全球硅酸盐岩化学风化—二氧化碳消耗定量模型研究进展<sup>*</sup>

doi:10.7605/gdlxb.2024.02.015

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Abstract

Silicate rocks are factors that influence the global carbon cycle as well as climate change by chemically reacting with carbon dioxide,removing atmospheric carbon dioxide and sequestering it in weathering products or ocean carbonate rocks. Quantifying the total amount of carbon dioxide consumed by weathering of global silicate rocks is key to understanding the Earth’s current and past climate change. This paper systematically investigates the data sources,research methods,calculation formulas,and main influencing factors of five quantitative models of chemical weathering-CO₂ consumption of silicate rocks. The CO₂ consumption calculated by the latest Celine model serves as a reference standard for comparing the advantages,disadvantages and scope of application of each model. The existing models estimate the global carbon dioxide consumption of chemical weathering of rock silicate rocks to be 69-169 Tg/yr,in which the main parameters of each model include climate(temperature,runoff)and lithology,and the secondary parameters include tectonic uplift,volcanism and plant interaction. Future exploration of the quantitative calculation of carbon dioxide consumed by the chemical weathering of silicate rocks should consider more control effects and the interconnections between factors. In addition,the use of big data analysis methods to generalize these quantitative models to the reconstruction of the palaeoclimate of the deep earth may be a future research trend.

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	Articles by authors
	BAI Jie
	ZHENG Dongyu
	HOU Mingcai
	CHEN Anqing
	MA Chao

Key words： chemical weathering of silicate rock quantitative model of CO₂ consumption global carbon cycle climatic change palaeoclimate reconstruction

Received: 06 January 2023

ZTFLH:

P512.2+2

Fund:

Co-funded by the National Natural Science Foundation of China Youth Program(No.42202125)and the “Deep-time Digital Earth” International Big Science Program

Corresponding Authors: ZHENG Dongyu,born in 1992,Ph.D.,associate professor,is mainly engaged in deep-time deep earth reconstruction,geoscience big data and artificial intelligence research. E-mail: dzheng9295@126.com.

About author: BAI Jie,born in 1998,master degree candidate,majors in sedimentology and stratigraphic paleontology. E-mail: 737105916@qq.com.

Cite this article:

BAI Jie,ZHENG Dongyu,HOU Mingcai et al. Research progress on quantitative models of chemical weathering-carbon dioxide consumption of global silicate rocks[J]. JOPC, 2024, 26(2): 460-474.

URL:

http://www.gdlxb.cn/EN/10.7605/gdlxb.2024.02.015 OR http://www.gdlxb.cn/EN/Y2024/V26/I2/460

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