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排序方式: 共有195条查询结果,搜索用时 15 毫秒
1.
马尔科夫链蒙特卡洛方法(MCMC)是一种启发式的全局寻优算法,可以用来解决概率反演的问题.基于MCMC方法的反演不依赖于准确的初始模型,可以引入任意复杂的先验信息,通过对先验概率密度函数的采样来获得大量的后验概率分布样本,在寻找最优解的过程中可以跳出局部最优得到全局最优解.MCMC方法由于计算量巨大,应用难度较高,在地球物理反演中的应用尚处于起步阶段.作者将MCMC方法应用到时移探地雷达(GPR)反演中,并结合双差法对时移的目标区域进行准确反演.在双差法时移反演的过程中,作者对目标区域使用拓展的Metropolis算法进行局部采样,减小了计算量的同时,进一步提高了目标区域的反演精度.最后对合成的数据进行了反演测试,对目标区域的反演误差进行了分析,说明了基于局部采样的MCMC反演方法的有效性,目标区域反演结果特征明显,反演效果好. 相似文献
2.
当土体总应力状态保持不变时,基质吸力的提高是导致孔隙水排水、土样体积收缩、孔隙结构改变的根本原因,通过吸力可以将土壤收缩曲线和土水特征曲线联系起来进行比对研究。采用广义有效应力原理分析超固结土样和正常土样的失水过程,结果表明:超固结土样中存在着相应的先期固结压力的吸力值,称之为先期固结吸力ψc。当土样吸力小于ψc时,超固结土样和正常固结土样的收缩曲线、土水特征曲线不同:超固结土孔隙比随吸力提高而减小的坡度较缓,约等于土样的回弹再压缩指数,土样处于结构性收缩阶段;先期固结压力越大,土水特征曲线的进气值越高。当土样吸力高于ψc时,超固结土样和正常固结土样的收缩曲线、土水特征曲线重合。 相似文献
3.
Spatial structure and land use control in Extended Metropolitan Region of Zhujiang River Delta,China 总被引:1,自引:0,他引:1
The Zhujiang (Pearl) River Delta is one of the most developed Extended Metropolitan Regions (EMR) in China.With the rapid urbanization,the agglomeration of population and industries has emerged,which has led to dramatic changes of spatial structure and land use in this region.With data of high resolution TM remote sensing images and Google Earth maps,this paper identified and analyzed the spatial pattern of the Zhujiang River Delta EMR using Envy and ArcGIS tools.It was found that 1) the industrial land uses were expanding substantially,particularly on the bank sides of the Zhujiang River estuary;2) large-scale housing developments were concentrated in the fringe of metropolitan areas such as those of Guangzhou and Shenzhen;3) a regional transportation network with the spatial pattern of ″1 circle +2 pieces + 3 axes″ had significantly affected the location choice of manufacture enterprises.At the same time,both highly specialized land use and severely mixed land use patterns were identified.As a consequence of the latter,land use efficiency of the whole EMR areas was reduced.Moreover,ecologic and environmental problems were severe.Based on the above analysis,suggestions were given from the viewpoint of spatial safety,land use efficiency,and the reorganization of spatial structure in the Zhujiang River Delta EMR. 相似文献
4.
Seismic response of single-column bent on pile: evidence of beneficial role of pile and soil inelasticity 总被引:2,自引:2,他引:0
While seismic codes do not allow plastic deformation of piles, the Kobe earthquake has shown that limited structural yielding
and cracking of piles may not be always detrimental. As a first attempt to investigate the consequences of pile yielding in
the response of a pile-column supported bridge structure, this paper explores the soil–pile-bridge pier interaction to seismic
loading, with emphasis on structural nonlinearity. The pile–soil interaction is modeled through distributed nonlinear Winkler-type
springs and dashpots. Numerical analysis is performed with a constitutive model (Gerolymos and Gazetas 2005a, Soils Found
45(3):147–159, Gerolymos and Gazetas 2005b, Soils Found 45(4):119–132, Gerolymos and Gazetas 2006a, Soil Dyn Earthq Eng 26(5):363–376)
materialized in the OpenSees finite element code (Mazzoni et al. 2005, OpenSees command language manual, p 375) which can
simulate: the nonlinear behaviour of both pile and soil; the possible separation and gapping between pile and soil; radiation
damping; loss of stiffness and strength in pile and soil. The model is applied to the analysis of pile-column supported bridge
structures, focusing on the influence of soil compliance, intensity of seismic excitation, pile diameter, above-ground height
of the pile, and above or below ground development of plastic hinge, on key performance measures of the pier as is: the displacement
(global) and curvature (local) ductility demands and the maximum drift ratio. It is shown that kinematic expressions for performance
measure parameters may lead to erroneous results when soil-structure interaction is considered. 相似文献
5.
Forests are important biomes covering a major part of the vegetation on the Earth, and as such account for seventy percent of the carbon present in living beings. The value of a forest’s above ground biomass (AGB) is considered as an important parameter for the estimation of global carbon content. In the present study, the quad-pol ALOS-PALSAR data was used for the estimation of AGB for the Dudhwa National Park, India. For this purpose, polarimetric decomposition components and an Extended Water Cloud Model (EWCM) were used. The PolSAR data orientation angle shifts were compensated for before the polarimetric decomposition. The scattering components obtained from the polarimetric decomposition were used in the Water Cloud Model (WCM). The WCM was extended for higher order interactions like double bounce scattering. The parameters of the EWCM were retrieved using the field measurements and the decomposition components. Finally, the relationship between the estimated AGB and measured AGB was assessed. The coefficient of determination (R2) and root mean square error (RMSE) were 0.4341 and 119 t/ha respectively. 相似文献
6.
The Wulanmulun site found in 2010 is an important Paleolithic site in Ordos (China), from which lots of stone and bone artifacts and mammalian fossils have been recovered. It was previously dated by radiocarbon and optically stimulated luminescence (OSL) techniques on quartz. To further confirm the reliability of the chronology constructed based on OSL ages and test the applicability of the recently developed pIRIR procedure on sediments from northern China, twenty-four sediment samples (including eolian, lacustrine and fluvio-eolian sands) from the site were determined using the multi-elevated-temperature post-IR IRSL (MET-pIRIR or pIRIR) procedure on potassium feldspar. The results show that the studied samples have two MET-pIRIR De preheat plateaus (280–320 and 340–360 °C), and the bleaching rates of the luminescence signals are associated with sample ages and stimulation temperatures. All the pIRIR ages (7–155 ka) corrected for anomalous fading and residual dose obtained after solar bleaching for 15 h are larger than the corresponding quartz OSL ages (4–66 ka) previously determined, even for the young eolian samples (<10 ka). But the corrected IRSL(50 °C) ages (6–85 ka) are broadly consistent with the quartz ages. It appears that the IRSL(50 °C) ages are more reliable, although this contradicts the previously results obtained by other people. On the other hand, we also obtained an extended age plateau between the stimulation temperatures of 50 and 290 °C in the plot of age versus stimulation temperature (A-T plot) by subtracting different residual doses obtained after different bleaching times. The reliability of the plateau ages requires further investigation. For the sediment samples from this site, quartz should be more suitable for dating than K-feldspar, and the quartz OSL ages of 50–65 ka for its cultural layer should be reliable. 相似文献
7.
利用Java语言,使用Microsoft SQL Server 2005数据库,利用MyEclipse工具研发地震仪器设备管理系统.使用该系统进行台站仪器设备信息管理,便于保存、查询、更新信息,实现数据资料的完整、准确、长期保存,工作效率增加. 相似文献
8.
9.
海洋GIS数据模型与结构 总被引:5,自引:1,他引:4
探讨了海洋 GIS中的数据模型和数据结构问题。根据物理海洋学的研究方法 ,提出了海洋 GIS的数据表达模型。针对海洋 GIS中水体的特点 ,提出了适合海洋 GIS水体的多级化格网型数据结构 ,给出了两种大尺度海洋常用的格网化方案 :全球等角格网化方案和全球等面积格网化方案。这种格网型数据结构是普通 GRID的扩展 ,具有鲜明的海洋数据应用特色。 相似文献
10.
We study the stability of motion in the 3-body Sitnikov problem, with the two equal mass primaries (m
1 = m
2 = 0.5) rotating in the x, y plane and vary the mass of the third particle, 0 ≤ m
3 < 10−3, placed initially on the z-axis. We begin by finding for the restricted problem (with m
3 = 0) an apparently infinite sequence of stability intervals on the z-axis, whose width grows and tends to a fixed non-zero value, as we move away from z = 0. We then estimate the extent of “islands” of bounded motion in x, y, z space about these intervals and show that it also increases as |z| grows. Turning to the so-called extended Sitnikov problem, where the third particle moves only along the z-axis, we find that, as m
3 increases, the domain of allowed motion grows significantly and chaotic regions in phase space appear through a series of
saddle-node bifurcations. Finally, we concentrate on the general 3-body problem and demonstrate that, for very small masses, m
3 ≈ 10−6, the “islands” of bounded motion about the z-axis stability intervals are larger than the ones for m
3 = 0. Furthermore, as m
3 increases, it is the regions of bounded motion closest to z = 0 that disappear first, while the ones further away “disperse” at larger m
3 values, thus providing further evidence of an increasing stability of the motion away from the plane of the two primaries,
as observed in the m
3 = 0 case. 相似文献