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Characterization of clay bound organic matter using activation energy calculated by weight loss on ignition method

机译:燃烧法失重计算的活化能表征粘土结合的有机物

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摘要

Soil organic matter (SOM) through intimate associations with clay particles forms clay bound organic matter (CBO), which contributes mainly to long-term stability of SOM in most soils. The CBO fraction contributes mainly to more meaningful carbon sequestration due to their long-term stability and hence storage. The formation and stabilization of CBO is a complex process and studies on determination of the exact composition of this fraction are meagre. In this study, an attempt was made to characterize the CBO of a soil in terms of the other SOM fractions such as fulvic fraction (FF), humic fraction (HF) and fine soil litter. The weight loss on ignition (LOI) data of extracted SOM fractions and fine soil litter were used to characterize CBO. Rate constants (k) of the oxidation reactions during the LOI were calculated using percentage weight losses at different temperatures of the FF, HF and fine soil litter. Calculated activation energies (E-a) of the other SOM fractions at different temperatureswere used in a multiple regression analysis to predict the Ea of the CBO fraction. The results showed that the activation energy of the CBO [E-a (CBO)] was positively related to that of the fine soil litter [E-a (fine soil litter)] and the FF [Ea (FF)].The relationship indicates that the CBO of the soil is composed of a mixture of fine soil litter and the FF, as also proposed in the literature.
机译:通过与粘土颗粒紧密结合的土壤有机质(SOM)形成了粘土结合有机质(CBO),这主要有助于大多数土壤中SOM的长期稳定性。 CBO馏分由于其长期稳定性和储存能力,主要有助于更有意义的碳固存。 CBO的形成和稳定是一个复杂的过程,有关确定该馏分的确切组成的研究还很薄弱。在这项研究中,尝试根据其他SOM组分,例如黄腐组分(FF),腐殖质组分(HF)和细土垫料来表征土壤的CBO。提取的SOM馏分和细土垫料的燃烧失重(LOI)数据用于表征CBO。 LOI期间氧化反应的速率常数(k)是使用FF,HF和细土垫料在不同温度下的重量损失百分比来计算的。在多元回归分析中使用了在不同温度下其他SOM馏分的计算出的活化能(E-a),以预测CBO馏分的Ea。结果表明,CBO [Ea(CBO)]的活化能与细土垫料[Ea(细土垫料)]和FF [Ea(FF)]的活化能呈正相关。如文献中所提出的,土壤中的一部分由细土屑和FF的混合物组成。

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