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21.
Evaluation of added resistance in regular incident waves by computational fluid dynamics motion simulation using an overlapping grid system 总被引:2,自引:0,他引:2
A computational fluid dynamics simulation method called WISDAM-X was developed to evaluate the added resistance of ships in waves. The Reynolds-averaged Navier–Stokes (RANS) equation was solved by the finite-volume method and a MAC-type solution algorithm. An overlapping grid system was employed to implement rigorous wave generation, the interactions of ships with incident waves, and the resultant ship motions. The motion of the ship is simultaneously solved by combining the solution of the motion of the ship with the solution of the flow about the ship. The free surface is captured by treatment by the density-function method. The accuracy of WISDAM-X is examined by a comparison with experimental data from a container carrier hull form, and shows a fairly good agreement with respect to ship motion and added resistance. Simulations were also conducted for a bow-form series of a medium-speed tanker to examine the effectiveness of the WISDAM-X method as a design tool for a hull form with a smaller resistance in waves. It was confirmed that the WISDAM-X method can evaluate the added resistance with sufficient relative accuracy and can be used as a design tool for ships. 相似文献
22.
The effect of uniform current on the generation of flexural gravity waves resulting from initial disturbances at a point was
analyzed in two dimensions. The problem was formulated as an initial boundary value problem under the assumptions of the linearized
theory of water waves. By direct application of the Laplace transform and then the Fourier transform, explicit expressions
for the velocity potential and free surface elevation were obtained in integral forms; these were evaluated asymptotically
for large distances and times by the application of the method of the stationary phase to obtain the far field behavior of
the surface elevations in specific cases. Simple numerical computations were performed to illustrate the effect of uniform
current on the surface elevation, wavelength, phase velocity, and group velocity of the flexural gravity waves and on the
far field behavior of the progressive waves in two different cases, namely, when there is an initial depression concentrated
at the origin and an initial impulse concentrated at the origin. 相似文献
23.
The need for a Global Ocean Observing System Global (GOOS) is now widely appreciated. Parts of GOOS are currently being implemented already. In this paper, written on the request of the joint Scientific and Technical Committee of GOOS, we present some of the scientific issues that need to be addressed for the further development of the Ocean and Marine Meteorology Service module of GOOS. This module is concerned with monitoring and prediction of sea level (both tsunamis and storm surges) and wind driven waves (wind–sea and swell), among other things. For each of these we discuss the current state-of-the-art, indicate what observations are needed and make suggestions for future modelling development. 相似文献
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Railway wheel-flat detection and measurement by ultrasound 总被引:1,自引:0,他引:1
J. Brizuela C. Fritsch A. Ibáñez 《Transportation Research Part C: Emerging Technologies》2011,19(6):975-984
This work presents an innovative ultrasound technique designed to detect and quantify flats formed in the rolling surface of railway wheels. Differently from other approaches, ultrasonic pulses (Rayleigh waves) are sent over a measuring rail. The variations in the round-trip time of flight (RTOF) of the ultrasound pulse to the rail-wheel contact point allow detecting and quantifying the wheel-flats. In spite of the wear state of the irregularity, the method provides the loss of material and the length of the flat originally formed by abrasion. A theoretical background supports the technique which offers many advantages for railway maintenance. Simulations and experimental results match the expected ones. 相似文献
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Laurence C. Breaker David B. Gilhousen Hendrik L. Tolman Lawrence D. Burroughs 《Journal of Marine Systems》1998,16(3-4)
Measurements of boundary layer moisture have been acquired from Rotronic MP-100 sensors deployed on two NDBC buoys in the northern Gulf of Mexico from June through November 1993. For one sensor, which was retrieved approximately 8 months after deployment, the post- and precalibrations agreed closely and fell well within WMO specifications for accuracy. The second sensor operated continuously from June 1993 to February 1997 (3.5 years). Buoy observations of relative humidity and supporting data were used to calculate specific humidity and the surface fluxes of latent and sensible heat. Specific humidities from the buoys were compared with observations of moisture obtained from nearby ship reports, and the correlations were generally high (0.7–0.9). Surface gravity wave spectra were also acquired. The time series of specific humidity and the other buoy parameters revealed three primary scales of variability, small (h), synoptic (days), and seasonal (months). The synoptic variability was clearly dominant and occurred primarily during September, October, and November. Most of the synoptic variability was due to frontal systems that dropped down into the Gulf of Mexico from the continental US followed by air masses which were cold and dry. Cross-correlation analyses of the buoy data indicated that: (1) the moisture field was highly coherent over distances of 800 km or more in the northern Gulf of Mexico; and (2) both specific humidity and air temperature served as tracers of the motion associated with propagating atmospheric disturbances. These correlation analyses also revealed that the prevailing weather systems generally entered the buoy domain from the South prior to September, but primarily from the North thereafter. Spectra of the various buoy parameters indicated strong diurnal and semidiurnal variability for barometric pressure and sea surface temperature (SST) and lesser variability for air temperature, wind speed and significant wave height. The surface fluxes of latent and sensible heat were dominated by the synoptic events which took place from September through November with the transfer of latent heat being primarily from the ocean to the atmosphere. Finally, an analysis of the surface wave observations from each buoy, which included calculations of wave age and estimates of surface roughness, indicate that major heat and moisture flux events coincide with periods of active wave growth, although the data were insufficient to identify any causal relationships. 相似文献
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高速列车通过隧道时诱发车厢内压力波动的数值分析 总被引:6,自引:1,他引:5
在假定列车车体为均匀多孔车体的基础上,根据一维可压缩非定常不等熵流动理论与广义黎曼特征线法,研制了高速列车通过隧道过程中诱发车厢内外空气瞬变压力耦合的计算方法和计算程序。其中,基于热力学第一定律的“充排法”建立了车厢内压力波动的计算方法,并成功地将该方法推广应用于隧道内会车条件下车厢内压力的计算分析中。通过与国外试验数据的验证表明了本文计算方法与程序的正确性,为准确合理地计算高速列车通过隧道时诱发车厢内瞬变压力提供了可靠的分析工具。 相似文献