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Numerical Modeling of Influence of the Thermal Power Plant with Considering the Hydrometeorological Condition at the Reservoir – Cooler

Numerical Modeling of Influence of the Thermal Power Plant with Considering the Hydrometeorological Condition at the Reservoir – Cooler

Alibek Issakhov
Copyright: © 2014 |Volume: 3 |Issue: 2 |Pages: 16
ISSN: 2160-9500|EISSN: 2160-9543|EISBN13: 9781466654082|DOI: 10.4018/ijeoe.2014040101
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MLA

Issakhov, Alibek. "Numerical Modeling of Influence of the Thermal Power Plant with Considering the Hydrometeorological Condition at the Reservoir – Cooler." IJEOE vol.3, no.2 2014: pp.1-16. http://doi.org/10.4018/ijeoe.2014040101

APA

Issakhov, A. (2014). Numerical Modeling of Influence of the Thermal Power Plant with Considering the Hydrometeorological Condition at the Reservoir – Cooler. International Journal of Energy Optimization and Engineering (IJEOE), 3(2), 1-16. http://doi.org/10.4018/ijeoe.2014040101

Chicago

Issakhov, Alibek. "Numerical Modeling of Influence of the Thermal Power Plant with Considering the Hydrometeorological Condition at the Reservoir – Cooler," International Journal of Energy Optimization and Engineering (IJEOE) 3, no.2: 1-16. http://doi.org/10.4018/ijeoe.2014040101

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Abstract

This paper presents the mathematical model of the thermal power plant in cooling pond under different hydrometeorological conditions, which is solved by three dimensional Navier - Stokes equations and temperature equation for an incompressible fluid in a stratified medium. A numerical method based on the projection method, which divides the problem into three stages. At the first stage it is assumed that the transfer of momentum occurs only by convection and diffusion. Intermediate velocity field is solved by method of fractional steps. At the second stage, three-dimensional Poisson equation is solved by the Fourier method in combination with tridiagonal matrix method (Thomas algorithm). Finally at the third stage it is expected that the transfer is only due to the pressure gradient. To increase the order of approximation compact scheme was used. Then qualitatively and quantitatively approximate the basic laws of the hydrothermal processes depending on different hydrometeorological conditions are determined.

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