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首页> 外文期刊>Agricultural and Forest Meteorology >Effect of thinning-induced gap size on soil CO2 efflux in a reforested spruce forest in the eastern Tibetan Plateau
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Effect of thinning-induced gap size on soil CO2 efflux in a reforested spruce forest in the eastern Tibetan Plateau

机译:青藏高原东部造林云杉林间伐间隙大小对土壤CO2排放的影响

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Understanding the effects of forest management practices (e.g. thinning) on soil respiration (R-s) is crucial for the accurate estimation of forest carbon budget. However, little is known about the response of R-s to forest thinning in the subalpine region and its linkage to changes in environmental factors induced by thinning. We aimed to quantify the response of R-s rate to various gap sizes following thinning treatments, and to explore the relationships between Rs and soil temperature and moisture and other biophysical factors in the different gap sizes. We applied the thinning by simulating gap formation (four gap sizes at 0, 74, 109 and 196 m(2)) in a 26-year old spruce plantation in the eastern Tibetan Plateau. We measured R-s monthly before (July to November 2008) and after (December 2008 to June 2012) thinning, as well as monthly soil temperature and moisture and other biophysical factors. Thinning tended to decrease fine root biomass, litterfall, soil extractable C, and increased soil temperature and soil moisture. The change in soil temperature and moisture depended on the time after thinning and the size of forest gap. We found that R-s showed an immediate decrease in initial stage after thinning, followed by a gradual increase with understory development towards the level at the control plot. Overall, thinning decreased R-s rate by 14.9%, 15.8% and 25.8% in the small, intermediate and large gap, respectively, as compared to the control. We concluded that the decrease in Rs rates by thinning in a spruce plantation was driven by the decline in tree root biomass and reduction in soil labile C. The positive effect of soil temperature elevation under thinning on Rs was masked by other factors, and the development of understory vegetation after thinning gradually offset the thinning-induced R-s reduction. Our results suggest the need to consider a set of abiotic and biotic factors induced by forest thinning intensity on R-s rates in modeling the response of soil C cycling to forest management practices. (C) 2016 Elsevier B.V. All rights reserved.
机译:了解森林管理实践(例如间伐)对土壤呼吸(R-s)的影响对于准确估算森林碳收支至关重要。然而,关于亚高山地区R-s对森林稀疏的反应及其与稀疏引起的环境因素变化的联系的了解甚少。我们旨在量化稀疏处理后Rs速率对各种间隙尺寸的响应,并探讨不同间隙尺寸下Rs与土壤温度和湿度以及其他生物物理因素之间的关系。我们通过模拟在青藏高原东部具有26年历史的云杉人工林中的间隙形成(0、74、109和196 m(2)处的四个间隙大小)来应用间伐。我们在稀疏之前(2008年7月至2008年11月)和之后(2008年12月至2012年6月)每月测量R-s,以及每月土壤温度,湿度和其他生物物理因素。间伐趋于减少细根生物量,凋落物,土壤可提取碳,并增加土壤温度和土壤湿度。土壤温度和湿度的变化取决于间伐时间和林隙的大小。我们发现,R-s在变薄后的初始阶段立即下降,随后随着底层发育向对照样地水平逐渐增加。总体而言,与对照相比,细化处理在小,中和大间隙中分别降低R-s率14.9%,15.8%和25.8%。我们得出的结论是,云杉人工林间伐变薄引起的Rs率降低是由树根生物量的下降和土壤不稳定碳的减少所驱动的。间伐下土壤温度升高对Rs的积极影响被其他因素所掩盖,并且其发展间伐后植被的减少逐渐抵消了间伐引起的Rs减少。我们的结果表明,在模拟土壤碳循环对森林管理实践的响应时,需要考虑由森林间伐强度对R-s速率诱导的一系列非生物和生物因素。 (C)2016 Elsevier B.V.保留所有权利。

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