全文获取类型
收费全文 | 38447篇 |
免费 | 3078篇 |
国内免费 | 4814篇 |
专业分类
测绘学 | 2699篇 |
大气科学 | 5091篇 |
地球物理 | 8049篇 |
地质学 | 19148篇 |
海洋学 | 3094篇 |
天文学 | 2217篇 |
综合类 | 3369篇 |
自然地理 | 2672篇 |
出版年
2024年 | 100篇 |
2023年 | 331篇 |
2022年 | 674篇 |
2021年 | 837篇 |
2020年 | 668篇 |
2019年 | 727篇 |
2018年 | 5346篇 |
2017年 | 4581篇 |
2016年 | 3314篇 |
2015年 | 955篇 |
2014年 | 1016篇 |
2013年 | 931篇 |
2012年 | 1804篇 |
2011年 | 3561篇 |
2010年 | 2861篇 |
2009年 | 3174篇 |
2008年 | 2634篇 |
2007年 | 3062篇 |
2006年 | 730篇 |
2005年 | 834篇 |
2004年 | 866篇 |
2003年 | 866篇 |
2002年 | 780篇 |
2001年 | 565篇 |
2000年 | 521篇 |
1999年 | 633篇 |
1998年 | 525篇 |
1997年 | 493篇 |
1996年 | 464篇 |
1995年 | 375篇 |
1994年 | 367篇 |
1993年 | 315篇 |
1992年 | 283篇 |
1991年 | 222篇 |
1990年 | 188篇 |
1989年 | 158篇 |
1988年 | 128篇 |
1987年 | 70篇 |
1986年 | 74篇 |
1985年 | 49篇 |
1984年 | 42篇 |
1983年 | 29篇 |
1982年 | 39篇 |
1981年 | 35篇 |
1980年 | 41篇 |
1979年 | 17篇 |
1978年 | 7篇 |
1977年 | 8篇 |
1976年 | 11篇 |
1958年 | 15篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
101.
Hydrodynamic and sediment transport measurements from instrumentation deployed during a 54-day winter period at two sites on the Louisiana inner shelf are presented. Strong extratropical storms, with wind speeds of 7.8 to 15.1 m s-1, were the dominant forcing mechanism during the study. These typically caused mean oscillatory flows and shear velocities about 33% higher than fair weather (averaging 12.3 and 3.2 cm s-1 at the landward site, and 11.4 and 2.7 cm s-1 at the seaward site, respectively). These responses were coupled with mean near-bottom currents more than twice as strong as during fair weather (10.3 and 7.5 cm s-1 at the landward and seaward sites, respectively). These flowed in approximately the same direction as the veering wind, causing a net offshore transport of fine sand. Weak storms were responsible for little sediment transport whereas during fair weather, onshore sand transport of approximately 25-75% of the storm values appears to have occurred. This contradicts previous predictions of negligible fair-weather sediment movement on this inner shelf. 相似文献
102.
派比安台风对上海黄浦江潮位的影响及成因探讨 总被引:3,自引:3,他引:3
2000年派比安台风产生的历史第二高潮位对上海的防汛带来严重影响。本文通过比较历史上的风暴潮,从动力机制、天文高潮与增水极值相碰头,潮波共振和水利工程的影响等四个方面分析了这次风暴潮造成的高水位,及台风余振期边缘波的影响,并用SLOSH(Sea,Lake,Overland Surge from Hurricanes)模式模拟了这次风暴潮,为防台减灾的正确决策提供了理论依据。 相似文献
103.
应用模糊综合评价方法对大连臭水套海域疏浚物预选倾倒区的水质状况进行了评价,得到了有益的结论。 相似文献
104.
于1985-1986年在长江口的底栖生物取样中,采到大量双壳类软体动物标本。鉴定表明,其中一新种,被定名为中华团结蛤Abra simica sp.nov。,属樱蛤超科中的双带科(Semelidae)。模式标本保存于中国科学院海洋研究所。 相似文献
105.
Remote estimation of surficial seafloor properties through the application Angular Range Analysis to multibeam sonar data 总被引:2,自引:2,他引:2
The variation of the backscatter strength with the angle of incidence is an intrinsic property of the seafloor, which can
be used in methods for acoustic seafloor characterization. Although multibeam sonars acquire backscatter over a wide range
of incidence angles, the angular information is normally neglected during standard backscatter processing and mosaicking.
An approach called Angular Range Analysis has been developed to preserve the backscatter angular information, and use it for
remote estimation of seafloor properties. Angular Range Analysis starts with the beam-by-beam time-series of acoustic backscatter
provided by the multibeam sonar and then corrects the backscatter for seafloor slope, beam pattern, time varying and angle
varying gains, and area of insonification. Subsequently a series of parameters are calculated from the stacking of consecutive
time series over a spatial scale that approximates half of the swath width. Based on these calculated parameters and the inversion
of an acoustic backscatter model, we estimate the acoustic impedance and the roughness of the insonified area on the seafloor.
In the process of this inversion, the behavior of the model parameters is constrained by established inter-property relationships.
The approach has been tested using a 300 kHz Simrad EM3000 multibeam sonar in Little Bay, NH. Impedance estimates are compared
to in situ measurements of sound speed. The comparison shows a very good correlation, indicating the potential of this approach for
robust seafloor characterization. 相似文献
106.
We collected surface water along the 142nd E meridian from Tasmania to Antarctica in December 1999. We measured temperature,
salinity and total chlorophyll a; additionally, we collected suspended particle size fractions and used fluorometric analysis to determine the quantity of
chlorophyll a in each of four cell size classes: picoplankton (<3 μm), two nanoplankton fractions (3–10 μm and 10–20 μm) and microplankton
(> 20 μm). Changes in temperature and salinity show that we crossed 6 water masses separated by 5 fronts. We found low abundance
(<0.2 mg m−3) of chlorophyll in all size classes, with the exception of higher values near the continent (0.2 to 0.4 mg m−3). Lowest chlorophyll values (<0.1 mg m−3) were found in the Polar Frontal Zone (51° to 54°S). Microplankton made up the largest portion of total chlorophyll throughout
most of the region. We conclude that biomass of all phytoplankton fractions, especially pico-and nanoplankton, was constrained
by limiting factors, most probably iron, throughout the region and that ecosystem dynamics within a zone are not circumpolar
but are regionalized within sectors. 相似文献
107.
Young-Ok Kim Eun Jin Yang Jung-Hoon Kang Kyoungsoon Shin Man Chang Cheol Soo Myung 《Ocean Science Journal》2007,42(1):9-17
The summer distributions of planktonic microbial communities (heterotrophic and phtosynthetic bacteria, phtosynthetic and
heterotrophic nanoflagellates, ciliate plankton, and microphytoplankton) were compared between inner and outer areas of Lake
Sihwa, divided by an artificial breakwater, located on the western coast of Korea, in September 2003. The semienclosed, inner
area was characterized by hyposaline surface water (<17 psu), and by low concentrations of dissolved oxygen (avg. 0.4 mg L1) and high concentrations of inorganic nutrients (nitrogenous nutrients >36 μM, phosphate <4 μM) in the bottom layer. Higher
densities of heterotrophic bacteria and nanoflagellates also occurred in the inner area than did in the outer area, while
microphytoplankton (mainly diatoms) occurred abundantly in the outer area. A tiny tintinnid ciliate, Tintinnopsis nana, bloomed
into more than 106 cells L1 at the surface layer of the inner area, while its abundance was much lower (103-104 cells L1) in the outer area of the breakwater. Ciliate abundance was highly correlated with heterotrophic bacteria (r = 0.886, p <
0.001) and heterotrophic flagellates (r = 0.962, p < 0.001), indicating that rich food availability may have led to theT. nana bloom. These results suggest that the breakwater causes the eutrophic environment in artificial lakes with limited flushing
of enriched water and develops into abundant bacteria, nanoflagellates, and ciliates. 相似文献
108.
109.
110.
研究取自于东太平洋CC48柱状样的钙质超微化石和底栖有孔虫的氧同位素成分变化的结果表明,该区下中新统至少可分出九个氧同位素地层(期),反映该区在早中新世期间至少经历了4次气温上升和5次下降的古气候变化。南极大陆冰川应是形成于早中新世而不是前人认为的中中新世。在早中新世,南极冰体体积有较大的变化。受古气候变化的影响,在早中新世期间东太平洋水柱热结构或温度梯度有比较大的变化,海平面出现多次上升与下降。 相似文献