Subgrid modeling for the filtered scalar transport equation

Author(s):  
A. Leonard
Author(s):  
S. Wan ◽  
M. S. W. Lau ◽  
J. Leong ◽  
N. An ◽  
K. L. Goh

The present work was movitated by an earlier study on pumps based on a Wankel geometry (Wankel pumps) which revealed a flow structure, rich in three dimensional vortices (including Taylor like counter-rotating ones), in the pump chamber, suggesting the possibility of a Wankel pump of also functioning as a mixer. To this end, numerical mixing experiments were run using the general scalar transport equation to model the evolution of species concentration. Interestingly, it was observed that species dispersion occurs predominantly sideways (laterally) and that vertical dispersion is almost non-existent. In other words, for binary mixing of two species with a Wankel pump, they must be introduced side by side to ensure effective mixing.


Author(s):  
А.В. Соловьев ◽  
А.В. Данилин

Предложена новая разностная схема класса Кабаре повышенного порядка точности для решения скалярного уравнения переноса. Порядок аппроксимации разностной схемы равен четырем. Построено балансно-характеристическое представление схемы и приведены дисперсионные свойства. Для предложенной разностной схемы в сравнении с классической схемой Кабаре рассмотрены примеры решения уравнения переноса для гладкого и разрывного профиля. A new difference scheme of the Cabaret class with a higher order of accuracy for solving the scalar transport equation is proposed. The order of approximation of this difference scheme is equal to four. The balance-characteristic representation of the scheme is constructed and the dispersion properties are given. For the proposed difference scheme, a number of examples to solve the transport equation for smooth and discontinuous profiles are considered in comparison with the classical Cabaret scheme.


1957 ◽  
Vol 4 (3) ◽  
pp. 193-206 ◽  
Author(s):  
Z. A. Melzak

Author(s):  
M. C. Lopes Filho ◽  
H. J. Nussenzveig Lopes

In this article we present a proof of existence of a weak solution for the semigeostrophic system of equations, formulated as an active scalar transport equation with Monge-Ampère coupling, with initial data in . This is an extension of a 1998 result due to Benamou and Brenier, who proved existence with initial data in .


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