Mean Oxidation Number of Organic Carbons for Quantifying Biomethane in Organophosphorous Compounds

Pong Kau Yuen, C. M. Lau
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Abstract

Anaerobic digestion is a complex biochemical process in which organic matters are mineralized and stabilized into biogas and digestate by microorganisms in the absence of oxygen. Buswell’s equation is an ideal model to represent anaerobic digestion for counting theoretical quantity of biogas and digestate in organic matters. Although the degradability and recovery of phosphorous element in digestate have been studied, the impact of phosphorous element on quantity of biomethane and theoretical biomethane potential in organophosphorous compounds are rarely explored. The quantity of biomethane is dependent on the elemental composition of organic matters, and the mean oxidation number of organic carbons is used as a counting parameter in Buswell’s equation. Biowastes which contain organophosphorous compounds are chosen to demonstrate this notion. This article has two purposes. First, the mathematical relationships among empirical formula of organic matter, mean oxidation number of organic carbons, quantity of biomethane, and theoretical biomethane potential are explored. Second, the impact of quantity of phosphorous element on quantity of biomethane, theoretical biomethane potential, and the ratio of biomethane to carbon dioxide are studied.
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用于量化有机磷化合物中生物甲烷的有机碳平均氧化数
厌氧消化是一个复杂的生化过程,在这个过程中,有机物被矿化并稳定成沼气,并在缺氧的情况下被微生物消化。Buswell方程是表示厌氧消化的理想模型,用于计算有机物中沼气和消化物的理论量。虽然对消化液中磷元素的可降解性和回收率进行了研究,但对有机磷化合物中磷元素对生物甲烷量和理论生物甲烷势的影响研究甚少。生物甲烷的数量取决于有机质的元素组成,有机碳的平均氧化数作为Buswell方程的计数参数。选择含有有机磷化合物的生物废物来证明这一概念。本文有两个目的。首先,探讨了有机质经验公式、有机碳平均氧化数、生物甲烷量和理论生物甲烷势之间的数学关系;其次,研究了磷元素含量对生物甲烷含量、理论生物甲烷势和生物甲烷/二氧化碳比的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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