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Simulation of turbulent mixing effects on chemical reactions in the convective boundary layer.

机译:模拟湍流混合对流边界层中的化学反应。

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The goal of this research is to quantitatively account for incomplete mixing of interacting chemical species when one species is emitted from ground level and the other species is mixed downward into the top of the daytime atmospheric boundary layer. Top-down and bottom-up (TDBU) diffusion of two species in an inhomogeneous convective boundary layer (CBL) are simulated by means of 1-D vertical turbulent chemical kinetics model (TKM). The concentration field splitting method (CSM) with a phenomenal extent of reaction and asymmetric convective model (ACM) schemes are implemented. Because of the lack of suitable experimental data, results of the TKM are compared with a box model (BM), with those of the conventional linear chemical kinetics model (LKM) ignored incomplete mixing of reaching species, and with those of a conventional turbulent kinetics model (CTKM) based on the CSM with a conventional extent of reaction.; The TKM simulations were performed to study the effects of convective turbulent mixing on chemical reaction rates in vertically asymmetric turbulence of the CBL. Important findings from those simulations include the following: (1) The results in the TKM prove that the effects of incomplete mixing (segregation of species) on the chemical reaction rates are not important in predicting in the mean concentrations of species in any realistic photochemical system in the convective boundary layer. (2) The TKM and the CTKM simulations provide almost the same results of species concentrations and segregations, under both equilibrium and non-equilibrium conditions, even though the chemical reactions and the dispersion effects are coupled and evolve simultaneously in space and time. (3) The CSM scheme works well with both the conventional extent of reaction and the phenomenal extent of reaction if the complex chemistry is used, the overall reaction rates are determined in the CBL, and the species fluxes from the boundary layers are not opposite. (4) In the TKM, the segregation effects and the concentrations are very sensitive to chemical characteristics (initial concentration and reaction rate constants) but less sensitive to the physical characteristics (deposition flux, exchange flux, turbulent timescales) and numerical resolution. They are also very sensitive to emission fluxes. (5) The segregation effects are most sensitive to the reaction rate constants, while all concentrations varied sensitively with the parameters groups at the surface except the sensitivity of ozone concentration is small in all cases tested.
机译:这项研究的目的是定量地解释当一种化学物质从地表发射出来而另一种化学物质向下混合到白天大气边界层的顶部时,相互作用的化学物质不完全混合的情况。通过一维垂直湍流化学动力学模型(TKM)模拟了非均匀对流边界层(CBL)中两种物质的自顶向下和自底向上(TDBU)扩散。实现了具有显着反应程度的浓度场分裂方法(CSM)和非对称对流模型(ACM)方案。由于缺乏合适的实验数据,将TKM的结果与盒模型(BM),常规线性化学动力学模型(LKM)的结果进行了比较,而忽略了到达物种的不完全混合,以及常规湍流动力学的结果。基于CSM的具有常规反应程度的模型(CTKM)。进行了TKM模拟,以研究CBL垂直非对称湍流中对流湍流混合对化学反应速率的影响。这些模拟的重要发现包括:(1)TKM中的结果证明,不完全混合(物质的分离)对化学反应速率的影响对于预测任何实际光化学系统中物质的平均浓度并不重要。在对流边界层。 (2)TKM和CTKM模拟在平衡和非平衡条件下提供了几乎相同的物种浓度和偏析结果,即使化学反应和分散效应在空间和时间上耦合并同时演化。 (3)如果使用复杂的化学反应,CSM方案既适用于常规反应程度,也适用于反应的显着程度,总反应速率由CBL确定,并且边界层的物质通量并不相反。 (4)在TKM中,偏析效应和浓度对化学特性(初始浓度和反应速率常数)非常敏感,而对物理特性(沉积通量,交换通量,湍流时间尺度)和数值分辨率则不太敏感。它们对发射通量也非常敏感。 (5)偏析作用对反应速率常数最敏感,而所有浓度都随表面参数组的变化而敏感变化,但在所有测试情况下,臭氧浓度的敏感性均很小。

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