首页 | 本学科首页   官方微博 | 高级检索  
文章检索
  按 检索   检索词:      
出版年份:   被引次数:   他引次数: 提示:输入*表示无穷大
  收费全文   995篇
  免费   137篇
  国内免费   190篇
测绘学   14篇
大气科学   8篇
地球物理   239篇
地质学   348篇
海洋学   437篇
天文学   139篇
综合类   25篇
自然地理   112篇
  2024年   1篇
  2023年   10篇
  2022年   19篇
  2021年   18篇
  2020年   20篇
  2019年   52篇
  2018年   35篇
  2017年   26篇
  2016年   24篇
  2015年   38篇
  2014年   55篇
  2013年   56篇
  2012年   43篇
  2011年   36篇
  2010年   27篇
  2009年   73篇
  2008年   66篇
  2007年   90篇
  2006年   85篇
  2005年   65篇
  2004年   64篇
  2003年   60篇
  2002年   38篇
  2001年   44篇
  2000年   25篇
  1999年   27篇
  1998年   31篇
  1997年   25篇
  1996年   41篇
  1995年   21篇
  1994年   17篇
  1993年   17篇
  1992年   10篇
  1991年   10篇
  1990年   12篇
  1989年   8篇
  1988年   9篇
  1987年   4篇
  1986年   2篇
  1985年   4篇
  1984年   1篇
  1983年   2篇
  1982年   5篇
  1981年   2篇
  1980年   1篇
  1979年   1篇
  1977年   1篇
  1954年   1篇
排序方式: 共有1322条查询结果,搜索用时 15 毫秒
1.
Average velocity in streams is a key variable for the analysis and modelling of hydrological and hydraulic processes underpinning water resources science and practice. The present study evaluates the impact of the sampling duration on the quality of average velocity measurements acquired with contemporary instruments such as Acoustic Doppler Velocimeters (ADV) an Acoustic Doppler Current Profilers (ADCP). The evaluation combines considerations on turbulent flows and principles and configurations of acoustic instruments with practical experience in conducting customized analysis for uncertainty analysis purposes. The study sheds new insights on the spatial and temporal variability of the uncertainty in the measurement of average velocities due to variable sampling durations acting in isolation from other sources of uncertainties. Sampling durations of 90 and 150 s are found sufficient for ADV and ADCP, respectively, to obtain reliable average velocities in a flow affected only by natural turbulence and instrument noise. Larger sampling durations are needed for measurements in most of the natural streams exposed to additional sources of data variability.  相似文献   
2.
Photoelectric radial-velocity measurements show that HD 118670 is a double-lined spectroscopic binary in an orbit which is not quite circular and whose period is about 48 days. Spectral types of K0 V and K7 V would satisfy the photometry and the mass ratio; the mass function would then suggest the possibility of eclipses. However, actual spectral classification indicates a luminosity somewhat above the main sequence  相似文献   
3.
The Rayleigh wave phase and group velocities in the period range of 24–39 sec, obtained from two earthquakes which occurred in northeastern brazil and which were recorded by the Brazilian seismological station RDJ (Rio de Janeiro), have been used to study crustal and upper mantle structures of the Brazilian coastal region. Three crustal and upper mantle models have been tried out to explain crustal and upper mantle structures of the region. The upper crust has not been resolved, due basically to the narrow period range of the phase and group velocities data. The phase velocity inversions have exhibited good resolutions for both lower crust and upper mantle, with shear wave velocities characteristic of these regions. The group velocity data inversions for these models have showed good results only for the lower crust. The shear wave velocities of the lower crust (3.86 and 3.89 km/sec), obtained with phase velocity inversions, are similar to that (=3.89 km/sec) found byHwang (1985) to the eastern South American region, while group velocity inversions have presented shear velocity (=3.75 km/sec) similar to that (=3.78 km/sec) found byLazcano (1972) to the Brazilian shield. It was not possible to define sharply the crust-mantle transition, but an analysis of the phase and group velocity inversions results has indicated that the total thickness of the crust should be between 30 and 39 km. The crustal and upper mantle model, obtained with phase velocity inversion, can be used as a preliminary model for the Brazilian coast.  相似文献   
4.
5.
针对海洋综合测量多种声学测量系统间的窄带相干声学干扰现象进行了理论分析,并针对克服窄带干扰提出了一些具有实用价值的建议。  相似文献   
6.
7.
8.
9.
10.
从射线声学和简正波声学的角度,概述了海洋声层析的基本理论,包括射线走时反演、简正波走时反演、简正波相位反演和简正波水平折射层析。海洋声层析以反演海水温度和流速为基础。还总结了声层析在海洋学研究中的应用。  相似文献   
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号