全文获取类型
收费全文 | 1554篇 |
免费 | 373篇 |
国内免费 | 350篇 |
专业分类
测绘学 | 91篇 |
大气科学 | 32篇 |
地球物理 | 690篇 |
地质学 | 1066篇 |
海洋学 | 81篇 |
天文学 | 8篇 |
综合类 | 159篇 |
自然地理 | 150篇 |
出版年
2024年 | 4篇 |
2023年 | 16篇 |
2022年 | 39篇 |
2021年 | 51篇 |
2020年 | 49篇 |
2019年 | 89篇 |
2018年 | 76篇 |
2017年 | 70篇 |
2016年 | 64篇 |
2015年 | 92篇 |
2014年 | 75篇 |
2013年 | 121篇 |
2012年 | 102篇 |
2011年 | 84篇 |
2010年 | 75篇 |
2009年 | 116篇 |
2008年 | 124篇 |
2007年 | 101篇 |
2006年 | 95篇 |
2005年 | 75篇 |
2004年 | 100篇 |
2003年 | 80篇 |
2002年 | 74篇 |
2001年 | 63篇 |
2000年 | 61篇 |
1999年 | 59篇 |
1998年 | 36篇 |
1997年 | 39篇 |
1996年 | 41篇 |
1995年 | 42篇 |
1994年 | 28篇 |
1993年 | 33篇 |
1992年 | 24篇 |
1991年 | 17篇 |
1990年 | 15篇 |
1989年 | 9篇 |
1988年 | 9篇 |
1987年 | 4篇 |
1986年 | 11篇 |
1985年 | 4篇 |
1984年 | 2篇 |
1983年 | 1篇 |
1979年 | 4篇 |
1978年 | 2篇 |
1954年 | 1篇 |
排序方式: 共有2277条查询结果,搜索用时 312 毫秒
91.
卫星地面站雷电防护工程通常采用接闪杆作为天线主体的雷电直击效应防护措施,接闪杆的高度不仅影响其保护范围,而且影响其截闪概率。通过计算年预计雷击次数对截闪概率进行量化分析,结果表明,截闪概率近似与接闪杆高度平方成正比,采用过高的接闪杆将增大地面站遭受雷击电磁脉冲损坏的风险。为优化接闪杆设计,定义了保护体积的概念,并利用折线法与滚球法分别计算了三维立体空间内的保护范围。结果表明:接闪杆的保护范围与高度呈现非线性相关,当接闪杆超过一定高度(折线法超过30m,滚球法超过0.8倍滚球半径)后,对保护范围的影响十分有限;当接闪杆高度低于0.4倍滚球半径时,滚球法保护范围较大,反之则折线法保护范围较大。对接闪杆接闪瞬间周边的磁场强度分析结果表明,无屏蔽环境下地面站电子系统与接闪杆的常规距离远小于两者的理论安全距离,实际工程中难以通过增大接闪杆与卫星地面站的间距消除雷击电磁脉冲危害。为降低这一风险,卫星地面站直击雷防护应优先采用天线自带接闪杆的方式,条件不具备时也应尽量避免采用单支高大接闪杆,可选取适当的计算方法,采用多支较低接闪杆共同防护的方案。 相似文献
92.
This paper presents two test procedures for evaluating the bond stress–slip and the slip–radial dilation relationships when the prestressing force is transmitted by releasing the steel (wire or strand) in precast prestressed elements. The bond stress–slip relationship is obtained with short length specimens, to guarantee uniform bond stress, for three depths of the wire indentation (shallow, medium and deep). An analytical model for bond stress–slip relationship is proposed and compared with the experimental results. The model is also compared with the experimental results of other researchers. Since numerical models for studying bond‐splitting problems in prestressed concrete require experimental data about dilatancy angle (radial dilation), a test procedure is proposed to evaluate these parameters. The obtained values of the radial dilation are compared with the prior estimated by numerical modelling and good agreement is reached. Copyright © 2012 John Wiley & Sons, Ltd. 相似文献
93.
94.
Frictional heat generation and seismic radiation in a foam rubber model of earthquakes 总被引:1,自引:0,他引:1
Results from a study of stick-slip particle motion at the interface between two stressed foam rubber blocks indicate that normal vibrations and interface separation are an important part of the stick-slip process in foam rubber. The dimension of the dynamic slip pulse is small compared to the dimension of the model (approximately 10 cm vs. 200 cm) consistent with the abrupt-locking slip pulse model ofBrune (1970, 1976), andHeaton (1990). A comparison of frictional heat generation between stable-sliding and stick-slip foam rubber models indicates a linear relation between the temperature increase on the fault surface (for a given distance of slip) and the driving shear force for the stable-sliding model, while for the stick-slip model there is essentially no variation in frictional heat generation with an increase in shear stress. We performed experiments to investigate the ratio of normal motion to shear motion at different levels of normal stress in the stick-slip foam rubber model. Preliminary result indicate that the normal component of the particle motion increases more rapidly with increasing normal stress than the shear component. The phenomenon of interface separation and normal vibrations may thus explain some of the most frustrating problems in earthquake mechanics, e.g., the heat flow paradox, the long-term weakness of major active faults, and anomalousP-wave radiation. 相似文献
95.
Evaluation of the Importance of Model Features For Cyclic Deformation Due to Dip-Slip Faulting 总被引:1,自引:0,他引:1
Steven C. Cohen 《Geophysical Journal International》1994,119(3):831-841
96.
沂沭活断层分段特征及地震趋势的预测 总被引:2,自引:0,他引:2
沂沭活断层以莒南—汤头一线为界可分成南北两大段。其中,北段以蠕滑为主,南段则表现为强烈的粘滑错动。另外,在南段内还存在着一个次一级的段落。文中详细分析了各段的断层滑动方式及地震活动的特点,并对沂沭断裂带今后的地震趋势作了预测。 相似文献
97.
98.
Thierry Winter Jean-Philippe Avouac Alain Lavenu 《Geophysical Journal International》1993,115(3):905-920
The northeast-trending Pallatanga right-lateral strike-slip fault runs across the Western Cordillera connecting N50E-N70E trending normal faults in the Gulf of Guayaquil with N-S reverse faults in the Interandean Depression. Over most of its length, the fault trace has been partly obscured by erosional processes and can be inferred in the topography only at the large scale. Only the northern fault segment, which follows the upper Rio Pangor valley at elevations above 3600 m, is prominent in the morphology. Valleys and ridges cut and offset by the fault provide an outstanding record of right-lateral cumulative fault displacement. The fault geometry and kinematics of this particular fault segment can be determined from detailed topographic levellings. The fault strikes N30E and dips 75 to the NW. Depending on their size and nature, transverse morphological features such as tributaries of the Rio Pangor and intervening ridges, reveal right-lateral offsets which cluster around 27 ± 11m, 41.5 ± 4 m, 590 ± 65 m and 960 ± 70 m. The slip vector deduced from the short-term offsets shows a slight reverse component with a pitch of about 11.5 SW. The 41.5 ± 4 m displacements are assumed to be coeval with the last glacial termination, yielding a mean Holocene slip-rate of 2.9- 4.6 mm yr−1 . Assuming a uniform slip rate on the fault in the long term, the 27 m offset appears to correlate with an identified middle Holocene morphoclimatic event, and the long term offsets of 590 m and 960 m coincide with the glacial terminations at the beginning of the last two interglacial periods. 相似文献
99.
We report two examples from the south of the French Alps, showing that radon emanation monitored by alpha-sensitive film may be used to locate certain discrete structural features revealed in data collected by remote sensing from a satellite. The variations observed in our data, over a period of several months, are in accordance with atmospheric changes and might correlate with local seismic activity when the detectors are located directly above structural fractures and the magnitude of the seismic event is greater than 2. 相似文献
100.
本文以滑波理论为依据,总结了山西地震带的两种不同特点的滑坡。即:振荡式滑坡及触发式滑坡。虽然两种滑坡都可分为变形、解体、滑动、毁灭等四个阶段,但其动力不同。振荡式滑波的滑动面倾角小,因而滑力来源于强震振动,而触发式滑坡的滑动面倾角大,因而滑力来自滑体本身静荷载。对两种滑坡的研究对预防及减轻强震带来的次生灾害有重要的意义。 相似文献