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    碳酸钙粉末添加对土壤交换性阳离子及对溶解性有机碳的耦合调控作用

    Coupling regulation of soil exchangeable cations and dissolved organic carbon by calcium carbonate powder addition

    • 摘要: 目标在碳中和背景下,“增强的碳酸盐岩风化碳汇”作为可交易的碳汇路径,通过大规模撒播碳酸盐岩粉末,以加速其溶解并固定大气CO2。然而,碳酸盐岩矿物粉末的输入在理论上将改变土壤pH及电荷特性,进而可能对交换性阳离子与溶解性有机碳(DOC)的相互作用过程产生影响,这一关键环节缺乏实证研究支撑。方法以典型岩溶土壤(棕色石灰土)和非岩溶土壤(地带性红壤)为供试材料开展了添加碳酸钙的土壤培养实验,探讨了石灰土和红壤交换性阳离子、溶解性有机碳含量以及土壤二氧化碳释放量的变化。结果石灰土和红壤添加碳酸钙后粉末pH均显著上升;石灰土交换性阳离子以交换性钙离子(E-Ca)为主,添加碳酸钙粉末后E-Ca含量占比略微上升,红壤交换性阳离子以交换性铝离子(E-Al)为主,添加碳酸钙粉末后E-Ca含量大幅升高,E-Al含量明显降低;石灰土和红壤添加碳酸钙粉末后DOC含量以及CO2释放量均显著增高(P<0.01)。结论外源碳酸钙输入改变了土壤交换性阳离子组成与含量,进而调控土壤DOC含量,短期内促进土壤CO2排放同步增加,长期尺度下可能参与无机碳循环而无明显释放。本文研究成果为增强的碳酸盐岩风化策略的制定提供科学依据,对实现国家“碳中和碳达峰”战略目标具有重要意义。

       

      Abstract: ObjectiveAgainst the background of carbon neutrality, the enhanced carbonate weathering carbon sink serves as a viable tradable carbon sink pathway. It accelerates carbonate rock dissolution and sequesters atmospheric CO₂ through large-scale application of carbonate rock powder. The input of carbonate mineral powder can theoretically change soil pH and charge properties, which may further affect the interaction between exchangeable cations and dissolved organic carbon (DOC). However, this critical process still lacks sufficient empirical research verification. MethodsA soil incubation experiment with calcium carbonate addition was conducted using typical karst soil (brown calcareous soil) and non-karst soil (zonal red soil) as test materials, to investigate the variations in exchangeable cations, dissolved organic carbon content and soil carbon dioxide release between calcareous soil and red soil. ResultsThe soil pH of both calcareous soil and red soil increased significantly after calcium carbonate addition. Exchangeable cations in calcareous soil were dominated by exchangeable calcium (E-Ca), and the relative proportion of E-Ca increased slightly following calcium carbonate application. By comparison, exchangeable cations in red soil were mainly dominated by exchangeable aluminum (E-Al). After calcium carbonate addition, E-Ca content rose substantially, while E-Al content decreased markedly. Both DOC content and soil CO₂ emissions in the two soil types increased significantly(p < 0.01). ConclusionsExogenous calcium carbonate input alters the composition and concentrations of soil exchangeable cations, thereby regulating soil DOC content and driving a synchronous increase in soil CO₂ emissions in the short term. In the long run, the relevant carbon may participate in the inorganic carbon cycle without obvious CO₂ release. The findings of this study provide a scientific basis for the formulation of enhanced carbonate weathering strategies, and are of great significance for realizing the national strategic goals of carbon peaking and carbon neutrality.

       

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