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缩尺效应对粗颗粒土静止侧压力系数影响规律试验
引用本文:蒋明杰,朱俊高,张小勇,梅国雄,赵辰洋.缩尺效应对粗颗粒土静止侧压力系数影响规律试验[J].四川大学学报(工程科学版),2023,55(2):259-266.
作者姓名:蒋明杰  朱俊高  张小勇  梅国雄  赵辰洋
作者单位:广西大学 工程防灾与结构安全教育部重点实验室,河海大学 岩土力学与堤坝工程教育部重点实验室,广西大学 工程防灾与结构安全教育部重点实验室,广西大学 工程防灾与结构安全教育部重点实验室,中山大学 广东省海洋土木工程重点实验室
基金项目:国家自然科学基金(No.51878185,No.52178321,No.52108309);国家自然科学基金委员会-雅砻江流域水电开发有限公司雅砻江联合基金(No.U1865104);长江水科学研究联合基金重点支持项目(No.U2040221);广西防灾减灾与工程安全重点实验室开放基金资助项目(No.2020ZDK003);广东省海洋土木工程重点实验室开放基金资助项目(No.LMCE202103)。
摘    要:准确把握粗颗粒土静止侧压力系数K0对分析以及设计土石坝等岩土工程有十分重要的作用。由于缩尺效应的存在,室内试验结果往往无法正确反映原级配粗颗粒土静止侧压力系数。为研究分析缩尺效应对粗颗粒土静止侧压力系数影响规律,找出消除其影响的方法,利用自行研制的大型K0测试仪对某砂卵砾石料及堆石料进行了大量K0试验。通过改变试样的颗粒最大粒径、缩尺方法,相对密实度等初始条件,研究了不同密实度条件下粗颗粒土静止侧压力系数随级配的演化规律。试验结果表明:相对密实度及缩尺方法不变时,粗颗粒土静止侧压力系数会随着颗粒最大粒径的增加而显著减小,因此,缩尺效应对粗颗粒土静止侧压力系数的影响无法忽略;缩尺方法对粗颗粒土静止侧压力系数有一定影响,相对密实度及颗粒最大粒径相同时,采用等量替代法缩尺后试样静止侧压力系数值最小,因此,采用等量替代法缩尺可减小缩尺效应对粗颗粒土静止侧压力系数的影响;相比颗粒最大粒径,相对密实度对粗粒土静止侧压力系数的影响更为显著,相对密实度越大的土样,颗粒最大粒径对粗粒土静止侧压力系数影响更明显。基于静止侧压力系数试验结果及前人的研究,建立根据室内试验结果反推现场粗颗粒土料静止侧压力系数的公式,以消除缩尺效应对粗颗粒土静止侧压力系数的影响。最后,利用K0试验结果验证了该经验公式的准确性及适用性。

关 键 词:粗颗粒土  静止侧压力系数  缩尺效应  颗粒最大粒径  缩尺方法
收稿时间:2021/11/3 0:00:00
修稿时间:2022/4/11 0:00:00

Experimental Investigation on Scale Effect of the At-rest Earth Pressure Coefficient of Coarse-grained Soil
JIANG Mingjie,ZHU Jungao,ZHANG Xiaoyong,MEI Guoxiong,ZHAO Chenyang.Experimental Investigation on Scale Effect of the At-rest Earth Pressure Coefficient of Coarse-grained Soil[J].Journal of Sichuan University (Engineering Science Edition),2023,55(2):259-266.
Authors:JIANG Mingjie  ZHU Jungao  ZHANG Xiaoyong  MEI Guoxiong  ZHAO Chenyang
Affiliation:Guangxi university,,,,
Abstract:The accurate measurement of the at-rest earth pressure coefficient K0 for coarse-grained soil is important in the analysis and design of geotechnical engineering such as the earth rockfill dam. The laboratory K0 test results of the coarse-grained soil usually cannot accurately reflect its K0 value due to scale effects. To investigate the scale effect of K0 for coarse-grained soil, and propose a method to eliminate its influence, several K0 tests for the sandy gravel and the rockfill were performed by using a special large-size K0 testing apparatus. By changing the maximum grain size dM, scale method, and relative density Dr0, 24 groups of specimens were designed. K0 tests for all specimens were conducted by a large-size K0 apparatus, to quantitatively study the multiple influences of dM, scale method and Dr0 on the K0 of coarse-grained soils, and investigate the method that can predict the K0 behavior of sandy gravel in situ based on the laboratory test results and eliminate the influence of scale effects on K0. The test data show that: when the scale method and Dr0 are the same, K0 for coarse-grained soil trend to decrease observably with increasing dM, therefore scale effect results in the obvious increasing value of K0 for coarse-grained soil, and the smaller dM for reducing scale soil, the stronger influence of scale effect on its K0; Scale method have some influence on K0 for coarse-grained soil with the same dM and Dr0, and the increasing value of K0 for test specimens prepared by replacement technique is the least, therefore adopting the replacement technique to prepare test specimen can reduce the influence of scale effect on K0 for coarse-grained soil; Compared with dM, Dr0 have a stronger influence on K0 for coarse-grained soil, and the larger Dr0, the stronger influence of dM on K0 for coarse-grained soil. Based on the K0 test data of sandy gravel and previous research results, an empire equation, which could predict the K0 behavior of sandy gravel in situ based on the laboratory test results, was proposed to eliminate the influence of scale size on K0 for coarse-grained soil. Furthermore, the accuracy and applicability of the empire equation were verified by the K0 test data of the rockfill.
Keywords:coarse grained soil  at-rest earth pressure coefficient  scale size  maximum grain size  preparation technique
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