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31.
Resolving a low-velocity zone with surface-wave data 总被引:2,自引:0,他引:2
Hendrik Jan van Heijst Roel Snieder Robert Nowack 《Geophysical Journal International》1994,118(2):333-343
32.
Near-surface electromagnetic, rock magnetic, and geochemical fingerprinting of submarine freshwater seepage at Eckernf?rde Bay (SW Baltic Sea) 总被引:1,自引:1,他引:0
Submarine groundwater discharge in coastal settings can massively modify the hydraulic and geochemical conditions of the seafloor.
Resulting local anomalies in the morphology and physical properties of surface sediments are usually explored with seismo-acoustic
imaging techniques. Controlled source electromagnetic imaging offers an innovative dual approach to seep characterization
by its ability to detect pore-water electrical conductivity, hence salinity, as well as sediment magnetic susceptibility,
hence preservation or diagenetic alteration of iron oxides. The newly developed electromagnetic (EM) profiler Neridis II successfully realized this concept for a first time with a high-resolution survey of freshwater seeps in Eckernf?rde Bay
(SW Baltic Sea). We demonstrate that EM profiling, complemented and validated by acoustic as well as sample-based rock magnetic
and geochemical methods, can create a crisp and revealing fingerprint image of freshwater seepage and related reductive alteration
of near-surface sediments. Our findings imply that (1) freshwater penetrates the pore space of Holocene mud sediments by both
diffuse and focused advection, (2) pockmarks are marked by focused freshwater seepage, underlying sand highs, reduced mud
thickness, higher porosity, fining of grain size, and anoxic conditions, (3) depletion of Fe oxides, especially magnetite,
is more pervasive within pockmarks due to higher concentrations of organic and sulfidic reaction partners, and (4) freshwater
advection reduces sediment magnetic susceptibility by a combination of pore-water injection (dilution) and magnetite reduction
(depletion). The conductivity vs. susceptibility biplot resolves subtle lateral litho- and hydrofacies variations. 相似文献
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34.
Armando Molina Gerard Govers Jean Poesen Hendrik Van Hemelryck Bert De Bivre Veerle Vanacker 《Geomorphology》2008,98(3-4):176
A large spatial variability in sediment yield was observed from small streams in the Ecuadorian Andes. The objective of this study was to analyze the environmental factors controlling these variations in sediment yield in the Paute basin, Ecuador. Sediment yield data were calculated based on sediment volumes accumulated behind checkdams for 37 small catchments. Mean annual specific sediment yield (SSY) shows a large spatial variability and ranges between 26 and 15,100 Mg km− 2 year− 1. Mean vegetation cover (C, fraction) in the catchment, i.e. the plant cover at or near the surface, exerts a first order control on sediment yield. The fractional vegetation cover alone explains 57% of the observed variance in ln(SSY). The negative exponential relation (SSY = a × e−b C) which was found between vegetation cover and sediment yield at the catchment scale (103–109 m2), is very similar to the equations derived from splash, interrill and rill erosion experiments at the plot scale (1–103 m2). This affirms the general character of an exponential decrease of sediment yield with increasing vegetation cover at a wide range of spatial scales, provided the distribution of cover can be considered to be essentially random. Lithology also significantly affects the sediment yield, and explains an additional 23% of the observed variance in ln(SSY). Based on these two catchment parameters, a multiple regression model was built. This empirical regression model already explains more than 75% of the total variance in the mean annual sediment yield. These results highlight the large potential of revegetation programs for controlling sediment yield. They show that a slight increase in the overall fractional vegetation cover of degraded land is likely to have a large effect on sediment production and delivery. Moreover, they point to the importance of detailed surface vegetation data for predicting and modeling sediment production rates. 相似文献
35.
Comprehensive Parametrization of Surface-Layer Transfer Coefficients for Use in Atmospheric Numerical Models 总被引:1,自引:0,他引:1
Hendrik Wouters Koen De Ridder Nicole P. M. van Lipzig 《Boundary-Layer Meteorology》2012,145(3):539-550
A new non-iterative bulk parametrization for surface-layer transfer coefficients for momentum and heat is presented. It is applicable for a wide range of aerodynamic and thermal roughness lengths, and includes the effect of the roughness sublayer. As a consequence, the non-iterative method is suitable for every surface type, especially for urban surfaces for which existing non-iterative parametrizations fail. The analytical approximation compares very well with an iterative approach. Our method can be easily implemented in atmospheric numerical models that already employ a non-iterative approach. 相似文献
36.
Hendrik Vogel Bernd Wagner Giovanni Zanchetta Roberto Sulpizio Peter Rosén 《Journal of Paleolimnology》2010,44(1):295-310
Lake Ohrid is probably of Pliocene age, and the oldest extant lake in Europe. In this study climatic and environmental changes
during the last glacial-interglacial cycle are reconstructed using lithological, sedimentological, geochemical and physical
proxy analysis of a 15-m-long sediment succession from Lake Ohrid. A chronological framework is derived from tephrochronology
and radiocarbon dating, which yields a basal age of ca. 136 ka. The succession is not continuous, however, with a hiatus between
ca. 97.6 and 81.7 ka. Sediment accumulation in course of the last climatic cycle is controlled by the complex interaction
of a variety of climate-controlled parameters and their impact on catchment dynamics, limnology, and hydrology of the lake.
Warm interglacial and cold glacial climate conditions can be clearly distinguished from organic matter, calcite, clastic detritus
and lithostratigraphic data. During interglacial periods, short-term fluctuations are recorded by abrupt variations in organic
matter and calcite content, indicating climatically-induced changes in lake productivity and hydrology. During glacial periods,
high variability in the contents of coarse silt to fine sand sized clastic matter is probably a function of climatically-induced
changes in catchment dynamics and wind activity. In some instances tephra layers provide potential stratigraphic markers for
short-lived climate perturbations. Given their widespread distribution in sites across the region, tephra analysis has the
potential to provide insight into variation in the impact of climate and environmental change across the Mediterranean. 相似文献
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39.
A version of the WAVEWATCH III wave model featuring a continuously moving spatial grid is presented. The new model option/version is intended for research into wind waves generated by tropical cyclones in deep water away from the coast. The main advantage of such an approach is that the cyclones can be modeled with spatial grids that cover much smaller areas than conventional fixed grids, making model runs with high spatial resolution more economically feasible. The model modifications necessary are fairly trivial. Most complications occur due to the Garden Sprinkler effect (GSE) and methods used to mitigate it. The basic testing of the model is performed using idealized wind fields consisting of a Rankine vortex. The model is also applied to hurricane Lili in the Gulf of Mexico in October 2002. The latter application shows that the moving grid approach provides a natural way to deal with hurricane wind fields that have a high-resolution in space, but a low resolution in time. Although the new model version is originally intended for tropical cyclones, it is suitable for high-resolution modeling of waves due to any moving weather pattern. 相似文献
40.
Simon D. Carrière Konstantinos Chalikakis Charles Danquigny Hendrik Davi Naomi Mazzilli Chloé Ollivier Christophe Emblanch 《Hydrogeology Journal》2016,24(7):1905-1918
Some portions of the porous rock matrix in the karst unsaturated zone (UZ) can contain large volumes of water and play a major role in water flow regulation. The essential results are presented of a local-scale study conducted in 2011 and 2012 above the Low Noise Underground Laboratory (LSBB – Laboratoire Souterrain à Bas Bruit) at Rustrel, southeastern France. Previous research revealed the geological structure and water-related features of the study site and illustrated the feasibility of specific hydrogeophysical measurements. In this study, the focus is on hydrodynamics at the seasonal and event timescales. Magnetic resonance sounding (MRS) measured a high water content (more than 10 %) in a large volume of rock. This large volume of water cannot be stored in fractures and conduits within the UZ. MRS was also used to measure the seasonal variation of water stored in the karst UZ. A process-based model was developed to simulate the effect of vegetation on groundwater recharge dynamics. In addition, electrical resistivity tomography (ERT) monitoring was used to assess preferential water pathways during a rain event. This study demonstrates the major influence of water flow within the porous rock matrix on the UZ hydrogeological functioning at both the local (LSBB) and regional (Fontaine de Vaucluse) scales. By taking into account the role of the porous matrix in water flow regulation, these findings may significantly improve karst groundwater hydrodynamic modelling, exploitation, and sustainable management. 相似文献