聚丙烯纤维和水泥对粘性土强度的影响及机理研究   总被引：5，自引：0，他引：5  

唐朝生  施斌  高玮 《工程地质学报》2007,15(1):108-113

选取聚丙烯纤维和水泥作为加固材料,在室内试验的基础上,研究了单独的纤维和水泥对粘性土强度的影响及其的综合作用,分析了它们的作用机理。试验中,3种不同百分比(0.05%,0.15%和0.25%素土重)的纤维和两种不同百分比的(5%和8%素土重)水泥分别掺入到粘土试样中,配制了12组试样,进行了无侧限抗压试验。试验结果表明,纤维和水泥均能够提高土体的强度,纤维的加入改善了水泥土样的脆性破坏模式;纤维水泥土样的强度远远高于相同掺量下的纯纤维土和纯水泥的强度,甚至高于它们的强度之和。运用扫描电镜(SEM)从微观层次上分析了纤维和水泥加固粘性土的力学机理,发现纤维表面与土介质之间的粘结力和摩擦力对加固效果有直接影响。  相似文献   

原状黄土显微结构特征与湿陷性状分析   总被引：6，自引：1，他引：5  

宋章  程谦恭  张炜  孟凡超 《工程地质学报》2007,15(5):646-653

基于原状黄土的显微结构扫描电镜及室内湿陷性试验,分析了黄土的微结构特性和不同压力不同含水量下黄土的湿陷性状及其之间的内在联系,结果表明:随着埋藏深度的增加,由支架大孔微胶结结构逐渐变为镶嵌微孔半胶结结构,支架大孔孔隙发育逐渐变为粒间孔隙发育,再为微孔孔隙发育;黄土在增湿情况下其湿陷系数-压力关系曲线由三部分组成,初始压缩变形阶段,是结构强度发挥阶段,变形较小,黄土微结构没有遭到破坏;曲线第一转折点s=0.015后,原有结构破坏,微结构发生变化,颗粒重新排列,湿陷速率增大,是湿陷变形主要阶段;达到峰值后,颗粒间形成了新的结构,湿陷变形幅度减小;随着骨架颗粒连接逐渐变为非架空的镶嵌排列,湿陷起始压力及峰值湿陷压力值随着埋藏深度的增加而增加,而峰值湿陷系数和湿陷变形量的压力范围随着埋藏深度的增加而变小;骨架颗粒特征和孔隙特征是黄土湿陷性的内在影响因素,而胶结物的多寡及胶结状态是黄土湿陷性强弱的主要影响因素之一。  相似文献   

勒氏笛鲷外周血细胞显微结构的观察     

李长玲  曹伏君  刘楚吾  陈刚 《广东海洋大学学报》2001,21(3):5-9

报道了勒氏笛鲷外周血细胞的显微结构,血涂片经过Wright染色液染色,可区分出红血细胞、血栓细胞、嗜中性粒细胞、单核细胞、淋巴细胞等五种血细胞,没有发现嗜碱性粒细胞、嗜酸性粒细胞.白血细胞中,血栓细胞体积最小,单核细胞体积最大;血栓细胞数目最多,淋巴细胞和单核细胞数目最少;淋巴细胞有大小两种类型大淋巴细胞和小淋巴细胞.此外,在外周血液中还观察到少量未成熟的红细胞和嗜中性粒细胞,偶而可见正在分裂的红细胞,提示红细胞也可在外周血直接分裂.  相似文献   

中国对虾复眼的研究 Ⅰ.解剖与组织结构   总被引：10，自引：1，他引：10  

胡景杰  陈宽智  包振民 《海洋科学》1997,21(2):30-34

中国对虾具一对有眼柄的复眼，复眼约由５５０００个小眼构成。每个小眼由角膜，成角膜细胞、晶状体、晶状体束、小网膜细胞及其细胞膜突出的微绒毛汇合而成的感杆束等部分组成，在复眼中还有起调节进入小网膜光量的远端色素和近端色素。小网膜细胞形成轴索，穿过基膜上的网眼，联系神经节瓣。  相似文献   

Sr对6A02铝合金组织和性能的影响          下载免费PDF全文

杨占寿 《盐湖研究》2020,28(2):50-55

通过电磁感应炉制备了含锶6A02铝合金,对制备的试样采用OM、XRD、硬度测试、拉伸测试,研究Sr含量对6A02铝合金组织和性能的影响。结果表明Sr元素的加入可以细化合金的铸态组织,改变组织形貌。当Sr含量为0.5%时,细化效果最好,合金其力学性能最优。随着Sr含量的增加,6A02铝合金出现新相Al_4Sr,随着组织中Al_4Sr相增多,Mg_2Si相的析出减少,减弱了对合金的强化效果,合金的力学性能呈下降趋势。  相似文献   

A simple experimental method to regain the mechanical behavior of naturally structured marine clays     

《Applied Ocean Research》2019

Quantitative laboratory studies on the structural behavior of natural intact marine clays require a large number of identical natural samples leading to an expensive and challenging task. This study proposes a simple method to reconstruct an artificial structured marine clay as the state of its natural intact clay at both macro and micro levels. For this purpose, the Shanghai marine clay is selected and mixed with low cement contents (1–6%). The clay-cement slurry is mixed in a container with the ice-covered sides at a low temperature about 0 ± 2 °C to postpone the hydration reactions until consolidation began. The purpose of adding cement is to generate the inter-particle bonding and structure in reconstituted samples. Initially, the reconstituted samples are consolidated under the in situ stress of 98 kPa and then under the pre-consolidation pressure of 50 kPa. Mechanical characteristics such as compression index, yield stress, unconfined compression strength, shear strength ratio, and the stress paths from triaxial tests are compared with natural intact clay accordingly. Scanning electron microscope and mercury intrusion porosimetry analyses are also performed to analyze the microstructure of clays for comparison. Furthermore, the proposed method is also examined by using natural intact marine clays of different locations and characteristics.  相似文献   

碳化对加填料氯氧镁胶凝材料力学性能的影响     

曼阳阳  肖学英  董金美  李颖  文静  常成功  郑卫新  黄青 《盐湖研究》2019,27(3)

以添加不同掺量填料的氯氧镁水泥(MOC) 试件为基体,在空气和碳化箱中分别养护至规定龄期,研究碳化对掺加填料MOC力学性能的影响,并与空气环境进行对比,运用XRD和SEM分析碳化后水化产物和微观结构的变化规律。结果表明,28d龄期内,随着填料掺量的增加MOC试件碳化后的抗折强度均有所增加,碳化后的抗压强度均有提升,碳化过程反应生成了MgCO<sub>3</sub>,不同碳化龄期的主要物相均为5Mg(OH)<sub>2</sub>.MgCl<sub>2</sub>.8H<sub>2</sub>O(5.1.8),而掺加填料不影响MOC的水化产物的组成。  相似文献   

The German Bight (North Sea) is a nursery area for both locally and externally produced sprat juveniles     

Hannes Baumann  Arne M. Malzahn  Rudi Voss  Axel Temming 《Journal of Sea Research》2009,61(4):234-243

To better understand the role of the German Bight (GB) as a nursery area for juvenile North Sea sprat Sprattus sprattus we sought to determine whether the area may receive only locally or also externally produced offspring. We sampled juveniles during 3 trawl surveys in the GB in August, September, and October 2004 and applied otolith microstructure analysis in order to reconstruct their distributions of the day-of-first-increment-formation (dif). These were contrasted with spatial and seasonal patterns of sprat egg abundance in the GB and its adjacent areas, observed during 6 monthly plankton surveys. It was found that the majority of juveniles originated mainly from April/May 2004, coinciding with high spawning activity west of the GB, whereas spawning and larval production inside the GB peaked notably later, in May/June. This indicated that a large proportion of juveniles was produced outside the GB and transported subsequently into it through passive and/or active migration. Shifts to later mean difs from one survey to the next and length distributions indicative of the simultaneous presence of multiple cohorts, supported the notion that the GB is a complex retention and nursery area for sprat offspring from different North Sea spawning grounds and times. Later born juveniles had significantly faster initial growth rates than earlier born conspecifics, which was likely temperature-mediated, given the strong correlation between back-calculated growth histories and sea surface temperature as a proxy for thermal histories of juveniles (r² = 0.52).  相似文献   

软粘土固结变形微观分维指标分析     

王珊珊  刘凯  杨艳  孙强  胡瑞林 《地震工程学报》2011,33(Z1)

软粘土宏观性质与其微结构有着密切联系。对天津滨海新区软粘土先后进行了固结实验和扫描电镜实验,并对扫描图像进行处理,提取微观结构指标进行分析。结果显示,随着固结压力的增加,软粘土原有微观结构遭到强烈破坏,粘土粒度分维、颗粒表面起伏分维降低,颗粒分布分维增大。表现为颗粒粒径和表面起伏程度降低,颗粒排列出现明显的定向方向,密实度增大。  相似文献   

http://www.sciencedirect.com/science/article/pii/S1674987113000054     

Dilip Saha 《地学前缘(英文版)》2013,4(3):289-304

Substantial part of the northern margin of Indian plate is subducted beneath the Eurasian plate during the Caenozoic Himalayan orogeny, obscuring older tectonic events in the Lesser Himalaya known to host Proterozoic sedimentary successions and granitic bodies. Tectonostratigraphic units of the Proterozoic Lesser Himalayan sequence (LHS) of Eastern Himalaya, namely the Daling Group in Sikkim and the Bomdila Group in Arunachal Pradesh, provide clues to the nature and extent of Proterozoic passive margin sedimentation, their involvement in pre-Himalayan orogeny and implications for supercontinent reconstruction. The Daling Group, consisting of flaggy quartzite, meta-greywacke and metapelite with minor mafic dyke and sill, and the overlying Buxa Formation with stromatolitic carbonate-quartzite-slate, represent shallow marine, passive margin platformal association. Similar lithostratigraphy and broad depositional framework, and available geochronological data from intrusive granites in Eastern Himalaya indicate strikewise continuity of a shallow marine Paleoproterozoic platformal sequence up to Arunachal Pradesh through Bhutan. Multiple fold sets and tectonic foliations in LHS formed during partial or complete closure of the sea/ocean along the northern margin of Paleoproterozoic India. Such deformation fabrics are absent in the upper Palaeozoic–Mesozoic Gondwana formations in the Lesser Himalaya of Darjeeling-Sikkim indicating influence of older orogeny. Kinematic analysis based on microstructure, and garnet composition suggest Paleoproterozoic deformation and metamorphism of LHS to be distinct from those associated with the foreland propagating thrust systems of the Caenozoic Himalayan collisional belt. Two possibilities are argued here: (1) the low greenschist facies domain in the LHS enveloped the amphibolite to granulite facies domains, which were later tectonically severed; (2) the older deformation and metamorphism relate to a Pacific type accretionary orogen which affected the northern margin of greater India. Better understanding of geodynamic evolution of the northern margin of India in the Paleoproterozoic has additional bearing on more refined model of reconstruction of Columbia.  相似文献