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A new approach to trenching experiments for measuring root-rhizosphere respiration in a lowland tropical forest

机译:测量低地热带森林根际根际呼吸的挖沟试验新方法

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Soil respiration in tropical forests is a major source of atmospheric CO sub(2). The ability to partition soil respiration into its individual components is becoming increasingly important to predict the effects of disturbance on CO sub(2) efflux from the soil as the responses of heterotrophic and autotrophic respiration to change are likely to differ. However, current field methods to partition respiration suffer from various methodological artefacts; root-rhizosphere respiration is particularly difficult to estimate. We used trenched subplots to estimate root-rhizosphere respiration in large-scale litter addition (L+), litter removal (L-) and control (CT) plots in a lowland tropical semi-evergreen forest in Panama. We took a new approach to trenching by making measurements immediately before-and-after trenching and comparing them to biweekly measurements made over one year. Root-rhizosphere respiration was estimated to be 38%, 17% and 27% in the CT, L+, and L- plots, respectively, from the measurements taken immediately before and one day after trenching in May-June 2007. Biweekly measurements over the following year provided no estimates of root-rhizosphere respiration for the first seven months due to decomposition of decaying roots. We were also unable to estimate root-rhizosphere respiration during the dry season due to differences in soil water content between trenched and untrenched soil. However, biweekly measurements taken during the early rainy season one year after trenching (May-June 2008) provided estimates of root-rhizosphere respiration of 39%, 24% and 36% in the CT, L+, and L- plots, respectively, which are very similar to those obtained during the first day after trenching. We suggest that measurements taken immediately before and one day after root excision are a viable method for a rapid estimation of root-rhizosphere respiration without the methodological artefacts usually associated with trenching experiments.
机译:热带森林中的土壤呼吸是大气中CO sub(2)的主要来源。由于异养和自养呼吸对变化的响应可能不同,因此将土壤呼吸划分为各个组成部分的能力对于预测扰动对土壤中CO sub(2)外流的影响变得越来越重要。然而,目前用于划分呼吸的现场方法受到各种方法学的影响。根际根际呼吸特别难以估计。在巴拿马低地热带半常绿森林中,我们使用挖沟子图估计了大型凋落物添加量(L +),清除凋落物(L-)和控制(CT)地块的根际根际呼吸。我们采用了一种新的挖沟方法,即在挖沟前后立即进行测量,并将其与一年中进行的每两周一次的测量进行比较。根据2007年5月至6月挖沟前后立即进行的测量,在CT,L +和L-图中,根际根际呼吸分别估计为38%,17%和27%。第二年没有提供由于腐烂的根分解而引起的头七个月根际根际呼吸的估计。由于沟渠土壤和未沟壑土壤之间的土壤水分含量差异,我们也无法估计干旱季节的根际根际呼吸。然而,在挖沟后一年(2008年5月至6月)的雨季初进行的每两周一次测量提供的CT,L +和L-图上根际根际呼吸的估计分别为39%,24%和36%,与挖沟后第一天获得的结果非常相似。我们建议,在根切除之前和之后立即进行的测量是一种快速估计根-根际呼吸的可行方法,而无需通常与挖沟实验相关的方法学假象。

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