| 碧水岩地下河中微量金属元素对降雨的响应特征及来源分析 |
| 摘要点击 1435 全文点击 890 投稿时间：2015-06-23 修订日期：2015-08-16 |
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| 中文关键词 岩溶地下河 降雨 微量金属 响应 来源 |
| 英文关键词 karst subterranean river rainfall trace metals response source |
| 作者 | 单位 | E-mail | | 邹艳娥 | 中国地质大学(北京)水资源与环境学院, 北京 100083
中国地质科学院岩溶地质研究所, 国土资源部/广西岩溶动力学重点实验室, 桂林 541004 | yanezou@sohu.com | | 蒋萍萍 | 中国地质科学院岩溶地质研究所, 国土资源部/广西岩溶动力学重点实验室, 桂林 541004
桂林理工大学环境科学与工程学院, 桂林 541004 | | | 张强 | 中国地质科学院岩溶地质研究所, 国土资源部/广西岩溶动力学重点实验室, 桂林 541004
中国地质大学(武汉)环境学院, 武汉 430074 | zhangq198203@163.com | | 汤庆佳 | 中国地质科学院岩溶地质研究所, 国土资源部/广西岩溶动力学重点实验室, 桂林 541004 | | | 康志强 | 广西壮族自治区地质调查院, 南宁 530023 | | | 龚晓萍 | 中国地质科学院岩溶地质研究所, 国土资源部/广西岩溶动力学重点实验室, 桂林 541004 | | | 陈长杰 | 中国地质科学院岩溶地质研究所, 国土资源部/广西岩溶动力学重点实验室, 桂林 541004 | | | 俞建国 | 中国地质科学院岩溶地质研究所, 国土资源部/广西岩溶动力学重点实验室, 桂林 541004 | |
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| 中文摘要 |
| 在降雨条件下,利用自动采样器对广西碧水岩地下河出口进行高频采样,分析了碧水岩地下河出口水体中Cu、Pb、Zn、Cd等微量金属元素的水化学动态变化特征,探讨了地下河水中微量金属来源及其对降雨的响应机制. 结果表明,地下河水化学组分表现出了较明显的规律,其中主要元素Ca2+、Mg2+、HCO3-等在降雨过程中稀释作用明显,而Al、Mn、TFe、Cu、Pb、Zn、Cd等金属元素对降雨响应敏感,其质量浓度在降雨过程中有所升高,相应质量浓度曲线均表现出多峰值特点,且在最大降雨发生后第9 h达到最大峰值. 推断水岩作用、河底沉积物再释放和水土流失是导致河水金属元素浓度增高的原因,金属元素不同来源及地下河双入口的结构特征是形成金属元素质量浓度曲线多峰值的原因,其中水岩作用引起的水化学变化较河底沉积物再释放和水土流失更敏感,而后者是导致河水重金属元素增加的主要原因. 监测期间,溶质在地下河中的平均迁移速度约为0.47 km ·h-1,污染物运移速度较快,因此,通过对岩溶地下河水化学动态的监测,掌握微量金属组分来源及迁移特性,对于地下河水环境污染治理具有重要意义. |
| 英文摘要 |
| High-frequency sampling was conducted at the outlet of Guangxi Bishuiyan karst subterranean river using an automatic sampler during the rainfall events. The hydrochemical drymanic variation characteristics of trace metals (Cu, Pb, Zn, Cd) at the outlet of Guangxi Bishuiyan karst subterranean river were analyzed, and the sources of the trace metals in the subterranean river as well as their response to rainfall were explored. The results showed that the rainfall provoked a sharp decrease in the major elements (Ca2+, Mg2+, HCO3-, etc.) due to dilution and precipitation, while it also caused an increase in the concentrations of dissolved metals including Al, Mn, Cu, Zn and Cd, due to water-rock reaction, sediment remobilization, and soil erosion. The water-rock reaction was more sensitive to rainfall than the others, while the sediment remobilization and soil erosion took the main responsibility for the chemical change of the heavy metals. The curves of the heavy metal concentrations presented multiple peaks, of which the maximum was reached at 9 hours later after the largest precipitation. Different metal sources and the double-inlet structure of the subterranean river were supposed to be the reasons for the formation of multiple peaks. During the monitoring period, the average speed of the solute in the river reached about 0.47 km ·h-1, indicating fast migration of the pollutants. Therefore, monitoring the chemical dynamics of the karst subterranean river, mastering the sources and migration characteristics of trace metal components have great significance for the subterranean river environment pollution treatment. |
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