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Effects of nitrogen deposition on soil organic carbon fractions in the subtropical forest ecosystems of S China

机译:氮沉降对中国亚热带森林生态系统土壤有机碳组分的影响

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Experiments were conducted between 2003 and 2008 to examine how N additions influence soil organic C (SOC) and its fractions in forests at different succession stages in the subtropical China. The succession stages included pine forest, pine and broadleaf mixed forest, and old-growth monsoon evergreen broadleaf forest. Three levels of N (NH_4NO_3)-addition treatments comprising control, low-N (50kg N ha~(-1) y~(-1)), and medium-N (100kg N ha~(-1) y~(-1)) were established. An additional treatment of high-N (150kg N ha~(-1) y~(-1)) was established in the broadleaf mixed forest. Soil samples were obtained in July 2008 for analysis. Total organic C (TOC), particulate organic C (POC, > 53 μm), readily oxidizable organic C (ROC), nonreadily oxidizable organic C (NROC), microbial biomass C (MBC), and soil properties were analyzed. Nitrogen addition affected the TOC and its fractions significantly. Labile organic-C fractions (POC and ROC) in the topsoil (0-10cm) increased in all the three forests in response to the N-addition treatments. NROC within the topsoil was higher in the medium-N and high-N treatments than in the controls. In the topsoil profiles of the broadleaf forest, N addition decreased MBC and increased TOC, while no significant effect on MBC and TOC occurred in the pine and mixed forests. Overall, elevated N deposition increased the availability of labile organic C (POC and ROC) and the accumulation of NROC within the topsoil irrespective of the forest succession stage, and might enhance the C-storage capacity of the forest soils.
机译:在2003年至2008年之间进行了实验,研究了氮的添加如何影响亚热带中国不同演替阶段的森林中的土壤有机碳(SOC)及其含量。演替阶段包括松林,松林和阔叶混交林,以及季风常绿阔叶林。三种水平的N(NH_4NO_3)加成处理,包括对照,低氮(50kg N ha〜(-1)y〜(-1))和中N(100kg N ha〜(-1)y〜(- 1))成立。在阔叶混交林中建立了一种额外的高氮处理方法(150kg N ha〜(-1)y〜(-1))。 2008年7月获得了土壤样本进行分析。分析了总有机碳(TOC),颗粒有机碳(POC,> 53μm),易氧化有机碳(ROC),非易氧化有机碳(NROC),微生物生物量C(MBC)和土壤性质。氮的添加会显着影响TOC及其馏分。由于添加了氮,所有三个森林中表层土壤(0-10厘米)中不稳定的有机碳分数(POC和ROC)均增加。在中氮和高氮处理下,表土中的NROC高于对照。在阔叶林的表层土壤剖面中,氮的添加降低了MBC并增加了TOC,而在松树林和混交林中对MBC和TOC没有显着影响。总体而言,无论森林演替阶段如何,增加的氮沉降都会增加表层土壤中不稳定有机碳(POC和ROC)的利用率以及NROC的积累,并可能增强森林土壤的C储量。

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