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Thirty four objects appearing in the SharplessCatalogue of H ii Regions with radio flux densities below 0.1 fu* at 1400 MHz, are studied. It is shown that two of them are planetary nebulae, two are reflection nebulae and two weak emission-reflection nebulae. From statistical arguments it is concluded that six may be evolved planetaries while the remaining are faint nearby Hii regions excited by stars of relatively advanced spectral type. 相似文献
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425.
The paper presents the results of field measurements of critical conditions for bedload motion conducted in the Rio Cordon, a steep boulder‐bed stream in the Italian Alps, under conditions of high Reynolds numbers and low relative submergence poorly explored before. Two methods have been used to determine threshold of motion: the displacement of marked clasts and the flow competence approach, which uses the largest grain size diameter transported by each flood event. The high values of confirm the great relevance of non‐bedload effective shear stresses in step–pool streams given by the additional form drag associated with this morphology. Relative submergence effects on the dimensionless critical shear stress have been quantified by considering the relative submergence ratio Rh/D84, and the major effect of relative size on the mobility of each particle in steep, widely graded bed mixtures has been evaluated. Finally, the dimensionless critical unit discharge has also been adopted in the regression equations as the critical hydraulic parameter, because it may represent an easier parameter to use than the critical shear stress for steep, rough mountain rivers. Copyright © 2006 John Wiley & Sons, Ltd. 相似文献
426.
Assessing multifaceted vulnerability and resilience in order to design risk-mitigation strategies 总被引:3,自引:1,他引:2
Scira Menoni Daniela Molinari Dennis Parker Francesco Ballio Sue Tapsell 《Natural Hazards》2012,64(3):2057-2082
Vulnerability studies have evolved significantly in recent decades. Although not overly theoretical compared with some other fields of science, some important conceptual progress has been made. At the practical level, vulnerability indicators have been used either at a generic level or for particular hazard contexts. However, these indicators are often predictably too narrow in their coverage of aspects of vulnerability. An important need remains to produce more conceptually informed vulnerability indicators or parameters and more satisfactory operational tools to assess weaknesses and resilience in coping with natural risks. In this paper, we present the methodology developed in the context of a recently concluded EU funded project, ENSURE (Enhancing resilience of communities and territories facing natural and na-tech hazards). The resulting vulnerability and resilience assessment framework tool adopts a systemic approach embedding and integrating as much as possible the multifaceted and articulated nature of concepts such as vulnerability and resilience. The tool guides evaluators towards a comprehensive and context-related understanding of strengths and fragilities of a given territory and community with respect to natural extremes. In this paper, both the framework tool and its application to Sondrio in Italy, which is exposed to flash floods, are presented and discussed. The merits and demerits of the new tool are discussed, and the results of the application to Sondrio indicate where data are currently missing, suggesting the kind of data, which will need to be gathered in future to achieve more complete assessments. The results also suggest vulnerability reduction policies and actions and further ways of revising the existing framework tool in the future. 相似文献
427.
In recent decades, slope instability in high-mountain regions has often been linked to increase in temperature and the associated permafrost degradation and/or the increase in frequency/intensity of rainstorm events. In this context we analyzed the spatiotemporal evolution and potential controlling mechanisms of small- to medium-sized mass movements in a high-elevation catchment of the Italian Alps (Sulden/Solda basin). We found that slope-failure events (mostly in the form of rockfalls) have increased since the 2000s, whereas the occurrence of debris flows has increased only since 2010. The current climate-warming trend registered in the study area apparently increases the elevation of rockfall-detachment areas by approximately 300 m, mostly controlled by the combined effects of frost-cracking and permafrost thawing. In contrast, the occurrence of debris flows does not exhibit such an altitudinal shift, as it is primarily driven by extreme precipitation events exceeding the 75th percentile of the intensity-duration rainfall distribution. Potential debris-flow events in this environment may additionally be influenced by the accumulation of unconsolidated debris over time, which is then released during extreme rainfall events. Overall, there is evidence that the upper Sulden/Solda basin (above ca. 2500 m above sea level [a.s.l.]), and especially the areas in the proximity of glaciers, have experienced a significant decrease in slope stability since the 2000s, and that an increase in rockfalls and debris flows during spring and summer can be inferred. Our study thus confirms that “forward-looking” hazard mapping should be undertaken in these increasingly frequented, high-elevation areas of the Alps, as environmental change has elevated the overall hazard level in these regions. 相似文献
428.
Giacomo D’Amato Avanzi Francesco Falaschi Roberto Giannecchini Alberto Puccinelli 《Natural Hazards》2009,50(3):591-603
This study aims at contributing to the soil slip susceptibility assessment in a typical basin of the southern Apuan Alps,
Italy. On June 1996, this basin (Cardoso Torrent, 13 km2 large) was hit by an extremely heavy rainstorm (maximum intensity of about 160 mm/h), which caused many landslides (debris
slide–debris flows) and valley bottom flows (hyperconcentrated flows), destruction and deaths. Detailed surveys provided the
characterization of the main factors (geological, geomorphologic, hydrological, hydrogeological and geotechnical) which contributed
in triggering landslides. In order to evaluate the soil slip susceptibility in this area, a physically based model was applied
and a GIS analysis of digital elevation model was performed. This approach couples a mechanical model based on an infinite
slope form of the Mohr–Coulomb failure criterion, and a steady-state hydrological one (a modified version of Shalstab, which
considers the cohesion of the debris material potentially involved in landsliding). GIS techniques allowed evaluating the
effects of topographic convergence and drainage area on slope failure. In this way, based on the infiltration rate, the triggering
of the June 1996 landslides was simulated and the critical rainfall thresholds assessed at about 200–250 mm/24 h. 相似文献
429.
Ashraf Owis Francesco Topputo Franco Bernelli-Zazzera 《Celestial Mechanics and Dynamical Astronomy》2009,103(1):1-16
The solution of a feedback optimal control problem arising in orbital mechanics is addressed in this paper. The dynamics is
that of a massless body moving in a central gravitational force field subject also to a drag and a radial modulated force.
The drag is linearly proportional to the velocity and inversely proportional to the square of the distance from the center
of attraction. The problem is tackled by exploiting the properties of a suitably devised linearizing map that transforms the
nonlinear dynamics into an inhomogeneous linear system of differential equations supplemented by a quadratic objective function.
The generating function method is then applied to this new system, and the solution is back transformed in the old variables.
The proposed technique, in contrast to the classical optimal control problem, allows us to derive analytic closed-loop solutions
without solving any two-point boundary value problem. Applications are discussed. 相似文献
430.
We compute the weak stability boundary in the planar circular restricted three-body problem starting from the algorithmic definition, and its generalization by García and Gómez. In addition, we consider a new set of primaries, Sun–Jupiter, to replace the case of Earth–Moon considered in previous studies. Numerical enhancements are described and compared to previous methods. This includes defining the equations of motion in polar coordinates and a modified numerical scheme for the derivation of both stable sets and their boundaries. These enhancements decrease the computational time. New results are obtained by considering the Sun–Jupiter case which we compare to the Earth–Moon case. 相似文献