Manure plume modeling in feedlot pen soils

2019 ◽  
Vol 78 (20) ◽  
Author(s):  
Ana Rosa García ◽  
Santiago Nicolás Fleite ◽  
Alicia Fabrizio de Iorio
Keyword(s):  
2005 ◽  
Vol 20 (1-2) ◽  
pp. 119-125 ◽  
Author(s):  
Chris Kennedy ◽  
Hans Ericsson ◽  
P. L. R. Wong

Author(s):  
Shuo Li ◽  
M. R. Flynn

AbstractVisible plumes above wet cooling towers are of great concern due to the associated aesthetic and environmental impacts. The parallel path wet/dry cooling tower is one of the most commonly used approaches for plume abatement, however, the associated capital cost is usually high due to the addition of the dry coils. Recently, passive technologies, which make use of free solar energy or the latent heat of the hot, moist air rising through the cooling tower fill, have been proposed to minimize or abate the visible plume and/or conserve water. In this review, we contrast established versus novel technologies and give a perspective on the relative merits and demerits of each. Of course, no assessment of the severity of a visible plume can be made without first understanding its atmospheric trajectory. To this end, numerous attempts, being either theoretical or numerical or experimental, have been proposed to predict plume behavior in atmospheres that are either uniform versus density-stratified or still versus windy (whether highly-turbulent or not). Problems of particular interests are plume rise/deflection, condensation and drift deposition, the latter consideration being a concern of public health due to the possible transport and spread of Legionella bacteria.


2011 ◽  
Vol 241 (5) ◽  
pp. 1667-1700 ◽  
Author(s):  
Timothy L. Norman ◽  
Shripad T. Revankar

2021 ◽  
Vol 147 (8) ◽  
pp. 04021028
Author(s):  
Minna Ho ◽  
Jeroen M. Molemaker ◽  
Fayçal Kessouri ◽  
James C. McWilliams ◽  
Timu W. Gallien

2021 ◽  
Vol 2056 (1) ◽  
pp. 012022
Author(s):  
A M Bishaev ◽  
M V Abgaryan

Abstract A problem related to the rarefied plasma plume of the stationary plasma thruster (SPT) is considered in the paper. The consideration is conducted fully in terms of kinetics, namely, distribution functions are introduced to describe motion of every plasma component. The system of kinetics equations for the distribution functions should be solved in combination with the Maxwell’s equations. The paper discusses methods for solving the stated problem.


2017 ◽  
Vol 47 (11) ◽  
pp. 2773-2792 ◽  
Author(s):  
Chen Cheng ◽  
Zhaomin Wang ◽  
Chengyan Liu ◽  
Ruibin Xia

AbstractThe ice shelf water (ISW) plume is a prevalent phenomenon at the base of an ice shelf or sea ice adjacent to the ice shelf front. Such plumes may become supercooled and deposit marine ice when they rise. In the existing frazil ice–laden ISW plume models, it is generally assumed that supercooling and frazil ice growth can be adequately treated by using depth-averaged freezing temperature and vertically uniform frazil ice concentration within a plume. In reality, however, the temperature deficit and frazil ice concentration both increase toward the top of the plume. Hence, frazil crystals typically experience a greater deficit than that suggested by the plume’s temperature subtracted from its depth-averaged freezing point. In this study, the authors considered the combined nonlinear effects of vertical structures of frazil ice concentration and thermal forcing within an ISW plume by introducing equilibrium vertical profiles of frazil ice concentration into a horizontal two-dimensional depth-integrated ISW plume model. A series of idealized numerical experiments and an observation-based simulation beneath the western side of Ronne Ice Shelf have been conducted by using the vertically modified and original depth-integrated ISW plume models. It was found that the supercooled area, supercooling level, and suspended frazil ice and marine ice productivities are all substantially underestimated by the original models. Moreover, the differences are sensitive to the selected frazil ice size configuration. These results suggest that the vertical modification introduced in this study can significantly improve simulated marine ice distribution and its corresponding production, in comparison with those estimated by previous depth-integrated models.


2012 ◽  
Vol 49 (5) ◽  
pp. 770-778 ◽  
Author(s):  
Michael P. Applebaum ◽  
William M. Eppard ◽  
Les Hall

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