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101.
With deep mining of coal mines, prospecting multilayer water-filled goaf has become a new content that results from geophysical exploration in coalfields. The central loop transient electromagnetic (TEM) method is favorable for prospecting conductive layers because of the coupling relationship between its field structure and formation. However, the shielding effect of conductive overburden would not only require a longer observation time when prospecting the same depth but also weaken the anomalous response of underlying layers. Through direct time domain numerical simulation and horizontal layered earth forward modeling, this paper estimates the length of observation time required to prospect the target, and the distinguishable criterion of multilayer water-filled goaf is presented with observation error according to the effect of noise on observation data. The observed emf curves from Dazigou Coal Mine, Shanxi Province can distinguish multilayer water-filled goaf. In quantitative inversion interpretation of observed curves, using electric logging data as initial parameters restrains the equivalence caused by coal formation thin layers. The deduced three-layer and two-layer water-filled goafs are confirmed by the drilling hole. The result suggests that when observation time is long enough and with the anomalous situation of underlying layers being greater than the observation error, the use of the central loop TEM method to prospect a multilayer water-filled goaf is feasible. 相似文献
102.
Chen Qiu 《中国海洋湖沼学报》1986,4(4):372-378
Acetes chinensis always ovulate in the dark at night. Two to five hours before ovulation, the mature oocytes change from white
to orange. In the meantime, meiosis of the oocytes occurs, and reaches the metaphase just prior to ovulation. If ovarian colour
change starts in the dark at night but ovulation does not start by break of dawn, ovulation will be inhibited and meiosis
of the cells will be blocked. 相似文献
103.
Some-geological problems and solid-liquid equilibria in petrogenetic processes are discussed in the light of olivine chemistry
based on 278 analyses of Cenozoic basalts and inclusions therefrom in eastern China. Prospective implications of these results
have also been evaluated. 相似文献
104.
A numerical model, called CCPF1 (C onsolidation with C ompressible P ore F luid 1 ), is presented for one‐dimensional large strain consolidation of a saturated porous medium with compressible pore fluid. The algorithm includes all the capabilities of a previous large strain consolidation code, CS2, written for incompressible pore fluid. In addition, fluid density and fluid viscosity are functions of fluid pressure in CCPF1. Generalization of the numerical approach to accommodate these functions requires several modifications to the CS2 method, including phase relationships, intrinsic permeability, pore pressure, fluid potential, and mass flux. Inertial forces are neglected and isothermal conditions are assumed. The development of CCPF1 is first presented, followed by an example that illustrates the effects of pore fluid compressibility on the mechanics of consolidation of saturated porous media. Copyright © 2004 John Wiley & Sons, Ltd. 相似文献
105.
106.
Maria D. Kazachenko Richard C. Canfield Dana W. Longcope Jiong Qiu 《Solar physics》2012,277(1):165-183
In order to better understand the solar genesis of interplanetary magnetic clouds (MCs), we model the magnetic and topological
properties of four large eruptive solar flares and relate them to observations. We use the three-dimensional Minimum Current Corona model (Longcope, 1996, Solar Phys.
169, 91) and observations of pre-flare photospheric magnetic field and flare ribbons to derive values of reconnected magnetic
flux, flare energy, flux rope helicity, and orientation of the flux-rope poloidal field. We compare model predictions of those
quantities to flare and MC observations, and within the estimated uncertainties of the methods used find the following: The
predicted model reconnection fluxes are equal to or lower than the reconnection fluxes inferred from the observed ribbon motions.
Both observed and model reconnection fluxes match the MC poloidal fluxes. The predicted flux-rope helicities match the MC
helicities. The predicted free energies lie between the observed energies and the estimated total flare luminosities. The
direction of the leading edge of the MC’s poloidal field is aligned with the poloidal field of the flux rope in the AR rather
than the global dipole field. These findings compel us to believe that magnetic clouds associated with these four solar flares
are formed by low-corona magnetic reconnection during the eruption, rather than eruption of pre-existing structures in the
corona or formation in the upper corona with participation of the global magnetic field. We also note that since all four
flares occurred in active regions without significant pre-flare flux emergence and cancelation, the energy and helicity that
we find are stored by shearing and rotating motions, which are sufficient to account for the observed radiative flare energy
and MC helicity. 相似文献
107.
108.
This study proposes a knowledge-based, computerized method to develop an initial sinkhole database as a basis for subsequent field investigation to improve on the established database. The knowledge-based data analysis represents sinks (i.e., topographic depressions) as isolines and associates them with contextual land use, land cover, and hydrologic information relevant to potential sinkhole hazard. Sinks of high priority for subsequent field investigation are identified based on combinations of contextual attributes. The proposed methodology for knowledge-based development of a preliminary sinkhole database is valuable for hazard planning and management. 相似文献
109.
Saline water intrusion and its influence in the Laizhou area 总被引:1,自引:0,他引:1
ImODUcrIONSalinewaterintrusionwasfoundinIsraelqacobsetal.,l96O),Thailand(Sun,l989),Spain(Custodi0,l985)andtheFujiarea,Japan"'InChina,thelargescaleseawaterintru-sioninthelasttwentyyearshasgtaduallyforrneserious,totheextentthattheintrusionareanachedto4OO~5OOkm2inthecoastalareaofShandongProvince(Zha0,l99l,Xueetal.,l992,Qiu,l991).Thereareaisos0mesmallaff~areasinLia0dongPenin-sulaandthesouthcoastareaofChina,lbrexamPle,SubeiPlain(Zhouetal.,l988),GuangxiOi,l988;Chenetal.,l99O)andHainan-… 相似文献
110.
河西地区的植被资源由于人们对它开发利用和管理不当已产生了明显的衰退, 例如: 森林植被资源、灌丛植被资源、草原植被资源分布面积的缩小和质量的下降, 荒漠植被资源变得愈来愈稀少, 草甸植被资源产生明显的衰退以至植物大量死亡, 等等。为了改善河西地区植被资源的质量和防止衰退, 必须对它进行合理利用、治理和保护, 积极种草种树, 合理地利用, 严禁乱砍滥伐和毁草毁林开荒, 适当进行封育和建立自然保护区等措施。 相似文献