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Carbon and nitrogen pools and mineralization rates in boreal forest soil after stump harvesting

机译:树桩收获后北方森林土壤的碳氮库和矿化速率

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摘要

The use of forest-derived biomass has steadily increased in Finland and Sweden during the past decades leading to more intensive forest management practices in the region, such as whole-tree harvesting, both above- and belowground. Stump harvesting results in a direct removal of stump and coarse-root carbon (C) from the stand and can cause extensive soil disturbance, which has been suggested to increase C mineralization. In this study, the effects of stump harvesting on soil C and nitrogen (N) mineralization, and soil surface disturbance were studied in two different clear-felled Norway spruce (Picea abies) sites in Central Finland. The treatments were whole-tree harvesting (WTH, removal of stems and logging residues), and WTH and stump harvesting (WTH + S). Both sites, Honkola (2 stands) and Haukilahti (6 stands) were mounded. In both treatments, soil samples were taken from different soil layers down to a total depth of 20 cm in the mineral soil from (i) mounds, (ii) undisturbed soil and (iii) pits. The sampling was performed 11-12 years after treatments. Soil C and N mineralization rates were determined in laboratory incubation experiments. In addition, total C and N pools (g m(2)) were estimated for each disturbance class and soil layer. Soil C and N pools had a tendency to be lower following stump harvesting, but no statistically significant treatment effect was detected. Stump harvesting increased soil mixing as indicated by a significant decrease in C concentration in the mound disturbance class. There was no significant effect of stump harvesting on soil C mineralization rates. A combination of mineralization rates and soil pool data showed that field C mineralization (g CO2-C m(-2) yr(-1)) did not significantly differ between stands where stumps were removed or were retained. Further, stump harvesting did not seem to have any stimulating effect on soil CO2 efflux 11-12 years after treatment. (C) 2016 Elsevier B.V. All rights reserved.
机译:在过去的几十年中,芬兰和瑞典对源自森林的生物量的使用稳步增长,从而导致该地区更加密集的森林管理实践,例如在地上和地下进行全树采伐。树桩收割可直接从林分中清除树桩和粗根碳(C),并可能引起广泛的土壤扰动,这提示增加C的矿化作用。在这项研究中,在芬兰中部的两个不同净空的挪威云杉(Picea abies)地点研究了树桩收获对土壤碳和氮(N)矿化以及土壤表面扰动的影响。处理方法是整树采伐(WTH,去除茎和伐木残渣),以及WTH和树桩采伐(WTH + S)。 Honkola(2个看台)和Haukilahti(6个看台)这两个地点均被堆砌。在这两种处理中,均从(i)土墩,(ii)未扰动的土壤和(iii)矿坑的不同土壤层中抽取土壤样品,直至矿物土壤的总深度为20 cm。在治疗后11-12年进行采样。在实验室培养实验中确定土壤碳和氮的矿化率。此外,估计了每种干扰类别和土壤层的总碳库和氮库(g m(2))。树桩收获后土壤碳和氮库有降低的趋势,但未检测到统计学上显着的处理效果。土墩扰动类别中碳浓度的显着降低表明树桩收割增加了土壤混合。树桩收获对土壤碳矿化速率没有显着影响。矿化速率和土壤池数据的组合显示,田间C矿化(g CO2-C m(-2)yr(-1))在去除或保留树桩的林分之间没有显着差异。此外,在处理后11-12年,树桩收割似乎对土壤CO2外流没有任何刺激作用。 (C)2016 Elsevier B.V.保留所有权利。

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