Soil Carbon Fluxes and Sensitivity Analysis – A Study in Pinus roxburghii Forest

Deepa Dhital, Bikash Gosain, S. R. Maharjan
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Abstract

The predicted increasing atmospheric carbon dioxide (CO2) level is responsive to altering the future climate, and a small change in the soil carbon may significantly affect the forest carbon cycle and climate system. Soil respiration (SR) and its influencing factors like soil temperature (ST), soil water content (SWC) and surface litter-fall were measured monthly over one year in a sub-tropical Pine (Pinus roxburghii) forest of Bhaktapur district located in central Nepal to determine the SR of the forest and, its variations and sensitivity. The results showed that SR varied to the changes in ST by an exponential significant positive correlation between them. The optimum SR was observed between 10 and 22ºC, and the highest SR were obtained above ST at 20ºC. The temperature sensitivity value of SR (Q10) was estimated at Q10 = 2.13. The significant exponential curve represented the effect of SWC on SR. The higher SR rate was mostly measured between 10 and 25% SWC. The monthly and seasonal variations of the SR rate were consistent with the ST, SWC and litter-fall variations. The study showed that the combined effect of temperature and precipitation might be the major cause of SR variations; however, ST is adequate for increasing SR. Hence, the warming further enhances carbon emission from the forest floor and inversely increases carbon to contribute to climatic change through this pine-dominated forest stand structure.
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刺梨松林土壤碳通量及其敏感性分析
预测的大气二氧化碳水平增加是对未来气候变化的响应,土壤碳的微小变化可能会显著影响森林碳循环和气候系统。在尼泊尔中部巴克塔普尔地区的亚热带松林中,对土壤呼吸(SR)及其影响因子如土壤温度(ST)、土壤含水量(SWC)和地表凋落物进行了1年的逐月测量,以确定森林的SR及其变化和敏感性。结果表明,SR与ST的变化呈指数显著正相关。在10 ~ 22℃温度范围内,产率最佳,在20℃温度范围内产率最高。估计SR (Q10)的温度敏感性值为Q10 = 2.13。显著的指数曲线反映了SWC对SR的影响,较高的SR率主要发生在10% ~ 25% SWC之间。SR率的月变化和季节变化与ST、SWC和凋落物变化基本一致。研究表明,温度和降水的共同作用可能是SR变化的主要原因;因此,气候变暖进一步增加了森林地表的碳排放,并通过这种以松树为主的林分结构反过来增加了碳,从而促进了气候变化。
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