1# Applications and Publications 2 3PETSc has been used for modeling in all of these areas: Acoustics, Aerodynamics, Air 4Pollution, Arterial Flow, Bone Fractures, Brain Surgery, Cancer Surgery, Cancer Treatment, 5Carbon Sequestration, Cardiology, Cells, CFD, Combustion, Concrete, Corrosion, Data 6Mining, Dentistry, Earth Quakes, Economics, Esophagus, Fission, Fusion, Glaciers, Ground 7Water Flow, Linguistics, Mantel Convection, Magnetic Films, Material Science, Medical 8Imaging, Ocean Dynamics, Oil Recover, PageRank, Polymer Injection Molding, Polymeric 9Membranes, Quantum computing, Seismology, Semiconductors, Rockets, Relativity, Surface 10Water Flow. 11 12## Images 13 14These are images and movies from application simulations developed by PETSc users. 15 16- [COOLFluiD Simulation Environment](https://github.com/andrealani/COOLFluiD/wiki/Gallery-of-applications) 17 18- [Defmod - Parallel multiphysics finite element code for modeling crustal deformation 19 during the earthquake/rifting cycle](https://bitbucket.org/stali/defmod/wiki/Gallery) 20 21- Pilhwa Lee, University of Michigan, Ann Arbor 22 23 - [Cardiopulmonary circulation simulation for the studying etiology of pulmonary 24 arterial hypertension](http://www.cims.nyu.edu/~leep/UMich/Cardiopulmonary_circulation.html) 25 - [Concentration dependent contraction of cardiomyocyte](http://www.cims.nyu.edu/~leep/UMich/Cardiac_differentiation.html) 26 - [Micro-organism swimming in two-phase micro-environment](http://www.cims.nyu.edu/~leep/UMich/Cancer_metastasis.html) 27 28- [Louis Moresi, Movie from a recent Nature paper using Underworld](http://youtu.be/cVulRP2tUGM) 29 30- [MOOSE Full-core reactor simulation](https://www.youtube.com/watch?v=4xTfQxpGAI4) 31 32- [Richard Katz, Journal of Petrology, 2008. doi 10.1016/j.jcp.2008.06.039](http://www.earth.ox.ac.uk/~richardk/res/magmaRidge/RidgeModelsKatz.mov) 33 34Two simulations of plate tectonic spreading at a mid-ocean ridge, driving mantle upwelling 35and melting. Axes are labelled with depth and distance in kilometres. Colours show the 36volume fraction of magma present; solid streamlines show the mantle flow; dashed contours 37are lines of constant temperature (the upper surface is cold, the deep mantle is hot); 38tracer particles mark the motion of the magma, where it is present. The upper panel has a 39plate speed of 1 cm/year; the bottom has 5 cm/year. Mid-ocean ridges host 80% of Earth’s 40volcanism. These simulation are PETSc-based numerical solutions of conservation of mass, 41momentum, and energy for two phases (mantle rock; magma) and two thermochemical 42components. 43 44- [Fokker-Planck kinetic calculation of the parallel current in the W7-X fusion experiment 45 in Greifswald, Germany. Contributed by Matt 46 Landreman.](https://github.com/landreman/sfincs/blob/master/doc/SFINCS_calculation_of_parallel_current_in_W7X_2040x1260.jpg) 47 48- [HiFi modeling framework, Vyacheslav Lukin](https://hifi-framework.webnode.com/hifi-framework/) 49 50 - [High resolution image](https://www.nersc.gov/assets/ScienceAtNERSC/SlavaFull.png) 51 - [Turbulence analysis of an experimental flux-rope plasma](https://iopscience.iop.org/0741-3335/56/6/064003/media/PPCF490028_movie1.mp4) 52 - [SSX Plasma Wind Tunnel -- Counter-helicity Merging](https://www.dropbox.com/s/v2g8vzns7na685v/merging_field.mpeg?dl=0) 53 - [Movie 1](https://www.dropbox.com/s/nc4vwnxw3lt01mi/full_movie.mpeg?dl=0) and 54 [Movie 2](https://www.dropbox.com/s/nn06fa8hsiqmqmw/zoom_movie.mpeg?dl=0) from 55 [Self-organization during spherical torus formation by flux rope merging in the Mega 56 Ampere Spherical Tokamak](https://www.mcs.anl.gov/article/10.1088/0741-3335/56/6/064009) 57 58- [CFDShip-Iowa simulations by Pablo Carrica](https://www.youtube.com/user/pcarrica) 59 60- [Simulation of Greenland present-day ice surface speed; it is a result of a PISM 61 simulation done by Andy Aschwanden at the University of Alaska Fairbanks](https://www.dropbox.com/s/3m8rphl81y70r3g/greenland-speed-pism.pdf?dl=0) 62 63- [Design Optimization of Aircraft Wings](https://www.youtube.com/user/MDOLaboratory) 64 discussed at <http://mdolab.engin.umich.edu> 65 66- [Fast deformation](https://web.cels.anl.gov/projects/petsc/download/images/FoldingAndErosion_FastDeformation.mov) and 67 [slower deformation](https://web.cels.anl.gov/projects/petsc/download/images/FoldingAndErosion_SlowerDeformationSteeperInitialSlope.mov) 68 from the code LaMEM developed by Boris Kaus, Johannes Gutenberg University of Mainz, 69 Mainz, Germany. 70 71The movies show the effects of erosion and tectonic motion on the deflection and folding 72of rock units in the upper few kilometers of the Earth. In one case we have a slower 73deformation rate and a steeper initial slope whereas on the other case tectonic 74deformation is an order of magnitude faster. The resulting folding patterns have some 75resemblance with natural folding patterns observed in the Zagros Mountains. From the paper 76Collignon, M., Kaus, B., May, D.A., Fernandez, N., 2014. Influences of surface processes 77on fold growth during 3-D detachment folding. Geochem Geophy Geosy 78doi:10.1002/2014GC005450 79
){kind=link}
){kind=link}