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111.
In the design of a global navigation satellite system receiver, the tracking performance depends on the code tracking loop
and the associated discriminator. An adaptive code discriminator under a multi-correlator architecture has been designed based
on a multi-objective principle to achieve a balance among various, sometimes conflicting, design objectives. With the proposed
optimization approach and adaptive logic, concerns of large pull-in region and small steady-state error can be addressed.
The proposed scheme is implemented in a digital signal processor/field programmable gate array board and an experiment is
conducted to process GIOVE-A signals. The test results reveal the advantages of the proposed code tracking architecture and
discriminator design. 相似文献
112.
GPS Solutions - A self-contained global ionospheric maps (GIM)-aided Abel retrieval method is adopted that can account for spherical non-uniformity along the radio wave path in the vicinity of the... 相似文献
113.
The Pb complexes in a synthetic brine solution with a composition comparable to that of the Atlantis II Deep 56°C Brine have been identified by UV absorption spectroscopy. The important species at ambient temperatures are PbCl2?4 and Pb(OH)BrCl22?. At 56°C the former complex partially dissociates to form lower chloro complexes while the latter undergoes halide exchange reactions forming Pb(OH)Br2Cl2?. Evidence has also been found for the following polymeric lead hydroxo complexes: Pb4(OH)4Cl4, Pb6(OH)3Cl12 and Pb3(OH)12Cl4. The predominant polynuclear complex in the brine, Pb4(OH)4Cl4, tends to dissociate at 56°C to form lower polymeric species. The formulation of the limiting binary chloro complex as PbCl42? rather than PbCl64? is supported by the reflectance spectrum of Cs4PbCl6. 相似文献
114.
115.
Local flow properties and regional weather or climate are strongly affected by land‐atmosphere interactions of momentum and scalars within the daytime convective boundary layer (CBL). In this study, we investigate the impact of green space scale on the daytime atmospheric boundary layer (ABL) over a synthetic urban domain using a recently developed large‐eddy simulation‐land surface model (LES–LSM) framework. With the use of realistic soundings as initial conditions, a series of numerical experiments over synthetic urban surfaces with varied scale of vegetated area is performed. Simulated micrometeorological properties, surface fluxes, basic CBL characteristics, and cloud distribution are analysed. The results show reference‐level air potential temperature and specific humidity as well as surface fluxes over green space are significantly affected by the scale of green space in the urban domain. The surface organization due to vegetated area scale also has impacts on horizontally averaged scalar and momentum profiles; however, the magnitude in this study is smaller than the results of a previous study using a set of offline surface fluxes as the lower boundary condition for LES. In addition, even though this study only performs a daytime diurnal cycle, the impact of green space scale on cloud distribution in simulations is significant. The cases with more organized green space yield lower‐elevated cumulus cloud and larger‐cloud cover fraction, which impacts the energy budget at the top of boundary layer and, in turn, could lead to additional surface cooling with respect to longer‐term weather and climate. Copyright © 2010 John Wiley & Sons, Ltd. 相似文献
116.
The solution describing the wellbore flow rate in a constant‐head test integrated with an optimization approach is commonly used to analyze observed wellbore flow‐rate data for estimating the hydrogeological parameters of low‐permeability aquifers. To our knowledge, the wellbore flow‐rate solution for the constant‐head test in a two‐zone finite‐extent confined aquifer has never been reported so far in the literature. This article is first to develop a mathematical model for describing the head distribution in the two‐zone aquifer. The Laplace domain solutions for the head distributions and wellbore flow rate in a two‐zone finite confined aquifer are derived using the Laplace transform, and their corresponding time domain solutions are then obtained using the Bromwich integral method and residue theorem. These new solutions are expressed in terms of an infinite series with Bessel functions and not straightforward to calculate numerically. A large‐time solution for the wellbore flow rate is therefore developed by employing the relationship of small Laplace variable versus large time variable and L'Hospital's rule. The result shows that the large‐time solution is identical to the steady‐state solution obtained after applying the Tauberian theorem into the Laplace domain solution. This large‐time solution can reduce to the Thiem equation in the case of no skin. Finally, the newly developed solution is used to investigate the effects of outer boundary distance and conductivity ratio on the wellbore flow rate. Copyright © 2011 John Wiley & Sons, Ltd. 相似文献
117.
An-Yi Tsai Gwo-Ching Gong Robert W. Sanders Chien-Fu Chao Kuo-Ping Chiang 《Journal of Oceanography》2010,66(6):873-883
This two-year study investigates the possible factors that determine spatial and temporal dynamics of picoplankton (heterotrophic
bacteria, autotrophic picoplankton—Synechococcus spp., Prochlorococcus, and picoeukaryotes) and nanoflagellate abundance in the subtropical Ilan Bay, Taiwan, where the inner bay is affected by
freshwater run-off from the Lanyang River and the eastern outer bay by the Kuroshio Current. In the inner bay, there was more
rain and freshwater discharge in 2005 than in 2004 during the warm season (>24° C, June–September). The abundance of bacteria,
Synechococcus spp., Prochlorococcus, and picoeukaryotes and the percentage contributions of pigmented nanoflagellate (PNF %) were two- to eight-fold greater
during this period (July in 2005) than for other sampling periods. Relatively low abundance of heterotrophic nanoflagellates
(HNF) in the presence of abundant picoplankton prey suggests that top-down control determined HNF abundance in the Ilan Bay,
Taiwan. 相似文献
118.
Influences of soil water characteristic curve on rainfall-induced shallow landslides 总被引:3,自引:2,他引:1
Tung-Lin Tsai 《Environmental Earth Sciences》2011,64(2):449-459
The analysis of slope instability induced by rainfall was usually performed using the main drying curve as the measurement
of the main wetting curve is a more time-consuming and costly task. In this study, the influences of the main drying and wetting
curves on rainfall-induced shallow landslides are examined. Three designed scenarios and a real case scenario are used to
conduct this examination. The prediction of shallow landslide occurrence is related to the main drying and wetting curves
due to the strong relation between groundwater pressure head and hysteresis effect. The main wetting curve may have a less
minimum landslide-triggering rainfall amount and a less rainfall duration threshold for landslide occurrence than the drying
wetting curve. For safety’s sake, an underestimation of shallow landslide occurrence may be produced by the commonly used
main drying curve. In addition, besides the shallow landslide occurrence, the failure depth and the time to failure are also
influenced by the main drying and wetting curves. The hysteresis effect should be taken into account for assessing rainfall-induced
shallow landslides. 相似文献
119.
Examination of influences of rainfall patterns on shallow landslides due to dissipation of matric suction 总被引:5,自引:4,他引:1
The influences of rainfall patterns on shallow landslides due to the dissipation of matric suction are examined in this study.
Four representative rainfall patterns including the uniform, advanced, intermediated, and delayed rainfalls are adopted. The
results show that not only the occurrence of shallow landslides but also the failure depth and the time of failure are affected
by the rainfall pattern. The different rainfall patterns seem to have the same minimum landslide-triggering rainfall amount.
There is a rainfall duration threshold for landslide occurrence for a rainfall event with larger than the minimum landslide-triggering
rainfall amount. For each rainfall pattern, the rainfall duration threshold for landslide occurrence decreases to constant
with the increase of rainfall amount. The uniform rainfall has the least rainfall duration threshold for landslide occurrence,
followed by the advanced rainfall, and then the intermediated rainfall. For each rainfall pattern, the failure depths and
the times of failure from the same amount of rainfall with different durations could be largely different. In addition, the
differences of the failure depths and the times of failure between various rainfall patterns with the same amount and duration
of rainfall could be also significant. The failure depth and the time of failure, as compared with the occurrence of shallow
landslides, are more sensitive to the rainfall condition. In other words, in comparison with the evaluation of the occurrence
of shallow landslides, it needs more accurate rainfall prediction to achieve reliable estimations of the failure depth and
the time of failure. 相似文献
120.
Peter S. Ross Jay Barlow Thomas A. Jefferson Brendan E. Hickie Tatiana Lee Christina MacFarquhar E. Christien Parsons Kimberly N. Riehl Naomi A. Rose Elisabeth Slooten Chia-Yang Tsai John Y. Wang Andrew J. Wright Shih Chu Yang 《Marine Policy》2011
The adoption of endangered species laws in various nations has intensified efforts to better understand, and protect, at-risk species or populations, and their habitats. In many countries, delineating a portion of a species' habitat as particularly worthy of protection has become a mantra of these laws. Unfortunately, the laws themselves often provide scientists and managers with few, if any, guidelines for how to define such habitat. Conservationists and scientists may view protecting part of the habitat of an endangered species as an ineffectual compromise, while managers may be under pressure to allow a range of human activities within the species' habitat. In the case of small cetaceans, establishing boundaries for such areas can also be complicated by their mobility, the fluid nature of their environment, and the often ephemeral nature of their habitat features. The convergence of multiple human impacts in coastal waters around the world is impacting many small cetaceans (and other species) that rely on these areas for feeding, reproducing, and resting. The ten guiding principles presented here provide a means to characterize the habitat needs of small, at-risk cetaceans, and serve as a basis for the delineation of ‘priority habitat’ boundaries. This conceptual approach should facilitate a constructive discourse between scientists and managers engaged in efforts to recover endangered species. The degree to which the recovery of an at-risk species can be reconciled with sustainable economic activity will depend in part on how well these principles are incorporated into the delineation of priority habitat. 相似文献