change in the same river, it related to such factors as river evaporation, the exchange interaction of surface and underground water and so on.
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篇名 Research of Hydrochemical Properties of Hyporheic Zone along the WeiHe River in Shanxi Segment
来源期刊 地球科学和环境保护期刊(英文) 学科 医学
关键词 HYPORHEIC Zone Weihe River HYDROCHEMISTRY PIPER
年,卷(期) 2017,(6) 所属期刊栏目
研究方向 页码范围 226-232
页数 7页 分类号 R73
字数 语种
DOI
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研究主题发展历程
节点文献
HYPORHEIC
Zone
Weihe
River
HYDROCHEMISTRY
PIPER
研究起点
研究来源
研究分支
研究去脉
引文网络交叉学科
相关学者/机构
期刊影响力
地球科学和环境保护期刊(英文)
月刊
2327-4336
武汉市江夏区汤逊湖北路38号光谷总部空间
出版文献量(篇)
901
总下载数(次)
1
总被引数(次)
0
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