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   969篇
  免费   104篇
  国内免费   3篇
  2013年   13篇
  2012年   18篇
  2011年   12篇
  2010年   15篇
  2009年   19篇
  2008年   16篇
  2007年   17篇
  2006年   9篇
  2005年   11篇
  2004年   8篇
  1999年   11篇
  1998年   8篇
  1997年   14篇
  1996年   13篇
  1995年   13篇
  1994年   14篇
  1993年   15篇
  1992年   18篇
  1991年   18篇
  1990年   11篇
  1989年   18篇
  1988年   12篇
  1987年   12篇
  1986年   10篇
  1985年   8篇
  1984年   15篇
  1983年   11篇
  1982年   10篇
  1981年   10篇
  1980年   18篇
  1979年   15篇
  1978年   9篇
  1977年   17篇
  1976年   11篇
  1975年   10篇
  1974年   8篇
  1972年   8篇
  1971年   12篇
  1959年   27篇
  1958年   43篇
  1957年   48篇
  1956年   50篇
  1955年   51篇
  1954年   49篇
  1953年   52篇
  1952年   54篇
  1951年   55篇
  1950年   32篇
  1949年   29篇
  1948年   21篇
排序方式: 共有1076条查询结果,搜索用时 453 毫秒
51.
MATHEW, B., 1992. A review of Erythronium L. (Liliaceae). The morphology, distribution and horticultural value of the genus is reviewed and a tentative key to the identification of the species is provided.  相似文献   
52.
53.
ABSTRACT

Bioacoustics researchers can use a computer as a powerful tool to measure, classify, compare and synthetise sounds. Vocalisations on tape are commonly converted to a digital format suitable for a computer by using an analogue to digital converter and then a Fourier transformation. Alternatively, sonagrams can be measured, for example by using a digitising pad or an image analysis system. Correlations and indices of similarity have been used to compare sounds, but variations in both the time and frequency dimensions of a noise are a problem. A solution may be the use of pattern recognition methods such as elastic matching and time warping. These methods are briefly described and assessed.  相似文献   
54.
55.
56.
57.
58.
59.
60.
Warmer and drier climates over Eastern Amazonia have been predicted as a component of climate change during the next 50–100 years. It remains unclear what effect such changes will have on forest–atmosphere exchange of carbon dioxide (CO2) and water, but the cumulative effect is anticipated to produce climatic feedback at both regional and global scales. To allow more detailed study of forest responses to soil drying, a simulated soil drought or 'throughfall exclusion' (TFE) experiment was established at a rain forest site in Eastern Amazonia, Brazil, for which time-series sap flow and soil moisture data were obtained. The experiment excluded 50% of the throughfall from the soil. Sap flow data from the forest plot experiencing normal rainfall showed no limitation of transpiration throughout the two monitored dry seasons. Conversely, data from the TFE showed large dry season declines in transpiration, with tree water use restricted to 20% of that in the control plot at the peak of both dry seasons. The results were examined to evaluate the paradigm that the restriction on transpiration in the dry season was caused by limitation of soil-to-root water transport, driven by low soil water potential and high soil-to-root hydraulic resistance. This paradigm, embedded in the soil–plant–atmosphere (SPA) model and driven using on-site measurements, provided a good explanation ( R 2 > 0.69) of the magnitude and timing of changes in sap flow and soil moisture. This model-data correspondence represents a substantial improvement compared with other ecosystem models of drought stress tested in Amazonia. Inclusion of deeper rooting should lead to lower sensitivity to drought than the majority of existing models. Modelled annual GPP declined by 13–14% in response to the treatment, compared with estimated declines in transpiration of 30–40%.  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