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A simple model for predicting plant residue decomposition based upon their C/N ratio and soil water content

机译:基于植物残渣碳氮比和土壤含水量预测植物残渣分解的简单模型

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This paper develops and tests a simple relationship for predicting the decomposition of plant residues of diverse composition under varying soil water conditions. Known weights of four plants samples comprising of groundnut (Gn), mucuna (Mc), maize (Mz) and bush fallow (Bf), were put in nylon bags and randomly buried in three plots with varying soil moisture conditions (viz:?W1 = 60% field capacity (FC); W2 = 75% FC and W3 = FC) and the weight losses of the samples in the bags determined at different time intervals. At the field capacity state, plant residue composition was the major controlling factor on decomposition rate constants (kd), with Gn (0.032 d-1) and Mc (0.022 d-1) having significantly higher?kd?than Mz (0.019 d-1) and Bf (0.016 d-1).Decreasing soil water reduced the?kd?values of the plant residues. Using a modified first order decay equation that included C/N ratio and soil water content, the patterns of plant residue decomposition of diverse composition under varying soil water conditions were adequately simulated (R2?= 0.95 and RMSE = 8.84). We conclude that plant residue decomposition patterns can be described using simple relationships that required knowledge of the routinely determined C/N ratio of the residues and the soil water content only.
机译:本文开发并测试了一种简单的关系,用于预测在不同土壤水分条件下不同组成的植物残渣的分解。将已知重量的四种植物样品(包括花生(Gn),粘液菌(Mc),玉米(Mz)和灌木休耕(Bf))放入尼龙袋中,并随机埋在三个土壤湿度条件不同的地块中(viz:?W1 = 60%的现场容量(FC); W2 = 75%FC,W3 = FC),并在不同的时间间隔确定袋子中样品的重量损失。在田间状态下,植物残渣组成是分解速率常数(kd)的主要控制因素,其中Gn(0.032 d-1)和Mc(0.022 d-1)的ΔkdΔ显着高于Mz(0.019 d-)。 1)和Bf(0.016 d-1)。减少土壤水分会降低植物残体的kd值。使用包含C / N比和土壤含水量的改进的一阶衰减方程,可以充分模拟在变化的土壤水分条件下不同组成的植物残渣分解的模式(R2α= 0.95,RMSE = 8.84)。我们得出的结论是,可以使用简单的关系来描述植物残渣的分解模式,这种关系仅需要常规确定的残渣C / N比和土壤含水量的知识即可。

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