全文获取类型
收费全文 | 106891篇 |
免费 | 2013篇 |
国内免费 | 948篇 |
专业分类
测绘学 | 2841篇 |
大气科学 | 8009篇 |
地球物理 | 21324篇 |
地质学 | 36941篇 |
海洋学 | 9538篇 |
天文学 | 24252篇 |
综合类 | 311篇 |
自然地理 | 6636篇 |
出版年
2021年 | 883篇 |
2020年 | 1045篇 |
2019年 | 1108篇 |
2018年 | 2285篇 |
2017年 | 2218篇 |
2016年 | 2928篇 |
2015年 | 1785篇 |
2014年 | 2872篇 |
2013年 | 5555篇 |
2012年 | 2993篇 |
2011年 | 4101篇 |
2010年 | 3612篇 |
2009年 | 4898篇 |
2008年 | 4334篇 |
2007年 | 4149篇 |
2006年 | 4073篇 |
2005年 | 3219篇 |
2004年 | 3338篇 |
2003年 | 3140篇 |
2002年 | 2984篇 |
2001年 | 2653篇 |
2000年 | 2584篇 |
1999年 | 2190篇 |
1998年 | 2222篇 |
1997年 | 2118篇 |
1996年 | 1889篇 |
1995年 | 1761篇 |
1994年 | 1584篇 |
1993年 | 1452篇 |
1992年 | 1394篇 |
1991年 | 1274篇 |
1990年 | 1466篇 |
1989年 | 1237篇 |
1988年 | 1158篇 |
1987年 | 1350篇 |
1986年 | 1194篇 |
1985年 | 1486篇 |
1984年 | 1700篇 |
1983年 | 1550篇 |
1982年 | 1453篇 |
1981年 | 1361篇 |
1980年 | 1210篇 |
1979年 | 1188篇 |
1978年 | 1234篇 |
1977年 | 1076篇 |
1976年 | 1031篇 |
1975年 | 986篇 |
1974年 | 943篇 |
1973年 | 982篇 |
1971年 | 608篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
991.
Measurements of underwater irradiance, transparency and Secchi disc depth were carried out in Liverpool Bay during 1974. The depth of the photic zone measured in the green portion of the spectrum ranged from 5 m to 50 m, depending on location and season. Inshore values of photic depth were smaller than those encountered offshore. By mid-summer the depth of the photic zone had reached or exceeded the depth of the sea bed over the whole study area.Consideration was given to the error terms associated with the optical measurements and to the problems of using standard optical relationships in coastal waters. The relationship between Secchi disc depth and the depth of the photic zone could not be taken as constant but was a function of the absorption and scattering properties of the water mass. 相似文献
992.
J. M. Auzende 《Marine Geophysical Researches》1971,1(2):162-177
Résumé Une série de profils de sismique réflexion effectués au large de la Tunisie et dans le détroit sardano-tunisien aboutissent à l'élaboration d'un schéma géologique interprétatif dans lequel nous replaçons le socle paléozoïque et sa couverture autochtone (Eocène et plio-quaternaire) et allochtone (nappe numidienne). Nous discutons ensuite des manifestations néotectoniques (bassins d'effondrements plio-quaternaires-mouvement de flexure-surrections locales-venues intrusives). Enfin la nature du substratum du détroit sardano-tunisien est discutée en liaison avec les hypothèses dynamiques et statiques relatives à la formation de la Méditerranée occidentale.
Serial seismic reflection profiles off Tunisia and between Sardinia and Tunisia are presented. Interpretation is given which includes paleozoïc basement and its autochtonous (Eocene and plioquaternary) and allochtonous (Numidian nappe) cover. Recent tectonic activity is discussed, (Plioquaternary foundered basins, flexure, local uplifts, intrusions). Then the nature of the basement of the Sardinia-Tunisia zone is discussed with respect to the various hypotheses on the region of the Western Mediterranean.相似文献
993.
994.
995.
Experiments were conducted in an oscillatory water tunnel to investigate what effects temporal inertia has on the resistance of a granular medium. The flow law governing stationary porous media flow is reasonably well accepted and understood but the effects of unsteady flow have commonly been neglected. The present research was designed to assess the magnitude of the acceleration effects on media of uniformly packed spheres of equal diameter and on one sample of randomly placed stone.Oscillatory flow tests were made in a large oscillatory flume tunnel with periods varying from 3 to 12 seconds. The influence of properties of the medium (grain size and porosity) were tested by using spheres with two different diameters and packing each size sphere in different geometric arrangements. Tests made on a stone sample provided a qualitative assessment of the effects of more random material properties.For the experiments described in this paper, the Forchheimer unsteady-stationary flow law described the oscillatory measurements well when velocities and energy losses were maximum. Empirical coefficients determined from steady-stationary flow were generally found to apply to the unsteady flow, however some evidence of dependency on the period of oscillation was noted. 相似文献
996.
分析表观耗氧量、滴定碱度及总二氧化碳量等资料来研判红海及亚丁湾间之海水交换。结果显示,红海深层水的方解石及霰石饱和度均比亚丁湾和阿拉伯海深层水的饱和度高。红海全水柱之方解石和霰石都处於过饱和状态,亚丁湾和阿拉伯海中各深度之方解石亦呈过饱和状态,但霰石的饱和探度则大约在500m左右。分析深层水之生物体无机碳与有机碳的分解比值,可以发现此地区深层水中,大约有25%的总二氧化碳增加量是由无机碳酸钙溶解而来。 相似文献
997.
998.
The Karman Vortex Street generated by a circular cylinder is investigated by the numerical solution of the compressible Navier–Stokes equations in the incompressible Mach number range (Mach<0.3) using the Beam and Warming implicit scheme. The agreement with the fully incompressible projection method (Chorin, 1968) is fairly good while convergence time is very much better. The investigation suggests that the compressible Navier–Stokes equations may be used as an efficient alternative to study incompressible flows as well. Mach numbers just below 0.3 are enough to simulate incompressible flow behavior and at the same time do not cause numerical ill-conditioning in the solution. In addition, some relevant features of the vortices generated and carried by the wake of the cylinder could be fairly well captured. 相似文献
999.
John P. Ryan Paulo S. Polito Peter G. Strutton Francisco P. Chavez 《Progress in Oceanography》2002,55(3-4)
Unusual large-scale accumulations of phytoplankton occurred across 10,000 km of the equatorial Pacific during the 1998 transition from El Niño to La Niña. The forcing and dynamics of these phytoplankton blooms were studied using satellite-based observations of sea surface height, temperature and chlorophyll, and mooring-based observations of winds, hydrography and ocean currents. During the bloom period, the thermocline (nutricline) was anomalously shallow across the equatorial Pacific. The relative importance of processes that enhanced nutrient flux into the euphotic zone differed between the western and eastern regions of the blooms. In the western bloom region, the important vertical processes were turbulent vertical mixing and wind-driven upwelling. In contrast, the important processes in the eastern bloom region were wave-forced shoaling of nutrient source waters directly into the euphotic zone, along-isopycnal upwelling, and wind-driven upwelling. Advection by the Equatorial Undercurrent spread the largest bloom 4500 km east of where it began, and advection by meridional currents of tropical instability waves transported the bloom hundreds of kilometers north and south of the equator. Many processes influenced the intricate development of these massive biological events. Diverse observations and novel analysis methods of this work advance the conceptual framework for understanding the complex dynamics and ecology of the equatorial Pacific. 相似文献
1000.