1*9b92b1d3SBarry Smith# Applications and Publications 2*9b92b1d3SBarry Smith 3*9b92b1d3SBarry SmithPETSc has been used for modeling in all of these areas: Acoustics, Aerodynamics, Air 4*9b92b1d3SBarry SmithPollution, Arterial Flow, Bone Fractures, Brain Surgery, Cancer Surgery, Cancer Treatment, 5*9b92b1d3SBarry SmithCarbon Sequestration, Cardiology, Cells, CFD, Combustion, Concrete, Corrosion, Data 6*9b92b1d3SBarry SmithMining, Dentistry, Earth Quakes, Economics, Esophagus, Fission, Fusion, Glaciers, Ground 7*9b92b1d3SBarry SmithWater Flow, Linguistics, Mantel Convection, Magnetic Films, Material Science, Medical 8*9b92b1d3SBarry SmithImaging, Ocean Dynamics, Oil Recover, PageRank, Polymer Injection Molding, Polymeric 9*9b92b1d3SBarry SmithMembranes, Quantum computing, Seismology, Semiconductors, Rockets, Relativity, Surface 10*9b92b1d3SBarry SmithWater Flow. 11*9b92b1d3SBarry Smith 12*9b92b1d3SBarry Smith## Images 13*9b92b1d3SBarry Smith 14*9b92b1d3SBarry SmithThese are images and movies from application simulations developed by PETSc users. 15*9b92b1d3SBarry Smith 16*9b92b1d3SBarry Smith- [COOLFluiD Simulation Environment](https://github.com/andrealani/COOLFluiD/wiki/Gallery-of-applications) 17*9b92b1d3SBarry Smith 18*9b92b1d3SBarry Smith- [Defmod - Parallel multiphysics finite element code for modeling crustal deformation 19*9b92b1d3SBarry Smith during the earthquake/rifting cycle](https://bitbucket.org/stali/defmod/wiki/Gallery) 20*9b92b1d3SBarry Smith 21*9b92b1d3SBarry Smith- Pilhwa Lee, University of Michigan, Ann Arbor 22*9b92b1d3SBarry Smith 23*9b92b1d3SBarry Smith - [Cardiopulmonary circulation simulation for the studying etiology of pulmonary 24*9b92b1d3SBarry Smith arterial hypertension](http://www.cims.nyu.edu/~leep/UMich/Cardiopulmonary_circulation.html) 25*9b92b1d3SBarry Smith - [Concentration dependent contraction of cardiomyocyte](http://www.cims.nyu.edu/~leep/UMich/Cardiac_differentiation.html) 26*9b92b1d3SBarry Smith - [Micro-organism swimming in two-phase micro-environment](http://www.cims.nyu.edu/~leep/UMich/Cancer_metastasis.html) 27*9b92b1d3SBarry Smith 28*9b92b1d3SBarry Smith- [Louis Moresi, Movie from a recent Nature paper using Underworld](http://youtu.be/cVulRP2tUGM) 29*9b92b1d3SBarry Smith 30*9b92b1d3SBarry Smith- [MOOSE Full-core reactor simulation](https://www.youtube.com/watch?v=4xTfQxpGAI4) 31*9b92b1d3SBarry Smith 32*9b92b1d3SBarry Smith- [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*9b92b1d3SBarry Smith 34*9b92b1d3SBarry SmithTwo simulations of plate tectonic spreading at a mid-ocean ridge, driving mantle upwelling 35*9b92b1d3SBarry Smithand melting. Axes are labelled with depth and distance in kilometres. Colours show the 36*9b92b1d3SBarry Smithvolume fraction of magma present; solid streamlines show the mantle flow; dashed contours 37*9b92b1d3SBarry Smithare lines of constant temperature (the upper surface is cold, the deep mantle is hot); 38*9b92b1d3SBarry Smithtracer particles mark the motion of the magma, where it is present. The upper panel has a 39*9b92b1d3SBarry Smithplate speed of 1 cm/year; the bottom has 5 cm/year. Mid-ocean ridges host 80% of Earth’s 40*9b92b1d3SBarry Smithvolcanism. These simulation are PETSc-based numerical solutions of conservation of mass, 41*9b92b1d3SBarry Smithmomentum, and energy for two phases (mantle rock; magma) and two thermochemical 42*9b92b1d3SBarry Smithcomponents. 43*9b92b1d3SBarry Smith 44*9b92b1d3SBarry Smith- [Fokker-Planck kinetic calculation of the parallel current in the W7-X fusion experiment 45*9b92b1d3SBarry Smith in Greifswald, Germany. Contributed by Matt 46*9b92b1d3SBarry Smith Landreman.](https://github.com/landreman/sfincs/blob/master/doc/SFINCS_calculation_of_parallel_current_in_W7X_2040x1260.jpg) 47*9b92b1d3SBarry Smith 48*9b92b1d3SBarry Smith- [HiFi modeling framework, Vyacheslav Lukin](https://hifi-framework.webnode.com/hifi-framework/) 49*9b92b1d3SBarry Smith 50*9b92b1d3SBarry Smith - [High resolution image](https://www.nersc.gov/assets/ScienceAtNERSC/SlavaFull.png) 51*9b92b1d3SBarry Smith - [Turbulence analysis of an experimental flux-rope plasma](https://iopscience.iop.org/0741-3335/56/6/064003/media/PPCF490028_movie1.mp4) 52*9b92b1d3SBarry Smith - [SSX Plasma Wind Tunnel -- Counter-helicity Merging](https://www.dropbox.com/s/v2g8vzns7na685v/merging_field.mpeg?dl=0) 53*9b92b1d3SBarry Smith - [Movie 1](https://www.dropbox.com/s/nc4vwnxw3lt01mi/full_movie.mpeg?dl=0) and 54*9b92b1d3SBarry Smith [Movie 2](https://www.dropbox.com/s/nn06fa8hsiqmqmw/zoom_movie.mpeg?dl=0) from 55*9b92b1d3SBarry Smith [Self-organization during spherical torus formation by flux rope merging in the Mega 56*9b92b1d3SBarry Smith Ampere Spherical Tokamak](https://www.mcs.anl.gov/article/10.1088/0741-3335/56/6/064009) 57*9b92b1d3SBarry Smith 58*9b92b1d3SBarry Smith- [CFDShip-Iowa simulations by Pablo Carrica](https://www.youtube.com/user/pcarrica) 59*9b92b1d3SBarry Smith 60*9b92b1d3SBarry Smith- [Simulation of Greenland present-day ice surface speed; it is a result of a PISM 61*9b92b1d3SBarry Smith simulation done by Andy Aschwanden at the University of Alaska Fairbanks](https://www.dropbox.com/s/3m8rphl81y70r3g/greenland-speed-pism.pdf?dl=0) 62*9b92b1d3SBarry Smith 63*9b92b1d3SBarry Smith- [Design Optimization of Aircraft Wings](https://www.youtube.com/user/MDOLaboratory) 64*9b92b1d3SBarry Smith discussed at <http://mdolab.engin.umich.edu> 65*9b92b1d3SBarry Smith 66*9b92b1d3SBarry Smith- [Fast deformation](https://web.cels.anl.gov/projects/petsc/download/images/FoldingAndErosion_FastDeformation.mov) and 67*9b92b1d3SBarry Smith [slower deformation](https://web.cels.anl.gov/projects/petsc/download/images/FoldingAndErosion_SlowerDeformationSteeperInitialSlope.mov) 68*9b92b1d3SBarry Smith from the code LaMEM developed by Boris Kaus, Johannes Gutenberg University of Mainz, 69*9b92b1d3SBarry Smith Mainz, Germany. 70*9b92b1d3SBarry Smith 71*9b92b1d3SBarry SmithThe movies show the effects of erosion and tectonic motion on the deflection and folding 72*9b92b1d3SBarry Smithof rock units in the upper few kilometers of the Earth. In one case we have a slower 73*9b92b1d3SBarry Smithdeformation rate and a steeper initial slope whereas on the other case tectonic 74*9b92b1d3SBarry Smithdeformation is an order of magnitude faster. The resulting folding patterns have some 75*9b92b1d3SBarry Smithresemblance with natural folding patterns observed in the Zagros Mountains. From the paper 76*9b92b1d3SBarry SmithCollignon, M., Kaus, B., May, D.A., Fernandez, N., 2014. Influences of surface processes 77*9b92b1d3SBarry Smithon fold growth during 3-D detachment folding. Geochem Geophy Geosy 78*9b92b1d3SBarry Smithdoi:10.1002/2014GC005450 79
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