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地球学报  2009 

鲁北平原地下水同位素年龄及可更新能力评价

DOI: 10.3975/cagsb.2009.02.12

Keywords: 地下水,环境同位素,年龄,更新能力,鲁北平原

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Abstract:

笔者采用大量的地下水环境同位素数据,利用天然放射性氚和14C的通用测年技术,分别估算浅、深层地下水的形成年龄,评价地下水的可更新能力。研究结果表明,鲁北平原浅层地下水的主要补给来自当地的大气降水和引黄河灌溉水,循环速度较快,循环时间20～50a,更新能力较强。深层地下水主要起源于古代大气降水,是在比现在寒冷的气候条件下由大气降水入渗形成,循环速度较慢,循环时间8～20ka,更新能力较弱。

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