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221.
Gregory E. Faiers Barry D. Keim Katherine K. Hirschboeck 《The Professional geographer》1994,46(2):156-163
This research classifies extreme three-hour and 24-hour rainfall events in Louisiana by synoptic weather types (Frontal, Gulf Tropical Disturbance, and Air Mass). These classes were used to analyze differences in frequencies and intensities of extreme rainfall. Significant differences were found in the storm frequencies by weather type. However, no significant differences were detected in rainfall intensities between weather types during either duration. These findings have a bearing on statistical procedures associated with estimating storm probabilities in the region. 相似文献
222.
Antony D. Clarke 《Journal of Atmospheric Chemistry》1989,9(1-3):255-266
Thermal and optical techniques were used at Barrow, Alaska during AGASP II (3/20/86–4/7/86) to measure in-situ variability of major aerosol components present in Arctic Haze. The experiment provided continuous data on the concentration, size distribution and relative proportions of sulfate species and refractory aerosol for particle diameters of 0.15 to 5 m. Filter samples were also taken for determination of aerosol optical absorption due to soot (EC-elemental carbon). Although pronounced haze events were absence during this period the haze aerosol present varied in concentration between 2 and 6 g/m3 but showed little change in relative constituents. Apart from local influences, the optical data indicated a persistent fine-mode sulfate aerosol with a NH4
+/SO4
– molar ratio of about 0.4 and a refractory component of somewhat less than 10% by mass. A preliminary comparison of soot estimates determined from the light absorption data with the size distributions of refractory aerosol observed independently by the optical particle counter showed good agreement during the sample period. In the absence of local pollution, values of single scatter albedo derived from light scattering and light absorption showed similar variation about the average value of 0.86 found by us during flights north of Barrow three years earlier during AGASP I. 相似文献
223.
Water-Soluble dicarboxylic acids, ketoacids and dicarbonyls in the atmospheric aerosols over the southern ocean and western pacific ocean 总被引:2,自引:0,他引:2
Water-soluble dicarboxylic acids (DCAs), ketoacids, and α-dicarbonyls in the marine aerosol samples collected over the Southern
Ocean and western Pacific Ocean were determined. Oxalic acid was the most abundant species, followed by malonic acid and then
succinic acid. It is suggested that aerosol concentrations of the organics over the Southern Ocean in this work represent
their global background levels. Over the Southern Ocean, total concentrations of DCAs ranged from 2.9 to 7.2 ng m−3 (average: 4.5 ng m−3), ketoacids from 0.14 to 0.40 ng m−3 (av.: 0.28 ng m−3), and dicarbonyls from 0.06 to 0.29 ng m−3 (av.: 0.11 ng m−3). Over the western Pacific, total concentrations of DCAs ranged from 1.7 to 170 ng m−3 (av.: 60 ng m−3), ketoacids from 0.08 to 5.3 ng m−3 (av.: 1.8 ng m−3), and dicarbonyls from 0.03 to 4.6 ng m−3 (av.: 0.95 ng m−3). DCAs over the western Pacific have constituted a large fraction of organic aerosols with a mean DCAs-C/TC (total carbon)
of 7.0% (range: 0.59–14%). Such a high value was in contrast to the low DCAs-C/TC (av.: 1.8%; range: 0.89–4.0%) for the Southern
Ocean aerosols. Based on the relative abundances and latitudinal distributions of these organics, we propose that long-range
atmospheric transport is more important over the western Pacific Ocean, in contrast, in situ photochemical production is more significant over the Southern Ocean although absolute concentrations of the organics are
much lower. 相似文献
224.
A. E. Poberezhnaya A. P. Fedotov T. Ya. Sitnikova M. Yu. Semenov G. A. Ziborova E. L. Otinova A. V. Khabuev 《Journal of Paleolimnology》2006,36(2):133-149
This paper deals with the investigation of the upper 11.6 m portion of a long drill core (KDP-01) taken from the bottom sediments of Lake Khubsugul. Ostracod species and their assemblages recovered from the core were analyzed. The data are compared with the carbonate and sulfate values obtained from bulk sediment, as well as with the flux of the coarse terrigenous fraction (>200 m) from the same core. Based on the previously calculated depth-age sedimentary model, the oldest age of the core studied here is about 230 ka. The four ostracod species recovered in the core are Cytherissa lacustris, Candona lepnevae, Limnocythere inopinata and Leucocythere sp. According to the distribution of those ostracods, we distinguish four main periods, each of about 50 ka long. Based on the ecological requirements of extant ostracods, two assemblages typifying a low water level and high salinity, on the first hand, and another representing freshwater and high lake level are recognized. The first “high salinity” ostracods correspond to “cold” periods as seen globally, while “freshwater” ostracods are associated with interglacials. Ostracod valves are absent during interglacial optima. This may be due to chemical dissolution of calcium carbonate related to organic matter decay at the initial stages of diagenesis, probably because during interglacials, in contrast to glacials, organic matter flux reaching the lake bottom were significantly higher. The periodicity in the development of ostracod species assemblages follows 17, 24 and 47 ka cycles related to orbital forcing. Its diversity is correlated with summer temperature fluctuations in northern altitudes for the past 230 ka. The maximum in species diversity follows the temperature maxima, by about 1.5 and 2 ka. Overall, the data obtained demonstrate a correlation between climatic changes and variations in specific and quantitative ratios of ostracod species during the last 230 ka. 相似文献
225.
226.
This study presents a framework for numerical simulations based upon micromechanical parameters in modeling progressive failures
of heterogeneous rock specimens under compression. In our numerical simulations, a Weibull distribution of the strength and
elastic properties of the finite elements is assumed, and the associated Weibull parameters are estimated in terms of microstructural
properties, such as crack size distribution and grain size, through microscopic observations of microcracks. The main uncertainty
in this procedure lies on the fact that various ways can be used to formulate a ``microcrack size distribution' in relating
to the Weibull parameters. As one possible choice, the present study uses the number of counted cracks per unit scanned volume
per grain size to formulate the crack distributions. Finally, as a tool, the Rock Failure Process Analysis code (RFPA2D) is adopted for simulating the progressive failure and microseismicity of heterogeneous rocks by using an elastic-damage
finite-element approach. To verify our framework, compression tests on marble specimens are conducted, and the measured acoustic
emissions (AE) are compared with those predicted by the numerical simulations. The mode of failure, compressive strength and
AE pattern of our simulations basically agree with experimental observations. 相似文献
227.
P. J. van Hengstum E. G. Reinhardt J. I. Boyce C. Clark 《Journal of Paleolimnology》2007,37(4):603-618
This study examines the anthropogenic alteration of sedimentation in Frenchman’s Bay in Lake Ontario, using high-resolution
particle size analysis in two 200 cm cores. Lithofacies were determined using the particle size data of both the terrigenous
sediment and terrigenous sediment + diatom fractions. Terrigenous particle size data from the centre of the lagoon provided
the most representative record of anthropogenic impacts. Three distinctive lithofacies were recognized: (1) a Natural Wetland
(NW) lithofacies (106–200 cm) had an average mean particle size of 49.4 μm, a mode of 29.4 μm and an average standard deviation
of 119.1 μm; (2) an Agricultural and Deforestation (AD) lithofacies (40–105 cm) had a statistically significant lower average
mean (30.8 μm), mode (13.5 μm), and standard deviation (48.5) μm; (3) an Urbanized (U) lithofacies (0–40 cm) showed a continued
trend towards smaller particle sizes with an average mean of 21.2 μm, a mode of 9.4 μm, and an average standard deviation
of 32.7 μm. The lithofacies correlated with previously identified trends in thecamoebian biofacies and magnetic susceptibility
data showing post-colonial lagoon eutrophication and increased overland soil erosion. The up-core trend towards finer and
less variable particle sizes is attributed to erosion of fine-grained watershed sediments (glacial Lake Iroquois silts and
clay) during land-clearance and modification of natural drainage patterns. The influx of silts and clays into the lagoon is
also recorded by increased sediment accumulation rates and a reduction in seasonal sediment variability in the wetland. Based
on the 210Pb dates, sedimentation rates increased at 1850 ±56 AD (AD lithofacies) and suggest an exponentially increasing trend in accumulation
rates. Increasing sedimentation rates can be attributed to the progressive loss of native vegetation and intensified erosion
of Lake Iroquois deposits via stream and hillslope erosion. Ecologically, the increased input of fine-grained sediments into
the wetland has resulted in reduced water clarity and has altered the wetland substrate contributing to wetland loss in Frenchman’s
Bay. 相似文献
228.
229.
A. Grassia 《Mathematical Geology》1986,18(3):323-328
A procedure is developed to determine the area sample required of polished sections of an abundant mineral in rock form to assess for presence of inbedded particles of a rare mineral, occurring in particulate form, with a prechosen probability level. 相似文献
230.
卡特巴阿苏金铜矿床是近年在西天山新发现的大型金铜矿床,资源储量有望继续扩大,后续勘探方向亟待明确。文章对矿区地表11条探槽和主矿段已完成的108个钻孔中金、铜品位进行了统计分析。研究结果表明,金铜成矿受构造断裂控制,沿断裂破碎带走向自西向东,成矿元素在平面和纵剖面中均显示Cu-Au→Au-Cu→Au(Cu)→Au的变化特征,暗示成矿流体自南西流向北东,成矿热源可能位于矿区63~47勘探线之间;在47勘探线剖面中,成矿元素自下而上显示Au-Cu→Au(Cu)→Au的变化特征,暗示成矿流体来自深部。结合在矿区63~47勘探线之间发现的与成矿有关的闪长岩小岩体,以及大比例尺勘查地球化学测量所反映的矿区自南西至北东具有W-CuAu→Au-Cu-Bi-Mo→Au(Cu)-Pb-Zn→Au-Ag的元素分布特征,认为矿区成矿中心可能在63~47勘探线之间,成矿流体由此沿断裂构造向北东方向迁移,后续正确的地质勘查方向应在63~47勘探线间的深部。 相似文献