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   783篇
  免费   1篇
  国内免费   4篇
测绘学   4篇
大气科学   31篇
地球物理   132篇
地质学   277篇
海洋学   152篇
天文学   175篇
自然地理   17篇
  2022年   13篇
  2021年   20篇
  2020年   21篇
  2019年   28篇
  2018年   59篇
  2017年   25篇
  2016年   32篇
  2015年   13篇
  2014年   27篇
  2013年   51篇
  2012年   47篇
  2011年   46篇
  2010年   36篇
  2009年   30篇
  2008年   35篇
  2007年   46篇
  2006年   33篇
  2005年   13篇
  2004年   20篇
  2003年   19篇
  2002年   16篇
  2001年   14篇
  2000年   6篇
  1999年   8篇
  1998年   10篇
  1997年   9篇
  1996年   6篇
  1995年   7篇
  1994年   5篇
  1993年   3篇
  1992年   4篇
  1991年   3篇
  1990年   8篇
  1989年   5篇
  1987年   6篇
  1986年   4篇
  1985年   4篇
  1984年   4篇
  1983年   6篇
  1981年   4篇
  1980年   2篇
  1978年   2篇
  1977年   5篇
  1976年   4篇
  1974年   4篇
  1973年   3篇
  1972年   4篇
  1970年   3篇
  1966年   2篇
  1965年   3篇
排序方式: 共有788条查询结果,搜索用时 15 毫秒
571.
Kosov  V. I.  Ivanov  G. N.  Levinskii  V. V.  Ezhov  E. V. 《Water Resources》2001,28(4):407-412
The distribution of heavy metals in the Volga bottom deposits is studied. According to the degree of pollution with heavy metals, three stretches are singled out within the river reach under consideration. A drastic increase in Cu and Cd concentrations in bottom deposits is established. A close statistical correlation between Cu and Pb accumulation and the organic matter content of bottom deposits is revealed.  相似文献   
572.
573.
Effective energy loss per electron-ion pair produced, <xi>(E 0), as a function of a particle’s initial energy has been obtained for proton transport in the atmosphere. The influence of some transport parameters on the shape of <xi>(E 0) has been studied. Comparisons with the case of electron transport and with other results were made. It has been shown that: 1. for E 0>1 keV, <xi>(E 0) varies within the range 30–36 eV; 2. as E 0 increases the value of <xi>(E 0) tries to attain an asymptotic value that is the same as for electrons (\approx35 eV); 3. <xi>(E 0) strongly depends on the average energy of secondary electrons, but the energy distribution of secondary electrons is not as important. The range of possible changes in <xi>(E 0) associated with discrepancies in cross sections has been obtained.  相似文献   
574.
Seismic velocity anisotropies measured in underground mines are compared within situ stress measurements in these mines. These underground data are also compared with seismic velocity anisotropies observed by large scale seismic sounding conducted from the earth's surface, The velocity anisotropies are about 10% and the data obtained by different methods on different scales and frequencies agree with each other. The directions of largest and smallest velocities coincide with the largest and smallest horizontal stresses, respectively. These results suggest that the direction and magnitude of stresses in potential mining areas could be estimated from velocity anisotropies observed in seismic prospecting of the area.  相似文献   
575.
The uptake coefficients () for OH radicals on some dry salts of tropospheric interest (NaCl and NH4NO3) have been investigated as a function of temperature using the flow tube technique combined with an EPR spectrometer as a detection method. The temperature dependence of -values measured over the temperature range 245–340 K can be expressed in Arrhenius form: OHNaCl=(1.2±0.7)×10−5exp[(1750±200)/T] and OHNH4NO3=(1.4±0.5)×10−4exp[(1000±100)/T]. These Arrhenius expressions lead to very similar -values (\approx4×10−3) for both salts studied at 300 K. It is shown that the heterogeneous OH sinks on solids aerosol play a very minor role in tropospheric chemistry in comparison with the homogeneous sinks.  相似文献   
576.
577.
Problems of geochronological correlation are considered for the formations established in the study region with due account for data on the Mezino-Lapshinovka, Lokh and Teplovka sections studied earlier on the northwest of the Saratov region. New paleontological data are used to define more precisely stratigraphic ranges of some stratigraphic subdivisions, to consider correlation between standard and local zones established for different groups of fossils, and to suggest how the Upper Cretaceous regional scale of the East European platform can be improved. Considered in addition are paleogeographic environments in the study region during the Late Cretaceous epoch and principal stages of the regional geological evolution.  相似文献   
578.
579.
This article presents an approach to computing K shortest paths in large buildings with complex horizontal and vertical connectivity. The building topology is obtained from Building Information Model (BIM) and implemented using directed multigraphs. Hierarchical design allows the calculation of feasible paths without the need to load into memory the topology of the entire building. It is possible to expand the graph with new connectivity on-the-fly. The paths calculated may be composed of traversable building components that are located inside the buildings or those that are both inside and outside buildings. The performance (computational time and heap size used) is optimized by using the appropriate collections (maps, lists and sets). The proposed algorithm is evaluated in several use-case scenarios – complete graphs and real building environments. In all test scenarios, the proposed path finding algorithm is faster and uses less memory when compared to the fast version of the Yen’s KSP algorithm. The proposed approach can be successfully used as a first level of coarse-to-fine path finding algorithms.  相似文献   
580.
The optimized (all iterative procedures are excluded) local one-dimensional thermody-namic model of the formation and melting of ice is proposed. The numerical computation of ice cover evolution in the Kerch Strait under the influence of thermodynamic factors for the period of 5 months is carried out for the real conditions of winter of 2011/12. Thec results agree well with the available obser-vational data on the timing of ice formation and on ice thickness in the southern part of the Sea of Azov and in the Taman Bay. In combination with the full three-dimensional hydrodynamic model and taking into account diurnal variations in external factors, the model simulates the spatial distribution of ice cover formation.  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