郝晨光,郭晓阳,邓存宝,等. 基于Bi-PTI模型的CT数字煤岩孔裂隙精准识别及阈值反演[J]. 煤炭学报,2023,48(4):1516−1526. DOI: 10.13225/j.cnki.jccs.2022.0602
引用本文: 郝晨光,郭晓阳,邓存宝,等. 基于Bi-PTI模型的CT数字煤岩孔裂隙精准识别及阈值反演[J]. 煤炭学报,2023,48(4):1516−1526. DOI: 10.13225/j.cnki.jccs.2022.0602
HAO Chenguang,GUO Xiaoyang,DENG Cunbao,et al. Precise identification and threshold inversion of pores and fissures in CT digital coal rock based on Bi-PTI model[J]. Journal of China Coal Society,2023,48(4):1516−1526. DOI: 10.13225/j.cnki.jccs.2022.0602
Citation: HAO Chenguang,GUO Xiaoyang,DENG Cunbao,et al. Precise identification and threshold inversion of pores and fissures in CT digital coal rock based on Bi-PTI model[J]. Journal of China Coal Society,2023,48(4):1516−1526. DOI: 10.13225/j.cnki.jccs.2022.0602

基于Bi-PTI模型的CT数字煤岩孔裂隙精准识别及阈值反演

Precise identification and threshold inversion of pores and fissures in CT digital coal rock based on Bi-PTI model

  • 摘要: 在CT数字煤岩研究领域,灰度阈值选取直接影响空间结构重建的准确性。为使孔裂隙空间重构数据能更精准地表征真实结构,提升煤岩微细观渗流研究的可靠性,建立了CT数字煤岩孔隙率与灰度阈值的映射关系,采用灰度阈值分布规律定量分析了孔裂隙和基质骨架的发育特征;构建了识别孔裂隙结构的Biphasic Pore Threshold Inversion灰度阈值模型(Bi-PTI模型),对不同变质煤CT扫描数据的孔裂隙最佳灰度阈值进行了数值反演,将模型计算获得的孔隙率与压汞测试值进行对比;基于最佳灰度阈值反演结果重建了孔裂隙空间结构,通过空间结构参数和拓扑结构参数与Otsu模型、MP-Otsu模型进行了对比分析。研究结果表明:CT数字煤岩孔隙率随灰度阈值的增加呈非对称S型分布,且具有指数增加−对数上升的分段特征;Bi-PTI模型能够较好地反映孔隙率与灰度阈值的映射关系,表征孔裂隙和基质骨架的发育特征;通过Otsu模型计算的孔隙率高达70%以上,MP-Otsu模型计算的孔隙率受矿物含量影响较大,而Bi-PTI模型在0.40%~16.22%,更接近压汞实测数据;Bi-PTI模型可以弥补因孔裂隙过度识别导致的空间重构缺陷,实现小尺度孔裂隙空间结构的精准识别;Otsu模型极易忽略部分孔隙拓扑结构,MP-Otsu模型对低矿物含量煤体的拓扑结构重建效果不佳,而Bi-PTI模型对缺陷位置拓扑特征具有较好的识别能力,能够真实还原孔裂隙拓扑体系的孔喉丰度和连通特性。

     

    Abstract: In the research area of the CT digital coal petrography, the selection of gray threshold directly affects the accuracy of spatial structure remodeling. To allow the pores and fissures space remodeling data to more accurately represent the real structure and improve the reliability of research on microscopic seepage of coal rock, the mapping relation between the CT digital coal rock porosity and gray threshold is established. Also, the distribution rule of gray threshold is adopted to conduct a quantitative analysis of the development features of pore, fissure and matrix. The Bi-PTI (Biphasic Pore Threshold Inversion) model is established for the identification of pore and fissure structures. The value inversion of the optimal gray threshold of pore and fissure based on the CT scanning data of metamorphic coal, and the comparison of porosity obtained with the model against the mercury injection test value are conducted. On the basis of the optimal gray threshold inversion results, the spatial structure of pore and fissure is remodeled and compared with the Otsu model through the parameters of spatial structure and topological structure. Research results indicate that the porosity based on the CT digital coal petrography is in asymmetrical S-shaped distribution as the threshold value increases, with the features of exponential increase and logarithmic climb at different sections. The Bi-PTI model can fairly reflect the mapping relation between porosity and gray threshold, and represent the development features of pore, fissure and matrix. The porosity calculated through the Otsu model is as high as over 70%, the porosity calculated by the MP-Otsu model is greatly affected by the mineral content while that calculated with the Bi-PTI model ranges from 0.40% to 16.22%, more close to the mercury injection test data. The Otsu model is most likely to neglect the topological structure with partial pores and fissures. The MP-Otsu model is not effective for constructing the topology of coal samples with low mineral content, while the Bi-PTI model can better identify the topological features in the locations of the defect and faithfully restore the pore throat abundance and connectivity in the pore and fissure topology.

     

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