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91.
Kensuke Naka Shinsuke Inagi Yoshiki Chujo 《Macromolecular rapid communications》2006,27(24):2113-2117
Summary: The first π‐conjugated poly(thioketene dimer) was synthesized via the homopolymerization of a silylthioketene dimer by a chemical oxidation‐reduction process. The polymerization of trimethylsilylthioketene dimer in the presence of FeCl3 (in CHCl3 at 70 °C for 24 h) gave the corresponding doped poly(thioketene dimer). After treatment of the doped polymer with an aqueous solution of ammonia, the neutral poly(thioketene dimer) was obtained with an incidental desilylation. The polymer obtained was soluble in DMF and DMSO. From gel permeation chromatographic analysis (DMF, polystyrene standards), the number‐average molecular weight of the polymer was found to be 7 460. The polymer showed low oxidation potentials derived from the thioketene dimer unit. An effective extension of the π‐conjugation was observed in the polymer.
92.
Journal of Algebraic Combinatorics - Motivated by the theory of correspondence functors, we introduce the notion of germ in a finite poset, and the notion of germ extension of a poset. We show that... 相似文献
93.
94.
A new method for the separation and determination of trace amounts of cadmium and zinc in water as their thenoyltrifluoroacetone
(TTA) complexes with dibenzo-18-crown-6 (DB18C6) in o-dichlorobenzene has been established by means of synergistic extraction
and back-extraction combined with atomic absorption spectrometry. The effect of various factors (synergism with TTA and DB18C6,
shaking time, composition of the extracted species, and mutual separation etc.) on the extraction and back-extraction of cadmium
and zinc has been in- vestigated. When the mixtures were extracted for 4 min at pH 4.9, only zinc was extracted quantitatively,
whereas cadmium remained in the aqueous phase. After the phases were separated, cadmium was again extracted quantitatively
at pH 7.5. Then, the two phases were each shaken with 0.05–0.1 mol/l HCl in order to back-extract cadmium and zinc from the
organic phases; the ions were determined individually by atomic absorption spectrometry. In the process cadmium and zinc TTA
chelates in o-dichlorobenzene form stable adducts with DB18C6 (Cd(TTA)2 ⋅ nDB18C6 and Zn(TTA)2 ⋅ nDB18C6, n=0∼2). The stability constants (βn) of the adducts determined by means of the curve fitting method were log β1=4.62 and log β2=6.74 for cadmium, and log β1=3.48 and log β2=5.18 for zinc.
Received: 8 September 1995/Revised: 22 January 1996/Accepted: 24 January 1996 相似文献
95.
Miharu Eguchi Hiroshi Tachibana Shinsuke Takagi Haruo Inoue 《Research on Chemical Intermediates》2007,33(1-2):191-200
The intercalation behavior of cationic porphyrin derivatives within the interlayer spaces of nano-layered clay minerals has been investigated. The porphyrins were successfully intercalated by the newly adopted method of repeated freeze-thaw cycles. The absorption spectra of the porphyrins were compared in the solution phase, adsorbed onto the exfoliated clay nano-sheets, intercalated within the interlayer spaces of clay sheets dispersed in water and intercalated in dry films. Substantial red shifts of the λmax values in the absorption spectra of the porphyrins were observed on the exfoliated clay sheets, and further red shifts were induced within the interlayer space. The dry films of the intercalated samples exhibited the largest red shifts. X-ray diffraction studies revealed that the clearance space between the layers in these intercalated hybrid compounds is only large enough for the porphyrins to be rigidly packed parallel to the clay layer. For the exfoliated clay nano-sheets, theoretical calculations were carried out on the correlation between the dihedral angle of the meso-substituted pyridiniumyl plane vs. the porphyrin ring and the λmax of the porphyrin Soret band. An extrapolation of the experimental λmax value to the correlation curve, afforded the dihedral angle to be 61.6°. The microscopic structure of the adsorbed state of the cationic porphyrins on the exfoliated clay nano-sheets was, thus, proposed to involve an orientation parallel to the clay surface, with a distance of 0.15 nm from the surface, which implies the expulsion of the solvent water molecules. 相似文献
96.
A new method for the preconcentration and determination of trace amounts of lead at the μg/L level in natural waters has
been established based on the formation of the thenoyltrifluoroacetone (TTA) complex with dibenzo-18-crown-6 (DB18C6) by means
of synergistic extraction and back-extraction combined with atomic absorption spectrometry (AAS). The effect of various factors
(synergism with TTA and DB18C6, shaking time, preconcentration factor, composition of the extracted species, and foreign ions
etc.) on the extraction and back-extraction of lead has been investigated in detail. The lead-TTA chelate in o-dichlorobenzene forms a stable adduct with DB18C6 as Pb(TTA)2 DB18C6. The stability constant (β) of the adduct determined by curve fitting method was log β = 4.2. The amount of lead in
natural waters such as tap water (Kanazawa University) and Kakehashi river (Komatsu City) determined by the present method
was found to be 0.64 ± 0.02 μg/L and 5.10 ± 0.03 μg/L, respectively.
Received: 14 July 1997 / Revised: 3 November 1997 / Accepted: 20 January 1998 相似文献
97.
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100.
Direct observations through a microscope and in-situ Raman scattering measurements of synthesized single-crystalline Kr hydrate have been performed at pressures up to 5.2 GPa and 296 K. We have observed that the initial cubic structure II (sII) of Kr hydrate successively transforms to a cubic structure I (sI), a hexagonal structure, and an orthorhombic structure (sO) called "filled ice" at 0.45, 0.75, and 1.8 GPa, respectively. The sO phase exists at least up to 5.2 GPa. In addition to these transformations, we have also found the new phase behavior at 1.0 GPa, which is most likely caused by the change of cage occupancy of host water cages by guest Kr atoms without structural change. Raman scattering measurements for observed phases have shown that the lattice vibrational peak at around 130 cm(-1) disappears in the pressure region of sI, which enables us to distinguish the sI phase from sII and sH phases. 相似文献