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951.
The experimental evidence that cohesive and granular soils possess an elastic range in which the elasticity is both nonlinear and anisotropic—with stiffness and directional characteristics strongly dependent on stress and plastic strain (the so‐called ‘stress history’)—is given a formulation based on hyperelasticity. This is accomplished within the framework of elastoplastic coupling, through a new proposal of elastic potentials and a combined use of a plastic‐strain‐dependent fabric tensor and nonlinear elasticity. When used within a simple elastoplastic framework, the proposed model is shown to yield very accurate simulations of the evolution of elastic properties from initial directional stiffening to final isotropic degradation. Within the proposed constitutive framework, it is shown that predictions of shear band formation and evolution become closer to the existing experimental results, when compared to modelling in which elasticity does not evolve. Copyright © 2007 John Wiley & Sons, Ltd. 相似文献
952.
Dunja Peri 《国际地质力学数值与分析法杂志》2006,30(5):363-387
Analytical solutions are derived for a three‐invariant Cam clay model subjected to proportional and circular drained loading histories. The solutions are presented for a specific volume, and volumetric and generalized shear strains. In the case of a proportional loading only straight effective stress paths are considered while in the case of a circular loading the maximum possible change in Lode's angle is π/3 due to plastic isotropy. Additionally, a concept of deviatoric stiffness is devised and an analytical expression for the generalized hardening modulus is derived. Qualitative and quantitative analyses are carried out in the form of direct comparisons between analytical solutions for drained and undrained loading histories thus offering an improved understanding of the three‐invariant model. Copyright © 2006 John Wiley & Sons, Ltd. 相似文献
953.
Conventional numerical predictions of deep excavations normally neglect the construction process of the retaining structure and choose the earth pressure at rest as initial condition at the beginning of the simulation. The presented results of simulation and measurements during the construction process of the Taipei National Enterprise Center show, that such an assumption leads to an underestimation of the horizontal wall deflection, the surface ground settlements as well as the loading of the struts in case of normally to slightly over‐consolidated clayey soil deposits. The stepwise installation process of the individual diaphragm wall panels results in a substantial modification of the lateral effective stresses in the adjacent ground. Especially the pouring process of the panel and the fresh concrete pressure causes a partial mobilization of the passive earth pressure and a distinct stress level increase in the upper half of the wall. As a consequence of the increased stresses prior to the pit excavation, up to 15% greater ground and wall movements are predicted. Moreover, the increased stress level due to the installation process of the diaphragm wall leads to substantial higher strut loadings during the excavation of the pit. Copyright © 2006 John Wiley & Sons, Ltd. 相似文献
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系统测定了陕西洛川黑木沟黄土/古土壤的总有机碳及其主要组分(稳定有机碳、矿物保护有机碳和化学稳定有机碳)的含量,并对总有机碳与粘粒含量及粘土矿物含量的相关性进行了分析。结果表明:(1)各层古土壤的总有机碳含量均高于其下伏的黄土层(S4例外),而稳定有机碳、矿物保护有机碳以及化学稳定有机碳的平均含量在黄土与古土壤之间无明显差异;(2)黄土和古土壤中有机碳含量达到稳定所需要的时间不同,分别是140~250 ka和330~410ka;(3)总有机碳和化学稳定有机碳与粘粒呈正相关关系(相关系数r分别为0.46和0.54),它们与粉粒和细砂粒的相关性较差,这说明粘粒是土壤固定有机碳的重要组分;(4)高岭石与总有机碳和化学稳定有机碳的相关性比较明显(r分别为0.74和0.61),伊利石和蒙脱石与它们不相关或相关性较差。 相似文献
957.
山西本溪组铝土矿成矿条件及成矿规律探讨 总被引:3,自引:0,他引:3
通过对山西石炭系本溪组铝土矿,即华北G层铝土矿形成的构造背景、古地理环境及铝土矿床的分布分析,指出了山西铝土矿矿床主要分布在各古陆、古岛边缘的成矿盆地中,且成矿盆地的封闭性越好越有利于成矿.古陆上广泛出露的铝硅酸盐岩经过风化分解,其中的K、Na、Ca、Mg等元素大多数被淋失,Fe、Al、Ti、Si等元素相对富集,残留在红土风化壳中,经海侵短距离机械搬运至沉积盆地沉积.通过对铝土矿成分及其围岩物质组分的分析,进一步确认沉积在古陆边缘的原始铝土矿层埋藏于潜水面以下的还原环境中,经地下水、地表水等酸性溶液的淋滤脱硅后沉积成矿,后经地壳抬升,通过对原始铝土矿的渗流作用、氧化改造而达到铝土矿的富集,且铝土矿多分布在靠近古陆边缘的缓坡一侧,在沟谷两侧的高山低洼处矿体较富,而埋藏越深越则不利于成矿. 相似文献
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Horst G. Brandes 《Ocean Engineering》2011,38(7):835-848
Geotechnical properties from a series of deep-sea sites in the North Atlantic and North Pacific oceans are examined to evaluate overall trends and to compare with similar fine-grained soils found on land. The study areas encompass a range of sedimentary environments dominated by combinations of turbidite and pelagic deposits. Carbonate content in excess of 20% is seen to result in a decrease in liquid limit and compressibility. Vertical profiles of geotechnical properties in the North Pacific show broader changes in down-core geotechnical properties compared to the North Atlantic and reflect the effects of long-term climatic changes and seafloor spreading. Sediments in the North Atlantic indicate significant differences depending on location, which is attributed to variability in turbidite deposition, water depth, distance from sediment sources, and the effects of bottom currents. Compared to equivalent fine-grained soils on land, deep-sea sediments are generally softer, more compressible and have higher friction angles at comparable Atterberg limits. Deeper and older sediments in the North Pacific are characterized by unusually large plastic limits, which are attributed to the presence of volcanic fractions. Empirical relationships for compression index and friction angle are discussed for sediments from both oceans. 相似文献