碳酸盐的风化过程:风化时间
Jin Chen1, Fangbing Li1, Xiangwei Zhao1
1Key Laboratory of Plant Resource Conservation and Germplasm Innovation in Mountainous Region, Collaborative Innovation Center for Mountain Ecology & Agro-Bioengineering (CICMEAB), College of Life Sciences/Institute of Agro-bioengineering, Guizhou University, Guiyang, Guizhou, China.
PeerJ
|August 7, 2023
概括
时间显著影响了几个世纪以来的碳酸气候变化. 早期阶段表现出快速气候变化和低变化,而后期阶段表现出较慢的速度和增加的元素丰富,建立了定量气候变化持续时间方法.
科学领域:
- 地质化学 地质化学
- 土壤科学 土壤科学
- 地质时间学 (Geochronology)
背景情况:
- 土壤形成受母体物质,气候,生物,地形和时间的影响.
- 量化碳酸盐气候变化的时间作用仍然具有挑战性.
- 需要一个百年级的碳酸气候持续时间的方法.
研究的目的:
- 通过使用墓碑建立一种方法来确定碳酸盐风的持续时间.
- 为了研究碳酸盐随着时间的推移的气候变化特征.
- 为了将气候变化的持续时间与气候变化的程度相关联.
主要方法:
- 利用了来自中国西南的废弃碳酸盐墓碑.
- 使用的墓碑立日期是气候变化的开始.
- 应用化学风化指数 (CIA,Lc,AC,Imob) 来评估风化程度.
主要成果:
- 观察到Mg,Al,Si,Fe,Ti的丰富以及碳酸盐规流体中的Ca的减少.
- 验证的化学指数用于评估不同时间段的气候变化程度.
- 确定碳酸盐气候变化的速率遵循时间的对数函数.
结论:
- 碳酸盐气候变化表现出不同的阶段:在早期阶段快速,在后期阶段缓慢.
- 该研究提供了一种定量方法,以评估碳酸盐染持续时间超过100年.
- 元素移动性和变化指数是气候变化的关键指标.
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