传统的化石燃料提取,相关的生物地化学过程和地形学影响甲地下水度在阿巴拉契亚
Yunpo Li1, Helen G Siegel2, Nathalie A Thelemaque1
1Department of Civil and Environmental Engineering, Parsons Laboratory, Massachusetts Institute of Technology, 15 Vassar Street, Cambridge, Massachusetts 02139, United States.
Environmental science & technology
|November 20, 2023
概括
化石燃料开采可以将甲释放到地下水中. 煤炭开采可能通过增加硫酸盐水平来抑制甲释放,从而影响地下水甲度.
科学领域:
- 环境科学 环境科学
- 地质化学 地质化学
- 微生物学 微生物学
背景情况:
- 化石燃料生产,包括石油,天然气和煤炭,是人为甲排放的主要来源.
- 化石燃料开采过程中释放的甲可以污染地下水,并可能到达大气层.
- 了解影响地下水甲的因素对于评估气候变化影响至关重要.
研究的目的:
- 调查影响化石燃料生产地区地下水中的甲度的因素.
- 探索石油和天然气 (O&G) 和煤炭开采活动与地下水甲水平之间的关系.
- 确定硫酸盐和地形学在调节地下水甲中的作用.
主要方法:
- 从非传统的石油和天然气 (UOG) 和O&G/煤炭生产地区收集了311个水样.
- 分析了甲和硫酸盐度与开采地点的邻近性和地形特征相关.
- 采用统计分析来识别相关性和混变量.
主要成果:
- 甲度与一个地区的O&G井的接近有负相关性,但这被地形所混.
- 硫酸盐度与甲度和距离煤矿的距离有负相关性,不依据地形.
- 这些发现表明,煤炭开采影响地下水硫酸盐,而硫酸盐反过来影响甲.
结论:
- 地下水中的甲度是由生物地化学过程,地形和化石燃料开采的复杂相互作用形成的.
- 煤矿对地下水中的硫酸盐的丰富可能会抑制甲生成并促进甲氧化.
- 需要进一步的研究,以充分阐明这些环境中甲释放和转化的途径.
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