首页> 外文OA文献 >Modelling of multiphase flows on adaptive unstructured meshes with applications to the dynamics of volcanic ash plumes
【2h】

Modelling of multiphase flows on adaptive unstructured meshes with applications to the dynamics of volcanic ash plumes

机译:自适应非结构​​网格上多相流的建模及其在火山灰羽流动力学中的应用

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

摘要

This thesis describes the development of two numerical models for the study of (1) incompressible multiphase flow and (2) compressible multiphase flow. Both models employ a state-of-the-art adaptive unstructured mesh-based approach which allows the mesh, upon which the model equations are discretised, to be optimised in order to focus numerical resolution in areas important to the dynamics and decrease it where it is not needed as a simulation progresses. The implementation of the models takes place within a computational fluid dynamics code called Fluidity.ududThe application of the models concerns the multi-scale simulation of volcanic ash transport in aqueous solutions and in the atmosphere. Simulations of ash settling in a water tank, which mimic published laboratory experiments, are performed primarily in two dimensions. The results demonstrate that ash particles can either settle slowly and individually, or rapidly and collectively as an ash-laden cloud, referred to as a plume. Two quantities used to measure the tendency for plumes to form are then evaluated with a parameter study. Particles settling collectively are slowed by inertial drag, rather than viscous drag, and it is shown that such quantities must account for this. An improvement to the measures is proposed, along with an alternative measure which uses a more accurate expression for the collective settling timescale. Finally, a two-dimensional kilometre-scale volcanic eruption of hot gas and ash into the atmosphere is simulated. The results are compared with those from MFIX, a leading multiphase flow code. Both Fluidity and MFIX are able to successfully capture the key characteristics of an eruption event.ududThe benefits of the adaptive unstructured mesh-based approach are highlighted throughout the thesis by demonstrating that it maintains solution accuracy whilst providing a substantial reduction in computational requirements when compared to the same simulation performed using a fixed mesh of uniform resolution.
机译:本文描述了两个用于研究(1)不可压缩多相流和(2)可压缩多相流的数值模型的发展。两种模型均采用基于自适应非结构​​化网格的最新方法,该模型可优化离散模型方程的网格,以便将数值分辨率集中在对动力学重要的区域上,并在对动力学重要的区域减小随着仿真的进行,不需要。模型的实现在称为“流动性”的计算流体动力学代码中进行。 ud ud模型的应用涉及水溶液和大气中火山灰运移的多尺度模拟。模拟已发布的实验室实验的水箱中灰烬沉降模拟主要在两个方面进行。结果表明,灰烬颗粒既可以缓慢缓慢地沉降,也可以迅速地共同沉积为充满灰烬的云,称为烟羽。然后,通过参数研究评估用于测量羽流形成趋势的两个量。惯性阻力而不是粘性阻力会减慢集体沉降的颗粒的速度,这表明这种量必须考虑到这一点。提出了对措施的改进,以及对集体解决时间表使用更准确表达的替代措施。最后,模拟了热气体和灰分向大气的二维千米级火山喷发。将结果与领先的多相流代码MFIX的结果进行比较。流动性和MFIX都能够成功捕获喷发事件的关键特征。 ud ud在整个论文中强调了自适应非结构​​基于网格的方法的优势,方法是证明它在保持求解精度的同时大大减少了计算需求与使用相同分辨率的固定网格进行的相同模拟进行比较时。

著录项

  • 作者

    Jacobs Christian Thomas;

  • 作者单位
  • 年度 2014
  • 总页数
  • 原文格式 PDF
  • 正文语种
  • 中图分类

相似文献

  • 外文文献
  • 中文文献
  • 专利

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号