CCPortal
DOI10.1016/j.epsl.2020.116239
A numerical examination of the effect of sulfide dissolution on silicate weathering
Kanzaki Y.; Brantley S.L.; Kump L.R.
发表日期2020
ISSN0012821X
卷号539
英文摘要Silicate weathering regulates climate on geological time scales as a net, climate-sensitive sink of atmospheric CO2. On the other hand, sulfuric acid produced through sulfide dissolution affects silicate weathering, diminishing its effectiveness as a climate regulator based on evidence from river chemistry. This study takes a theoretical approach to quantitatively examine the effect of sulfide dissolution, coupling a one-dimensional model of pyrite weathering to that of albite transformation to kaolinite. The coupled model reveals that when the reaction front of sulfide is deeper than that of silicates reacting with CO2, the silicate-weathering feedback on climate is not directly affected by sulfide dissolution, but only indirectly through oceanic processes such as reverse weathering and carbonate deposition. In turn, when sulfide dissolution occurs within zones of CO2-silicate reactions close to the surface, the feedback between climate and silicate weathering can be significantly weakened because sulfuric acid competes effectively with carbonic acid in mineral dissolution. As the depth of the sulfide reaction front can be changed by variations in water table depth, the latter feedback weakening could have occurred in concert with climate-change-driven water table fluctuations, amplifying atmospheric CO2 variations during the Phanerozoic. © 2020 Elsevier B.V.
关键词atmospheric CO2climatePhanerozoicsilicate weatheringsulfide weatheringwater table
英文关键词Atmospheric chemistry; Carbon dioxide; Climate change; Climate models; Dissolution; Feldspar; Groundwater; Kaolinite; Pyrites; Silicates; Sulfur compounds; Sulfuric acid; Surface reactions; climate; Numerical examination; One-dimensional model; Phanerozoic; Silicate weathering; Theoretical approach; Water table fluctuations; Water tables; Weathering; carbon dioxide; chemical weathering; climate effect; dissolution; numerical method; Phanerozoic; river water; silicate; sulfide; water depth; water table
语种英语
来源期刊Earth and Planetary Science Letters
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/202691
作者单位Department of Earth and Planetary Sciences, University of California – Riverside, Riverside, CA 92521, United States; Earth and Environmental Systems Institute, The Pennsylvania State University, University Park, PA 16802, United States; Department of Geosciences, The Pennsylvania State University, University Park, PA 16802, United States
推荐引用方式
GB/T 7714
Kanzaki Y.,Brantley S.L.,Kump L.R.. A numerical examination of the effect of sulfide dissolution on silicate weathering[J],2020,539.
APA Kanzaki Y.,Brantley S.L.,&Kump L.R..(2020).A numerical examination of the effect of sulfide dissolution on silicate weathering.Earth and Planetary Science Letters,539.
MLA Kanzaki Y.,et al."A numerical examination of the effect of sulfide dissolution on silicate weathering".Earth and Planetary Science Letters 539(2020).
条目包含的文件
条目无相关文件。
个性服务
推荐该条目
保存到收藏夹
导出为Endnote文件
谷歌学术
谷歌学术中相似的文章
[Kanzaki Y.]的文章
[Brantley S.L.]的文章
[Kump L.R.]的文章
百度学术
百度学术中相似的文章
[Kanzaki Y.]的文章
[Brantley S.L.]的文章
[Kump L.R.]的文章
必应学术
必应学术中相似的文章
[Kanzaki Y.]的文章
[Brantley S.L.]的文章
[Kump L.R.]的文章
相关权益政策
暂无数据
收藏/分享

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。