Measurements in Agro-ecologic Micrometeorology Need New Model of Multi-component Reacting Gaseous Flow
Advances in Bioscience and Bioengineering
Volume 5, Issue 4, August 2017, Pages: 51-55
Received: Oct. 30, 2016; Accepted: Dec. 8, 2016; Published: Oct. 18, 2017
Views 1954      Downloads 156
Nurgaliev I. S., UNESCO Chair of Renewable Energy and Electrification of Agriculture at VIESH, Moscow, Russia
Article Tools
Follow on us
New approach to the electrification measurements in agro-ecologic micrometeorology is suggested on the bases of new turbulent model of the flow. Analytical dynamic model of the turbulent multi-component flow in the three-layer boundary system is presented. Turbulence is simulated by the non-zero vorticity, but not only. Other mathematical aspects of the turbulence are an introducing new model of the material point and considering a torsion of their trajectories. The generalized advection-diffusion-reaction equation is derived for an arbitrary number of components in the flow. The flows in the layers are objects for matching requirements on the boundaries between the layers. Different types of transport mechanisms are dominant on the different levels of the layers and space scales. The same models of mass and energy transfer are instrumental in rural electrification concepts.
Rural Electrification, Green House Gas, Mathematical Model, Turbulent Flow, Vorticity, Material Point, Micrometeorology, Turbulent Diffusion
To cite this article
Nurgaliev I. S., Measurements in Agro-ecologic Micrometeorology Need New Model of Multi-component Reacting Gaseous Flow, Advances in Bioscience and Bioengineering. Vol. 5, No. 4, 2017, pp. 51-55. doi: 10.11648/
Copyright © 2017 Authors retain the copyright of this article.
This article is an open access article distributed under the Creative Commons Attribution License ( which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
Vasenev I. I., Valentini R. Experience in Organization Green House Gases Monitoring, C- and N-stockpiles in the Anthropologically Changed Ecosystems in the European Part of Russia. Report on the 1st Annual Scientific-Organizational Conference, Laboratory for Agro-ecological Monitoring, Modeling and Forecasting in Ecosystems (LAMP), Russian State Agrarian University – Moscow Agricultural Academy named after K. A. Timiryazev. December 12, 2012.
Landau L. D., Lifshitz E. M. (1987). Fluid Mechanics. Vol. 6 (2nd ed.). Butterworth–Heinemann.
Burba G. Eddy Covariance Method for Scientific, Industrial, Agricultural and Regulatory Applications. A Field Book on Measuring Ecosystem Gas Exchange and Areal Emission Rates. ISBN 978-0-615-76827-4. LI-COR Biosciences, Lincoln, Nebraska, 332 pp.
Aubinet, M., Vesala T., and Papale D. (Eds.), 2012. Eddy Covariance: A Practical Guide to Measurement and Data Analysis. Springer, Dordrecht, London, New York, 442 pp.
Nurgaliev I. S. «Singularities Are Averted by Vortices». Gravitation and Cosmology, 2010, Vol. 16, No. 4, pp. 313–315.
Nurgaliev I. S.. Modern astronomical knowledge as component of general education for sustainable development. Astronomical and Astrophysical Transactions (AApTr), 2012, Vol. 27, Issue 3, pp. 429–430. ISSN 1055-6796, Cambridge Scientific Publishers.
Nurgaliev I. S. “Confirmation of Cosmological Bounces Predicted by Alexander Friedmann.” International Journal of. Modern Physics: Conference Series, Vol. 3 (2011), pp 281–285.
Baldocchi D. D. “Assessing the eddy covariance technique for evaluating carbon dioxide exchange rates of ecosystems: past, present and future. Global Change Biology, Volume 9, Issue 4, pages 479–492, April 2003.
Webb, E. K., Pearman, G. I., and Leuning, R.: 1980, ‘Correction of Flux Measurements for Density Effects Due to Heat and Water Vapour Transfer’, Quart. J. Roy. Meteorol. Soc. 106, 85–100.
Wyngaard J. C. 1990: Scalar fluxes in the planetary boundary layer -- Theory, modeling, Boundary-Layer Meteorology and measurement. Boundary Layer Meteorology, 50, 49-75.
Fuehrer P. L., C. A. Friehe. Flux Corrections Revisited. Boundary-Layer Meteorology, 102: 415–457, 2002.
Rashevsky P. K. Riemann Geometry and Tensor Analysis (in Russian), Nauka. Eds, Moscow, 1967.
Blokhintsev D. I., Acoustics of a Non-homogeneous Moving Medium, Gostekhizdat, 1945 (English translation: N. A. C. A. Technical Memorandum no. 1399 (1956)).
Howe D. I. Acoustics of Fluid–Structure Interactions, Cambridge University Press, Cambridge, 1998.
Nurgaliev I. S. Physical Kinetics of Demography. Economic Strategies. - 2009. - N 1. - pp. 170-175.
Nurgaliev I. S. Turbulency of the New Risks Demand Revising Strategies of Development. Economic Strategies – 2011, N 6, pp. 56-60
Batchelor, George K.(1973). An introduction to fluid dynamics. Cambridge: Cambridge University Press. ISBN 0-521-09817-3.
Science Publishing Group
1 Rockefeller Plaza,
10th and 11th Floors,
New York, NY 10020
Tel: (001)347-983-5186