一种静力触探模型箱试验装置的研制及其试验研究

设计了一套静力触探模型箱试验装置,该装置可以在模型箱水平面内任意位置进行贯入试验,贯入速率在一定范围可控,贯入倾角可调节。将该装置用于TJ-1模拟月壤静力触探力学特性的研究,试验结果表明：地基表层模拟月壤发生刺入剪切破坏;贯入阻力随贯入深度的增加而增加;探杆周围同一深度处土体的水平土压力表现出轴对称特征,其值在探头靠近土压力盒过程中逐渐增大至最大值,后随探头远离土压力盒又逐渐减小至0,且不同深度土体水平土压力峰值随贯入深度增加而增大;贯入点正下方土体的垂直土压力随贯入深度的增加而增加,主要影响范围约为距探头200 mm处。基于以上试验研究,表明该模型箱的设计是合理的,且TJ-1模拟月壤力学特性的研究成果能够为将来涉及到TJ-1模拟月壤的航天试验提供必要的技术参考。     

粉细砂的室内无填料振冲试验研究

在室内严格控制的边界条件下,通过室内模型试验研究了粉细砂无填料在振冲中孔隙水压力增长与消散的规律、孔隙水压力空间分布规律、相对密度和静力触探指标与振冲次数之间的关系等。定性地验证了无填料振冲对于规范中未推荐使用的粉细砂土的适应性,并为后来某工程大面积地基处理成功地提供了参考。     

塔克拉玛干沙漠砂静力触探试验研究

在控制相对密度和含水量的条件下进行了系列室内大型槽和中型槽原位测试模拟试验及相关土工试验,取得了塔克拉玛干沙漠砂静力触探指标锥尖阻力qc与容许承载力pa、内摩擦角? 、相对密度Dr和变形模量E0.01的一系列有效数对,建立了qc- pa,qc-? ,qc-Dr,qc-E0.01等相关关系,并给出了适合在沙漠地区应用的数字化表格,为在沙漠地基勘察中推广应用静力触探技术积累了经验。     

地基承载力经验公式的变异性分析

应用随机场理论,研究了地基承载力表、CPT等地基承载力经验公式的变异性分析方法,提出经验公式确定地基承载力的变异性是由经验公式本身的不确定性和土性参数的不确定性组成,提出了考虑土性参数自相关性的地基承载力经验公式的变异性分析方法,通过对编制CPT确定地基承载力经验公式资料的计算分析,得出CPT确定地基承载力的变异系数在0.1~0.135之间。     

Dimensionless and unbiased CPT interpretation in sand

The cone penetration test (CPT) is widely used, and although initially developed as a stratigraphic logging tool its excellent repeatability and accuracy offers a benchmark quantitative test for sand in particular. A continuing difficulty, however, is that the CPT does not measure any soil property directly, so that parameters of interest must be recovered from solution of an inverse boundary value problem, which is difficult. To date most CPT interpretations in sand have been based on very limited calibration testing carried out in large chambers on a few sands from which mappings are developed. But there are differences in the CPT response from one sand to another leaving the interpretation imprecise (and arguably even speculative) because these differences remain poorly understood. In this paper we use the familiar spherical cavity expansion analogy to the CPT including large strains and a good, critical-state-based, soil model to develop a pattern of behaviour which we then compare to some of the reference chamber test data. We find that one of the issues of dispute in the empirical interpretation methods, the so-called stress-level effect, is caused by neglect of elasticity and that there are several additional parameters of first-order significance to cavity expansion in sands. More generally, we show that the difference in CPT response between various chamber sands in predicted. Our results are cast in dimensionless form and the inversion illustrates that extreme care is required in interpreting CPT data if the in situ sand state is to be determined with precision approaching that suggested as achievable by the repeatability of the CPT data itself. Aspects requiring particular care in interpreting CPT data in sand are discussed. © 1998 John Wiley & Sons, Ltd.     

多级存储优化的大规模全局光照快速计算

针对大规模复杂场景渲染的全局光照计算量大从而影响其渲染实时性的问题,提出了一种基于多级分辨率纹理存储结构的改进体素锥追踪全局光照算法。算法首先采用基于人眼视觉特性的多级分辨率纹理存储结构高效存储光照信息,并在直接光照计算时,结合存储结果特点,然后采用混合存储的GPU硬件加速与无贡献节点丢弃的软件加速相结合方法,进一步提高光照渲染效率,最后基于多级纹理及闭合体节点自适应合并对锥波滤器进行改进,实现全局光照的高效计算。试验结果表明,改进算法减少了光照计算量,降低了系统内存占用,并取得了与经典算法相近的场景光照渲染效果,从而验证了其在大规模光照计算的有效性。     

Physical experimental study on the formation mechanism of pockmark by aeration

Abstract

As one of the common geological disasters on the seafloor, the occurrence of pockmarks often indicates the existence of submarine fluid. And the formation of the pockmarks is generally attributed to the soil carried away by the fluid. The research established physical model test and found: (1) The pockmark formed after aeration, and particle gradation changed in the center area of the pockmark where coarse particle (particle size/0.25?mm) increased obviously and fine particle (particle size ≤0.075?mm) decreased significantly; (2) Comparing the volume of the pockmark with the volume of the soil extracted by siphon, it can be found that the volume of the pockmark was much larger than the loss of soil, and the difference reached its peak when the inflation pressure was 20?kPa; (3) Comparing the cone resistance of the soil in the surface and boundary, it can be found that the resistance of the center and marginal soil was much bigger than the outside, and the cone resistance of the boundary was also improved greatly. The research considered that the formation of pockmark was not only related to the soil being carried away by the bottom current, but also the consolidation by vibration existed.     

深水土工调查技术和分析方法新进展

简要介绍了近年来国外在深水土工调查技术和分析方法方面取得的新进展,包括:钻孔取样技术在钻入模式和取样器的多样化和有效组合,从而实现不同水深和不同土类条件下的高质量取样;带孔压测量的圆锥触探试验在测量方法、孔压测量单元设计、探头的小型化和多样化、数据的快速传输以及分析理论方面的进展;减少土样扰动,准确评估粘土不排水抗剪强度的“SHANSEP”室内试验方法及应用。     

原土环境下水泥土强度衰减过程室内试验研究

在水土耦合的室内原土环境中,通过微型贯入、扫描电镜(SEM)、能谱(EDS)分析、X射线衍射(XRD)、离子含量及pH值测试等多种试验手段,研究滨海相软土场地形成的水泥土强度的分布规律及其衰减过程,并阐明水泥土劣化层和未劣化层的发展规律。结果表明:水泥土劣化深度随养护时间的增长和水泥掺入比的减小不断增大,至360d时最大劣化深度达到11.9mm,明显大于同龄期海水环境中养护的水泥土的劣化深度;与未劣化层相比,劣化层的孔径增大,孔隙增多,水泥水化产物减少;经原土养护相同时间,水泥土中pH值及主要离子含量分布规律与室内海水环境中的水泥土相似,其中pH值和Ca^2+含量随着试样深度的增大而增大,而Mg^2+、SO4^2-、Cl^-含量随试样深度的增大而减小;水泥土中Ca^2+含量沿试样深度方向的分布规律与强度变化规律相似。在原土条件下,水泥土中Ca的溶出更加显著,导致后期水泥土强度衰减加剧。原土中水泥土强度衰减过程与海水中相同。