环境科学
无机碳总量
土壤水分
碳纤维
吨
陆地生态系统
土壤碳
固碳
碳循环
碳酸盐
环境化学
生态系统
氮气
土壤科学
地理
生态学
二氧化碳
化学
复合数
生物
复合材料
考古
有机化学
材料科学
作者
Yuanyuan Huang,Xiaodong Song,Ying‐Ping Wang,Josep G. Canadell,Yiqi Luo,Philippe Ciais,Anping Chen,Songbai Hong,Yugang Wang,Feng Tao,Wei Li,Yiming Xu,Reza Mirzaeitalarposhti,Heba Elbasiouny,I. Yu. Savin,D. Shchepashchenko,Raphael A. Viscarra Rossel,Daniel S. Goll,Jinfeng Chang,Benjamin Z. Houlton
出处
期刊:Science
[American Association for the Advancement of Science]
日期:2024-04-11
卷期号:384 (6692): 233-239
被引量:70
标识
DOI:10.1126/science.adi7918
摘要
Global estimates of the size, distribution, and vulnerability of soil inorganic carbon (SIC) remain largely unquantified. By compiling 223,593 field-based measurements and developing machine-learning models, we report that global soils store 2305 ± 636 (±1 SD) billion tonnes of carbon as SIC over the top 2-meter depth. Under future scenarios, soil acidification associated with nitrogen additions to terrestrial ecosystems will reduce global SIC (0.3 meters) up to 23 billion tonnes of carbon over the next 30 years, with India and China being the most affected. Our synthesis of present-day land-water carbon inventories and inland-water carbonate chemistry reveals that at least 1.13 ± 0.33 billion tonnes of inorganic carbon is lost to inland-waters through soils annually, resulting in large but overlooked impacts on atmospheric and hydrospheric carbon dynamics.
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