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701.
702.
目前的景观建筑设计中往往更注重建筑的景观性,而忽略了建筑的安全稳定性,导致景观建筑的整体抗震效果较差,在景观建筑设计中加入挡土墙设计可以有效提高其抗震性。为此,设计一种具有一定抗震性能的景观建筑挡土墙,利用建筑施工过程中保留的复合纤维材料、建筑垃圾以及纤维绳等作为土墙填充物,并加入具有一定抗拉能力的拉筋材料,以保持土墙内部的稳定性。考虑景观建筑通常注重外观视觉效果,使用"平改坡"设计,在墙体表面种植具有一定视觉冲击的植物,增加土墙自重,促进土墙整体结构的稳定性。分析挡土墙后面无限倾斜填土受力状态,选取菱形微小单元体作为研究对象,计算景观建筑的挡土墙土压力强度。实验证明,优化设计的景观建筑挡土墙结构可以有效增强景观建筑的整体抗震能力。 相似文献
703.
选取乌加河地震台2015-2018年地电阻率观测资料,分析数据异常变化,结合观测环境及实地调查,发现存在降雨、雷电、金属管线、农田灌溉、设备漏电等影响因素,对比分析并总结各类干扰曲线形态、变化幅度、影响时间、干扰频次等特征,以便正确认识并排除地电阻率干扰,为地震异常信息识别提供帮助。 相似文献
704.
AN EXPERIMENTAL STUDY ON THE PROCESS OF INTERGRANULAR PRESSURE SOLUTION OF PLAGIOCLASE GOUGE UNDER HIGH TEMPERATURE AND PRESSURE: METHOD AND PRELIMINARY RESULTS 下载免费PDF全文
To understand the mechanism of lower-crust earthquake and slow slips, it is necessary to study the frictional properties of mafic rocks and their major rock-forming minerals. Previous studies have performed a series of experimental researches on gabbro, basalt and their major constituents.
According to the results of previous experiments, frictional sliding of plagioclase under hydrothermal conditions(100~600℃)shows a property of velocity weakening, and the experimental results show that both the direct rate effect parameter(a)and the healing effect parameter(b)increase with temperature, a typical feature for thermally-activated processes. Velocity weakening means property of a shear band that has a stronger friction healing effect than the direct rate effect in the rate and state friction constitutive framework, and the healing effect(b value)in constitutive relation mainly reflects the increase in contact area with time under hydrothermal conditions, with some minor effect of structural changes. Since the microphysical mechanism of feldspar minerals at the contacts is mainly brittle cataclasis for temperatures below 600℃, the significant frictional healing effect in this case can only be explained by the mechanism of pressure solution. In order to determine if the dissolution process of plagioclase actually occurs on the laboratory time scale, we conducted hydrostatic experiments on plagioclase powder samples under hydrothermal conditions whereby frequent contact switch between particles seen in frictional sliding experiments can be avoided, making the observation on the dissolution sites possible.
Experimental temperatures were 400℃ and 500℃, with confining pressure of 90~150MPa, pore pressure of 30MPa, with 2mm initial thickness of fault gouge. The mechanical data show that a creep process occurred in the plagioclase fault gouge in the experimental temperature and pressure range; and the microstructures of the experiment show that precipitation of new grains is prevalent as the product of pressure solution process between plagioclase particles. At the same time, it is observed that the contact points have an appearance similar to fused, fuzzy structure as signatures of dissolution. The results of our experiments provide a definite experimental evidence for the healing mechanism in friction of plagioclase and for the theoretical relation between unstable slip and the pressure solution process.
The results of the experiments are summarized as follows:
(1)Drainage rate of pore water in plagioclase gouge was high in the first few hours of experiment, but gradually decreases over time for both temperature and pressure series of experiments slowing down to a steady state. This feature indicates that there is a creep process that evolves inside the plagioclase gouge.
In the temperature-series experiments, the drainage rate of the pore water in the plagioclase gouge at 400℃ is relatively low than the cases for higher temperatures. Thus, the applied temperature is positively correlated with the creep of plagioclase gouge.
(2)Scanning electron microscopy(SEM)observations of the experimentally deformed samples were performed on thin sections cut along the sample axis. Firstly, from the images of microstructure, it was found that the degree of particle fracture became more significant at a higher effective pressure, with smaller pore volume between particles. In the temperature-series experiments it was found that the degree of compaction of plagioclase gouge increased with increasing temperature. Precipitation of plagioclase grains in layered structures was generally observed in high-magnification images, indicating the presence of pressure solution processes. Contact points were also found to be in a state of ambiguity that seems to be a fused morphology, but the details of the structure remain to be determined by further observations.
The above results indicate that the pressure solution process of plagioclase particles can occur on a typical laboratory time scale, and the results of this study provide robust experimental evidences for the theory that links between pressure solution and the mechanism of frictional healing and unstable slips for plagioclase. 相似文献
705.
706.
简要介绍承德地震前兆台网2014—2017年数据跟踪分析工作,对常见典型干扰事件进行分类统计,分析影响制约承德前兆台网观测数据质量的主要因素,为进一步提高数据分析能力与观测资料质量提供有效的技术参考及应对措施。 相似文献
707.
对于涉县地震台水管倾斜仪观测资料,根据地球物理数据跟踪分析方法,将干扰源按照自然因素、场地环境因素、观测系统、地球物理事件等类型进行分析,并给出数据处理建议。 相似文献
708.
709.
常温和压力0.1~1300 MPa下硬石膏的拉曼光谱研究 总被引:1,自引:0,他引:1
利用立方氧化锆压腔装置测量了高压下硬石膏中硫酸根离子内部S-O键的四个振动(对称伸缩振动、弯曲振动、反对称伸缩振动和变形弯曲振动)的拉曼位移,研究结果表明:在25℃和0.1~1300MPa压力范围内硬石膏未发生相变,所观察到的硬石膏各个拉曼峰的位移值随压力的增加而线性增加,它们与压力之间的关系可分别表达为:υ1018=0.0053p+1016.8,υ417=0.0013p+416.82,υ498=0.0044P+499.25,υ1129=0.0052p+1128.5,υ1160=0.0067p+1159.5,υ608=0.0028p+608.76,υ627=0.0036p+627.01,υ675=0.0039p+675.32,且伸缩振动受压力的影响比弯曲振动大。其1018cm^-1峰强度大,是石英464cm^-1峰的6倍,因此硬石膏也是宝石压腔良好的压力标定物质。 相似文献
710.