全文获取类型
收费全文 | 1201篇 |
免费 | 53篇 |
国内免费 | 1篇 |
专业分类
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 |
出版年
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
Tréguer P Nelson DM Van Bennekom AJ Demaster DJ Leynaert A Quéguiner B 《Science (New York, N.Y.)》1995,268(5209):375-379
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.
Berman A Addadi L Kvick A Leiserowitz L Nelson M Weiner S 《Science (New York, N.Y.)》1990,250(4981):664-667
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.
Nelson B 《Science (New York, N.Y.)》1968,160(3824):170-173
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.