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91.
It has been well documented that natural marine Ariake clays are sensitive clays. In this study, extensive data of marine Ariake clays are obtained to investigate the gravitational compression behavior for sensitive clays. Analysis results indicate that the compression behavior of remolded Ariake clays is not different from that of other remolded/reconstituted soils. But natural Ariake clays do not follow the gravitational compression pattern reported by Skempton (1970) for natural sedimentary soils. At a given value of effective overburden pressure, the void ratios of natural Ariake clays are almost independent of liquid limits. Most natural Ariake clays lie above the sedimentation compression line proposed by Burland (1990). When the liquid limit is larger than 90% and the ratio of natural water content over liquid limit ranges 0.8–1.1, the natural Ariake clays lie around the sedimentation compression line. In addition, the natural Ariake clay with higher value of the ratio of natural water content over liquid limit lies above the natural Ariake clay with lower value of the ratio of natural water content over liquid limit. Salt removal is the most probable cause for such a phenomenon. 相似文献
92.
The laboratory model tests and numerical analyses have been performed on reinforced granular piles installed in very soft clay. The granular piles were reinforced with geosynthetic in the form of vertical encasement, horizontal strips and combined vertical-horizontal reinforcement. The short term-displacement control model tests were carried out either only a granular pile loaded or with an entire area loaded. The laboratory results in the form of vertical load intensity-settlement behaviour were compared with that obtained from FEM software, PLAXIS 3D. The results indicated significant improvement in ultimate load intensity and stiffness of treated ground due to inclusion of geosynthetic. 相似文献
93.
This paper focuses on the rate-dependent yield stress, undrained strength, and long-term undrained strength of clay. Various oedometer and triaxial tests were performed on Wenzhou marine clay. The uniqueness of rate-dependent and long-term yield stress and strength is discussed. A new anisotropic elastic viscoplastic model is proposed by adopting the concept of anisotropy and isotropy processes. The determination of model parameters is discussed, demonstrating how all model parameters can be determined in a straightforward way requiring the same basic tests as for the Modified Cam Clay model. Experimental verifications are carried out using the constant strain-rate and creep tests on the Wenzhou marine clay. 相似文献
94.
Sheng-Feng Zou Xin-Yu Xie Zhong-Jin Wang Heng-Yu Wang 《Marine Georesources & Geotechnology》2013,31(6):660-670
AbstractThis paper presents a novel elasto-viscoplastic constitutive formulation based on the isotache concepts and the Nishihara model. Incorporating a novel viscoelastic body to include the delay elastic deformation of marine soft clays under the external load, the proposed model is used to evaluate the theories of consolidation-creep coupling, strain rate dependency and stress relaxation of saturated marine soft clays, and hence, the methodology used to determine the parameters of the model is discussed. Ningbo marine soft clay is selected as an example to interpret the determination of the model parameters on a field scale. A series of conventional oedometer tests are conducted as well. Eventually, we utilize the model to simulate several kinds of rheological tests, including one-dimensional (1-D) long-term compression tests on Ningbo marine soft clays, 1-D constant rate of strain (CRS) tests on Batiscan clays and 1-D stress relaxation tests on Hong Kong marine deposits. These findings indicate good agreement between the computational and experimental results, suggesting the given model can provide reliable forecasts for the rheological characteristics of marine soft clays. 相似文献
95.
Coal mine restoration projects increase public perception of mining companies. Spain has relatively few examples of completed
opencast mine rehabilitation projects. This study seeks to obtain the use of mine spoils from coal mines in Teruel. The studied
mine spoils may be used as raw material for the Spanish ceramic industry, located in the provinces of Castellon, Valencia
and Teruel. This study specifically discusses the mineralogical and geochemical characteristics of the Lower Cretaceous materials
from coal deposits in Estercuel basin, around Teruel and Castellon in Spain. These provinces have a large ceramic industry.
A characterization of mine spoils from coal deposits has been carried out. This characterization is based on the data of both
mineral and chemical analysis. The mineralogical characterization was complemented with SEM/EDAX. The study of the chemical
composition allows the evaluation of the applicability of the studied mine spoils to the following industries: refractory,
fine clay, red clay for pavement and coating, and heavy clay. The clay used for refractory industry has the highest compositional
demand. The positive results obtained on this set of preliminary tests lead us to envisage new research programs, focusing
on testing these mine spoils on a semi-industrial scale. 相似文献
96.
开展了张紧式吸力锚在侧壁最优系泊点处遭受平均荷载和循环荷载共同作用下的模型试验,着重研究了软黏土中吸力锚在等幅及变幅循环荷载下的变形失稳过程。研究发现,循环累积位移过大是锚发生破坏的主要原因。对于等幅循环加载试验,由于竖向附加荷重的施加,锚在水平向的循环累积位移要明显大于竖向,表现为明显的水平破坏模式。在特定的平均荷载水平下,循环荷载水平越高,锚的累积位移发展得越快,达到破坏所需的循环次数就越少。循环位移随循环次数的增长变化不明显,但随循环荷载水平的增大而增大。对于变幅循环加载试验,系泊点各方向的循环累积位移与循环位移均与循环荷载水平成正比。不同的循环加载时程下,锚的竖向累积位移均比水平累积位移大,表现为偏向于竖向破坏的中间破坏模式。锚前期的循环加载历史对后续加载产生的累积变形有明显影响。与静力加载相比,循环加载时锚的运动方向角有所增大,这可能是由于锚底孔压的累积要大于锚侧孔压的累积,从有效应力的角度分析,锚底有效应力的减少相对锚侧明显,进而使得锚竖向承载力减小得更多,导致锚的竖向运动更明显。 相似文献
97.
98.
Landslide phenomena in the area of Pomarico (Basilicata–Italy): methods for modelling and monitoring
F Bozzano C Cherubini M Floris M Lupo F Paccapelo 《Physics and Chemistry of the Earth》2002,27(36):1601-1607
This paper takes into consideration landslide phenomena in the clayey slopes facing the built-up area of Pomarico which is situated in the southern part of the “Fossa Bradanica”, in Basilicata (Italy). Based on the great number of geologic, geomorphologic and historic informations a geotechnical model of the slope was built. Particular attention has been paid to define the geotechnical parameters of the soil and which mechanical models are to be used. The studies point out a correlation between the water level in the detritus cover and the stability condition of the slope showing that phenomena at first located at the foot of the slope spread quickly towards its summit as the piezometric height increases. 相似文献
99.
Jacques Yvon Jean-Maurice Cases Frédéric Villiéras Laurent Michot Fabien Thomas 《Comptes Rendus Geoscience》2002,334(9):717-730
By nature minerals are heterogeneous materials for many of their properties. These properties also vary according to composition and structure fluctuations, compared to definitions. Technical minerals are used in applications where their performances depend on intrinsic properties and processing conditions. It is possible to base rankings on simple criteria, allowing estimating the abilities of minerals for each utilisation. The research of the corresponding mechanisms concerns the molecular level. These questions are discussed for kaolins, raw materials for baked clays, talqueous materials and montmorillonites. To cite this article: J. Yvon et al., C. R. Geoscience 334 (2002) 717–730. 相似文献
100.
Luis Martinez Joëlle Duplay Isabel Suarez-Ruiz Jean Robert Disnar Geneviève Farjanel Philippe Larqué Nicole Liewig 《Comptes Rendus Geoscience》2002,334(14):1021-1028
Two wells, Balazuc (BA1) and Morte-Mérie (MM1), located in a confined area (1200 m apart) and separated by the Uzer fault (a Liassic structure with a dip fault of 1300 m) were analysed using conventional methodologies and techniques (PRV, TAI, XRD, STEM) in order to compare the diagenetic evolution of clays and organic matter. The thermal convective process allows the circulation of hot fluids and the oxidation of organic matter. The conductive process allows the maturation of the organic matter, the expulsion of hydrocarbons and the deposit of pyrobitumes in the migration channels. To cite this article: L. Martinez et al., C. R. Geoscience 334 (2002) 1021–1028. 相似文献