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841.
An experimental study of temperature cycles and the heat budget in the Duplin River, a tidal creek bordered by extensive intertidal salt marshes, was carried out in late summer of 2003 and spring of 2004 near Sapelo Island on the central Georgia coast in the southeastern US. Three water masses are identified with differing temperature and salinity regimes, the characteristics of which are dictated by channel morphology, tidal communication with the neighboring sound, ground water hydrology, the extent of local intertidal salt marshes and side channels and the spring–neap tidal cycle (which controls both energetic mixing and, presumably, ground water input). For the first experiment, heat budgets are constructed for the upper (warmer) and lower (cooler) areas of the Duplin River showing the diminishing importance of tidal advection away from the mouth of the creek along with the concomitant increase in the importance of both direct atmospheric fluxes and of interactions with the marsh and side creeks. The second experiment, in the spring of 2004, reexamines the heat budget on seasonal and daily averaged scales revealing the decreased importance of advective fluxes relative to direct atmospheric fluxes on this scale but the constant importance of marsh/creek interactions regardless of time scale or season. Short period temperature fluctuations which affect larval development are examined and analogies are drawn to use heat to understand the marsh as a source of sediment, carbon and other nutrients. 相似文献
842.
843.
Fatigue reliability analysis of deep water rigid marine risers associated with Morison-type wave loading 总被引:1,自引:0,他引:1
Muddassir Nazir Faisal Khan Paul Amyotte 《Stochastic Environmental Research and Risk Assessment (SERRA)》2008,22(3):379-390
This work presents a simple and efficient framework for the fatigue reliability assessment of a vertical top-tensioned rigid
riser. The fatigue damage response is considered as a narrow-band Gaussian stationary random process with a zero mean for
the short-term behavior of a riser. Non-linearity in a response associated with Morison-type wave loading is accounted for
by using a factor, which is the ratio of expected damage according to a non-linear probability distribution to the expected
damage according to a linear method of analysis. Long-term non-stationary response is obtained by summing up a large number
of short-term stationary responses. Uncertainties associated with both the strength and stress parts of the limit state function
are quantified by a lognormal distribution. A closed form reliability analysis is carried out, which is based on the limit
state function formulated in terms of Miner’s cumulative damage rule. The results thus obtained are compared with the well-documented
lognormal format of reliability analysis based on time to fatigue failure. The validity of using the lognormal hazard rate
function in predicting the fatigue life is discussed. A Monte Carlo simulation technique is also used as a reliability assessment
method. A simple algorithm is used to reduce the uncertainty associated with direct sampling at small probability of failure
values and a small number of simulations. Simulation results are compared with closed form solutions. A worked example is
included to show the practical riser design problem based on reliability analysis. 相似文献
844.
Sarah F. Trainor Monika Calef David Natcher F. Stuart Chapin III A. David McGuire Orville Huntington Paul Duffy T. Scott Rupp La'Ona DeWilde Mary Kwart Nancy Fresco & Amy Lauren Lovecraft 《Polar research》2009,28(1):100-118
This paper explores whether fundamental differences exist between urban and rural vulnerability to climate-induced changes in the fire regime of interior Alaska. We further examine how communities and fire managers have responded to these changes and what additional adaptations could be put in place. We engage a variety of social science methods, including demographic analysis, semi-structured interviews, surveys, workshops and observations of public meetings. This work is part of an interdisciplinary study of feedback and interactions between climate, vegetation, fire and human components of the Boreal forest social–ecological system of interior Alaska. We have learned that although urban and rural communities in interior Alaska face similar increased exposure to wildfire as a result of climate change, important differences exist in their sensitivity to these biophysical, climate-induced changes. In particular, reliance on wild foods, delayed suppression response, financial resources and institutional connections vary between urban and rural communities. These differences depend largely on social, economic and institutional factors, and are not necessarily related to biophysical climate impacts per se. Fire management and suppression action motivated by political, economic or other pressures can serve as unintentional or indirect adaptation to climate change. However, this indirect response alone may not sufficiently reduce vulnerability to a changing fire regime. More deliberate and strategic responses may be required, given the magnitude of the expected climate change and the likelihood of an intensification of the fire regime in interior Alaska. 相似文献
845.
Nathalie Vigouroux A. E. Williams-Jones Paul Wallace Thomas Staudacher 《Bulletin of Volcanology》2009,71(9):1077-1089
The November 2002 eruption of Piton de la Fournaise in the Indian Ocean was typical of the activity of the volcano from 1999
to 2006 in terms of duration and volume of magma ejected. The first magma erupted was a basaltic liquid with a small proportion
of olivine phenocrysts (Fo81) that contain small numbers of melt inclusions. In subsequent flows, olivine crystals were more abundant and richer in Mg
(Fo83–84). These crystals contain numerous melt and fluid inclusions, healed fractures, and dislocation features such as kink bands.
The major element composition of melt inclusions in this later olivine (Fo83–84) is out of equilibrium with that of its host as a result of extensive post-entrapment crystallization and Fe2+ loss by diffusion during cooling. Melt inclusions in Fo81 olivine are also chemically out of equilibrium with their hosts but to a lesser degree. Using olivine–melt geothermometry,
we determined that melt inclusions in Fo81 olivine were trapped at lower temperature (1,182 ± 1°C) than inclusions in Fo83–84 olivine (1,199–1,227°C). This methodology was also used to estimate eruption temperatures. The November 2002 melt inclusion
compositions suggest that they were at temperatures between 1,070°C and 1,133°C immediately before eruption and quenching.
This relatively wide temperature range may reflect the fact that most of the melt inclusions were from olivine in lava samples
and therefore likely underwent minor but variable amounts of post-eruptive crystallization and Fe2+ loss by diffusion due to their relatively slow cooling on the surface. In contrast, melt inclusions in tephra samples from
past major eruptions yielded a narrower range of higher eruption temperatures (1,163–1,181°C). The melt inclusion data presented
here and in earlier publications are consistent with a model of magma recharge from depth during major eruptions, followed
by storage, cooling, and crystallization at shallow levels prior to expulsion during events similar in magnitude to the relatively
small November 2002 eruption. 相似文献
846.
Kimberly Novick Ram Oren Paul Stoy Jehn-Yih Juang Mario Siqueira Gabriel Katul 《Advances in water resources》2009
Terrestrial ecosystems are dominated by vascular plants that form a mosaic of hydraulic conduits to water movement from the soil to the atmosphere. Together with canopy leaf area, canopy stomatal conductance regulates plant water use and thereby photosynthesis and growth. Although stomatal conductance is coordinated with plant hydraulic conductance, governing relationships across species has not yet been formulated at a practical level that can be employed in large-scale models. Here, combinations of published conductance measurements obtained with several methodologies across boreal to tropical climates were used to explore relationships between canopy conductance rates and hydraulic constraints. A parsimonious hydraulic model requiring sapwood-to-leaf area ratio and canopy height generated acceptable agreement with measurements across a range of biomes (r2=0.75). The results suggest that, at long time scales, the functional convergence among ecosystems in the relationship between water-use and hydraulic architecture eclipses inter-specific variation in physiology and anatomy of the transport system. Prognostic applicability of this model requires independent knowledge of sapwood-to-leaf area. In this study, we did not find a strong relationship between sapwood-to-leaf area and physical or climatic variables that are readily determinable at coarse scales, though the results suggest that climate may have a mediating influence on the relationship between sapwood-to-leaf area and height. Within temperate forests, canopy height alone explained a large amount of the variance in reference canopy conductance (r2=0.68) and this relationship may be more immediately applicable in the terrestrial ecosystem models. 相似文献
847.
Real-time seismology for the 05/12/2008 Wenchuan earthquake of China: A retrospective view 总被引:2,自引:0,他引:2
Paul SOMMERVILLE 《中国科学D辑(英文版)》2009,52(2):155-165
The devastating 05/12/2008 Wenchuan earthquake (Mw7.9) in Sichuan Province of China showed very few precursory phenomena and occurred on a fault system once assigned to be
of moderate long term seismic risk. Given the existing coverage of seismograph stations in Sichuan Province, real-time seismology
could have been effective in avoiding some earthquake damage and helping post-earthquake emergency response. In a retrospective
view, we demonstrated that the epicenter can be located with 20 km accuracy using just two broadband stations with three-component,
which takes only about 10 s after the onset of the earthquake. Initial magnitude is estimated to be M7 with the Tc measurement
over first 4 seconds of P waves. Better magnitude estimate can be obtained within 2 min by modeling Pnl waves for stations
about 500 km away where the S waveforms are clipped. The rupture area is well revealed by teleseismically-recorded >M5 early
aftershocks within two hours after the mainshock. Within a few hours, teleseismic body waves were inverted to derive a more
detailed rupture process and the finite fault model can be readily used to calculate ground motions, thus providing vital
information for rescue efforts in the case where no real-time strong motion records are available.
Supported by the Knowledge Innovation Program of the Chinese Academy of Sciences (Grant No. KZCX2-YW-116-1) and National Key
Technology Research and Development Program of China (Grant No. 2006BAC03B00) 相似文献
848.
Nitrogen uptake and denitrification in restored and unrestored streams in urban Maryland, USA 总被引:2,自引:0,他引:2
Carolyn A. Klocker Sujay S. Kaushal Peter M. Groffman Paul M. Mayer Raymond P. Morgan 《Aquatic Sciences - Research Across Boundaries》2009,71(4):411-424
There is growing interest in rates of nitrate uptake and denitrification in restored streams to better understand the effects
of restoration on nitrogen processing. This study quantified nitrate uptake in two restored and two unrestored streams in
Baltimore, Maryland, USA using nitrate additions, denitrification enzyme assays, and a 15N isotope tracer addition in one of the urban restored streams, Minebank Run. Restoration included either incorporation of
stormwater ponds below a storm drain and catch basins to attenuate flow or hydrologic “reconnection” of a stream channel to
its floodplain. Stream restoration was conducted for restoring aging sanitary and bridge infrastructure and introducing some
stormwater management in watersheds developed prior to current regulations. Denitrification potential in sediments was variable
across streams, whereas nitrate uptake length appeared to be significantly correlated to surface water velocity, which was
low in the restored streams during summer baseflow conditions. Uptake length of NO3
−–N in Minebank Run estimated by 15N tracer addition was 556 m. Whole stream denitrification rates in Minebank Run were 153 mg NO3
−–N m−2 day−1, and approximately 40% of the daily load of nitrate was estimated to be removed via denitrification over a distance of 220.5 m
in a stream reach designed to be hydrologically “connected” to its floodplain. Increased hydrologic residence time in Minebank
Run during baseflow likely influenced rates of whole stream denitrification, suggesting that hydrologic residence time may
be a key factor influencing N uptake and denitrification. Restoration approaches that increase hydrologic “connectivity” with
hyporheic sediments and increase hydrologic residence time may be useful for stimulating denitrification. More work is necessary,
however, to examine changes in denitrification rates in restored streams across different seasons, variable N loads, and in
response to the “flashy” hydrologic flow conditions during storms common in urban streams. 相似文献
849.
850.
Hong Luo Paul Dahlen Paul C. Johnson Tom Peargin Todd Creamer 《Ground Water Monitoring & Remediation》2009,29(1):81-91
Data requirements for assessing the significance of the soil vapor intrusion pathway are evolving, and the collection and interpretation of subslab and near-slab soil-gas samples are under discussion. The potential for different assessment paradigms for aerobically biodegradable and recalcitrant chemicals is also frequently debated. In this work, the soil-gas distribution beneath and around a slab-on-grade building overlying shallow (0.5 to >1.5 m below ground surface) petroleum hydrocarbon–impacted coarse alluvial soils was studied. The study spanned about 12 months, including the sampling of soil-gas hydrocarbon and oxygen concentrations, subslab soil vs. building pressure differentials and included weather conditions. Three-dimensional soil-gas concentration "snapshots" using samples from 79 soil-gas sampling points are presented here. Significant spatial variability was observed with hydrocarbon and oxygen concentrations ranging from about <0.01 to 200 mg/L and 0 to 21% v/v, respectively. The presence of oxygen and the depth to petroleum-impacted soils appeared to be the dominant factors in controlling the soil-gas distribution; the depletion of hydrocarbons over short lateral and vertical distances (<2 m) was observed in the well-oxygenated regions. Composition data suggest preferential biodegradation of lighter compounds at some points, as reflected in the ratio of the masses of chemicals eluting on the gas chromatography between methane and pentane (C1 and C5) and all others after pentane (>C5). 相似文献