processing:synthetic_dataset
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| processing:synthetic_dataset [2019/01/17 15:22] – estelle | processing:synthetic_dataset [2019/02/23 20:43] (current) – [Input file example 3: olivine from a CIF file] estelle | ||
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| ====== Creation of the synthetic dataset ====== | ====== Creation of the synthetic dataset ====== | ||
| - | Synthetic data sets are useful to learn how to process data. You can input the experimental parameters you will use in your actual experiment and your actual sample. The software to do so is [[software: | + | Synthetic data sets are useful to learn how to process data. You can input the experimental parameters you will use in your actual experiment and your actual sample. The software to do so is [[software: |
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| + | For high pressure experiments, | ||
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| + | The simulation will provide 2D diffraction images but also G-vectors, inverse UB matrices (UBi) for all grains, and some more files. You will get at least 7 different files from the simulation as well as the diffraction images. The amount of diffraction images depends on the ω range and the step size defined in the input file. For example, a ω range Δω = [-28°; | ||
| ===== Basic usage ===== | ===== Basic usage ===== | ||
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| This third example is a test of calculation from a [[fileformat: | This third example is a test of calculation from a [[fileformat: | ||
| - | Our problem was that the widely used space group for olivine, Pbnm, do not have a space groupe number and we need a space group number for the index.ini input file for GrainSpotter. So we use a CIF file to translate the cristallographic | + | Our problem was that the widely used space group for olivine, |
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| + | The transformation | ||
| * a (Pbnm) -> c (Pnma) | * a (Pbnm) -> c (Pnma) | ||
| * b (Pbnm) -> a (Pnma) | * b (Pbnm) -> a (Pnma) | ||
| Line 52: | Line 58: | ||
| But we need to specify it to PolyXSim in order to have the good symetry of the olivine, and hence, the good corresponding diffraction peaks. | But we need to specify it to PolyXSim in order to have the good symetry of the olivine, and hence, the good corresponding diffraction peaks. | ||
| - | We get a Pbnm CIF file from the American Mineralogist crystal structure database and we transform it to have a CIF file for Pnma space group. | + | First get a //Pbnm// CIF file from the American Mineralogist crystal structure database and transform it to have a CIF file for //Pnma// space group. |
| [[fileformat: | [[fileformat: | ||
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| Then, before the simulation of your data, in the .inp file for PolyXSim you should put a # before the space group line and make the structure_phase_0 line active. You should have : | Then, before the simulation of your data, in the .inp file for PolyXSim you should put a # before the space group line and make the structure_phase_0 line active. You should have : | ||
| - | * ### Structural | + | < |
| - | | + | ### Structural |
| - | | + | unit_cell |
| - | | + | #sgno 62 #space group number |
| - | | + | #oR |
| - | | + | # |
| - | | + | #or |
| - | + | structure_phase_0 ' | |
| - | Don't forget to change the order of the axes in the unit_cell line of PolyXSim too! | + | </ |
| - | + | ||
| - | From here, PolyXSim simulate grains in the Pnma system so the peaks you obtain (and then the G-vectors) are in Pnma. Be carefull when comparing with real data study where the Pbnm system is more widespread! Use the space group number 62 in the .ini file of GrainsPotter to find the grains from these Pnma G-vectors. | + | |
| + | Do not forget to change the order of the axes in the unit_cell line of PolyXSim as well! | ||
| + | From here, PolyXSim simulate grains in the //Pnma// system so the peaks you obtain (and then the G-vectors) are in //Pnma//. Be carefull when comparing with other studies for which the //Pbnm// system is more common! Use the space group number 62 in the .ini file of GrainsPotter to find the grains from these Pnma G-vectors. | ||
| ==== Remarks ==== | ==== Remarks ==== | ||
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| ===== Output files ===== | ===== Output files ===== | ||
| - | There are a number of possible output files from this procedure. Possible output files include: | + | There are a number of possible output files from this procedure. |
| + | |||
| + | The time consuming process is the creation of synthetic diffraction images. This time highly depends on the parameters in the input file, e.g. the amount of grains, the peak shape, strain tensors, or additional noise. For a simple test, it is wise to use an input file with very simple parameters (only a few grains, no strain tensors, no noise, small ω range etc.). | ||
| + | |||
| + | Possible output files include: | ||
| * [[fileformat: | * [[fileformat: | ||
| * [[fileformat: | * [[fileformat: | ||
| - | * [[fileformat: | + | * [[fileformat: |
| - | * [[fileformat: | + | * [[fileformat: |
| - | * [[fileformat: | + | * [[fileformat: |
| - | * [[fileformat: | + | * [[fileformat: |
| * [[fileformat: | * [[fileformat: | ||
| * [[fileformat: | * [[fileformat: | ||
| - | * [[fileformat: | + | * [[fileformat: |
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