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International Intercomparison of Solar UVR Spectral Measurement Systems in Melbourne in 2013
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Peter Gies Rebecca Hooke Richard McKenzie John O'Hagan Stuart Henderson Andy Pearson Marina Khazova John Javorniczky Kerryn King Matt Tully Michael Kotkamp Bruce Forgan Stephen Rhodes 《Photochemistry and photobiology》2015,91(5):1237-1246
Monitoring ambient solar UVR levels provides information on how much there is in both real time and historically. Quality assurance of ambient measurements of solar UVR is critical to ensuring accuracy and stability and this can be achieved by regular intercomparisons of spectral measurement systems with those of other organizations. In October and November of 2013 a solar UVR spectroradiometer from Public Health England (PHE) was brought to Melbourne for a campaign of intercomparisons with a new Bentham spectrometer of Australian Radiation Protection and Nuclear Safety Agency (ARPANSA) and one at the Australian Bureau of Meteorology (BOM), supported by New Zealand's National Institute for Water and Atmosphere (NIWA). Given all three spectroradiometers have calibrations that are traceable to various national standards, the intercomparison provides a chance to determine measurement uncertainties and traceability that support UV measurement networks in Australia, New Zealand and the UK. UV Index measurements from all three systems were compared and ratios determined for clear sky conditions when the scans from each instrument were within 2 min of each other. While wavelengths below 305 nm showed substantial differences between the PHE unit and the two other systems, overall the intercomparison results were encouraging, with mean differences in measured UV Index between the BOM/NIWA and those of PHE and ARPANSA of <0.1% and 7.5%, respectively. 相似文献
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Mazur Milan Valko Marian Rhodes Christopher J. 《Journal of Sol-Gel Science and Technology》2017,82(3):855-861
Journal of Sol-Gel Science and Technology - The influence of the hydration and drying process on the line shape and signal intensity of the electron paramagnetic resonance spectra recorded from... 相似文献
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The Optical Fourier Transform (OFT) is one of the most fundamental operations in analogue Optical Signal Processing (OSP). There are many optical arrangements for implementing the OFT, however one which is particularly popular is the Scaled Optical Fourier Transform (SOFT) because it offers the user the ability to scale the output Fourier distribution. In this paper we study some of the practical limits introduced by using a converging spherical lens of finite aperture to produce the illuminating field in the implementation of the SOFT. By deriving simple rules of thumb, based on examining phase and intensity deviations from the ideal unapertured case, we define an area inside the geometric shadow, which we refer to as a sub-geometric shadow. Inside this sub-geometric shadow we show that the worst-case errors in the resulting SOFT, arising due to diffraction, can be quantified and avoided. 相似文献
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E. Perelli-Cippo G. Gorini M. Tardocchi C. Andreani A. Pietropaolo R. Senesi N.J. Rhodes E.M. Schooneveld 《Applied Physics A: Materials Science & Processing》2006,83(3):453-460
Strong demand exists for an experimental facility enabling new experimental investigations on condensed matter systems based
on epithermal neutron scattering at high energy and low momentum transfers. This need will be met by the very low angle detector
(VLAD) bank, to be installed on the VESUVIO spectrometer at the ISIS spallation neutron source. The equipment will operate
in the scattering angular range 1°<2θ<5°. Scattering measurements from a polycrystalline ice sample using a VLAD prototype
demonstrates the effectiveness of the detection technique adopted for the construction of the full detector array. The resulting
density of states in ice is 9±2 atoms/cell, in agreement with previous measurements.
PACS 61.12.Ex; 63.20.Dj; 63.50.+x 相似文献
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Diaz L Liauw CM Edge M Allen NS McMahon A Rhodes N 《Journal of colloid and interface science》2005,287(2):379-387
Flow microcalorimetry and infrared spectroscopy were used to study the surface structure and adsorptive properties of a series of calcined and uncalcined porous silicas. The adsorbates DL-menthol, (R)-(+)-limonene, (+/-)-citronellal and carvone were selected for their functionality, that included carbonyl, vinylic and hydroxyl groups. The amounts of probe retained by the silicas together with the energy exchange involved in the adsorption/desorption process were determined by flow microcalorimetry. The functional groups involved in these interactions were studied by means of infrared spectroscopy. It was observed that the strongest interactions with the silica surface took place through hydrogen bonding onto the surface silanol. The most retentive probes were found to be those with a carbonyl group in their structure. Adsorption onto calcined silicas was found to be less energetic than onto the equivalent calcined samples. The adsorption densities were compared with theoretical predictions based on molecular models. In all cases apart from citronellal monolayer coverage were not observed due to steric effects. 相似文献
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