In-Situ Monitoring and Characteristic Analysis of Freezing-Thawing Cycles in a Deep Vadose Zone

Ce Zheng,Yudong Lu,Huanhuan Li,Jiří Šimůnek,Xiuhua Liu,Yijian Zeng,Changchun Shi

doi:10.3390/w12051261

Ce Zheng, Yudong Lu + Show 5 more

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https://doi.org/10.3390/w12051261

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Abstract

Freeze-thaw cycles play a critical role in affecting ecosystem services in arid regions. Monitoring studies of soil temperature and moisture during a freeze-thaw process can generate data for research on the coupled movement of water, vapor, and heat during the freezing-thawing period which can, in turn, provide theoretical guidance for rational irrigation practices and ecological protection. In this study, the soil temperature and moisture changes in the deep vadose zone were observed by in-situ monitoring from November 2017 to March 2018 in the Mu Us Desert. The results showed that changes in soil temperatures and temperature gradients were largest in soil layers above the 100-cm depth, and variations decreased with soil depth. The relationship between soil temperature and unfrozen water content can be depicted well by both theoretical and empirical models. Due to gradients of the matric potential and temperature, soil water flowed from deeper soil layers towards the frozen soil, increasing the total water content at the freezing front. The vapor flux, which was affected mainly by temperature, showed diurnal variations in the shallow 20-cm soil layer, and its rate and variations decreased gradually with increasing soil depths. The freeze-thaw process can be divided into three stages: the initial freezing stage, the downward freezing stage, and the thawing stage. The upward vapor flux contributed to the formation of the frozen layer during the freezing process.

Highlights

Regions with frozen soil are widely distributed in middle and high latitudes, affecting approximately 50% of the land around the world [1,2]
According to the measured soil temperature and moisture data, the total freeze-thaw process, with the maximum freezing depth to be at a depth of
Based on in-situ observations in the Mu Us Desert, the changes in soil temperatures and water contents during the freeze-thaw period were studied in this manuscript

Summary

Introduction

Regions with frozen soil are widely distributed in middle and high latitudes, affecting approximately 50% of the land around the world [1,2] Soils in these regions will freeze or thaw in response to variations in soil temperatures, resulting in the phase change of soil water among ice, liquid water, and water vapor [3,4,5]. The freeze-thaw process has a substantial impact on the surface energy balance and soil moisture distribution, significantly affecting soil properties, such as soil structure, permeability, conductivity, and bulk density, making it difficult and complicated to study water flow, heat transport, and related parameters in seasonally frozen soils [9,10,11]. Physical properties of frozen soil in cold regions are strongly dependent on temperature when unfrozen water is present, and both unfrozen water and soil temperature control the freeze-thaw process and soil water migration [2,14,15]

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