A study on geoelectrical recognition model of seawater/freshwater interface based on convolutional neural network: an application in sand tank experiments

IF 2.3 4区 地球科学 Acta Geophysica Pub Date : 2024-09-18 DOI:10.1007/s11600-024-01441-0
Jun Ma, Lusi Wei, Jia Xiong, Zhifang Zhou, Shumei Zhu
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Abstract

Seawater intrusion is a global environmental issue, and seawater intrusion monitoring requires a multidisciplinary approach to improve accuracy. Simplified seawater/freshwater interface models for coastal aquifers are generally divided into two types: abrupt interface models and wedge-shaped interface models. Electrical resistivity tomography (ERT) is the visualization of subsurface resistivity distributions in 2D or 3D and has been widely used in seawater intrusion monitoring. This paper presents a geoelectrical recognition model for classifying simplified seawater/freshwater interface types based on a convolutional neural network (CNN). The CNN structure is composed of three convolutional layers, three max pooling layers, two fully connected layers, and one Softmax layer. A total of 686 samples were combined for model training, and obtained 0.9581 for the average accuracy (ACU) and 1.3500 for the average cross-entropy loss (CEL). Sand tank experiments were carried out to simulate the process of seawater intrusion caused by a rise in the water level of sea water rise or a decrease in the water level of fresh water, the ERT method was used to monitor the resistivity of the aquifer during the experiments, and the fully trained CNN model was used to classify the interface types. According to the output data, the probability of observing the wedge-shaped interfaces during the experiments at 300 and 345 min were 98.85% and 99.89%, while the probability of observing the abrupt interfaces were 1.15% and 0.11%. The results showed that the ERT method offers a fast and nondestructive approach for monitoring seawater intrusion, and accurate recognition results of interface types were obtained using a well-trained recognition model in the laboratory experiments.

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基于卷积神经网络的海水/淡水界面地电识别模型研究:在沙池实验中的应用
海水入侵是一个全球性的环境问题,海水入侵监测需要采用多学科方法来提高准 确性。沿海含水层的简化海水/淡水界面模型一般分为两类:突变界面模型和楔形界面模型。电阻率层析成像(ERT)是地下电阻率分布的二维或三维可视化技术,已广泛应用于海 水入侵监测。本文提出了一种基于卷积神经网络(CNN)的地质电学识别模型,用于对简化的海水/淡水界面类型进行分类。CNN 结构由三个卷积层、三个最大池化层、两个全连接层和一个 Softmax 层组成。模型训练共结合了 686 个样本,获得了 0.9581 的平均准确率(ACU)和 1.3500 的平均交叉熵损失(CEL)。通过沙槽实验模拟海水水位上升或淡水水位下降引起的海水入侵过程,采用 ERT 方法监测实验过程中含水层的电阻率,利用完全训练的 CNN 模型对界面类型进行分类。根据输出数据,在 300 和 345 min 的实验中观察到楔形界面的概率分别为 98.85% 和 99.89%,而观察到突变界面的概率分别为 1.15% 和 0.11%。结果表明,ERT 方法为监测海水入侵提供了一种快速、无损的方法,并且在实验室实验中使用训练有素的识别模型获得了准确的界面类型识别结果。
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来源期刊
Acta Geophysica
Acta Geophysica GEOCHEMISTRY & GEOPHYSICS-
CiteScore
3.80
自引率
13.00%
发文量
251
期刊介绍: Acta Geophysica is open to all kinds of manuscripts including research and review articles, short communications, comments to published papers, letters to the Editor as well as book reviews. Some of the issues are fully devoted to particular topics; we do encourage proposals for such topical issues. We accept submissions from scientists world-wide, offering high scientific and editorial standard and comprehensive treatment of the discussed topics.
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