Inorganic carbon losses by soil acidification jeopardize global efforts on carbon sequestration and climate change mitigation

环境科学 固碳 碳纤维 土壤碳 土壤水分 气候变化 具有碳捕获和储存功能的生物能源 减缓气候变化 温室气体清除 全球变暖 自然资源经济学 环境保护 二氧化碳 土壤科学 生态学 地质学 海洋学 经济 复合材料 材料科学 复合数 生物
作者
Sajjad Raza,Kazem Zamanian,Sami Ullah,Yakov Kuzyakov,Iñigo Virto,Jianbin Zhou
出处
期刊:Journal of Cleaner Production [Elsevier BV]
卷期号:315: 128036-128036 被引量:186
标识
DOI:10.1016/j.jclepro.2021.128036
摘要

Soil plays a significant role in controlling the global carbon (C) cycle. Studies on climate change mitigation have focused entirely on soil organic carbon (SOC) to increase C sequestration and decrease carbon dioxide (CO2) emissions. In contrast, the contribution of soil inorganic carbon (SIC) to CO2 emissions is usually neglected because SIC is generally considered to be very stable. However, the significant worldwide increase in soil acidification, mainly because of intensive N fertilization and high atmospheric deposition, causes a considerable decrease in SIC stocks, leading to very high unaccounted CO2 efflux. Additionally, large areas of acidic soils worldwide are regularly subjected to high SIC applications in the form of lime to remediate acidity, which is another direct source of CO2 emission. Consequently, global efforts to mitigate climate change through SOC sequestration need a revisit as SIC-borne C losses are significant both in terms of C stocks and soil fertility loss, upon which future SOC sequestration will be reduced. Compared to SOC, wherein C stocks can be increased through management, SIC losses are irreversible and cause significant decline in soil health, ecosystem services, and functions. The present review is the first to summarize the current information about acidification-induced intensified SIC losses and their mechanisms. It included: (i) natural and anthropogenic sources and causes of soil acidification, (ii) losses of SIC as HCO3− leaching and CO2 efflux from calcareous soils (7.5 Tg C yr−1) and liming (273 Tg C yr−1) during acidity neutralization, (iii) the relationship between climate change and SIC stocks, (iv) consequences of SIC depletion in soil-plant-water systems, and (v) strategies to remediate and control soil acidification. We concluded that acidification-induced SIC-borne CO2 losses are a major C loss pathway and could jeopardize global efforts to mitigate climate change through SOC sequestration.
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