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31.
Pedro Martínez-Santos Pedro E. Martínez-Alfaro Eugenio Sanz Angel Galindo 《Hydrogeology Journal》2010,18(6):1525-1537
Evaluating aquifer–river interactions is naturally complex, particularly within urban settings. This is largely due to the difficulties involved in quantifying most elements of the water balance. The ability of numerical models to deal with several dynamic variables simultaneously makes them valuable tools to address this kind of problem. An applied, modeling-based approach to investigate the spatial and temporal variations of aquifer–river connectivity within a shallow urban aquifer is presented. Model development is based on comprehensive field campaigns in Langreo, Spain. Two calibration runs (for summer and winter conditions) were carried out in order to evaluate the spatial distribution of recharge rates. The model suggests that baseflows are largely negligible in comparison with total streamflows. This is mostly attributed to the abrupt nature of the catchment, which prevents the existence of sufficiently large alluvial systems to a great extent. Modelling results also show that aquifer–river connectivity at the study site is constrained by urban pumping as well as by seasonal fluctuations. 相似文献
32.
Near‐source pulse‐like records resulting from rupture's directivity have been found to depart from so‐called ordinary ground motions in terms of both elastic and inelastic structural seismic demands. In fact, response spectra may be strong if compared with what is expected from common ground motion prediction equations. Moreover, because not all spectral ordinates are affected uniformly, a peculiar spectral shape, with an especially amplified region depending on the pulse period, may follow. Consequently, inelastic seismic demand may show trends different to records not identified as pulse‐like (i.e., ordinary). This latter aspect is addressed in the study reported in this short communication, where a relatively large dataset of identified impulsive near‐source records is used to derive an analytical‐form relationship for the inelastic displacement ratio. It is found that, similar to what was proposed in literature for soft soil sites, a double‐opposite‐bumps form is required to match the empirical data as a function of the structural period over the pulse period ratio. The relationship builds consistently on previous studies on the topic, yet displays different shape with respect to the most common equations for static structural assessment procedures. Copyright © 2012 John Wiley & Sons, Ltd. 相似文献
33.
Herrera Antonio M. Suhandri Hendy F. Realini Eugenio Reguzzoni Mirko de Lacy M. Clara 《GPS Solutions》2016,20(3):595-603
GPS Solutions - goGPS is a positioning software application designed to process single-frequency code and phase observations for absolute or relative positioning. Published under a free and... 相似文献
34.
Roberto Ventura Santos Carlos Eduardo Ganade Christian M. Lacasse Iago S. L. Costa Ivo Pessanha Eugenio P. Frazo Elton L. Dantas Jos A. Cavalcante 《地学学报》2019,31(5):424-429
Crystalline continental rocks and associated crust‐contaminated basaltic rocks were unexpectedly dredged on the crest and at seamounts of the Rio Grande Rise, South Atlantic. Zircon U–Pb ages of one gabbro (ca. 2,200 Ma) and four granitoids (between ca. 1,430–480 Ma) indicate that the breakup of SW Gondwana left behind continental fragments of dominantly African age. These rocks may have been incorporated into the oceanic lithosphere by complex processes including rifting and interaction of the Tristan‐Gough mantle plume with hyperextended continental margins. Until ca. 80–70 Ma, the Rio Grande Rise and an old portion of the Walvis Ridge formed a conjugate pair of aseismic ridges, and the Tristan‐Gough plume was positioned at the Mid‐Atlantic Ridge. The finding of continental rock fragments in one of these conjugate pairs opens new perspectives on the mechanisms of continental break‐up, the nature of this conjugate pair, and the geodynamic evolution of rifted Gondwana margins in the South Atlantic. 相似文献
35.
This paper describes the research carried out in a karst aquifer located in Soria, Spain. The system presents considerable
good-quality water resources, yielding a series of springs which constitute a “Natural Monument”. An integral study of the
hydrological cycle is presented in order to characterize the hydrodynamic behavior of the aquifer. Research combines conventional
geological and hydrogeological approaches with more innovative techniques such as speleo-diving. On the basis of relatively
little available data, quantitative results are obtained. These include estimations on porosity, hydraulic conductivity, transmissivity,
and groundwater renewal rate and aquifer reserves. A vulnerability assessment is carried out to evaluate the potential effects
of overpumping. This is followed by a proposal for sustainable aquifer management. Since aquifers such as the one in this
study are frequently found, this methodology could be successfully extrapolated to other cases. 相似文献
36.
Carmelo Ferlito Marco Viccaro Eugenio Nicotra Renato Cristofolini 《Bulletin of Volcanology》2012,74(2):533-543
Mount Etna volcano (Italy) during the period 2001–2005 has undergone a period of intense eruptive activity marked by three
large eruptions (2001, 2002–2003 and 2004–2005). These eruptions encompassed diverse eruptive styles and regimes: from intensely
explosive, during 2001 and 2002–2003 eruptions, to exclusively effusive in the 2004–2005 event. In this work, we put forward
the idea that these three eruptions are the response of the progressive arrival into the uppermost segment of the open-conduit
system of a new magma, which was geochemically distinct in terms of trace element and Sr–Nd–Pb isotope signature from the
products previously emitted by the Etnean volcano. The magma migrated upwards mainly through a peripheral tectonic system,
which can be considered as eccentric in spite of its relative proximity to the main system. The ingress of the new magma and
its gradual displacement from the eccentric system into the uppermost sector of the open-conduit gave rise to different eruptive
behaviours. At the beginning, the ascent of the undegassed magma, able to exsolve a gas phase at depth, and its interaction
with closed-system magma reservoirs less than 10 km deep gave rise to the explosive events of 2001 and 2002–2003. Later, when
the same magma entered into the open-conduit system, it took part in the steady-state degassing and partially lost its volatile
load, leading to a totally effusive eruption during the 2004–2005 event. One further consideration highlighted here is that
in 2001–2005, migration of the feeding axis from an eccentric and peripheral position towards the main open-conduit has led
to the development of a new vent (South East Crater 2) located at the eastern base of the South East Crater through which
most of the subsequent Etnean activity occurred. 相似文献
37.
38.
The use of nonlinear static procedures for performance‐based seismic design (PBSD) and assessment is a well‐established practice, which has found its way into modern codes for quite some time. On the other hand, near‐source (NS) ground motions are receiving increasing attention, because they can carry seismic demand systematically different and larger than that of the so‐called ordinary records. This is due to phenomena such as rupture forward directivity (FD), which can lead to distinct pulses appearing in the velocity time‐history of the ground motion. The framework necessary for taking FD into account in probabilistic seismic hazard analysis (PSHA) has recently been established. The objective of the present study is to discuss the extension of nonlinear static procedures, specifically the displacement coefficient method (DCM), with respect to the inelastic demand associated with FD. In this context, a methodology is presented for the implementation of the DCM toward estimating NS seismic demand, by making use of the results of NS‐PSHA and a semi‐empirical equation for NS‐FD inelastic displacement ratio. An illustrative application of the DCM, with explicit inclusion of NS‐pulse‐like effects, is given for a set of typical plane R/C frames designed under Eurocode provisions. Different scenarios are considered in the application and nonlinear dynamic analysis results are obtained and discussed with respect to the static procedure estimates. Conclusions drawn from the results may help to assess the importance of incorporating NS effects in PBSD. Copyright © 2014 John Wiley & Sons, Ltd. 相似文献
39.
This paper describes a modal weighting technique that improves the stability characteristics of explicit time-integration schemes used in structural dynamics. The central difference method was chosen as the trial algorithm because of its simplicity, both in terms of formulation and ease of numerical stability and convergence analysis. It is shown how explicit algorithms may be reformulated in order to make them stable for any integration time by attenuating high-frequency oscillation modes that are generated by mesh geometry rather than generic dynamical features. We discuss results from trial calculations obtained from mathematical models that represent hysteretic restoring force elements and an application on a physical, four-degree-of-freedom, base-isolated structure using the pseudodynamic technique. © 1998 John Wiley & Sons, Ltd. 相似文献
40.
Gaseous nitric acid and ammonia were sampled with annular denuders at a forest savannah site from April to December 1987. The analysis of the extract was made spectrophotometrically and by a selective electrode for NO3
– and NH4
+, respectively. Higher concentrations were observed during the vegetation burning period at the end of the dry season. In the studied savannah area, large soil emissions of NO occur during the rainy season, although very low concentrations of HNO3 (0.035 ppb) and also of particulate NO3
– (0.43 g m-3) were observed; it is likely that NOx are lost by fast vertical transport to the upper troposphere. During the nonburning period, the average concentration of NH3 was 2.7 ppb, which is much lower than values given in the literature for the tropical America atmosphere. The concentrations of HNO3 and NH3 were always below the values needed to produce ammonium nitrate aerosols. 相似文献