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: Promma K., Zheng C., Asnachinda P.
Format: Article
Language:English
Published: 2014
Online Access:http://www.scopus.com/inward/record.url?eid=2-s2.0-34247609490&partnerID=40&md5=1adff06927b75b5da9e13e28decbbd12
http://cmuir.cmu.ac.th/handle/6653943832/5264
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Institution: Chiang Mai University
Language: English

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