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首页> 外文期刊>European Journal of Soil Science >Reproducibility of a soil organic carbon fractionation method to derive RothC carbon pools
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Reproducibility of a soil organic carbon fractionation method to derive RothC carbon pools

机译:土壤有机碳分馏方法可再现RothC碳库的重现性

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摘要

Fractionation of soil is undertaken to isolate organic carbon with distinct functional properties, such as stability and turnover times. Soil organic carbon (SOC) fractionation helps us to understand better the response of SOC to changes in land use, management or climate. However, fractionation procedures are often poorly defined and there is little information available on their reproducibility in different laboratories. In a ring trial, we assessed the reproducibility of a SOC fractionation method introduced by Zimmermann et al. (2007). The isolated fractions were linked to the model pool sizes of the Rothamsted carbon model (RothC). We found significant differences between six laboratories for all five defined fractions in three different soils with coefficients of variation ranging from 14 to 138%. During ultrasonic dispersion, the output power (energy per unit time) was identified as an important factor controlling the distribution of SOC within these five fractions, while commonly only the output energy is standardized. The amount of water used to wet-sieve dispersed soil slurry significantly influenced the amount of extracted dissolved organic carbon (DOC). We therefore suggest using a fixed amount of power for ultrasonic dispersion (20W) and a minimum amount of water for wet sieving (2000ml). RothC pool sizes were predicted from the measured fractions and compared with RothC equilibrium pool size distributions. This model initialization using measured SOC fractions, however, led to an over-estimation of stable RothC SOC pools when compared with pool size distributions derived from RothC equilibrium runs under a bare fallow soil model simulation. To improve the isolation of particulate organic matter from stable mineral-bound organic matter, we suggest that the density should be increased from 1.8 to 2.0gcm(-3) in the density fractionation step. We formulated a modified fractionation procedure, which aims specifically to enhance reproducibility across laboratories and to improve the match of the isolated SOC fractions with RothC's SOC pools.
机译:进行土壤分级分离以分离具有不同功能特性(例如稳定性和周转时间)的有机碳。土壤有机碳(SOC)分级有助于我们更好地了解SOC对土地利用,管理或气候变化的响应。但是,分馏程序通常定义不清,在不同实验室中几乎没有关于其重现性的信息。在一项环形试验中,我们评估了Zimmermann等人介绍的SOC分馏方法的重现性。 (2007)。分离的馏分与Rothamsted碳模型(RothC)的模型库大小相关。我们发现六个实验室之间在三种不同土壤中所有五个定义的馏分之间存在显着差异,变异系数在14%至138%之间。在超声分散过程中,输出功率(每单位时间的能量)被确定为控制这五个部分中SOC分布的重要因素,而通常只有输出能量是标准化的。用于湿筛分散土壤浆液的水量显着影响提取的溶解有机碳(DOC)的量。因此,我们建议使用固定量的功率进行超声波分散(20W),并使用最少量的水进行湿筛(2000ml)。 RothC库大小由测得的馏分预测,并与RothC平衡库大小分布进行比较。但是,与裸露土壤模型模拟下的RothC平衡得出的池大小分布相比,使用测得的SOC分数进行的模型初始化导致对RothC SOC稳定池的估计过高。为了改善从稳定的矿物结合的有机物中分离出颗粒状有机物的方法,我们建议在密度分级步骤中将密度从1.8gcm(-3)增加到2.0gcm(-3)。我们制定了一种改进的分级分离程序,该程序专门旨在提高各个实验室的重现性,并改善分离的SOC组分与RothC的SOC池的匹配度。

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