Study of the effect of the compaction level on the hydrodynamic properties of loamy sand soil in an agricultural context

IF 2.6 Q2 WATER RESOURCES Frontiers in Water Pub Date : 2023-10-25 DOI:10.3389/frwa.2023.1255495
Yasmin Mbarki, Silvio José Gumiere, Paul Celicourt, Jhemson Brédy
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Abstract

Agricultural soil compaction adversely affects crop water use and yield performance and should be avoided or remediated through appropriate soil management strategies. The investigation of the impact of different levels of soil compaction on its hydrodynamic properties remains a crucial step in improving water use and crop yields. We examined five compaction levels of silty sand soil sampled from a potato field in the agricultural regions of northern Quebec (Canada). Soil hydraulic characteristics (saturated and unsaturated hydraulic conductivity, soil water retention capacity) were measured using the constant head method, the HYPROP device, and a WP4C dew point potentiometer. The sixteen hydraulic models integrated into the HYPROP software were fitted to the soil water retention curve (SWRC) data for the studied compaction levels. Statistical parameters such as the mean bias error, mean absolute error, correlation coefficient, and root mean square error were used to measure the performance of the models. The results show that saturated and unsaturated conductivity decreases with increasing soil compaction. The lowest saturated hydraulic conductivity (Ks) value is observed for the highest level of soil compaction, reflecting a solid medium with less pore space and connectivity. Among the hydraulic models, the Peters-Durner-Iden (PDI) variant of van Genuchten's unconstrained bimodal model (VGm-b-PDI) outperformed all other models for SWRC simulation of different soil compaction levels and was, accordingly, selected as the optimal model. This model was implemented in HYDRUS-1D to estimate the amount of irrigation for different compaction levels. We simulated irrigation scenarios with the dual-porosity model. The results indicated that soil compaction can strongly influence soil hydraulic properties and water differently. However, the amount of irrigation for the potato crop was optimal at a moderate level of soil compaction. Overall, combined HYPROP and HYDRUS 1D can provide helpful information on the soil hydraulics properties dynamics and a rigorous simulation for irrigation planning and management in potato fields.
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农业环境下压实程度对壤土砂土水动力特性影响的研究
农业土壤压实对作物水分利用和产量表现有不利影响,应通过适当的土壤管理策略加以避免或补救。研究不同程度的土壤压实对其水动力特性的影响仍然是改善水分利用和作物产量的关键步骤。我们检查了从魁北克北部农业区(加拿大)的马铃薯田取样的粉砂质土壤的五个压实水平。采用恒水头法、HYPROP装置和WP4C露点电位器测量土壤水力特性(饱和和非饱和导电性、土壤保水能力)。将集成到HYPROP软件中的16个水力模型与所研究的压实水平的土壤保水曲线(SWRC)数据拟合。使用平均偏置误差、平均绝对误差、相关系数和均方根误差等统计参数来衡量模型的性能。结果表明,饱和和非饱和电导率随土壤压实度的增加而减小。土壤压实程度最高时,饱和水导率(Ks)值最低,反映了孔隙空间和连通性较少的固体介质。在水力模型中,van Genuchten的无约束双峰模型(VGm-b-PDI)的Peters-Durner-Iden (PDI)变异体在不同土壤压实水平下的SWRC模拟效果优于其他所有模型,因此被选为最优模型。该模型在HYDRUS-1D中实现,用于估算不同压实水平下的灌溉量。我们用双重孔隙度模型模拟灌溉情景。结果表明,土壤压实对土壤水力学性质和水分有不同程度的影响。然而,在中等土壤压实水平下,马铃薯作物的灌溉量是最佳的。总的来说,HYPROP和HYDRUS 1D的结合可以为马铃薯田的灌溉规划和管理提供有用的土壤水力学特性动态信息和严格的模拟。
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来源期刊
Frontiers in Water
Frontiers in Water WATER RESOURCES-
CiteScore
4.00
自引率
6.90%
发文量
224
审稿时长
13 weeks
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