China Rural Water and Hydropower. 2013, (8):
25-27.
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Songnen Plain is a large water storage basin of a multi-layer stacked structure including widespread distribution of phreatic and Quaternary and former Quaternary confined water. Each aquifer groundwater has different hydrochemistry that is affected by geological, geomorphological and hydrogeological conditions. Quaternary phreatic widely distributed native environment is poor, vulnerable to artificially pollution, in which fluoride is higher than the standard in the central of the Songnen low plains, easily lead to fluorosis, not suitable for drinking. Quaternary confined water is mainly distributed in the central of low plains and eastern high plains in Songnen Plain, in which fluorine is higher, not suitable for drinking in low plain area and lower, suitable for drinking in high plain area, influenced by the native environment. Former Quaternary confined water mainly distributed in vast areas outside the western piedmont sloping plain, water quality is better, and fluorine meet the drinking water requirements, but the amount of water changes lager. Neogene Daan group and Paleogene Yian group confined water is abundantd and depth is large, supply conditions is poor, that is suitable for drinking, but controlling exploiting in low plain. Cretaceous aquifer group, which has better water quality, lower fluorine in high plain is suitable for drinking, but the distribution is uneven, so to scientific development. It is proposed that scientific and rational development and utilization model of groundwater in Songnen Plain, provides the basis for government decision-making.