全文获取类型
收费全文 | 37627篇 |
免费 | 7687篇 |
国内免费 | 11403篇 |
专业分类
测绘学 | 1882篇 |
大气科学 | 8730篇 |
地球物理 | 6803篇 |
地质学 | 20631篇 |
海洋学 | 6241篇 |
天文学 | 348篇 |
综合类 | 3155篇 |
自然地理 | 8927篇 |
出版年
2024年 | 143篇 |
2023年 | 498篇 |
2022年 | 1354篇 |
2021年 | 1550篇 |
2020年 | 1569篇 |
2019年 | 1830篇 |
2018年 | 1654篇 |
2017年 | 1748篇 |
2016年 | 1798篇 |
2015年 | 1957篇 |
2014年 | 2500篇 |
2013年 | 2558篇 |
2012年 | 2652篇 |
2011年 | 2651篇 |
2010年 | 2207篇 |
2009年 | 2626篇 |
2008年 | 2493篇 |
2007年 | 2820篇 |
2006年 | 2782篇 |
2005年 | 2449篇 |
2004年 | 2289篇 |
2003年 | 2050篇 |
2002年 | 1852篇 |
2001年 | 1552篇 |
2000年 | 1384篇 |
1999年 | 1320篇 |
1998年 | 1044篇 |
1997年 | 986篇 |
1996年 | 848篇 |
1995年 | 690篇 |
1994年 | 638篇 |
1993年 | 529篇 |
1992年 | 422篇 |
1991年 | 352篇 |
1990年 | 209篇 |
1989年 | 232篇 |
1988年 | 144篇 |
1987年 | 95篇 |
1986年 | 50篇 |
1985年 | 46篇 |
1984年 | 24篇 |
1983年 | 17篇 |
1982年 | 15篇 |
1981年 | 8篇 |
1980年 | 13篇 |
1979年 | 18篇 |
1978年 | 14篇 |
1977年 | 18篇 |
1976年 | 3篇 |
1954年 | 8篇 |
排序方式: 共有10000条查询结果,搜索用时 46 毫秒
991.
2001年昆仑山口8.1级巨震后中国大陆、云南地震趋势研究 总被引:2,自引:1,他引:2
分析研究了2001年11月14日昆仑山口8.1级巨震对中国大陆云南未来几年地震趋势的影响,指出巨震后6年大陆可能仍然处于地震活跃期,其间大陆西部发生7.0级以上大震可能性较大;受2000-2001年欧亚带东南段大震活动过程及巨震调整影响,未来1-3年云南省可能进入新的活跃期,6.5级以上强震危险性增加。 相似文献
992.
大姚地热动态特征分析 总被引:3,自引:1,他引:3
通过大姚高精度水温观测井水地质、井孔条件的分析,震例观测资料、实验观测数据的处理,以及井水水质分析结果,表明大姚水温周期性变化的突出位置是井深75m左右,根本原因是该地层石膏脉稳定释热,含水层热水与井内冷水混合过程中,在通道内形成钙盐类沉淀物(如CaSO4CaCO3),堵塞对流通道,含水层内外压差突破被阻塞通道,热水反复侵入井内,便形成水温周期性变化。地震的孕育、发生和调整过程,由于应力场作用,产生附加地热场,水温基值发生变化,周期畸变或消失,这种附加地热动态是可以恢复的。所以认为大姚地热动态是井区特殊地层地热信息的反映。 相似文献
993.
Benthic foraminiferal oxygen and carbon isotopic records from Southern Ocean sediment cores show that during the last glacial period, the South Atlantic sector of the deep Southern Ocean filled to roughly 2500 m with water uniformly low in δ13C, resulting in the appearance of a strong mid-depth nutricline similar to those observed in glacial northern oceans. Concomitantly, deep water isotopic gradients developed between the Pacific and Atlantic sectors of the Southern Ocean; the δ13C of benthic foraminifera in Pacific sediments remained significantly higher than those in the Atlantic during the glacial episode. These two observations help to define the extent of what has become known as the ‘Southern Ocean low δ13C problem’. One explanation for this glacial distribution of δ13C calls upon surface productivity overprints or changes in the microhabitat of benthic foraminifera to lower glacial age δ13C values. We show here, however, that glacial-interglacial δ13C shifts are similarly large everywhere in the deep South Atlantic, regardless of productivity regime or sedimentary environment. Furthermore, the degree of isotopic decoupling between the Atlantic and Pacific basins is proportional to the magnitude of δ13C change in the Atlantic on all time scales. Thus, we conclude that the profoundly altered distribution of δ13C in the glacial Southern Ocean is most likely the result of deep ocean circulation changes. While the characteristics of the Southern Ocean δ13C records clearly point to reduced North Atlantic Deep Water input during glacial periods, the basinal differences suggest that the mode of Southern Ocean deep water formation must have been altered as well. 相似文献
994.
995.
新疆北部降水的气候分布特片及其对ENSO的响应 总被引:1,自引:2,他引:1
分析研究了新疆北部地区近50年(1951-2000年)全年各月降水的气候分布特征和各季降水的年际变化规律,重点揭示了北疆多雨季节(4-7月)及其各月降水量对赤道东太平洋的海温SST和南方涛动指数SOI的显著响应关系,并用前期SST和SOI作为预报因子,建立了北疆地区雨季水量的预报方程。该方程可用于北疆地区雨季降水量的长期预报。 相似文献
996.
997.
PRELIMINARY NUMERICAL STUDY OF TOPOGRAPHIC EFFECTS OF THE TIBETAN PLATEAU ON SURFACE DIRECT RADIATION 总被引:3,自引:0,他引:3
To improve the simulating ability of a model,this paper presents a scheme of calculatingdirect radiation at land surface with topography in the model.A numerical study is conducted forthe topographic effects of the Tibetan Plateau on the direct radiation using NCEP terrain data.Results show that,after taking account into the topographic radiation effect,the regional averageof the radiation over the Plateau obviously increases in the local early morning and late afternoon,but changes less around noon.The effect is stronger in winter than that in summer.Andheterogeneous topography has also affected the distribution of the radiation in this area.A simplenumerical experiment shows that considering the effect will lead ground temperature to increase onthe slope having more sunshine,and vice versa. 相似文献
998.
SIMULATION OF HEAVY RAINFALL IN THE SUMMER OF 1998 OVER CHINA WITH REGIONAL CLIMATE MODEL 总被引:11,自引:0,他引:11
The heavy rainfall in the summer of 1998 over China has been simulated with the NCCRegional Climate Model(RegCM_NCC).It was successful for RegCM_NCC to reproduce thelocation and seasonal shift of the seasonal rain belt in the summer of 1998 over China.The rainyseason in the summer of 1998 over China can be divided into 7 episodes,including the pre-summerrainy season in South China.the Meiyu onset over the Yangtze-Huaihe River Basin,shortappearance of North China rain season and the retreat of seasonal rain belt,the second Meiyuseason over the Yangtze River Valley,the rainy period over the Yellow and Huaihe River Valleyand the seasonal retreat of rain belt over North China.The shortcoming of the RegCM_NCC isover-estimation of precipitation amounts.The regions with large latent heat flux,upper soilmoisture and total runoff are located in the rainy area and move with the simulated rain belt duringthe different episodes.On the contrary,the regions with small sensible heat flux are located in thesimulated rainy area and move with the simulated rain belt during the different episodes. 相似文献
999.
Quantitative reconstruction of the lake water paleotemperature of Daihai Lake, Inner Mongolia, China and its significance in paleoclimate 总被引:5,自引:2,他引:5
By measuring Sr/Ca ratios of the ostracod shells (Limnocthere cf. inopinata) in sediments of the Daihai Lake, and combined with Sr2+/Ca2+ ratios of the lake water, this paper obtained paleosalinity of the lake water. Vaporizing experiment of the lake water in
laboratory showed that there was a quantitative relationship between salinity and oxygen isotope. Using this relationship,
oxygen isotope values of the paleo-lake water were calculated. By measuring the oxygen isotope of the authigenic carbonate
in the lake’s sediments, and in combination with the oxygen isotope values of the paleo-lake water, the paleotemperature of
the lake water was calculated. Finally, based on these proxies, the paleoclimate in the lake basin was explored. 相似文献
1000.
中国耕地有机质含量变化对土地生产力影响的定量研究 总被引:23,自引:6,他引:23
在土地持续利用与管理研究中,土地质量变化对土地生产力影响的定量研究是核心内容之一。借助新古典经济学的生产函数法,构建了我国耕地的生产函数模型,定量模拟了我国耕地有机质含量变化的边际产出率性和边际生产力。初步结果表明,由于我国长期存在耕过度利用导致有机质含量及肥力下降问题,当前提高耕地质量的增产潜力十分可观。 相似文献