两种冲积土中阿特拉津迁移率的实测与模拟比较

D. Persicani, P. Siro, G. Gasparetti, M. Bonvini
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引用次数: 7

摘要

1989年3月28日,在沙质壤土“典型Fluvaquent”和粉质壤土“典型udifluent”上以每年1.4 kg公顷- 1的速度施用阿特拉津。1个月后,在60 cm深度取土样,测定阿特拉津浓度。在两种土壤中测量到相似的浓度。利用基于物理的模型(HYDRUS)模拟了阿特拉津的迁移。分析表明,HYDRUS预测了阿特拉津的迁移率。模型对吸附、降解和水力参数的敏感性分析表明,吸附参数在模拟过程中最相关。通过用最佳拟合的Kd值校准模型,模型预测得到了明显改善。
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Comparison of measured and simulated atrazine mobility in two alluvial soils

Atrazine was applied on a sandy loam, Typic Fluvaquent and a silty loam, Typic Udifluvent at a 1.4 kg ha−1 a.i. rate on March 28, 1989. One month later, soil samples were taken at a 60 cm depth for measurement of the atrazine concentration. Similar concentrations were measured in the two soils. The atrazine transport was also simulated by using a physically-based model (HYDRUS). Analyses showed that HYDRUS predicted the atrazine mobility. A sensitivity analysis of the model with respect to sorption, degradation and hydraulic parameters showed that the sorption one was the most relevant in the simulation process. By calibrating the model with the best-fitted Kd value, the model predictions were appreciably improved.

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