生成式深度神经网络作为协同控制的替代方案

IF 2.6 Q2 COMPUTER SCIENCE, INTERDISCIPLINARY APPLICATIONS Applied Computing and Geosciences Pub Date : 2024-10-01 DOI:10.1016/j.acags.2024.100198
Herbert Rakotonirina , Paul Honeine , Olivier Atteia , Antonin Van Exem
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引用次数: 0

摘要

在地球科学领域,克里金法是空间插值的主要方法,而共克里金法是通过纳入次变量信息来完成目标变量空间插值的最常用方法。共克里金法依赖于空间静止性假设,但这一假设并非在所有地理空间环境中都成立,因此可能导致插值不准确。在数据稀少的地区,协同定位的有效性可能会大打折扣,影响插值结果的可靠性。此外,在使用大量数据进行插值时,特别是在三维插值的情况下,可能会耗费大量资源。在本文中,我们介绍了一种新的空间插值方法,它使用生成式深度神经网络考虑了两个变量。这种方法利用具有编码器-解码器架构的卷积神经网络,通过一个编码器和两个解码器来处理两个变量。此外,我们还引入了一个损失函数,便于控制两个变量之间的关系。传统的深度学习方法需要事先训练和标注数据,而我们提出的方法则消除了这一要求,简化了插值过程。为了评估我们方法的性能,我们使用了两个真实世界的数据集。第一个是土壤有机碳总量与归一化植被指数相结合的二维数据集。第二个数据集是一个三维数据集,结合了通过对钻孔数量非常有限的土壤岩心进行高光谱分析获得的碳氢化合物和氟化物的浓度。实验结果表明,所提出的方法优于普通克里金法和协同克里金法,当同时使用两个变量时,效果显著。我们还证明了加入辅助变量是如何减轻模型过拟合的。
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A generative deep neural network as an alternative to co-kriging
In geosciences, kriging is leading spatial interpolation, and co-kriging is the most commonly used method for accomplishing spatial interpolation of a target variable by incorporating information from a secondary variable. Co-kriging relies on the assumption of spatial stationarity, which may not hold true in all geospatial contexts, leading to potential inaccuracies in interpolation. The effectiveness of co-kriging can be compromised in areas with sparse data, impacting the reliability of interpolated results. Moreover, it can be resource-intensive when used for interpolation with a substantial volume of data, especially in the case of 3D interpolation. In this paper, we introduce a new method for spatial interpolation that considers two variables using a generative deep neural network. This approach utilizes a convolutional neural network with an encoder–decoder architecture, featuring a single encoder and two decoders to handle the two variables. Additionally, we introduce a loss function that facilitates the control over the relationships between the two variables. Traditional Deep Learning methods require prior training and labeled data, whereas the proposed approach eliminates this requirement and simplifies the interpolation process. In order to assess the performance of our method, we use two real-world datasets. The first one is a 2D dataset of total soil organic carbon combined with the Normalized Difference Vegetation Index. The second one is a 3D dataset that combines concentrations of Hydrocarbon and Fluoride obtained from hyperspectral analysis of soil cores with very limited number of boreholes. The experimental results demonstrate that the proposed method outperforms ordinary kriging and co-kriging, showing a significant improvement when both variables are used. We also demonstrate how the inclusion of the auxiliary variable serves as a means to mitigate the overfitting of the model.
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来源期刊
Applied Computing and Geosciences
Applied Computing and Geosciences Computer Science-General Computer Science
CiteScore
5.50
自引率
0.00%
发文量
23
审稿时长
5 weeks
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