1984
DOI: 10.1061/(asce)0733-9429(1984)110:10(1340)
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Two‐Dimensional Mass Transport in Estuaries

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Cited by 19 publications
(7 citation statements)
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“…the effective stresses in (3, (6), (9) and (10) represent the composite actions resulting from turbulence and molecular diffusion and dispersion. Here Cf is the resistance coefficient at the bed (Cf= n2g/h"3 for the natural situation, where n is the Manning coefficient and h = (( -Z, , = hu+hJ is the total depth) and u* and v* are the depth-averaged velocity components in the 5-and ?-directions respectively, i.e.…”
Section: (3) Thusmentioning
confidence: 99%
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“…the effective stresses in (3, (6), (9) and (10) represent the composite actions resulting from turbulence and molecular diffusion and dispersion. Here Cf is the resistance coefficient at the bed (Cf= n2g/h"3 for the natural situation, where n is the Manning coefficient and h = (( -Z, , = hu+hJ is the total depth) and u* and v* are the depth-averaged velocity components in the 5-and ?-directions respectively, i.e.…”
Section: (3) Thusmentioning
confidence: 99%
“…In this step the convection and diffusion terms are first separated from the momentum equations (5), (6), (9) and (lo), i.e. the following equations are solved (k = u, 1):…”
Section: Advection and Difusionji-actional Stepmentioning
confidence: 99%
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“…[1][2][3][4][5][6][7][8]). In [5] an eutrophication models for simulation of seasonal algae concentrations prior to fertilizer application are developed.…”
Section: Introductionmentioning
confidence: 99%
“…In [5] an eutrophication models for simulation of seasonal algae concentrations prior to fertilizer application are developed. These models led to computer implementation of the methodology developed in [7,8] and a number of computer simulations. Further in [6] a three-dimensional numerical eutrophication model has been developed.…”
Section: Introductionmentioning
confidence: 99%