全文获取类型
收费全文 | 572篇 |
免费 | 215篇 |
国内免费 | 31篇 |
专业分类
测绘学 | 9篇 |
大气科学 | 61篇 |
地球物理 | 550篇 |
地质学 | 76篇 |
海洋学 | 34篇 |
天文学 | 18篇 |
综合类 | 26篇 |
自然地理 | 44篇 |
出版年
2024年 | 1篇 |
2023年 | 15篇 |
2022年 | 15篇 |
2021年 | 18篇 |
2020年 | 33篇 |
2019年 | 34篇 |
2018年 | 13篇 |
2017年 | 30篇 |
2016年 | 21篇 |
2015年 | 32篇 |
2014年 | 39篇 |
2013年 | 42篇 |
2012年 | 33篇 |
2011年 | 41篇 |
2010年 | 31篇 |
2009年 | 49篇 |
2008年 | 40篇 |
2007年 | 35篇 |
2006年 | 29篇 |
2005年 | 26篇 |
2004年 | 16篇 |
2003年 | 15篇 |
2002年 | 25篇 |
2001年 | 12篇 |
2000年 | 17篇 |
1999年 | 15篇 |
1998年 | 19篇 |
1997年 | 18篇 |
1996年 | 13篇 |
1995年 | 13篇 |
1994年 | 12篇 |
1993年 | 14篇 |
1992年 | 11篇 |
1991年 | 6篇 |
1990年 | 6篇 |
1989年 | 9篇 |
1987年 | 5篇 |
1985年 | 3篇 |
1982年 | 1篇 |
1981年 | 1篇 |
1980年 | 1篇 |
1979年 | 1篇 |
1978年 | 3篇 |
1977年 | 2篇 |
1954年 | 3篇 |
排序方式: 共有818条查询结果,搜索用时 15 毫秒
91.
92.
梭梭幼苗死亡与土壤和大气干旱的关系研究 总被引:8,自引:3,他引:5
以古尔班通古特沙漠南缘沙漠中的一年生梭梭幼苗为研究对象,对环境气象因子、土壤含水率、幼苗根系垂直伸展状况、幼苗死亡动态进行了全生长期的连续监测研究。结果表明,尽管梭梭幼苗根系伸展迅速,当年可达1.5 m,幼苗死亡率动态变化仍然与土壤表层含水率显著相关,而与根区或深层含水率不显著相关。但统计分析结果显示,土壤表层含水率并不总是梭梭幼苗死亡率波动的主导因素。当土壤含水率低至0.82%时,无论大气干旱程度如何,幼苗死亡率都急剧升高;而当土壤含水率高于1.25%时,幼苗可以耐受大气干旱,幼苗死亡只与土壤表层含水率显著相关;当土壤含水率在0.82~1.25%之间时,幼苗死亡率与大气干旱程度(空气饱和差)显著相关。据此我们推测,当土壤表层含水率低于1.25%时,大气干旱主导死亡率的变化;反之,则土壤水分主导。 相似文献
93.
Boundary shear stress and flow variability due to its interaction with main flow and secondary currents were investigated under conditions that extend previous research on trapezoidal channels. Secondary currents that scale with the flow depth were found over the entire width in all experiments. These findings contradict the widespread perception that secondary currents die out at a distance of 2.5 times the flow depth from the bank, a perception which is largely based on experiments with smooth boundaries. The reported results indicate that a stable pattern of secondary currents over the entire channel width can only be sustained over a fixed horizontal bed if the bed's roughness is sufficient to provide the required transverse oscillations in the turbulent shear stresses. Contrary to laboratory flumes, alluvial river bed always provide sufficient roughness. The required external forcing of this hydrodynamic instability mechanism is provided by the turbulence-generated near-bank secondary currents. The pattern of near-bank secondary currents depends on the inclination and the roughness of the bank. In all configurations, secondary currents result in a reduction of the bed shear stress in the vicinity of the bank and a heterogeneous bank shear stress that reaches a maximum close to the toe of the bank. Moreover, these currents cause transverse variability of 10–15% for the streamwise velocities and 0.2u*2–0.3u*?2 for the bed shear stress. These variations are insufficient to provide the flow variability required in river restoration projects, but nevertheless must be accounted for in the design of stable channels. 相似文献
94.
A series of experiments for the incipient motion of frazil particles under ice cover have been carried out in laboratory under different flow and boundary conditions.Measurements on flow velocities across the measuring cross-section at different water depths have been conducted.Based on these experiments under both ice-covered and open flow conditions,the impacts of solid boundary(such as ice cover and flume sidewall) on the distribution of flow velocity profiles have been discussed.The criteria for the inc... 相似文献
95.
In this experimental study,field observations and laboratory experiments have been carried out to assess the impacts of the vegetated channel walls and aspect ratio on flow velocity profiles,shear stress distribution and roughness coefficient of channel.Results show that the presence of vegetation cover on channel wall causes deviation of the Reynolds stress distribution from the linear one under uniform flow condition.It is also noticed that the Reynolds stress distribution is influenced by the aspect rati... 相似文献
96.
97.
Vertical profiles of fluid velocity and suspended sediment concentration in nearshore 总被引:2,自引:0,他引:2
Based on the power function of velocity and the friction velocity,a velocity profile is obtained.By solving the Schmidt’s diffusion equation,an equilibrium suspended sediment concentration profile is further deduced.The profiles of velocity and suspended sediment concentration agree well with the field data,and the profile of suspended sediment concentration avoids the unreasonableness of the classical Rouse profile such as a zero value at the water surface.According to these profiles,an expression which is easy to use for calculating the suspended sediment transport rate is derived. 相似文献
98.
Both P- and S-wave arrivals were collected for imaging upper crustal structures in the source region of the April 20, 2013 Lushan earthquake. High-resolution, three- dimensional P and S velocity models were constructed by travel-time tomography. Moreover, more than 3700 after- shocks of the Lushan earthquake were relocated via a grid search method. The P- and S-wave velocity images of the upper crust show largely similar characters, with high and low velocity anomalies, which mark the presence of sig- nificant lateral and vertical heterogeneity at the source region of the Lushan earthquake. The characteristics of the velocity anomalies also reflect the associated surface geo- logical tectonics in this region. The distributions of high velocity anomalies of both P- and S-waves to 18 km depth are consistent with the distributions of relocated after- shocks, suggesting that most of the ruptures were localized inside the high velocity region. In contrast, low P and S velocities were found in the surrounding regions without aftershocks, especially in the region to the northeast of the Lushan earthquake. For the relocated aftershocks of the Lushan earthquake from this study, we found that mostaftershocks were concentrated in a zone of about 40 km long and 20 km wide, and were located in the hanging wall of Dayi-Mingshan fault. The focal depths of aftershocks increase from the southeast to the northwest region in the direction perpendicular to the fault strike, suggesting that the fault ruptured at an approximate dip angle of 45°. The main depths of the aftershocks in the northwest of the main shock are significantly shallower than expected, revealing the different seismogenic conditions in the source region. 相似文献
99.
100.
Predicting the velocity within the ship’s propeller jet is the initial step to investigate the scouring made by the propeller jet. Albertson et al. (1950) suggested the investigation of a submerged jet can be undertaken through observation of the plain water jet from an orifice. The plain water jet investigation of Albertson et al. (1950) was based on the axial momentum theory. This has been the basis of all subsequent work with propeller jets. In reality, the velocity characteristic of a ship’s propeller jet is more complicated than a plain water jet. Fuehrer and Römisch (1977), Blaauw and van de Kaa (1978), Berger et al. (1981), Verhey (1983) and Hamill (1987) have carried out investigations using physical model. Current paper reviews the state-of-art of the equations used to predict the time-averaged axial, tangential and radial components of velocity within the zone of flow establishment and the zone of established flow of a ship’s propeller jet. 相似文献