作为煤矿岩石中酸盐来源的可交换氨的化
M Jim Hendry1, Erin Schmeling2, S Lee Barbour3
1Department of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, SK, S7N 5E2, Canada. jim.hendry@usask.ca.
Environmental geochemistry and health
|January 12, 2026
概括
煤矿废物岩石中的可交换氨迅速化为酸盐,导致地表水污染. 较小的颗粒比较大的颗粒更快地释放酸盐,影响水生系统.
科学领域:
- 环境科学 环境科学
- 地质化学 地质化学
- 土壤科学 土壤科学
背景情况:
- 加拿大埃尔克谷的煤矿废物岩石中含有有机和粘土矿物中的可交换氨 (NH4+-ex).
- 虽然有机是丰富的,可交换的更具反应性,经历快速化为酸盐 (NO3-).
研究的目的:
- 为了调查煤矿废物中的酸盐的释放,岩石.
- 了解可交换氨在酸盐形成中的作用及其对地表水的影响.
主要方法:
- 进行了批量实验,以建模NH4+的释放和扩散 - 例如.
- 对老旧的矿山岩石进行了不同颗粒大小的氧化实验和N型分析.
主要成果:
- 可交换的氨 (NH4+-ex) 在50天内迅速化为酸盐 (NO3-),而有机仍然没有反应.
- 矿山岩石颗粒<75毫米的酸盐释放速度很快 (<1年),较小的颗粒 (<几十毫米) 释放速度更快.
- 较大的颗粒 (>75毫米) 由于NH4+迁移速度较慢,导致酸盐释放延迟.
结论:
- 化NH4+-ex是矿山岩石堆中的酸盐加载到地表水的重要来源.
- 这一过程可能会导致长时间的酸盐释放,可能会影响相关的水生生态系统.
- 区分从爆炸剂和NH4+-ex中酸盐的贡献需要进一步的研究.
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