全文获取类型
| 收费全文 | 1344篇 |
| 免费 | 494篇 |
| 国内免费 | 538篇 |
专业分类
| 测绘学 | 236篇 |
| 大气科学 | 34篇 |
| 地球物理 | 592篇 |
| 地质学 | 1087篇 |
| 海洋学 | 90篇 |
| 天文学 | 13篇 |
| 综合类 | 154篇 |
| 自然地理 | 170篇 |
出版年
| 2024年 | 9篇 |
| 2023年 | 41篇 |
| 2022年 | 96篇 |
| 2021年 | 87篇 |
| 2020年 | 107篇 |
| 2019年 | 94篇 |
| 2018年 | 94篇 |
| 2017年 | 90篇 |
| 2016年 | 71篇 |
| 2015年 | 104篇 |
| 2014年 | 131篇 |
| 2013年 | 144篇 |
| 2012年 | 134篇 |
| 2011年 | 109篇 |
| 2010年 | 91篇 |
| 2009年 | 103篇 |
| 2008年 | 115篇 |
| 2007年 | 104篇 |
| 2006年 | 95篇 |
| 2005年 | 81篇 |
| 2004年 | 75篇 |
| 2003年 | 58篇 |
| 2002年 | 53篇 |
| 2001年 | 25篇 |
| 2000年 | 42篇 |
| 1999年 | 38篇 |
| 1998年 | 32篇 |
| 1997年 | 33篇 |
| 1996年 | 18篇 |
| 1995年 | 23篇 |
| 1994年 | 21篇 |
| 1993年 | 22篇 |
| 1992年 | 10篇 |
| 1991年 | 9篇 |
| 1990年 | 11篇 |
| 1988年 | 2篇 |
| 1987年 | 1篇 |
| 1957年 | 1篇 |
| 1954年 | 2篇 |
排序方式： 共有2376条查询结果，搜索用时 15 毫秒
51.
《Ocean Modelling》2010,35(3-4):92-110
A convective adjustment (CA) algorithm is thought to be responsible for grid-scale oceanic-state sustained oscillations seen in oceanic general circulation models (OGCM), an effect that is most evident in simulations with coarse spatio-temporal scales. The CA algorithm is thought to inadvertently create a salt oscillator. Several studies have confirmed that a flip-flop type salt oscillator, which is reminiscent in some respects of simple CA schemes, can develop sustained oscillations. Subsequently, several researchers were able to show how coupled salt oscillators, reacting in a particular temporal sequence, are capable of producing large-scale oscillations not unlike those found in the OGCM simulations. However, the proxy models used to study how CA can create these oscillations in large-scale simulations were never directly related to OGCM results.Here we couple hydrodynamics to the CA and look at zonally-driven flows in the low-frequency, large-scale limit. Adding flow is a step in the direction of developing an analytically tractable model with which to understand the basics of OGCMs. We analytically determine whether, and under what circumstances, the CA scheme is responsible for sustained oscillations.We carry out this program for four basic box-model configurations, each inspired by the general shape of the eigenfunctions and constraints of the large-scale zonally-averaged forced flow over a hemisphere. Furthermore, in order to make our results relevant to the Meridional Ocean Circulation, we also investigate the effect of replacing the usual assumption of a linear relation between thermohaline flow rate and horizontal density gradient with a nonlinear hydraulic relationship.We find that a salt oscillator does not occur in the most common box-model configurations. In one of our models, however, we find wide parameter ranges in which all steady states calculated for the model fail to satisfy the CA scheme, the situation which is expected to result in CA-induced oscillations. The model in question corresponds to a hemispheric shallow thermohaline flow over a deep reservoir. However, we find that oscillations occur in these parameter ranges only if the density threshold for convection is negative, i.e., if the CA scheme turns on convection between vertically adjacent boxes when the density stratification between them is still slightly stable. In this situation, the amplitude and period of the oscillations depend strongly on the size of the density threshold, both vanishing as the threshold is taken toward zero. We also show that the same is true in the Welander flip-flop model of a single salt oscillator. For positive values of the threshold, that is, when the CA scheme is allowed to ignore small unstable stratification changes, oscillations do not occur in the limit of integration time step going to zero, but can still be seen when the time step is finite, even if small. Moreover, the system evolves toward a new steady state, one in which the stratification in one box is exactly the threshold value itself. We show how to calculate these new steady states, and explain why they give way to oscillations when the density threshold is negative. 相似文献
52.
随着长江上游梯级水库的陆续建成投运，三峡水库的水文情势和功能需求与设计条件相比发生了显著变化，仍维持固定的汛限水位运行已不能适应新形势需求。本文通过辨析三峡水库设计阶段汛限水位的设置条件，挖掘流域洪水特性和洪水遭遇规律，论证三峡水库汛期运行水位动态控制的可行性。结果表明：① 三峡水库设计推求的汛限水位145 m的适用条件是应对流域性大洪水，而流域性洪水发生概率小且特征明显，可以通过水文水情分析提前预判。② 根据流域洪水类型、洪水分期和遭遇规律，预判发生区域性大洪水时，三峡水库6月初至梅雨期结束汛限水位按145 m设置，从梅雨期结束后逐渐提高水位，8月20日后过渡到155 m。③ 在考虑上游水库群联合调度和气象水文预报的配合下，正常年份三峡水库汛期运行水位可在155 m上下浮动，并考虑提前蓄水。④ 三峡水库汛期运行水位动态控制，不会增加防洪风险和库区淤积风险，对中下游江湖关系和水文情势有利，可显著提高发电、航运、生态保护和供水等综合利用效益。 相似文献
53.
54.
55.
56.
57.
58.
本文介绍了武汉大学哨声组研制的KDX-87型甚低频宽带定向接收与微机分析系统.该系统适用于测量与分析哨声波传播路径出口、偏振和动态谱.此系统具有以下优点:1.设计制造了小型化天线和便携式接收机,便于携带和架设;合理设计了输入耦合与平衡电路,加上有效的标定方法,使接收系统具有良好的频率响应和通道间性能的一致性.2.实现了数字化宽频带定向分析,有利于减小多路径效应误差,并可获得哨声路径出口与波频率之间的关系.3.利用微机进行哨声动态谱分析,采取了有效的抑制干扰处理,所得谱图分辨率优于普通声图仪制作的谱图.该系统在1988年中日联合哨声定向实验中使用,取得了满意的结果. 相似文献
59.
Jiangrong Xiao Tianyou Peng Dingning Ke Ling Zan Zhenghe Peng 《Physics and Chemistry of Minerals》2007,34(4):275-285
CdS/rectorite nanocomposite was synthesized via a cation-exchange reaction followed by a sulfurization process. The obtained
samples were characterized by using X-ray diffraction (XRD), fourier transform infrared spectra (FTIR), transmission electron
microscope (TEM), UV-Vis diffuse reflectance spectra (DRS), and thermal analysis. The measured results indicate that CdS species
in the composites exist in the form of pillars and nanoparticles, the crystallized CdS particles are in the hexagonal symmetry.
The photocatalytic activities of the pillared nanocomposite were enhanced significantly comparing with the bare rectorite
and the pure CdS. Moreover, the photostabilities of the obtained nanocomposites are also better than that of the pure CdS
due to the hosts retard the photocorrosion of the CdS. 相似文献
60.
Crustacean zooplankton distribution patterns and their biomass as related to trophic indicators of 29 shallow subtropical lakes 总被引：3，自引：0，他引：3
A comparative limnological study was carried out to present a snapshot of crustacean zooplankton communities and their relations to environmental factors to test whether there is a consistent relationship between crustacean biomass and trophic indicators among lake groups with similar trophic conditions. The study lakes showed a wide range of trophic status, with total phosphorus (TP) ranging from 0.008 to 1.448 mg L−1, and chlorophyll a from 0.7 to 146.1 μg L−1, respectively. About 38 species of Crustacea were found, of which Cladocera were represented by 25 taxa (20 genera), and Copepoda by 13 taxa (11 genera). The most common and dominant species were Bosmina coregoni, Moina micrura, Diaphanosoma brachyurum, Cyclops vicinus, Thermocyclops taihokuensis, Mesocyclops notius and Sinocalanus dorrii. Daphnia was rare in abundance. Canonical correspondence analysis showed that except for four species (D. hyalina, S. dorrii, C. vicinus and M. micrura), almost all the dominant species had the same preference for environmental factors. Temperature, predatory cyclopoids and planktivorous fishes seem to be the key factors determining species distribution. TP was a relatively better trophic indicator than chlorophyll a to predict crustacean biomass. Within the three groups of lakes, however, there was no consistent relationship between crustacean biomass and trophic indicators. The possible reason might be that top-down and bottom-up control on crustaceans vary with lake trophic state. The lack of significant negative correlation between crustacean biomass and chlorophyll a suggests that there was little control of phytoplankton biomass by macrozooplankton in these shallow subtropical lakes. 相似文献