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91.
Laurence Pinturier-Geiss Jeanne Laureillard Catherine Riaux-Gobin Joëlle Fillaux Alain Saliot 《Marine Chemistry》2001,75(4)
Deep-sea sediment samples were collected in the Western Crozet Basin (Indian sector of the Southern Ocean) through Permanently Open Ocean Zone (POOZ), Polar Frontal Zone (PFZ) and Sub-Antarctic Zone (SAZ). Lipid class and fatty acid compositions were investigated to determine the sources and fate of organic matter in the first centimeter of sediment and, above this layer, in the fluff (when present) and particles in the overlying water. The total lipid content varied from 74 to 1033 μg l−1 in the overlying particles and fluffs, and from 24 to 97 μg g−1 dry mass (DM) in surficial sediments. Lipid composition was always dominated by phospholipids in the first centimeter of sediment and often in the overlying particles. The amount of phospholipids (labile compounds representative of fresh material) was compared to the amount of chlorophyll a (Chl a), another compound that is susceptible to rapid degradation. A strong N–S gradient was observed in the distribution of these two compounds, which was attributed to the contrasting hydrodynamic of the study area. The high sedimentation rate in POOZ resulted in better preservation of Chl a in this zone than in other zones of the Crozet Basin (PFZ and SAZ). Phospholipid fatty acids suggested the presence of viable as well as morphologically intact organisms, and these organisms consisted essentially of bacteria with some diatom cysts in the fluff of POOZ. These spores were able to grow in the culture, indicating that they were still viable. Despite the strong hydrodynamic variability, phospholipid fatty acids analysed from the deep-sea surficial sediments were never representative of plankton. This pointed to the extremely labile nature of the phospholipids originally present in planktonic material compared with Chl a, which was always found in overlying particles and surficial sediments. 相似文献
92.
Jason W. Barnes Jacob Bow Jacob Schwartz Robert H. Brown Jason M. Soderblom Alexander G. Hayes Graham Vixie Stéphane Le Mouélic Sebastien Rodriguez Christophe Sotin Ralf Jaumann Katrin Stephan Laurence A. Soderblom Roger N. Clark Bonnie J. Buratti Kevin H. Baines Philip D. Nicholson 《Icarus》2011,216(1):136-140
We report the discovery of organic sedimentary deposits at the bottom of dry lakebeds near Titan’s north pole in observations from the Cassini Visual and Infrared Mapping Spectrometer (VIMS). We show evidence that the deposits are evaporitic, making Titan just the third known planetary body with evaporitic processes after Earth and Mars, and is the first that uses a solvent other than water. 相似文献
93.
We present two case studies of cluster encounters with foreshock cavities. For one event, we are able, for the first time, to accurately relate the observation of a foreshock cavity to the measured position of the bow shock. This allows us to compute the shock angle, a vital parameter in models of foreshock cavity formation, with greater confidence than any previous study. This cavity appears to be elongated along the magnetic field and we use the multispacecraft nature of the Cluster mission to constrain its field-parallel and -perpendicular extent. We show that this event is embedded within a region of field-aligned ion beams. This is the first time a foreshock cavity has been shown to be surrounded by foreshock ion beams. A second foreshock cavity is associated with a small rotation in the interplanetary magnetic field (IMF). We show that this event appears on the boundary between an interval when the spacecraft were inside the ion foreshock, and an excursion upstream. This is the first report of a foreshock cavity observed during the traversal of the global foreshock. This second event has some features expected from the new Sibeck et al. (2008) model of cavities as brief encounters with a spatial boundary in the global foreshock. 相似文献
94.
Laurence Jones 《International journal of geographical information science》2013,27(5):1045-1047
95.
96.
A proxy named “upwelling age”, defined as the ratio of wind time scale to “advection time”, was developed to quantify the
local tendency for coastal upwelling. The formulation of the “advection time” was derived from Ekman theory. A 3D numerical
model was used to validate and refine the theoretical formula by simulating a total of 30 cases of different bottom topographies
and wind stresses. The results agree reasonably well with the theoretical formulation although some modifications are necessary.
The final formulation of the “advection time” was parameterized as a function of pycnocline depth, bottom slope, and wind
stress. 相似文献
97.
Laurence Laperrière Marie-Andrée Fallu Sonja Hausmann Reinhard Pienitz Derek Muir 《Journal of Paleolimnology》2008,40(1):309-324
Qualitative and quantitative analysis of fossil diatoms and geochemical signals preserved in the sediments of Lac Dauriat
(subarctic Quebec) were performed to evaluate the impacts of nearby mining activity and the expansion of the town of Schefferville
on the water quality of the lake, and to reconstruct the changes of its trophic status. The presence of taxa typical of nutrient-enriched
environments (e.g., Cyclostephanos invisitatus, Nitzschia gracilis, Nitzschia perminuta) and the low percentages of chrysophytes were indicative of the advanced state of eutrophication of the lake during the peak
of mining activity, and were evidence of the negative impacts of municipal waste on the water quality of Lac Dauriat. Sedimentary
analysis of metals, notably lead, mercury, cadmium, bismuth, cobalt, copper and zinc, showed maximum concentrations between
1940 and 1960 with mining era to pre-development enrichment factors ranging from 4.5 to 7.9. The changes seen in recent sediments
reflected 3 distinct stages in the recent history of this ecosystem: (a) the non-perturbed, pre-mining (1882–1939), (b) the
perturbed, mining period (1939–1977) with accelerated eutrophication, and (c) the post-mining period (1977–1999) with indications
of natural recovery of the system after the installation of a water treatment plant in 1975, the closing of the mine in 1983,
and the subsequent exodus of the town’s population. Despite the trajectory towards a return to the lake’s natural conditions,
water resource managers and (paleo-)limnologists should be alarmed that the impacts of past human disturbance are still in
evidence more than 20 years after the closure of the mines, and that Lac Dauriat has yet to reach its natural state of the
period preceding extreme anthropogenic impact. 相似文献
98.
ABSTRACT. Pressured by structural adjustment loan conditions, Côte d'Ivoire reduced state support for rice production and processing during the 1990s. In this article we examine how various actors in the rice commodity chain adapted to the macroeconomic reforms. Following a brief history of the rice sector, we present the results of fieldwork based on interviews conducted in 2002 of farmers, millers, traders, and workers in the state extension service and nongovernmental organizations. We found that, in the absence of state supports for farmers, private millers became the focal point of regional producer‐processor rice networks. The four networks identified became the sole source of domestic commercial rice when the state removed subsidies for fertilizer and modern seeds, privatized extension, and liberalized prices and imports. To increase their role in the national rice supply, the rice networks may need support through microlending and a focus on niche markets. 相似文献
99.
Future heat vulnerability in California, Part II: projecting future heat-related mortality 总被引:1,自引:0,他引:1
Scott C. Sheridan Michael J. Allen Cameron C. Lee Laurence S. Kalkstein 《Climatic change》2012,115(2):311-326
Through the 21st century, a significant increase in heat events is likely across California (USA). Beyond any climate change, the state will become more vulnerable through demographic changes resulting in a rapidly aging population. To assess these impacts, future heat-related mortality estimates are derived for nine metropolitan areas in the state for the remainder of the century. Heat-related mortality is first assessed by initially determining historical weather-type mortality relationships for each metropolitan area. These are then projected into the future based on predicted weather types created in Part I. Estimates account for several levels of uncertainty: for each metropolitan area, mortality values are produced for five different climate model-scenarios, three different population projections (along with a constant-population model), and with and without partial acclimatization. Major urban centers could have a greater than tenfold increase in short-term increases in heat-related mortality in the over 65 age group by the 2090s. 相似文献
100.