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   26838篇
  免费   4919篇
  国内免费   6458篇
测绘学   1183篇
大气科学   5929篇
地球物理   7224篇
地质学   13391篇
海洋学   2947篇
天文学   1379篇
综合类   3045篇
自然地理   3117篇
  2024年   130篇
  2023年   514篇
  2022年   1163篇
  2021年   1350篇
  2020年   1120篇
  2019年   1211篇
  2018年   1528篇
  2017年   1338篇
  2016年   1602篇
  2015年   1256篇
  2014年   1630篇
  2013年   1491篇
  2012年   1362篇
  2011年   1396篇
  2010年   1507篇
  2009年   1466篇
  2008年   1322篇
  2007年   1275篇
  2006年   1022篇
  2005年   887篇
  2004年   778篇
  2003年   802篇
  2002年   741篇
  2001年   691篇
  2000年   920篇
  1999年   1389篇
  1998年   1120篇
  1997年   1115篇
  1996年   1004篇
  1995年   880篇
  1994年   828篇
  1993年   696篇
  1992年   544篇
  1991年   442篇
  1990年   324篇
  1989年   303篇
  1988年   269篇
  1987年   172篇
  1986年   149篇
  1985年   114篇
  1984年   70篇
  1983年   58篇
  1982年   70篇
  1981年   56篇
  1980年   30篇
  1979年   29篇
  1978年   10篇
  1977年   4篇
  1976年   7篇
  1958年   27篇
排序方式: 共有10000条查询结果,搜索用时 0 毫秒
941.
本试验是利用对虾(扇贝)育苗池进行室内常温培育裙带菜苗。试验证明,育苗数量完全可以达到生产上的要求,这样既可充分提高对虾(扇贝)育苗池的利用率,又可解决裙带菜苗源不足的问题,促进裙带菜养殖事业的发展。  相似文献   
942.
长江口区浮游动物生态研究   总被引:3,自引:0,他引:3  
长江口区终年有大量长江淡水流入,营养盐丰富,并且泥沙含量较大,透明度低,盐度变化幅度大(3-33)。 长江口区是我国重要渔场之一,凤鲚、刀鲚、银鱼、鲻、鲳等均在此产卵,许多海产鱼类的仔、幼鱼也在此索饵、栖息。因此长江口区浮游动物生物量的分布与其附近渔场有密切关系。  相似文献   
943.
三峡工程对长江口区无脊椎动物资源影响的预测   总被引:1,自引:0,他引:1  
长江大量径流给其河口及邻近海域带来丰富的营养物质,维持了长江河口生态系统的巨大生产力,并使之成为多种重要经济鱼虾类的索饵和产卵场。长江口生态环境的变化,对我国最大、最重要的浙江舟山渔场和江苏吕四渔场的渔业资源有举足轻重的影响。三峡工程的兴建将使长江入海径流量及其季节分配有很大改变,也不可避免地影响到河口和近海的海洋环境、经济动物的组成及资源状况。为研究长江口无脊椎动物资源结构及其分布特征,以及预测三峡工程对自然生态环境的影响,于1985年9月至1986年8月进行了无脊椎动物资源底拖网试捕调查。本文系统整理调查所得资料,结合历史资料进行分析研究。  相似文献   
944.
本文描述了1989年11月在青岛即墨岙山养殖基地所做的海水叶绿素σ浓度遥感测量的基础实验。该实验获得了高浓度叶绿素α含量的海水反射光谱。该反射光谱的特征波段为:波谷在485nm;波峰在450nm 和535nm;“节点”在572nm.根据该实验数据选取了叶绿素α浓度两种双波段估算模式.分析结果表明;两种模式的精度都在50%以上,且双波段反射率的差值法优于双波段反射率比值法.  相似文献   
945.
By using the atmosphere-ocean coupled model (CGCM) which is composed of a 2-level global atmospheric general circulation model and a 4-layer Pacific oceanic general circulation model developed in the Institute of Atmospheric Physics of Chinese Academy of Sciences, and two model climatological fields got from the two independent models' numerical integrations respectively, the Pacific sea surface temperature anomalies (SSTA) from 1988 to 1989 are simulated in this paper with observed atmospheric general circulation data and sea surface temperature fields as initial conditions and monthly coupling scheme. In order to remove systematic biases of the model climatological fields, interaction variables between atmosphere and ocean are also corrected simultaneously. The experiments show that the simulation results can be improved effectively if these interaction variables are corrected in spite of the fact that there always exist systematic biases in independent numerical simulations of atmospheric part and oc  相似文献   
946.
947.
Li  Shi-min  Cui  Pu  Zhang  Shuai  Liu  Wen-tao  Peng  Yu-xiang 《中国海洋工程》2020,34(6):828-839
China Ocean Engineering - This study is concerned with the dynamic characteristics of bubbles near two connected walls (one horizontal and the other inclined with an obtuse angle from the...  相似文献   
948.
The South Yellow Sea basin is filled with Mesozoic–Cenozoic continental sediments overlying pre-Palaeozoic and Mesozoic–Palaeozoic marine sediments. Conventional multi-channel seismic data cannot describe the velocity structure of the marine residual basin in detail, leading to the lack of a deeper understanding of the distribution and lithology owing to strong energy shielding on the top interface of marine sediments. In this study, we present seismic tomography data from ocean bottom seismogra...  相似文献   
949.
Toxic harmful algal blooms(HABs) can cause deleterious effects in marine organisms, threatening the stability of marine ecosystems. It is well known that different strains, natural populations and growth conditions of the same toxic algal species may lead to different amount of phycotoxin production and the ensuing toxicity. To fully assess the ecological risk of toxic HABs, it is of great importance to investigate the toxic effects of phycotoxins in marine organisms. In this study, the short-te...  相似文献   
950.
The East China Sea Shelf Basin generated a series of back-arc basins with thick successions of marine- and terrestrial-facies sediments during Cenozoic. It is enriched with abundant oil and gas resources and is of great significance to the petroleum exploration undertakings. Therein, the Lishui Sag formed fan delta, fluvial delta and littoral-to-neritic facies sediments during Paleocene–Eocene, and the research on its sedimentary environment and sediment source was controversial. This study analyzed the paleontological combination characteristics, and conducted a source-to-sink comparative analysis to restore the sedimentary environment and provenance evolution of the Lishui Sag during Paleocene–Eocene based on the integration of detrital zircon U-Pb age spectra patterns with paleontological assemblages. The results indicated that Lishui Sag was dominated by littoral and neritic-facies environment during time corroborated by large abundance of foraminifera, calcareous nannofossils and dinoflagellates. Chronological analysis of detrital zircon U-Pb revealed that there were significant differences in sediment sources between the east and west area of the Lishui Sag. The western area was featured by deeper water depths in the Paleocene–Eocene, and the sediment was characterized by a single Yanshanian peak of zircon U-Pb age spectra, and mainly influenced from Yanshanian magmatic rocks of South China Coast and the surrounding paleo-uplifts. However, its eastern area partly showed Indosinian populations. In particular, the upper Eocene Wenzhou sediments were featured by increasingly plentiful Precambrian zircons in addition to the large Indosinian-Yanshanian peaks, indicating a possible impact from the Yushan Low Uplift to the east. Therefore, it is likely that the eastern Lishui Sag generated large river systems as well as deltas during time. Due to the Yuquan Movement, the Lishui Sag experienced uplifting and exhumation in the late stage of the late Eocene and was not deposited with sediments until Miocene. Featured by transitional-facies depositions of Paleocene–Eocene, the Lishui Sag thus beared significant potential for source rock and oil-gas reservoir accumulation.  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