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A cost-efficient method to assess carbon stocks in tropical peat soil

机译:一种经济有效的方法来评估热带泥炭土壤中的碳储量

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摘要

Estimation of belowground carbon stocks in tropical wetland forests requires funding for laboratory analyses and suitable facilities, which are often lacking in developing nations where most tropical wetlands are found. It is therefore beneficial to develop simple analytical tools to assist belowground carbon estimation where financial and technical limitations are common. Here we use published and original data to describe soil carbon density (kgCm ~(?3); Cd) as a function of bulk density (gC cm~(?3); Bd), which can be used to rapidly estimate belowground carbon storage using Bd measurements only. Predicted carbon densities and stocks are compared with those obtained from direct carbon analysis for ten peat swamp forest stands in three national parks of Indonesia. Analysis of soil carbon density and bulk density from the literature indicated a strong linear relationship (Cd = Bd×495.14+5.41, R2 = 0.93, n = 151) for soils with organic C content >40 %. As organic C content decreases, the relationship between Cd and Bd becomes less predictable as soil texture becomes an important determinant of Cd. The equation predicted belowground C stocks to within 0.92% to 9.57% of observed values. Average bulk density of collected peat samples was 0.127 g cm~(?3), which is in the upper range of previous reports for Southeast Asian peatlands. When original data were included, the revised equation Cd = Bd ×468.76+5.82, with R2 = 0.95 and n = 712, was slightly below the lower 95% confidence interval of the original equation, and tended to decrease Cd estimates. We recommend this last equation for a rapid estimation of soil C stocks for well-developed peat soils where C content >40 %.
机译:估算热带湿地森林的地下碳储量需要资金用于实验室分析和合适的设施,而在大多数热带湿地被发现的发展中国家,这通常是缺乏的。因此,在财务和技术局限性很普遍的情况下,开发简单的分析工具来辅助地下碳估算是有益的。这里我们使用公开和原始的数据来描述土壤碳密度(kgCm〜(?3); Cd)与体积密度(gC cm〜(?3); Bd)的函数关系,可用于快速估算地下碳储量仅使用Bd测量。将预测的碳密度和储量与通过直接碳分析获得的印度尼西亚三个国家公园中十个泥炭沼泽林地的碳密度和储量进行比较。根据文献对土壤碳密度和堆积密度的分析表明,对于有机碳含量> 40%的土壤,其线性关系很强(Cd = Bd×495.14 + 5.41,R2 = 0.93,n = 151)。随着有机碳含量的降低,土壤质地成为Cd的重要决定因素,Cd和Bd之间的关系变得难以预测。该公式预测地下C储量在观测值的0.92%至9.57%之内。收集到的泥炭样品的平均堆积密度为0.127 g cm〜(?3),在以前的东南亚泥炭地报告中处于较高范围。当包括原始数据时,修正方程Cd = Bd×468.76 + 5.82,R2 = 0.95,n = 712,略低于原始方程的较低95%置信区间,并倾向于降低Cd估计值。我们建议使用此最后一个方程式,以快速估算碳含量> 40%的发达泥炭土壤的土壤碳储量。

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