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基于多信息融合的地应力场模拟研究OA

中文摘要英文摘要

地应力是各类矿冶工程中岩体稳定性分析和工程设计的重要参数,大量的现场地应力测量取心难度大、成本高,建立一种节约高效的地应力场预测方法具有重要的意义.该文以 SX 深层地层为研究对象,开展岩石力学特性评价实验、古地磁实验和差应变实验,确定区域地层的岩石力学参数信息和井点地应力信息,再结合地质构造信息,运用有限元模拟方法对多信息进行融合,反演得到区域地应力场的分布云图和等值线图,模拟结果显示区域 3 个主应力主要分布在 87.4~113.8、75.6~104.8 和 67.6~78.1 MPa.该方法测试量小、成本低,能够为矿区工程设计提供可靠的基础数据.

The in-stiu stress is the foundation of all kinds of engineering design,such as drilling and fracturing.It is very difficult to measure a lot of in-situ stress,and it is very important to establish an effective method to predict the stress field.Taking the SX deep formation as the research object,rock mechanical property evaluation experiments,paleomagnetism experi-ments and differential strain experiments were carried out to determine the rock mechanical parameter information of the regional formation and the geostress information of the well point.Combined with the geological structure information,the finite element simulation method was used to fuse multiple information,and the distribution nephogram and contour map of the regional geostress field were obtained by inversion.The simulation results showed that the three principal stresses in the region were mainly distributed in the range of 87.4~113.8,75.6~104.8 and 67.6~78.1 MPa.This method has small test volume and low cost,and can provide reliable basic data for mining engineering design.

陶良清

中海油能源发展股份有限公司上海工程技术分公司,上海 200335

能源科技

三轴应力实验差应变地应力场多信息融合古地磁实验

tri-axial stress experimentdifferential strainin-situ stress fieldmultiple information fusionpaleomagnetic experiment

《科技创新与应用》 2026 (25)

58-61,4

10.19981/j.CN23-1581/G3.2026.25.013

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