How agriculture managements influence biogeochemical cycles of soil carbon: processes, mechanisms and ecological consequences
As the largest terrestrial carbon (C) pool, soil C includes soil organic carbon (SOC) and soil inorganic carbon (SIC, mainly solid carbonate). The global soil carbon pool is ~3 times the size of the atmospheric pool and ~4 times the size of the biotic pool. Recently, Earth is becoming more vegetated and biological carbon sequestration is significant. The carbon sink capacity of agricultural and degraded soils can account for approximate 50-66% of the historic carbon loss at the global scale. Similarly, individual countries (e.g. China) have seen SOC increases across agroecosystems over the last decades mainly due to the intensive agricultural activities in terms of nitrogen (N) fertilizers. However, substantial reactive N was involved into the ecosystem and thus significantly accelerated soil acidification at the global scales. This evidenced phenomenon shifted our class view of SIC as an unresponsive carbon pool with a turnover time of millennia. During the last decades, soil carbon pool has gained considerable interest, as a potential solution to combat climate change and to enhance soil fertility. Plenty of case studies have shown the effects of agricultural managements on the biogeochemical cycles of soil C. Nevertheless, few attentions have been paid to the dynamics of SIC cycling and the indirect coupling of SOC-SIC. In addition, the effects of warming on soil C dynamics remain uncertain due to the limited understanding of biogeochemical processes. Hence, there are still knowledge gaps in the understanding how agriculture managements influence biogeochemical cycles of both SOC and SIC.
This VSI focuses on following topics: (i) new methods, techniques and models to accurately simulate the spatiotemporal variation in SOC and SIC stock, especially regarding the agricultural managements; (ii) new knowledge in the origin, formation processes, morphology, cycling and carbon sequestration potential of SIC. (iii) The indirect coupling of SOC and SIC.
Guest editors:
Xiaodong Song
Institute of Soil Science, Chinese Academy of Sciences, Nanjing, 211135, China
Wenxiu Zou
Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Harbin, 150081, China
Jinsong Wang
Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, 100101, China
Feng Tao
Cornell University, Ithaca, NY, United States
Manuscript submission information:
Please refer to the Guide for authors to prepare your manuscript, and select the article type of "VSI: biogeochemical cycles" when submitting your manuscript online through https://www.editorialmanager.com/agee/default2.aspx. The submission period is from 01 October 2024 to 30 September 2025.
For any inquiries about the appropriateness of contribution topics, please contact Executive Guest Editor Xiaodong Song via xdsong@issas.ac.cn.
Keywords:
Agriculture managements, Soil organic carbon, Soil inorganic carbon, Spatiotemporal variation, Cycling, Coupling
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