Carrera Lucie, Springer Fanny, Lipeme-Kouyi Gislain, Buffiere Pierre
Univ. Lyon, INSA-Lyon, Laboratory of Waste, Water, Environment, Pollution, 9 rue de la physique, F-69621 Villeurbanne Cedex, France E-mail:
Water Sci Technol. 2017 Apr;75(7-8):1899-1908. doi: 10.2166/wst.2017.070.
HS emission dynamics in sewers are conditioned by the mass transfer coefficient at the interface. This work aims at measuring the variation of the mass transfer coefficient with the hydraulic characteristics, with the objective of estimating HS emission in gravity pipes, and collecting data to establish models independent of the system geometry. The ratio between the HS and O mass transfer coefficient was assessed in an 8 L mixed reactor under different experimental conditions. Then, oxygen mass transfer measurements were performed in a 10 m long gravity pipe. The following ranges of experimental conditions were investigated: velocity flow [0-0.61 m.s], Reynolds number [0-23,333]. The hydrodynamic parameters at the liquid/gas interface were calculated by computational fluid dynamics (CFD). In the laboratory-scale reactor, the O mass transfer coefficient was found to depend on the stirring rate (rph) as follows: K = 0.016 + 0.025 N. A K/K ratio of 0.64 ± 0.24 was found, in accordance with previously published data. CFD results helped in refining this correlation: the mass transfer coefficient depends on the local interface velocity u (m.h): K = 0.016 + 1.02 × 10 u In the gravity pipe device, K also exponentially increased with the mean flow velocity. These trends were found to be consistent with the increasing level of turbulence.
下水道中硫化氢(HS)的排放动态受界面传质系数的制约。这项工作旨在测量传质系数随水力特性的变化,目的是估算重力管道中的HS排放量,并收集数据以建立独立于系统几何形状的模型。在一个8升的混合反应器中,在不同实验条件下评估了HS与氧气传质系数的比值。然后,在一根10米长的重力管道中进行了氧气传质测量。研究了以下实验条件范围:流速[0 - 0.61米/秒],雷诺数[0 - 23,333]。通过计算流体动力学(CFD)计算了液/气界面处的流体动力学参数。在实验室规模的反应器中,发现氧气传质系数取决于搅拌速率(转/小时),如下所示:K = 0.016 + 0.025N。发现K/K比值为0.64 ± 0.24,与先前发表的数据一致。CFD结果有助于完善这种相关性:传质系数取决于局部界面速度u(米/小时):K = 0.016 + 1.02 × 10u。在重力管道装置中,K也随平均流速呈指数增加。发现这些趋势与湍流程度的增加一致。