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JOURNALS // Matematicheskaya Biologiya i Bioinformatika // Archive

Mat. Biolog. Bioinform., 2012 Volume 7, Issue 1, Pages 81–101 (Mi mbb90)

This article is cited in 1 paper

Proceedings of The Second National Conference "Mathematical Modeling in Ecology"

Determination of gas exchange on the border between ecosystem and atmosphere: inverse modeling

M. V. Glagolevabcd, A. F. Sabrekovc

a Institute of Ecological Soil Science of Moscow State University, Moscow, 119899, Russia
b Yugra State University, Khanty-Mansiysk, Tyumen Oblast, 628012, Russian Federation
c Faculty of Soil Science, Lomonosov Moscow State University, Moscow, 119991, Russian Federation
d Tomsk State Pedagogical University, Tomsk, 634061, Russian Federation

Abstract: Technique of data receiving, which is able for determination of the gas flux from the soil by inverse modeling, was suggested. Evaluation of methane flux, using this method, was carried out in a middle taiga oligotrophic wetland. Flux values, determined by suggested technique (1.5–3 mgÑ–ÑÍ$_4$ m$^2$h$^{-1}$), are equal to flux values, determined by static chamber technique in the same wetland. Flux footprint also was determined. It was varied from a few hundred meters (under unstable meteorological conditions) to several thousand meters (under strongly stable meteorological conditions). Suggested technique allows to identify the difference of flux values between two series of measurements, even we takes into account errors of the method and errors, caused by footprint changing during diurnal observations. Dynamic of such factors of methane emission, as water table level and temperature of the soil surface layer can be a cause of this difference.

Key words: micrometeorological methods, inverse scattering method, gas flow from the soil, ethane.

UDC: [551.510.41+551.510.522]:[547.211+556.56]

Received 21.11.2011, Published 26.01.2012



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