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重庆南山老龙洞地下河系统重金属分布与迁移特征及其自净能力

[Distribution and Transportation Characteristics of Heavy Metals in Nanshan Laolongdong Subterranean River System and Its Capacity of Self-Purification in Chongqing].

作者信息

Ren Kun, Liang Zuo-bing, Yu Zheng-liang, Zhang Yu, Wang Rong, Yuan Dao-xian

出版信息

Huan Jing Ke Xue. 2015 Nov;36(11):4095-102.

PMID:26910995
Abstract

For figuring out the distribution and transportation characteristics of heavy metals Mn, Pb, Cu and As among overlying water-pore water-surface sediments so as to offer a scientific basis for the development of urban construction and protection of karst groundwater, overlying water, pore water and surface sediment samples were collected in December 2013 ( winter) and June 2014 (summer) respectively. Results show that the detection rates of Mn, Pb, Cu and As are 100% both in overlying water and pore water with the concentration Mn > Pb > Cu > As, summer > winter, pore water > overlying water, respectively, and the groundwater could not be a source of drinking water because of the excessive content of Mn and Pb. In addition, the concentration of heavy metals Mn, Pb, Cu and As in pore water are higher than that in overlying water, indicating that heavy metals could diffuse into overlying water from pore water because of concentration gradient, especially in summertime. Moreover, study also finds that heavy metals are accumulated in surface sediments, the total content of four heavy metals has a decreasing trend between UGR6( sampling site 7) and UGR5 (sampling site 6), but has an increasing trend from UGR5 (sampling site 6) to URG0 (sampling site 1). Mn, in surface sediments, has strong instability and mobility, which can not only cause the pollution of overlying water but also enlarge contaminated area. In a word, Laolongdong subterranean river has strong capacity of self-purification, especially the surface sediments.

摘要

为了弄清重金属锰、铅、铜和砷在上覆水 - 孔隙水 - 表层沉积物中的分布及迁移特征,以便为城市建设发展和岩溶地下水保护提供科学依据,分别于2013年12月(冬季)和2014年6月(夏季)采集了上覆水、孔隙水和表层沉积物样本。结果表明,锰、铅、铜和砷在上覆水和孔隙水中的检出率均为100%,其浓度分别为锰>铅>铜>砷、夏季>冬季、孔隙水>上覆水,且由于锰和铅含量超标,该地下水不能作为饮用水源。此外,孔隙水中重金属锰、铅、铜和砷的浓度高于上覆水,这表明重金属会因浓度梯度从孔隙水扩散到上覆水,尤其是在夏季。而且,研究还发现重金属在表层沉积物中积累,四种重金属的总含量在UGR6(采样点7)和UGR5(采样点6)之间呈下降趋势,但从UGR5(采样点6)到URG0(采样点1)呈上升趋势。表层沉积物中的锰具有很强的不稳定性和迁移性,不仅会对上覆水造成污染,还会扩大污染面积。总之,老龙洞地下河具有较强的自净能力,尤其是表层沉积物。

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