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301.
This investigation deals with the torsional balance of the earthquake response and design of elastic asymmetric structures with frictional dampers. Plan asymmetry leads to an uneven lateral deformation demand among structural members and to unbalanced designs with larger capacities in some resisting planes. Frictional dampers are capable of controlling lateral‐torsional coupling by placing the so‐called empirical center of balance (ECB) of the structure at equal distance from all edges of the building. This rule is developed for single‐story systems with linear and inelastic behavior. However, recently obtained theoretical and experimental results demonstrate that this rule carries over to multistory structures. Results show that the peak displacement demand at the building edges and that of resisting planes equidistant from the geometric center may be similar if the damper is optimally placed. It is also shown that torsional amplification of the edge displacements of arbitrary asymmetric structures relative to the displacement of the symmetric counterparts are approximately bound by a factor of 2. Furthermore, frictional dampers are equally effective in controlling lateral‐torsional coupling of torsionally flexible as well as stiff structures. Copyright © 2005 John Wiley & Sons, Ltd. 相似文献
302.
低应力区岩石变形记忆效应形成机制及失忆性 总被引:1,自引:0,他引:1
地应力信息储存于开挖后的岩石中,变形率变化法(DRA)是基于岩石变形记忆效应测量地应力的方法,正确的机制是认识变形记忆效应与推广、改进DRA法的基础。传统推测的机制并不能解释低应力区存在变形记忆效应及失忆性等现象。首先进行火山沉积岩试样的物理试验,证明低应力区仍然存在变形记忆效应,记忆信息可同时采用侧向应变及轴向应变测量,两者精度一致。提出在低应力区,岩石变形记忆效应机制为微裂纹接触面及颗粒接触面的摩擦滑动。基于此机制,采用弹性元件、黏性元件和圣维南体构建相应的轴对称理论基本单元模型及多接触面理论模型。进行不同放置时间下的单轴循环压缩试验。结果表明,由轴对称理论模型可以得到低应力区岩石变形记忆效应、侧向DRA曲线与轴向DRA曲线准确度一致且在记忆信息处向上弯曲等、并对失忆性现象进行了初探。理论模型与物理试验结果一致,由此证明微裂纹接触面及颗粒接触面的摩擦滑动可以得到低应力区岩石变形记忆效应。同时,理论模型及物理试验结果为提高DRA法的测量准确度提供了依据。 相似文献
303.
304.
The shaft resistance of rock-socketed piles depends not only on the properties of its surrounding rock, but also on the radial force induced by the load imposed on the top of the pile. This paper deduced a plastic zone of rock around a single pile and obtained the shaft resistance of a rock-socketed pile based on the theories of cavity expansion and shear strength. The research results showed that the magnitude of the radial force in the socketed portion of a rock-socketed pile was related to the pile diameter, Poisson’s ratio, and properties of the surrounding rock. The influence area of rock decreased with increasing pile diameter. The radial force and lateral friction decreased with the increasing relative stiffnesses of the pile and rock. The radial stress on the elastic–plastic interface can be analytically determined based on the rock properties and depth. A field test was used to validate the proposed method, and a good agreement was obtained between the field data and predicted results of the proposed method. The research results in this paper are beneficial to guide actual practice. 相似文献
305.