全文获取类型
收费全文 | 76699篇 |
免费 | 1134篇 |
国内免费 | 765篇 |
专业分类
测绘学 | 2260篇 |
大气科学 | 5553篇 |
地球物理 | 14583篇 |
地质学 | 27356篇 |
海洋学 | 6673篇 |
天文学 | 18190篇 |
综合类 | 324篇 |
自然地理 | 3659篇 |
出版年
2022年 | 479篇 |
2021年 | 860篇 |
2020年 | 895篇 |
2019年 | 938篇 |
2018年 | 2107篇 |
2017年 | 2020篇 |
2016年 | 2521篇 |
2015年 | 1411篇 |
2014年 | 2419篇 |
2013年 | 4063篇 |
2012年 | 2507篇 |
2011年 | 3250篇 |
2010年 | 2791篇 |
2009年 | 3616篇 |
2008年 | 3116篇 |
2007年 | 3139篇 |
2006年 | 3001篇 |
2005年 | 2265篇 |
2004年 | 2229篇 |
2003年 | 2161篇 |
2002年 | 2072篇 |
2001年 | 1826篇 |
2000年 | 1735篇 |
1999年 | 1462篇 |
1998年 | 1480篇 |
1997年 | 1388篇 |
1996年 | 1234篇 |
1995年 | 1197篇 |
1994年 | 1070篇 |
1993年 | 924篇 |
1992年 | 876篇 |
1991年 | 887篇 |
1990年 | 933篇 |
1989年 | 788篇 |
1988年 | 774篇 |
1987年 | 888篇 |
1986年 | 761篇 |
1985年 | 953篇 |
1984年 | 1043篇 |
1983年 | 957篇 |
1982年 | 916篇 |
1981年 | 789篇 |
1980年 | 759篇 |
1979年 | 712篇 |
1978年 | 704篇 |
1977年 | 618篇 |
1976年 | 556篇 |
1975年 | 552篇 |
1974年 | 548篇 |
1973年 | 600篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
91.
Variation in Specific Capacity in Fractured Rocks, Pennsylvania 总被引:1,自引:0,他引:1
92.
93.
The article presents self-consistent computations of the spherically symmetric envelope of a massive (M=20M ⊙) star whose envelope is flowing outward under the action of continuum radiation pressure. A system of equations describing the out flow for arbitrary optical depth, degree of ionization, and opacity κ are obtained. A numerical solution is obtained for the case of constant κ and degree of ionization via approaching integrations from the singularities and smooth joining in the intermediate region. Asymptotic solutions are found in the vicinity of the sonic point and the singularity at infinity. 相似文献
94.
The stratospheric concentrations of many minor constituents change rapidly at sunrise or sunset. If this happens, there is an inherent error when retrieving the vertical profiles of the constituents from measurements of their absorption of sunlight. For retrievals of NO at sunset the error can be estimated from in-situ measurements alone, without appeal to a model of stratospheric photochemistry. Below 20 km this error can approach 100% so that the retrieved NO is zero. But at 40 km, and at 25 km when the absorption is strong and Lorentzian, it can be less than 20%. Precise calculations of the error, even if small, require model calculations of the sunset and sunrise changes. With a model, we have calculated the error for NO, NO2, OH and ClO. 相似文献
95.
96.
Ohne Zusammenfassung 相似文献
97.
Motivated by the various examples of spatial variability in the power of the acoustic spectrum, we attempted to look for spatial variability in the peak frequency of the spectrum. However, the determination of this peak frequency on a spatial scale of a single pixel (8 arc sec for the GONG data) is limited by the stochastic variations in the power spectrum presumably caused by the stochastic nature of the excitation process. Averaging over a large number of spectra (100 spectra from a 10 × 10 pixel area) produced stabler spectra. The peak frequencies of 130 such locations were found to be distributed with a FWHM of about 130 Hz. A map of the spatial variation of this peak frequency did not show any strong feature with statistically significant deviation from the mean of the distribution. Likewise, the scatter in the peak frequencies masked the detection of magnetic-field-induced changes in the peak frequency. On a much larger scale, the N latitudes showed a slightly lower value of the peak frequency as compared to the S latitudes, although the difference (25 Hz) is barely larger than the r.m.s. spread (20 Hz). 相似文献
98.
99.
100.