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161.
162.
Zusammenfassung Im ersten, der Festlegung der theoretischen Grundlagen der Trübung gewidmeten Kapitel wird die Sinkgeschwindigkeit kleiner
Teilchen auf Grund der Gesetze der ?Schwebetheorie? vonWesenberg-Lund, W. Ostwald sowie der Stokesschen Formel diskutiert.
Ein weiteres Kapitel orientiert anhand bisheriger Kenntnisse über die Erscheinungen der Lichtdurchl?ssigkeit (bzw.-absorption)
und des Lichtklimas in verschiedenen Tiefen unserer Seen. Die Trübung der in einer Reihe von Flu?systemen und Seen erhobenen
W?sser wurde mittels der absoluten Messung im Pulfrich-Stufenphotometer festgestellt. Sodann wurden die analysierten Proben
nach steigenden Trübungswerten geordnet und unterteilt in ?Klarseen?, ?mitteltrübe? und ?trübe? Seen. Schliesslich wurde zusammen
mitH. Züllig der Grad der Trübung, der Transparenz und die Seefarbe zueinander in Beziehung gebracht, wobei unterschieden wird zwischen
Seen, die a) durch vorwiegend anorganische Stoffe, b) durch vorwiegendOscillatoria-armes Plankton, c) durch vorwiegendOscillatoria rubescens getrübt sind.
Die in mehreren Tabellen und Abbildungen wiedergegebenen Werte der Wassertrübung spiegeln die unterschiedlichen Verh?ltnisse
wider, die sich im Laufe einer ausgedehnteren Flu?strecke oder in einem See ergeben aus der Mischung des verschieden stark
mit Schwebestoffen belasteten Wassers von Haupt- und Nebenfluss, sodann aus der fortschreitenden oder von Strecke zu Strecke
wechselnden Sedimentation, und natürlich auch von der lokalen oder regionalen Wetterlage (Niederschl?ge und Schneeschmelze).
In ausgedehnten und zum Teil über Monate hinweg durchgeführten Sedimentationsversuchen im Laboratorium wurde schliesslich
der Kl?rvorgang von W?ssern verschiedener Herkunft in Funktion der Zeit untersucht. Dabei ergaben sich unterschiedliche Kurven,
die ein Bild zu vermitteln verm?gen über den mittleren Durchmesser der die Trübung verursachenden sedimentierbaren, anorganischen
Partikeln. 相似文献
163.
A series of numerical studies on the behaviour of magnetic fields and motions in a spherical body of an electrically conducting incompressible fluid have been carried out. The magnetic field was assumed to be maintained by a given electromotive force inside the body and to continue as a potential field in outer space. In view of the motion an external forcing was taken into account, and boundary conditions were considered which correspond to a stress-free surface. The stability of several steady states has been studied as well as the evolutions starting from unstable states. In this paper a configuration with a poloidal magnetic field and a differential rotation, both symmetric about the same axis, is considered. This configuration is stable only for sufficiently small Hartmann numbers but evolves, if disturbed, in the case of larger Hartmann numbers toward a non-axisymmetric state. In this case the well-known symmetrization effect of differential rotation in magnetic fields is destroyed. 相似文献
164.
165.
166.
Mean bulk densities of various samples of dry atmospheric aerosol particles sampled at different sites and during different seasons and weather situations range between 1.8 and more than 3 gm cm3. 相似文献
167.
Walter Riesen Heinz Gamsjäger Paul W. Schindler 《Geochimica et cosmochimica acta》1977,41(9):1193-1200
The carbonato and hydrogencarbonato complexes of Mg2+ were investigated at 25 and 50° in solutions of the constant ClO4? molality (3 M) consisting preponderantly of NaClO4. The experimental data could be explained assuming the following equilibria: Mg2+ + CO2B + H2O ag MgHCO+3 + H+, , Mg2+ + 2 CO2g + 2 H2Oag Mg(HCO3)02 ± 2 H+, , ?15.37 ± 0.39 (50°), Mg2+ + CO2g + H2Oag MgCO03 + 2 H+, ,?15.23 ± 0.02 (50°), with the assumption γMgCO30 = γMg(HCO3)02, ΔG0(I = 0) for the reaction MgCO03 + CO2g + H2O = Mg(HCO3)02 was estimated to be ?3.91 ± 0.86 and 0.6 ± 2.4 kJ/mol at 25 and 50°C, respectively. The abundance of carbonate linked Mg(II) species in fresh water systems is discussed. 相似文献
168.
Studies on the thermoluminescence depth profile produced by 600-MeV protons in artificial lunar soil
The thermoluminescence (TL) of various plagioclase feldspars embedded in a thick target of 150 kg of artificial lunar soil was measured after a 600-MeV proton irradiation. No correlation was observed between the parameters of the characteristic feldspar glow peak and the anorthite contents. The relative TL sensitivities of the individual plagioclase variants were measured and found to be practically the same for60Co-γ- and 600-MeV proton-irradiated samples.The TL intensity distribution within the target arrangement, converted to a 2π isotropic p-influx, resulted in an approximate TL depth profile of a thermally undisturbed lunar soil bomarded by galactic cosmic protons. The undisturbed TL intensity at a depth of 28 g/cm2 (? 17 cm) decreased to 39% at a depth of 106 g/cm2 (? 60 cm). For the evaluation of the temperature gradients by TL in lunar samples the experimental data at the sites of Taurus-Littrow and of Hadley-Rille yielded minimum depth intervals for sampling of ~ 20 cm and ~ 40 cm respectively, presuming an error of ± 15% in the TL determination. Certain aspects are seen by using the relation TL intensity/22Na-activity ratio versus depth (thus representing the total ionization profile) to establish22Na depth profiles. 相似文献
169.
P. Eberhardt J. Geiss H. Graf N. Grögler U. Krähenbühl H. Schwaller A. Stettler 《Geochimica et cosmochimica acta》1974,38(1):97-120
The noble gases He, Ne, Ar, Kr and Xe and also K and Ba were measured in the Apollo 11 igneous rocks 10017 and 10071, and in an ilmenite and two feldspar concentrates separated from rock 10071. Whole rock K/Ar ages of rocks 10017 and 10071 are (2350 ± 60) × 106 yr and (2880 ± 60) × 106 yr, respectively. The two feldspar concentrates of rock 10071 have distinctly higher ages: (3260 ± 60) × 106 yr and (3350 ± 70) × 106 yr. These ages are still 10 per cent lower than the Rb/Sr age obtained by Papanastassiouet al. (1970) and some Ar40 diffusion loss must have occurred even in the relatively coarse-grained feldspar.The relative abundance patterns of spallation Ne, Ar, Kr and Xe are in agreement with the ratios predicted from meteoritic production rates. However, diffusion loss of spallation He3 is evident in the whole rock samples, and even more in the feldspar concentrates. The ilmenite shows little or no diffusion loss. The isotopic composition of spallation Kr and Xe is similar to the one observed in meteorites. Small, systematic differences in the spallation Kr spectra of rocks 10017 and 10071 are due to variations in the irradiation hardness (shielding). The Kr spallation spectra in the mineral concentrates are different from the whole rock spectra and also show individual variations, reflecting the differences in target element composition. The relative abundance of cosmic ray produced Xe131 differs by nearly 50 per cent in the two rocks. The other Xe isotopes show no variations of similar magnitude. The origin of the Xe131 yield variability is discussed.Kr81 was measured in all the samples investigated. The Kr81/Kr exposure ages of rocks 10017 and 10071 are (480 ± 25) × 106 yr and (350 ± 15) × 106 yr, respectively. Exposure ages derived from spallation Ne21, Ar38, Kr83 and Xe126 are essentially in agreement with the Kr81/Kr ages. The age of rock 10071 might be somewhat low because of a possible recent exposure of our sample to solar flare particles. 相似文献
170.
Anne Lähteenmäki Merja Tornikoski Talvikki Hovatta Esko Valtaoja 《Astrophysics and Space Science》2007,311(1-3):347-351
A wealth of information on the properties of jets in Active Galactic Nuclei (AGNs) can be derived from total flux density observations at high radio frequencies. This includes, for example, the Doppler factor, the Lorentz factor, and the viewing angle of the jet. We have earlier calculated these parameters for a sample of ~80 sources of different AGN types using almost 20 years of 22 and 37 GHz data from Metsähovi Radio Observatory. We have now gathered data for an additional ten years, and studied the long term characteristic variability time scales of a large sample of AGNs using the first order structure function, the discrete autocorrelation function and the Lomb-Scargle periodogram. Some of the results will be presented in this paper. We also stress the importance of long term observations of AGNs, the main reason for this being misinterpretations of source properties due to insufficient time coverage. Only a few observing epochs will too easily lead to incorrect conclusions about variability, continuum spectra, and the general detectability of the source, not to mention the exclusion of interesting objects from further studies. This is particularly important when considering, for example, the Planck satellite for which the quality of the main mission product, the accurate cosmic microwave background anisotropy maps, depends heavily on the elimination of foreground sources such as AGNs. 相似文献