A generalized formula for predicting soil compression index using multi-evolutionary algorithm

IF 6.9 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL
Khanh Pham , Khiem Nguyen , Kyuhyeong Lim , Younseo Kim , Hangseok Choi
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Abstract

Correlation between soil compression index (Cc) and state parameters is frequently referenced in studies investigating the fundamental mechanisms underlying changes in soil compressibility. However, developing an efficient formula for Cc that adequately captures the complexity of soil compressive behavior has been challenging for conventional approaches. This study utilized contemporary symbolic regression (SR) to propose a generalized formula for Cc that can represent the nonlinear relationships with state parameters across various soil types. A geological database from southern Vietnam was utilized to establish this data-driven formula. Data exploration revealed the apparent combined effects of moisture content (w), initial void ratio (e0), and moist density (ρ) on soil compressive behavior. Statistical indicators and graphical analysis were adopted to comprehensively assess the performance of the proposed formula against empirical equations found in the literature, aiming to gain a deeper understanding of the mechanism influencing changes in soil compressibility. The evaluation results demonstrated the efficiency of the proposed formula in predicting Cc, as evidenced by low error metrics and a good balance between precision and accuracy. Moreover, the applicability and limitations of the proposed formula were examined using different regional soils with specified geologic origins. Given its reliability and adequacy, the proposed formula explicitly quantified the nonlinear combined effects of e0, ρ and w on the compressibility of undisturbed soils. However, further research accounting for clay minerals, specimen preparation, and geologic origins is needed to enhance the universal applicability of our understanding of soil compressive behavior.
利用多进化算法预测土壤压缩指数的通用公式
在研究土壤压缩性变化的基本机制时,经常会提到土壤压缩指数(Cc)与状态参数之间的相关性。然而,对于传统方法而言,为 Cc 开发一个能充分捕捉土壤压缩行为复杂性的有效公式一直是个挑战。本研究利用当代符号回归法(SR)提出了一个通用的 Cc 公式,该公式可以表示各种土壤类型中与状态参数的非线性关系。越南南部的地质数据库被用来建立这个数据驱动的公式。数据探索显示了含水量(w)、初始空隙率(e0)和湿密度(ρ)对土壤压缩行为的明显综合影响。通过统计指标和图形分析,对照文献中的经验公式,全面评估了所提公式的性能,旨在深入了解土壤压缩性变化的影响机制。评估结果表明,所提公式预测 Cc 的效率较高,误差指标较低,精度和准确度之间的平衡较好。此外,还利用不同地区的特定地质成因土壤对所提公式的适用性和局限性进行了研究。鉴于其可靠性和充分性,所提出的公式明确量化了 e0、ρ 和 w 对未扰动土壤可压缩性的非线性综合影响。不过,还需要进一步研究粘土矿物、试样制备和地质起源,以提高我们对土壤压缩行为理解的普遍适用性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Engineering Geology
Engineering Geology 地学-地球科学综合
CiteScore
13.70
自引率
12.20%
发文量
327
审稿时长
5.6 months
期刊介绍: Engineering Geology, an international interdisciplinary journal, serves as a bridge between earth sciences and engineering, focusing on geological and geotechnical engineering. It welcomes studies with relevance to engineering, environmental concerns, and safety, catering to engineering geologists with backgrounds in geology or civil/mining engineering. Topics include applied geomorphology, structural geology, geophysics, geochemistry, environmental geology, hydrogeology, land use planning, natural hazards, remote sensing, soil and rock mechanics, and applied geotechnical engineering. The journal provides a platform for research at the intersection of geology and engineering disciplines.
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