全文获取类型
收费全文 | 972篇 |
免费 | 114篇 |
国内免费 | 183篇 |
专业分类
测绘学 | 33篇 |
大气科学 | 163篇 |
地球物理 | 227篇 |
地质学 | 389篇 |
海洋学 | 163篇 |
天文学 | 71篇 |
综合类 | 44篇 |
自然地理 | 179篇 |
出版年
2024年 | 3篇 |
2023年 | 11篇 |
2022年 | 32篇 |
2021年 | 19篇 |
2020年 | 24篇 |
2019年 | 36篇 |
2018年 | 26篇 |
2017年 | 37篇 |
2016年 | 29篇 |
2015年 | 31篇 |
2014年 | 50篇 |
2013年 | 72篇 |
2012年 | 44篇 |
2011年 | 44篇 |
2010年 | 41篇 |
2009年 | 63篇 |
2008年 | 48篇 |
2007年 | 57篇 |
2006年 | 55篇 |
2005年 | 58篇 |
2004年 | 44篇 |
2003年 | 37篇 |
2002年 | 47篇 |
2001年 | 39篇 |
2000年 | 39篇 |
1999年 | 32篇 |
1998年 | 41篇 |
1997年 | 35篇 |
1996年 | 31篇 |
1995年 | 23篇 |
1994年 | 24篇 |
1993年 | 20篇 |
1992年 | 17篇 |
1991年 | 11篇 |
1990年 | 8篇 |
1989年 | 7篇 |
1988年 | 4篇 |
1987年 | 7篇 |
1986年 | 5篇 |
1985年 | 5篇 |
1984年 | 2篇 |
1983年 | 5篇 |
1981年 | 3篇 |
1980年 | 1篇 |
1978年 | 1篇 |
1977年 | 1篇 |
排序方式: 共有1269条查询结果,搜索用时 203 毫秒
251.
月球早期经历了岩浆洋阶段,岩浆洋的研究对认识月球内部构造有着重要意义。月球岩浆洋演化主导模型认为:岩浆洋结晶到80%左右,斜长石开始结晶,并上浮形成斜长岩月壳。该模型与观察事实存在两点矛盾:1)基于该模型计算结晶的斜长石An牌号比高地样品斜长石An牌号测试结果低;2)该模型散热速率计算指示岩浆洋在几个百万年时间内固化,而同位素体系对月球岩石样品定年结果表明月壳的结晶年龄十分古老,并且结晶区间跨越了270Myr,这与主导模型之间存在矛盾。以解决以上两点矛盾为目的,本文论证岩浆洋在演化之初硕部存在冷却"盖层",并将硅酸盐熔体在温度梯度下的热扩散效应引入岩浆洋演化模型。热扩散效应指均一的物质在温度梯度下发生分异的过程。本文工作模型是:由于月球的重力常数小,不能有效的保持大气,因此月球的岩浆洋表面温度很低。此时岩浆洋自上而下存在一个过渡的瞬态固化"盖层"(淬火层),岩浆洋自上而下存在温度梯度,岩浆洋在该梯度下发生热扩散效应(Soret效应),Soret效应导致上部结晶斜长石的熔体富Ca和贫Na,因此结晶的斜长石An牌号高。 相似文献
252.
Ick-Hoi Kim Chen-Chieh Feng Yi-Chen Wang Brian H. Spitzberg Ming-Hsiang Tsou 《The Professional geographer》2017,69(4):629-643
The 2015 Middle East respiratory syndrome (MERS) outbreak in South Korea gave rise to chaos caused by psychological anxiety, and it has been assumed that people shared rumors about hospital lists through social media. Sharing rumors is a common form of public perception and risk communication among individuals during an outbreak. Social media analysis offers an important window into the spatiotemporal patterns of public perception and risk communication about disease outbreaks. Such processes of socially mediated risk communication are a process of meme diffusion. This article aims to investigate the role of social media meme diffusion and its spatiotemporal patterns in public perception and risk communication. To do so, we applied analytical methods including the daily number of tweets for metropolitan cities and geovisualization with the weighted mean centers. The spatiotemporal patterns shown by Twitter users' interests in specific places, triggered by real space events, demonstrate the spatial interactions among places in public perception and risk communication. Public perception and risk communication about places are relevant to both social networks and spatial proximity to where Twitter users live and are interpreted in reference to both Zipf's law and Tobler's law. 相似文献
253.
254.
A small, simple and inexpensive device is described which allows the sampling of waters with a minimum of disturbance. This is particularly important when determining near-surface profiles, for example, following a dye release. 相似文献
255.
The diffusion attenuation coefficient for downwelling irradiance, Ka(490), is an important optical parameter of seawater. The optical property, Kd(490), around Nansha Islands in the South China Sea was analyzed based on optical data profiles measured with SPMR (SeaWiFS Profiling Multichannel Radiometer) and SMSR ( SeaWiFS Multichannel Surface Reference ) instrument in April and May, 1999. The results show that Kd(490) is closely correlated with chlorophyll-a concentration, Ccgka, and that the vertical distribution of Kd(490) shows the strong stratification of the water column in this area. Kd(490) has a similar vertical co-variation as KL(490), the diffusive attenuation coefficient for upwelling radiance.Both coefficients increase with depth in the upper layer, where KL(490) is greater than Kd(490); and after a depth, approximatively at the chlorophyll maximum, they decrease with depth, with the former being smaller than the latter. 相似文献
256.
When a steep bottom slope exists, it is well known that conventional methods for calculating horizontal diffusion in sigma-coordinate coastal ocean models causes spurious transport (e.g. salinity, temperature, and sediments) and currents. In this study, a second-order accurate finite-difference algorithm and program have been developed to reduce the spurious numerical diffusion errors. In the proposed algorithm, the finite differencing is performed in the x-z coordinate system to approximate the horizontal gradient. Each variable in the finite differential formation is calculated in the sigma-coordinate grid cells using a second-order Lagrangian interpolation polynomial. In conjunction with a stepwise bottom boundary condition, numerical experiments show that the proposed finite-difference scheme considerably reduces numerical errors compared to conventional approaches when dealing with horizontal diffusion over steep topography, which often occurs in coastal oceans and navigation channels. 相似文献
257.
Gu Jie Kuang Cuiping
Engineer Nanjing Environmental Protection Research Institute Nanjing .
Senior Engineer Doctor Nanjing Hydraulic Research Institute Nanjing 《中国海洋工程》1996,(3)
- A combined numerical model for computing mixing areas of pollution vertical jet discharging into tidal flows has been developed. This numerical model is composed of a 2-D depth-averaged dynamic far-field numerical model and a 2-D vertical dynamic near-field numerical model. The former uses finite node method to compute velocity, and improved finite node method to compute pollutant concentration distribution; the latter is a k-e turbulence model, and uses SIMPLE (Semi-Implicit Method for Pressure Linked Equations) method to compute velocity. At the same time, the former provides boundary conditions for the latter. This model can simulate both far- field pollutant concentration distribution and near-field vertical recirculation quickly and precisely. This model has been verified by measured data of pollutant F of the Dachang reach of the Changjing River and test data presented by Chen el al. (1992). On the basis of verification, the authors use a designed hydrograph to compute this mixing area for a cer 相似文献
258.
259.
260.
Oceanic double-infusion: introduction 总被引:1,自引:0,他引:1
Double-diffusion, the mixing of fluids with two constituents of different molecular diffusivities, was originally discovered in the mid-1800s, forgotten, then rediscovered as an ‘oceanographic curiosity’ a century later. Many oceanographers suspect that double-diffusion has major effects on oceanic water masses and circulation, but direct measurement of the effects has proven difficult. In 1996, a Working Group was formed under the auspices of the Scientific Committee on Ocean Research (SCOR WG108), with the goal to identify progress and barriers to quantifying oceanic double-diffusive fluxes, and make recommendations for further progress. This document gives a brief history of double-diffusion, a review of evidence of its potential effects in the ocean, and gives an overview of the review articles contained in this volume, written by the Working Group members with the above aim in mind. 相似文献