全文获取类型
收费全文 | 8782篇 |
免费 | 1969篇 |
国内免费 | 3198篇 |
专业分类
测绘学 | 1192篇 |
大气科学 | 1318篇 |
地球物理 | 1767篇 |
地质学 | 5924篇 |
海洋学 | 1847篇 |
天文学 | 113篇 |
综合类 | 754篇 |
自然地理 | 1034篇 |
出版年
2024年 | 100篇 |
2023年 | 260篇 |
2022年 | 561篇 |
2021年 | 655篇 |
2020年 | 535篇 |
2019年 | 655篇 |
2018年 | 575篇 |
2017年 | 542篇 |
2016年 | 589篇 |
2015年 | 652篇 |
2014年 | 665篇 |
2013年 | 698篇 |
2012年 | 791篇 |
2011年 | 745篇 |
2010年 | 729篇 |
2009年 | 691篇 |
2008年 | 728篇 |
2007年 | 655篇 |
2006年 | 643篇 |
2005年 | 502篇 |
2004年 | 394篇 |
2003年 | 276篇 |
2002年 | 216篇 |
2001年 | 227篇 |
2000年 | 219篇 |
1999年 | 137篇 |
1998年 | 83篇 |
1997年 | 82篇 |
1996年 | 63篇 |
1995年 | 53篇 |
1994年 | 28篇 |
1993年 | 32篇 |
1992年 | 25篇 |
1991年 | 25篇 |
1990年 | 9篇 |
1989年 | 19篇 |
1988年 | 11篇 |
1987年 | 18篇 |
1986年 | 8篇 |
1985年 | 11篇 |
1984年 | 6篇 |
1983年 | 10篇 |
1982年 | 3篇 |
1981年 | 2篇 |
1980年 | 2篇 |
1979年 | 2篇 |
1978年 | 2篇 |
1976年 | 2篇 |
1957年 | 2篇 |
1954年 | 7篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
151.
2002年3月3日大桥水库诱发了Ms4.6级水库地震,其发震构造是安宁河东支断裂近傍具有正断层性质的一个分支断裂。据大桥台网7年多库区地震观测事件记录,地震空间分布上水体附近有一个明显的活跃过程,大坝上游发生小震群,大坝下游发生主震序列。地震的震源深度在蓄水前后有明显变化。4.6级地震的震源机制解的主压应力轴方位和倾角与大多数活动断裂上的地震有明显的差别,主压应力轴的倾角与其它的水库地震相比也存在较大差别。 相似文献
152.
The time history of strong ground motion can be synthesized by empirical Green's function (EGF) method.Firstly a large seismic event is discretized into a series of subevents; secondly recordings of earthquakes with proper size and spatial distribution are chosen as time history (EGF) of those subevents; finally the EGFs are summated to get the time history of ground motion caused by the large event. 相似文献
153.
High buildings or architectural complex in urban areas remarkably distort the urban surface wind fields. As the air flow approaches,local strong wind may appear around the buildings. The strong wind makes the pedestrians on sidewalks, entrances and terrace very uncomfortable and causes the pedestrian level wind environment problem. In this studies, hot-wire wind measurement, wind scouring in wind tunnel and numerical computation were carried out to evaluate the wind environment of tall buildings in the prevailing flow conditions in Beijing areas. The results obtained by three techniques were compared and mutually verified. The conclusions drawn from three approaches agree with each other. Also the advantages and limitations of each method were analyzed. It is suggested that the combination of different techniques may produce better assessment of wind environment around high buildings. 相似文献
154.
155.
The influence of cavern’s span on surrounding rock classification is getting more and more recognition along with large span underground working’s increasingly coming forth. The authors analyse the timbering expense of cavern in jointed rock mass, the radius of plastic loosened zone and the size effect of macroscopical mechanical parameters of rock mass. Based on the complexion of depressing of surrounding rock’s stability due to increment of cavern’s span, the authors pinpoint attaching importance to the influence of cavern’s span on surrounding rock classification; and suggest reckoning the factor of cavern’s span in surrounding rock classification scientifically by studying the size effect of rock mass’s physico-mechanical parameters. 相似文献
156.
Bin Chen 《Geochimica et cosmochimica acta》2005,69(22):5387-5388
157.
158.
159.
Piecewise prediction model for watershed‐scale erosion and sediment yield of individual rainfall events on the Loess Plateau,China 下载免费PDF全文
Yu Guo‐Qiang Zhang Mao‐Sheng Li Zhan‐Bin Li Peng Zhang Xia Cheng Sheng‐Dong 《水文研究》2014,28(21):5322-5336
Establishing a universal watershed‐scale erosion and sediment yield prediction model represents a frontier field in erosion and soil/water conservation. The research presented here was conducted on the Chabagou watershed, which is located in the first sub‐region of the hill‐gully area of the Loess Plateau, China. A back‐propagation artificial neural model for watershed‐scale erosion and sediment yield was established, with the accuracy of the model, then compared with that of multiple linear regression. The sensitivity degree of various factors to erosion and sediment yield was quantitatively analysed using the default factor test. On the basis of the sensitive factors and the fractal information dimension, the piecewise prediction model for erosion and sediment yield of individual rainfall events was established and further verified. The results revealed the back‐propagation artificial neural network model to perform better than the multiple linear regression model in terms of predicting the erosion modulus, with the former able to effectively characterize dynamic changes in sediment yield under comprehensive factor conditions. The sensitivity of runoff erosion power and runoff depth to the erosion and sediment yield associated with individual rainfall events was found to be related to the complexity of surface topography. The characteristics of such a hydrological response are thus closely related to topography. When the fractal information dimension is greater than the topographic threshold, the accuracy of prediction using runoff erosion power is higher than that of using runoff depth. In contrast, when the fractal information dimension is smaller than the topographic threshold, the accuracy of prediction using runoff depth is higher than that of using runoff erosion power. The developed piecewise prediction model for watershed‐scale erosion and sediment yield of individual rainfall events, which introduces runoff erosion power and runoff depth using the fractal information dimension as a boundary, can be considered feasible and reliable and has a high prediction accuracy. Copyright © 2013 John Wiley & Sons, Ltd. 相似文献
160.
Huawu Wu Jinglu Wu Kadyrbek Sakiev Jinzhao Liu Jing Li Bin He Ya Liu Beibei Shen 《水文研究》2019,33(12):1658-1669
Characterization of spatial and temporal variability of stable isotopes (δ18O and δ2H) of surface waters is essential to interpret hydrological processes and establish modern isotope–elevation gradients across mountainous terrains. Here, we present stable isotope data for river waters across Kyrgyzstan. River water isotopes exhibit substantial spatial heterogeneity among different watersheds in Kyrgyzstan. Higher river water isotope values were found mainly in the Issyk‐Kul Lake watershed, whereas waters in the Son‐Kul Lake watershed display lower values. Results show a close δ18O–δ2H relation between river water and the local meteoric water line, implying that river water experiences little evaporative enrichment. River water from the high‐elevation regions (e.g., Naryn and Son‐Kul Lake watershed) had the most negative isotope values, implying that river water is dominated by snowmelt. Higher deuterium excess (average d = 13.9‰) in river water probably represents the isotopic signature of combined contributions from direct precipitation and glacier melt in stream discharge across Kyrgyzstan. A significant relationship between river water δ18O and elevation was observed with a vertical lapse rate of 0.13‰/100 m. These findings provide crucial information about hydrological processes across Kyrgyzstan and contribute to a better understanding of the paleoclimate/elevation reconstruction of this region. 相似文献