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The ecosystem carbon accumulation after conversion of grasslands to pine plantations in subtropical red soil of south China

机译:中国南方亚热带红壤草地向松树林转化后的生态系统碳积累

摘要

Since 1980s, afforestation in China has led to the establishment of over 0.53 x 10(8) ha of new plantation forests. While this leads to rapid accumulation of carbon (C) in vegetation, the effects of afforestation on soil C are poorly understood. In this study, a new version of the Atmosphere-Vegetation Interaction Model (AVIM2) was used to examine how changes in plant C inputs following afforestation might lead to changes in soil C at one of the Chinaflux sites and to estimate the effect of afforestation on ex-grassland. The potential total C accumulation of tree plantation was also predicted. The model was calibrated by net ecosystem exchange (NEE), ecosystem respiration (RE) and gross primary production (GPP) based on eddy-covariance measurements. The simulated vegetation C and soil C stocks were compared with the filed observations. The simulates indicate that after 22 yr of conversion of grassland to needle leaf forests (Pinus massoniana and Pinus elliottii), the net carbon accumulation in tree ecosystem was 1.96 times more than that in grassland. The soil C in the initial 7 yr of planting decreased at a rate of 0.1871 kg C m(-2) yr(-1), and after that it increased at a rate of 0.090 kg C m(-2) yr(-1). The C accumulation in the studied plantation ecosystem is estimated to be 76-81% of that value in equilibrium state (the net ecosystem productivity approaches to zero). Sensitivity analyses show that conversion from grassland to plantation caused an initial (7 or 8 yr) periods of decrease in soil C stocks in wider red soil area of southern China. The soil C stocks were reduced between 19.2 and 20.4% in the initial decreasing period. After 7 or 8 yr C loss, the increased in soil C stocks was predicted to be between 0.073 and 0.074 kg C m(-2) yr(-1).
机译:自1980年代以来,中国的植树造林导致建立了超过0.53 x 10(8)公顷的新型人工林。虽然这会导致植被中碳(C)的快速积累,但造林对土壤C的影响知之甚少。在这项研究中,使用了新版本的“大气-植被相互作用模型”(AVIM2)来研究造林后植物碳输入的变化如何导致Chinaflux站点之一土壤C的变化,并评估造林对生态系统的影响。前草原。还预测了人工林潜在的总碳积累。基于涡度-协方差测量,通过净生态系统交换(NEE),生态系统呼吸(RE)和初级生产总值(GPP)对该模型进行了校准。将模拟的植被碳和土壤碳储量与实测值进行了比较。模拟表明,在草地转化为针叶林(马尾松和松树)22年后,树木生态系统的净碳积累是草地的1.96倍。播种的最初7年土壤碳以0.1871 kg C m(-2)yr(-1)的速率下降,此后以0.090 kg C m(-2)yr(-1)的速率增加。 )。在平衡状态下,研究的人工林生态系统中的碳积累估计为该值的76-81%(净生态系统生产力接近于零)。敏感性分析表明,从草地到人工林的转变导致了中国南方红壤地区土壤碳储量下降的初始阶段(7年或8年)。在最初的减少期中,土壤碳储量减少了19.2%至20.4%。损失7或8年的C后,土壤C储量的增加预计在0.073至0.074 kg C m(-2)yr(-1)之间。

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