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A HEAD LOSS MODEL FOR SLURRY TRANSPORT BASED ON ENERGY CONSIDERATIONS

机译:基于能量考虑的泥浆运输头部损失模型

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In the last decades many head loss models for slurry transport have been developed. Not just for the dredging industry but also for coal and phosphate transport and in the chemical industries. Some models are based on the phenomena occurring combined with dimensionless parameters, resulting in semi-empirical equations (Durand, Condolios, Gibert, Worster, Jufin Lopatin, Zandi & Govatos, Fuhrboter), while others are based on physics with 2 and 3 layer models (Newitt, Doron, Wilson, Matousek). The physical models are based on stationary transport in time and space, while the semi-empirical models may incorporate non-stationary processes. An analysis of these models and of data collected from numerous publications for particles with densities ranging from 1.24 ton/m~3 to 3.65 ton/m~3, diameters ranging from 0.08 mm up to 22.5 mm, concentrations up to 45% and pipe diameters from 0.0254 m up to 0.9 m has led to an overall model of head losses in slurry transport. The model is based on a set of characteristic velocities determining the source of energy losses. One can distinguish viscous friction losses, dry friction losses, potential energy losses, kinetic energy losses, Magnus lift work, turbulent lift work and turbulent eddy work. The losses do not have to occur at the same time. Usually one or two will be dominant depending on the flow regime. Most well-known head loss equations for heterogeneous transport, Durand & Condolios (1952), Fuhrboter (1961), Newitt et al. (1955), Jufin & Lopatin (1966) and Wilson et al. (1992) are based on a single excess pressure term. This term is based on curve fitting, some physics or dimensionless numbers. The main question is, can the excess pressure accurately be described by just one term and if so, does this term depend on the hydraulic resistance of the carrier fluid or is it independent. The model as derived here is based on the assumption that the excess pressure is the result of energy losses. These energy losses are identified as potential energy losses and kinetic energy losses. One could distinguish more types of energy losses and maybe come with a more accurate equation, but the current approach already gives a good correlation with the data of many researchers. The potential energy losses are dominated by the terminal settling velocity of the particles, including hindered settling. The kinetic energy losses are dominated by the ratio between the slip velocity of the particles and the terminal settling velocity of the particles (without hindered settling). The slip velocity cannot be derived fundamentally (yet), but is approximated by a function with the dimension of velocity. The final result is an equation with 3 independent terms. The viscous friction losses according to Darcy Weisbach, using the Moody diagram for the friction coefficient, the potential energy losses, using an approach similar to Newitt et al. (1955) and the kinetic energy losses as has been derived here. The paper describes the overall model and a verification of the different regimes is given based on data from the literature. The overall model correlates very well with the data measured.
机译:在最近的几十年中,已经开发了许多用于泥浆输送的水头损失模型。不仅用于疏industry行业,而且还用于煤炭和磷酸盐运输以及化学行业。一些模型基于与无量纲参数结合发生的现象,从而产生半经验方程(Durand,Condlios,Gibert,Worster,Jufin Lopatin,Zandi&Govatos,Fuhrboter),而其他模型则基于具有2层和3层模型的物理学(纽威特,多伦,威尔逊,马图切克)。物理模型基于时间和空间上的平稳传输,而半经验模型可能包含非平稳过程。分析这些模型以及从众多出版物中收集的有关密度范围从1.24 ton / m〜3到3.65 ton / m〜3,直径范围从0.08 mm到22.5 mm,浓度到45%以及管道直径的颗粒的数据从0.0254 m到0.9 m形成了泥浆运输中压头损失的整体模型。该模型基于确定能量损失来源的一组特征速度。可以区分粘性摩擦损失,干摩擦损失,势能损失,动能损失,马格努斯升力功,湍流升力功和湍流涡流功。损失不必同时发生。通常情况下,一到两个将取决于流动状态。最著名的非均质输运水头损失方程,Durand&Condolios(1952),Fuhrboter(1961),Newitt等。 (1955),Jufin&Lopatin(1966)和Wilson等。 (1992)是基于一个单一的过压项。该术语基于曲线拟合,一些物理量或无量纲数。主要问题是,可以仅用一个术语来准确地描述过压,如果这样,该术语是否取决于载液的水力阻力,或者它是独立的。此处得出的模型基于以下假设:过高的压力是能量损失的结果。这些能量损失被标识为潜在能量损失和动能损失。人们可以区分出更多类型的能量损失,也许可以得出一个更精确的方程,但是当前的方法已经与许多研究人员的数据提供了很好的相关性。潜在的能量损失由颗粒的最终沉降速度(包括阻碍沉降)决定。动能损失由颗粒的滑移速度和颗粒的最终沉降速度(无沉降)之间的比率决定。滑移速度尚不能从根本上推导出,但可以通过一个具有速度维数的函数来近似。最终结果是一个包含3个独立项的方程。根据达西·魏斯巴赫(Darcy Weisbach)的观点,粘滞摩擦损失采用穆迪图作为摩擦系数,势能损失采用类似于Newitt等人的方法。 (1955年)和动能损失已推导到这里。本文描述了整体模型,并根据文献数据对不同的方案进行了验证。总体模型与测得的数据非常相关。

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