SWAP 50 years: Advances in modelling soil-water-atmosphere-plant interactions

IF 5.9 1区 农林科学 Q1 AGRONOMY Agricultural Water Management Pub Date : 2024-05-17 DOI:10.1016/j.agwat.2024.108883
Marius Heinen , Martin Mulder , Jos van Dam , Ruud Bartholomeus , Quirijn de Jong van Lier , Janine de Wit , Allard de Wit , Mirjam Hack - ten Broeke
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Abstract

This paper highlights the evolution and impact of the SWAP model (Soil – Water – Atmosphere – Plant), which was initiated by R.A. Feddes and colleagues fifty years ago, in 1974. Since then, the SWAP model has played a crucial role in the advancement of agrohydrology. This paper highlights some major advances that have been made, especially focussing on the last fifteen years. The domain of the SWAP model deals with the simulation of the soil water balance in both unsaturated and saturated conditions. The model solves the Richards equation using the water retention and hydraulic conductivity functions as described by the Van Genuchten – Mualem equations. Bimodal extensions of the Van Genuchten - Mualem relationships have been implemented, as well as modifications near saturation and addressing hysteresis. An important sink term in the Richards equation is root water uptake. Crop development plays an important role in a robust simulation of root water uptake. That is why a link has been made with the dynamic crop growth model WOFOST. Instead of using a prescribed crop development, a distinction between potential and actual crop development is calculated by reducing the potential photosynthesis as a result of water or oxygen stress. Since the early days of SWAP, empirical and macroscopic concepts have been used to simulate root water uptake. Recently two process-based concepts of root water uptake and oxygen stress have also been implemented. Another important sink-source term in the Richards equation is the interaction with artificial drains. In SWAP, drainage can be simulated by either using prescribed or simulated drain heads and simulation of controlled drainage with subirrigation is possible. Finally, we briefly elaborate on three studies using SWAP: water stresses in agriculture in the Netherlands, regional water productivity in China, and controlled drainage with subirrigation. We finish discussing promising developments for the near future.

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SWAP 50 周年:土壤-水-大气-植物相互作用建模的进展
本文重点介绍了五十年前(1974 年)由 R.A. Feddes 及其同事提出的 SWAP 模型(土壤-水-大气-植物)的演变和影响。从那时起,SWAP 模型在农业水文学的发展中发挥了至关重要的作用。本文重点介绍了该模型取得的一些重大进展,尤其是在过去 15 年中取得的进展。SWAP 模型的领域是模拟非饱和和饱和条件下的土壤水分平衡。该模型利用 Van Genuchten - Mualem 方程所描述的水分保持和水力传导函数来求解理查兹方程。对 Van Genuchten - Mualem 关系进行了双模扩展,并在接近饱和时进行了修改,以解决滞后问题。理查兹方程中的一个重要汇项是根系吸水。作物生长对根系吸水的稳健模拟起着重要作用。因此,我们将其与动态作物生长模型 WOFOST 相结合。该模型不使用规定的作物生长情况,而是通过减少水分或氧气胁迫导致的潜在光合作用来计算潜在和实际作物生长情况之间的区别。自 SWAP 推出之初,就一直使用经验和宏观概念来模拟根系吸水。最近,还采用了根系吸水和氧胁迫这两个基于过程的概念。理查兹方程中另一个重要的汇源项是与人工排水系统的相互作用。在 SWAP 中,可以使用规定的或模拟的排水沟头来模拟排水,还可以通过灌溉来模拟受控排水。最后,我们简要阐述了使用 SWAP 进行的三项研究:荷兰农业用水压力、中国区域水生产力和灌溉控制排水。最后,我们讨论了不久的将来的发展前景。
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来源期刊
Agricultural Water Management
Agricultural Water Management 农林科学-农艺学
CiteScore
12.10
自引率
14.90%
发文量
648
审稿时长
4.9 months
期刊介绍: Agricultural Water Management publishes papers of international significance relating to the science, economics, and policy of agricultural water management. In all cases, manuscripts must address implications and provide insight regarding agricultural water management.
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