Simulation algorithm of greenhouse soil water movement based on cellular automata

IF 5.7 3区 环境科学与生态学 Q1 WATER RESOURCES
Jinjun Zhou, Tianyi Huang, Hao Wang, Ruirui Sun, Jiahong Liu, Meilin Zhou
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Abstract

Soil moisture movement reveals the hydrological environment and irrigation characteristics of plants, which is very important and basic hydrological problem. A soil moisture movement algorithm based on cellular automata suitable for greenhouse was proposed to simulate the lateral flow and vertical penetration of soil water in different soil layers. Artemisia annua was used as an experimental plant, and two numerical simulations were set up to determine the minimum water replenishment and the degree of upward soil modification. To verify the performance of the model, corn was used as an experimental plant for application simulation. The numerical simulation results show that the effect of only water for plant cells is superior to soil cells, and the disturbance behavior of the underlying soil layer should be minimized during the cultivation process. The average MAE/RMSE of all soil layers is 0.86/1.06 and in deep layer (50 cm and 60 cm) is 0.53/0.64. It shows the model has a certain prediction and simulation ability, especially in deep soil layers. The proposed algorithm can simply calculate soil flow, set the minimum water replenishment, and evaluate the water replenishment efficiency, which can provide a theoretical reference for the water replenishment and soil replacement scheme.

Abstract Image

基于细胞自动机的温室土壤水分运动模拟算法
土壤水分运动揭示了水文环境和植物灌溉特性,是非常重要和基本的水文问题。本文提出了一种基于蜂窝自动机的适合温室的土壤水分运动算法,用于模拟土壤水在不同土层中的横向流动和垂直渗透。以黄花蒿为实验植物,建立了两个数值模拟,以确定最小补水量和土壤向上改良的程度。为了验证模型的性能,以玉米为实验植物进行了应用模拟。数值模拟结果表明,只给植物细胞补水的效果优于给土壤细胞补水的效果,在栽培过程中应尽量减少对下层土壤的扰动行为。所有土层的平均 MAE/RMSE 为 0.86/1.06,深层(50 厘米和 60 厘米)为 0.53/0.64。这表明该模型具有一定的预测和模拟能力,尤其是在深土层。提出的算法可以简单计算土壤流量、设定最小补水量、评价补水效率,为补水换土方案提供理论参考。
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来源期刊
Applied Water Science
Applied Water Science WATER RESOURCES-
CiteScore
9.90
自引率
3.60%
发文量
268
审稿时长
13 weeks
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