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311.
Influence of rock types and structures in the development of drainage network in hard rock area 总被引:6,自引:0,他引:6
Remote sensing techniques has proved to be an extremely useful tool in morphometric analysis and groundwater studies. Remote
sensing techniques with an emphasis on lineament identifications can play a great role in groundwater prospecting in semi-arid
hard rock areas of Purulia district. In the present study, morphometric analysis using remote sensing technique has been carried
out in parts of Baghmundi block, Purulia district, West Bengal. The parameters worked out include Bifurcation ratio (Rb), Stream length (Lu), Form factor (Rc), Circulatory ratio (Rc), and Drainage density (D). The morphometric analysis suggests that fractured, resistant, permeable rocks cover the area,
the drainage network not so affected by tectonic disturbances. Using satellite imageries of two dates of IRS, different hydrogeomorphological
units have been delineated. Among different hydrogeomorphic units (i) very shallow weathered pediment and (ii) Structural
hills/ residual hills/inselbergs have very poor ground water prospects, while moderately weathered pediplains and valley fills
are good prospective zones for groundwater exploration. 相似文献
312.
Arun Chakraborty H. C. Upadhyaya O. P. Sharma Divya Jaisawal S. K. Deb 《Meteorology and Atmospheric Physics》2003,83(3-4):197-220
Summary ?A three-dimensional Ocean General Circulation Model has been developed in stretched coordinate from scratch. The same model
has been used to perform some numerical experiments to simulate the basic circulation pattern and the model variability to
atmospheric forcing. For numerical simulations 72 × 25 grid points in the horizontal directions and nine (10, 30, 75, 250,
500, 1000, 1500, 2000 and 3000 m) vertical levels are considered. The lateral boundaries are set at 60° N and 60° S. The basic
focus of the paper is on the demonstration of the performance of the model and its assessment by employing appropriate forcing
from the outputs of an atmospheric general circulation model. Hence, the model was forced with the forcing (wind and thermodynamic)
derived from the ECMWF runs from the AMIP archives. The preliminary results show the realistic simulation of basic pattern
of different fields. The model simulations show that the model is able to reproduce some of the general features of the ocean,
such as surface currents, surface temperature and salinity, mass transport and meridional heat transport. It is also to be
noted that the model is capable to capture the El-Ni?o and La-Ni?a type events.
Received April 3, 2002; revised June 6, 2002; accepted July 24, 2002
Published online: February 20, 2003 相似文献
313.
N. K. Patel M. Chakraborty S. Dutta C. Patnaik J. S. Parihar S. C. Moharana A. Das B. K. Sarangi G. Behera 《Journal of the Indian Society of Remote Sensing》2004,32(2):125-143
Considering the requirement of multiple pre-harvest crop forecasts, the concept of Forecasting Agricultural output using Space,
Agrometeorology and Land based observations (FASAL) has been formulated. Development of procedure and demonstration of this
technique for four in-season forecasts for kharif rice has been carried out as a pilot study in Orissa State since 1998. As
the availability of cloud-free optical remote sensing data during kharif season is very poor for Orissa state, multi-date
RADARSAT SCANSAR data were used for acreage estimation of kharif rice. Meteorological models have been developed for early
assessment of acreage and prediction of yield at mid and late crop growth season. Four in-season forecasts were made during
four kharif seasons (1998-2001); the first forecast of zone level rice acreage at the beginning of kharif crop season using
meteorological models, second forecast of district level acreage at mid growth season using two-date RADARSAT SCANSAR data
and yield using meteorological models, third forecast at late growth season of district level acreage using three-date RADARSAT
SCANSAR data and yield using meteorological models and revised forecast incorporating field observations at maturity. The
results of multiple forecasts have shown rice acreage estimation and yield prediction with deviation up to 14 and 11 per cent
respectively. This study has demonstrated the potential of FASAL concept to provide inseason multiple forecasts using data
of remote sensing, meteorology and land based observations. 相似文献
314.
Literature review underlines uncertainty in the configuration of the Neoproterozoic supercontinent, (with Rodinia and Palaeopangaea reconstructions enjoying wide support), that stems primarily from inadequate palaeomagnetic data. Nonetheless, breakup of this supercontinent at ca. 0.65 Ga was conducive for epeiric sea formation globally. In the Vindhyan basin, India, a carbonate depositing sea developed over a fluvial-aeolian plain, at approximately 0.6 Ga. The top part of the Vindhyan Supergroup, the Upper Bhander Sandstone, was, however, able to prograde because of a decline in the rate of relative sea level rise. Within this general setting, temporal increases in this rate caused storm deposition at the coastline, largely in a supralittoral setting. Bizarre amalgamation of these storm beds without erosion likely owes its origin to severe curtailment of the velocity of the downwelling flow on the very gentle, muddy coastal slopes, and is thought to be a hallmark of deposition in an open epeiric setting. The storm domination in the Bhander embayment shelf is compatible with the Palaeopangaea supercontinental configuration. 相似文献
315.
In this paper we discuss the particle trajectories in a uniform magnetic field superimposed on Kerr geometry. The rotation axis of the Kerr black hole makes an angle with the asymptotic magnetic field. We find that the particle is trapped for suitable initial conditions. 相似文献
316.
K. R. Chakraborty 《Contributions to Mineralogy and Petrology》1977,65(1):101-110
The methods used by earlier workers for evaluating material balance in core-mantle-matrix type differentiated systems are examined in detail. It is demonstrated that these methods can be successfully employed only when the true core-mantle volume ratio is known. On geometric grounds, it is rarely possible to have a reliable estimate of this ratio from natural specimen. Consequently, the scope of balance evaluation by these methods is severely restricted. From theoretical consideration of mass transfer relations in differentiated systems, a new computational method is proposed that can be effectively employed for quantitative balance evaluation without any prior knowledge of the core-mantle volume ratio provided the chemical analyses of the core, mantle and matrix are available. This method involves the application of the following mass balance equation: $$m_1 x_1^i + m_2 x_2^i = m_0 x_0^i {\text{ (}}i = {\text{1,2}}...{\text{,}}n{\text{)}}$$ where m 1 and m 2 are the mass of the core and mantle respectively, m 0 is the mass of the matrix involved in differentiation, and x 1 i , x 2 i , x 0 i are the weight fractions of the component i in the core, mantle and matrix respectively. This method would also permit a quantitative estimation of the materials added to or removed from the system. Three differentiated systems previously investigated by Mehnert (1951, 1968), Loberg (1963) and Kretz (1966) are selected for balance evaluation by the proposed method and the results are compared with the published balance analyses. 相似文献
317.
We present new experimental data on diffusion of divalent cations in almandine-spessartine diffusion couples in graphite capsules in the P-T range of 14–35 kb, 1100–1200° C. The tracer diffusion coefficients of the major divalent cations, viz. Fe, Mg and Mn, retrieved from the multicomponent diffusion profiles, have been combined with earlier data from our laboratory at 29–43 kb, 1300–1480° C (Loomis et al. 1985) to derive expressions of the P-T dependence of the diffusion coefficients at fO2 approximately corresponding to that defined by equilibrium in the system graphite-O2. We review the conditions, discussed earlier by Cooper, under which the flux of a component in a multicomponent system becomes proportional to its concentration gradient (Fickian diffusion), as if the entire solvent matrix behaves as a single component, and also suggest a method of incorporating the thermodynamic effect on diffusion in the same spirit. Regardless of the magnitude or sign of the off-diagonal terms of the D matrix, it is always possible to define an effective binary diffusion coefficient (EBDC) of a component in a semi-infinite multicomponent diffusion-couple experiment such that it has the property of the Fickian diffusion coefficient, provided that there is no inflection on the diffusion profiles. It is shown that the success of Elphick et al. in fitting the experimental diffusion profiles of all components over a limited concentration range by a single diffusion coefficient is due to fortuitous similarity of the EBDCs of the components (Fe, Mg, Mn and Ca) in their diffusion couple experiments. In common metapelitic garnets showing compositional zoning, the EBDCs of the divalent cations do not differ from each other by more than a factor of 2.5. However, the EBDC of a component changes from core to rim by a factor of 3 to 12, depending on the composition. We suggest a method of volume averaging of the EBDC which should prove useful in approximate calculations of diffusion flux during relaxation of compositional zoning. The EBDC of Mn is found to reduce essentially to D
MnMn, the main diagonal term of the D matrix, and consequently can be calculated quite easily. Evaluation of EBDC of Fe, Mg and Mn in garnets from a prograde Barrovian sequence did not reveal any significant dependence on the extent of relaxation of garnet. The diffusion data have been applied to calculate the cooling rate of natural biotite-garnet diffusion couple from eastern Finland and diffusional modification of growth zoning in garnet in early Proterozoic Wopmay orogen, Canada. The results are in good agreement with geochronological and other independent constraints.Symbols and abbreviations
a
Radius of a spherical garnet crystal
-
BSE
Back-scattered electron imaging
-
C
Column vector of (n-1) independent components
-
D
Diffusion coefficient matrix
-
D
ij
An element of the diffusion matrix on the i th row and j th column
-
D
*
i
Tracer diffusion coefficient of component i
-
D(i)
Effective interdiffusion coefficient (EIC) of various components in a multicomponent solution rich in the component i
-
D(i-j)
Interdiffusion coefficient of components i and j in a binary solution
-
D
i
(EB)
Effective binary diffusion coefficient of component i in a multicomponent solution
-
D
i
(EB:Ideal)
D
i
(EB) under condition of ideal thermodynamic mixing of the diffusing species
-
D
i
(EB:thermo)
Thermodynamic component of D
i(EB)
-
D
O
A
Interdiffusion coefficient at peak temperature T
0 in the phase A
-
D
0
Pre-exponential factor in an Arrhenius relation
-
EBDC
Effective binary diffusion coefficient between a solute and a multicomponent solvent matrix
-
FEC
Fixed edge composition model
-
EIC
Effective interdiffusion coefficient
-
f
i
Fugacity of component i
-
HM
Hematite-magnetite oxygen fugacity buffer
- kb
Kilobars
-
P
Pressure
-
Q
Activation energy (enthalpy) of diffusion
-
Extent of relaxation defined as the difference between core and rim compositions normalized to the same difference in the initial zoning profile
-
R
Gas constant
-
s
Cooling rate
-
T
0, T
Ch
Peak temperature and characteristic temperature, respectively
-
t
Time
-
VEC
Variable edge composition model
- V
+
Activation volume
-
W
ij
Simple mixture interaction parameter between i and j
-
W
i(EB)
Effective simple mixture interaction parameter of a component i in a multicomponent solution
-
ij
Margules interaction parameter between i and j
-
X
i
Mole fraction of component i
- i
Activity coefficient of component i
-
A dimensionless variable =D t/a
2
-
ij
Kronecker delta (i=j,
ij
=1; ij,
ij
=0)
- Zi
Charge on the ion i 相似文献
318.
In this work the junction conditions between the exterior Reissner-Nordstrom-Vaidya space-time with the interior quasi-spherical
Szekeres space-time have been studied for analyzing gravitational collapse in the presence of a magneto-hydrodynamic fluid
undergoing dissipation in the form of heat flow. We have discussed about the apparent horizon and have evaluated the time
difference between the formation of apparent horizon and central singularity.
相似文献
319.
The feasibility of an artificial neural network based approach is investigated to estimate the values of mean grain size of
seafloor sediments using four dominant echo features, extracted from acoustic backscatter data. The acoustic backscatter data
were collected using a dual-frequency (33 and 210 kHz) single-beam, normal-incidence echo sounder at twenty locations in the
central part of the western continental shelf of India. Statistically significant correlations are observed between the estimated
average values of mean grain size of sediments and the ground-truth data at both the frequencies. The results indicate that
once a multi-layer perceptron model is trained with back-propagation algorithm, the values of mean grain size can reasonably
be estimated in an experimental area. The study also revealed that the consistency among the estimated values of mean grain
size at different acoustic frequencies is considerably improved with the neural network based method as compared to that with
a model-based approach. 相似文献
320.
Vijay Kumar Kalyani Amalendu Sinha Pallavika Swapan Kumar Chakraborty N. C. Mahanti 《Acta Geophysica》2008,56(4):1074-1089
Reported in the present paper are the results of the study of propagation of SH waves in the plane of mirror symmetry of a monoclinic multilayered medium with displacement normal to the plane. Dispersion equation has been obtained analytically ussing Haskell’s matrix method, while the finite-difference method has been employed to model the SH-wave propagation to study its phase and group velocities. The stability analysis has been carried out to minimize the exponential growth of the error of finite difference approximation in order to make the finite difference method stable and convergent. Further, variations of phase velocity with respect to both wave number and dispersion parameter for different stability ratios in monoclinic media have been examined and shown graphically. The effect of change of stability ratio on the group velocity of the wave propagation has been also investigated. Likewise, the effects of change of dispersion parameter on phase velocity and the variation of frequency with increase of wave number have been graphically represented and discussed. 相似文献