Empirical modeling of streambed hydraulic conductivity in ephemeral rivers: Insights from sediment characteristics in arid environments

IF 2.8 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Ehsan Karrabi, Mohammad Reza Majdzadeh Tabatabai
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Abstract

This study presents a pioneering investigation into the relationships between vertical hydraulic conductivity (Kv) and sediment properties through an extensive field measurement of 15 ephemeral sandy-bed rivers in Razavi Khorasan province, Iran. A robust dataset comprising 300 in situ Kv measurements and grain size analyses was collected from 2019 to 2022, including both main channel and bar morphological units. Statistical analyses, such as coefficient of variation and skewness, revealed significant deviations from normality in the data distributions, particularly pronounced for bar samples, emphasizing the limitations of conventional statistical frameworks based on normality assumptions. Applying nonparametric techniques of Kruskal–Wallis and Mann–Whitney, the study uncovered strong interdependencies between Kv and key sediment descriptors, including armor ratio, mud percentage, and grain size (d10). Notably, main channel data indicated a stronger tendency towards normality relative to the bar data, reflecting the inherent disparities in sediment dynamics and hydrologic regimes across these various morphological units. The data samples were randomly split into two groups: 70% for calibration and 30% for validation to develop a novel empirical model, explicitly incorporating the interdependent effects of armor ratio, mud percentage, and d10 on Kv. On the 70% calibration set, R2 and RMSE were calculated to evaluate model fit. On the 30% validation set, RMSE was calculated to evaluate predictive accuracy. Thereafter, the validated data were used to assess performance of the adopted model. The model is meant for a specific range of sediment characteristics, including uniformity coefficients (5.2 < Uc < 141), characteristic grain sizes (0.05 mm < d10 < 0.62 mm), mud percentages (0.01 < mp < 7.2), and armor ratios (0.9 < Ar < 6.2), which are particularly relevant in ephemeral rivers. Finally, the proposed model yielded results outperform those of several widely adopted empirical models, reflecting the effect of mud percentage and armor ratio to provide accurate prediction of the Kv within the scope of this study.

Abstract Image

短期河流河床水力传导性的经验模型:来自干旱环境中沉积物特征的见解
本研究通过对伊朗拉扎维呼罗珊省15条短暂砂床河流的广泛实地测量,对垂直水力传导率(Kv)与沉积物特性之间的关系进行了开创性的调查。从2019年到2022年,收集了300 Kv原位测量和粒度分析的强大数据集,包括主河道和沙洲形态单元。统计分析,如变异系数和偏度,揭示了数据分布中与正态性的显著偏差,尤其是条形样本,强调了基于正态性假设的传统统计框架的局限性。应用Kruskal-Wallis和Mann-Whitney的非参数技术,该研究发现Kv和关键沉积物描述符之间存在很强的相互依赖性,包括装甲比、泥浆百分比和粒度(d10)。值得注意的是,与沙洲数据相比,主河道数据显示出更强的正态性趋势,反映了这些不同形态单元之间泥沙动力学和水文制度的内在差异。数据样本随机分为两组:70%用于校准,30%用于验证,以开发新的经验模型,明确纳入装甲比,泥浆百分比和d10对Kv的相互影响。在70%的校正集上,计算R2和RMSE来评估模型的拟合。在30%的验证集上,计算RMSE来评估预测的准确性。然后,使用验证后的数据来评估所采用模型的性能。该模型适用于沉积物特征的特定范围,包括均匀性系数(5.2 < Uc < 141),特征粒度(0.05 mm < d10 < 0.62 mm),泥浆百分比(0.01 < mp < 7.2)和护甲比(0.9 < Ar < 6.2),这些与短暂河流特别相关。最后,该模型的结果优于几种广泛采用的经验模型,反映了泥浆百分比和装甲比的影响,为本研究范围内的Kv提供了准确的预测。
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来源期刊
Earth Surface Processes and Landforms
Earth Surface Processes and Landforms 地学-地球科学综合
CiteScore
6.40
自引率
12.10%
发文量
215
审稿时长
4 months
期刊介绍: Earth Surface Processes and Landforms is an interdisciplinary international journal concerned with: the interactions between surface processes and landforms and landscapes; that lead to physical, chemical and biological changes; and which in turn create; current landscapes and the geological record of past landscapes. Its focus is core to both physical geographical and geological communities, and also the wider geosciences
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