Frictional Head Loss of Various Bimodal Settling Slurry Flows in Pipe

V. Matoušek, R. Visintainer, J. Furlan, A. Sellgren
{"title":"Frictional Head Loss of Various Bimodal Settling Slurry Flows in Pipe","authors":"V. Matoušek, R. Visintainer, J. Furlan, A. Sellgren","doi":"10.1115/ajkfluids2019-5395","DOIUrl":null,"url":null,"abstract":"\n Pipe flows of bimodal settling slurries exhibit frictional head losses quite different from those determined simply as a sum of loss contributions by the individual fractions. Mechanisms governing flow friction and resulting from an interaction of grains of different fractions in transported slurry are not well understood. This makes a prediction of the frictional head loss in flows of bimodal slurries with Newtonian carrier uncertain. An extensive experimental campaign was conducted in GIW Hydraulic Laboratory in 2016 with slurries of four narrow graded fractions of the virtually same grain densities and very different grain sizes (carrier-liquid fraction, pseudo-homogeneous-, heterogeneous-, and stratified fractions). Besides testing of the individual fractions, different combinations of the fraction mixtures (bimodal, three- and four-component) were tested as well.\n In our previous work published in 2018, we employed experimental results for bimodal slurry composed of coarse granite rock (the stratified fraction) and fine sand (the pseudo-homogeneous fraction) to analyze the observed considerable reduction of the frictional head loss caused by an addition of the fine sand to the granite rock slurry.\n In this work, we extend our analysis to the other bimodal slurries composed of permutations of the four fractions (in total 3 additional bimodal slurries) with a major objective to identify possible mechanisms leading to a modification of the frictional head loss due to an addition of a finer fraction to a coarser mono-disperse slurry, and to quantify this effect for the purposes of a predictive four-component model (4CM). The investigation shows that the frictional loss of bimodal slurry is always smaller than the theoretical loss obtained as the sum of losses of the fractions, although the massive reduction observed in the slurry composed of the stratified rock and fine sand is not observed in any other bimodal slurry. The investigation also suggests that the friction effect obtained by the finer fraction addition is due to different mechanisms for different bimodal slurries although all mechanisms are associated with altering mechanical friction due to granular contacts.\n It is shown that the observed effects can be well reproduced by the friction loss model 4CM, calibrated by the experimental data set from the 203-mm pipe and validated by the data set from the 103-mm pipe.","PeriodicalId":322380,"journal":{"name":"Volume 5: Multiphase Flow","volume":"4 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2019-07-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Volume 5: Multiphase Flow","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1115/ajkfluids2019-5395","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1

Abstract

Pipe flows of bimodal settling slurries exhibit frictional head losses quite different from those determined simply as a sum of loss contributions by the individual fractions. Mechanisms governing flow friction and resulting from an interaction of grains of different fractions in transported slurry are not well understood. This makes a prediction of the frictional head loss in flows of bimodal slurries with Newtonian carrier uncertain. An extensive experimental campaign was conducted in GIW Hydraulic Laboratory in 2016 with slurries of four narrow graded fractions of the virtually same grain densities and very different grain sizes (carrier-liquid fraction, pseudo-homogeneous-, heterogeneous-, and stratified fractions). Besides testing of the individual fractions, different combinations of the fraction mixtures (bimodal, three- and four-component) were tested as well. In our previous work published in 2018, we employed experimental results for bimodal slurry composed of coarse granite rock (the stratified fraction) and fine sand (the pseudo-homogeneous fraction) to analyze the observed considerable reduction of the frictional head loss caused by an addition of the fine sand to the granite rock slurry. In this work, we extend our analysis to the other bimodal slurries composed of permutations of the four fractions (in total 3 additional bimodal slurries) with a major objective to identify possible mechanisms leading to a modification of the frictional head loss due to an addition of a finer fraction to a coarser mono-disperse slurry, and to quantify this effect for the purposes of a predictive four-component model (4CM). The investigation shows that the frictional loss of bimodal slurry is always smaller than the theoretical loss obtained as the sum of losses of the fractions, although the massive reduction observed in the slurry composed of the stratified rock and fine sand is not observed in any other bimodal slurry. The investigation also suggests that the friction effect obtained by the finer fraction addition is due to different mechanisms for different bimodal slurries although all mechanisms are associated with altering mechanical friction due to granular contacts. It is shown that the observed effects can be well reproduced by the friction loss model 4CM, calibrated by the experimental data set from the 203-mm pipe and validated by the data set from the 103-mm pipe.
查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
管道内各种双峰沉降浆流的摩擦水头损失
双峰沉降浆料的管道流动表现出的摩擦水头损失与那些简单地作为单个分数损失贡献的总和而确定的摩擦水头损失大不相同。控制流动摩擦的机制以及由输送浆中不同组分颗粒的相互作用所引起的流动摩擦尚未得到很好的理解。这使得具有牛顿载流子的双峰浆体流动中摩擦水头损失的预测具有不确定性。2016年,在GIW水力实验室进行了一项广泛的实验,使用了四种颗粒密度几乎相同但颗粒尺寸差异很大的窄级配泥浆(载液馏分、伪均质馏分、非均质馏分和分层馏分)。除了测试单个馏分外,还测试了馏分混合物的不同组合(双峰、三组分和四组分)。在我们之前发表于2018年的工作中,我们使用了由粗花岗岩(分层分数)和细砂(伪均匀分数)组成的双峰浆的实验结果,分析了在花岗岩浆中添加细砂所观察到的摩擦水头损失的显著降低。在这项工作中,我们将分析扩展到由四个馏分排列组成的其他双峰浆料(总共3个额外的双峰浆料),主要目的是确定由于在较粗的单分散浆料中添加更细的馏分而导致摩擦水头损失改变的可能机制,并量化这种影响,以用于预测四组分模型(4CM)。研究表明,尽管在层状岩石和细砂组成的双峰浆体中观察到的大量减少在任何其他双峰浆体中都没有观察到,但双峰浆体的摩擦损失始终小于各组分损失之和的理论损失。研究还表明,尽管所有的机制都与颗粒接触引起的机械摩擦的改变有关,但对于不同的双峰浆,添加更细的分数所获得的摩擦效果是由于不同的机制造成的。结果表明,用摩擦损失模型4CM可以很好地再现所观察到的效果,该模型用203-mm管道的实验数据集进行了校准,并用103-mm管道的实验数据集进行了验证。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 去求助
来源期刊
自引率
0.00%
发文量
0
期刊最新文献
A Transient Approach for Estimating Concentration of Water Droplets in Oil and Corrosion Assessment in the Oil and Gas Industry Effect of Interstage Injection on Compressor Flow Characteristic Air Entrainment and Bubble Generation by a Hydrofoil in a Turbulent Channel Flow Experimental Study of Bubble-Droplet Interactions in Improved Primary Oil Separation Effects of Liquid Viscosity on Laser-Induced Shock Dynamics
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1