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81.
Strong benthic–pelagic coupling is an important characteristic of shallow coastal marine ecosystems. Building upon a rich
history of benthic metabolism data, we measured oxygen uptake and nutrient fluxes across the sediment–water interface along
a gradient of water column primary production in Narragansett Bay, RI (USA). Despite the strong gradients seen in water column
production, sediment oxygen demand (SOD) and benthic nutrient fluxes did not exhibit a clear spatial pattern. Some of our
sites had been studied in the 1970s and 1980s and thus allowed historical comparison. At these sites, we found that SOD and
benthic fluxes have not changed uniformly throughout Narragansett Bay. In the uppermost portion of the bay, the Providence
River Estuary, we observed a significant decrease in dissolved inorganic phosphorus fluxes which we attribute to management
interventions. At another upper bay site, we observed significant declines in SOD and dissolved inorganic nitrogen fluxes
which may be linked to climate-induced decreases in water column primary production and shifts in bloom phenology. In the
1970s, benthic nutrient regeneration supplied 50% to over 200% of the N and P needed to support primary production by phytoplankton.
Summer nutrient regeneration in the Providence River Estuary and Upper bay now may only supply some 5–30% of the N and 3–20%
of the P phytoplankton demand. 相似文献
82.
Light extinction by atmospheric particles is strongly dependent on their chemical composition and water content. Since light extinction directly impacts climate, optical measurements of atmospherically relevant aerosols at varying relative humidities (RH) are needed. Recent studies have highlighted the possibility that some atmospheric aerosols are glassy under ambient conditions. Here, the particle optical growth factor, fRHext, was measured for liquid and glassy particles using cavity ring-down aerosol extinction spectroscopy. The particles were composed of ammonium sulfate (AS), 1,2,6-hexanetriol, sucrose, raffinose, and mixed particles containing AS and either sucrose or raffinose. Both sucrose and raffinose can be glassy at room temperature. For the pure organics, the highly viscous sucrose and raffinose particles have similar optical growth curves to the liquid 1,2,6 hexanetriol particles. However, for particles composed of sucrose or raffinose mixed with AS, optical growth depends on the AS weight-percent, which in turn controls the phase state of the AS and ultimately the water uptake. 相似文献
83.
Georgina E. King David C. W. Sanderson Ruth A. J. Robinson Adrian A. Finch 《Boreas: An International Journal of Quaternary Research》2014,43(4):955-972
Analysis of a high‐resolution suite of modern glacial sediments from Jostedalen, southern Norway, using a portable optically stimulated luminescence (OSL) reader, provides insights into the processes of sediment bleaching in glacial environments at the catchment scale. High‐magnitude, low‐frequency processes result in the least effective sediment bleaching, whereas low‐magnitude, high‐frequency events provide greater bleaching opportunities. Changes in sediment bleaching can also be identified at the scale of individual bar features: tails of braid‐bars and side‐attached bar deposits have the lowest portable reader signal intensities, as well as the smallest conventional OSL residual doses. In addition to improving our understanding of the processes of sediment bleaching, portable reader investigations can also facilitate more rapid and comprehensive modern analogue investigations, which are commonly used to confirm that the OSL signals of modern glacial sediments are well bleached. 相似文献
84.
Lane D.M. Davies J.B.C. Robinson G. O'Brien D.J. Sneddon J. Seaton E. Elfstrom A. 《Oceanic Engineering, IEEE Journal of》1999,24(1):96-111
This paper describes the mechanical design, finger modeling, and sensor signal processing for a dextrous subsea robot hand incorporating force and slip contact sensing. The hand uses a fluid-filled tentacle for each finger, which has inherent passive compliance, and no moving parts. Force sensing uses strain gauges mounted in the fingertip, potted within a silicon elastomer. Slip sensing uses a piezoelectric strip to detect vibration, embedded 1 mm below the elastomer surface. Static models of finger motion are presented and validated based on bending moments and hydraulic pressure. The design of a stochastic estimator is also described for sensor fusion of contact force magnitude and direction data, obtained using redundant strain gauges in the fingertip. Finally, linear dynamic models of the finger dynamics in contact with a rigid surface are obtained using least squares and recursive least squares parameter estimation, as a precursor to closed-loop force control during grasping 相似文献
85.
Eric Robinson 《Geology Today》1999,15(3):110-113
Before the Roman came to Rye or out to Severn strode,
The rolling English drunkard made the rolling English road. 相似文献
The rolling English drunkard made the rolling English road. 相似文献
86.
87.
D. A. Robinson A. Binley N. Crook F. D. Day‐Lewis T. P. A. Ferré V. J. S. Grauch R. Knight M. Knoll V. Lakshmi R. Miller J. Nyquist L. Pellerin K. Singha L. Slater 《水文研究》2008,22(18):3604-3635
We want to develop a dialogue between geophysicists and hydrologists interested in synergistically advancing process based watershed research. We identify recent advances in geophysical instrumentation, and provide a vision for the use of electrical and magnetic geophysical instrumentation in watershed scale hydrology. The focus of the paper is to identify instrumentation that could significantly advance this vision for geophysics and hydrology during the next 3–5 years. We acknowledge that this is one of a number of possible ways forward and seek only to offer a relatively narrow and achievable vision. The vision focuses on the measurement of geological structure and identification of flow paths using electrical and magnetic methods. The paper identifies instruments, provides examples of their use, and describes how synergy between measurement and modelling could be achieved. Of specific interest are the airborne systems that can cover large areas and are appropriate for watershed studies. Although airborne geophysics has been around for some time, only in the last few years have systems designed exclusively for hydrological applications begun to emerge. These systems, such as airborne electromagnetic (EM) and transient electromagnetic (TEM), could revolutionize hydrogeological interpretations. Our vision centers on developing nested and cross scale electrical and magnetic measurements that can be used to construct a three‐dimensional (3D) electrical or magnetic model of the subsurface in watersheds. The methodological framework assumes a ‘top down’ approach using airborne methods to identify the large scale, dominant architecture of the subsurface. We recognize that the integration of geophysical measurement methods, and data, into watershed process characterization and modelling can only be achieved through dialogue. Especially, through the development of partnerships between geophysicists and hydrologists, partnerships that explore how the application of geophysics can answer critical hydrological science questions, and conversely provide an understanding of the limitations of geophysical measurements and interpretation. Copyright © 2008 John Wiley & Sons, Ltd. 相似文献
88.
M. S. Robinson P. C. Thomas J. Veverka S. L. Murchie B. B. Wilcox 《Meteoritics & planetary science》2002,37(12):1651-1684
Abstract— The global high‐resolution imaging of asteroid 433 Eros by the Near‐Earth Asteroid Rendezvous (NEAR) Shoemaker spacecraft has made it possible to develop the first comprehensive picture of the geology of a small S‐type asteroid. Eros displays a variety of surface features, and evidence of a substantial regolith. Large scale facets, grooves, and ridges indicate the presence of at least one global planar structure. Directional and superposition relations of smaller structural features suggest that fracturing has occurred throughout the object. As with other small objects, impact craters dominate the overall shape as well as the small‐scale topography of Eros. Depth/diameter ratios of craters on Eros average ~0.13, but the freshest craters approach lunar values of ~0.2. Ejecta block production from craters is highly variable; the majority of large blocks appear to have originated from one 7.6 km crater (Shoemaker). The interior morphology of craters does not reveal the influence of discrete mechanical boundaries at depth in the manner of craters formed on lunar mare regolith and on some parts of Phobos. This lack of mechanical boundaries, and the abundant evidence of regolith in nearly every high‐resolution image, suggests a gradation in the porosity and fracturing with depth. The density of small craters is deficient at sizes below ~200 m relative to predicted slopes of empirical saturation. This characteristic, which is also found on parts of Phobos and lunar highland areas, probably results from the efficient obliteration of small craters on a body with significant topographic slopes and a thick regolith. Eros displays a variety of regolith features, such as debris aprons, fine‐grained “ponded” deposits, talus cones, and bright and dark streamers on steep slopes indicative of efficient downslope movement of regolith. These processes serve to mix materials in the upper loose fragmental portion of the asteroid (regolith). In the instance of “ponded” materials and crater wall deposits, there is evidence of processes that segregate finer materials into discrete deposits. The NEAR observations have shown us that surface processes on small asteroids can be very complex and result in a wide variety of morphologic features and landforms that today seem exotic. Future missions to comets and asteroids will surely reveal still as yet unseen processes as well as give context to those discovered by the NEAR Shoemaker spacecraft. 相似文献
89.
Eric Robinson 《Geology Today》2003,19(6):219-222
90.
David J. Axon A. Marconi F.D. Macchetto A. Capetti Andrew Robinson 《Astrophysics and Space Science》1997,248(1-2):69-77
We have obtained HST FOC f/48 long-slit spectroscopy of the central 2 arcseconds of the Narrow Line Region of NGC 1068 between
3500-5400\OA with a spectral resolution of 1.78\OA/pixel. At a spatial scale of 0″.0287 per pixel these data provide an order
of magnitude improvement in resolution over previous ground based spectra and allow us to trace the interaction between the
radio jet and the gas in the NLR. Our results show that, within ±0″.5 of the radio-jet the emission lines are split into two
components whose velocity separation is 1500 km s-1. The emission line structure is reminiscent of that seen previously around
the jet of 3C120. Furthermore, this material enveloping the radio-jet is in a much higher ionization state than that of the
surrounding NLR gas. The highest excitation is coincident with the jet axis where emission in the coronal line of [FeVII]
λ3769\OA is detected but where [OII] λ3727 \OA is depressed. These results imply that we are witnessing a cocoon of hot gas
in expansion around the radio-jet created by its interaction with the gas, and that these shocks are sufficiently fast, at
least ± km s-1, that they are creating localized ionization effects.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献