全文获取类型
收费全文 | 3283篇 |
免费 | 581篇 |
国内免费 | 463篇 |
专业分类
测绘学 | 445篇 |
大气科学 | 255篇 |
地球物理 | 1002篇 |
地质学 | 1374篇 |
海洋学 | 327篇 |
天文学 | 101篇 |
综合类 | 231篇 |
自然地理 | 592篇 |
出版年
2024年 | 12篇 |
2023年 | 41篇 |
2022年 | 125篇 |
2021年 | 124篇 |
2020年 | 138篇 |
2019年 | 180篇 |
2018年 | 135篇 |
2017年 | 140篇 |
2016年 | 153篇 |
2015年 | 154篇 |
2014年 | 167篇 |
2013年 | 220篇 |
2012年 | 212篇 |
2011年 | 223篇 |
2010年 | 152篇 |
2009年 | 198篇 |
2008年 | 172篇 |
2007年 | 212篇 |
2006年 | 234篇 |
2005年 | 181篇 |
2004年 | 147篇 |
2003年 | 130篇 |
2002年 | 112篇 |
2001年 | 120篇 |
2000年 | 114篇 |
1999年 | 96篇 |
1998年 | 80篇 |
1997年 | 77篇 |
1996年 | 73篇 |
1995年 | 48篇 |
1994年 | 37篇 |
1993年 | 25篇 |
1992年 | 22篇 |
1991年 | 20篇 |
1990年 | 11篇 |
1989年 | 14篇 |
1988年 | 7篇 |
1987年 | 8篇 |
1986年 | 2篇 |
1985年 | 3篇 |
1984年 | 2篇 |
1983年 | 1篇 |
1982年 | 1篇 |
1981年 | 1篇 |
1980年 | 1篇 |
1979年 | 2篇 |
排序方式: 共有4327条查询结果,搜索用时 203 毫秒
31.
在洋浦近岸海域计算潮流场基础上,计算预选排污口附近海水质点运动轨迹及预测污染物浓度分布,最后,从环保角度出发,推荐了洋浦地区各开发区的排污口位置,为洋浦近岸海域污染控制规划方案的制定及其优化提供了依据。 相似文献
32.
利用模式识别中特征提取和特征选择的相关理论对遥感影像的纹理特征进行遴选和变换处理,得到描述纹理的二次特征。实验证明这些新特征能够提高影像分类精度和分类效率。 相似文献
33.
34.
35.
王艳江 《测绘与空间地理信息》2008,(1)
1∶50000地形数据库更新是一项复杂的地形数据库制作工程。传统的缩编技术工艺与相应的工具难以适应新的生产需要,适应于数字环境下的缩编生产工具的需求则变得非常迫切。GENTOOLS很好地解决了1∶50000数据库更新工程中的诸多难题,采用半自动和手动相结合的方法,大大提高了缩编效率,同时也为地形图缩编提供了一种新的选择。 相似文献
36.
对照现行《建筑抗震设计规范》(GB50011-2001)场地类别划分方法,应用模糊数学原理,推导了场地类别的模糊二次评价方法,得出了场地类别的模糊向量和模糊特征周期,实现了场地类别划分的连续化;在此基础上,基于收集到的杭州市254个建筑场地波速钻孔实测资料,通过建立场地类别地质模型,实现了场地类别、特征周期的模糊等值线,与实测资料对比,结果表明:由该模糊等值线得出的建筑场地抗震类别与现行《建筑抗震设计规范》给出的场地类别是统一的,模糊特征周期与规范给出的特征周期基本上是吻合的,该模糊等值线对建筑抗震设计具有指导意义。 相似文献
37.
辽宁中部一些地区的含煤地层以前被认为是白垩系下统的沙海组、阜新组,该观点导致区域地层对比混乱。通过对该区含煤地层组合特征综合分析,认为其应属下侏罗统北票组含煤岩系。此结论对进一步明确该地区找煤方向、确定找煤远景区具有重要意义。 相似文献
38.
Olivier Rossier Emmanuel Castella Jean-Bernard Lachavanne 《Aquatic Sciences - Research Across Boundaries》1996,58(1):1-14
The abundance of different size classes of perch and roach in the littoral zone of Lake Geneva was compared between submerged aquatic vegetation and unvegetated zones. Samples were taken with gillnets during four periods between June and October 1993. During the vegetation period (June to September), perch 9 cm and roach 10 cm were more abundant in vegetation whereas roach > 20 cm were more abundant in open water. Perch larger than 18 cm and medium roach were equally distributed in both habitats whatever the period, whereas medium perch distribution fluctuated according to the period. In October, after the decline of the vegetation, no more differences in fish distribution were observed except for small roach, which were always more abundant in the vegetated sites. 相似文献
39.
Xian-Huan Wen 《Mathematical Geology》1994,26(6):717-731
Field tests of hydraulic conductivity (e.g., injection test, pumping test, etc.) in low permeability formations are subject to censoring due to the detection limit of the instruments used. An iterative method of estimating the mean and variance of hydraulic conductivity data with a presumed log-normal distribution function is presented. This method accounts for the data that are actually below the lower detection limit (called truncated data) and thus gives distribution parameters that are more representative for the underlying distribution. The proposed method is then tested on two simulated normally distributed random datasets having different variances. The results show that the means and variances estimated by the proposed method are very accurate. Finally, the method is used to estimate the mean and variance of hydraulic conductivity data from single hole water injection tests in a fractured geological formation. 相似文献
40.
Weak and strong ground motions were numerically predicted for three stations of the Ashigara Valley test site. The prediction was based on the records from a rock-outcrop station, one weak-motion record from a surface-sediments station, and the standard geotechnical model. The data were provided by the Japanese Working Group on the Effects of Surface Geology as a part of an international experiment. The finite-difference method for SH waves in a 2-D linear viscoelastic medium (a causalQ model) was employed.Comparison with the real records shows that at two stations the predictions fit better than at the third one. Strangely, the two better predictions were for stations situated at larger distances from the reference rock station (one station was on the surface, the other in a borehole). The strong ground motion (the peak acceleration of about 200 cm s–2) was not predicted qualitatively worse than the weak motion (8 cm s–2). A less sophisticated second prediction (not submitted during the experiment), in which we did not attempt to fit the available weak-motion record at the sedimentary station, agrees with the reality significantly better. 相似文献