从单峰粒度分布和孔隙比估计沙土土-水特征曲线族

IF 5.9 1区 地球科学 Q1 ENGINEERING, CIVIL
Siqi Zhang , Daoyuan Tan , Honghu Zhu , Chao Zhou
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引用次数: 0

摘要

土壤-水特征曲线(swcc)是含水量值与土壤吸力的关系曲线,反映了自然土壤的滞回性。在岩土工程和水文学中,准确、高效地估算swcc是必不可少的。本文旨在建立一个综合模型,利用单峰粒度分布(GSD)准确估计沙质土壤中swcc族。首先,将基于物理的MV模型与统计估计相结合,建立了一种改进的模型来预测初始干燥SWCC。该模型明确量化了土壤均匀性和残余含水量对基于GSD估算的SWCC的影响。其次,通过引入残余空气含量、接触角滞后和“墨瓶”效应,进一步发展模型,从估计的干燥曲线预测主润湿曲线。对任意给定的过渡点进行了干湿扫描曲线的预测。然后,通过与不同砂质土试验数据的对比、交叉验证、敏感性分析和不确定度量化,对模型的性能进行了评价。结果表明,与经典模型相比,该模型具有更高的精度和方便性。它为广泛的沙质土壤(从砾石到粘土)提供了整个swcc家族的可靠预测。最后,讨论了该模型在其他领域的应用前景和局限性。该模型还显示了扩展到各种土壤类型的潜力,包括间隙级配土壤、细粒土壤和含有机质土壤。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Estimating family of soil–water characteristic curves for sandy soils from unimodal grain size distribution and void ratio
Soil-water characteristic curves (SWCCs) are a family of water content values versus soil suction, illustrating the hysteresis in natural soil. The accurate and efficient estimation of SWCCs is indispensable in geotechnical engineering and hydrology. This paper aims to develop a comprehensive model for accurately estimating the family of SWCCs for sandy soils using their unimodal grain size distribution (GSD). First, an improved model is developed by combining the physical-based MV model with statistical estimation to predict the initial drying SWCC. This model explicitly quantified the effects of soil uniformity and residual water content on estimated SWCC based on GSD. Second, the model is further developed to predict the main wetting curve from the estimated drying curve by introducing residual air content, contact angle hysteresis, and “ink bottle” effects. The drying and wetting scanning curves are predicted for any given transition point. Then, the model’s performance is evaluated through comparison with experimental data from various sandy soils, cross-validation, sensitivity analysis, and uncertainty quantification. Results show that the model stands out for its superior accuracy and convenience compared to classical models. It provides reliable predictions of the entire family of SWCCs for a wide range of sandy soils, from gravelly to clayey sand. Finally, the potential application in other fields and limitations of the model are discussed. The model also demonstrates the potential to be extended to various soil types, including gap-graded soils, fine-grained soils, and soils with organic matter.
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来源期刊
Journal of Hydrology
Journal of Hydrology 地学-地球科学综合
CiteScore
11.00
自引率
12.50%
发文量
1309
审稿时长
7.5 months
期刊介绍: The Journal of Hydrology publishes original research papers and comprehensive reviews in all the subfields of the hydrological sciences including water based management and policy issues that impact on economics and society. These comprise, but are not limited to the physical, chemical, biogeochemical, stochastic and systems aspects of surface and groundwater hydrology, hydrometeorology and hydrogeology. Relevant topics incorporating the insights and methodologies of disciplines such as climatology, water resource systems, hydraulics, agrohydrology, geomorphology, soil science, instrumentation and remote sensing, civil and environmental engineering are included. Social science perspectives on hydrological problems such as resource and ecological economics, environmental sociology, psychology and behavioural science, management and policy analysis are also invited. Multi-and interdisciplinary analyses of hydrological problems are within scope. The science published in the Journal of Hydrology is relevant to catchment scales rather than exclusively to a local scale or site.
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