首页|高围压状态下堆石料湿化变形特性

高围压状态下堆石料湿化变形特性

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堆石料是土石坝的主要填筑材料,其湿化变形特性对土石坝蓄水期变形有显著影响.对两河口水电站的2种筑坝堆石料,采用单线法分别开展围压为0.5、1.0、2.0、3.0 MPa的大型三轴湿化变形试验.结果表明:随着应力水平和围压增加,堆石料轴向湿化变形和体积湿化变形都显著增大,与中低围压下的湿化变形规律相近.高围压下的各向等压湿化变形,堆石料体积湿化应变与围压在双对数坐标中仍服从直线关系,轴向湿化应变与围压不再满足直线关系.高围压下的偏压湿化变形,堆石料体积湿化应变与轴向湿化应变之比一般在0~2范围内,与围压呈现近似水平发展趋势,随应力水平的增加而逐渐降低.采用六参数湿化模型,仍能准确表达轴向湿化变形、体积湿化变形随应力水平、围压的变形规律.
Wetting Deformation Characteristics of Rockfill under High Stress State
Rockfill serves as the primary filling material in earth rock dams.Its wetting deformation characteristics have a significant influence on dam deformation during impoundment.Employing the single line method,we con-ducted extensive indoor triaxial wetting deformation tests under confining pressures of 0.5,1.0,2.0,and 3.0 MPa on two types of rockfill materials sourced from Lianghekou Hydropower Station.Results indicate a substantial in-crease in both axial and volumetric wetting deformations as stress levels and confining pressures escalate.This be-havior aligns with wetting deformation patterns observed under medium and low confining pressures.Notably,under high isotropic confining pressure,volumetric wetting strain correlates linearly with confining pressure in double log-arithmic coordinates,whereas axial wetting strain and confining pressure no longer meet a linear relationship.More-over,at high unsymmetrical confining pressures,the ratio of volumetric wetting strain to axial wetting strain typical-ly ranges from 0 to 2,exhibiting a nearly horizontal trend with increasing confining pressure.The six-parameter wet-ting model remains adept at accurately characterizing the axial and volumetric wetting deformation behaviors under varying stress levels and confining pressures.

rockfillwetting deformationsingle-line methodhigh confining pressure statestress level

左永振、张贵科、孙向军、潘家军、周跃峰

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长江科学院水利部岩土力学与工程重点实验室,武汉 430010

雅砻江流域水电开发有限公司,成都 610065

堆石料 湿化变形 单线法 高围压状态 应力水平

国家自然科学基金-西藏联合基金重点项目国家自然科学基金-雅砻江联合基金重点项目国家自然科学基金面上项目

U21A20158U176520351979010

2024

长江科学院院报
长江科学院

长江科学院院报

CSTPCD北大核心
影响因子:0.618
ISSN:1001-5485
年,卷(期):2024.41(4)
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