Peng Gao, Ruiyan Wang, Gengxing Zhao, Yuhuan Li
College of Resources and Environment, Shandong Agricultural University, Tai'an, China.
National Engineering Laboratory for Efficient Utilization of Soil and Fertilizer Resources, Tai'an, China.
PLoS One. 2020 Jul 22;15(7):e0235489. doi: 10.1371/journal.pone.0235489. eCollection 2020.
The ability to accurately measure the geometric characteristics of soil wetted bodies (SWBs) is very important for conserving water in agriculture. However, measurements of SWBs obtained using conventional methods have a number of defects. Ground penetrating radar (GPR) is a promising technique for detecting buried features. In this paper, we used GPR to nondestructively investigate SWBs formed under drip irrigation. First, numerical simulations were performed to obtain the theoretical radar-gram of SWBs. Then, controlled irrigation experiments were performed to obtain radar scan datasets in a laboratory. The GPR image was interpreted according to the numerical simulation results, and the SWB thickness detection accuracy was estimated. Finally, GPR detection was performed in the field with different irrigation volumes, and the detection effect was assessed. The GPR reflections in the laboratory and field measurements were more complex than in the numerical simulation images, but the location and thickness of SWBs were still clear; the accuracy of the measured thickness was high, and the accuracy decreased with an increase in irrigation volume. The radar image resolution and thickness accuracy measured in the field were slightly less than the values measured in the laboratory. Thus, GPR is able to quickly and accurately characterize SWBs formed by drip irrigation based on the thickness and relative position in the soil. Furthermore, the F-K offset transformation was an effective GPR data processing method for focusing reflections from SWBs to obtain their true position and physical extent.
准确测量土壤湿润体(SWB)的几何特征对于农业节水至关重要。然而,使用传统方法获得的SWB测量结果存在一些缺陷。探地雷达(GPR)是一种用于探测地下特征的有前景的技术。在本文中,我们使用GPR对滴灌条件下形成的SWB进行无损探测。首先,进行数值模拟以获得SWB的理论雷达图。然后,在实验室进行控制灌溉实验以获取雷达扫描数据集。根据数值模拟结果对GPR图像进行解释,并估计SWB厚度检测精度。最后,在田间进行不同灌溉量的GPR探测,并评估探测效果。实验室和田间测量中的GPR反射比数值模拟图像中的更复杂,但SWB的位置和厚度仍然清晰;测量厚度的精度较高,且精度随灌溉量增加而降低。田间测量的雷达图像分辨率和厚度精度略低于实验室测量值。因此,GPR能够基于土壤中的厚度和相对位置快速准确地表征滴灌形成的SWB。此外,F-K偏移变换是一种有效的GPR数据处理方法,用于聚焦来自SWB的反射以获得其真实位置和物理范围。