Groundwater and surface-water interactions in a confined alluvial aquifer between two rivers: Effects of groundwater flow dynamics on high iron anomaly

In a confined alluvial aquifer located between two rivers, discrete zones of anomalously high concentrations of redox species such as iron, are thought to be a result of groundwater flow dynamics rather than a chemical evolution along continuous flow paths. This new hypothesis was confirmed at a stu...

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Bibliographic Details
Main Authors: Kitchakarn Promma, Chunmiao Zheng, Pongpor Asnachinda
Format: Journal
Published: 2018
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Online Access:https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=34247609490&origin=inward
http://cmuir.cmu.ac.th/jspui/handle/6653943832/61022
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Institution: Chiang Mai University

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