The Application and Improvement of Soil–Water Characteristic Curves through In Situ Monitoring Data in the Plains

In order to study the soil–water characteristic curve and soil–water movement in the unsaturated zone of the humid plain area and investigate its influence on the regional water cycle process, this study conducted a long series of hydrometeorological data monitoring on the whole process of precipita...

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Main Authors: Pingnan Zhang, Gang Chen, Jinning Wu, Chuanhai Wang, Shiwei Zheng, Yue Yu, Youlin Li, Xiaoning Li
Format: Article
Language:English
Published: MDPI AG 2022-12-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/14/24/4012
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author Pingnan Zhang
Gang Chen
Jinning Wu
Chuanhai Wang
Shiwei Zheng
Yue Yu
Youlin Li
Xiaoning Li
author_facet Pingnan Zhang
Gang Chen
Jinning Wu
Chuanhai Wang
Shiwei Zheng
Yue Yu
Youlin Li
Xiaoning Li
author_sort Pingnan Zhang
collection DOAJ
description In order to study the soil–water characteristic curve and soil–water movement in the unsaturated zone of the humid plain area and investigate its influence on the regional water cycle process, this study conducted a long series of hydrometeorological data monitoring on the whole process of precipitation, evaporation, soil water content, pore water pressure and depth of groundwater level at the Jintan field hydrological test in the plain area of the Taihu Basin, China. Based on the collected data, the soil water dynamic at different depths was analyzed, and the results showed that the soil water fluctuated most frequently and drastically at a soil horizon depth of 0–40 cm, with an obvious soil moisture wetting and drying cycle. The van Genuchten model (VG model) was used to describe the soil–water characteristic curve, and the parameters of the VG model were obtained by numerical inversion of field monitoring data using numerical code (HYDRUS-1D). The obtained parameters were used to simulate soil water movement in each soil horizon for six precipitation events and were compared with the simulation results of laboratory data. The study shows that the soil water simulation based on field data is better, which verifies the accuracy and reliability of the VG model obtained from field observation and provides a reliable theoretical basis for soil water movement and the calculation of runoff yield in the plain area of the Taihu Basin.
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spelling doaj.art-4c3e370b89cc4f23b45d7b8c108911712023-11-24T18:41:20ZengMDPI AGWater2073-44412022-12-011424401210.3390/w14244012The Application and Improvement of Soil–Water Characteristic Curves through In Situ Monitoring Data in the PlainsPingnan Zhang0Gang Chen1Jinning Wu2Chuanhai Wang3Shiwei Zheng4Yue Yu5Youlin Li6Xiaoning Li7College of Hydrology and Water Resources, Hohai University, Nanjing 210098, ChinaCollege of Hydrology and Water Resources, Hohai University, Nanjing 210098, ChinaChangzhou Branch of Jiangsu Province Hydrology and Water Resources Survey Bureau, Changzhou 213022, ChinaCollege of Hydrology and Water Resources, Hohai University, Nanjing 210098, ChinaCollege of Hydrology and Water Resources, Hohai University, Nanjing 210098, ChinaCollege of Hydrology and Water Resources, Hohai University, Nanjing 210098, ChinaCollege of Hydrology and Water Resources, Hohai University, Nanjing 210098, ChinaCollege of Hydrology and Water Resources, Hohai University, Nanjing 210098, ChinaIn order to study the soil–water characteristic curve and soil–water movement in the unsaturated zone of the humid plain area and investigate its influence on the regional water cycle process, this study conducted a long series of hydrometeorological data monitoring on the whole process of precipitation, evaporation, soil water content, pore water pressure and depth of groundwater level at the Jintan field hydrological test in the plain area of the Taihu Basin, China. Based on the collected data, the soil water dynamic at different depths was analyzed, and the results showed that the soil water fluctuated most frequently and drastically at a soil horizon depth of 0–40 cm, with an obvious soil moisture wetting and drying cycle. The van Genuchten model (VG model) was used to describe the soil–water characteristic curve, and the parameters of the VG model were obtained by numerical inversion of field monitoring data using numerical code (HYDRUS-1D). The obtained parameters were used to simulate soil water movement in each soil horizon for six precipitation events and were compared with the simulation results of laboratory data. The study shows that the soil water simulation based on field data is better, which verifies the accuracy and reliability of the VG model obtained from field observation and provides a reliable theoretical basis for soil water movement and the calculation of runoff yield in the plain area of the Taihu Basin.https://www.mdpi.com/2073-4441/14/24/4012soil–water characteristic curve (SWCC)wetting and drying cyclenumerical inversionsoil water movementprecipitation event simulationplain area
spellingShingle Pingnan Zhang
Gang Chen
Jinning Wu
Chuanhai Wang
Shiwei Zheng
Yue Yu
Youlin Li
Xiaoning Li
The Application and Improvement of Soil–Water Characteristic Curves through In Situ Monitoring Data in the Plains
Water
soil–water characteristic curve (SWCC)
wetting and drying cycle
numerical inversion
soil water movement
precipitation event simulation
plain area
title The Application and Improvement of Soil–Water Characteristic Curves through In Situ Monitoring Data in the Plains
title_full The Application and Improvement of Soil–Water Characteristic Curves through In Situ Monitoring Data in the Plains
title_fullStr The Application and Improvement of Soil–Water Characteristic Curves through In Situ Monitoring Data in the Plains
title_full_unstemmed The Application and Improvement of Soil–Water Characteristic Curves through In Situ Monitoring Data in the Plains
title_short The Application and Improvement of Soil–Water Characteristic Curves through In Situ Monitoring Data in the Plains
title_sort application and improvement of soil water characteristic curves through in situ monitoring data in the plains
topic soil–water characteristic curve (SWCC)
wetting and drying cycle
numerical inversion
soil water movement
precipitation event simulation
plain area
url https://www.mdpi.com/2073-4441/14/24/4012
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