{"title":"中国植树造林加强风化作用的潜在碳汇效应展望","authors":"Weihua Wu , Werner Nel , Junfeng Ji , Jun Chen","doi":"10.1016/j.jseaes.2024.106370","DOIUrl":null,"url":null,"abstract":"<div><div>The carbon sink effect of afforestation is key to mitigating current global warming. China’s planted forest area accounts for more than a quarter of the global afforestation efforts and has made a prominent contribution to carbon sequestration. Previously, afforestation as a carbon sink was primarily evaluated in terms of the biomass carbon pool and soil organic carbon pool. Plants play a significant role in enhancing the chemical weathering of rocks and minerals, which can lead to more CO<sub>2</sub> consumption. However, role of plants in enhancing chemical weathering and contributing to CO<sub>2</sub> removal has not been considered when calculating the artificial sink. This paper reviews relevant studies on the carbon sinks from weathering and forest biomass in China and synthesizes the research on how plants affecting weathering in natural ecosystems. Based on this, we estimate the atmospheric CO<sub>2</sub> consumption from afforestation-enhanced weathering in China. If afforestation increases the natural weathering rate by a factor of four on average, the national carbon sink through weathering could increase by 33 %. This increase in carbon sink capacity amounts to 35 million tonnes CO<sub>2</sub>/y and represents ∼1/6 of China’s afforestation biomass carbon sink during 2014–2018. The significant contribution underscores the need for further comprehensive research into the carbon sink effect of afforestation-enhanced weathering in the future. Understanding how afforestation, global warming, and other anthropogenic activities interact to affect weathering will provide insights to accurately evaluate the role of large-scale afforestation in China’s efforts to meet its “dual-carbon” goals and mitigate global warming.</div></div>","PeriodicalId":50253,"journal":{"name":"Journal of Asian Earth Sciences","volume":"276 ","pages":"Article 106370"},"PeriodicalIF":2.7000,"publicationDate":"2024-10-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Prospects for the potential carbon sink effects of afforestation to enhance weathering in China\",\"authors\":\"Weihua Wu , Werner Nel , Junfeng Ji , Jun Chen\",\"doi\":\"10.1016/j.jseaes.2024.106370\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>The carbon sink effect of afforestation is key to mitigating current global warming. China’s planted forest area accounts for more than a quarter of the global afforestation efforts and has made a prominent contribution to carbon sequestration. Previously, afforestation as a carbon sink was primarily evaluated in terms of the biomass carbon pool and soil organic carbon pool. Plants play a significant role in enhancing the chemical weathering of rocks and minerals, which can lead to more CO<sub>2</sub> consumption. However, role of plants in enhancing chemical weathering and contributing to CO<sub>2</sub> removal has not been considered when calculating the artificial sink. This paper reviews relevant studies on the carbon sinks from weathering and forest biomass in China and synthesizes the research on how plants affecting weathering in natural ecosystems. Based on this, we estimate the atmospheric CO<sub>2</sub> consumption from afforestation-enhanced weathering in China. If afforestation increases the natural weathering rate by a factor of four on average, the national carbon sink through weathering could increase by 33 %. This increase in carbon sink capacity amounts to 35 million tonnes CO<sub>2</sub>/y and represents ∼1/6 of China’s afforestation biomass carbon sink during 2014–2018. The significant contribution underscores the need for further comprehensive research into the carbon sink effect of afforestation-enhanced weathering in the future. Understanding how afforestation, global warming, and other anthropogenic activities interact to affect weathering will provide insights to accurately evaluate the role of large-scale afforestation in China’s efforts to meet its “dual-carbon” goals and mitigate global warming.</div></div>\",\"PeriodicalId\":50253,\"journal\":{\"name\":\"Journal of Asian Earth Sciences\",\"volume\":\"276 \",\"pages\":\"Article 106370\"},\"PeriodicalIF\":2.7000,\"publicationDate\":\"2024-10-20\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Asian Earth Sciences\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S1367912024003651\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Asian Earth Sciences","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1367912024003651","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
Prospects for the potential carbon sink effects of afforestation to enhance weathering in China
The carbon sink effect of afforestation is key to mitigating current global warming. China’s planted forest area accounts for more than a quarter of the global afforestation efforts and has made a prominent contribution to carbon sequestration. Previously, afforestation as a carbon sink was primarily evaluated in terms of the biomass carbon pool and soil organic carbon pool. Plants play a significant role in enhancing the chemical weathering of rocks and minerals, which can lead to more CO2 consumption. However, role of plants in enhancing chemical weathering and contributing to CO2 removal has not been considered when calculating the artificial sink. This paper reviews relevant studies on the carbon sinks from weathering and forest biomass in China and synthesizes the research on how plants affecting weathering in natural ecosystems. Based on this, we estimate the atmospheric CO2 consumption from afforestation-enhanced weathering in China. If afforestation increases the natural weathering rate by a factor of four on average, the national carbon sink through weathering could increase by 33 %. This increase in carbon sink capacity amounts to 35 million tonnes CO2/y and represents ∼1/6 of China’s afforestation biomass carbon sink during 2014–2018. The significant contribution underscores the need for further comprehensive research into the carbon sink effect of afforestation-enhanced weathering in the future. Understanding how afforestation, global warming, and other anthropogenic activities interact to affect weathering will provide insights to accurately evaluate the role of large-scale afforestation in China’s efforts to meet its “dual-carbon” goals and mitigate global warming.
期刊介绍:
Journal of Asian Earth Sciences has an open access mirror journal Journal of Asian Earth Sciences: X, sharing the same aims and scope, editorial team, submission system and rigorous peer review.
The Journal of Asian Earth Sciences is an international interdisciplinary journal devoted to all aspects of research related to the solid Earth Sciences of Asia. The Journal publishes high quality, peer-reviewed scientific papers on the regional geology, tectonics, geochemistry and geophysics of Asia. It will be devoted primarily to research papers but short communications relating to new developments of broad interest, reviews and book reviews will also be included. Papers must have international appeal and should present work of more than local significance.
The scope includes deep processes of the Asian continent and its adjacent oceans; seismology and earthquakes; orogeny, magmatism, metamorphism and volcanism; growth, deformation and destruction of the Asian crust; crust-mantle interaction; evolution of life (early life, biostratigraphy, biogeography and mass-extinction); fluids, fluxes and reservoirs of mineral and energy resources; surface processes (weathering, erosion, transport and deposition of sediments) and resulting geomorphology; and the response of the Earth to global climate change as viewed within the Asian continent and surrounding oceans.