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   5732篇
  免费   1321篇
  国内免费   1720篇
测绘学   244篇
大气科学   1430篇
地球物理   700篇
地质学   1704篇
海洋学   3237篇
天文学   83篇
综合类   454篇
自然地理   921篇
  2024年   14篇
  2023年   97篇
  2022年   211篇
  2021年   285篇
  2020年   267篇
  2019年   272篇
  2018年   291篇
  2017年   268篇
  2016年   281篇
  2015年   332篇
  2014年   359篇
  2013年   462篇
  2012年   342篇
  2011年   340篇
  2010年   277篇
  2009年   405篇
  2008年   377篇
  2007年   411篇
  2006年   383篇
  2005年   373篇
  2004年   323篇
  2003年   314篇
  2002年   285篇
  2001年   256篇
  2000年   231篇
  1999年   201篇
  1998年   188篇
  1997年   162篇
  1996年   131篇
  1995年   105篇
  1994年   112篇
  1993年   90篇
  1992年   66篇
  1991年   49篇
  1990年   50篇
  1989年   45篇
  1988年   38篇
  1987年   16篇
  1986年   5篇
  1985年   17篇
  1984年   7篇
  1983年   10篇
  1982年   10篇
  1981年   9篇
  1980年   2篇
  1979年   2篇
  1977年   1篇
  1954年   1篇
排序方式: 共有8773条查询结果,搜索用时 375 毫秒
131.
1996年6月初,对福建省平潭县真鲷网箱养殖场发生的弧菌病进行研究,并确定该病病原菌为最小弧菌(Vibrio mimicus)。采用硫酸铵沉淀、DEAE-纤维素层析及Sephadex-G100层析等方法对最小弧菌产生的外毒素进行研究。结果表明,该外毒素为单一的多肽,分子量为30.456kD,对真鲷的LD50为4.48μg,对真鲷等养殖动物的溶血性最强,对Vero细胞的CD50值为0.48μg,肠毒性弱阳性。该外毒素与最小弧菌产生的其他毒力因子相比,性质独特,是一类新的毒力因子,建议命名为Vm-Pm毒素。  相似文献   
132.
Phytoplankton pigments and size-fractionated biomass in the Chukchi and Beaufort Seas showed spatial and temporal variation during the spring and summer of 2002. Cluster analysis of pigment ratios revealed different assemblages over the shelf, slope and basin regions. In spring, phytoplankton with particle sizes greater than 5 μm, identified as diatoms and/or haptophytes, dominated over the shelf. Smaller (<5 μm) phytoplankton containing chlorophyll b, most likely prasinophytes, were more abundant over the slope and basin. Due to extensive ice cover at this time, phytoplankton experienced low irradiance, but nutrients were near maximal for the year. By summer, small prasinophytes and larger haptophytes and diatoms co-dominated in near-surface assemblages in largely ice-free waters when nitrate was mostly depleted. Deeper in the water column at 1–15% of the surface irradiance larger sized diatoms were still abundant in the upper nutricline. Phytoplankton from the shelf appeared to be advected through Barrow Canyon to the adjacent basin, explaining similar composition between the two areas in spring and summer. Off-shelf advection was much less pronounced for other slope and basin areas, which are influenced by the low-nutrient Beaufort gyre circulation, leading to a dominance of smaller prasinophytes and chlorophytes. The correlation of large-sized fucoxanthin containing phytoplankton with the higher primary production measurements shows promise for trophic status to be estimated using accessory pigment ratios.  相似文献   
133.
Hydrographic properties from CTD and discrete bottle sample profiles covering the Japan (East) Sea in summer, 1999, are presented in vertical sections, maps at standard depths, maps on isopycnal surfaces, and as property–property distributions. This data set covers most of the Sea with the exception of the western boundary region and northern Tatar Strait, and includes nutrients, pH, alkalinity, and chlorofluorocarbons, as well as the usual temperature, salinity, and oxygen observations.  相似文献   
134.
Gerald Müller   《Ocean Engineering》2007,34(11-12):1786-1789
Wave run-up, and flow visualization experiments were conducted with a 1:2 sloped sea wall model. The visualization experiments gave an overview of flow fields in reflected, non-breaking conditions. Maximum particle velocities were found to be significantly smaller than suggested in the literature. Downrush produced a fast sheet flow, extending down to the toe of the sea wall. This created a ‘reverse’ breaker during the retreat of the initially non-breaking wave, which explains the high-energy dissipation rates for non-breaking waves reported in the literature. Embankments may therefore be exposed to wave impact pressures in areas up to 1.18H0 below MWL.  相似文献   
135.
The global community's ability to assess the environmental effects of marine scientific research (MSR) as required by the 1982 United Nations Convention on the Law of the Sea's (UNCLOS) marine environment provisions (MEP) is limited, as shown by experimental activities that intentionally manipulate the marine environment. Such work enhances knowledge of the ocean, but it may also have significant environmental effects. This growing use of the ocean as a laboratory has global scientific, environmental, legal and policy implications. Examined here is the relationship between the MSR and the MEP provisions of UNCLOS. International, science-driven guidelines are proposed.  相似文献   
136.
By using remote sensing (ERS) data, FSU data, COADS data and Hellerman & Rosen-stein objective analysis data to analyze the sea surface wind stress in the South China Sea, it is found that the remote sensing data have higher resolution and more reasonable values. Therefore we suggest that remote sensing data be chosen in the study of climatological features of sea surface wind stress and its seasonal variability in the South China Sea, especially in the study of small and middle scale eddies.  相似文献   
137.
南沙群岛海域水体漫衰减系数Kd(490)的特性研究   总被引:6,自引:1,他引:6  
对南沙群岛海区水体Kd(490)的特性进行了深入分析和探讨,研究结果表明:Kd(490)的垂直分布与同步测量的海水叶绿素a浓度的垂直分布有很强的相关性;Kd(490)的垂直分布反映出该区域海水存在较强的分层现象,研究中还发现上行辐亮度漫衰减系数KL(490)与Kd(490)垂直变化趋势相当一致,但是以二者达到最大值的深度为界,上层水体的KL(490)值稍大于Kd(490)值,在这一深度以下则相反。  相似文献   
138.
海水温度和盐度对泥蚶幼虫和稚贝生长及存活的影响   总被引:24,自引:0,他引:24  
1996~1997和1999年在浙江省乐清市东发水产育苗场和福建省宁德市四海水产育苗场分别研究了海水温度和盐度对泥蚶浮游幼虫和稚贝生长及存活的影响,结果表明,泥蚶浮游幼虫的适宜温度为25~33℃,最适生长温度为28~30℃.稚贝的适宜温度为15~35℃,最适生长温度为25~30℃.浮游幼虫的适宜盐度为16.54~30.02,最适生长盐度为1654~23.38;稚贝的适宜盐度为10.01~30.02,最适生长盐度为10.01~23.38.泥蚶幼虫和稚贝对高温和低盐海水有较强的适应能力,这与它们夏季的繁殖期和自然分布于内湾河口区是相适应的.  相似文献   
139.
本文记述了南海晚第四纪沉积物中发现的两个新种[线形辐环藻(Actinocyclus lineatus Liu,Cheng et Lan sp.nov.)、星圆筛藻(Coscinodiscus aster-aeus Cheng,Liu et Lan sp.nov.)]以及在我国首次记录的圆筛藻的7个种。  相似文献   
140.
The aim of the Japanese-French Kaiyo 87 cruise was the study of the spreading axis in the North Fiji Basin (SW Pacific). A Seabeam and geophysical survey allowed us to define the detailed structure of the active NS spreading axis between 16° and 22° S and its relationships with the left lateral motion of the North Fiji Fracture Zone. Between 21° S and 18°10′ S, the spreading axis trends NS. From 18°10 S to 16°40 S the orientation of the spreading axis changes from NS to 015°. North of 16°40′ S the spreading axis trends 160°. These two 015° and 160° branches converge with the left lateral North Fiji fracture zone around 16°40′ S to define an RRFZ triple junction. Water sampling, dredging and photo TV deep towing give new information concerning the hydrothermal activity along the spreading axis. The discovery of hydrothermal deposits associated with living communities confirms this activity.  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