阐明瓦多斯区中的生物地化学特征,整合地化学,微生物和数值模拟
Lei Duan1, Xiaobang Liu1, Yaqiao Sun1
1School of Water and Environment, Chang'an University, Xi'an 710054, Shaanxi, China; Key Laboratory of Underground Hydrology and Ecological Effects in Arid Regions of the Ministry of Education, Chang'an University, Xi'an 710054, Shaanxi, China.
The Science of the total environment
|July 12, 2024
概括
了解瓦多斯区的循环是防止土壤和地下水污染的关键. 这项研究揭示了微生物活动,液压和地质驱动的驱动力.
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:
- 瓦多斯区的生物地质化学对于管理土壤和地下水污染至关重要.
- 现有的研究还没有完全描述不同地质环境中的行为.
研究的目的:
- 调查农业瓦多斯地区的生态化学过程.
- 了解地质化学,微生物学和水力动力学在循环上的相互作用.
主要方法:
- 综合地质化学,微生物学和数值模拟方法.
- 对微生物多样性,物种组成和功能性微生物的分析.
- 确定调节代谢的关键环境因素.
主要成果:
- - (NH4+-N) 在土壤表层 (0-40厘米) 积累.
- 酸- (NO3-N) 是水力动力学运输垂直和水平.
- 土壤深度显著影响微生物群落;环境因素如ORP,TOC和水分调节变化 (固定,化,脱化).
结论:
- 在瓦多斯区形成了明显的生化反应区,受水力动力学和地形学的影响.
- 流平原的粘土沙子对地下水构成了NO-N污染的风险.
- 洛斯裂结构可以促进洛斯高原的地下水污染.
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