• Title/Summary/Keyword: 머드유동층

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Estimation of Entrainment Rate of Fluid Mud using Annular Flume (환형수조를 이용한 머드유동층의 연행부상률 산정)

  • Kim, Dong-Ho;Kim, Won-Kyu;Hwang, Kyu-Nam
    • Journal of Korean Society of Coastal and Ocean Engineers
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    • v.28 no.5
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    • pp.257-264
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    • 2016
  • In this study, experiments for measurements of entrainment rate of fluid mud were carried out using annular flume domestically for the first time. Six entrainment tests using kaolinite sediments were conducted with different initial concentrations of fluid mud. It is shown that sediment settling counteracts the otherwise buoyancy dependent entrainment of fluid mud, and that the settling effect leads to a measurably decreased entrainment rate at higher Richardson numbers in comparison with entrainment of salt water, due to additional dissipation of turbulent kinetic energy in the interfacial layer. Through the comparison with previous other studies, the overall performance of the annular flume, the experimental procedure and the test results in simulating the entrainment of fluid mud are shown to be good enough to verify.

A Laboratory Study on Rheological Properties of Fluid Mud (머드유동층의 유동학적 특성에 관한 실험적 연구)

  • Nguyen, Dinh Phuc;Jung, Eui-Taek;Park, Kun-Chul;Hwang, Kyu-Nam
    • Journal of Korean Society of Coastal and Ocean Engineers
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    • v.24 no.3
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    • pp.203-209
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    • 2012
  • In this study, rheological properties of kaolinite and three different porcelain fluid muds are quantitatively estimated with the latest rheometer, in which variations of their viscosities and yield stresses with their densities are estimated. This study also involves the measurements for the basic physico-chemical properties of fluid muds and the qualitative analysis of their correlation between physico-chemical and rheological properties. Experimental results of rheological tests show that fluid muds in general belong to Pseudo-plastic fluids and both viscosities and yield stresses of them increase exponentially with the increase of density while they are remarkably different in quantity depending on sediments.