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山体地区花岗岩风化层标贯击数衰减的岩土性状判定与工程验证分析

Geotechnical Behavior Assessment and Engineering Verification Analysis of SPT N-value Attenuation in Weathered Granite Strata of Mountainous Regions

  • 摘要: 广东地区现行规范中花岗岩风化层的定名依据是标贯实测击数。然而,对于山体地区,采用实测标贯击数划分地层会引起定名争议。本研究解决了山体开挖前后花岗岩风化层因标贯击数显著衰减引发的岩土定名争议。通过系统性因素分析,揭示了试验条件变异是标贯击数衰减的主导机制。静载试验与标贯试验数据表明,开挖后地基承载力(特征值500 kPa)与勘察报告参数高度吻合。这一结果证实,可直接采用既定岩土参数进行工程验收。针对现行规范中花岗岩地层单一指标(标贯实测击数)定名体系的局限性,创新性提出通过现场荷载试验对花岗岩风化层岩土定名(性状)进行动态标定的方法。该方法成功构建了花岗岩风化地层“勘察-设计-验证”全链条技术范式,为山体地区花岗岩风化层地基验收提供了可迁移解决方案。

     

    Abstract: The current regulations in Guangdong region stipulate that the naming of weathered granite layers is based on the measured number of standard penetration blows. However, for mountainous areas, using measured standard penetration counts to divide strata can cause naming disputes. This study resolves the geotechnical designation disputes caused by significant attenuation of Standard Penetration Test (SPT) N-values in weathered granite layers during pre- and post-excavation phases in mountainous regions. Through systematic causal analysis, the research identifies variability in testing conditions as the dominant mechanism driving SPT N-value attenuation. The static load test and standard penetration test data indicate that the bearing capacity of the excavated foundation (characteristic value of 500 kPa) is highly consistent with the parameters in the survey report. This result confirms that the established geotechnical parameters can be directly used for engineering acceptance.Addressing the limitations of the current single-index classification system (solely based on in-situ SPT N-values) for granite formations, this study innovatively proposes a dynamic calibration methodology that integrates field load tests to refine the geotechnical designation and behavioral characterization of weathered granite strata. The developed approach establishes a comprehensive "investigation-design-verification" technical framework, providing transferable solutions for foundation acceptance of weathered granite layers in mountainous areas.

     

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