Liquefaction behavior of dredged silty-fine sands under cyclic loading for land reclamation: laboratory experiment and numerical simulation     

Jianxiu Wang  Yansheng Deng  Yule Shao  Xiaotian Liu  Bo Feng  Linbo Wu  Jie Zhou  Yao Yin  Na Xu  Haihua Peng 《Environmental Earth Sciences》2018,77(12):471

Medium-coarse sands (CS) were dredged and exhausted in land reclamation. However, the remaining silty-fine sands (FS) were wasted. The liquefaction behavior of dredged silty-FS and the possibility of utilizing the remaining silty-FS as dredger fill source for land reclamation should be investigated. Cyclic consolidation-undrained triaxial tests were performed to investigate the liquefaction resistance of dredged silty-FS under different influencing factors. The cyclic stress ratio (CSR) of dredged silty-FS increased with the increase in initial relative density and consolidation stress ratio and decreased with the increase in silt content and consolidation stress. The CSR first decreased with the increase in clay content up to a threshold value and increased with the increase in clay content. A regression model was created to estimate the relationship between CSR and silt content, clay content, initial relative density, consolidation stress, consolidation stress ratio, and cyclic resistance ratio. Response surface methodology (RSM) was employed to investigate the mutual influence among the five independent variables. On the basis of cyclic triaxial tests, particle flow code models were introduced to investigate the microscopic internal fabric changes of dredged silty-FS and the influence of extended factors on liquefaction. The average microscopic contact force and coordination number between particles controlled the macroscopic mechanical behavior of sands. Sand liquefaction was due to the cumulative loss of coordination number under cyclic loading. The average contact force between particles was linearly decreased to 0 and the coordination number sharply decreased when the sample reached initial liquefaction. On the basis of numerical tests, CSR increased with the increase in D₅₀ and vibration frequency. The influence of vibration frequency was relatively small. In addition, the CS–FS and CS–FS–CS combination layers showed greater liquefaction resistance than the FS layer. In the filling process, the interbed of FS and CS improved the liquefaction resistance of dredged silty-FS to a certain extent.  相似文献   

电磁干扰实验研究     

张继红  李波  韩海华  李润贤  佟瑞清  赵会蓬 《中国地震》2005,21(3):429-436

本文分析了地电、地磁同台观测中出现的干扰问题，并针对地电观测对地磁场测量的影响进行了研究。通过实地测量和对长直导线产生的磁场模拟计算，得出不同距离（20～120m）的感应磁场强度值，由此判断通电导线对周围地磁场的影响。结果表明：电流为2A时，单根导线距地磁场观测点距离应大于150m；导线两侧在相等距离处对地磁总场的干扰并不遵循“数值相等，方向相反”的规律，而是一侧增加量大于另一侧减少量。这项实验研究为地磁、地电同台观测及排除干扰提供了有价值的依据。  相似文献   

用颗粒锆石分层蒸发确定云开群罗罅组的时代   总被引：2，自引：0，他引：2  

张志兰  袁海华 《地球学报》1997,18(Z1):105-107

用颗粒锆石分层蒸发法对开云群罗罅组变英安斑岩及变流纹斑岩中不同成因锆石分别进行年龄测定，获得该火山岩之形成年龄922-940Ma；后期地质事件年龄427-473Ma、643-716Ma及物源区的年龄1616-2084Ma。  相似文献   

海南岛及邻近地区潜在震源近期强震发生概率的研究     

傅昌洪  李海华 《地震地磁观测与研究》1996,17(1):61-68

海南岛及其邻近地区属于中国南弱地震区，但它是该地震区内地震活动水平相对较高的东南沿海地震带的一部分，该地区经济发达，人口稠密，１９９４年９月１６日发生台湾海峡７．４级地震，１９９４年１２月３１日和１９９５年１月１０日相断在北部湾发生了６．１级和６．２级地震，如何估计未来本区的地震趋势是一件十分重要和困难的事情。  相似文献   

Analysis of a Mesoscale Convective System that Produced a Single Sprite     

Jing YANG  Gaopeng LU  Ningyu LIU  Haihua CUI  Yu WANG  Morris COHEN 《大气科学进展》2017,34(2):258-271

Sprites are brief optical emissions occurring above thunderstorms. Features of sprites and their parent thunderstorms and lightning activities have been studied by many researchers. Here, we report a single sprite recorded over a mesoscale convective system during its life cycle in Northeast China. The results show that the sprite might have been a dancing one,with a 20 km horizontal displacement from its parent cloud-to-ground flash(CG) and a 38 ms time delay; all the sprite elements occurred during the continuing current process of the parent flash. The peak current of the parent CG was the largest during the almost one-hour time window containing the sprite, and the absolute values of all the negative flashes were smaller than 100 k A during the same time period and did not produce sprite. The sprite did not occur during the time period in which the maximum area of the thunderstorm reached. The occurrence of sprite corresponded well with the decay of the thunderstorm convection, and no significant relationship between the occurrence of sprite and the increase in the 30–35 d BZ and 35–40 d BZ interval was found. The large wind gradient in the 8–12 km region of the thunderstorm may have played an important role in the sprite production.  相似文献   

火山气体喷发量的一种计算方法——以汉诺坝浮岩为例     

夏成  朱永峰  王海华  鲍景新 《矿物岩石地球化学通报》1998,(2)

火山气体喷发量的一种计算方法———以汉诺坝浮岩为例夏成朱永峰王海华鲍景新（北京大学地质系,北京１００８７１）关键词浮岩二相分流气体喷发量以火山方式将地幔气体排出是地球内部向地表输出的一条重要途径。火山喷发过程中流体（岩浆及地幔气体）带出大量动能,喷出...  相似文献   

7株海洋微藻强化褶皱臂尾轮虫效果的研究     

赵明日  孙世春  麦康森  江海华 《中国海洋大学学报(自然科学版)》2002,32(1):32-38

该文用 7株富含 EPA、DHA的海洋微藻对褶皱臂尾轮虫 (Brachionus plicatilis)进行强化 ,通过检测轮虫的脂肪酸组成和含量来研究这几种微藻对轮虫的营养价值。结果表明 :轮虫中的脂肪酸组成和含量与所用饵料密切相关 ,尤其是 EPA、DHA等多不饱和脂肪酸 (PUFA)主要取决于这些脂肪酸在藻中的含量 ;强化 12 h后 ,轮虫中的 n- 3PUFA含量一般为饵料中含量的 75 %左右 ,强化 2 4 h达 80 %以上 ,强化 7d的轮虫可达 90 %以上。  相似文献   

直接测定颗粒锆石^207Pb／^206Pb年龄的方法   总被引：13，自引：1，他引：13  

袁海华  张志兰 《矿物岩石》1991,11(2):72-79

用B·Kober(1986—1987)所提出的热离子源发射质谱计分层蒸发、直接测定颗粒锆石~(207)Pb/~(206)Pb年龄的方法,6件锆石样品试验表明,其年龄值能与同一样品的常规锆石U-Pb法的交点年龄及其它方法的结果完全一致,并能给出更多具有一定地质意义的年龄信息。  相似文献   

Development of subcracks betweenen echelon fractures in rock plates     

Yonghong Zhao  Haihua Liang  Jiefan Huang  Jinda Geng  Ren Wang 《Pure and Applied Geophysics》1995,145(3-4):759-773

Uniaxial compression tests on marble plates containing two prefabricateden echelon fractures were performed in this study. Photographs showing the typical characteristics of subcrack development were taken under direct scanning electron microscope (SEM) observation during the test. From these photographs, the effects of the lengthL of a single fracture, the separation distanced and overlapping proportiona/L between two prefabricateden echelon fractures on the development of subcracks were analyzed. The results show that the interaction betweenen echelon fractures strengthened with decreasingd. FordL, there was little interaction and the development of subcracks near one of theen echelon fractures was unaffected by the existence of the other. Whereas ford, the number of subcracks in the area intermediate betweenen echelon fractures tended to increase with increasinga and decreasingd. In order to ascertain whether the experiment can furnish some implications for research on earthquake prediction and neotectonic activity, the test results were compared with the spatial-temporal development of foreshocks and ground-water anomalies before the 1975 Haicheng earthquake and the structural framework of the Ganzi pull-apart basin. The results of the comparison are encouraging. According to the similarity between the test results in the laboratory and the natural phenomena in the field, the fault on which the Haicheng earthquake would occur, could be inferred immediately from the relative geometry of the two sub-parallel active faults in the area. Thus, it is considered that the test results would advance our understanding of the process of neotectonic activities and give us inspiration for earthquake prediction.  相似文献