全文获取类型
收费全文 | 17069篇 |
免费 | 3012篇 |
国内免费 | 3945篇 |
专业分类
测绘学 | 1248篇 |
大气科学 | 3109篇 |
地球物理 | 4201篇 |
地质学 | 8702篇 |
海洋学 | 2142篇 |
天文学 | 867篇 |
综合类 | 1617篇 |
自然地理 | 2140篇 |
出版年
2024年 | 88篇 |
2023年 | 311篇 |
2022年 | 855篇 |
2021年 | 978篇 |
2020年 | 835篇 |
2019年 | 931篇 |
2018年 | 1064篇 |
2017年 | 907篇 |
2016年 | 989篇 |
2015年 | 841篇 |
2014年 | 1061篇 |
2013年 | 1065篇 |
2012年 | 1026篇 |
2011年 | 1068篇 |
2010年 | 1053篇 |
2009年 | 1000篇 |
2008年 | 887篇 |
2007年 | 803篇 |
2006年 | 669篇 |
2005年 | 635篇 |
2004年 | 478篇 |
2003年 | 436篇 |
2002年 | 413篇 |
2001年 | 451篇 |
2000年 | 476篇 |
1999年 | 646篇 |
1998年 | 540篇 |
1997年 | 488篇 |
1996年 | 485篇 |
1995年 | 382篇 |
1994年 | 378篇 |
1993年 | 318篇 |
1992年 | 290篇 |
1991年 | 194篇 |
1990年 | 165篇 |
1989年 | 132篇 |
1988年 | 109篇 |
1987年 | 79篇 |
1986年 | 67篇 |
1985年 | 59篇 |
1984年 | 45篇 |
1983年 | 50篇 |
1982年 | 41篇 |
1981年 | 26篇 |
1980年 | 21篇 |
1979年 | 22篇 |
1978年 | 18篇 |
1976年 | 18篇 |
1973年 | 16篇 |
1972年 | 15篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
151.
厦门嵩屿附近海底的冲淤变化 总被引:2,自引:0,他引:2
本文通过地形剖面测量比较、浅地层剖面勘探,结合水文泥沙测验和沉积物粒径资料,分析嵩屿附近海域在各历史时期和九江洪水期、枯水期的中淤变鼓水道近十几年来淤积速度加快。其主要原因是该海域动力要素明显减弱,携沙能力降低;其次,九龙江大量的泥沙主要集中在洪水期较短的时间内泄出河口,伴随涨潮流进入嵩鼓水道淤积。 相似文献
152.
一个简单食物链的能流实验 总被引:1,自引:0,他引:1
食物链能量转换是生态系统的主要功能之一。海洋生物生产就是海洋食物链能量流动的一种表现形式。它把来自以藻类为主的植物性生产,通过被食-取食多级转换,形成了贝、虾、鱼等各级动物性生产,这就为人类提供了丰富的渔业资源。海岸带水域是我国目前海洋开发的主攻目标,揭示这个海区中食物链能流转移过程,对其经济生物生产力估算和开发前景预测有着重要意义。测定自然条件下海洋食物链能流是极其困难的。借助实验结果进而推算,就比较方便。本研究选择我国海岸带水域中属于不同营养级的4个经济种,构成一个简单的人工食物链,即金藻(… 相似文献
153.
21世纪将是全面开发利用海洋的时代,许多沿海国家将把海洋开发作为国家战略。我国是世界上人口最多的国家,陆地资源人均占有量少,更应该重视开发海洋,建设临海工业带,发展海洋农牧化,开发建设海运网络等。发展海洋经济必须走科技兴海之路,抓科技储备,改造传统产业,发展新兴产业,不断提高海洋开发生产力水平。 相似文献
154.
本文选择酒石酸消除海水基体对铜信号的干扰,用塞曼石墨炉原子吸收法直接测定海水中的铜。从Cu的原子化曲线可知,加入酒石酸后,背景值减小,Cu原子吸收信号增强,且出现时间提前,表明酒石酸是有效的海水基体改进剂。用P.E.Z3030光谱仪测得双蒸水及海水中的元素Cu的特征质量(m。)分别为12.5pg及12.7pg;检测限分别为0.18μg/L和0.19μg/L,表明基体效应已消除,符合海洋监测要求。可用纯Cu标准溶液作校正曲线,以国家海洋局的两个标准海水样品中的Cu评定本法的准确度,相对偏差为0及-4.6%,与经典的经富集后的FAAS法的结果相比,相对偏差在3.0—6.5%范围内。用不同类型的光谱仪测定了30个海水样品,回收率在89—104%范围内。本法操作简便、快速。 相似文献
155.
中国对虾新病害—肠结节病的观察 总被引:1,自引:0,他引:1
1991年7~8月浙江省宁波、舟山地区一些中国对虾Penaeruschinensis的养虾场中爆发了一种肠结节新病害,危害十分严重。本文报导该病发生与危害的情况以及症状、病原、组织病理观察的结果。 相似文献
156.
An improved Ewing heat probe frame 总被引:3,自引:0,他引:3
The standard Ewing heat probe frame has been improved through the design of a new takedown model whose parts are held together by lynch pins. When a 600 lb (272 kg) unit of this type is taken apart, the heaviest single piece of the dismantled unit weighs only 75 lb (34 kg).This makes it feasible for one person to handle, transport, and assemble the new unit. A central, main support member of a heat probe using this frame can be suspended over the side of a research vessel while the heavier temperature recorder and ballast weights are attached by means of the quickaction lynch pins. This makes it possible to use this device on relatively small vessels which are not designed for coring work, having a minimum of free deck space and without launching platforms or hydraulic A-frame booms. 相似文献
157.
158.
High precision geoid models HKGEOID-2000 for Hong Kong and SZGEOID-2000 for Shenzhen, China, have been developed with a hybrid approach of so-called sequential processing, using high precision GPS/leveling data, land and sea gravity anomalies, and digital terrain models. These two local geoid models have the same 1-km resolution. The estimated accuracy (external accuracy) is better than 1.7 cm for HKGEOID-2000 and 1.4 cm for SZGEOID-2000. Some common areas are covered by HKGEOID-2000 and SZGEOID-2000. So these two geoid models, along with high quality GPS/leveling data collected on the overlapping areas, can be used to detect the systematic bias between HKGEOID-2000 and SZGEOID-2000, as well as the difference between Hong Kong Principal Datum and 1956 yellow sea height datum of China, yielding RMS errors of 1.011 m and 1,003 m, respectively. Moreover, HKGEOID-2000, along with GPS ellipsoidal heights, is employed to determine the errors of the “orthometric heights” from purely trigonometric heighting, yielding an RMS error of 0.102 m. The combination of SZGEOID-2000 and GPS ellipsoidal heights has been used to replace the traditional spirit leveling and mapping, called GPS mapping. 相似文献
159.
Dot enzyme-linked immunosorbent assay (dot-ELISA), indirect ELISA and Westem blot were performed to detect the virulent protease secreted by Vibrio anguillarum which was isolated from the diseased left-eyed flounder, Paralichthys olivaceous. Sensitivity results showed that dot-ELISA is a more sensitive, rapid and simple technique for the protease detection. The minimal detectable amount of protease is about 7 pg in the dot-ELISA test, while 7.8 ng in the indirect ELISA and 6.25 ng in the Westem blot respectively. Protease could be detected 2 h after incubation of V. anguillarum in the 2216E liquid medium but enzyme activity was very low at that period. From 6 to 12 h, the amount and enzyme activity of protease increased markedly and reached maximum at stationary phase. Analysis of serum samples periodically collected from the infected flounders showed that after 2 h of infection by V. anguillarum, the pathogenic bacteria could be detected in the blood of the infected flounders but no protease was found. It was 5-6 h after infection that the protease was detected in blood and then the amount increased as infection advanced. Quantitative detection of protease either incubation in the medium or from the blood of infected flounders could be accomplished in virtue of positive controls of quantificational protease standards ("marker") so that the alterations ofprotease secretion both in vitro and in vivo could be understood generally. In addition, the indirect ELISA and dot-ELISA were also performed to detect V. anguillarum cells. Results indicated that the sensitivity of indirect ELISA to bacteria cells is higher than that of the dot-ELISA, and that the minimal detectable amount is approximately 10^4 cell/mL in the indirect ELISA, while 10^5 cell/mL in the dot-ELISA. 相似文献
160.
Frank Rske 《Ocean Modelling》2006,11(3-4):235-297
A global dataset based on the ECMWF Re-Analyses (ERA) is presented that can be used as surface boundary conditions for ocean models with sea-ice components. The definition of these conditions is based on bulk formulae. To study the mean ocean circulation, a mean annual cycle on a daily basis was constructed from ERA for all relevant parameters including wind stress. Continental runoff is considered by using information about the catchment areas of the rivers and about the main drainage basins. The bulk formulae were extended by using sea ice concentration.To estimate meridional heat transports (MHT) and to avoid any drift in ocean model simulations, the heat and fresh water budgets have been closed by applying an inverse procedure to fine-tune the fluxes towards observed transports. To improve the MHTs on the Southern Hemisphere the winds and the short wave radiation at southern higher latitudes should be corrected. Furthermore, tests were performed concerning short wave radiation which was increased in the tropics and decreased in the subsidence zones.The heat and fresh water fluxes are assessed by using a scheme of Macdonald and Wunsch based on hydrographic sections. The net heat fluxes of ERA and of the forcing dataset are consistent with the heat flux divergences and convergences estimated by this scheme except for parts of the South Atlantic and the Indian Ocean sector of the Southern Ocean where none of these datasets is consistent with these estimates. In the subtropical South Indian Ocean the forcing dataset is consistent with these estimates while ERA are not. The flux components of ERA and the forcing dataset were compared to several observational datasets (SRB, SOC, HOAPS, GPCP, and CMAP). For each component, at least one of these datasets (especially HOAPS) supports the effects of the inverse procedure and the bulk formulae almost globally with some regional exceptions: short wave radiation in the tropical oceans and the subtropical North Atlantic, latent heat flux at higher latitudes, and precipitation in the northern North Atlantic.Comparisons to the NCAR/NCEP Re-Analyses (NRA) (versions 1 and 2) and the ECHAM model in place of ERA lead to similar results. In the North Atlantic the net heat fluxes of the model based datasets approach the hydrographic estimate with increasing resolution. Applied to any ocean/sea-ice model and compared to ERA, the forcing dataset would induce only a relative small net sea-surface buoyancy loss.A comparison of the forcing dataset to measurements made using one buoy deployed in the western Pacific warm pool and five buoys deployed in the subduction region of the Northeast Atlantic shows that at the site of the first buoy the net heat fluxes of the forcing dataset are in poorer agreement than those of ERA. At the sites of two subduction buoys both datasets show the same level of agreement within the error bars specified. At the sites of the three remaining subduction buoys the forcing dataset shows a marginal improvement on ERA. 相似文献