Contactless estimation of soil moisture using leaky Rayleigh waves and a fully convolutional network

IF 2.5 3区 地球科学 Q3 ENVIRONMENTAL SCIENCES
Seoungmin Lee, Dong Kook Woo, Hajin Choi
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Abstract

Abstract Soil moisture is a key factor that influences various aspects of ecosystem functioning. Measuring soil moisture without installing any objects in the soil is desirable because it allows for accurate characterizations of soil moisture while minimizing impacts on soil structure and ecology. In this study, we explored the potential of leaky Rayleigh waves as a proxy to contactlessly estimate soil moisture. We developed an ultrasonic system containing a transducer, receivers, and acoustic barrier. The specimens of sand, silt, and clay were utilized. Experiments were conducted over 4 months. We used a widely used soil‐embedded moisture sensor to compare and develop relationships between leaky Rayleigh waves and soil moisture. Our results showed that as soil moisture increased, the velocity and amplitude of leaky Rayleigh waves decreased because water molecules attracted to the soils led to their attenuation. However, their magnitudes were not considerable except for very dry soils. To overcome these limited relations to estimate soil moisture from leaky Rayleigh waves, we constructed authentic images based on the observed leaky Rayleigh waves and used them as inputs for a fully convolutional network. We found that the combination of the ultrasonic system and deep learning approach developed in this study were suitable for estimating soil moisture without soil disturbances (RMSE = 0.01 m 3 m −3 ). This study suggests that leaky Rayleigh waves have the potential to serve as a reliable proxy for determining soil moisture without the need for physical contact.
利用泄漏瑞利波和全卷积网络进行土壤湿度的非接触估计
土壤水分是影响生态系统各方面功能的关键因素。无需在土壤中安装任何物体即可测量土壤湿度是可取的,因为它可以准确表征土壤湿度,同时最大限度地减少对土壤结构和生态的影响。在这项研究中,我们探索了泄漏瑞利波作为非接触估计土壤湿度的代理的潜力。我们开发了一种包含换能器、接收器和声障的超声波系统。利用了砂、粉和粘土的试样。实验进行了4个多月。我们使用一种广泛使用的土壤嵌入式湿度传感器来比较和发展泄漏瑞利波与土壤湿度之间的关系。结果表明,随着土壤湿度的增加,漏失瑞利波的速度和振幅减小,这是由于土壤吸收的水分子导致其衰减。然而,除了非常干燥的土壤外,它们的大小并不大。为了克服这些有限的关系,从泄漏瑞利波中估计土壤湿度,我们基于观测到的泄漏瑞利波构建了真实图像,并将其用作全卷积网络的输入。我们发现,超声波系统和本研究开发的深度学习方法相结合适用于在没有土壤扰动的情况下估计土壤水分(RMSE = 0.01 m 3 m−3)。这项研究表明,漏瑞利波有潜力作为确定土壤湿度的可靠代理,而不需要物理接触。
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来源期刊
Vadose Zone Journal
Vadose Zone Journal 环境科学-环境科学
CiteScore
5.60
自引率
7.10%
发文量
61
审稿时长
3.8 months
期刊介绍: Vadose Zone Journal is a unique publication outlet for interdisciplinary research and assessment of the vadose zone, the portion of the Critical Zone that comprises the Earth’s critical living surface down to groundwater. It is a peer-reviewed, international journal publishing reviews, original research, and special sections across a wide range of disciplines. Vadose Zone Journal reports fundamental and applied research from disciplinary and multidisciplinary investigations, including assessment and policy analyses, of the mostly unsaturated zone between the soil surface and the groundwater table. The goal is to disseminate information to facilitate science-based decision-making and sustainable management of the vadose zone. Examples of topic areas suitable for VZJ are variably saturated fluid flow, heat and solute transport in granular and fractured media, flow processes in the capillary fringe at or near the water table, water table management, regional and global climate change impacts on the vadose zone, carbon sequestration, design and performance of waste disposal facilities, long-term stewardship of contaminated sites in the vadose zone, biogeochemical transformation processes, microbial processes in shallow and deep formations, bioremediation, and the fate and transport of radionuclides, inorganic and organic chemicals, colloids, viruses, and microorganisms. Articles in VZJ also address yet-to-be-resolved issues, such as how to quantify heterogeneity of subsurface processes and properties, and how to couple physical, chemical, and biological processes across a range of spatial scales from the molecular to the global.
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