全文获取类型
收费全文 | 258篇 |
免费 | 19篇 |
国内免费 | 2篇 |
专业分类
测绘学 | 9篇 |
大气科学 | 22篇 |
地球物理 | 60篇 |
地质学 | 129篇 |
海洋学 | 14篇 |
天文学 | 27篇 |
自然地理 | 18篇 |
出版年
2024年 | 1篇 |
2023年 | 2篇 |
2022年 | 2篇 |
2021年 | 9篇 |
2020年 | 7篇 |
2019年 | 14篇 |
2018年 | 12篇 |
2017年 | 16篇 |
2016年 | 19篇 |
2015年 | 14篇 |
2014年 | 13篇 |
2013年 | 19篇 |
2012年 | 11篇 |
2011年 | 29篇 |
2010年 | 29篇 |
2009年 | 16篇 |
2008年 | 12篇 |
2007年 | 10篇 |
2006年 | 7篇 |
2005年 | 4篇 |
2004年 | 8篇 |
2003年 | 2篇 |
2002年 | 7篇 |
2001年 | 1篇 |
2000年 | 2篇 |
1999年 | 1篇 |
1998年 | 1篇 |
1995年 | 3篇 |
1992年 | 1篇 |
1986年 | 1篇 |
1978年 | 1篇 |
1975年 | 2篇 |
1974年 | 2篇 |
1973年 | 1篇 |
排序方式: 共有279条查询结果,搜索用时 15 毫秒
231.
232.
The 1D version of the Model for Applications at Regional Scale is used to parameterize the effects of sea surface waves in
2D in a horizontally homogeneous offshore zone of the Iroise sea. Here we present the first simulation of the Iroise sea including
sea surface waves forcing, and more generally, the first study of a boundary layer including the Hasselmann force with a tidal
wave. We use a single equation turbulence closure based on a non-local diagnosis for energetic and dissipation length scales.
The turbulent energy flux at the surface due to whitecaps and the Hasselmann force induced by Stokes drift are assessed using
the whole sea surface waves spectrum given by the Wave Watch Third generation model. The ability of the parameterization to
reproduce surface currents over a period of 1 year (2007) is tested with high frequency radar using spectral and time-frequency
analysis. One problem with 1D modelling, corresponding to overestimation of current oscillating at inertial frequency is illustrated
by comparing 1D and 3D simulations. We found an overall improvement by including the Hasselmann force mainly within the bandwidth
of less than one cycle per day to one cycle per day for surface currents. Turbulence is induced by whitecaps decaying rapidly
below the ocean surface but the mixed layer below 40 m is deeper due to waves breaking on the sea surface. 相似文献
233.
Guillaume de Combarieu Michel L. Schlegel Delphine NeffEddy Foy Delphine VantelonPhilippe Barboux Stéphane Gin 《Applied Geochemistry》2011,26(1):65-79
Glass-iron-clay setups were reacted at 90 °C for 6-18 months to investigate the coupled interactions between glass alteration, Fe corrosion and clay transformation. The reacted interfaces were probed at the microscopic level using complementary characterization methods (scanning electron microscopy coupled with energy-dispersive X-ray analysis, micro-Raman spectroscopy, micro X-ray diffraction, micro X-ray fluorescence spectroscopy, and micro X-ray absorption near-edge structure spectroscopy). The 10-μm thick Fe foil was fully corroded within 10 months, exposing glass to the pore solution. Iron corrosion led to the formation of a layer containing mostly magnetite, siderite and Fe-rich phyllosilicates with one tetrahedral and one octahedral sheet (TO) or two tetrahedral and one octahedral (TOT) sheet per layer. The clay in contact with this corrosion layer was enriched in siderite (FeCO3). Glass alteration resulted in the formation of a gel layer whose thickness increased with reaction time (from 20 μm after 6 months to 80 μm after 18 months) and a thin layer of secondary precipitates that concentrated lanthanides, P, and Mo. Assuming conservative behavior of Zr, the Si molar concentration in the gel is about 57% that in the glass. Glass dissolution remained at a rate close to the initial dissolution rate r0. The data are consistent with glass dissolution sustained by the uptake of dissolved Si and charge-compensating cations on secondary (corrosion) products, thus maintaining the gel porosity open and facilitating the leaching of easily soluble elements. 相似文献
234.
Guillaume Morard Denis Andrault Nicolas Guignot Julien Siebert Gaston Garbarino Daniele Antonangeli 《Physics and Chemistry of Minerals》2011,38(10):767-776
High pressure melting behavior of three Fe-alloys containing 5 wt% Ni and (1) 10 wt% Si, (2) 15 wt% Si or (3) 12 wt% S was
investigated up to megabar pressures by in situ X-ray diffraction and laser-heated diamond anvil cell techniques. We observe
a decrease in melting temperature with increasing Si content over the entire investigated pressure range. This trend is used
to discuss the melting curve of pure Fe. Moreover, our measurements of eutectic melting in the Fe–Fe3S system show a change in slope around 50 GPa concomitant with the fcc–hcp phase transition in pure solid iron. Extrapolations
of our melting curve up to the core–mantle boundary pressure yield values of 3,600–3,750 K for the freezing temperature of
plausible outer core compositions. 相似文献
235.
Guillaume Pierre 《Geodinamica Acta》2013,26(1):45-54
RésuméLa question de la capture de la Meuse lorraine est abordée par le biais de l’étude des sables tertiaires qui jalonnent les plateaux de l’Ardenne méridionale. Toujours polygéniques, ces sables ont une histoire plus ou moins longue qui débute à l’Éocène où l’altération poussée du socle produit un épais manteau sableux. Certains gisements in situ fossilisés sont restés quasiment intacts (Régniowez) tandis que d’autres (Doisches) portent la marque de remaniements successifs (marins et/ou continentaux) qui se suivent jusqu’au Miocène sans que leur filiation avec le matériau d’origine, attestée par la nature de leurs barylites, ne se perde. Comme les sables fluviatiles miocènes (in fine) du plateau ardennais ne portent pas la signature minéralogique d’une Meuse lorraine, à l’inverse de la Traînée mosane (datée du Miocène moyen), la capture se trouve à la fois confirmée et datée. L’ancien réseau de la Meuse lorraine, quant à lui, n’a pu se mettre en place qu’après l’Oligocène, époque à laquelle un glacis incliné de l’Ardenne vers le Bassin parisien fonctionnait encore. © 2000 Éditions scientifiques et médicales Elsevier SAS 相似文献
236.
Suzanne A. Pierce John M. Sharp Jr. Joseph H. A. Guillaume Robert E. Mace David J. Eaton 《Hydrogeology Journal》2013,21(2):331-340
Groundwater availability is at the core of hydrogeology as a discipline and, simultaneously, the concept is the source of ambiguity for management and policy. Aquifer yield has undergone multiple definitions resulting in a range of scientific methods to calculate and model availability reflecting the complexity of combined scientific, management, policy, and stakeholder processes. The concept of an aquifer-yield continuum provides an approach to classify groundwater yields along a spectrum, from non-use through permissive sustained, sustainable, maximum sustained, safe, permissive mining to maximum mining yields, that builds on existing literature. Additionally, the aquifer-yield continuum provides a systems view of groundwater availability to integrate physical and social aspects in assessing management options across aquifer settings. Operational yield describes the candidate solutions for operational or technical implementation of policy, often relating to a consensus yield that incorporates human dimensions through participatory or adaptive governance processes. The concepts of operational and consensus yield address both the social and the technical nature of science-based groundwater management and governance. 相似文献
237.
Integrating economic and groundwater models for groundwater-management can help improve understanding of trade-offs involved between conflicting socioeconomic and biophysical objectives. However, there is significant uncertainty in most strategic decision-making situations, including in the models constructed to represent them. If not addressed, this uncertainty may be used to challenge the legitimacy of the models and decisions made using them. In this context, a preliminary uncertainty analysis was conducted of a dynamic coupled economic-groundwater model aimed at assessing groundwater extraction rules. The analysis demonstrates how a variety of uncertainties in such a model can be addressed. A number of methods are used including propagation of scenarios and bounds on parameters, multiple models, block bootstrap time-series sampling and robust linear regression for model calibration. These methods are described within the context of a theoretical uncertainty management framework, using a set of fundamental uncertainty management tasks and an uncertainty typology. 相似文献
238.
Confirming regional 1 cm differential geoid accuracy from airborne gravimetry: the Geoid Slope Validation Survey of 2011 总被引:3,自引:3,他引:0
Dru A. Smith Simon A. Holmes Xiaopeng Li Sébastien Guillaume Yan Ming Wang Beat Bürki Daniel R. Roman Theresa M. Damiani 《Journal of Geodesy》2013,87(10-12):885-907
A terrestrial survey, called the Geoid Slope Validation Survey of 2011 (GSVS11), encompassing leveling, GPS, astrogeodetic deflections of the vertical (DOV) and surface gravity was performed in the United States. The general purpose of that survey was to evaluate the current accuracy of gravimetric geoid models, and also to determine the impact of introducing new airborne gravity data from the ‘Gravity for the Redefinition of the American Vertical Datum’ (GRAV-D) project. More specifically, the GSVS11 survey was performed to determine whether or not the GRAV-D airborne gravimetry, flown at 11 km altitude, can reduce differential geoid error to below 1 cm in a low, flat gravimetrically uncomplicated region. GSVS11 comprises a 325 km traverse from Austin to Rockport in Southern Texas, and includes 218 GPS stations ( $\sigma _{\Delta h }= 0.4$ cm over any distance from 0.4 to 325 km) co-located with first-order spirit leveled orthometric heights ( $\sigma _{\Delta H }= 1.3$ cm end-to-end), including new surface gravimetry, and 216 astronomically determined vertical deflections $(\sigma _{\mathrm{DOV}}= 0.1^{\prime \prime })$ . The terrestrial survey data were compared in various ways to specific geoid models, including analysis of RMS residuals between all pairs of points on the line, direct comparison of DOVs to geoid slopes, and a harmonic analysis of the differences between the terrestrial data and various geoid models. These comparisons of the terrestrial survey data with specific geoid models showed conclusively that, in this type of region (low, flat) the geoid models computed using existing terrestrial gravity, combined with digital elevation models (DEMs) and GRACE and GOCE data, differential geoid accuracy of 1 to 3 cm (1 $\sigma )$ over distances from 0.4 to 325 km were currently being achieved. However, the addition of a contemporaneous airborne gravity data set, flown at 11 km altitude, brought the estimated differential geoid accuracy down to 1 cm over nearly all distances from 0.4 to 325 km. 相似文献
239.
Kristin Stock Vera Karasova Anne Robertson Guillaume Roger Mark Small Mohamed Bishr Jens Ortmann Tim Stojanovic Femke Reitsma Lukasz Korczynski Boyan Brodaric Zoe Gardner 《Transactions in GIS》2013,17(4):612-639
Current approaches to the discovery of scientific resources (publications, data sets and web services) are dominated by keyword search. These approaches do not allow scientists to search on the deeper semantics of scientific resources, or to discover resources on the basis of the scientific approaches taken. This article evaluates a user interface that allows users to discover scientific resources through structured knowledge in the form of ontologies describing the domain and the scientific knowledge inherent within the scientific resource, and also through informal user tags. These combined capabilities provide scientists with new and powerful options for resource discovery. A qualitative user evaluation explored how scientists felt about the approach for resource discovery in the context of their scientific work. The study showed that marine scientists were enthusiastic about the capabilities of such an approach and appreciated the ability to browse the visual structure of the knowledge and query on scientific method but, overall, preferred the use of tags over ontologies. The exploratory nature of the user study was used to identify future directions for such improvements. 相似文献
240.
Wei Yang Marc Jolivet Guillaume Dupont‐Nivet Zhaojie Guo Zhicheng Zhang Chaodong Wu 《Basin Research》2013,25(2):219-240
The tectonic evolution of the Tian Shan, as for most ranges in continental Asia is dominated by north‐south compression since the Cenozoic India‐Asia collision. However, precollision governing tectonic processes remain enigmatic. An excellent record is provided by thick Palaeozoic – Cenozoic lacustrine to fluvial depositional sequences that are well preserved in the southern margin of the Junggar Basin and exposed along a foreland basin associated to the Late Cenozoic rejuvenation of the Tian Shan ranges. U/Pb (LA‐ICP‐MS) dating of detrital zircons from 14 sandstone samples from a continuous series ranging in age from latest Palaeozoic to Quaternary is used to investigate changes in sediment provenance through time and to correlate them with major tectonic phases in the range. Samples were systematically collected along two nearby sections in the foreland basin. The results show that the detrital zircons are mostly magmatic in origin, with some minor input from metamorphic zircons. The U‐Pb detrital zircon ages range widely from 127 to 2856 Ma and can be divided into four main groups: 127–197 (sub‐peak at 159 Ma), 250–379 (sub‐peak at 318 Ma), 381–538 (sub‐peak at 406 Ma) and 543–2856 Ma (sub‐peak at 912 Ma). These groups indicate that the zircons were largely derived from the Tian Shan area to the south since a Late Carboniferous basin initiation. The provenance and basin‐range pattern evolution of the southern margin of Junggar Basin can be generally divided into four stages: (1) Late Carboniferous – Early Triassic basin evolution in a half‐graben or post‐orogenic extensional context; (2) From Middle Triassic to Upper Jurassic times, the southern Junggar became a passively subsiding basin until (3) being inverted during Lower Cretaceous – Palaeogene; (4) During the Neogene, a piedmont developed along the northern margin of the North Tian Shan block and Junggar Basin became a true foreland basin. 相似文献