2022年petrel地质建模软件的曲率计算原理及方法 .pdf
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1、1Curvature Modeling BackgroundThis extensive workflow can calculate the curvature of a reservoir based on the geometry of the 3D grid. This in turn can be used in combination with fracture modeling. Curvature is often regarded a good indicator of fracture intensity for specify types of conjugate fra
2、cture pairs. Curvature can be used as a secondary variable in fracture modeling. It can also be used to spot irregularities in a 3D grid in general ResultA new, continues curvature property will be added to the 3D grid, the name of which will depend on the chosen method of curvature calculation (min
3、, max, mean or gauss). Prerequisites This workflow has been tested on simple and moderately complex grids. One needs a 3D grid with “segments ” modeled as a property under geometrical modeling. This segment property must be specified in the input. The workflow is most accurate when all the faults ar
4、e also segment boundaries. In case of (steep) faults not acting as a segment boundary (faults terminating or dying out within a segment), the modeling workflow becomes less accurate, because of the possibility of comparing depth values from both sides of the fault and thereby giving rise to an artif
5、icially high curvature. This can be partly counteracted by using the “distance from fault” property and a low value for the parameter “surface expansion”, but it is highly recommended to use a 3D grid with only segment dividing faults. If you do not have this, you can use trends set as segment bound
6、ary in the pillar gridding process. The workflow is fully compatible with the zone and segment filters. Curvature calculation itself is done per layer and per segment. The workflow itself works as follows. -The property “Curvature” is created, having values of zero everywhere. This property will pro
7、gressively be filled while the workflow is running. A suffix to the name will denote the curvature type -The property “K_Curve ” is created, giving an index to each layer. (0 to N from top to bottom) -The first loop will run from the min to the max layer index, starting with the top layer. -The seco
8、ndary loop progressively goes through all segments. -For the top layer in the first segment, the property Z (depth) will be calculated -An average map will be created from the Z values of that layer. Since map calculation is limited to only one layer, the map will simply represent the depth of the l
9、ayer (measured for cell center) -min, max, mean or gauss curvature is calculated for this layer and recreated as a separated surface -This calculation will return a curvature surface for one layer in one segment. Workflow SpecificsWorkflow Specifics Petrel Version 2009.1 Domain Geology Modules Geosc
10、ience Core or Combined Core Expert Level Advanced 名师资料总结 - - -精品资料欢迎下载 - - - - - - - - - - - - - - - - - - 名师精心整理 - - - - - - - 第 1 页,共 5 页 - - - - - - - - - 2-A property operation is used to extract the values of this surface and plot them back onto the grid, a calculator statement is used to limit
11、 the results to the proper layer in the correct segment. -The curvature results from the single layer will be added to the previously empty “Curvature” property. -The workflow will no go through the same layer in the next segment and run over again. -Once finished with all segments, the next layer (
12、below) is modeled, gradually populating the “Curvature”. Note that this workflow represents a 3D property for one layer as a surface, then performs a surface calculation and finally plots the results back in the grid. There are five adjustable numeric variables controlling the accuracy of the curvat
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