土木工程类专业英文文献及翻译(共6页).doc

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1、精选优质文档-倾情为你奉上PAVEMENT PROBLEMS CAUSEDBY COLLAPSIBLE SUBGRADESBy Sandra L. Houston,1 Associate Member, ASCE(Reviewed by the Highway Division)ABSTRACT: Problem subgrade materials consisting of collapsible soils are com-mon in arid environments, which have climatic conditions and depositional andweathe

2、ring processes favorable to their formation. Included herein is a discussionof predictive techniques that use commonly available laboratory equipment andtesting methods for obtaining reliable estimates of the volume change for theseproblem soils. A method for predicting relevant stresses and corresp

3、onding collapsestrains for typical pavement subgrades is presented. Relatively simple methods ofevaluating potential volume change, based on results of familiar laboratory tests,are used.INTRODUCTIONWhen a soil is given free access to water, it may decrease in volume,increase in volume, or do nothin

4、g. A soil that increases in volume is calleda swelling or expansive soil, and a soil that decreases in volume is called acollapsible soil. The amount of volume change that occurs depends on thesoil type and structure, the initial soil density, the imposed stress state, andthe degree and extent of we

5、tting. Subgrade materials comprised of soils thatchange volume upon wetting have caused distress to highways since the be-ginning of the professional practice and have cost many millions of dollarsin roadway repairs. The prediction of the volume changes that may occur inthe field is the first step i

6、n making an economic decision for dealing withthese problem subgrade materials.Each project will have different design considerations, economic con-straints, and risk factors that will have to be taken into account. However,with a reliable method for making volume change predictions, the best design

7、relative to the subgrade soils becomes a matter of economic comparison, anda much more rational design approach may be made. For example, typicaltechniques for dealing with expansive clays include: (1) In situ treatmentswith substances such as lime, cement, or fly-ash; (2) seepage barriers and/or dr

8、ainage systems; or (3) a computing of the serviceability loss and a mod-ification of the design to accept the anticipated expansion. In order to makethe most economical decision, the amount of volume change (especially non-uniform volume change) must be accurately estimated, and the degree of roadro

9、ughness evaluated from these data. Similarly, alternative design techniquesare available for any roadway problem.The emphasis here will be placed on presenting economical and simplemethods for: (1) Determining whether the subgrade materials are collapsible;and (2) estimating the amount of volume cha

10、nge that is likely to occur in theAsst. Prof., Ctr. for Advanced Res. in Transp., Arizona State Univ., Tempe, AZ85287.Note. Discussion open until April 1, 1989. To extend the closing date one month,a written request must be filed with the ASCE Manager of Journals. The manuscriptfor this paper was su

11、bmitted for review and possible publication on February 3, 1988.This paper is part of the Journal of Transportation.Engineering, Vol. 114, No. 6,November, 1988. ASCE, ISSN 0733-947X/88/0006-0673/$1.00 + $.15 per page.Paper No. 22902.673field for the collapsible soils. Then this information will plac

12、e the engineerin a position to make a rational design decision. Collapsible soils are fre-quently encountered in an arid climate. The depositional process and for-mation of these soils, and methods for identification and evaluation of theamount of volume change that may occur, will be discussed in t

13、he followingsections.COLLAPSIBLE SOILSFormation of Collapsible SoilsCollapsible soils have high void ratios and low densities and are typicallycohesionless or only slightly cohesive. In an arid climate, evaporation greatlyexceeds rainfall. Consequently, only the near-surface soils become wettedfrom

14、normal rainfall. It is the combination of the depositional process andthe climate conditions that leads to the formation of the collapsible soil.Although collapsible soils exist in nondesert regions, the dry environment inwhich evaporation exceeds precipitation is very favorable for the formationof

15、the collapsible structure.As the soil dries by evaporation, capillary tension causes the remainingwater to withdraw into the soil grain interfaces, bringing with it soluble salts,clay, and silt particles. As the soil continues to dry, these salts, clays, andsilts come out of solution, and tack-weld

16、the larger grains together. Thisleads to a soil structure that has high apparent strength at its low, naturalwater content. However, collapse of the cemented structure may occurupon wetting because the bonding material weakens and softens, and the soilis unstable at any stress level that exceeds tha

17、t at which the soil had beenpreviously wetted. Thus, if the amount of water made available to the soilis increased above that which naturally exists, collapse can occur at fairlylow levels of stress, equivalent only to overburden soil pressure. Additionalloads, such as traffic loading or the presenc

18、e of a bridge structure, add tothe collapse, especially of shallow collapsible soil. The triggering mechanismfor collapse, however, is the addition of water.Highway Problems Resulting from Collapsible SoilsNonuniform collapse can result from either a nonhomogeneous subgradedeposit in which differing

19、 degrees of collapse potential exist and/or fromnonuniform wetting of subgrade materials. When differential collapse ofsubgrade soils occurs, the result is a rough, wavy surface, and potentiallymany miles of extensively damaged highway. There have been several re-ported cases for which differential

20、collapse has been cited as the cause ofroadway or highway bridge distress. A few of these in the Arizona and NewMexico region include sections of 1-10 near Benson, Arizona, and sectionsof 1-25 in the vicinity of Algadonas, New Mexico (Lovelace et al. 1982;Russman 1987). In addition to the excessive

21、waviness of the roadway sur-face, bridge foundations failures, such as the Steins Pass Highway bridge,1-10, in Arizona, have frequently been identified with collapse of foundationsoils.Identification of Collapsible SoilsThere have been many techniques proposed for identifying a collapsiblesoil probl

22、em. These methods range from qualitative index tests conducted on674disturbed samples, to response to wetting tests conducted on relatively un-disturbed samples, to in situ meausrement techniques. In all cases, the en-gineer must first know if the soils may become wetted to a water contentabove thei

23、r natural moisture state, and if so, what the extent of the potentialwetted zone will be. Most methods for identifying collapsible soils are onlyqualitative in nature, providing no information on the magnitude of the col-lapse strain potential. These qualitative methods are based on various func-tio

24、ns of dry density, moisture content, void ratio, specific gravity, and At-terberg limits.In situ measurement methods appear promising in some cases, in that manyresearchers feel that sample disturbance is greatly reduced, and that a morenearly quantitative measure of collapse potential is obtainable

25、. However,in situ test methods for collapsible soils typically suffer from the deficien-cy of an unknown extent and degree of wetting during the field test. Thismakes a quantitative measurement difficult because the zone of materialbeing influenced is not well-known, and, therefore, the actual strai

26、ns, in-duced by the addition of stress and water, are not well-known. In addition,the degree of saturation achieved in the field test is variable and usuallyunknown.Based on recently conducted research, it appears that the most reliablemethod for identifying a collapsible soil problem is to obtain t

27、he best qualityundisturbed sample possible and to subject this sample to a response to wet-ting test in the laboratory. The results of a simple oedometer test will indicatewhether the soil is collapsible and, at the same time, give a direct measureof the amount of collapse strain potential that may

28、occur in the field. Potentialproblems associated with the direct sampling method include sample distur-bance and the possibility that the degree of saturation achieved in the fieldwill be less than that achieved in the laboratory test.The quality of an undisturbed sample is related most strongly to

29、the arearatio of the tube that is used for sample collection. The area ratio is a measureof the ratio of the cross-sectional area of the sample collected to the cross-sectional area of the sample tube. A thin-walled tube sampler by definitionhas an area ratio of about 10-15%. Although undisturbed sa

30、mples are bestobtained through the use of thin-walled tube samplers, it frequently occursthat these stiff, cemented collapsible soils, especially those containing gravel,cannot be sampled unless a tube with a much thicker wall is used. Samplershaving an area ratio as great as 56% are commonly used f

31、or Arizona col-lapsible soils. Further, it may take considerable hammering of the tube todrive the sample. The result is, of course, some degree of sample distur-bance, broken.bonds, densification, and a correspondingly reduced collapsemeasured upon laboratory testing. However, for collapsible soils

32、, which arecompressive by definition, the insertion of the sample tube leads to localshear failure at the base of the cutting edge, and, therefore, there is lesssample disturbance than would be expected for soils that exhibit general shearfailure (i.e., saturated clays or dilative soils). Results of

33、 an ongoing studyof sample disturbance for collapsible soils indicate that block samples some-times exhibit somewhat higher collapse strains compared to thick-walled tubesamples. Block samples are usually assumed to be the very best obtainableundisturbed samples, although they are frequently difficu

34、lt-to-impossible toobtain, especially at substantial depths. The overall effect of sample distur-bance is a slight underestimate of the collapse potential for the soil.675译文：湿陷性地基引起的路面问题作者：.摘要：在干旱环境中，湿陷性土壤组成的路基材料是很常见的，干旱环境中的气候条件、沉积以及风化作用都有利于湿陷性土的形成。在这方面包括了一种使用常用的实验室设备和测试方法获得这些问题的土壤的体积变化的可靠估计的预测技性讨论。

35、对典型的路面路基提供了一种方法去预测相关的应力和相应的湿陷张力。基于熟悉的实验室测试结果，使用相对简单的方法评估潜在体积的变化。引言：当土壤接触到水的时候，可能体积会减小或扩大，也可能不变化。遇到水体积增大的土叫做膨胀土，而体积减小的称为湿陷性土。土壤的类型结构、最初的土壤密度、施加应力状态以及土壤浸湿的程度范围决定了体积变化量的大小。自从专业实践开始由这些遇水体积变化的土组成的路基材料已经导致了许多公路病害，并且在维修方面已经花费了数百万美元。处理这种路基材料做出经济决策的第一步是做出可能发生的体积变化的预测。每个工程项目都有不同的设计考虑、经济限制和风险因素，所有这些情况都必须考虑到。然而

36、，最好的和最合理的设计可能会具有更大的经济优势相比于可靠的体积变化预测。例如，典型的处理膨胀黏土的技术有：(1)在现场用例如石灰、粉煤灰或者水泥等处置处理；(2)设置渗流屏障或者排水设施；(3)进行适用性散失的计算来变更设计来接受预期膨胀。为了做出最经济的决定，体积变化（特别是不均匀的体积变化）的量必须要精确计算，并且要从计算出的数据上估测出路面的平整度。同样，不寻常的设计技术可利用到任何道路问题中。 这里将重点对以下两点提供简单和经济的方法：(1)决定路基材料是否是湿陷性膨胀性或者其他;(2)估算湿陷性土在路基中极有可能发生的体积变化量。这些信息将会是工程师做出合理的决定。湿陷性土在干旱地区

37、是非常常见的。这种土的形成过程以及计算可能发生的体积变化量将在下文中介绍。美国亚利桑那州皇家经济学会高级助理教授Tempe注：讨论开放至1989年4月1日。增加截止日期一个月，必须要有ASCE期刊经理批准的书面请求。这篇文章是提交复审的初稿，可能出版的时间在1988年2月3日。本文是运输杂志收录的的一篇文章。114工程卷，6号，1988年11月。ASCE，ISSN 0733-947x / / / 88 0006-0673 1美元+每页15美元。22902号文件湿陷性土湿陷性土的结构湿陷性土有高孔隙率、低密度和较弱的黏性等特点。在干旱地区，有很高的蒸发量，而降水量较低。因此，当有降水时只有地面土

38、壤湿润。沉积作用和气候条件共同造成了湿陷性土的形成。尽管湿陷性土存在于非沙漠地区，但干旱环境中蒸发量远超降水量这一特点非常有利于湿陷性土结构的形成。当土壤在蒸发过程中变干后，毛细张力使其余的水进入土壤颗粒的界面，同时带出可溶性盐、粘土和粉砂颗粒。随着土壤继续变干，可溶性盐、黏土和粉砂颗粒逐渐从溶解状态脱离出来，大量的颗粒物聚集在一起。这就导致这种土壤在低含水量时具有较高的表面强度。然而，当遇到水时，由于结合材料的弱化和软化，土壤承受应力超过浸湿之前，会使土结构发生崩塌。这样，如果提供给土壤水量高于自然状态水量，可能在较低水平的压力时就发生崩溃，或许就在上覆土压力作用下。额外的负荷，如交通荷载或

39、桥梁结构的存在，增加了湿陷性，特别是对于浅层土。无论怎样，触发湿陷性的原因就是加入水。湿陷性土引起的公路问题不均匀的沉陷可能是因为地基矿床存在不同程度的不均匀性或者是地基材料湿度不一样。当路基土发生微分崩溃时，结果是一个粗糙的、波浪状的表面，并潜在存在许多英里路基的广泛灾害。已经有一些报道，微分崩溃已被引用作为道路或公路桥梁病害的原因。其中一些在亚利桑那州和新墨西哥州地区包括靠近本森,亚利桑那州1 - 10,部分和新墨西哥附近Algadonas的1 - 25部分。除了道路表面的过度波动，桥梁基础的问题，比如在亚利桑那州斯坦通公路桥梁，其他的经常被确定地基土的崩溃。鉴别湿陷性土已经有许多技术，提

40、出了鉴别湿陷性土的问题。这些方法的范围从干扰样品进行质量指标的测试到比较浸湿前后土的性状再到现场观测技术。在所有的情况下，工程师首先必须要知道是否被浸湿的土壤含水量在天然含水量之上，如果是，那么就要确定潜在的浸湿范围。大部分鉴定湿陷性土的方法在本质上都是定性的，没有提供潜在崩塌规模的大小。这些定性的方法是基干密度、水分含量、空隙率、比重和阿太堡界限之上的。原位检测出现在某些较有前途的研究中，因为许多专家认为样品干扰大大减少，而定量检测更能得到潜在的崩塌结论。然而，湿陷性土原位测试方法在现场测试时通常遭受润湿分布范围和程度未知这一问题的困扰。由于该区域材料材料以及水和应力的影响是未知的，使得定量

41、检测难以进行。此外，在现场试验取得的饱和度是变化的，通常也不能确定。根据最近的研究，表明鉴别湿陷性土的最可靠地方法是在试验室中观测最优质的原状样品在接触到水时的反应。简单的土压缩试验结果将表明土壤是否是湿陷性的，与此同时，还能得到这些区域潜在湿陷应力的直接测量值。直接测量的方法存在的现在的问题包括样品干扰以及测到的饱和度可能低于实验室测得的。未受干扰的样品质量是与收集样品的管的面积比有很大关系的。面积比是收集到的样品横截面积与样品管横截面积的比。根据定义，A型薄壁样品管具有10%-15%的面积比率。虽然最好通过薄壁管来获得原状样品，但实际情况下样品很容易发生僵硬、胶结，尤其是封闭的砂砾，所以通常情况用较厚的管来采样。亚利桑那州的土壤通常有56%的面积比。另外，可能需要相当大的锤击该管一驱动样品。当然，其结果是，样品一定程度的干扰、断键、致密化，并相应的减小实验室测量时的崩溃。然而，符合定义的湿陷性土，样品管插入时导致局部剪切破坏，比一般剪切的土壤样品量更少干扰失败。专心-专注-专业