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981.
Havvanur Kılıç Saadet Arzu Berilgen Perihan Biçer Mustafa Yildirim 《Marine Georesources & Geotechnology》2013,31(4):303-323
Istanbul, the largest city in Turkey and one of the major metropolitan areas in the world, cleaned one of its environmentally polluted areas—Golden Horn—by dredging 5 million m3 of the bottom sediments and pumping the resulting sludge to a storage area behind a dam built at an abandoned rock quarry site in Alibey district. The reclamation of the land that formed over the storage area of Golden Horn dredged material is socially and economically very desirable. In this paper, results from experimental studies that are focused on determining the shear strength behavior of the dredge material and undisturbed soil are presented. Slurry consolidometer test, large model tests and small model tests are used to consolidate the dredged soil samples from Halic to simulate the natural consolidation behavior of these soils. Shear strength parameters are determined by laboratory vane tests; unconfined compression tests; undrained-unconsolidated (UU) and consolidated-undrained (CU) triaxial tests on samples that are obtained through in situ undisturbed samples and laboratory model tank and slurry consolidation. Moreover, the effects of fly ash and lime additives on the undrained shear strength were determined by mixing the materials with the dredged clay from Golden Horn during the model experiments conducted in the laboratory. Based on these findings, equations are proposed that govern the relationships between undrained shear strength and water content value. 相似文献
982.
Zhaoyun Chen Xiao-Hai Yan Yuwu Jiang Lide Jiang Young-Heon Jo 《Journal of Oceanography》2013,69(4):443-450
Satellite images of sea surface temperature (SST) show that the location of cross-shore SST minimum (LCSM) stretches along the isobaths in the Northwest Africa Upwelling System. To understand and interpret these observations better, we set up a two-dimensional analytical model that takes into account the surface and bottom Ekman transport and the alongshore geostrophic current, as well as bottom friction and variations in bottom topography. The structure of vertical velocity with a realistic topography clearly illustrates the variations of SST drop in a sample cross-shore section. Some idealized theoretical model experiments are carried out to examine the effects of eddy viscosity, Coriolis force, and cross-shore wind on the location of the cross-shore maximum upwelling intensity. The results show that the cross-shore wind largely impacts on the location where the coldest water outcrops to the surface through an adjustment of the cross-shore pressure gradient. This is also verified by the remotely sensed data, which indicate that the maximum correlation coefficient between cross-shore wind stress and the depth of LCSM is ?0.65 with a lag of approximately 1 day. 相似文献
983.
Bouchet VM Debenay JP Sauriau PG Radford-Knoery J Soletchnik P 《Marine environmental research》2007,64(3):358-383
Sediment cores were collected from April to August 2004 on tidal mudflats of the macrotidal Marennes-Oléron Bay (SW France), famous for the cultivation of Pacific oysters (Crassostrea gigas). The response of living (stained) benthic foraminifera to short-term biogeochemical disturbances in the sediment and overlying water, which may be involved in oyster summer mortality, was monitored. Short-term hypoxia occurred in early June, in conjunction with a sudden rise in temperature. In mid-June, the ammonia content of sediment porewater increased, leading to potentially maximal flux towards overlying waters. Foraminiferal assemblages, particularly in the topmost layer, were altered. Ammonia tepida was the most tolerant to temperature increase and hypoxic conditions whereas Brizalina variabilis and Haynesina germanica were sensitive to organic degradation and hypoxia. Cribroelphidium gunteri was the most opportunistic during recolonisation. Benthic foraminifera showed that short-term biochemical changes in the sediment are toxic and may be involved in the summer mortality of Pacific oysters. 相似文献
984.
Gündüz Horasan Aysun Boztepe Güney Ayşegül Küsmezer Feyza Bekler Zafer Öğütçü Nebiye Musaoğlu 《Journal of Asian Earth Sciences》2009,34(1):90-99
Scientists have proposed two fault systems of different ages in the Sea of Marmara: the Thrace-Eski?ehir Fault Zone of Early Miocene–Early Pliocene age and the North Anatolian Fault Zone of Late Pliocene–Recent age. Different seismicity rates and extensions of these faults onto land near ?stanbul have been suggested. One of the reasons for these differences is the contamination of seismicity catalogs by seismic events from quarries operated in ?stanbul and its vicinity, including Gaziosmanpa?a (Cebeci and Kemerburgaz), Çatalca, Ömerli, Gebze, and Hereke.In this study, we investigated waveforms of 179 seismic events (1.8 < Md < 3.0) from the KOERI, NEMC digital database. We determined differences between earthquakes and quarry blasts based on time- and frequency-domain analyses of their seismograms (amplitude peak ratio, power ratio, and spectral amplitude ratio) and used these differences as discriminants. The results of this study indicate that 15% and 85% of the investigated seismic events are earthquakes and quarry blasts, respectively. 相似文献
985.
Bertrand Bessagnet Laurent Menut Gabriele Curci Alma Hodzic Bruno Guillaume Catherine Liousse Sophie Moukhtar Betty Pun Christian Seigneur Michaël Schulz 《Journal of Atmospheric Chemistry》2008,61(3):175-202
In this study, an improved and complete secondary organic aerosols (SOA) chemistry scheme was implemented in the CHIMERE model.
The implementation of isoprene chemistry for SOA significantly improves agreement between long series of simulated and observed
particulate matter concentrations. While simulated organic carbon concentrations are clearly improved at elevated sites by
adding the SOA scheme, time correlation are impaired at low level sites in Portugal, Italy and Slovakia. At several sites
a clear underestimation by the CHIMERE model is noticed in wintertime possibly due to missing wood burning emissions as shown
in previous modeling studies. In Europe, the CHIMERE model gives yearly average SOA concentrations ranging from 0.5 μg
m
− 3 in the Northern Europe to 4 μg
m
− 3 over forested regions in Spain, France, Germany and Italy. In addition, our work suggests that during the highest fire emission
periods, fires can be the dominant source of primary organic carbon over the Mediterranean Basin, but the SOA contribution
from fire emissions is low. Isoprene chemistry has a strong impact on SOA formation when using current available kinetic schemes. 相似文献
986.
Geomorphological heritage is a widely used term in European and North-American countries, but is still scarcely mentioned
in Africa. Nevertheless, the attractiveness of the African countries is often intimately connected to its breathtaking and
endless geological landscapes. Morocco is one of those countries that has the widest diversity in landscapes and landforms,
ranging from the Mediterranean and Atlantic coasts over the Rif, Middle Atlas, High Atlas and Anti-Atlas mountain chains to
the great rocky and sandy deserts in the South. A wide variety of geological units hosting different types of important economic
mineral deposits cover a temporal range from Late Precambrian to Quaternary. A detailed geomorphological study has been carried
out in the region of Ifrane and Azrou (Middle Atlas, Central Morocco) using a combination of high resolution satellite data
and direct field observations integrated by geological maps and scientific literature. In order to describe and evaluate the
geomorphological heritage of this area, 40 geomorphosites have been selected comprising springs, karst landforms (polje, dolines,
caves, sinkholes, stone forests, cryptokarstic dolines), carbonate depositional landforms (travertines and waterfalls), fluvial
landforms (meanders, canyons, palaeo-valleys, etc.), structural landforms (triangular facets, hogbacks, cuestas, residual
outcrops, etc.) and volcanic landforms (volcanoes, caldeira, pyroclastic cones, lava tube). The results of this research have
been summarised in a thematic map, representing the geomorphosites related to various landscape units. 相似文献
987.
The general subject of this paper is subglacial deformation beneath Breiðamerkurjökull, a surging Icelandic glacier. More specifically it discusses the evolution and the role of fluid pressure on the behaviour of subglacial sediments during deformation. During Little Ice Age maximum, the two outcrops studied, North Jökulsarlon (N-Jk) and Brennhola-Alda (BA), were located at 2550 m and 550 m respectively from the front of the Breiðamerkurjökull. Sedimentological analysis at the forefield of the glacier shows thick, coarse glaciofluvial deposits interbedded with thin, fine-grained shallow lacustrine/swamp deposits, overlain by a deformed till unit at N-Jk. BA outcrop shows fine-grained shallow lacustrine/swamp deposits overlain by a deformed till unit. The sequence of deformation events from one outcrop to the other is similar. First, major thrust planes, which were rooted in shallow lacustrine/swamp deposits developed by glacially induced simple shear. Next, the thrusts were folded, indicating the deformation of hydroplastic sediment assisted by moderate fluid pressure. Then clastic dyke swarms crosscut the sedimentary succession, proving that fluid overpressure caused hydrofracturing associated with fluidisation. Finally, as water escaped from the glacier bed, fluid pressure dropped, and normal faulting occurred in brittle-state subglacial sediments. Fluid-pressure variations are related to glacier dynamics. They control the deformation sequence by modifying subglacial rheological behaviour and the nature of the subglacial tectonism. 相似文献
988.
989.
We study the evolution of the longitudinal asymmetry in solar activity through the wave packet technique applied to the period
domain of 25 – 31 days (centered at the 27-day solar rotation period) for the sunspot number and geomagnetic aa index. We observe the occurrence of alternating smaller and larger amplitudes of the 11-year cycle, resulting in a 22-year
periodicity in the 27-day signal. The evolution of the 22-year cycle shows a change of regime around the year 1912 when the
22-year period disappears from the sunspot number series and appears in the aa index. Other changes, such as a change in the correlation between solar and geomagnetic activity, took place at the same
time. Splitting the 27-day frequency domain of aa index shows an 11-year cycle for higher frequencies and a pure22-year cycle for lower frequencies, which we attribute to
higher latitude coronal holes. This evidence is particularly clear after 1940, which is another benchmark in the evolution
of the aa index. We discuss briefly the mechanisms that could account for the observed features of the 22-year cycle evolution. 相似文献
990.
Non-degenerate stars of essentially all spectral classes are soft X-ray sources. Their X-ray spectra have been important in
constraining physical processes that heat plasma in stellar environments to temperatures exceeding one million degrees. Low-mass
stars on the cooler part of the main sequence and their pre-main sequence predecessors define the dominant stellar population
in the galaxy by number. Their X-ray spectra are reminiscent, in the broadest sense, of X-ray spectra from the solar corona.
The Sun itself as a typical example of a main-sequence cool star has been a pivotal testbed for physical models to be applied
to cool stars. X-ray emission from cool stars is indeed ascribed to magnetically trapped hot gas analogous to the solar coronal
plasma, although plasma parameters such as temperature, density, and element abundances vary widely. Coronal structure, its
thermal stratification and geometric extent can also be interpreted based on various spectral diagnostics. New features have
been identified in pre-main sequence stars; some of these may be related to accretion shocks on the stellar surface, fluorescence
on circumstellar disks due to X-ray irradiation, or shock heating in stellar outflows. Massive, hot stars clearly dominate
the interaction with the galactic interstellar medium: they are the main sources of ionizing radiation, mechanical energy
and chemical enrichment in galaxies. High-energy emission permits to probe some of the most important processes at work in
these stars, and put constraints on their most peculiar feature: the stellar wind. Medium and high- resolution spectroscopy
have shed new light on these objects as well. Here, we review recent advances in our understanding of cool and hot stars through
the study of X-ray spectra, in particular high-resolution spectra now available from XMM-Newton and Chandra. We address issues related to coronal structure, flares, the composition of coronal plasma, X-ray production in accretion
streams and outflows, X-rays from single OB-type stars, massive binaries, magnetic hot objects and evolved WR stars. 相似文献