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   1201篇
  免费   53篇
  国内免费   1篇
林业   67篇
农学   35篇
基础科学   7篇
  118篇
综合类   331篇
农作物   83篇
水产渔业   31篇
畜牧兽医   495篇
园艺   16篇
植物保护   72篇
  2022年   10篇
  2020年   14篇
  2019年   18篇
  2018年   16篇
  2017年   17篇
  2016年   26篇
  2015年   23篇
  2014年   23篇
  2013年   38篇
  2012年   38篇
  2011年   40篇
  2010年   30篇
  2009年   15篇
  2008年   47篇
  2007年   39篇
  2006年   29篇
  2005年   36篇
  2004年   33篇
  2003年   34篇
  2002年   33篇
  2001年   22篇
  2000年   33篇
  1999年   21篇
  1998年   20篇
  1997年   15篇
  1995年   9篇
  1992年   32篇
  1991年   25篇
  1990年   35篇
  1989年   29篇
  1988年   20篇
  1987年   12篇
  1986年   21篇
  1985年   18篇
  1984年   13篇
  1983年   16篇
  1982年   14篇
  1981年   9篇
  1979年   12篇
  1976年   11篇
  1975年   11篇
  1974年   12篇
  1973年   10篇
  1972年   9篇
  1971年   15篇
  1970年   19篇
  1969年   29篇
  1968年   38篇
  1967年   35篇
  1966年   21篇
排序方式: 共有1255条查询结果,搜索用时 31 毫秒
101.
102.
The silica balance in the world ocean: a reestimate   总被引:8,自引:0,他引:8  
The net inputs of silicic acid (dissolved silica) to the world ocean have been revised to 6.1 +/- 2.0 teramoles of silicon per year (1 teramole = 10(12) moles). The major contribution (about 80 percent) comes from rivers, whose world average silicic acid concentration is 150 micromolar. These inputs are reasonably balanced by the net ouputs of biogenic silica of 7.1 +/- 1.8 teramoles of silicon per year in modern marine sediments. The gross production of biogenic silica (the transformation of dissolved silicate to particulate skeletal material) in surface waters was estimated to be 240 +/- 40 teramoles of silicon per year, and the preservation ratio (opal accumulation in sediment/gross production in surface waters) averages 3 percent. In the world ocean the residence time of silicon, relative to total biological uptake in surface waters, is about 400 years.  相似文献   
103.
Sea urchin skeletal elements are composed of single crystals of calcite. Unlike their synthetic counterparts, these crystals do not have well-developed cleavage and are consequently much more resistant to fracture. This phenomenon is due in part to the presence of acidic glycoproteins occluded within the crystals. By means of x-ray diffraction with synchrotron radiation, it is shown that the presence of the protein in synthetic calcite only slightly decreases the coherence length but significantly increases the angular spread of perfect domains of the crystals. In biogenic calcite, the coherence length is 1/3 to 1/4 as much as that in synthetic calcite and the angular spread is 20 to 50 times as wide. It is proposed that the presence of macromolecules concentrated at mosaic boundaries that are oblique to deavage planes is responsible for the change in fracture properties. These results may be important in the material sciences, because of the unusual nature of this material, namely, a composite based on the controlled intercalation of macromolecules inside single-crystal lattices.  相似文献   
104.
105.
106.
Spatial Variability of Turbulent Mixing in the Abyssal Ocean   总被引:3,自引:0,他引:3  
Ocean microstructure data show that turbulent mixing in the deep Brazil Basin of the South Atlantic Ocean is weak at all depths above smooth abyssal plains and the South American Continental Rise. The diapycnal diffusivity there was estimated to be less than or approximately equal to 0.1 x 10(-4) meters squared per second. In contrast, mixing rates are large throughout the water column above the rough Mid-Atlantic Ridge, and the diffusivity deduced for the bottom-most 150 meters exceeds 5 x 10(-4) meters squared per second. Such patterns in vertical mixing imply that abyssal circulations have complex spatial structures that are linked to the underlying bathymetry.  相似文献   
107.
108.
109.
Volcanic glass in marine sediments off Oregon and Washington correlates with continental deposits of Mount Mazama ash by stratigraphic position, refractive index, and radiocarbon dating. Ash deposited in the abyssal regions by turbidity currents is used for tracing of the dispersal routes of postglacial sediments and for evaluation of marine sedimentary processes.  相似文献   
110.
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