Vertical soil moisture dynamics in the vadose zone: A high-resolution GPR reflection study

C. Steelman, A. Endres
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引用次数: 2

Abstract

This paper presents a multi-year field study in which high-frequency 900 MHz reflection traveltime measurements were used to monitor vertical soil moisture distribution in the upper 3.0 m of vadose zone. GPR reflection profiles and common-midpoint (CMP) soundings were collected over the complete annual cycle of soil conditions characterized by numerous wetting, drying and freezing cycles typical of mid-latitude climates. The presence of four distinct stratigraphic reflection events at well-defined depths permitted quantitative assessment of seasonal moisture processes and their temporal dynamics during the study period. The incorporation of direct ground wave measurements from coincidently collected CMP soundings yielded improved resolution at the air-soil interface which facilitated characterization of the hydraulic coupling between shallow and deeper moisture conditions.
渗透带垂直土壤水分动态:高分辨率探地雷达反射研究
本文介绍了利用900 MHz高频反射行时测量方法,在多年的野外研究中,监测了渗透带3.0 m上部土壤水分的垂直分布。GPR反射剖面和共中点(CMP)测深数据收集了土壤条件的完整年循环,其特征是中纬度气候典型的多次湿润、干燥和冻结循环。在定义明确的深度,存在四个不同的地层反射事件,可以定量评估季节性水分过程及其在研究期间的时间动态。结合直接地波测量数据,同时收集CMP测深数据,提高了空气-土壤界面的分辨率,有助于表征浅层和深层水分条件之间的水力耦合。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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