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91.
    
Summary A four-year set of tilt data (1986–1989) recorded at three sites of the Central Apennines (Italy) and which in the past pointed out quite good raw tilt responses to seismicity, only with moderate thermoelastic effects, have been investigated to search for the possible existence of tilt anomalies accompanying the main earthquakes of the region. It has been observed that, even if fairly good tilt responses to principal evants seem to appear, correlations of similar or better quality are obtained when comparing the same tilts with pressure and mainly with temperature. However, when taking into account earthquakes with magnitudesM≥3.0 and more strictE (strain) andL (source dimension) threshold values (the last two parameters being used to evaluate tilt field at a distanceR), only one event (M=3.5;R=5.1 km) has been selected and tectonic from non-tectonic contributions have been pointed out clearly at one tilt site. The quoted earthquake showed the bestE andR/L values (E=10−6;R/L=2.4) in the whole period and it was preceded by a clear tilt anomaly with amplitude and duration of about 5 μrad and 2 months, respectively. Since the tilt signal in this period is not affected by any non-tectonic effect (maximum correlation coefficient with temperaturer=0.2) the quoted anomaly has been considered as a probable precursor of the above-mentioned earthquake it preceds. Residual, tilt vector oscillations along the direction-including the epicentral area of this event, were also observed. On the contrary, all the remaining anomalous tilts proved to be well justified with pressure and/or temperature variations (r values up to 0.8).  相似文献   
92.
In an experiment performed at the CERN-SPS charged hyperon beam, we have observed the radiative decay Λ→nγ, using well identified Λ from the decays of Ο? of 116 GeV/c momentum. Neutrons and photons from the Λ decays were observed in liquid argon and lead glass detectors. From a sample of 31 candidates, containing an estimated background of 7.3 events, the decay branching ratio was measured to be Γ(Λ→nγ)/Γ(Λ→all)=(1.02±0.33)×10?3.  相似文献   
93.
The static quadrupole moments of the first excited Jπ = 2+ states in 20Ne and 22Ne and the reduced electric quadrupole transition probabilities of these states to the ground states were measured via projectile Coulomb excitation. The quadrupole moments were deduced from the shapes of γ-ray angular distributions. The results are: Q(20Ne, 2+) = −0.20±0.05 b and Q(22Ne, 2+) = −0.11±0.05 b. The transition strengths were deduced from yield measurements and by comparison with the yields of target γ-rays. The results are: B(E2; 0+ → 2+, 20Ne) = 0.037±0.003 e2 · b2 and B(E2; 0+ → 2+, 22Ne) = 0.025±0.002 e2· b2. The results for the transition strengths are consistent with the results of accurate timing methods and resolve discrepancies between previous experiments. The results for the quadrupole moments are consistent with earlier measurements, although the mean values we obtain are slightly lower. The experimental measurements are compared with theoretical predictions and a detailed discussion is given of corrections to this type of reorientation experiment.  相似文献   
94.
The substituted 4H-pyrido[1, 2-a]pyrimidin-4-ones (I) were obtained by the condensation of substituted 2-aminopyridines with δ-ketocarboxylic esters in PPA. Some of the derivatives I were transformed into the corresponding 1, 8-naphthyridines II and III.  相似文献   
95.
Summary For more than ten years several measurements sites able to detect geophysical and geochemical precursory phenomena of earthquakes have been working in Soviet Georgia. On the occasion of the destructive Armenia earthquake of December 7, 1988 (M=6.9) premonitory signals relative to geophysical and geochemical parameters seem to be observed. In this paper anomalous variations of the water level in a well, of the helium content in thermal waters and of the electromagnetic signals in air, obtained in three measurements sites located at about 80 km from the epicentre, are reported. These variations appear beginning from about a month up to some hours before the occurrence of the earthquake and it seems reasonable to consider them as short-time or very short-time precursory phenomena of the earthquake.  相似文献   
96.
    
Summary Ground tilt measurements carried out at three tilt sites of the Central Apennines (Italy) revealed a quite good correspondence with seismicity (M≤4.9) which took place within a distance of 100 km from the sites and over a period of four years (1986–1989). The best correlation is obtained when the tilt signals are delayed by about 1.5 months with respect to the seismic one (number of earthquakes per month), suggesting that seismicity is predictable to a certain extent from the local tilt response. Correlations of similar quality showed also that tiltmeters located at different sites seem to react in a different way to events distributed along the two main active fault zones (namely, the Apennine and anti-Apennine ones), indicating an anisotropic response of the medium. To explain how the seismicity, selected along the Apennine and anti-Apennine directions, give rise to different tilt responses at tilt sites located at a relative small distance, the behaviour of the geological structures and of the geodynamic processes of the investigation area have been taken into account.  相似文献   
97.
The two-dimensional self-assembly of a terbium(III) double-decker phthalocyanine on highly oriented pyrolitic graphite (HOPG) was studied by atomic force microscopy (AFM), and it was shown that it forms highly regular rectangular two-dimensional nanocrystals on the surface, that are aligned with the graphite symmetry axes, in which the molecules are organized in a rectangular lattice as shown by scanning tunneling microscopy. Molecular dynamics simulations were run in order to model the behavior of a collection of the double-decker complexes on HOPG. The results were in excellent agreement with the experiment, showing that-after diffusion on the graphite surface-the molecules self-assemble into nanoscopic islands which align preferentially along the three main graphite axes. These low dimension assemblies of independent magnetic centers are only one molecule thick (as shown by AFM) and are therefore very interesting nanoscopic magnetic objects, in which all of the molecules are in interaction with the graphite substrate and might therefore be affected by it. The magnetic properties of these self-assembled bar-shaped islands on HOPG were studied by X-ray magnetic circular dichroism, confirming that the compounds maintain their properties as single-molecule magnets when they are in close interaction with the graphite surface.  相似文献   
98.
Structural complexity has been shown to be a measure of the variety of load paths in structures with high degree of static indeterminacy, for example, frames. The variations of the value of complexity parameters across different structures have been investigated in previous researches. Herein, the effects of scaling on load distribution and on geometry of the structural scheme are outlined. A scale invariance is shown for load magnitude. Complexity variation is outlined for geometric similar structures, depending essentially on the consistency of the load set. A transition in the behavior of the structural scheme under loads is recorded in case of similar structures from small to large scales. The results are discussed. © 2014 Wiley Periodicals, Inc. Complexity 20: 57–63, 2014  相似文献   
99.
We have isolated at T < 150 K a weakly adsorbed dimethyl disulfide (DMDS) layer on Au(111) and studied how the vibrational states, S core hole level shifts, valence band photoemission, and work function measurements evolve upon transforming this system into chemisorbed methylthiolate (MT) self-assembled monolayers (SAM) by heating above 200 K. By combining these observations with detailed theoretical electronic structure simulations, at the density functional level, we have been able to obtain a detailed picture of the electronic interactions at the interface between Au and adsorbed thiolates and disulfides. All of our measurements may be interpreted with a simple model where MT is bound to the Au surface with negligible charge transfer. Interfacial dipoles arising from Pauli repulsion between molecule and metal surface electrons are present for the weakly adsorbed DMDS layer but not for the chemisorbed species. Instead, for the chemisorbed species, interfacial dipoles are exclusively controlled by the molecular dipole, its interaction with the dipoles on neighboring molecules, and its orientation to the surface. The ramifications of these results for alignment of molecular levels and interfacial properties of this class of materials are discussed.  相似文献   
100.
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