降水丰枯周期年的变化在岩溶水化学成分的变化上，也有很好的显示。
The variation of hydrochemical compositions of karst water can be well reflected in the variation of precipitation high and low water circle year.
从赣南横迳温泉区采集10个水样并分析了温泉及冷泉的水化学成分，认为热水起源于大气降水补给。
In the Hengjing hot springs area, southern Jiangxi Province, 10 samples taken from hot springs and cold springs are analyzed for hydrochemistry.
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