南疆渍土路基冻胀变形特性研究
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摘要
新疆南疆分布有大面积的渍土,以硫酸渍土和氯化物渍土为主。在南疆季节性冻土地区,渍土路基的-冻胀变形往往造成南疆渍土地区道路的变形和破坏。如何对变形破坏道路进行有效的修复和重建是一个十分重要的课题,也是一个难题,其中一个重要内容就是要开展南疆渍土路基-冻胀变形特性的研究。本文的主要研究工作和成果如下:
     通过采用现场调研和试验对比研究的方法,对南疆不同地区渍土的分布、形成、工程特性进行研究,结果表明:南疆不同地区受地理位置、区域地形、地貌及地下水分布的差异和地质构造的影响,其渍土的分布、形成、类型及分组成具有明显的区域差异性。
     通过对S207线和阿拉尔市变形破坏路段进行路基-冻胀变形监测试验。试验结果表明:路面-冻胀变形量与日平均气温、路基土不同深度的地温值及地下水位的变化具有明显的相关性;路基最大-冻胀变形量在时间上滞后于日平均最低气温和路基不同深度最低地温值。
     通过对阿拉尔市和S207线试验路段的路面变形量、路基不同深度地温、测区气温和地下水位进行现场监测试验和室内-冻胀变形试验研究。研究结果表明:S207线路基的变形破坏主要是硫酸钠胀变形与氯化物的溶陷变形相互作用的结果。其分来源于高矿化度的地下水经毛细作用将路基深层土体中易溶的硫酸、氯化物迁移积聚至路基结构层中。在温度交替变化过程中产生反复的胀、溶陷变形。阿拉尔市道路变形破坏属于冻胀和胀变形破坏。产生胀的硫酸钠使路基水泥稳定基层膨胀破坏,路面产生裂缝变形;地表水经路面裂缝和路基侧面入渗路基,在U形不透水隔断层上形成上层滞水,加之阿拉尔市11月份的高地下水位,为冬季低温环境下路基土体的冻胀变形提供了充足的冻结水,加速了路面的变形破坏。
     根据南疆渍土工程性质及-冻胀变形试验研究结果,总结提出了“一个加强、两个严格、三个注重”的渍土路基-冻胀变形综合防治原则;针对南疆渍土路基-冻胀工程灾害,提出“五步骤”综合防治方法与工程措施,在南疆渍土路基的改建工程中得到了应用,取得明显的防治效果。
There are large areas of distribution of saline soil in southern Xinjiang, mainly saline soil with sulfuric acid and chlorine-based saline soil. In seasonal frozen soil areas in southern Xinjiang, the expansion of sulfate salts and chloride salts dissolved collapsible caused deformation and damage of the road. How to effective repair and reconstruction the roads of deformation and damage is a very important issue, it is also a problem, it is an important part which of To carry out research work of saline soil subgrade salt-frost heave deformation properties in southern Xinjiang. The main research work and results are as follows:
     By adopting the comparative method of the use of On-site investigation and trial, to study the distribution、formation and engineering characteristics of saline soil in different parts of the southern Xinjiang ,and the results showed that: There are clear regional differences in the distribution, formation, type and composition of the salt saline soil in different parts of the southern Xinjiang by the impact of geographical location, the region's topography, geomorphology and water distribution and geological differences.
     Through carry out salt-frost heave deformation monitoring test about the section of deformation and damage of Road S207 and Alar urban road. The results showed that: road surface salt-frost heave deformation and the average daily temperature and different depths of the roadbed soil temperature and change the water table have obvious relevance; the maximum salt-frost heave deformation in time lags behind the minimum temperature of daily average and at different depths to the minimum temperature value of roadbed.
     Through tested the road surface deformation, the roadbed ground temperature at different depths, the temperature of measurement area and the water table on-site testing and monitoring indoor salt- frost heave deformation of in Alaer City line and S207-line .The results show that: S207-line’s deformation failure is mainly because of the sodium chloride and the salt expansion deformation of the salt solution collapse deformation interaction. Salt from its high salinity of the water by capillary action will be deep roadbed soil in the soluble sulfate, chloride salts migrate to the accumulation of separation layer structure. At the turn of temperature changes in the process of repeated expansion of salt, the melting depression change.The form of frost damage to the road in Alaer City belongs to the expansion of salt and deformation failure. The sodium salt resulting expansion of cement road salt so that the stability of the expansion of the damage to the grass-roots level, have a surface crack deformation; surface water through surface cracks and infiltration side of the road embankment, in the U-shaped cut off impermeable layer on the formation of the upper stagnant water and Alar City in November of a high water table for the winter low temperature environment road frost heave deformation of the soil to provide sufficient water to freeze and accelerated the deformation of the surface damage.
     According to the Southern Xinjiang saline soil and salt nature of the project - the evaluation of frost heave deformation test results, the sum put forward "a Strengthen ,two Strict , three Attention " ----the principle of Salt saline soil subgrade - integrated control of frost heave deformation; for Southern Xinjiang road salt saline soil - frost heave engineering disaster, "five steps" comprehensive prevention and control methods and measures, saline soil in Southern Xinjiang of the road reconstruction works has been applied to obtain a clear effect.
引文
[1]徐攸在等,渍土地基[M].中国建筑工业出版社.1993,19~88.
    [2]陈肖柏,刘建坤,刘鸿绪等.土的冻结作用与地基[M].北京:科学出版社.2006.170-171.
    [3]牛玺荣.硫酸渍土地区路基水.热..力四场耦合机理及数值模拟研究[D].2006.17-20.
    [4] Halan.R.I.Analysis of coupled heat-fluid transport in partially frozen soil [J].Water Resour Res.Vol.9.No.5.1973.
    [5] Taylor.G.S., Luthin, J.N. A model for coupled heat and moisture transfer during soil freezing [J]. Can.Geotech.J., Vol.15.1978.
    [6] Cary, J. W., Mayland, H. F.Salt and water movement in Unsaturated frozen soil [J]. Proceedings of the Soil Science Society of America.V36.N4.Jul-Aug. 1972. p:549-555.
    [7] Kang Shuangyang,Gao Weiyue and Xu Xiaozu.1994.Fild observation of solute migrationin freezing and thawing soils,Procedings of the 7th International Symposium on Ground Freezing.397~398.
    [8] Everett D H. The thermo dynamics of frost damage to porous solids[J].Trans Faraday Soc.1961. 57:1541~1551.
    [9]徐学祖,王家澄,张立新,邓友生,陶兆祥.1995.土体冻胀和胀机理[M].科学出版社.126.
    [10]高江平,杨荣尚.含氯化钠硫酸渍土在单向降温时水分和分迁移规律的研究[J].西安公路交通大学学报.1997.3(17).
    [11]王俊臣.新疆水磨河细土平原区硫酸(亚硫酸)渍土填土胀和冻胀研究[D].2005a.100~103.
    [12]邱国庆等.关于冻结过程中易溶迁移方向的讨论[A].第三届全国冻土学术会议论文集[C].科学出版社. 1989.211~217.
    [13]徐学祖,邓友生,王家澄,王玉杰.开放系统饱和含氯化钠正冻土中的水迁移[A].第五届全国冰川冻土学大会论文集[C].甘肃文化出版社.1996a,597~600.
    [14]徐学祖,邓友生,王家澄,王玉杰.封闭系统非饱和含氯化钠正冻土中的水迁移[A].第五届全国冰川冻土学大会论文集[C].甘肃文化出版社.1996b.601~606.
    [15]张立新,徐学祖,陶兆祥.含硫酸钠冻土的未冻含水量[A].第五届全国冰川冻土学大会论文集[C].甘肃文化出版社.1996.693~698.
    [16]徐学祖,奥利奋特,J.L,泰斯,A.R..土水势未冻含水量和温度[J].冰川冻土.1985.7 (1):1~14.
    [17]习春飞.硫酸渍土-冻胀性的微观试验研究,击实硫酸渍土的-冻胀性研究[D]. 2005.37~43.
    [18]徐学祖,邓友生,王家澄,王玉杰.含正冻土的冻胀和胀[A].第五届全国冰川冻土学大会论文集[C].甘肃文化出版社, 1996.607~618.
    [19]高江平,吴家惠.硫酸渍土胀特性的单因素影响规律研究[J].岩土工程学报.1997.19(1): 37~42.
    [20]彭铁华,李斌.硫酸渍土在不同降温速率下的胀规律[J].冰川冻土.1997.19(3).252~257.
    [21]王俊臣.新疆水磨河细土平原区硫酸(亚硫酸)渍土填土胀和冻胀研究[D]. 2005b.215~259.
    [22]樊子卿.红当公路渍土病害治理[J].公路交通科技.1990.7(3):17~26.
    [23]张文虎.对新疆焉耆盆地渍土铁路路基的浅析[J].1992.11.
    [24]丁永勤,陈肖柏.掺氯化钠治理硫酸渍土膨胀的应用范围[J].冰川冻土.1992.4(2):107~114.
    [25]黄立度,席元伟,李俊超.硫酸土道路胀病害的基本特征及防治[J].中国公路学报. 1997. 10 (2).
    [26]王鹰,谢强.含地层工程性能及其对铁路工程施工的影响[J].矿物岩石.2000.20(4).
    [27]金培杰,戴玉.南疆铁路库喀段渍土路基病害与防治措施研究[J].路基工程.2006(1):116~118.
    [28]新疆渍土地区公路路基路面设计与施工规范XJTJ01-2001.新疆.2001.
    [29]中华人民共和国铁道部行业标准.2001.铁路工程地质勘察规范J124-2001.中国铁道出版社.
    [30]中华人民共和国铁道部行业标准.2001.铁路工程特殊土勘察规程J126-2001.中国铁道出版社.
    [31]中华人民共和国行业标准.2004.公路路基设计规范JTG D30-2004.人民交通出版社.
    [32]杨煜.G314线阿克苏-阿图什段渍土公路路基施工常遇问题及处理措施[J].岩土工程界.2005(7):70~72.
    [33]王志伟.高地下水位渍土地区路基维护[J].路基工程.2004(3):54~55.
    [34] Y.J.CUT and P.DELAGE. Yielding and plastic behavior of an unsaturated compacted silt.
    [35]中华人民共和国国家标准.冻土工程地质勘察规范GB50324-2001.中国计划出版社.
    [36]徐攸在等.渍土地基[M].中国建筑工业出版社.1993.19~88.
    [37]陈肖柏,刘建坤,刘鸿绪等.土的冻结作用与地基[M].北京:科学出版社.2006.170-171.
    [38]刘宝兴.路基工程新技术实用全书[M].北京:海潮出版社.2001.5.315-317.
    [39]新疆公路学会主编.渍土地区公路设计与施工指南[M].北京:人民交通出版社.2006:33~36.41~47.51~52.
    [40]中国科学院新疆综合考察队.中国科学院土壤研究所.新疆土壤地理[M].北京:科学出版社.1965.
    [41]新疆维吾尔自治区农业厅.新疆维吾尔自治区土壤普查办公室.新疆土壤[M].北京:科学出版社.1996.
    [42]郗金标,张福锁,毛达如等.新疆渍土分布与生植物资源[J].土壤通报. 2005a.36(3): 299 ~ 303.
    [43]赵军,杜卫.阿克苏河下游冲洪积平原渍土的室内试验分析[J].西部探矿工程. 2006.13: 28 ~30.
    [44]郗金标,张福锁,毛达如等.新疆渍土分布与生植物资源[J].土壤通报. 2005b . 36(3): 299 ~ 300.
    [45]周华,李全胜,朱瑞成等.新疆库尔勒地区渍土的工程地质特征[J].西部探矿工程. 2000.64 (3):37~38.
    [46]李琦,原诗.对新疆库尔勒新城区渍土的认识[J].岩土工程界.2004.7(12).
    [47]陈肖柏,刘建坤,刘鸿绪等.土的冻结作用与地基[M].北京:科学出版社.2006.183-190.205-207.
    [48]陈肖柏等.重渍土在温度变化时的物理化学性质和力学性质.中国科学.1988.(A)4:429-438.
    [49] Chen Xiaobai, Wang Yaqing.1988.Salt redistribution and heave of saline soils during temperature change.In:Proceedings of 88 ISCORD.Harbin.327-336.
    [50] Chen Xiaobai, Wang Yaqing.1988.Influence of saturated-dehydrated-frozen cycles on density of fill. In:Proceedings of 88 ISCORD.Harbin.337-342.
    [51]邢爱国,李世争,陈龙珠.高速公路水泥固化渍土的试验研究[J].公路.2007.7:76~79.
    [52]包卫星.喀什地区渍土工程性质试验研究[D].2005.28~29.
    [53]包卫星,张洪萍.新疆渍土的胀特性及其病害防治[J].山西建筑.2 0 0 5. Vol.31 No.4.
    [54]薛明,朱玮玮,金众赞.渍土路基分迁移防治与养护[J].公路交通科技.应用技术版.2008.1:28~31.
    [55]王小生,章洪庆,薛明,房建宏.渍土地区道路病害与防治[J].同济大学学报.2003.10.Vol.31 No.10.
    [56]邓卫东,张兴强,陈波等.路基不均匀沉降对沥青路面受力变形影响的有限元分析[J].中国公路学报.2004.1. Vol.17No.1:12~15.
    [57]张志权,王志勇.硫酸渍土地区公路胀影响因素及防治措施[J].路基工程.2006.3: 148~150.
    [58] Maggio.A, Reddy.M .P, Joly R.J, Leaf gas exchange and solute accumulation in the halophyte Salvadora persica grown at moderate salinity [J]. Environmental and Experimental Botany, 2000, 44 : 31~38.
    [59]贾恢先.内陆渍化生物防治研究[J].甘肃农业.2002年第9期:42~44.
    [60] Glenn E .P, Brown J .J., Blumwal .E . Salt tolerance and crop potential of halophytes[J]. Cri tical Review of Plant Science. 1999.18 : 227~255.
    [61]李伟强,刘小京,赵可夫,刘海亮.NaCl胁迫下3种生植物生长发育及离子在不同器官分布特性研究[J].中国生态农业学报.2 0 0 6 .Vol .14 No .2:40-52.
    [62]赵可夫,李法增.中国生植物[M].北京:科学出版社.1999 .104~110.
    [63]赵可夫,范海,江行玉等.生植物在渍土壤改良中的作用[J].应用与环境生物学报.2002.8 (1) :31~35.
    [64]赵可夫.利用生植物改良碱地[J].植物生理学通讯.1997.33 (6):501~502.
    [65] Mandak B., Pysek P. Effects of plant density and nutrient levels on fruit polymorphism in Artiplex Sagittata[J].Oecologia.1999.119:63~72.
    [66]王玉珍,刘永信,魏春兰,缪金伟.6种生植物对碱地土壤改良情况的研究[J].安徽农业科学. 2006.34(5):951-952~957.
    [67]薛焱,王迎春.生植物长叶红砂泌特性的研究[J].中国沙漠.2008.Vol. 28.No.3:437-441.
    [68]任健美,尤莉,高建峰等.鄂尔多斯高原40 a气候变化研究[J].中国沙漠,2005.25(6):847-879.
    [69]张海燕.胁迫下地碱蓬体内无机离子含量分布特点的研究[J].西北植物学报.2002. 22(1):129-135.
    [70] Rozema J, Gude H.An ecophysiological study of the salt secretion of four halophytes [J].New Phytol.1981.89:201-217.
    [71]王苗,齐树亭,葛美丽.生植物对滨海渍土生物改良的研究进展.安徽农业科学. 2008. 36(7): 2898-2899.2954.
    [72]张世绥.渍土地区公路边坡的生物防护.中外公路. 2 0 0 7年8月第27卷.第4期308-311.

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