全文获取类型
收费全文 | 296篇 |
免费 | 18篇 |
国内免费 | 2篇 |
专业分类
测绘学 | 14篇 |
大气科学 | 18篇 |
地球物理 | 109篇 |
地质学 | 93篇 |
海洋学 | 26篇 |
天文学 | 43篇 |
综合类 | 1篇 |
自然地理 | 12篇 |
出版年
2024年 | 1篇 |
2022年 | 1篇 |
2021年 | 4篇 |
2020年 | 16篇 |
2019年 | 10篇 |
2018年 | 21篇 |
2017年 | 14篇 |
2016年 | 16篇 |
2015年 | 10篇 |
2014年 | 17篇 |
2013年 | 20篇 |
2012年 | 7篇 |
2011年 | 20篇 |
2010年 | 21篇 |
2009年 | 28篇 |
2008年 | 15篇 |
2007年 | 21篇 |
2006年 | 8篇 |
2005年 | 13篇 |
2004年 | 9篇 |
2003年 | 5篇 |
2002年 | 4篇 |
2001年 | 2篇 |
2000年 | 2篇 |
1999年 | 3篇 |
1998年 | 2篇 |
1996年 | 2篇 |
1995年 | 1篇 |
1994年 | 1篇 |
1993年 | 1篇 |
1992年 | 1篇 |
1991年 | 1篇 |
1990年 | 2篇 |
1989年 | 1篇 |
1986年 | 1篇 |
1984年 | 2篇 |
1983年 | 1篇 |
1982年 | 2篇 |
1981年 | 1篇 |
1980年 | 2篇 |
1978年 | 1篇 |
1977年 | 2篇 |
1976年 | 1篇 |
1975年 | 2篇 |
1973年 | 1篇 |
排序方式: 共有316条查询结果,搜索用时 15 毫秒
301.
Theoretical and Applied Climatology - A gridded 0.25° reconstruction of rainfall kinetic energy (RKE) over the UK, on the basis of pluviometric observations and reanalysis back to 1765, shows... 相似文献
302.
Dissolution experiments on a serpentinite were performed at 70 °C, 0.1 MPa, in H2SO4 solution, in open and closed systems, in order to evaluate the overall dissolution rate of mineral components over different times (4, 9 and 24 h). In addition, the serpentinite powder was reacted with a NaCl-bearing aqueous solution and supercritical CO2 for 24 h at higher pressures (9-30 MPa) and temperatures (250-300 °C) either in a stirred reactor or in an externally-heated pressure vessel to assess both the dissolution rate of serpentinite minerals and the progress of the carbonation reaction. Results show that, at 0.1 MPa, MgO extraction from serpentinite ranges from 82% to 98% and dissolution rate varies from 8.5 × 10−10 mole m−2 s−1 to 4.2 × 10−9 mole m−2 s−1. Attempts to obtain carbonates from the Mg-rich solutions by increasing their pH failed since Mg- and NH4- bearing sulfates promptly precipitated. On the other hand, at higher pressures, significant crystallization (5.0-10.4 wt%) of Ca- and Fe-bearing magnesite was accomplished at 30 MPa and 300 °C using 100 g L−1 NaCl aqueous solutions. The corresponding amount of CO2 sequestered by crystallization of carbonates is 9.4-15.9 mole%. Dissolution rate (from 6.3 × 10−11 mole m−2 s−1 to 1.3 × 10−10 mole m−2 s−1) is lower than that obtained at 0.1 MPa and 70 °C but it is related to pH values much higher (3.3-4.4) than that (−0.65) calculated for the H2SO4 solution.Through a thorough review of previous experimental investigations on the dissolution kinetics of serpentine minerals the authors propose adopting: (i) the log rate [mole m−2 s−1] value of −12.08 ± 0.16 (1σ), as representative of the neutral dissolution mechanism at 25 °C and (ii) the following relationship for the acidic dissolution mechanism at 25 °C:
log rate=-0.45(±0.09)×pH-10.01(±0.30). 相似文献
303.
Hervé Martin Francis Albarède Philippe Claeys Muriel Gargaud Bernard Marty Alessandro Morbidelli Daniele L. Pinti 《Earth, Moon, and Planets》2006,98(1-4):97-151
Except the old Jack Hills zircon crystals, it does not exit direct record of the first 500 Ma of the Earth history. Consequently, the succession of events that took place during this period is only indirectly known through geochemistry, comparison with other telluric planets, and numerical modelling. Just after planetary accretion several episodes were necessary in order to make life apparition and development possible and to make the Earth surface habitable. Among these stages are: the core differentiation, the formation of a magma ocean, the apparition of the first atmosphere, oceans and continents as well as the development of magnetic field and of plate tectonics. In the same time, Earth has been subject to extraterrestrial events such as the Late Heavy Bombardment (LHB) between 3.95 and 3.8 Ga. Since 4.4–4.3 Ga, the conditions for pre-biotic chemistry and appearance of life were already met (liquid water, continental crust, no strong meteoritic bombardment, etc...). This does not mean that life existed as early, but this demonstrates that all necessary conditions assumed for life development were already present on Earth. 相似文献
304.
Daniele Nizzoli Giuseppe Castaldelli Marco Bartoli David Thomas Welsh Patricia Arriaga Gomez Anna Elisa Fano Pierluigi Viaroli 《Marine Ecology》2002,23(S1):297-306
Abstract. Dark respiration rates, dissolved inorganic nitrogen (DIN) fluxes and nitrification rates were measured at two sites in the microtidal Sacca di Goro lagoon in September 2000. DIN fluxes correlated with the biomass of the dominant macrofauna species (the amphipod Corophium spp. at station Giralda and the polychaete Neanthes spp. at station Faro). Respiration (> 6 mmol O2 m−2 h−1 ) and ammonium fluxes (> 80μmol N m−2 h−1 ) were higher at station Giralda despite the lower organic matter content (4.5 %) and lower macrofauna biomass (4 g AFDW m−2 ). At both sites ammonium fluxes were significantly correlated with the biomass of the benthic infauna, but Corophium stimulated ammonium NH4 + fluxes 3-fold compared to Neanthes. The amphipod also enhanced nitrification rates (> 300 μmol N m−2 h−1 ) due to the high density of its burrows, the higher NH4 + regeneration rates and the enhanced oxygen supply to the bacteria. 相似文献
305.
306.
Lidia Contarino Francesca Zuccarello Paolo Romano Daniele Spadaro Salvatore L. Guglielmino Viviana Battiato 《Acta Geophysica》2009,57(1):52-63
Our comprehension of solar flares is still lacking in many aspects and the possibility of observing active regions during
the first phases of flare occurrence is limited by our capability of doing accurate flare forecasting. In order to give a
contribution to this aspect, we focused our attention on the characteristics that must be fulfilled by sunspot-groups in order
to be flare-productive. We addressed this problem using a statistical approach: first, we analyzed sunspot-groups parameters
(i.e., Zürich class, magnetic configuration, area, morphology of the penumbra) and evolution; then, we performed a flare forecasting
campaign, based on the results obtained in the first phase and on real-time observations. The results obtained by comparing
the flare forecasting probability with the number of flares that have actually occurred are quite encouraging; we plan to
improve this procedure by including a bigger statistical sampling. 相似文献
307.
Daniele Boyer Jean-Louis Le Mouël Vincent Courtillot 《Earth and Planetary Science Letters》1981,52(2):372-380
A very broad band (10?3 to 104 Hz) magnetotelluric investigation of the axial zone of the Ghoubbet-Asal rift (Djibouti) has revealed a shallow (2–4 km) magma chamber which can be mapped in some detail. The suggested roof of the chamber is shallowest very close to the Ardoukoba volcano which was built during the November 1978 rifting episode. 相似文献
308.
Influence of glass polymerisation and oxidation on micro-Raman water analysis in alumino-silicate glasses 总被引:1,自引:0,他引:1
Maxime Mercier Andrea Di Muro Daniele Giordano Priscille Lesne Bruno Scaillet Gilles Montagnac 《Geochimica et cosmochimica acta》2009,73(1):197-217
The development of an accurate analytical procedure for determination of dissolved water in complex alumino-silicate glasses via micro-Raman analysis requires the assessment of the spectra topology dependence on glass composition. We report here a detailed study of the respective influence of bulk composition, iron oxidation state and total water content on the absolute and relative intensities of the main Raman bands related to glass network vibrations (LF: ∼490 cm−1; HF: ∼960 cm−1) and total water stretching (H2OT: ∼3550 cm−1) in natural glasses. The evolution of spectra topology was examined in (i) 33 anhydrous glasses produced by the re-melting of natural rock samples, which span a very large range of polymerisation degree (NBO/T from 0.00 to 1.16), (ii) 2 sets of synthetic anhydrous basaltic glasses with variable iron oxidation state (Fe3+/FeT from 0.05 to 0.87), and (iii) 6 sets of natural hydrous glasses (CH2OT from 0.4 to 7.0 wt%) with NBO/T varying from 0.01 to 0.76.In the explored domain of water concentration, external calibration procedure based on the H2OT band height is matrix-independent but its accuracy relies on precise control of the focusing depth and beam energy on the sample. Matrix-dependence strongly affects the internal calibrations based on H2OT height scaled to that of LF or HF bands but its effect decreases from acid (low NBO/T, SM) to basic (high NBO/T, SM) glasses. Structural parameters such as NBO/T (non-bridging oxygen per tetrahedron) and SM (sum of structural modifiers) describe the matrix-dependence better than simple compositional parameters (e.g. SiO2, Na2O + K2O). Iron oxidation state has only a minor influence on band topology in basalts and is thus not expected to significantly affect the Raman determinations of water in mafic (e.g. low SiO2, iron-rich) glasses. Modelling the evolution of the relative band height with polymerisation degree allows us to propose a general equation to predict the dissolved water content in natural glasses:
309.
E. Bruce Watson Daniele J. Cherniak Elizabeth A. Frank 《Geochimica et cosmochimica acta》2009,73(16):4792-5705
Self-diffusion of sulfur in pyrite (FeS2) was characterized over the temperature range ∼500-725 °C (∼1 bar pressure) by immersing natural specimens in a bath of molten elemental 34S and characterizing the resulting diffusive-exchange profiles by Rutherford backscattering spectroscopy (RBS). The temperature dependence of the sulfur diffusivity (DS) conforms to DS = Do exp(−Ea/RT), where the pre-exponential constant (Do) and the activation energy (Ea) are constrained as follows:
310.
This work proposes a Lunar Global Positioning System (LGPS) and a Lunar Global Communication System (LGCS) using two constellations
of satellites on Lissajous trajectories around the collinear L
1 and L
2 libration points in the Earth–Moon system. This solution is compared against a Walker constellation around the Moon similar
to the one used for the Global Positioning System (GPS) on the Earth to evaluate the main differences between the two cases
and the advantages of adopting the Lissajous constellations. The problem is first studied using the Circular Restricted Three
Body Problem to find out its main features. The study is then repeated with higher fidelity using a four-body model and higher-order
reference trajectories to simulate the Earth-Moon-spacecraft dynamics more accurately. The LGPS performance is evaluated for
both on-ground and in-flight users, and a visibility study for the LGCS is used to check that communication between opposite
sides of the Moon is possible. The total ΔV required for the transfer trajectories from the Earth to the constellations and the trajectory control is calculated. Finally,
the estimated propellant consumption and the total number of satellites for the Walker constellation and the Lissajous constellations
is used as a performance index to compare the two proposed solutions. 相似文献