首页 | 本学科首页   官方微博 | 高级检索  
文章检索
  按 检索   检索词:      
出版年份:   被引次数:   他引次数: 提示:输入*表示无穷大
  收费全文   641篇
  免费   103篇
  国内免费   136篇
测绘学   69篇
大气科学   140篇
地球物理   166篇
地质学   260篇
海洋学   112篇
天文学   54篇
综合类   53篇
自然地理   26篇
  2024年   7篇
  2023年   27篇
  2022年   60篇
  2021年   50篇
  2020年   29篇
  2019年   37篇
  2018年   9篇
  2017年   17篇
  2016年   45篇
  2015年   22篇
  2014年   30篇
  2013年   17篇
  2012年   26篇
  2011年   39篇
  2010年   35篇
  2009年   39篇
  2008年   59篇
  2007年   36篇
  2006年   41篇
  2005年   38篇
  2004年   24篇
  2003年   31篇
  2002年   23篇
  2001年   25篇
  2000年   23篇
  1999年   25篇
  1998年   13篇
  1997年   8篇
  1996年   7篇
  1995年   5篇
  1994年   7篇
  1993年   7篇
  1992年   7篇
  1991年   1篇
  1990年   3篇
  1989年   1篇
  1988年   2篇
  1987年   1篇
  1985年   1篇
  1984年   1篇
  1981年   1篇
  1976年   1篇
排序方式: 共有880条查询结果,搜索用时 15 毫秒
841.
数据融合是增强纹理处理的一种方法,是土地利用动态变化监测的重要基础,针对不同的应用目的与数据源应选择不同的融合算法。该文针对IRS-P5/P6影像在土地利用动态遥感监测中的应用,分别应用乘积法、Brovey变换、HIS变换3种常规的融合方法进行了融合试验,并对融合质量从目视分析和定量分析2个方面进行了比较,认为HIS变换比较适合于IRS-P5/P6影像数据的融合。  相似文献   
842.
孙迪  冯乔  刘震  卢朝进  夏鲁 《地质学报》2017,91(11):2521-2544
由于构造位置的特殊性和勘探开发工作的局限性,鄂尔多斯盆地西南部上三叠统延长组6段的物源分析一直存在较大的分歧。本文选取鄂尔多斯盆地西南部里78井、庄33井、演40井以及汭水河地区上三叠统长6段砂岩为研究对象,运用LA-ICP-MS U-Pb方法对样品中的碎屑锆石进行了年代学研究。结果表明,4个样品都存在250~350 Ma、400~660 Ma、920~1200 Ma、1750~1950 Ma和2200~2600 Ma 5个基本相近的年龄区间,与之对应的峰值年龄主要集中在284~330 Ma、430~460 Ma、950~1000 Ma、1850~1915 Ma以及2250~2450Ma。通过与邻区碎屑锆石年龄分布特征对比并结合重矿物资料,对研究区长6段物源的方向、母岩时代及岩性进行了系统全面的分析,认为研究区物源具有多方向、多时期、多岩石类型的特点,主要来自于盆地西南缘、南缘分布的北秦岭西段、北祁连东段及西秦岭的加里东期岩浆岩、晋宁期岩体和位于盆地东北部的古元古代孔兹岩系,盆地西北缘阿拉善地块的华力西期岩浆岩、鄂尔多斯地块东南部的变质基底也提供了部分物源。这一研究结果将有助于进行原盆沉积环境的恢复和指导下一步油气勘探的部署。  相似文献   
843.
Elizabeth B. Oswald  Ellen Wohl   《Geomorphology》2008,100(3-4):549-562
A jökulhlaup burst from the head of Grasshopper Glacier in Wyoming's Wind River Mountains during early September 2003. Five reaches with distinct sedimentation patterns were delineated along the Dinwoody Creek drainage. This paper focuses on a portion of the jökulhlaup route where erosion of the forested banks created 16 large logjams spaced at longitudinal intervals of tens to hundreds of meters. Aggradation within the main channel upstream from each logjam created local sediment wedges, and the jams facilitated overbank deposition during the jökulhlaup. Field surveys during 2004 and 2006 documented logjam characteristics and associated erosional and depositional features, as well as initial modification of the logjams and flood deposits within the normal seasonal high-flow channel. Overbank deposits have not been altered by flows occurring since 2003. Field measurements supported three hypotheses that (i) logjams present along the forested portions of the jökulhlaup route are larger and more closely spaced than those along adjacent, otherwise comparable stream channels that have not recently experienced a jökulhlaup; (ii) logjams are not randomly located along the jökulhlaup route, but instead reflect specific conditions of channel and valley geometry and flood hydraulics; and (iii) the presence of logjams facilitated significant erosional and depositional effects. This paper documents a sequence of events in which outburst floodwaters enhance bank erosion and recruitment of wood into the channel, and thus the formation of large logjams. These logjams sufficiently deflect flow to create substantial overbank deposition in areas of the valley bottom not commonly accessed by normal snowmelt peak discharges, and through this process promote valley-bottom aggradation and sediment storage. Changes in the occurrence of glacier outburst floods thus have the potential to alter the rate and magnitude of valley-bottom dynamics in these environments, which is particularly relevant given predictions of worldwide global warming and glacial retreat. Processes observed at this field site likely occur in other forested catchments with headwater glaciers.  相似文献   
844.
Study On Development And Application Of A Regional Pbl Numerical Model   总被引:9,自引:0,他引:9  
A regional scale (a few km to a few hundred km, minutes to days)planetary boundary layer (PBL) numerical model (RPBLM) has been successfully developed to simulateprecisely the boundary-layer three-dimensional characteristics. The RPBLM model with a high-resolutionnon-hydrostatic E - turbulence closure scheme has been applied to diagnose and prognosticate the PBL characteristicsover a complex underlying surface in the Hong Kong area of 60 km × 48 km. It is shown that the RPBLMmodel can be used to simulate the PBL characteristics including wind, temperature, water vapour andturbulence over such a complex underlying surface and that the simulated result is reasonably in agreementwith observations.  相似文献   
845.
在十二烷基硫酸钠存在下,于pH48~74的缓冲溶液中,2_〔2_(6_甲基苯并噻唑)偶氮〕_5_二乙氨基苯甲酸(6_Me_BTAEB)与Co(Ⅱ)发生显色反应,形成稳定的蓝紫色络合物,其组成为nCo(Ⅱ)∶n6_Me_BTAEB=1∶2,最大吸收波长为650nm,ε为138×105L·mol-1·cm-1,Co(Ⅱ)质量浓度在0~032mg/L时服从比尔定律。方法可直接用于维生素B12和含钴分子筛中微量Co(Ⅱ)的测定,结果与原子吸收法相符。对于w(Co)=0.82%的含钴分子筛测定8次,其RSD为134%。  相似文献   
846.
It is demonstrated that the blind deconvolution method is fully capable of recovering the unknown Greens function and of estimating the source time functions from observed seismic data of small earthquakes. Based on the assumption of the Gaussian-mixture model of the Greens function, the newly-formulated algorithm is evaluated using synthetic seismic data along with those of the May 8, 1996 Mexico earthquake (Mc = 4.6). Since the estimated results closely match the theoretical input very well, the method is then employed to analyze the source time functions of the July 7, 1995 Pu-Li, Taiwan earthquake (ML = 5.3). The stations triggered by this event were azimuthally well covered. Using the estimated source time functions, information pertaining to the directivity effect is readily obtained, and the actual fault plane of this event is identified, thus clearly indicating that this method provides a most efficient way to estimate the source time function of a small earthquake.Acknowledgment The authors would like to express their thanks to two anonymous reviewers for their valuable suggestions and Dr. I. Santamarias courteous assistance. They also appreciate the efforts of Drs. H.C. Chiu and R.J. Rau, who provided the seismic data and the fault plane solutions. The National Science Council, Taiwan, has supported this research (NSC 91-2119-M-194-011).  相似文献   
847.
We present XMM-Newton European Photon Imaging Camera (EPIC) observations of the bright Seyfert 1 galaxy MCG–6-30-15, focusing on the broad Fe K α line at ∼6 keV and the associated reflection continuum, which is believed to originate from the inner accretion disc. We find these reflection features to be extremely broad and redshifted, indicating an origin in the very central regions of the accretion disc. It seems likely that we have caught this source in the 'deep minimum' state first observed by Iwasawa et al. The implied central concentration of X-ray illumination is difficult to understand in any pure accretion disc model. We suggest that we are witnessing the extraction and dissipation of rotational energy from a spinning black hole by magnetic fields connecting the black hole or plunging region to the disc.  相似文献   
848.
Chayes' t-test for closure correlations is developed from various approximations and assumptions. The empirical behavior of this test is observed through the use of random-sampling number matrices of order to thirteen. The experiments demonstrate a lower limit for the reliability of Chayes' model of about 91/100. That is, about one chance in ten remains that an error due to the statistical testing is committed on some product-moment correlations in a given matrix of correlation, given a confidence level of 90 percent. With increase in the number of variables, the test for departure from zero correlation can be used provided the sample size remains small.  相似文献   
849.
The optical properties and spatial distribution of chromophoric dissolved organic matter (CDOM) in Meiliang Bay of Lake Taihu were evaluated and compared to the results in literature. Concentrations of dissolved organic carbon (DOC) ranged from 8.75 to 20.19 mg L?1 with an average of (13.10 ± 3.51) mg L?1. CDOM absorption coefficients a(λ) at 280 nm, 355 nm, and 440 nm were in the range 11.28...33.46 m?1 (average (20.95 ± 5.52) m?1), 2.42...7.90 m?1 (average (4.92 ± 1.29) m?1), and 0.65...2.44 m?1 (average (1.46 ± 0.44) m?1), respectively. In general, CDOM absorption coefficient and DOC concentration were found to decrease away from the river inflow to Meiliang Bay towards the lake center. The values of the DOC‐specific absorption coefficients a*(λ), given as absorption coefficient related to mass concentration of organic carbon (C) ranged from 0.28 to 0.47 L mg?1 m?1 at 355 nm. The determination coefficients between CDOM absorption and DOC concentration decreased with the increase of wavelength from 280 to 550 nm. The linear regression relationship between CDOM absorption at 280 nm and DOC concentration was following: a(280 nm) = 1.507 L mg?1 m?1 · DOC + 1.215 m?1. The spectral slope S values were dependent on the wavelength range used in the regression. The estimated S values decreased with increasing wavelength range used. A significant negative linear relationship was found between CDOM absorption coefficients, DOC‐specific absorption coefficients and estimated S values especially in longer wavelength range. The linear regression relationship between DOC‐specific absorption coefficients at 440 nm and estimated S values during the wavelength range from 280 to 500 nm was following: a*(440 nm) = (–0.021 μm · S + 0.424) L mg?1 m?1.  相似文献   
850.
针对HY-1A CCD数据处理的瑞利查找表   总被引:6,自引:1,他引:6  
孙凌  张杰  郭茂华 《遥感学报》2006,10(3):306-311
在海洋水色遥感中,瑞利散射占大气顶(TOA)处测量信号的绝大部分,作为大气修正的第一步,必须精确计算瑞利散射的贡献,并从总信号中去除.本文针对HY-1A CCD传感器的波段设置,利用6S模型计算了不同情况下的瑞利反射率;基于计算结果,分析了瑞利反射率的特征,包括大气类型的影响、波长的影响,以及宽波段设置带来的波段平均效应的影响等;构造了针对HY-1A CCD的瑞利反射率查找表,并应用于实际卫星数据处理,初步评估了方法的有效性.  相似文献   
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号