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一种基于TIN-CPG混合空间数据模型的精细三维地质模型构建方法

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  • 1. 南阳理工学院 软件学院,河南 南阳 473004;2. 中国地质大学(武汉)资源学院,湖北 武汉 430074; 3. 中国地质大学(武汉)计算机学院,湖北 武汉 430074;4. 中国地质大学(武汉)教育部长江三峡库区地质灾害研究中心,湖北 武汉 430074
唐丙寅,男,1986年生,博士,讲师,主要从事地学信息三维可视化和地理信息系统相关的研究工作。

收稿日期: 2015-05-25

  网络出版日期: 2018-06-05

基金资助

国家高技术研究发展计划(863计划)(No. 2008AA121602)。

A fine 3D geological modeling method based on TIN-CPG hybrid spatial data model

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  • 1. School of Software, Nanyang Institute of Technology, Nanyang, Henan 473004, China; 2. Faculty of Earth Resources, China University of Geosciences(Wuhan), Wuhan, Hubei 430074, China; 3. College of Computer Science, China University of Geosciences(Wuhan), Wuhan, Hubei 430074, China; 4. Three Gorges Research Center for Geo-hazard of Ministry of Education, China University of Geosciences(Wuhan), Wuhan, Hubei 430074, China

Received date: 2015-05-25

  Online published: 2018-06-05

Supported by

This work was supported by the National High Technology Research and Development Program of China (863 Program) (2008AA121602).

摘要

精细三维地质模型的构建是实现地质体真三维可视化分析的难题之一。提出一种基于不规则三角网(TIN)和角点网格(CPG)的混合空间数据模型来构建三维精细地质模型的方法。首先建立基于TIN的构造-地层格架三维地质模型,然后进行TIN面元模型到CPG体元模型的转换,将基于TIN的构造-地层格架模型转换为基于CPG的精细网格体元地质模型,从而实现“表达上”精细三维地质模型的构建。在转换过程中首先要进行地层序列的定义,然后对空间格网进行划分,在此基础上计算格网中各个单元格的空间坐标和各个网格的有效性,并将计算结果存储为GRDECL格式文件,最后通过QuantyView3D系统读取该文件实现精细地质属性模型的展示。利用该方法对沿海某城市一个重点区域进行精细水文地质模型的构建,验证了其方法的可行性。

本文引用格式

唐丙寅,吴冲龙,李新川, . 一种基于TIN-CPG混合空间数据模型的精细三维地质模型构建方法[J]. 岩土力学, 2017 , 38(4) : 1218 -1225 . DOI: 10.16285/j.rsm.2017.04.037

Abstract

The construction of fine 3D geological modeling is one of challenges in realizing true 3D visualization of geological body. Based on Triangulate Irregular Network (TIN) and Corner Point Grid (CPG) spatial data model, we propose a hybrid spatial data model for constructing fine 3D geological model. Firstly, a tectonic-stratigraphic framework model is set up based on TIN. Then, the framework model is converted into fine volumetric 3D geological model based on CPG voxel data model, and thus the fine expression of inner space of 3D geological body is achieved. During the converting process, it is necessary to define the order of strata. The mesh of the geological body is further realized by calculating the spatial coordinate of each grid cell and validating and saving data file in GRDECL format. Finally, the fine geological model is displayed by inputting the file into QuantyView3D system. A fine 3D hydrogeological model of the key area of a coastal city is constructed successfully by using the proposed method, and the feasibility of this method is verified.
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