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611.
赤潮藻的显微图形测量方法研究 总被引:2,自引:0,他引:2
介绍了一种在实验室环境下通过显微镜及CCD成像的办法观察采集微小藻类图像,并通过计算机软件进行图像识别统计,最终得到所测藻类统计信息的方法。 相似文献
612.
613.
基于单调链的Red/Blue扫描线求交算法 总被引:3,自引:0,他引:3
提出了一种基于单调链的Red/Blue平面扫描线算法。该算法针对GIS中线段之间具有连接关系的特性,将平面连接线段集分解为一组单调链,通过对单调链的粗扫描过滤和对线段的精扫描求交,减少了扫描过程中的冗余计算,提高了线段集求交点的效率。实验证明,该算法对于处理具有连接关系的线段集的求交点问题具有很高的效率。 相似文献
614.
WATER POLLUTION IN THE RIVER MOUTHS AROUND BOHAI BAY 总被引:10,自引:0,他引:10
Cheng LIU Zhao-Yin WANG Yun HE Dr. Asso. Prof. International Research Training Center on Erosion Sedimentation Beijing .China Prof.. Dept. of Hydraulic Engineering Tsinghua University & International Research Training Center onErosion Sedimentation Beijing China.China Institute of Water Resources Hydropower Research. Beijing China 《国际泥沙研究》2003,18(4)
Twelve water samples were collected and analyzed. The samples were taken from the river mouths around Bohai Bay including the Jiyun. New Yongding, Haihe, Dagu, Duliujian, Qingjinghuang, Qikou, Dakou, and Yellow Rivers, and tested for concentrations of heavy metals, arsenic, total nitrogen (TN) and total phosphorus (TP). The results show that the river mouths are polluted and the water quality exceeds Class V of the Environmental Quality Standard for Surface Water (EQSSW). The main pollutants are Hg, nitrogen (N) and phosphorus (P). The concentrations of the other pollutants are within Class II of the Standard. The Hg content in the Haihe River mouth is now 10 times higher than it was 20 years ago, indicating that the accelerating water pollution has reached an alarming level. The high concentrations of N and P cause eutrophication of the waters. Analysis indicates that the terrestrial pollutants and nutrients are the main cause of frequently occurring red tides in the Bohai Sea. 相似文献
615.
616.
EARTHQUAKE FOCAL MECHANISM AND ITS TECTONIC SIGNIFICANCE ALONG THE TWO SIDES OF THE RED RIVER FAULT ZONE 总被引:1,自引:0,他引:1
The Red River Fault Zone is a gigantic slide-slip fault zone extending up to 1000km from Tibet to South China Sea. It has been divided into the north, central and south segments according to the difference of the geometry, kinetics, and seismicity on the land, but according to the contacted relationship between the old pre-Cenozoic block in Indochina Peninsula and the South China block, the Red River Fault Zone was divided into two parts extending from land to ocean, the north and south segments. Since the Tertiary, the Red River Fault Zone suffered first the sinistral movement and then the dextral movement. The activities of the north and the south segments were different. Based on the analysis of earthquakes and focal mechanism solutions, earthquakes with the focus depths of 0-33km are distributed over the whole region and more deep earthquakes are distributed on the northeastern sides of the Red River fault. Types of faulting activities are the thrust in the northwest, the normal in the north and the 相似文献
617.
The Maastrichtian oyster Lopha villei (Coquand) occurs abundantly in the upper part of the Duwi Formation in the Red Sea region, Egypt. It forms thin undulating sharp-based shell beds that comprise both reclining and encrusting morphotypes of Lopha villei. Bed-by-bed biostratinomic and facies analyses of these shell beds confirm their shallow marine origin and formation by storm events. A tempestite model, explaining the mode of formation and the idealized sequence of events of such storm shell beds, has been inferred. 相似文献
618.
水分胁迫下棉花冠层叶片氮素状况的高光谱估测研究 总被引:4,自引:3,他引:4
在不同灌水量条件下,对棉花单叶叶绿素含量和单叶全氮含量做相关分析,并采用地物光谱仪。获取北疆棉花冠层关键生育时期的高光谱数据。应用一阶微分光谱,衍生出基于光谱位置变量的分析方法。以红边积分面积(SDr)为白变量,冠层全氮(TN)含量为因变量,做相关分析。结果表明:叶绿素含量与TN含量呈显著的正相关(R=0.8723^**。n=39),叶绿素含量能有效的估计棉花单叶TN含量;红边积分面积变量与冠层TN含量呈显著的相关性,相关系数是0.7394^**(n=40),利用构建的相关模型可以较为精确地估测新陆早6号、8号冠层叶片的全氮含量,RMSE分别为0.3859和0.4272。研究认为红边积分面积变量具有预测棉花冠层全氮含量的应用潜力。 相似文献
619.
We report a study of the Holocene coastal sediments of the Hai Phong area of the Bac Bo Plain (also known as the Red River Delta) in northern Vietnam. This is the first attempt to interpret the region's coastal depositional environments in the light of a geological model of Holocene environmental change recognising the interacting roles of Holocene sea-level change, alluvial responses to sea-level fluctuation, and tidal environment sedimentation. The coastal sediments overlie a Pleistocene land surface, and represent the Holocene marine transgression and regression. Prior to c .6000 bp , the sea rose to around or above its present elevation, converting the Pleistocene terrestrial landscape to a Holocene tidal landscape of tidal flat, channel and mangrove environments. Sea-level lowering by c .4000 bp triggered a switch in dominant sedimentary processes, allowing floodplain sediments to be deposited increasingly seawards. 相似文献
620.
W. W. Duley 《Monthly notices of the Royal Astronomical Society》1998,301(4):955-959
An analysis of the intensity and spatial distribution of the discrete 5800-Å emission band in the spectrum of the Red Rectangle has been used to constrain the abundance and physical properties of the carrier of this emission. An origin in a large (>30 C atom) molecule is indicated. This molecule is formed in situ in the Red Rectangle, but is also a component of the diffuse interstellar medium. The UV photodissociation probability for this molecule is ≲10−5 per absorbed photon, and the luminescence efficiency is in the range 10−2 –10−3 . This molecule may be a product of the dissociation of carbonaceous dust. 相似文献