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Methods to estimate aggregate protected soil organic carbon, 2: Does the grinding of the plant residues affect the estimations of the aggregate protected soil organic carbon?

机译:估算保护性土壤有机碳总量的方法,2:植物残渣的研磨是否会影响保护性土壤有机碳总量的估算?

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摘要

A method to estimate the amount of soil organic carbon (SOC) physically protected within macroaggregates (>200 micro m) consists of crushing soil samples and measuring the following SOC mineralization increase. This study investigated the effect of grinding the plant residues during soil crushing on the calculated amount of the protected SOC on two tropical soils (Arenosol and Ferralsol). Incubations of crushed and uncrushed soil samples amended with ground or unground plant residues were conducted. Our results showed that soil crushing increased SOC mineralization and that the presence of plant residues enhanced soil respiration also. The plant residues of the two soils had different decomposition rates, but grinding plant residues did not increase the amounts of cumulative carbon (C) mineralized after the 28 days of the experiment. We propose that the extra C mineralized after soil crushing is due to the breakdown of the soil structure and not to the grinding of plant residues.
机译:估算大型集料(> 200微米)中物理保护的土壤有机碳(SOC)量的方法包括粉碎土壤样品并测量随后的SOC矿化度增加。这项研究调查了土壤压碎过程中研磨植物残留物对两种热带土壤(Arenosol和Ferralsol)上受保护SOC的计算量的影响。进行压碎和未压碎土壤样品的培养,并用已研磨或未研磨的植物残渣进行培养。我们的结果表明,土壤压碎增加了SOC的矿化作用,而且植物残渣的存在也增强了土壤的呼吸作用。两种土壤的植物残渣具有不同的分解速率,但磨碎的植物残渣并没有增加实验28天后矿化的累积碳(C)量。我们认为,土壤压碎后矿化的多余碳是由于土壤结构的破坏而不是植物残渣的磨碎。

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