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A Laboratory Study on Rheological Properties of Fluid Mud

머드유동층의 유동학적 특성에 관한 실험적 연구

  • Received : 2012.04.30
  • Accepted : 2012.06.08
  • Published : 2012.06.29

Abstract

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.

본 연구에서는 최신의 유동측정기를 이용하여 고령토 및 세 종류의 도자기토 시료에 대해 머드유동층의 유동학적 특성, 즉 밀도에 따른 점성 및 항복응력의 변화특성이 정량적으로 산정되었다. 본 연구에서는 또한 이러한 머드유동층의 물리화학적 기본특성들이 각 시료별로 측정되었으며, 이 기본특성들과 유동학적 특성들 사이의 상관관계가 정성적으로 분석되었다. 본 연구결과에 따르면, 머드유동층은 일반적으로 의가소성 거동특성을 보이며, 그 점성 및 항복응력은 모두 밀도가 증가함에 따라 지수함수적으로 급격히 증가하나, 각 시료별로 이 값들은 정량적으로 큰 차이를 보이는 것으로 나타났다.

Keywords

References

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