首页|沁水盆地煤层气井排采水微量元素地球化学特征及其环境意义

沁水盆地煤层气井排采水微量元素地球化学特征及其环境意义

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在能源结构调整的过程中,煤层气作为重要的非常规天然气资源,其开发和利用引起广泛关注.然而,煤层气开采伴随的排采水排放也引发了水污染等环境问题.沁水盆地是我国煤层气开发的重要区域,因此本研究以该地区的6个区块为研究对象,对煤层气井排采水中微量元素的来源与演化进行了深入分析,以提供地球化学数据支撑,为排采水的后续处理提供依据.分析结果显示,沁水盆地煤层气井排采水中主要微量元素包括Li、B、F、Mn、Fe、Sr、Ba等.其中,F和Mn的含量分别超出中国饮用水卫生标准7倍和1.4倍,地下水质量标准中分别达到Ⅴ类和Ⅲ~Ⅳ类水质标准.长期的煤层气开采导致了这些元素的过度积累,对周围环境及人类健康构成严重威胁.本研究指出,岩浆活动为沁水盆地煤层带来了大量的F,富含HCOi的地下水环境促进了含氟矿物的溶解,从而导致了煤层水中F的富集.同时,榆社和郑庄区块的锰富集现象最为严重,含锰菱铁矿溶解作用是煤层水中高浓度溶解锰的主要控制因素.随着煤层气井深度的增加和pH值的降低,煤层水中Mn的富集程度逐渐增加.本研究通过汇总其他煤层气区域的数据,发现中国的煤层水中普遍存在F和Mn的异常富集现象,因此在排放煤层水前,有必要采取适当的处理措施.
Geochemical Characteristics and Environmental Significance of Trace Elements in Co-produced Water of Coalbed Methane in Qinshui Basin
In the process of energy structure adjustment,as an unconventional natural gas resources,the development and utilization of coalbed methane(CBM)has gradually attracted attention,since CBM is an important unconventional natural gas resources.The large amount of water produced by the exploitation of coalbed methane has therefore raised concerns about water pollution and other related environmental issues.Qinshui Basin is an important area for the development of CBM in China.This study analyzed samples from 6 blocks in the Qinshui Basin to trace the source and evolution of trace elements in CBM co-produced water,and provided geochemical data support for the follow-up treatments.The main trace element compositions of the water samples in Qinshui Basin include Li,B,F,Mn,Fe,Sr,and Ba.Particularly,F and Mn levels exceed the Chinese drinking water health standards by 7 times and 1.4 times,respectively,corresponding to groundwater quality standards of Class Ⅴ and Class Ⅲ-Ⅳ.The long-term accumulation of elements due to CBM exploitation poses a serious threat to the surrounding environment and human health.Magmatic activities bring a large amount of F to the coal seam in Qinshui Basin.The local water environment,riched in HCO3-,promotes the dissolution of fluoride-containing minerals.The situation of Mn exceeding the standard was the most serious in Yushe and Zhengzhuang.The dissolution of manganese siderite is the main control factor for high concentration of dissolved Mn in coal seam water,and with the increase of buried depth of coal seams and the decrease of pH value,Mn is gradually enriched in CBM co-produced water.The phenomenon of F and Mn exceeding the standard exists widely in coal seam water in China.It is necessary to take appropriate treatment measures for F and Mn before discharging CBM co-produced water.

Qinshui Basincoalbed methane co-produced waterwater qualitytrace elements

方鲁加、陈碧莹、能惠、刘燚、崔丽峰、徐胜

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天津大学地球系统科学学院,天津 300072

沁水盆地 煤层气井排采水 水质评价 微量元素

2024

地球与环境
中国科学院地球化学研究所

地球与环境

CSTPCD北大核心
影响因子:0.875
ISSN:1672-9250
年,卷(期):2024.52(6)