Modelling Seasonal Variability in Parameters Defining Volumetric Water Content in a Low Permeability Soil in Central Illinois: An Application of MODFLOW-6 and the Unsaturated Zone Flow Package

IF 3.2 3区 地球科学 Q1 Environmental Science Hydrological Processes Pub Date : 2024-11-26 DOI:10.1002/hyp.70007
Michael P. Krasowski, Esra Gulsen, Allan E. Jones, Daniel B. Abrams
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Abstract

Increasing interest in solute transport phenomena in agricultural systems on a sub-annual basis necessitates a better understanding of seasonal changes in natural systems and how these changes can be incorporated into modelling. A better understanding of the seasonal timing of nutrient loading in tile drained agricultural systems in particular is essential for efforts trying to replicate or predict the occurrence of harmful algal blooms. Literature exists showing there are seasonal dynamics (freeze–thaw, plant-root processes, land management practices, etc.) that may cause changes in the hydraulic properties of the soil zone including hydraulic conductivity and porosity. To test whether these changes are important in an agricultural system, a MODFLOW-6 model using the unsaturated zone flow package was constructed. The simulation was comprised of separate, seasonal models to be run sequentially with each year being broken into a winter and summer seasons. As part of this architecture, model parameters representing soil hydraulic properties were allowed to vary by season. The model was calibrated against soil moisture observations at multiple depths using a genetic algorithm machine learning technique. The parameters of the sub-models were compared for the winter and summer seasons. Brook-Corey epsilon, saturated vertical conductivity, saturated volumetric water content and residual volumetric water content were found to be consistently different between the modelled summer and winter periods. A more traditional model which did not allow hydraulic properties to vary seasonally was also run and compared to the seasonal architecture and the seasonal architecture was found to improve simulation results. The hydrologic dynamics of the unsaturated zone—particularly in tile drained agricultural systems—control the residence time for water and solutes, which is critical for in-field chemical processes such as denitrification. This work has important implications for seasonal transport phenomena in agricultural systems and improving the simulation and prediction of harmful algal blooms.

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伊利诺伊州中部低渗透性土壤体积含水量定义参数的季节变化建模:MODFLOW-6 和非饱和区流软件包的应用
由于人们对农业系统中一年以下的溶质迁移现象越来越感兴趣,因此有必要更好地了解自然系统的季节变化以及如何将这些变化纳入建模。更好地了解瓦片排水农业系统中养分负荷的季节性时间安排,对于复制或预测有害藻华的发生至关重要。现有文献表明,季节性动态(冻融、植物根系过程、土地管理方法等)可能会导致土壤区域的水力特性(包括水力传导性和孔隙度)发生变化。为了测试这些变化在农业系统中是否重要,使用非饱和带流量包构建了 MODFLOW-6 模型。该模拟由独立的季节性模型组成,每年分为冬夏两季依次运行。作为该结构的一部分,代表土壤水力特性的模型参数可随季节变化。利用遗传算法机器学习技术,根据多个深度的土壤水分观测结果对模型进行校准。对冬季和夏季的子模型参数进行了比较。结果发现,在模拟的夏季和冬季期间,Brook-Corey epsilon、饱和垂直传导率、饱和容积含水量和残余容积含水量始终存在差异。还运行了一个不允许水力特性随季节变化的更传统的模型,并与季节性结构进行了比较,发现季节性结构改善了模拟结果。非饱和带的水文动态--尤其是在瓦片排水农业系统中--控制着水和溶质的停留时间,这对反硝化等田间化学过程至关重要。这项工作对农业系统中的季节性迁移现象以及改善有害藻华的模拟和预测具有重要意义。
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来源期刊
Hydrological Processes
Hydrological Processes 环境科学-水资源
CiteScore
6.00
自引率
12.50%
发文量
313
审稿时长
2-4 weeks
期刊介绍: Hydrological Processes is an international journal that publishes original scientific papers advancing understanding of the mechanisms underlying the movement and storage of water in the environment, and the interaction of water with geological, biogeochemical, atmospheric and ecological systems. Not all papers related to water resources are appropriate for submission to this journal; rather we seek papers that clearly articulate the role(s) of hydrological processes.
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Issue Information Modelling Seasonal Variability in Parameters Defining Volumetric Water Content in a Low Permeability Soil in Central Illinois: An Application of MODFLOW-6 and the Unsaturated Zone Flow Package Snow Depth Distribution in Canopy Gaps in Central Pyrenees Microscopic Mechanism of Particle Clogging in Porous Media During Managed Aquifer Recharge: From X-Ray Computed Tomography (CT) Imaging to Numerical Modelling Quantifying Hydraulic Geometry and Whitewater Coverage for Steep Proglacial Streams to Support Process-Based Stream Temperature Modelling
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