Evidence map›Paper›PMID 27126870›Full record

ArticleEnvironmental science and pollution research international2016

Simplified continuous simulation model for investigating effects of controlled drainage on long-term soil moisture dynamics with a shallow groundwater table.

Huaiwei Sun, Juxiu Tong, Wenbing Luo, Xiugui Wang, Jinzhong Yang

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Article in Environmental science and pollution research international, 2016. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

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5 · Who and what money

Authors and funding

5 authors.

Huaiwei SunSchool of hydropower and information engineering, Huazhong University of Science & Technology, Wuhan, 430074, China. huaiweisun@whu.edu.cn.
Juxiu TongKey Laboratory of Groundwater Circulation and Evolution, Ministry of Education, China University of Geosciences, Beijing, 100083, China.
Wenbing LuoState Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University, Wuhan, 430072, China.
Xiugui WangInstitute of agricultural water conservancy, The Yangtze River academy of Sciences, Wuhan, 430010, China.
Jinzhong YangInstitute of agricultural water conservancy, The Yangtze River academy of Sciences, Wuhan, 430010, China.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Accurate modeling of soil water content is required for a reasonable prediction of crop yield and of agrochemical leaching in the field. However, complex mathematical models faced the difficult-to-calibrate parameters and the distinct knowledge between the developers and users. In this study, a deterministic model is presented and is used to investigate the effects of controlled drainage on soil moisture dynamics in a shallow groundwater area. This simplified one-dimensional model is formulated to simulate soil moisture in the field on a daily basis and takes into account only the vertical hydrological processes. A linear assumption is proposed and is used to calculate the capillary rise from the groundwater. The pipe drainage volume is calculated by using a steady-state approximation method and the leakage rate is calculated as a function of soil moisture. The model is successfully calibrated by using field experiment data from four different pipe drainage treatments with several field observations. The model was validated by comparing the simulations with observed soil water content during the experimental seasons. The comparison results demonstrated the robustness and effectiveness of the model in the prediction of average soil moisture values. The input data required to run the model are widely available and can be measured easily in the field. It is observed that controlled drainage results in lower groundwater contribution to the root zone and lower depth of percolation to the groundwater, thus helping in the maintenance of a low level of soil salinity in the root zone.

Indexed as

AgrochemicalsCalibrationGroundwaterModels, TheoreticalSalinitySoilWaterWater Pollutants, ChemicalAgrochemicalsSoilWaterWater Pollutants, ChemicalCapillary riseControlled drainageDeep percolationShallow groundwater levelSoil moisture balance

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Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.