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821.
Tomales Bay, California, has been the site oflong-term study of carbon-nitrogen-phospho-rus fluxes in the coastal zone. It has also one of severalcoastal sites being used for comparison of C-N-Pbiogeochemical fluxes. The site releases phosphorusand consumes dissolved nitrogen. It also producesdissolved inorganic carbon, mostly as elevatedalkalinity. The overall interpretation placed on thebiogeochemical fluxes is as follows. The system is netheterotrophic; that is, it consumes more organicmatter than it produces. A pathway of consumption thatis of particular importance to the nitrogen cycle isdenitrification. The combination of net heterotrophyand denitrification is the simultaneous release ofdissolved inorganic phosphorus and the uptake ofdissolved inorganic nitrogen. Much of the dissolvedinorganic carbon released during the net heterotrophyis bound in alkalinity, apparently the result ofsulfate reduction.Because this work can be traced by to the trainingthat one of the authors (SVS) received from KeithChave, it is appropriate to present a summary of theTomales Bay research in memory of Keith. 相似文献
822.
Electrogeochemical sampling with
Reinhard W. Leinz Donald B. Hoover David L. Fey David B. Smith Thaxson Patterson 《Journal of Geochemical Exploration》1998,61(1-3)
Electrogeochemical extraction methods are based on the migration of ions in an electric field. Ions present in soil moisture are transported by an applied current into fluids contained in special electrodes placed on the soil. The fluids are then collected and analyzed. Extractions are governed by Faraday's and Ohm's laws and are modeled by the operation of a simple Hittorf transference apparatus. Calculations show that the volume of soil sampled in an ideal electrogeochemical extraction can be orders of magnitude greater than the volumes used in more popular geochemical extraction methods, although this has not been verified experimentally.
is a method of in-situ electrogeochemical extraction that was developed in the former Soviet Union and has been tested and applied internationally to exploration for buried mineral deposits. Tests carried out at the United States Geological Survey (
) indicated that there were problems inherent in the use of
technology. The cause of the problems was determined to be the diffusion of acid from the conventional electrode into the soil. The
electrode incorporates two compartments and a salt bridge in a design that inhibits diffusion of acid and enables the collection of anions or cations. Tests over a gold-enriched vein in Colorado and over buried, Carlin-type, disseminated gold deposits in northern Nevada show that there are similarities and differences between
results and those by partial extractions of soils which include simple extractions with water, dilute acids and solutions of salts used as collector fluids in the electrodes. Results of both differ from the results obtained by total chemical digestion. The results indicate that
responds to mineralized faults associated with disseminated gold deposits whereas partial and total chemical extraction methods do not. This suggests that faults are favored channels for the upward migration of metals and that
may be more effective in exploration for the deposits. It defines anomalies that are often narrow and intense, an observation previously made by
researchers. The field tests show that
is less affected by surface contamination. A test over the Mike disseminated gold deposit indicates that the method may not be effective for locating deposits with impermeable cover. Faradaic extraction efficiencies of 20–30%, or more, are frequently achieved with
and the method generally shows good reproducibility, especially in extraction of major cations. However, ions of other metals that are useful in exploration, including Au and As, may be collected in low and temporally variable concentrations. The reason for this variability is unclear and requires further investigation. 相似文献
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823.
Agronomic impact of tephra fallout from the 1995 and 1996 Ruapehu Volcano eruptions, New Zealand 总被引:2,自引:0,他引:2
Eruptions from Ruapehu Volcano on 11 and 14 October 1995 and 17 June 1996 distributed at least 36×106 m3 of sulphur(S)-rich tephra over the central and eastern North Island of New Zealand. The tephras added between 30–1500 kg
ha–1 S to at least 25 000 km2 of land in primary production. Smaller but beneficial amounts of selenium (Se) and in some areas potassium and magnesium
were also supplied. Addition of S to the soils in the form of sulphate and elemental S resulted in a drop in soil pH and an
increase in pasture S contents within seven weeks of the eruptions. The soils affected by the tephra are naturally low in
S and Se, but following the eruptions S was not required in fertilizer applications in many areas. The strongest and longest
lasting effects of S and Se deposition were in high anion-retention soils particularly Hapludands (moist, moderately weathered
soils, derived from volcanic ash). Soluble fluorine concentrations within the tephras were low compared to historic Icelandic
and Chilean examples. However, pastoral livestock deaths were apparently caused by fluorosis in addition to starvation when
tephra covered feed. The Ruapehu tephra contained very low concentrations of other soluble toxic elements.
Received: 17 January 1997 · Accepted: 31 March 1997 相似文献
824.
Cycling of methane (CH4) in Tomales Bay, a 28-km2 temperature estuary in northern California with relatively low inputs of organic carbon, was studied over a 1-yr period. Water column CH4 concentrations showed spatial and temporal variability (range=8–100 nM), and were supersaturated with respect to the atmosphere by a factor of 2–37. Rates of net water column CH4 production-oxidation were determined by in situ experiments, and were not found to be significantly different from zero. Fluxes across the sediment-water interface, determined by direct measurement using benthic chambers, varied from ?0.1 μmol m?2 d?1 to +16 μmol m?2 d?1 (positive fluxes into water). Methane concentrations in the two perennial creeks feeding the bay varied annually (140–950 nM); these creeks were a significant CH4 source to the bay during winter. In addition, mass-balance calculations indicate a significant additional inter CH4 source, which is hypothesized to result from storm-related runoff from dairy farms adjacent to the bay. Systemwide CH4 budgets of the 16-km2 inner bay indicate benthic production (110 mol d?1) and atmospheric evasion (110 mol d?1) dominated during summer, while atmospheric evasion (160 mol d?1) and runoff from dairy farms (90 mol d?1) dominated during winter. 相似文献
825.
Michael D. Smith 《Astrophysics and Space Science》1998,261(1-4):183-184
The youngest protostars are obscured from direct view by a high column of molecular gas. Nevertheless, their presence is betrayed
through spectacular infrared outflows. I demonstrate here that infrared spectroscopy has the potential to reveal a remarkable
variety of details concerning the underlying physics.
Near-infrared spectroscopic analyses of the OMC-1, DR 21 & Cepheus A outflows are discussed here. Molecular hydrogen is vibrationally
excited by collisions in shock waves. In OMC-1, the ortho-para ratio has been mapped. The ratio is close to 3, suggesting
efficient shock thermalisation. In DR 21, shocked (up to the first vibrational level) and fluorescent (higher v-levels) components
have been successfully separated. In Cepheus A, non-LTE effects imply low densities.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
826.
Marco M. Maldoni R. G. Smith Garry Robinson & V. L. Rookyard 《Monthly notices of the Royal Astronomical Society》1998,298(1):251-258
We present new absorbance spectra of the 3-, 6- and 12-μm features of amorphous and crystalline H2 O ice obtained between 10 and 140 K. Three sets of measurements have been made. In series I, the ice film was initially deposited on to a CsI substrate at 10 K and successive spectra were then obtained at intermediate temperatures as the ice was warmed up to 140 K. The second set, series II, comprises spectra for ice films deposited and measured at temperatures between 10 and 140 K. In the third set of measurements, series III, spectra were obtained for an ice film deposited at 140 K and then at intermediate temperatures as the film was cooled down to 10 K. The series I and II results show that the ice undergoes an amorphous-to-crystalline phase transition in the 110–120 K range. The 3- and 12-μm bands have similar trends in full width at half-maximum (FWHM) and opposite peak wavelength shifts. The temperature behaviour of the 6-μm band is different, as no clear phase transition temperature can be discerned from its FWHM and peak wavelength position data. In the series III spectra the peak wavelength positions and FWHM of the three bands remain relatively constant, thus demonstrating the stability of the crystalline phase against thermal cycling. A comparison between the laboratory results and astronomical spectra suggests that the identification of the librational band of H2 O ice in OH 231.8 + 4.2 may be incorrect. 相似文献
827.
Michael D. Smith Jochen Eislöffel & Christopher J. Davis 《Monthly notices of the Royal Astronomical Society》1998,297(3):687-691
We demonstrate that a wide range of molecular hydrogen excitation can be observed in protostellar outflows at wavelengths in excess of 5 μm. Cold H2 in DR 21 is detected through the pure rotational transitions in the ground vibrational level (0–0). Hot H2 is detected in pure rotational transitions within higher vibrational levels (1–1, 1–2, etc.). Although this emission is relatively weak, we have detected two 1–1 lines in the DR 21 outflow with the ISO SWS instrument. We thus investigate molecular excitation over energy levels corresponding to the temperature range 1015–15 722 K, without the uncertainty introduced by differential extinction when employing near-infrared data.
This gas is thermally excited. We uncover a rather low H2 excitation in the DR 21 West Peak. The line emission cannot be produced from single C-shocks or J-shocks; a range of shock strengths is required. This suggests that bow shocks and/or bow-generated supersonic turbulence is responsible. We are able to distinguish this shock-excited gas from the fluoresced gas detected in the K band, providing support for the dual-excitation model of Fernandes, Brand & Burton. 相似文献
This gas is thermally excited. We uncover a rather low H
828.
829.
Christopher J. Davis Michael D. Smith & Gerald H. Moriarty-Schieven 《Monthly notices of the Royal Astronomical Society》1998,299(3):825-833
Near-infrared images in H2 line emission and submillimetre maps in CO J = 3–2 emission illustrate the remarkable association between a molecular bow shock and the redshifted molecular outflow lobe in W75N. The flow lobe fits perfectly into the wake of the bow, as one would expect if the lobe represented swept-up gas. Indeed, these observations strongly support the 'bow shock' entrainment scenario for molecular outflows driven by young stars. The characteristics of the bow shock and CO outflow lobe are compared with those of numerical simulations of jet-driven flows. These models successfully reproduce the bulge and limb-brightening in the CO outflow, although the model H2 bow exhibits more structure extending back along the flow axis. We also find that the size of the flow, the high mass fraction in the flow at low outflow velocities (low γ values) and the high CO/H2 luminosity ratio indicate that the system is evolved. We also predict a correlation, in evolved systems, between outflow age and the CO/H2 luminosity ratio. 相似文献
830.