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Organic carbon stocks and sequestration rates of forest soils in Germany

机译:德国的有机碳储量和森林土壤的固存率

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摘要

The National Forest Soil Inventory (NFSI) provides the Greenhouse Gas Reporting in Germany with a quantitative assessment of organic carbon (C) stocks and changes in forest soils. Carbon stocks of the organic layer and the mineral topsoil (30 cm) were estimated on the basis of ca. 1.800 plots sampled from 1987 to 1992 and resampled from 2006 to 2008 on a nationwide grid of 8 × 8 km. Organic layer C stock estimates were attributed to surveyed forest stands and CORINE land cover data. Mineral soil C stock estimates were linked with the distribution of dominant soil types according to the Soil Map of Germany (1 : 1 000 000) and subsequently related to the forest area. It appears that the C pool of the organic layer was largely depending on tree species and parent material, whereas the C pool of the mineral soil varied among soil groups. We identified the organic layer C pool as stable although C was significantly sequestered under coniferous forest at lowland sites. The mineral soils, however, sequestered 0.41 Mg C ha−1 yr−1. Carbon pool changes were supposed to depend on stand age and forest transformation as well as an enhanced biomass input. Carbon stock changes were clearly attributed to parent material and soil groups as sandy soils sequestered higher amounts of C, whereas clayey and calcareous soils showed small gains and in some cases even losses of soil C. We further showed that the largest part of the overall sample variance was not explained by fine-earth stock variances, rather by the C concentrations variance. The applied uncertainty analyses in this study link the variability of strata with measurement errors. In accordance to other studies for Central Europe, the results showed that the applied method enabled a reliable nationwide quantification of the soil C pool development for a certain period.
机译:国家森林土壤清单(NFSI)为德国的温室气体报告提供了对有机碳(C)储量和森林土壤变化的定量评估。有机层和矿物表层土壤(30厘米)的碳储量是根据约1。在1987年至1992年期间对1800个样地进行了采样,并在2006年至2008年对全国8×8 km的网格进行了重新采样。有机层C的存量估算值归因于调查的林分和CORINE土地覆盖数据。根据德国土壤图(1:1 000 000),矿质土壤碳储量估算值与主要土壤类型的分布有关,并随后与森林面积有关。看来,有机层的碳库很大程度上取决于树木和母本,而矿物土壤的碳库在不同的土壤类别之间变化。我们确定有机层C池稳定,尽管C在低地站点的针叶林下被大量隔离。然而,矿质土壤中螯合了0.41 Mg C ha -1 yr -1 。碳库的变化被认为取决于林分年龄和森林改造以及增加的生物量输入。碳储量变化显然归因于母体材料和土壤组,因为沙质土壤固存了较高的C,而粘土质和石灰质土壤的C增幅很小,在某些情况下甚至是损失。我们进一步表明,总体样本中最大的一部分变异不是由细土资源变异解释的,而是由C浓度变异解释的。本研究中应用的不确定性分析将地层的可变性与测量误差联系在一起。根据对中欧地区的其他研究,结果表明,所应用的方法能够在一定时期内对全国土壤碳库的发育进行可靠的量化。

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