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991.
992.
993.
Víctor Leiva Antonio Sanhueza José M. Angulo 《Stochastic Environmental Research and Risk Assessment (SERRA)》2009,23(3):299-307
In this article, we develop a new model based on the Birnbaum-Saunders distribution that results to be both useful and practical
for environmental sciences. The density, distribution and hazard functions, moments and properties of this new model are presented.
A graphical analysis of the density is also provided. Furthermore, we estimate parameters, propose asymptotic inference and
discuss influence diagnostics by using likelihood methods for the new distribution. An illustrative example with real data
related to water quality indicates the adequacy on the new distribution. 相似文献
994.
Shear effects on hollow section piers under seismic actions: experimental and numerical analysis 总被引:1,自引:0,他引:1
Raimundo Delgado Pedro Delgado Nelson Vila Pouca António Arêde Patrício Rocha Aníbal Costa 《Bulletin of Earthquake Engineering》2009,7(2):377-389
Shear effects are often a very important issue on the seismic behaviour of piers, particularly for hollow section bridge piers.
In fact, for this type of piers the cyclic response is similar to that of a structural wall in which both the transverse reinforcement
ratio and the detailing can play an important role on its performance, even likely to be determinant in terms of the failure
mechanism. On the other hand, codes and design guidelines are usually very conservative concerning shear capacity in order
to avoid any shear failure mechanism likely to trigger well known catastrophic consequences. Therefore, research studies on
this topic are still needed for a better understanding of pier cyclic shear response and also for improvement of the performance
under seismic actions. Pursuing this general objective, this paper partially reports on an experimental/numerical campaign
carried out on 1:4 reduced scale bridge piers in order to highlight and investigate shear-type problems. Within the scope
of this paper, two specimens types were selected having equal rectangular hollow section (900 × 450 mm2, 75 mm thick) but different transverse reinforcement detailing, namely one with a single stirrup per wall (representative
of typical bridge construction without seismic design requirements) and another with multiple stirrups, according to Eurocode
8 provisions. Numerical simulations of the experimental results were also conducted aiming at contributing for complete and
consistent interpretations of experimental results. Detailed modelling was performed allowing for realistic simulations of
the non linear behaviour, particularly suitable when a significant shear component is involved. Therefore, the numerical strategy
was based on a detailed 3D FEM discretization using a two-scalar variable damage model for the concrete constitutive law and
a suitable cyclic behaviour law for steel bars represented by truss elements. Results have shown that shear deformation and
failure modes are well simulated, while providing detailed insight concerning concrete damage pattern and distribution of
yielding on the transverse and longitudinal reinforcement. 相似文献
995.
Study of Metal Distribution in Raw and Screened Swine Manure 总被引:1,自引:0,他引:1
Ricardo Luís Radis Steinmetz Airton Kunz Valderi Luiz Dressler Érico Marlon de Moraes Flores Ayrton Figueiredo Martins 《洁净——土壤、空气、水》2009,37(3):239-244
The growth of industrial swine production over the last few years has led to a growth in concern over effluents generated by the activity. Several elements, mainly toxic metals, can be present in swine wastewater and can have a serious environmental impact. It is important, therefore, to know the metal concentration before the discharge of wastewater. In this work the temporal metal distribution in swine manure and its potential reduction using coarse (2 mm) and fine (<0.45 μm) liquid‐solid separation techniques were investigated. In order to do this, different swine manure sample preparation methods for Al, Ba, Cd, Co, Cr, Cu, Fe, Mg, Mn, Ni, Pb, Sr and Zn determination by Inductively Coupled Plasma Optical Emission Spectrometry (ICP OES) were tested. The acid mixtures used to digest the manure sample significantly affected the metal recovery. Good analyte recoveries were observed with nitric acid/hydrogen peroxide mixtures or nitric acid/perchloric acid mixtures. Sulfuric acid/hydrogen peroxide mixtures produced inconsistent results and poor recoveries, mainly for Ba and Pb. It was observed that metal concentrations in swine manure varied greatly with time, up to one order of magnitude, due to changes in swine production such as feed and animal numbers. Metals concentrations observed in the raw wastewater exceeded Brazilian limits for discharge into water bodies and recommendations for agricultural use. Results obtained from the liquid‐solid separation study showed that metals in the raw swine manure were not removed with coarse screening. However, the major fraction of metals were removed by filtration (0.45 μm), with the exception of Na, K and Sr. Thus, the use of liquid‐solid separation techniques that capture the fine solid fractions (and associated metals) from raw manure can have a favorable impact on the environment and contribute to swine production wastewater treatment. 相似文献
996.
The simplified hydraulic two-layer model for a katabatic flow is analysed using the outputs from a high-resolution mesoscale
simulation. A stably stratified night is simulated for the Duero basin, a complex terrain area located in the northern Spanish
plateau, with large vertical and horizontal spatial resolution. Well-defined katabatic flows on the basin slopes are generated
by the simulation, that are relatively stationary and quasi-bidimensional for some areas in the central part of the night.
The bulk quantities used in the two-layer approach as well as the different terms in the equations are computed from the three-dimensional
information provided by the mesoscale simulation. This method allows to inspect how well the simplified approach represents
the katabatic flow generated by the mesoscale model. The study shows that the hydraulic model allows for a comprehensive analysis
of the basic mechanisms of the slope flows but is not able to close the budget equations, since the residuals are large. 相似文献
997.
998.
999.
Maria Teresa Gómez-Pugnaire Peter Ulmer Vicente López-Sánchez-Vizcaíno 《Contributions to Mineralogy and Petrology》2000,139(4):436-457
Mafic igneous rocks are widespread in the Nevado-Filábride Complex, the lowermost metamorphic unit of the internal zones
of the Betic Cordilleras. They form intrusive, small, discontinuous bodies, predominantly dikes with subordinate small lava
flows. The entire complex underwent alpine compressional metamorphism during the Paleogene continental collision, resulting
in eclogites and blueschists in the mafic bodies and high-pressure assemblages in the intruded metasediments. Locally, weakly
metamorphosed or completely unmetamorphosed igneous rocks with the same textural features occur as patches surrounded by eclogitized
igneous rocks. The bulk rock chemistry of unmetamorphosed and completely metamorphosed mafic igneous rocks is consistent with
an alkaline to transitional tholeiitic magmatism with typical within-plate geochemical characteristics. All but a few samples
are nepheline normative and display REE and trace element characteristics typical of continental, rift-related magmatism.
This conclusion is strongly supported by the mineral chemistry of the major constituents, in particular the calcic Ti-rich
character of clinopyroxene, the lack of orthopyroxene, and the occurrence of kaersutitic amphibole. Incompatible trace element
abundances and Sr and Nd isotopes support the provenance of these magmas from a variably metasomatized previously depleted
sub-continental lithospheric mantle source.
Received: 5 July 1999 / Accepted: 28 February 2000 相似文献
1000.
The CO2-rich thermal groundwater in the Betic Cordilleras in Spain has been studied with regard to the geological and hydrogeological
setting, physical and chemical characteristics, and 13C-isotope content. The study area is about 60 km northeast of Almería city, in southeastern Spain. The thermomineral waters
are plentiful and are related to regional geothermal anomalies. Temperatures of 20 −41°C, high bicarbonate concentrations
(183–1824 mg/L), and high amounts of PCO2 (<1.1 bar) characterize the groundwater. CO2 spatial variations are related to proximity to the Carboneras, Palomares, and Guadalentín fault systems, which may be the
surface representation of the zone of crustal thinning and magmatism. δ
13C values probably indicate a deep source for the CO2, either the mantle or perhaps carbonate rocks in the metamorphic substratum. The high amount of CO2 in the groundwater causes problems in wells and severely restricts water usage. The hydrothermal features of this area are
probably related to neotectonic activity.
Received, September 1998/Revised, June 1999, September 1999/Accepted, December 1999 相似文献