全文获取类型
收费全文 | 21305篇 |
免费 | 3853篇 |
国内免费 | 4951篇 |
专业分类
测绘学 | 1301篇 |
大气科学 | 4364篇 |
地球物理 | 5911篇 |
地质学 | 10128篇 |
海洋学 | 2923篇 |
天文学 | 877篇 |
综合类 | 2053篇 |
自然地理 | 2552篇 |
出版年
2024年 | 89篇 |
2023年 | 336篇 |
2022年 | 929篇 |
2021年 | 1080篇 |
2020年 | 874篇 |
2019年 | 967篇 |
2018年 | 1108篇 |
2017年 | 1043篇 |
2016年 | 1196篇 |
2015年 | 972篇 |
2014年 | 1170篇 |
2013年 | 1290篇 |
2012年 | 1172篇 |
2011年 | 1156篇 |
2010年 | 1237篇 |
2009年 | 1149篇 |
2008年 | 986篇 |
2007年 | 1047篇 |
2006年 | 756篇 |
2005年 | 745篇 |
2004年 | 574篇 |
2003年 | 650篇 |
2002年 | 665篇 |
2001年 | 632篇 |
2000年 | 747篇 |
1999年 | 1061篇 |
1998年 | 826篇 |
1997年 | 846篇 |
1996年 | 801篇 |
1995年 | 716篇 |
1994年 | 626篇 |
1993年 | 555篇 |
1992年 | 450篇 |
1991年 | 321篇 |
1990年 | 247篇 |
1989年 | 205篇 |
1988年 | 189篇 |
1987年 | 110篇 |
1986年 | 124篇 |
1985年 | 75篇 |
1984年 | 60篇 |
1983年 | 61篇 |
1982年 | 61篇 |
1981年 | 43篇 |
1980年 | 45篇 |
1979年 | 38篇 |
1978年 | 15篇 |
1977年 | 9篇 |
1974年 | 9篇 |
1958年 | 17篇 |
排序方式: 共有10000条查询结果,搜索用时 62 毫秒
121.
122.
南海尖峰海山多金属结壳地球化学 总被引:4,自引:5,他引:4
南海尖峰海山多金属结壳富含30多种元素,其锰铁矿物主要由钡镁锰矿,δ-MnO_2和FeOOH·xH_2O组成。与其它海区的结壳相比,尖峰海山结壳富含Cu、Ni、Ba、Zn、Pb等元素,而Co、Ti、稀土元素(REE)、Sr等元素相对较贫。研究表明,HREE亏损,具明显的Ce正异常,较明显的Tb正异常和Yb负异常。这是氧化弱碱性海洋环境所致。结壳是水成作用的产物,它的形成受南海独特的古海洋环境所控制,海底火山热液作用,可能也是影响因素之一。 相似文献
123.
珠江口现代沉积速率及其反映的沉积特征 总被引:2,自引:0,他引:2
文章分析了珠江河口海区泥沙来源及淤积动态,采用以历史海图分析对比为主,~(210)Pb测年数据校核等方法,参考有关沉积速率定性方面的标志,推算出珠江口不同地段的现代沉积速率,并相应划分出高速率沉积、快速率沉积、中速率沉积和慢速率沉积或稍有侵蚀等4个分区.进而,还论述了沉积作用的特征. 相似文献
124.
A one-dimentional three-layer model for the thermal structure in the Huanghai Sea is presented in this study, me model consists of the upper mixed layer caused by heating and wind mixing, the lower mixed layer driven by tidal mixing, and the thermocline with certain thickness. The entrainment velocities of the upper and lower layers are obtained respectively. The results show that the model is capable of describing the development and decline processes of the seasonal thermocline in the Huanghai Sea, simulating successfully the Huanghai Sea Cold Water Mass, the nearshore front and surface cold water off North Jiangsu and explaining reasonably their formation mechanisms as well as the strong thermocline off Qingdao. It is suggested that the tidal mixing plays key role in the formation of the nearshore front off North Jiangsu and the strong thermocline off Qingdao. The wind mixing and the tidal mixing make the lower layer water with high nutrients go up to the upper layer. This physical process may be sig 相似文献
125.
Under the artificial condition the 59Fe morphology in sea water, its concentration in sediment and phytoplankton, its distribution and metabolism in tissue organs of marine animals were studied. The results showed that the morphology of 59Fe was in a particulate state in sea water. The adsorption rule of 59Fe by three kinds of sediments was similar. The concentration ability of 59Fe by phytoplankton was very strong. The critical concentration organs of S9Fe by marine animals were viscera. The gross radioactivity of 59Fe was mainly concentrated in protein. The concentration factor of 59Fe by DNA was the highest one. After excretion experiment, 59Fe of all the tissue organs was not detected. Small part of59Fe remained in the organic acid and protein state. There was a redistribution process in sediment for59Fe. 相似文献
126.
Wen Shengchang 《海洋学报(英文版)》1988,7(3):325-343
The method developed by Wen et al. (1988 a) for deriving theoretical wind wave frequency spectrum in deep water is extended to the case of water of finite depth, in which a parameter η=H/d is introduced, where H and d represent the average wave height and water depth respectively. The derived spectra reduce to those in deep water when η=0. The case of η=1/2 corresponds to waves impending to break because of the effect of the bottom. Simplified forms of spectra are given. The theoretical results agree with the observed spectra well. 相似文献
127.
128.
Magnetic properties were measured on 370 vibrocores obtained from the outer continental shelf of the East China Sea, with
the aim of reconstructing environmental changes during the late Quaternary. High SIRM/χ values (>25 kA m−1) found in stiff muds of late Pleistocene age suggest the presence of magnetic iron sulfides, especially greigite. Framboidal
aggregates of greigite were further identified by scanning electron microscopy (SEM) and attached energy dispersive X-ray
(EDAX) analyses, as well as powder X-ray diffraction (XRD) analyses of the magnetic separates. The occurrence of magnetic
iron sulfides indicates the complex oxidation–reduction of the stiff muds, resulting from exposure and inundation during the
last glacial maximum (LGM) and the post-glacial transgression, respectively. 相似文献
129.
INTRODUCTIONDissolvedorganiccarbon (DOC)makesupthesecondlargestofthebioactivepoolsofcar bonintheocean ,secondtothelargestpoolofdissolvedinorganiccarbon .Theglobaldissolvedorganiccarbonpoolisestimatedtobe 6 85Gt,avaluecomparabletothemassofCO2 intheat mosphere (Hedges,1 992 ) .Thesizeofthereservoir,aswellasitsdynamics ,indicatesthatDOCplaysacentralroleintheoceancarboncycle .AsitrelatestogreenhousegasessuchasCO2 andassociatesclimatecycle ,oceanicDOCbiogeochemicalcycleshavebeenoneoftheh… 相似文献
130.
Variation of reactivity of particulate and sedimentary organic matter along the Zhujiang River Estuary 总被引:3,自引:0,他引:3
To investigate organic matter source and reactivity in the Zhujiang River (Pearl River)Estuary and its adjacent areas, particulate organic carbon (POC), particulate hydrolysable amino acids (PHAA), and Chl a during two cruises in July 1999 and July 2000 were measured. The highest POC and PHAA concentration was observed in the waters with maximum Chl a. The spectra distribution,relative content (dry weight in milligram per gram), PHAA-C% POC and other indicators such as the ratios of amino acids vs. amino sugars (AA/AS) and glucosamine vs. galactosamine (Glum/Gal) suggested that particulate amino acids in the water column and sediments in the Zhujiang River Estuary were mainly derived from biogenic processes rather than transported from terrestrial erosion. In inner estuary where high turbidity was often observable, organic matter was mainly contributed by re-suspension of bottom sediments with revealed zooplankton, microbial reworked characteristics, which suggest that these organic matters were relatively “old“. In the estuarine brackish region, organic matter in water column is mainly contributed by relatively fresh, easily degradable phytoplankton derived organic matter.During physical - biological processes within the eastuary, organic matter derived from phytoplankton was subjected to alteration by zooplankton grazing and bacterial reworking. 相似文献