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Updated: May 13, 2025

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在增强岩石气候变化中平衡有机和无机碳动态:对碳封存的影响

Kaiyu Lei1, Franziska B Bucka1,2, Pedro P C Teixeira1

  • 1Chair of Soil Science, School of Life Science, Technical University of Munich, Freising, Germany.

Global change biology
|April 16, 2025
PubMed
概括

增强岩石风化 (ERW) 可以去除二氧化碳,但影响土壤有机碳 (SOC). 新鲜的玄武岩增加了无机碳 (IC),但损失了SOC,而经过气候变化的玄武岩稳定了土壤碳,突出了维持SOC的必要性,以有效地封存碳.

关键词:
13C同位素的追踪13C同位素的追踪玄武岩气候变化 基础盐气候变化碳封存是一种碳封存方式.无机碳的形成 无机碳的形成有机和无机碳池是有机和无机碳池.有机碳的营业额随着pH值的上升土壤碳流是指土壤的碳流.

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