-
-
June 26, 2019 at 6:16 pm
julia.hartig
SubscriberI'm struggling to understand the meaning behind the "algebraic" solution to the granular energy equation (i.e. neglecting convection and diffusion in the granular temperature PDE). The terms in the equation from the Fluent theory manual (top of attachment) don't seem to match the algebraic form of the granular temperature equation it references in the MFiX documentation (bottom of attachment). I tried plugging in and rearranging the forms of the collisional dissipation and diffusive granular energy terms from the Fluent manual into the simplified granular PDE, but I still can't come up with the K1m/K2m/etc. coefficients in the MFiX documentation.Â
Even if you could simply point me to the 2005 paper the MFiX documentation refers to, that would be helpful. I've tried a literature search for the derivation of this MFiX algebraic granular temperature and haven't found anything. I've also tried talking to several PhD students and postdocs who've worked with MFiX and they weren't familiar with the algebraic form of granular temperature either. -
June 27, 2019 at 4:42 am
Amine Ben Hadj Ali
Ansys EmployeeNo transport processes is the backbone of algebraic. -
June 27, 2019 at 7:39 pm
julia.hartig
SubscriberI guess I wasn't confused about the concept of algebraic granular temperature, but about how the coefficients from the MFiX documentation relate to the equation from the Fluent theory manual. I finally figured it out - I hadn't realized that you can rearrange and solve the (nonlinear) algebraic granular energy equation using u-substitution and the quadratic formula.
For anyone else who is curious/confused, this is what those MFiX coefficients actually mean:
K1m = coefficient for granular pressure (basically P_s/theta_s). The MFiX documentation ignores the kinetic term of granular pressure and just includes the collisional granular pressure coefficient.
K2m = coefficient for viscous energy generation from velocity divergence "Dmii" (i.e. (lambda_s - 2/3*mu_s)/sqrt(theta_s))
K3m = coefficient for viscous energy generation from velocity gradient "Dmij" (i.e. mu_s/sqrt(theta_s))
K4m = coefficient for collisional dissipation (i.e. gamma_theta/(theta_s)^(3/2))Â
So basically, K1m through K3m come from the "generation of energy by the solids stress tensor" and K4m comes from "the collisional dissipation of energy" in the Fluent theory manual. I wrote out a derivation but it's rather messy, if anyone reading this post wants some more details feel free to let me know and I can post them!
-
- The topic ‘Theory: Rationale behind algebraic granular temperature approach?’ is closed to new replies.
- air flow in and out of computer case
- Varying Bond model parameters to mimic soil particle cohesion/stiction
- Eroded Mass due to Erosion of Soil Particles by Fluids
- Centrifugal Fan Analysis for Determination of Characteristic Curve
- Guidance needed for Conjugate Heat Transfer Analysis for a 3s3p Li-ion Battery
- I am doing a corona simulation. But particles are not spreading.
- Issue to compile a UDF in ANSYS Fluent
- JACOBI Convergence Issue in ANSYS AQWA
- affinity not set
- Resuming SAG Mill Simulation with New Particle Batch in Rocky
-
3912
-
1414
-
1256
-
1118
-
1015
© 2025 Copyright ANSYS, Inc. All rights reserved.