基于Kostiakov-Lewis模型的植被覆盖与非植被覆盖间土壤水分入渗速率转换

IF 0.9 Q4 WATER RESOURCES
N. O. Vieira, D. A. Zanoni, G. A. Carvalho, J. A. Anache, P. T. S. Oliveira, T. A. Sobrinho
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引用次数: 1

摘要

土壤水分渗透速率对于水文研究、灌溉和排水系统的规划和设计以及其他应用至关重要。在有植被覆盖和没有植被覆盖的样地进行了各种研究,旨在确定植被覆盖对土壤水分入渗过程的影响。然而,一些工作已经解决了有植被覆盖和没有植被覆盖地块的入渗率之间的关系。在这里,我们研究了有和没有植被覆盖的入渗率之间的迭代能力,试图确定潜在的相关性。我们提出了一个创新且易于使用的经验模型,该模型允许将有植被覆盖的系统中的入渗率转换为没有植被覆盖的系统的入渗率,反之亦然。总共使用了142个降雨模拟实验数据集,包括6种不同类型的土壤和18种不同类型的土地覆盖和管理。该模型基于Kostiakov-Lewis模型,具有与其他入渗模型相似的性能,适用于多种种植和植被覆盖系统。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Conversion of soil water infiltration rates between vegetated and non-vegetated land covers by using the Kostiakov-Lewis model
ABSTRACT Soil water infiltration rates are essential for hydrological studies, planning and design of irrigation and drainage systems, among other applications. Various studies have been carried out in plots with and without vegetation cover, aiming to identify the influence of the cover on the water infiltration process in soil. However, a few works have addressed the relationship between infiltration rates of a plot with and without vegetation cover. Here we investigated the ability to iterate between infiltration rates with and without vegetation cover, seeking to identify potential correlations. We propose an innovative and easy-to-use empirical model that allows the conversion of infiltration rates in systems with vegetation cover into infiltration rates without coverage and vice versa. Altogether, we used a dataset comprising 142 rainfall simulation experiments under plots with and without cover, including 6 different types of soil and 18 types of land cover and management. The proposed model was based on the Kostiakov-Lewis model, presenting performance similar to other infiltration models, which is effective in a variety of planting and vegetation cover systems.
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来源期刊
CiteScore
1.60
自引率
12.50%
发文量
18
审稿时长
16 weeks
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