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Numerical simulation of flow and melting characteristics of seawater-ice crystals two-phase flow in inlet straight pipe of shell and tube heat exchanger of polar ship

机译:极地舰船壳管式换热器进口直管内海水冰晶两相流动与熔融特性的数值模拟

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The ice crystal particles are easy to enter into the seawater cooling system of polar ship together with seawater when it sails in the Arctic. They are easy to accumulate in the pipeline, causing serious blockage of the cooling pipe. In this study, the flow and melting characteristics of ice particles-seawater two-phase flow in inlet straight pipe of shell-and-tube heat exchanger were numerically simulated by using Eulerian-Eulerian two-fluid model coupled with the interphase heat and mass transfer model. The influences of inlet ice packing factor, ice crystal particle diameter, and inlet velocity on the distribution and melting characteristics of ice crystals were investigated. The degree of asymmetry of the distribution of ice crystals in the cross section decreases gradually when the IPF changes from 5 to 15%. The volume fractions of ice crystals near the top of the outlet cross section are 19.59, 19.51, and 22.24% respectively for ice packing factor of 5, 10 and 15%. When the particle diameter is 0.5mm, the ice crystals are gradually stratified during the flow process. With particle diameters of 1.0 and 2.0mm, the region with the highest volume fraction of ice crystals is a small circle and the contours in the cloud map are compact. The greater the inlet flow velocity, the less stratified the ice crystals and the more obvious the turbulence on the outlet cross section. The average volume fraction of ice crystals along the flow direction is firstly rapidly reduced and then stabilized after 300mm.
机译:当冰晶在北极航行时,它们很容易与海水一起进入极地船的海水冷却系统。它们很容易在管道中积聚,从而导致冷却管严重堵塞。本研究利用管式换热器的欧拉-欧拉二流体模型,结合相间传热传质,对管壳式换热器进口直管中冰粒-海水两相流的流动和融化特性进行了数值模拟。模型。研究了入口冰的堆积因子,冰晶粒径和入口速度对冰晶的分布和融化特性的影响。当IPF从5%变为15%时,横截面中冰晶分布的不对称度逐渐降低。对于冰堆积因子为5、10和15%的情况,出口横截面顶部附近的冰晶的体积分数分别为19.59%,19.51和22.24%。当粒径为0.5mm时,冰晶在流动过程中逐渐分层。粒径为1.0和2.0mm时,冰晶体积分数最高的区域是一个小圆圈,并且云图中的轮廓很紧凑。入口流速越大,冰晶分层越少,出口横截面上的湍流越明显。冰晶沿流动方向的平均体积分数首先迅速降低,然后在300mm之后稳定下来。

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