MC5 


Rheology of Soil, Mud and Construction Materials


Understanding the rheology of kaolinite clay suspensions using Bayesian inference


October 10, 2022 (Monday) 11:10


Track 7 / Ontario

(Click on name to view author profile)

  1. Ran, Ranjiangshang (University of Pennsylvania, Department of Mechanical Engineering and Applied Mechanics)
  2. Pradeep, Shravan (University of Pennsylvania, Earth and Environmental Sciences)
  3. Kosgodagan Acharige, Sebastien (University of Pennsylvania, Department of Earth and Environmental Science)
  4. Blackwell, Brendan (University of Pennsylvania, Department of Mechanical Engineering and Applied Mechanics)
  5. Christoph, Kammer (University of Pennsylvania, Department of Mechanical Engineering and Applied Mechanics)
  6. Jerolmack, Doug J. (University of Pennsylvania)
  7. Arratia, Paulo E. (University of Pennsylvania, Mechanical Engineering & Applied Mechanics)

(in printed abstract book)
Ranjiangshang Ran1, Shravan Pradeep2, Sebastien Kosgodagan Acharige2, Brendan Blackwell1, Kammer Christoph1, Doug J. Jerolmack2 and Paulo E. Arratia1
1Department of Mechanical Engineering and Applied Mechanics, University of Pennsylvania, Philadelphia, PA 19104; 2Department of Earth and Environmental Science, University of Pennsylvania, Philadelphia, PA 19104


Pradeep, Shravan


colloids; mud rheology; suspensions


Mud, a mixture of fine-grained particles (sand, silt, and clay) in water, exhibits complex rheology that is crucial for both natural (mudslide, soil erosion etc.) and industrial processes (civil construction, oil drilling etc.). The rheology of mud is dominated by the attractive nature of clay minerals, since these charged plated-shaped constituents tend to aggregate and form gel-like structures, leading to distinct rheological features from hard-sphere suspensions.. Here, we experimentally examine the flow behavior of kaolinite clay suspensions using steady shear rheology; the flow curves exhibit both yield stress and rheological hysteresis behaviors for various kaolinite volume fractions. A structure-dependent viscoelastic model using Markov Chain Monte Carlo (MCMC) fit, a Bayesian inference method, is employed to explain the observed rheological behavior. The comparison of inherent relaxation timescales suggests that kaolinite clay suspensions are strongly viscoelastic and weakly thixotropic at relatively low volume fractions, while being almost fully thixotropic, or inelastic. At high volume fractions. Our results provide insights for developing powerful predictive models of natural materials, like mud and clay, and can be extended to other known structured fluids.