程久龙,王慧杰,徐忠忠,等. 基于全卷积神经网络的钻孔瞬变电磁法岩层富水性预测研究[J]. 煤田地质与勘探,2023,51(1):289−297. DOI: 10.12363/issn.1001-1986.22.12.0937
引用本文: 程久龙,王慧杰,徐忠忠,等. 基于全卷积神经网络的钻孔瞬变电磁法岩层富水性预测研究[J]. 煤田地质与勘探,2023,51(1):289−297. DOI: 10.12363/issn.1001-1986.22.12.0937
CHENG Jiulong,WANG Huijie,XU Zhongzhong,et al. Research on aquifer water abundance evaluation by borehole transient electromagnetic method based on FCNN[J]. Coal Geology & Exploration,2023,51(1):289−297. DOI: 10.12363/issn.1001-1986.22.12.0937
Citation: CHENG Jiulong,WANG Huijie,XU Zhongzhong,et al. Research on aquifer water abundance evaluation by borehole transient electromagnetic method based on FCNN[J]. Coal Geology & Exploration,2023,51(1):289−297. DOI: 10.12363/issn.1001-1986.22.12.0937

基于全卷积神经网络的钻孔瞬变电磁法岩层富水性预测研究

Research on aquifer water abundance evaluation by borehole transient electromagnetic method based on FCNN

  • 摘要: 巷道掘进前方采用钻探或地球物理方法进行超前探测含水层的位置及富水性,提前做好防治水工作对煤矿安全生产至关重要。利用钻孔瞬变电磁法(BTEM)进行超前探测优势明显,目前解释方法是根据计算的电阻率进行岩层富水性的定性分析,还无法实现对含水层富水性等级进行预测。提出利用钻孔瞬变电磁法探测,采用全卷积神经网络(FCNN)方法进行钻孔外围含水层富水性等级的准确预测。首先,依据阿尔奇公式、Kozeny–Carman公式、导水系数公式和单位涌水量公式,建立砂岩含水层单位厚度的电阻率与按钻孔单位涌水量划分的含水层富水性4个等级的对应关系;其次,建立全空间条件下不同富水性岩层的地质–地球物理模型,采用三维时域有限差分法(FDTD)进行全空间瞬变电磁场数值模拟;为了接近实际情况,在正演结果中加入了5%~15%的随机噪声,提取与岩层富水性等级关联的特征参数,采用全卷积神经网络(FCNN)进行了岩层富水性等级预测的训练和仿真测试,测试集预测的富水性等级平均准确率为91.8%;最后,利用某矿煤层水力压裂后的钻孔瞬变电磁法实测数据进行煤岩层富水性等级预测,检验FCNN方法预测效果。研究结果表明:采用全卷积神经网络预测钻孔附近岩层富水性是可行和有效的,可以实现钻孔径向方向岩层富水性等级的准确预测,提高了钻孔瞬变电磁法对钻孔外围岩层富水性的探测精度,该方法将在超前探测岩层富水性方面发挥重要作用。

     

    Abstract: Predicting the location and water abundance of aquifers by drilling or geophysical methods before tunneling is very important to prevent water disasters in advance for the safety of coal mine production. The use of borehole transient electromagnetic method (BTEM) for advanced detection has obvious advantages. At present, the interpretation method is based on the calculated resistivity to qualitatively analyze rock water abundance, and it is impossible to predict the aquifer water abundance grade. So, the fully convolutional neural network (FCNN) method is proposed to predict the aquifer water abundance grade for BTEM. Firstly, according to the Archie formula, Kozeny-Carman formula, conductivity formula, and unit water inflow formula, the corresponding relationship between the resistivity per unit thickness of the sandstone and the four grades of aquifer water abundance grades according to the amount of water inflow per borehole is established. Then, the geological-geophysical model of different rock water abundance under the whole space condition is simulated by the three-dimensional finite difference time domain (FDTD) method, and the characteristic parameters used to predict the water abundance grades are extracted. To be close to the actual situation, 5%-15% random noise is added to the forward modeling results, and FCNN is used to train and simulate the prediction of aquifer water abundance. The average accuracy of aquifer water abundance grade predicted by the test set is 91.8%. Finally, the proposed method is used to predict the water abundance grade of coal seam after hydraulic fracturing in a mine. The results show that FCNN method is feasible and effective to predict the aquifer water abundance grade in the radial direction of the borehole and improve the detection accuracy of BTEM. This method will play an important role in the advanced detection of aquifer water abundance.

     

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