REPLY TO A.V. SMAGIN: V. WHAT IS WRONG WITH AN “ABIOTIC PAPER” AND DO WE ALWAYS NEED TO TAKE INTO ACCOUNT THE ABIOTIC GAS ABSORPTION BY SOIL?

M. Glagolev, A. Sabrekov
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引用次数: 2

Abstract

A paper of prof. A.V. Smagin [2007] is analyzed (both from outer scientometric and inner meaningful points of view). In this paper he considers the abiotic absorption of gases by organogenic soils. In this regard, claims of the author of the article to the work of V. M. Stepanenko and his colleagues on the modeling of methane emissions from lakes on the territory of permafrost are also discussed. An idea that (in contrast to the views of A.V. Smagin) a necessity to account for abiotic uptake depends on properties of modeled object is formulated. In particular, if blocks of climate models are developed (like the Stepanenko model), which should work on timescales of 103÷104 hours and more, it makes no sense to take into account the abiotic uptake that occurs within significantly shorter time intervals and concerns an extremely small amount of methane (compared to its total amount, which is released within the indicated 103-104 hours). In addition potential uncertainties of deep soil chamber technique that could be generated by abiotic absorption and biogenic oxidation of methane are discussed.
回复a.v. smagin:“非生物纸”有什么问题,我们是否总是需要考虑土壤对非生物气体的吸收?
本文分析了A.V. Smagin教授[2007]的一篇论文(从外在科学计量学和内在意义两个角度)。在本文中,他考虑了有机土壤对气体的非生物吸收。在这方面,还讨论了文章作者对v·m·斯捷潘年科及其同事关于永久冻土地区湖泊甲烷排放建模的工作的主张。一个想法(与A.V. Smagin的观点相反)考虑非生物吸收的必要性取决于建模对象的特性。特别是,如果开发了一系列气候模型(如斯捷潘年科模型),这些模型应该在103÷104小时或更长时间尺度上工作,那么考虑在明显较短的时间间隔内发生的非生物吸收是没有意义的,并且只涉及极少量的甲烷(与在指示的103-104小时内释放的甲烷总量相比)。此外,还讨论了甲烷的非生物吸收和生物氧化对深层土壤室技术可能产生的不确定性。
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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