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全球硅酸盐岩化学风化—二氧化碳消耗定量模型研究进展

白洁 郑栋宇 侯明才 陈安清 马超

古地理学报2024,Vol.26Issue(2):460-474,15.
古地理学报2024,Vol.26Issue(2):460-474,15.DOI:10.7605/gdlxb.2024.02.015

全球硅酸盐岩化学风化—二氧化碳消耗定量模型研究进展

Research progress on quantitative models of chemical weathering-carbon dioxide consumption of global silicate rocks

白洁 1郑栋宇 1侯明才 1陈安清 1马超1

作者信息

  • 1. 成都理工大学沉积地质研究院,四川成都 610059
  • 折叠

摘要

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 in-fluencing 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 ad-vantages,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 second-ary parameters include tectonic uplift,volcanism and plant interaction.Future exploration of the quantita-tive 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.

关键词

硅酸盐岩化学风化/二氧化碳消耗定量模型/全球碳循环/气候变化/古气候重建

Key words

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

分类

天文与地球科学

引用本文复制引用

白洁,郑栋宇,侯明才,陈安清,马超..全球硅酸盐岩化学风化—二氧化碳消耗定量模型研究进展[J].古地理学报,2024,26(2):460-474,15.

基金项目

国家自然基金青年项目(编号:42202125)和"深时数字地球"(Deep-time Digital Earth)国际大科学计划联合资助.[Co-funded by the National Natural Science Foundation of China Youth Program(No.42202125)and the"Deep-time Digital Earth"International Big Science Program] (编号:42202125)

古地理学报

OA北大核心CSTPCD

1671-1505

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