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   583篇
  免费   23篇
  国内免费   4篇
测绘学   15篇
大气科学   50篇
地球物理   153篇
地质学   210篇
海洋学   30篇
天文学   120篇
综合类   1篇
自然地理   31篇
  2021年   5篇
  2020年   4篇
  2018年   17篇
  2017年   13篇
  2016年   17篇
  2015年   24篇
  2014年   18篇
  2013年   23篇
  2012年   24篇
  2011年   43篇
  2010年   31篇
  2009年   34篇
  2008年   21篇
  2007年   24篇
  2006年   13篇
  2005年   16篇
  2004年   12篇
  2003年   18篇
  2002年   10篇
  2001年   9篇
  2000年   16篇
  1999年   14篇
  1998年   13篇
  1997年   10篇
  1996年   5篇
  1995年   9篇
  1993年   9篇
  1992年   9篇
  1991年   5篇
  1990年   6篇
  1989年   7篇
  1988年   9篇
  1987年   5篇
  1986年   6篇
  1984年   6篇
  1983年   5篇
  1982年   4篇
  1981年   5篇
  1980年   4篇
  1979年   4篇
  1976年   6篇
  1975年   4篇
  1973年   7篇
  1970年   8篇
  1969年   4篇
  1968年   4篇
  1952年   6篇
  1951年   4篇
  1950年   4篇
  1949年   4篇
排序方式: 共有610条查询结果,搜索用时 15 毫秒
141.
142.
143.
144.
As evidenced by catastrophic cadmium and mercury poisonings in japan, heavy metals belong to the most toxic environmental pollutants. Through the investigation of sediments, the extent, distribution and provenance of heavy metal contamination in rivers and lakes can be determined and traced. Eight heavy metals from the clay fraction of sediments from major rivers within the Federal Republic of Germany were determined by means of atomic adsorption spectrometry. Heavy metals especially known for their high toxicity are enriched most: mercury, lead and zinc by a factor of 10; cadmium by a factor of 50, as compared with the natural background of these elements. A mobilisation of heavy metals from the suspended load and from the sediments, as to be observed in rivers approaching the marine enviromment, could endanger marine organisms, thus negatively influencing the acquatic food chain. With a further increase of heavy metal pollution, a threat to the drinking water supplied by rivers and lakes cannot be excluded.  相似文献   
145.
146.
The structural phase transition in titanite is correlated with a strong temperature dependence of Raman scattering cross sections and, to a somewhat lesser extent, with shifts of the phonon frequencies. Their quantitative temperature evolution in the low-symmetry phase (P21/a) is compatible with a nearly 2D Ising behaviour with β≈0.12 and T c = 497 K. At temperatures above 860 K, the phonon signals agree with A 2/a symmetry but not in the temperature interval between 497 K and 860 K. In this temperature range new structural states give rise to additional phonon signals. A model based on mobile APBs between slabs of P21/a material, first proposed by van Heurck et al. (1991), is in qualitative agreement with our experimental observations.  相似文献   
147.
Summary Analysis of saturation magnetization measurements and data from the literature indicate that the cation distribution in the titanomagnetite solid solution series is temperature dependent. The ionic configuration of ferric and ferrous ions on both lattice sites of their spinel structure can be described by a modified Boltzmann relation in agreement with theoretical consideratios. Thermodynamic equilibrium isotherms for the cation distribution and the resulting variation of saturation magnetization are calculated on the basis of the experimental values. These results should be especially valuable for the interpretation of magnetic properties of rapidly cooled igneous rock units where a respective high-temperature metastable state may exist in the magnetic ore component.Further measurements of the Curie temperature and lattice constant did not confirm a similar effect. Both these parameters should therefore be qualified for the identification of naturally occurring titanomagnetites.  相似文献   
148.
149.
The growth of algae in batch cultures is often well characterized by the logistic growth function. The equation used contents three parameters which have to be estimated. Two methods are presented: The linearizing procedure, and the direct method of least squares. We give an example for comparing several logistic growth curves.  相似文献   
150.
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