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Analytical Solution Of The Advection-diffusion Equation For A Ground-level Finite Area Source

机译:地平面有限面积源对流扩散方程的解析解

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An advection-diffusion equation for a ground-level finite area source is solved analytically in a closed form using the superposition method. Power laws are assumed for height-dependent wind speed and vertical eddy diffusivity and for the downwind distance-dependent standard deviation of concentration distribution in the lateral direction. Results of the analysis show that the ground-level concentration increases with increasing downwind distance inside the source region and then decreases rapidly beyond the downwind edge of the source region. The ground-level concentration inside the source region is sensitive to exponents in the power laws for wind speed and vertical eddy diffusivity, while the ground-level concentration outside the source region is sensitive to the standard deviation of concentration distribution in the lateral direction. The solution for the ground-level finite area source is compared with solutions for a laterally infinite area source and a point source. The ratio of the ground-level concentration for the finite area source to that for the laterally infinite area source is highly dependent on lateral eddy diffusivity but almost independent of exponents in the power laws for wind speed and vertical eddy diffusivity. This is also true for the ratio of the ground-level concentration for the finite area source to that for the point source.
机译:地面有限区域源的对流扩散方程采用叠加法以封闭形式解析求解。假定功率定律是针对高度相关的风速和垂直涡流扩散率,以及与下风向相关的横向浓度分布标准偏差。分析结果表明,地面浓度随源区内部顺风距离的增加而增加,然后在源区顺风边缘以外迅速减小。源区域内部的地平面浓度对风速和垂直涡流扩散率的幂律指数敏感,而源区域外部的地平面浓度对横向浓度分布的标准偏差敏感。将地面有限区域源的解决方案与横向无限区域源和点源的解决方案进行了比较。有限面积源与横向无限面积源的地平面浓度之比高度取决于横向涡流扩散率,但几乎与风速和垂直涡流扩散率幂律中的指数无关。对于有限区域源的地面浓度与点源的地面浓度之比也是如此。

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