在地下水蒸发排放区的无机碳迁移和转化
Shaogang Dong1, Lu Li1, Xiaolong Shi2
1School of Ecology and Environment, Inner Mongolia University, Hohhot, Inner Mongolia, 010021, China.
The Science of the total environment
|July 28, 2024
概括
地下水蒸发排放区可以充当碳汇. 水与岩石的相互作用,如多洛米特溶解,固定了大量的碳,抵消了大气中的二氧化碳排放,影响了陆地碳循环.
科学领域:
- 地质化学 地质化学
- 环境科学 环境科学
- 水文学 水文学
背景情况:
- 地下水蒸发排放通过碳相关的水岩相互作用对陆地碳循环产生重大影响.
- 这些地区碳迁移和转变的精确机制尚未完全理解.
研究的目的:
- 分析地下水蒸发期间的碳转移机制.
- 为地下水蒸发排放区域构建碳平衡方程.
主要方法:
- 使用了质量平衡原理.
- 采用了水地化学模拟方法.
- 在内蒙古的图莫川平原进行了案例研究.
主要成果:
- 图莫川平原的蒸发排放区作为一个碳汇.
- 碳固定率 (37.15 g/m2·a) 超过大气排放率 (7.35 g/m2·a).
- 多洛米特溶解 (30.56 g/m2·a) 和石沉是控制溶解无机碳 (DIC) 迁移的关键过程.
结论:
- 多洛米特岩的溶解抵消了石沉期间排放的大量二氧化碳.
- 从多洛米特和矿溶解中释放的促进了矿沉,使地下水成为碳汇.
- 了解这些过程对于评估陆地碳循环对地下水蒸发的反应至关重要.
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