全球硅酸盐岩化学风化&mdash;二氧化碳消耗定量模型研究进展<sup>*</sup>

doi:10.7605/gdlxb.2024.02.015

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

所属专题：沉积岩石学进展；

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

成都理工大学沉积地质研究院,四川成都 610059

收稿日期:2023-01-06 修回日期:2023-07-12 出版日期:2024-04-01 发布日期:2024-04-03
通讯作者: 郑栋宇,男,1992年生,博士,副教授,主要从事深时深地数字地球重建、地学大数据与人工智能研究。E-mail: dzheng9295@126.com。
作者简介:白洁,女,1998年生,硕士研究生,沉积学与地层古生物学专业。E-mail: 737105916@qq.com。
基金资助:
*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

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

BAI Jie, ZHENG Dongyu, HOU Mingcai, CHEN Anqing, MA Chao

Institute of Sedimentary Geology,Chengdu University of Technology,Chengdu 610059,China

Received:2023-01-06 Revised:2023-07-12 Online:2024-04-01 Published:2024-04-03
Contact: 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.
Supported by:
Co-funded by the National Natural Science Foundation of China Youth Program(No.42202125)and the “Deep-time Digital Earth” International Big Science Program

摘要/Abstract

摘要：

硅酸盐岩通过与二氧化碳的化学反应,去除大气二氧化碳并将其封存在风化产物或海洋碳酸盐岩中,是影响全球碳循环以及气候变化的要素之一。定量计算全球硅酸盐岩通过风化作用消耗的二氧化碳总量是了解地球现今与过去气候变化的关键。作者系统调研了5个硅酸盐岩化学风化—二氧化碳消耗定量模型的数据来源、研究方法、计算公式以及各模型的主要影响因素, 并且以最新的Celine模型所计算得出的二氧化碳消耗量为参考标准,对比了各模型的优缺点与适用范围。现有模型估计全球硅酸盐岩化学风化的二氧化碳消耗量为69~169 Tg/yr,其中各模型的主要参数包括气候(温度、径流)与岩性,次要参数包括构造隆升、火山与植物作用等。在未来探索硅酸盐岩化学风化所消耗二氧化碳的定量计算中,应考虑更多控制作用的影响以及各因素之间的相互联系。此外,利用大数据分析方法将这些定量模型推广应用于深时地球古气候重建可能是未来的研究趋势。

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

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.

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

中图分类号:

P512.2+2

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.

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

http://www.gdlxb.cn/CN/Y2024/V26/I2/460

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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^*