青海盐湖区路基结构层级配及其阻盐效果  

Gradation of Subgrade Soil and Its Salt-Resistance Effect in Salt Lake Area in Qinghai

作　　者：张文 罗艳珍[3,4] 刘昕[3,4] 李斌 王珑霖[4] 杨晓旭 ZHANG Wen;LUO Yanzhen;LIU Xin;LI Bin;WANG Longlin;YANG Xiaoxu(School of civil Engineering,Qinghai University,Xining 810016,China;State Key Laboratory of Plateau Ecology and Agriculture,Qinghai University,Xining 810016,China;The Northern Qinghai-Tibet Plateau Cenozoic Laboratory of Resources and Environment,Qinghai University,Xining 810016,China;Department of Geological Engineering,Qinghai University,Xining 810016,China)

机构地区：[1]青海大学土木工程学院,青海西宁810016 [2]青海大学三江源生态与高原农牧业国家重点实验室,青海西宁810016 [3]青海大学青藏高原北缘新生代资源环境重点实验室,青海西宁810016 [4]青海大学地质工程系,青海西宁810016

出　　处：《西南交通大学学报》2020年第6期1264-1271,1296,共9页Journal of Southwest Jiaotong University

基　　金：国家自然科学基金(51468055);青海省“135高层次人才”工程基金;青海省自然科学基金(2012-Z-705)。

摘　　要：青海盐湖地区的路基工程处于隐蔽性盐风化作用强烈的寒旱岩土环境.分别采取青海茶卡盐湖地区工程建设层天然盐渍土土样和已建路基结构土层土样,研究青海盐渍土地区路基结构防护盐风化作用的效果.通过易溶盐含量测定、颗粒分析实验和毛细管水上升实验,对青海茶卡盐渍土区路基结构土层中的毛细管水上升最大高度开展理论计算.研究表明:青海茶卡地区盐渍土中毛细水上升高度大于一般土中毛细水上升高度,细粒组(0.250~0.075 mm)含量有利于水盐运移上升,粗粒组(>0.250 mm)含量不利于水盐运移上升;在水盐运移和汽盐运移双重作用下,茶卡盐渍土地区路基结构土层均出现次生盐渍化现象,建议在茶卡盐渍土地区的路基工程中,设置卵砾石阻盐隔断层的粒组级配范围控制在2.0~5.0 mm之间,该粒组含量大于75%,厚度在300.0~1000.0 mm为宜;阻盐隔断层的设置位于路堤上部,高于一般路基规范中规定的高度,可以提高阻止水盐运移上升、增强汽盐淋滤作用的效果.A subgrade project in Qinghai salt lake area,China was in a cold and dry geotechnical environment with strong concealed salt weathering.Taking the natural saline soil samples of the above subgrade construction project and soil samples of the built subgrade structure in Chaka Salt Lake area of Qinghai,comparative tests were conducted to study the effect of the subgrade structure protection against salt weathering in the saline soil area of Qinghai province.On the basis of soluble salt content measurements,particle analysis and capillary water rising experiment,the maximum height of capillary water rising in subgrade soil layer in Chaka saline soil area was calculated theoretically.The results indicate that the rising height of capillary water in the saline soil was higher than that in the general soil;the content of fine grains(0.250–0.075 mm)was conducive to the increase of water and salt migration,while the content of coarse grains(>0.250 mm)would inhibit water and salt migration.Under the dual action of water and salt migration and vapor salt migration,secondary salinization occurred in the subgrade soil layer of Chaka saline soil area.It was suggested to set up the gravel salt-blocking layer in the subgrade project of the Chaka saline land area;the grading range of particles should be controlled between 2.0 and 5.0 mm,and the fraction of grains in this size range should be greater than 75%,while the thickness of the gravel salt-blocking layer should be between 300.0 and 1000.0 mm.Besides,the location of the blocking layer should be on the upper part of the embankment,higher than the height specified in the general subgrade code,which can improve the effect of preventing the movement of water-salt and enhancing the effect of vapor-salt leaching.

关 键 词：盐渍土路基 水盐运移 汽盐运移 阻盐隔断层 次生盐渍化 

分 类 号：U416.166[交通运输工程—道路与铁道工程]