全文获取类型
收费全文 | 26115篇 |
免费 | 3905篇 |
国内免费 | 5250篇 |
专业分类
测绘学 | 3354篇 |
大气科学 | 4330篇 |
地球物理 | 6461篇 |
地质学 | 10393篇 |
海洋学 | 3369篇 |
天文学 | 1093篇 |
综合类 | 1863篇 |
自然地理 | 4407篇 |
出版年
2024年 | 111篇 |
2023年 | 307篇 |
2022年 | 780篇 |
2021年 | 972篇 |
2020年 | 1112篇 |
2019年 | 1403篇 |
2018年 | 961篇 |
2017年 | 1264篇 |
2016年 | 1227篇 |
2015年 | 1316篇 |
2014年 | 1641篇 |
2013年 | 1974篇 |
2012年 | 1651篇 |
2011年 | 1753篇 |
2010年 | 1358篇 |
2009年 | 1765篇 |
2008年 | 1731篇 |
2007年 | 1804篇 |
2006年 | 1755篇 |
2005年 | 1369篇 |
2004年 | 1281篇 |
2003年 | 1086篇 |
2002年 | 849篇 |
2001年 | 745篇 |
2000年 | 669篇 |
1999年 | 620篇 |
1998年 | 610篇 |
1997年 | 551篇 |
1996年 | 434篇 |
1995年 | 388篇 |
1994年 | 322篇 |
1993年 | 307篇 |
1992年 | 222篇 |
1991年 | 171篇 |
1990年 | 133篇 |
1989年 | 128篇 |
1988年 | 101篇 |
1987年 | 58篇 |
1986年 | 54篇 |
1985年 | 51篇 |
1984年 | 31篇 |
1983年 | 15篇 |
1982年 | 24篇 |
1981年 | 19篇 |
1980年 | 21篇 |
1978年 | 14篇 |
1977年 | 19篇 |
1976年 | 25篇 |
1973年 | 17篇 |
1971年 | 14篇 |
排序方式: 共有10000条查询结果,搜索用时 343 毫秒
641.
砷的仪器分析方法新进展 总被引:2,自引:0,他引:2
砷是自然界中广泛存在的一种物质在工业,农业,医药等方面应用很广。笔者着重介绍了近几个来砷的仪器分析方法新进展,主要有光度法,电化学法,原子吸收法等。 相似文献
642.
小波分析在地质分形科学中的应用前景 总被引:1,自引:0,他引:1
在概述小波分析在分形研究中的应用原理及在分形构造与结构分析中的一些进展基础上,展望了小波分析在地质分形科学中的应用前景。 相似文献
643.
644.
Li ZhongInstitute of Geology Chinese Academy of Sciences Beijing Sun YongchuanDepartment of Petroleum Geology China University of Geosciences Wuhan 《中国地质大学学报(英文版)》1997,(1)
ReservoirDiagenesisSequenceandFrameworkinIntracontinentRiftBasin,EastChina*LiZhongInstituteofGeology,ChineseAcademyofSciences... 相似文献
645.
DYNAMIC VARIATIONS OF WATER QUALITY IN TAIHU LAKE AND MULTIVARIATE ANALYSIS OF ITS INFLUENTIAL FACTORS 总被引:1,自引:0,他引:1
Cai Qiming Gao Xiyun Chen Yuwei Ma Shengwei Nanjing Institute of Geography Limnology CAS Nanjing People''s Republic of ChinaMartin Dokulil Institute of Limnology Austria 《地理学报(英文版)》1997,(3)
LakeTaihuisalargeshallowlakeinChina,whichpalysanimportantroleinwater-quantityregulation,watersupply,cultivationetc.Withrapiddevelopmentofagricultureandindustryinthearea,alargenumberofpollutantshavebeendischargedintothelake,leadingtoanincreaseinnutrients… 相似文献
646.
Delineation of detailed mantle structure frequently requires the separation of source signature and structural response from seismograms recorded at teleseismic distances. This deconvolution problem can be posed in a log-spectral domain where the operation of time-domain convolution is reduced to an additive form. The introduction of multiple events recorded at many stations leads to a system of consistency equations that must be honoured by both the source time functions and the impulse responses associated with propagation paths between sources and receivers. The system is inherently singular, and stabilization is accomplished through the supply of an initial estimate of the source time function. Although alternative choices exist, an effective estimate is derived from the eigenimage associated with the largest eigenvalue in a singular-value decomposition of the suite of aligned seismograms corresponding to a given event. The relation of the deconvolution scheme to simultaneous least-squares deconvolution is examined. Application of the methodology to broadband teleseismic P waveforms recorded on the Canadian National Seismograph Network demonstrates the retrieval of effective Green's functions including secondary phases associated with upper-mantle structure. 相似文献
647.
Fully normalized spherical cap harmonics: application to the analysis of sea-level data from TOPEX/POSEIDON and ERS-1 总被引:2,自引:0,他引:2
We introduce two sets of fully normalized harmonics for the spectral analysis of functions defined on a spherical cap. The harmonics are the products of Fourier functions and the fully normalized associated Legendre functions of non-integer degree. Using Sturm-Liouville theory for boundary-value problems, we present two convenient and stable formulae for computing the zeros of the associated Legendre functions that form two sets of orthogonal functions. Formulae for the stable numerical evaluation of the fully normalized associated Legendre functions of non-integer degree that avoid the gamma function are also derived. The result from the expansions of sea-level anomaly from altimetry into Set 2 fully normalized cap harmonics shows fast convergence of the series, and the degree variances decay rapidly without aliasing effects. The zero-degree coefficients (Set 2) of sea-level anomaly from TOPEX/ POSEIDON (T/P) and ERS-1 indicate an El Niño event during 1993 January-1993 July, and a La Niño event during 1993 November-1994 July, although the ERS-1 result is less obvious. Ocean circulations over the South China Sea and the Kuroshio area are clearly identified with the low-degree expansions of sea-surface topography (SST) from T/P and ERS-1. A cold-core eddy of 4° in diameter centred at 17.5°N, 118 E was detected with the expansion of SST from T/P cycle 47, and a property of the cap harmonics is used to compute this eddy's kinetic energy. The kinetic energy is at a low in winter and high in summer, and its variation seems to be periodic with an amplitude of 0.4 m2 S-2 . 相似文献
648.
There have been several claims that seismic shear waves respond to changes in stress before earthquakes. The companion paper develops a stress-sensitive model (APE) for the behaviour of low-porosity low-permeability crystalline rocks containing pervasive distributions of fluid-filled intergranular microcracks, and this paper uses APE to model the behaviour before earthquakes. Modelling with APE shows that the microgeometry and statistics of distributions of such fluid-filled microcracks respond almost immediately to changes in stress, and that the behaviour can be monitored by analysing seismic shear-wave splitting. The physical reasons for the coupling between shear-wave splitting and differential stress are discussed.
In this paper, we extend the model by using percolation theory to show that large crack densities are limited at the grain-scale level by the percolation threshold at which interacting crack clusters lead to pronounced increases in rock-matrix permeability. In the simplest formulation, the modelling is dimensionless and almost entirely constrained without free parameters. Nevertheless, APE modelling of the evolution of fluid-saturated rocks under stress reproduces the observed fracture criticality and the narrow range of shear-wave azimuthal anisotropy in crustal rocks. It also reproduces the behaviour of temporal variations in shear-wave splitting observed before and after the 1986, M = 6, North Palm Springs earthquake, Southern California, and several other smaller earthquakes.
The agreement of APE modelling with a wide range of observations confirms that fluid-saturated crystalline rocks are stress-sensitive and respond to changes in stress by critical fluid-rock interactions at the microscale level. This means that the effects of changes in stress and other parameters can be numerically modelled and monitored by appropriate observations of seismic shear waves. 相似文献
In this paper, we extend the model by using percolation theory to show that large crack densities are limited at the grain-scale level by the percolation threshold at which interacting crack clusters lead to pronounced increases in rock-matrix permeability. In the simplest formulation, the modelling is dimensionless and almost entirely constrained without free parameters. Nevertheless, APE modelling of the evolution of fluid-saturated rocks under stress reproduces the observed fracture criticality and the narrow range of shear-wave azimuthal anisotropy in crustal rocks. It also reproduces the behaviour of temporal variations in shear-wave splitting observed before and after the 1986, M = 6, North Palm Springs earthquake, Southern California, and several other smaller earthquakes.
The agreement of APE modelling with a wide range of observations confirms that fluid-saturated crystalline rocks are stress-sensitive and respond to changes in stress by critical fluid-rock interactions at the microscale level. This means that the effects of changes in stress and other parameters can be numerically modelled and monitored by appropriate observations of seismic shear waves. 相似文献
649.
650.
This paper investigates the role of housing age in constraining residential mobility, measured as the percent of households that have moved into their homes in the past 15 months. The leading explanation for why mobility rates differ so much among regions of the United States has been the overall level of growth. The present analysis shows that the growth effect operates through both the newness of population (migration) and the newness of housing available for occupancy by all local residents. The posited explanation for this housing age effect is that progressively older units contain increasingly settled occupants, yielding fewer opportunities for in-movers in areas with older housing. It is empirically demonstrated that households in older housing have lower likelihood of recent mobility even after controlling for age, tenure, migration status, and state location of residence. The analysis reveals the temporal interdependency of mobility, migration, person age, and housing age. 相似文献