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Manipulating forests to increase soil carbon storage: Calcium and nitrogen fertilization of red spruce stands (Picea rubens).

机译:操纵森林以增加土壤碳储量:红色云杉林(Picea rubens)的钙和氮肥施肥。

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Sequestering atmospheric carbon (C) in forests is a commonly suggested approach to mitigating global climate change. Most analyses have considered vegetation as the primary forest C sink, It has been assumed that soil C pools can be changed only over long time periods. In the research presented here, it was hypothesized that experimental manipulation of calcium (Ca) and nitrogen (N) could increase soil C storage over a short (5-year) period, through effects on the quantity and chemical quality of decomposing litter.; This study examined the effects of Ca and N fertilization on tree productivity, litterfall, and soil C storage in three red spruce (Picea rubens) stands in northeastern U.S. (Big Moose NY (BM), Groton VT (GR), and Hubbard Brook NH (HB)). Thirty-m square plots were fertilized with calcium (160 kg ha--1 yr--1), nitrogen (100 kg ha --1 yr--1), or calcium+nitrogen each year from 1992--1999 (in addition to unfertilized controls). Tree species and diameter at breast height (DBH) were recorded. Litterfall was collected annually and analyzed for C and N. Soil cores were taken in November 1996.; Soil inputs of C and N from litterfall increased in all treatments. There was a significant increase in soil C and N at HB in the calcium+nitrogen treatment after 5 years of fertilization. At BM, soil C and N were lower in fertilized plots than in controls, suggesting a different pattern of forest floor decomposition due to treatment. However, soil C content in unfertilized plots was significantly greater at BM than at HB or GR.; The observed increase in litterfall C was insufficient to account for the increased soil C at HB. It is suggested that, in some stands, nitrogen forms complexes with organic matter that make it more resistant to decomposition, increasing soil C storage over a short time. However, individual site characteristics strongly affected sequestration capacity. Furthermore, it appears that more soil C can be stored in a system changing to a different forest type, as at BM (a spruce stand converting to mixed hardwood-spruce).
机译:在森林中隔离大气中的碳是缓解全球气候变化的一种常用方法。大多数分析都将植被作为主要的森林碳汇,并认为土壤碳库只能在很长的一段时间内改变。在这里提出的研究中,假设钙(Ca)和氮(N)的实验操作可以通过影响分解垃圾的数量和化学质量,在短(5年)内增加土壤碳的存储。这项研究调查了美国东北部三个大的红云杉(Picea rubens)林分(纽约州大驼鹿(BM),格罗顿VT(GR)和新罕布什尔州布鲁克)的钙和氮施肥对树木生产力,凋落物和土壤碳储量的影响。 (HB))。从1992--1999年起,每年在30平方米的土地上施以钙(160 kg ha--1 yr--1),氮(100 kg ha-1yr--1)或钙+氮(另外到未受精的对照)。记录树木种类和胸高直径(DBH)。每年收集凋落物并分析碳和氮。1996年11月取土芯。在所有处理中,凋落物引起的土壤碳和氮的输入均增加。施肥5年后,钙+氮处理使HB上的土壤C和N显着增加。在BM,施肥地的土壤C和N低于对照,表明由于处理,林地分解的模式不同。但是,未施肥地块的土壤碳含量在BM时显着高于HB或GR。观察到的凋落物C的增加不足以说明HB处土壤C的增加。建议在某些林分中,氮与有机物形成络合物,使其更耐分解,从而在短时间内增加了土壤碳的储存量。但是,各个地点的特征严重影响了隔离能力。此外,似乎在BM(将云杉林转变为硬木云杉混合林)的系统中,可以将更多的土壤C存储在更改为不同森林类型的系统中。

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