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Computational Fluid Dynamics Simulation Data of Spatial Deposition. In Lawrence Livermore National Laboratory (LLNL) Open Data Initiative

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DataCite Commons2026-04-17 更新2026-05-06 收录
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Relevant Information: This dataset’s physics problem is a two-dimensional, spatial pattern formed from a pollutant that has been released into the atmosphere and dispersed for up to an hour while undergoing deposition to the surface. The pollutant’s release location (s<sub>x</sub>,s<sub>y</sub>) is assumed to occur anywhere in a two-dimensional domain of 5000 m × 5000 m. The release is initialized from a small bubble that is centered five meters above the surface, has a radius of five meters, and has internal momentum that causes it to expand radially and rise to a height of about 100 meters within the initial minute of simulation time. The same bubble source was used for all the simulations as a simplification. Only the (s<sub>x</sub>,s<sub>y</sub>) coordinates of the locations of the bubble source are relevant. All the realizations used unit mass releases, and the resulting deposition patterns can be scaled proportionately for other mass amounts. The time scale of the simulated data represents the cumulative mass deposited on the surface for one hour. The pollutant is blown in a direction controlled by the large-scale atmospheric inflow winds expressed as wind speed (w<sub>s</sub>), which varies from 0.5 to 15 m/s, and wind direction (w<sub>d</sub>), which can be anywhere in the interval [0,360) degrees following standard mathematical convention. The files “inputs_15k_train.npy” and “inputs_1k_test.npy”, however, includes w<sub>u</sub> = w<sub>s</sub> cos(w<sub>d</sub>) and w<sub>v</sub> = w<sub>s</sub> sen(w<sub>d</sub>), the wind velocity components projected onto the x and y axes. We assume that the spatial patterns were collected by a hypothetical imaging device that records the magnitude of the logarithm of deposition as a red, green, and blue (RGB) color image with channels containing integer values ranging from 0 to 255. The goal is to predict a deposition image given its associated release location and wind velocity (four scalar quantities). In other words, we are interested in the following mapping: [s<sub>x</sub>,s<sub>y</sub>,w<sub>u</sub>,w<sub>v</sub>]→[height×width×RGB channel]. See [1]. The data is obtained from simulations and later post-processed to make it adequate for machine learning training. Given large-scale winds as an inflow boundary condition, the CFD code Aeolus [2] uses millions of grid cells to simulate fluid flow and material transport in complex, three-dimensional environments at high resolution, accounting for turbulence from structures, terrain features, and obstacles and predicting deposition on the ground and other surfaces. Megapixel deposition images were obtained by processing the output of Aeolus simulations, which were run using a resolution of (x,y,z)=1000×1000×100 cells, each cell representing 5 m × 5 m × 5 m. Within Aeolus, pollutant concentration and deposition values are calculated by releasing and transporting Lagrangian particles of specified masses and sizes within the flow field. Particles that intersect the ground or other surfaces through turbulence or gravitational settling are removed from the atmosphere and recorded as deposition having units of mass per area. The releases were modeled as small, rising bubbles of mass carried by the winds about a minute into the simulations. Note that the actual deposition values are not given in this dataset. The entire dataset, created by running Aeolus multiple times, contains 16,000 deposition images. The data images are stored as [number of images, height, width, RGB channels]= [16,000, 1000, 1000, 3]. Each megapixel image shows the spatial deposition pattern of a unique release scenario in Aeolus changing source location and inflow wind, [s<sub>x</sub>,s<sub>y</sub>,w<sub>u</sub>,w<sub>v</sub>], using Latin hypercube sampling technique within the design of experiment. The data can potentially be augmented for different wind directions by rotating the spatial plume pattern to predict deposition patterns. This augmentation is not always possible in practice due to terrain-based asymmetries in transport and dispersion. The Python rainbow colormap is used to create the RGB images for training and testing the autoencoder. As previously noted, RGB pixel colors are associated with the logarithm of the deposition values.
提供机构:
UC San Diego Library Digital Collections
创建时间:
2023-06-01
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