Main.Research History
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Electrical Activity in Myocardial Tissue
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Polar Sea Ice
Electrical Activity in Myocardial Tissue
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Sedimentation in Stratified Fluids
Polar Sea Ice
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Sedimentation in Stratified Fluids
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Sedimentation in Stratified Fluids
Sedimentation in Stratified Fluids
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Electrical Activity in Myocardial Tissue
Electrical Activity in Myocardial Tissue
Polar Sea Ice http://www.math.utah.edu/~lin/images/AntarcticCover.jpg
http://www.math.utah.edu/~lin/images/AntarcticCover.jpg Polar Sea Ice
http://www.math.utah.edu/~lin/images/AntarcticCover.jpg Polar Sea Ice
Polar Sea Ice http://www.math.utah.edu/~lin/images/AntarcticCover.jpg
http://www.math.utah.edu/~lin/images/AntarcticCover.jpg
http://www.math.utah.edu/~lin/images/AntarcticCover.jpg
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http://www.math.utah.edu/~lin/images/AntarcticCover.JPG
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http://www.math.utah.edu/~lin/images/AntarcticCover.JPG
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Sedimentation in Stratified Fluids
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Sphere falling through stratified fluid at low Reynolds number
Advisors: Roberto Camassa and Richard M. McLaughlin
Laboratory Assistants: Claudia Falcon, Anna Miller, and Nicholas Mykins
Description of the problem
Consider a solid body moving at low Reynolds number through a sharp, stable stratification of miscible fluids. We study the hydrodynamics of the forces in the system, including the fluid flow and the resultant behavior of the sphere.
As the sphere passes through the interface, the importance of the entrained fluid is due to its buoyancy in the lower, denser fluid. We find that the sphere will slow down dramatically as it passes through the density transition. We develop a model from first principles of the highly coupled system to capture this effect.
Results
Our model, with no adjustable parameters, can predict the velocity field of the fluid, and thus the shape of the interface between the stratified fluids. The velocity profile, which shows this non-monotonic transition between terminal velocities of the upper layer and lower layer, can also be compared with the experimental data.
http://www.math.utah.edu/~lin/images/FluidFlow.jpg
http://www.math.utah.edu/~lin/images/plastic2.jpg
For more information
Camassa, R., Falcon, C., Lin, J., McLaughlin, R. M. & Parker, R., Prolonged residence times for particles settling through stratified miscible fluids in the Stokes regime, Phys. Fluids 21(2009), 031702-1–4.
American Physical Society Virtual Press Room
Falling sphere experiments
Marine Science and Applied Math Fluids Lab
Work is supported by NSF RTG DMS-0502266
Electrical Activity in Myocardial Tissue
Polar Sea Ice
Sedimentation in Stratified Fluids
As the sphere passes through the interface, the importance of the entrained fluid is due to its buoyancy in the lower, denser fluid. We find that the sphere will slow down dramatically as it passes through the density transition. We develop a model from first principles of the highly coupled system to capture this effect.
As the sphere passes through the interface, the importance of the entrained fluid is due to its buoyancy in the lower, denser fluid. We find that the sphere will slow down dramatically as it passes through the density transition. We develop a model from first principles of the highly coupled system to capture this effect.
Marine Science and Applied Math Fluids Lab
Marine Science and Applied Math Fluids Lab
Marine Science and Applied Math Fluids Lab
Claudia Falcon and Nicholas Mykins
Claudia Falcon, Anna Miller, and Nicholas Mykins
Camassa, R., Falcon, C., Lin, J., McLaughlin, R. M. & Parker, R., Prolonged residence times for particles settling through stratified miscible fluids in the Stokes regime, Phys. Fluids 21(2009), 031702-1–4. American Physical Society Virtual Press Room
Camassa, R., Falcon, C., Lin, J., McLaughlin, R. M. & Parker, R., Prolonged residence times for particles settling through stratified miscible fluids in the Stokes regime, Phys. Fluids 21(2009), 031702-1–4.
American Physical Society Virtual Press Room\\
For more information
Camassa, R., Falcon, C., Lin, J., McLaughlin, R. M. & Parker, R., Prolonged residence times for particles settling through stratified miscible fluids in the Stokes regime, Phys. Fluids 21(2009), 031702-1–4.
American Physical Society Virtual Press Room
Falling sphere experiments\\
http://www.unc.edu/~jtlin/images/Header2.jpg
http://www.unc.edu/~jtlin/images/Body.jpg
http://www.math.utah.edu/~lin/images/Header2.jpg
http://www.math.utah.edu/~lin/images/Body.jpg
http://www.unc.edu/~jtlin/images/FluidFlow.jpg http://www.unc.edu/~jtlin/images/plastic2.jpg
http://www.math.utah.edu/~lin/images/FluidFlow.jpg http://www.math.utah.edu/~lin/images/plastic2.jpg
Our model, with no adjustable parameters, can predict the velocity field of the fluid, as well as the shape of the interface between the stratified fluids. The velocity profile, which shows this non-monotonic transition between terminal velocities of the upper layer and lower layer, can also be compared with the experimental data.
Our model, with no adjustable parameters, can predict the velocity field of the fluid, and thus the shape of the interface between the stratified fluids. The velocity profile, which shows this non-monotonic transition between terminal velocities of the upper layer and lower layer, can also be compared with the experimental data.
As the sphere passes through the interface, the importance of the entrained fluid is enhanced by the buoyancy. We find that the sphere will slow down dramatically as it passes through the density transition. We develop a model from first principles of the highly coupled system to capture this effect.
As the sphere passes through the interface, the importance of the entrained fluid is due to its buoyancy in the lower, denser fluid. We find that the sphere will slow down dramatically as it passes through the density transition. We develop a model from first principles of the highly coupled system to capture this effect.
Solid body moving at low Reynolds number through a sharp, stable stratification of miscible fluids. We study the hydrodynamics of the forces in the system, including the fluid flow and the resultant behavior of the sphere.
Consider a solid body moving at low Reynolds number through a sharp, stable stratification of miscible fluids. We study the hydrodynamics of the forces in the system, including the fluid flow and the resultant behavior of the sphere.
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http://www.unc.edu/~jtlin/images/plastic2.jpg
http://www.unc.edu/~jtlin/images/plastic2.jpg
Work is supported by NSF RTG DMS-0502266
http://www.unc.edu/~jtlin/images/Header2.jpg
http://www.unc.edu/~jtlin/images/Body.jpg
Sphere falling through stratified fluid at low Reynolds number
Advisors: Roberto Camassa and Richard M. McLaughlin
Laboratory Assistants: Claudia Falcon and Nicholas Mykins
Description of the problem
Solid body moving at low Reynolds number through a sharp, stable stratification of miscible fluids. We study the hydrodynamics of the forces in the system, including the fluid flow and the resultant behavior of the sphere.
As the sphere passes through the interface, the importance of the entrained fluid is enhanced by the buoyancy. We find that the sphere will slow down dramatically as it passes through the density transition. We develop a model from first principles of the highly coupled system to capture this effect.
Results
Our model, with no adjustable parameters, can predict the velocity field of the fluid, as well as the shape of the interface between the stratified fluids. The velocity profile, which shows this non-monotonic transition between terminal velocities of the upper layer and lower layer, can also be compared with the experimental data.
http://www.unc.edu/~jtlin/images/FluidFlow.jpg
http://www.unc.edu/~jtlin/images/plastic2.jpg