全文获取类型
收费全文 | 2443篇 |
免费 | 459篇 |
国内免费 | 410篇 |
专业分类
测绘学 | 629篇 |
大气科学 | 176篇 |
地球物理 | 857篇 |
地质学 | 1018篇 |
海洋学 | 258篇 |
天文学 | 31篇 |
综合类 | 194篇 |
自然地理 | 149篇 |
出版年
2024年 | 18篇 |
2023年 | 38篇 |
2022年 | 62篇 |
2021年 | 75篇 |
2020年 | 97篇 |
2019年 | 108篇 |
2018年 | 77篇 |
2017年 | 102篇 |
2016年 | 122篇 |
2015年 | 136篇 |
2014年 | 147篇 |
2013年 | 159篇 |
2012年 | 151篇 |
2011年 | 175篇 |
2010年 | 144篇 |
2009年 | 167篇 |
2008年 | 200篇 |
2007年 | 204篇 |
2006年 | 172篇 |
2005年 | 144篇 |
2004年 | 127篇 |
2003年 | 116篇 |
2002年 | 84篇 |
2001年 | 69篇 |
2000年 | 71篇 |
1999年 | 48篇 |
1998年 | 42篇 |
1997年 | 56篇 |
1996年 | 42篇 |
1995年 | 21篇 |
1994年 | 19篇 |
1993年 | 25篇 |
1992年 | 21篇 |
1991年 | 14篇 |
1990年 | 8篇 |
1989年 | 13篇 |
1988年 | 10篇 |
1987年 | 7篇 |
1986年 | 7篇 |
1985年 | 3篇 |
1984年 | 2篇 |
1983年 | 2篇 |
1982年 | 1篇 |
1977年 | 1篇 |
1972年 | 1篇 |
1954年 | 4篇 |
排序方式: 共有3312条查询结果,搜索用时 15 毫秒
211.
岩浆岩的侵入问题一直严重影响着煤矿的安全和高效生产,如何准确地划分出岩浆岩侵入区范围是急需解决的关键问题之一。通过对正演模型数据和实际数据的谱分解分析,发现正常煤层与岩浆岩侵入煤层间存在着明显的频谱差异。正常煤层反射波在其主频对应的谱分解切片上的能量较强,而岩浆岩侵入煤层反射波在同一谱分解切片上的能量较弱。对于实际煤层数据来说,通过钻井标定,即可以定量、准确地划分出岩浆岩侵入区的范围。以大屯煤电公司徐庄煤矿为例,对7煤层谱分解沿层切片与振幅沿层切片进行了对比解释,结果证实谱分解技术对预测煤层岩浆侵入范围是切实可行的。 相似文献
212.
Multi-Time Scale Analysis of Runoff at the Yangtze Estuary Based on the Morlet Wavelet Transform Method 总被引:1,自引:1,他引:0
KUANG Cui-ping SU Ping GU Jie CHEN Wu-jun ZHANG Jian-le ZHANG Wan-lei ZHANG Yong-feng 《山地科学学报》2014,(6):1499-1506
Runoff series of the Yangtze River presents an intricate variation tendency under the reinforced influence of human activities.The Morlet Wavelet Transform method has been applied to analyze the annual runoff data from 1950 to 2011 at the Yangtze River Estuary.It can clearly reveal the multi-time scales structure,break point,change and distribution of periodic variation in the different time scales of the runoff series.The main conclusions are that:1) Repeated periodic oscillations accompanied by an extremely large fluctuation are presented in the runoff series with an obvious difference between wet and dry years,and the major periods of the time series are about 3,8,16 and 23 years respectively.Among them,the presented maximum periodic oscillation is 23 years scale.2) In the 23-year time scale,the wet periods are 1950-1958,1969-1980 and 1992-2003,and the dry periods are 1959-1968,1981-1991 and 2004-2011.3) It can be predicted from the view of long time scales that the low annual runoff will likely occur in the near future. 相似文献
213.
Homologous feature point extraction is a key problem in the optical and synthetic aperture radar (SAR) image registration for islands. A new feature point extraction method using a threshold shrink operator and non-subsampled wavelet transform (TSO-NSWT) for optical and SAR image registration was proposed. Moreover, the matching for this proposed feature was different from the traditional feature matching strategies and was performed using a similarity measure computed from neighborhood circles in low-frequency bands. Then, a number of reliably matched couples with even distributions were obtained, which assured the accuracy of the registration. Application of the proposed algorithm to SPOT-5 (multi-spectral) and YG-1 (SAR) images showed that a large number of accurately matched couples could be identified. Additionally, both of the root mean square error (RMSE) patterns of the registration parameters computed based on the TSO-NSWT algorithm and traditional NSWT algorithm were analyzed and compared, which further demonstrated the effectiveness of the proposed algorithm. The algorithm can supply the crucial step for island image registration and island recognition. 相似文献
214.
Considering the discontinuous characteristics of sea ice on various scales,a modified discrete element model(DEM) for sea ice dynamics is developed based on the granular material rheology.In this modified DEM,a soft sea ice particle element is introduced as a self-adjustive particle size function.Each ice particle can be treated as an assembly of ice floes,with its concentration and thickness changing to variable sizes under the conservation of mass.In this model,the contact forces among ice particles are calculated using a viscous-elastic-plastic model,while the maximum shear forces are described with the Mohr-Coulomb friction law.With this modified DEM,the ice flow dynamics is simulated under the drags of wind and current in a channel of various widths.The thicknesses,concentrations and velocities of ice particles are obtained,and then reasonable dynamic process is analyzed.The sea ice dynamic process is also simulated in a vortex wind field.Taking the influence of thermodynamics into account,this modified DEM will be improved in the future work. 相似文献
215.
针对卫星云图数据量大,但传输通道和存储空间相对狭小的问题,本文基于Tetrolet变换,利用相邻时次云图的时空相关性,实现了一种高重构质量的卫星云图压缩感知方法。该方法将善于表达图像方向纹理及边缘信息的Tetrolet变换引入压缩感知的稀疏表示环节,从而很好地体现了卫星云图细节丰富、纹理结构复杂的特性;同时,考虑到卫星云图序列间的相关性,将时间相邻的卫星云图组成图像组,以中间时刻云图作为参考图像,计算其与相邻时次云图的差异,通过在参考图片及序列差异图片间合理分配采样率,获取测量数据,在压缩感知框架下,采用带平滑处理的投影Landweber算法,重构出相邻时次的图像组。实验结果表明,Tetrolet变换适用于卫星云图的稀疏表示,而且图像组时空相关性的利用可显著提高重构云图的视觉效果及客观评价指标;在采样率低于0.2时,红外1、水汽和可见光3个通道重构云图的峰值信噪比(PSNR)较传统方法平均提高了7.48 dB,13.51 dB和6.15 dB。由此可见,本文方法可以通过获取少数随机测量值,重构出高质量的卫星云图,不仅为云图数据的低比特率压缩提供了一种可行的解决方案,而且对于其他序列图像的压缩采样具有借鉴意义。 相似文献
216.
217.
218.
基于τ-p变换原理,研究一种基于τ-p变换的地震数据重构方法,运用该方法对待重构道用零道替代,通过τ-p正反变换及一定的迭代处理实现地震道数据重构。理论模型与实际资料应用表明,基于τ-p变换的地震道重构方法效果明显,重构数据稳健。 相似文献
219.
We investigate the quasi‐static simple shear flow of a two‐dimensional assembly of cohesionless particles using discrete element method (DEM) simulations. We focus on the unsteady flow regime where the solid would experience significant evolution of stresses, mobilised shear strength and dilation. We construct the DEM model using a discretised‐wall confined granular cell where the apparent boundary is allowed to dilate or contract synchronously with the confined solid. A rather uniform simple shear field is achieved across the whole assembly, which benefits rheological studies in generalising constitutive laws for continuum methods. We examine two aspects of the simple shear behaviour: macroscopic stress and strain rate evolution, particularly the non‐coaxiality between the principal directions of the two; and micromechanics such as evolution of fabric. For an initially anisotropic specimen sheared under constant normal pressure, the direction of principal stress rotates towards that of the principal strain rate, gradually reducing the degree of non‐coaxiality from about 45° to fluctuating around 0°. The rate in approaching coaxiality is slower in samples with larger initial porosity, stress ratio and mean stress. Generally, a faster rate in approaching coaxiality in simple shear is observed in a more dilatant sample, which often shows a larger degree of mobilised fabric anisotropy, suggesting the possible important role of instantaneous internal friction angle. The evolution of principal fabric direction resembles that of the principal stress direction. © 2013 The Authors. International Journal for Numerical and Analytical Methods in Geomechanics published by John Wiley & Sons, Ltd. 相似文献
220.