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851.
Hu Yi-li Xu Jun Duan Yong-kong Xu Zhao-yong Yang Run-hai Zhao Jin-ming 《地震学报(英文版)》2004,17(6):725-734
A new method of detecting the vertical bearing capacity for single-pile with high strain is discussed in this paper. A heavy
hammer or a small type of rocket is used to strike the pile top and the detectors are used to record vibration graphs. An
expression of higher degree of strain (deformation force) is introduced. It is testified theoretically that the displacement,
velocity and acceleration cannot be obtained by simple integral acceleration and differential velocity when long displacement
and high strain exist, namely when the pile phase generates a whole slip relative to the soil body. That is to say that there
are non-linear relations between them. It is educed accordingly that the force P and displacement S are calculated from the amplitude of wave train and (dynamic) P-S curve is drew so as to determine the yield points. Further, a method of determining the vertical bearing capacity for single-pile
is discussed. A static load test is utilized to check the result of dynamic test and determine the correlative constants of
dynamic-static P(Q)-S curve.
Foundation item: Key projects of the tenth Five-year Plan of Yunnan Province (documented Yunnan district [2002]54-02-02) and Geophysical
Society of Yunnan Province. 相似文献
852.
Xian-Kang Zhang Zhuo-Xin Yang Yu-Chun Yang Jian Yang Jian-Li Song Ping Zhao 《地震学报(英文版)》1995,8(4):519-529
In this paper, the theory and method, obtaining the tomographic determination of three-dimensional velocity structure of the
crust by use of the joint inversion of explosion and earthquake data, are given. The velocity distribution of the crust is
regarded as a continuous function of the spatial coordinates without parametrization of the velocity model ahead, so that
the inversion solution would not be influenced by different parametrization procedures. The expressions of integration kernels,
which relates the two kinds of data sets, are also given. The authors have processed the observed data in Tangshan earthquake
region by the method proposed in this paper, and obtained the tomographic results of the middle and upper crust structures
in this region. The comparison of these results with the result obtained only by the explosion data, has also been made. 相似文献
853.
地理学视角的物流网络研究已成为物流科学领域的热点方向。从地理学的空间视角出发,在明确城乡物流网络理论来源和相关概念的基础上,对城乡物流网络的内涵、构成及研究框架进行梳理。基于研究,首先给出了城乡物流网络的定义,认为城乡物流网络的本质是旧的城市物流网络和乡村物流网络在空间上的延伸、衔接和提效。其次,从空间视角将城乡物流网络分解为节点、连线和域面3要素,指出网络各要素均出现了功能强化和更新,如节点的管理、衔接和经济社会功能强化;连线的联结功能和平衡功能出现,域面的协同组织、动态调整功能突出。最后,遵循地理学“格局-过程-机理-决策”的科学逻辑,提出“数据采集与融合、要素映射与解析、时空比较与分析、机理探究与优化”4个模块的城乡物流网络分析框架,为深刻揭示城乡物流网络结构及其演化机理提供基础。进一步指出未来应探讨城乡物流节点、连线、域面及网络的地区类型、区域适宜性及要素间相互作用机制,提炼适应不同区域、能有效提升要素流通效应的多尺度空间组织模式,加强对城乡要素流通系统的科学认知,科学支撑城乡地域融合发展实践。 相似文献
854.
855.
X. M. Wang J. R. Shi G. Zhao 《Monthly notices of the Royal Astronomical Society》2009,399(3):1264-1274
Abundances of O, Na, Mg, Al, Si, K, Ca, Sc, Ti, V, Cr, Fe, Ni and Ba are determined for 30 nearby lower-main-sequence stars in the Northern sky using high-resolution, high signal-to-noise ratio spectra. Our results show an equilibrium of [Fe/H]I and [Fe/H]II and a much smaller star-to-star scatter of the abundance ratios as a function of metallicity compared with the results of Kotoneva et al. The non-local thermodynamic equilibrium (non-LTE) corrections for oxygen are considered and found to be small (∼−0.04 dex) . A flat trend of [O/Fe] exists over the whole metallicity range. The non-LTE effects for some important elements are discussed, and it is found that the abundance pattern for our programme stars is very similar to that of F and G dwarfs. 相似文献
856.
经过十余年理论技术持续攻关,中国陆上实现了致密砂岩气规模发展、页岩气快速发展、煤层气持续发展、致密油稳步发展和页岩油加快探索,源岩层系油气已成为中国非常规油气增储上产的主要组成部分.源岩层系油气包括源岩油气和致密油气2种资源类型,普遍具备有效配置的烃源岩、储集层和聚集保存3个方面基础地质形成条件,展现出源内或近源大面积连续分布标志特征,海相页岩气主要分布于深水陆棚区,致密砂岩气和煤层气一般分布于主要聚煤期煤系,页岩层系石油一般主要发育于长期持续沉降的富油湖盆.源岩层系油气开发追求“平面甜点区”“纵向甜点段”较好经济资源条件,页岩气需含气量高、孔隙度高、TOC含量高、热演化程度适中、气层埋藏适中、保存条件好、储层可压性好、储量规模大,致密砂岩气需全天候气源、中粗粒砂岩、含气层系多、大面积聚集、稳定斜坡区、中浅层埋藏,致密油甜点区段一般具有烃源性、储集性、含油性、流动性、成缝性和经济性“六特性”经济资源条件.中国非常规源岩层系油气资源丰富,源岩层系天然气是天然气上产的“主力”,源岩层系石油是石油稳产的“砝码”,实现地下原位“煤岩燃烧气化、页岩熟化气化”“2个革命性领域”突破是推进源岩层系油气领域“跨越式”发展的关键路径. 相似文献
857.
858.
2005年7月4-6日在捷克共和国首都布拉格召开了世界气象组织的科学研究项目“世界气候研究项目”(WCRP)下设的两个课题“20世纪气候”(C20C)和“季节与年际气候预测”(WGSIP)联合专题研讨会。会议由两个课题的负责单位英国哈得莱中心(HADL)和美国海洋-陆地-大气研究中心(COLA)的有关领导和科学家主持,包括来 相似文献
859.
860.
Numerous Fe–Cu deposits are hosted in the late Paleoproterozoic Dongchuan and Dahongshan Groups in the Kangdian region, SW
China. The Dongchuan Group is composed of siltstone, slate, and dolostone with minor volcanic rocks, whereas the Dahongshan
Group has undergone lower amphibolite facies metamorphism and consists of quartz mica-schist, albitite, quartzite, marble
and amphibolite with local migmatite. Deposits in the Dongchuan Group are commonly localized in the cores of anticlines, in
fault bends and intersections, and at lithological contacts. Orebodies are closely associated with breccias, which are locally
derived from the host rocks. Fe-oxides (magnetite and/or hematite) and Cu-sulfides (chalcopyrite, bornite) form disseminated,
vein-like and massive ores, and typically fill open spaces in the host rocks. The deposits have extensive albite alteration
and local K-feldspar alteration overprinted by quartz, carbonate, sericite and chlorite. Deposits in the Dahongshan Group
have orebodies sub-parellel to stratification and show crude stratal partitioning of metals. Fe-oxide ores occur as massive
and/or banded replacements within the breccia pipes, whereas Cu-sulfide ores occur predominantly as disseminations and veinlets
within mica schists and massive magnetite ores. Ore textures suggest that Cu-sulfides formed somewhat later than Fe-oxides,
but are possibly within the same mineralization event. Both ore minerals predated regional Neoproterozoic metamorphism. Both
orebodies and host rocks have undergone extensive alteration of albite, scapolite, amphibole, biotite, sericite and chlorite.
Silica and carbonate alterations are also widespread. Ore-hosting strata have a LA-ICP-MS zircon U–Pb age of 1681 ± 13 Ma,
and a dolerite dyke cutting the Fe-oxide orebodies has an age of 1659 ± 16 Ma. Thus, the mineralization age of the Dahongshan
deposit is constrained at between the two. All ores from the two groups have high Fe and low Ti, with variable Cu contents.
Locally they are rich in Mo, Co, V, and REE, but all are poor in Pb and Zn. Sulfides from the Fe–Cu deposits have δ34S values mostly in the range of +2 to +6 per mil, suggesting a mix of several sources due to large-scale leaching of the strata
with the involvement of evaporites. Isotopic dating and field relationships suggest that these deposits formed in the late
Paleoproterozoic. Ore textures, mineralogy and alteration characteristics are typical of IOCG-type deposits and thus define
a major IOCG metallogenic province with significant implications for future exploration. 相似文献