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Hello,
im trying to simulate powder flowing through a nozzle carried with a gas.
The particles are small (30µm) and the volume fracion is low.
However its important for me to simulate the interaction, which is why i activated the DEM model, but no particles are injected or tracked.
Can someone tell me what might be the cause of that happening?
Thank you!
Kind regards
Marie
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Are you still working on this problem? I have done a lot of particle tracking (publications, models, examples) and even wrote a book on the subject. I may be able to help.
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Dear all,
I have experience in DEM with Trubal code, and I am wondering mastering PFC 3D to use it in my future research studies (in the area of geotechnical engineering or industrial processes). How should I start? I mean, what are the best resources on PFC 3D?
Thank you in advance,
Ahmad
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When you have installed this software and have the license, you can read the tutorial in the PFC help, which provides some cases from simple to complex models in the simulation. By practicing these cases, you can handle the basic skills and start your simulation using PFC.
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I am using LAMMPS to model additive manufactured material and not clear to me how to choose and validate the potential of this sintered material at that scale. I think transferring to the DEM method.
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Mohamed Adel Please take a look at my PhD dissertation here:
I used LAMMPS to simulate the interactions between Clay materials (both long-range and granular), also explained how we validated our models.
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Which is the best software to perform DEM (discrete element modellin) for debris flow and similar phenomenon.
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Dear M. Wasif Naqvi,
I would recommend PFC3D for debris flow single phase analysis. In order to carry out two phase modelling you have use DEM-CFD.
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How can we model multiphase flow of DEM (discrete element modelling) and SPH (smooth particle hydrodynamics)/ lattice boltzman method using comsol. Also if there is any other good software to perform similar problem
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You can check below mentioned article:
Article A LBM-DEM solver for fast discrete particle simulation of pa...
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Dear All,
I would like to ask you, in Fluent Multi-phase flow (Eulerian), 
How secondary phase block primary phase ?
If my have very high fraction of secondary phase, the primary will be blocked or change the direction or velocity.
Anyone can explain mechanism or physics underlying this situation?
Best Regards,
Yannapol S.
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Hi sir Can u please tell me how to calculate volume fraction boundary condition for secondary phase ( Biomass) for three phase fluidized bed reactor working with air as a primary phase and sand and biomass as secondary phase
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Hello, everyone!
I need a software that could pack the arbitrary shaped particles (random packing).
Particle models are prepared in CAD software (see figure for example). Now I need to fill the column (cylinder) with them.
The software is highly preferrable to be free, maybe even open-source.
I heard about Blender could pack spheres, and how about user-defined particles?
Please, advice.
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Dear Ivan,
You're right. I forgot that YADE only uses spherical particles. Best regards,
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Dear researchers,
I am wondering how to get the grain size distribution of a granular assembly using measure logic. As I read from the manual that we can use measure dump command but it is not working. Could any one provide the support in this regard?
Looking forward to hear form you.
Regards
Shiva
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You need to write a Fish code for this: two dimensional arrays.
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I am simulating cylindrical shapes using DEM. From the literature survey, I got to know two methods, first is to create real cylindrical shape and the second is using multi sphere to approximate the cylinder shape.
I decided to use cylindrical shape. As I see in many papers, the spheres are overlapping, wouldn't this create a problem in mass distribution? How is this problem tackled?
Now say that the body is deformable, then how can I move the individual spheres accordingly?
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Thank you Md.Mahmud Sazzad. I will give a try.
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Rock masses presents structural features that are generated as a response to the stress changes along the geological time. As it has been widely described these structures are one of the main precursors of failure in any kind of rock engineering project. Therefore, these shall be mapped, measured and identified.
It is clear that structural mapping in any project is time consuming, may be hazardous for the person on field and may not provide enough information. Therefore, remote sensing techniques have been proposed in order to obtain greater information in less time without exposing the personal to any kind of risks. This allows us to obtain significant information that we can process and obtain pretty statistical distributions (This information includes orientation, persistence and density of the fractures), that may gives us an insight of how are these fractures distributed along the rock mass.
Additionally, with the development of Discrete Fracture Networks and Discrete Element Software, we can reproduce models that considers jointed rocks masses. However, there is still long ways to go with this technology.
How close do you think that even with large volumes of information a statistical distribution can represent the structure of the rock mass?
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Thank you very much Neil for your response.
I completely agree with you. The engineer/geologist should never stop visiting the site. I also agree and that this remote sensing techniques only provides you half of the information, since mechanical properties also should be measured.
I am working with Discrete Element Models and for me is really interesting to hear what other engineers think about this.
Best regards,
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Linear and Hertz-Mindlin Contact models are the most used models in modelling the granular material. The contact forces between two spheres are calculated based on the equations of motion (Summation of forces=0). However, does these equations account for the inertial forces (F=ma), where F is the inertial force due the acceleration of the sphere (a) with mass=m.
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The question has in my opinion two aspects:
Firstly, the contact forces, regardless of the contact model, will of course simply enter the equation of motion, as it was said in the two previous answers (Note, that the contact models don't "account for inertia", they just give forces as functions of displacements and velocities).
However, there is another problem: the Hertz- or Hertz-Mindlin solution (as basically all contact models) are derived from equilibrium conditions of an infinite elastic medium, i.e. dynamic effects like wave propagation etc. are neglected. Thus, if you incorporate these contact solutions in dynamic simulations, this is only possible in the quasi-static limit, i.e.
i) the contact area (or more precise the deformed volume) must be small compared to the macroscopic bodies (spheres)
ii) all macroscopic velocities must be small compared to the smallest speed of wave propagation in the elastic medium
If both those assumptions are fulfilled, you can use static contact models like the Hertzian solution in dynamic simulations.
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Hello,
I am a graduate student working on Discrete Element Modeling, and I have a simple question on modeling continuous media using DEM. As you may know, packing fraction in 3D DEM was less than 0.74, thus it may contain at least 26% porosity, which was much higher that of the majority of materials. Accordingly, I intend to know what we can do to address this problem ? Using overlapped particles to increase packing fraction works or not ?
Thanks in advance,
Huihuang
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To model 3D continuous media with dicrete element method, several intrinsec characteristics of the granular packing have to be controlled.
1- The coordination number which is the mean number of particles in contact with a given one, is nearly to 6.
2- The area fraction of particles which is the ratio between the area of particles and the total volume domain is nearly to 0.64.
3- Furthermore, an isotropic material is characterized by a homogeneous distribution of contact angles with respect to the orientation.
For more details, see our work: Application of DEM to predict the elastic behavior of particulate composite materials.
In practical, a discrete domain is considrerd with at least 10000 particles. The particles size distribution follows Gaussian distribution.
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I need to measure the dissipated energy and total energy inside measure circles (RVE). PFC already has commands that calculates these energies in the whole system but there is nothing presented for the mentioned problem!!
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Measure the consumed power in the overall power supply circuit (measure I and V and conclude) !
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Hello all,
My master thesis is on soil compaction simulation using DEM and for calibration of the contact model, I use Oedometer test. I simulate the Oedometer test and compare it with experimental values. The material properties of the calibrated oedometer simulation is then used in the soil compaction simulation. In Oedometer test, I use particles of radius 1mm. However, to reduce the computation time in soil compaction simulation, I scale the radius of the particles 10 times the original value(i.e. 1cm). Therefore. I should also scale up the material property values. I would like to know whether there are any relationship between the radius of the particle and the material properties like stiffness, friction coefficient etc. Thanks in advance.
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Hello,
According to User manual of PFC3D (2005), sphere particle stiffness  is related to the radius as follows: 
k=4ER, where k= stiffness, E=Young's modulus, R = mean radius of two contacting particles.
Hope this helps. 
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I am a PhD candidate trying to use DE-LBM for modeling the behavior of a porous media (sandy soil for instance) subjected to fluid flow. I just started to understand the fundamentals of LBM. Is the LBM formulation independent of the coefficient of permeability (k)?
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Hello,
Please read this article : Quantitative analysis of numerical estimates for the permeability of porous media from lattice-Boltzmann simulations by Ariel Narvaez (doi:10.1088/1742-5468/2010/11/P11026)
There's a link between the viscosity and the boundary conditions, which may be reduced when the MRT algorithm is used.
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Hello,
In my work with DEM (Discrete Element Modeling) I am often approximating a shape, for example a rock, with N spheres. The normal work flow is to load in a STL file that contains the shape that I would like to approximate. I then pack the interior of the stl outline with the N spheres. I try to match the general shape but there really is no rhyme or reason in placing a sphere in a certain location with some radius.
I would like to write/use an algorithm that can find the "best" way to pack a given stl file. I have been looking into the sphere packing problem from mathematics and physics but they do no allow overlapping. 
I have been working on a program in matlab that would do this for me. Its process is as follows.
1) Import a STL file and find its bounding box.
2) Create a bounding grid with dimensions (7,7,7) (for example...)
3) Out of these points, find only the ones that are inside the Polygon
4) Pick a random point from step 3 and minimize a function F solving for the radius of the sphere (more on F in a bit)
5) Repeat steps 3 and step 4, 50 times (for example...)
6) Pick the best minimum value from the step 5s 50 values that minimized F
7) Using the x,y,z values that yielded the minimum value from step 6, reduce the grid such that the grid is now centered around the x,y,z values that minimized F the most. 
8) Repeat steps 3 through 7 until a convergence on x,y,z,r is found.
The function F was a little tricky to formulate and I don't know if it yields exactly what I want, but the general Idea is as follows.
I would like to compare the volumes of the sphere with relationship to the volume of the polygon as follows.
F = (V_s not V_p) - (V_s and V_p) + (V_p not V_s) or
F = Vol of s that is not in the polygon minus the Vol of s that is in the polygon plus the volume of the poly that is not in the spheres
My question is a combination of if anyone has ran into a similar problem and in what ways could I improve my algorithm.
Thank you for any and all suggestions!
Please let me know in what ways I can improve my question.
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The following paper may help you.
Cheng-Qing Li,Wen-Jie Xu,Qing-Shan Meng.Multi-sphere approximation of real particles for DEM simulation based on a modified greedy heuristic algorithm. Powder Technology,Volume 286, December 2015, Pages 478–487
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Hi friends,
I'm trying to model a Fixed bed reactor whose particle are cylindrical in shape. I would like to use multisphere DEM approach to create packing. Can any of you suggest me about the best among the open source software: LIGGGHTS,YADE or ESys.
Through the Google I came to know that Multisphere approach of LIGGGHTS is available for commercial users. So I can't afford it
I would like to know whether I can use Multisphere approach in YADE or ESys software.
Any help will be of great appreciation
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Hi,
YADE supports the multi-sphere (clmp) approach. Beside that it also has the possibility to model cylinder-like elements and polyhedra. There are no restrictions as they are in LIGGGHTS, everything is open-source :-)
HTH
Klaus
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In slope analysis, how to take the initial stress into account using DEM ,such as UDEC?
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Initial stresses should be ideally measured in field and applied over the model. In the absence of field measurements, vertical stress at any point should represent the gravity field and horizontal stress should be computed using a suitable K value, which depends on the type of rock./rock mass.
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particle flow code, rock mechanics
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You see "Getting Started" and "Command reference" in manual.
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I am working on the reduction of WOx into W by using an extended discrete element method approach and I need to model the WOx->W reactions in a single particle model. I already have some ideas, but I am constantly brainstorming. Any contributions?
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The chemical vapour transport occurs via gaseous WO2(OH)2, similar to molybdenum oxide reduction (MoO2(OH)2.
Lassner and  Schubert: Tungsten: properties, chemistry, technology of the element, alloys, and chemical compounds, Kluwer Academic/Plenum Publishers (1999)
Schulmeyer et al. Int. Journal of RM&HM 20 (2002) 261-269
Etc.
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I'm gonna model a 3D fractured media using ITASCA discrete element package "3DEC". The aim of the model is obtaining deformability modulus of the rock mass. As you know, there is no direct method to do that. So,... I wonder if anyone could present any helpful numerical or statistical way to obtain the deformability.
Thanks in advance.
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Dear Saleh,
Deformability moduli are the most important parameters in dam engineering and it is why to use jacking or plate loading tests. I recommend you to refer to Amadei & Goodman (1981) and Huang et al (1995). These articles will help you have a broad vision on rock mass deformation. The study I am dealing with, comprises a wide framework in which determination of deformability of the abutments of a dam has been considered.
Wish the best. 
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I am looking for a program to model soil under large deformation and analyze induced excess pore water pressure due to this deformation.
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Depending on your available funds, the best would be PFC. There are still some freeware apps that you may check to see if they fit your needs.
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Hello, 
I am looking for a recommendation to evaluate underground excavations in rock and a defined criteria to select type analysis (FEM or DEM) and perform a stress-strain analysis in tunnel section and pillar.
Thank you!
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It depends on the condition of your rock mass. If there are too make joint sets in rock to be modeled, UDEC/3DEC can be used in which discontinuous medium is represented as an assemblage of discrete blocks while the discontinuities are treated as boundary conditions between blocks. If there are not too many joint sets to be modelled, then FLAC, which is based on Lagrangian analysis can be used effectively. The solution scheme in both these codes is based on finite difference method. Many people have used these codes successfully to simulate excavations in rock mass. One of my papers on this topic:
Sitharam,T.G. and G. Madhavi Latha, G. (2002).Simulation of excavations in jointed rock masses using a practical equivalent continuum approach, International Journal of Rock Mechanics and Mining Sciences, Elsevier, Vol. 39(4), pp. 517-525. DOI: 10.1016/S1365-1609(02)00024-2.
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Hi All,
In qualitative level, I am expert to run model using Discrete Element Method. Recently, I have developed associated and non-associate flow rule based Elastic-viscoplastic (EVP) models under FEM, considering reconstitute as well as natural soft sensitive clay and validated my models using seven clays under conventional triaxial test along with true triaxail tests. I am interested to explore micro mechanical features of soft clays. I have used DEM during my Master's in 2007, but they were in qualitative level rather than quantitative. I have never concentrated to extract DEM parameters through experimental data and wondering, is there any one, who can extend his/her co-operation, how to calibrate DEM parameters from experimental or any guide line to extract them for quantitative research? I found couple of papers, where comparisons of DEM and triaxial compression were presented, but calibration process are still elusive.
Thanks in advance.
Mohammad Nurul Islam
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Hi Jean-Luc Charles,
Thank you very much for your references.
Regards,
Mohammad Nurul Islam 
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I have been reading about semi-supervised techniques and would like to ask if anyone could direct me to any semi-supervised machine learning methods capable of generating probability distribution in a graph-based environment for discrete data? E.g. a Bayesian network like for semi-supervised category.
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You can also try a semi-supervised graph-label propagation algorithm called Modified Adsorption.
Reference: New Regularized Algorithms for Transductive Learning [ Slides ] [ Video ]
Partha Pratim Talukdar, Koby Crammer, ECML 2009, 
Here is a link to the Junto package that implements this algorithm: http://code.google.com/p/junto/
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modeling of separation of grains from other unwanted parts in combine harvester
please introduce me  an easy DEM software 
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With regard to DEM simulation software there are some commercial products such as EDEM (from DEM Solutions Ltd. - http://www.dem-solutions.com) or PFC (2D & 3D) (from Itasca - http://www.itascacg.com/software/pfc). On the other hand there are some popular open source and non-commercial products such as Yade (Yet Another Dynamic Engine - https://yade-dem.org), LIGGGHTS (http://www.cfdem.com/liggghts-open-source-discrete-element-method-particle-simulation-code) and other.
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I'm trying to model events happening at certain time intervals in function of the total time. For instance if a doctor visited patients every 12 hours, it would be intuitive to assume that a group of patients with a mean length of stay (LoS) of 12 hours have an average of 1.0 follow-up visit (and so forth, 1.5 visits for 18 hours etc.). In reality, the actual mean number of visits is consistently smaller because all patients below 10 hours (which would be approx. half of them for a normal distribution) receive 0 visits. Is there a "formal" method to estimate the number of visits from the LoS?
I have been suggested to round down the number of visits as an approximation but I'm not sure that would be academically acceptable... I hope this makes sense as I'm not a statistician. Thanks in advance!
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Queueing theory is a good place to start. You can also try using a Poisson Regression. You can create a response variable, say patients per hour/12hrs. On top of that, you can use Doctor and Day of the week as predictor variables, among others. 
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To approximate numerically the solution U we consider the Galerkin space discretization and time discretizations based on the Crank-Nicolson method and on the fourth-order Padé approximation R2,2.
What are the steps required to compute the approximate solution Un+1 at the time level tn+1 using both these discretization schemes?
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Hi Ghaffar! Once you have descritized and your numerical scheme is obtained. I suppose you have a two level scheme. Taking initial condition as Un , compute your rhs. Apply boundary conditions to obtain a system of equations whose size depends on the points taken along space direction. This system will be linear if given PDE is linear else it is non-linear. Solve it to obtain solution Un+1.
Now Un+1 is obtained , transfer it to Un and get solution at new time step 2Dt as explained above.