首页> 外文期刊>Geoderma: An International Journal of Soil Science >Linking short-term soil carbon and nitrogen dynamics: Environmental and stoichiometric controls on fresh organic matter decomposition in agroecosystems
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Linking short-term soil carbon and nitrogen dynamics: Environmental and stoichiometric controls on fresh organic matter decomposition in agroecosystems

机译:联系短期土壤碳和氮动力学:农业生态系统中新鲜有机物分解的环境和化学计量控制

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We developed a continuous, nonlinear model (FLOG-CN) linking carbon mineralization and nitrogen mineralization-immobilization with respect to time that successfully reproduced the complex CO2-C and SMN dynamics for a collection of 70 paired C and N soil datasets. Application of the model to diverse C and N datasets showed that incorporating latency into the model of C mineralization, and using C to drive N dynamics, allows heterogeneous data from many different soil amendments to be described by the same model. We successfully modeled complex CO2-C and SMN dynamics of widely different shapes and from a variety of soil amendments containing plant and animal residues. The re-interpretation of these datasets with the FLOG-CN models improved the quantitative analysis of C and N dynamics, yielding new insights into how amendment characteristics and experimental conditions influence the timing and quantity of C and N mineralized. Model parameters were responsive to varying soil characteristics (pH, C, N, C:N), amendment N:C, amendment rate, incubation temperature, and N additions. Stepwise regression was used to predict model parameters using metadata available for 56 of these datasets. Significant relationships were developed to estimate model parameters independently using measured system properties or other model parameters that could be independently estimated. Estimates of C and N dynamics both fell along a 1:1 line indicating that the model parameters could be adequately described by the measured properties, but the available metadata was not able to describe C dynamics with high precision. Nitrogen mineralization-immobilization was strongly related to amendment N:C, and switched between the two processes at an amendment N:C between 0.077 and 0.085 (C:N between 11.7 and 12.9). We believe that the modeling approach described here will allow quantitative and objective comparisons of diverse C and N datasets that have been hindered by subjective descriptions of the past. (C) 2016 Elsevier B.V. All rights reserved.
机译:我们开发了一个连续的非线性模型(FLOG-CN),该模型将碳矿化和氮矿化固定有关的时间相关联,该模型成功地重现了复杂的CO2-C和SMN动态,收集了70对成对的C和N土壤数据集。该模型在不同的C和N数据集上的应用表明,将潜伏期纳入C矿化模型中,并使用C来驱动N动力学,可以用同一模型描述来自许多不同土壤改良剂的异质数据。我们成功地模拟了形状和形状各异的复杂CO2-C和SMN动力学,这些动力学来自包含植物和动物残留物的多种土壤改良剂。用FLOG-CN模型重新解释这些数据集可改善对C和N动力学的定量分析,从而获得关于修正特征和实验条件如何影响矿化C和N的时间和数量的新见解。模型参数响应于变化的土壤特性(pH,C,N,C:N),修正N:C,修正率,孵育温度和氮添加。使用逐步回归来预测模型参数,使用可用于这些数据集中的56个数据集的元数据。开发了重要的关系以使用测得的系统属性或其他可以独立估计的模型参数来独立估计模型参数。 C和N动力学的估计值均沿1:1线下降,这表明模型参数可以由所测量的特性充分描述,但是可用的元数据无法高精度地描述C动力学。氮矿化固定与修正N:C密切相关,并且在修正N:C在0.077和0.085之间(C:N在11.7和12.9之间)之间在两个过程之间切换。我们相信这里描述的建模方法将允许定量和客观地比较过去受主观描述阻碍的各种C和N数据集。 (C)2016 Elsevier B.V.保留所有权利。

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