脉冲激光抽运铷原子钟研究   总被引：1，自引：0，他引：1  

杜志静  赵文宇  刘杰  张首刚 《武汉大学学报(信息科学版)》2011,36(10):1236-1240

对脉冲激光抽运、微波分立场共振和自由感应微波辐射或者光吸收检测方案（POP）的铷原子钟进行了理论和实验研究。理论研究表明,POP原子钟,可以消除光频移,有效地减小腔牵引频移,从而有利于提高原子钟的稳定度;且微波脉冲面积为π/2时,微波Ramsey条纹的线宽为传统Ramsey条纹的一半,从而提高了原子品质因数。实验获得了...  相似文献   

河口往复流中潮流不对称与推移质输沙的关系   总被引：2，自引：0，他引：2  

李谊纯  董德信  陈波 《海洋科学》2015,39(6):99-103

潮流不对称现象是近岸潮波运动的基本特征之一,为了研究潮流不对称对推移质泥沙长期净输运的作用机制,首先在往复流情况下对Bagnold推移质输沙率公式(1966)由于不包含起动流速所可能导致的误差进行理论分析,进而由统计学中的"偏度"的概念出发,推导了河口潮流不对称与推移质输沙之间的定量关系。研究认为,虽然Bagnold推移质输沙率公式不包含泥沙起动流速,但是只要泥沙起动流速和最大流速的比值在一定范围内,则在理论上公式的计算误差是可以接受的。由偏度结合Bagnold公式导出了潮流不对称与推移质输沙之间的关系,表明推移质泥沙的长期净输运不仅与余流有关,而且与不同分潮组合之间、余流与分潮之间的相互作用紧密相关。该关系还给出了一个由潮流调和常数估算河口推移质输沙的简便方法。经对比,从潮流不对称出发估算推移质输沙与直接采用推移质输沙率公式结果一致。  相似文献   

红树植物无瓣海桑果实的化学成分研究   总被引：1，自引：0，他引：1       下载免费PDF全文

曹雷雷  田海妍  王友绍  周雪峰  江仁望  刘永宏 《热带海洋学报》2015,34(1):77-82

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北京平原构造断块划分及微断块第四纪活动性探讨   总被引：4，自引：3，他引：1       下载免费PDF全文

赵勇 蔡向民  王继明张 磊刘 予吕金波 《中国地质》2015,(6):1876-1876

在对北京平原地区地质构造特征综合分析的基础上,依据近年来在活动断裂研究中遇到的问题,本文提出对北京平原区进行构造断块划分的方案。将北京平原区划分为7个"断块",即马池口—沙河、小汤山、顺义、平谷、丰台—来广营、大兴—通州及房山断块。据断块内次一级活动断裂和第四纪地层沉降发育情况,进一步可划出活动微断块,把以研究单一活动断裂重点转变为以控制微断块边界的交汇活动断裂组相互作用为中心。从而揭示出第四纪以来微断块边界交汇活动断裂组的特征、活动方式及其规律等,可为首都城市建设规划和减轻地质灾害等提供有价值的参考,为保障城市地质安全提供地质依据。  相似文献   

小兴安岭-张广才岭地区晚古生代至中生代花岗岩的成因及其地质意义     

葛茂卉  张进江  刘恺  王盟  李壮 《岩石矿物学杂志》2020,39(4):385-405

中国东北地区显生宙花岗岩的成因一直是中亚造山带东段研究的热点之一,尤其是小兴安岭-张广才岭地区的花岗岩其成因及形成的大地构造背景一直存在较大争议。本文新获得小兴安岭-张广才岭铁力和依兰地区的二长花岗岩LA-ICP-MS锆石U-Pb年龄分别为188±1 Ma和257±3 Ma。地球化学数据显示,两地区的二长花岗岩均为Ⅰ型花岗岩并且富集大离子亲石元素(Th和U等)和轻稀土元素,亏损高场强元素(Nb和Ta等)和重稀土元素具有弧岩浆岩的地球化学特征。锆石Hf同位素数据显示,铁力地区二长花岗岩的岩浆源区可能来自于中新元古代的下地壳部分熔融。综合前人在小兴安岭-张广才岭地区已发表的花岗岩类岩石的地质年代学和地球化学数据,初步推测小兴安岭-张广才岭地区在晚古生代至中生代期间处于活动大陆边缘环境。同时,小兴安岭-张广才岭地区晚古生代至中生代的岩浆岩具有自东向西形成时代逐渐变年轻的趋势,这可能是由于东侧的牡丹江洋在晚古生代至中生代期间俯冲角度逐渐变缓造成的。  相似文献   

Three-dimensional active earth pressure from cohesive backfills with tensile strength cutoff     

Zheng-Wei Li  Tian-Zheng Li  Xiao-Li Yang 《国际地质力学数值与分析法杂志》2020,44(7):942-961

Most of previous analyses on the active earth pressure were performed in two-dimensional cases using the Mohr-Coulomb (M-C) failure function to describe the soil strength. However, all failures of retained slopes indicate a somewhat three-dimensional (3D) feature, and the M-C function is found to overestimate the tensile strength of cohesive soil. In this work, a kinematic limit analysis–based approach is developed for computing the 3D active earth pressure resulting from cohesive backfills. The concept of tensile strength cutoff is adopted to implement the reduction or elimination of tensile strength from the strength envelope. An extended 3D horn failure mechanism that is associated with the modified strength envelope is developed to characterize the collapse of retained slopes. The resultant of active earth pressure is evaluated from the work rate balance equation and expressed as an unfactored coefficient. The obtained results indicate that less support provided by the wall is required when allowing the existence of soil cohesion and 3D effects and that eliminating the tensile strength can observably increase the active earth pressure, especially for the backfill with a great level of cohesion.  相似文献   

A climatic trigger for catastrophic Pleistocene–Holocene debris flows in the Eastern Andean Cordillera of Colombia          下载免费PDF全文

N. HOYOS  O. MONSALVE  J. L. ANTINAO  H. GIRALDO  C. SILVA  G. OJEDA  G. BAYONA  J. ESCOBAR  C. MONTES 《第四纪科学杂志》2015,30(3):258-270

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A simple way to classify supermassive black holes     

A. Feoli 《Astronomische Nachrichten》2014,335(2):193-197

We propose a classification of supermassive black holes (SMBHs) based on their efficiency in the conversion of infalling mass in emitted radiation. We use a theoretical model that assumes a conservation of angular momentum between the gas falling inside the hole and the photons emitted outwards, and suggests the existence of the scaling relation M_•‐R_eσ³, where M_• is the mass of the central SMBH, whereas R_e and σ are the effective radius and velocity dispersion of the host galaxies (bulges), respectively. We apply our model on a data set of 57 galaxies of different morphological types and with M_• measurements, obtained through the analysis of Spitzer /IRAC 3.6‐µ m images. In order to find the best fit of the corresponding scaling law, we use the FITEXY routine to perform a least‐squares regression of M_• on R_eσ³ for the considered sample of galaxies. Our analysis shows that the relation is tight and our theoretical model allows to easily estimate the efficiency of mass conversion into radiation of the central SMBHs. Finally we propose a new appealing way to classify the SMBHs in terms of this parameter. (© 2014 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim)  相似文献   

面向服务架构下主动地理信息服务模型研究     

王珂珂  张立朝  王青山 《测绘科学》2010,35(5):146-148

通过引入服务的主动发现、定制、加载与使用机制,支持新服务、新应用的按需创建,为用户发现、定制和运行能够满足用户需求的服务,从而改变当前用户只能被动地使用现有服务的应用模式,以应对信息化需求的不断发展和变化。主动型的地理信息服务在Web服务框架模型、基础协议的基础之上,增加识别用户需求和处理的能力,使用户能够根据特定需要选择合适的服务,使服务能够自动适应用户的需求。本文讨论了面向服务架构下的主动地理信息服务模型,该模型以Web服务技术为支撑,以扩展的UDDI等协议为规范,并对该模型进行测试,实验证明该模型可以有效地主动式的地理信息服务。  相似文献   

The sensitivity of simulated flow and water quality response to spatial heterogeneity on a hillslope in the Tarrawarra catchment,Australia     

L. N. Neumann  A. W. Western  R. M. Argent 《水文研究》2010,24(1):76-86

Models are widely used to simulate hydrological response and the generation and transport of constituents such as salt, phosphorus, and nitrogen from catchments to streams. Several models use a spatial representation with catchments divided into subcatchments. Variations in land use and other characteristics within subcatchments are represented by spatially lumped hydrologic response units (HRUs) or functional units instead of using fully distributed models. This approach disregards any spatial interaction between HRUs, including their connectivity to each other and to the stream and the influence of these interactions on water and constituent export. A spatially explicit hydrological model (Thales) was used to simulate a variety of theoretical catchments with soils dominated by combinations of infiltration excess, saturation excess, and subsurface stormflow processes and different soil constituent concentrations that were spatially interacting (i.e. located along a hillslope sequence). The modelling results show that the response of both runoff and concentration is sensitive to varying spatial arrangements due to interactions of runoff, infiltration, and chemical processes between the different soil types in many but not all situations. Results highlight the importance of considering connectivity of pathways when modelling hydrological response and constituents export. This is achieved by comparing pairs of simulations and the corresponding differences in the exported loads. Copyright © 2009 John Wiley & Sons, Ltd.  相似文献