全文获取类型
收费全文 | 498篇 |
免费 | 24篇 |
国内免费 | 28篇 |
专业分类
测绘学 | 226篇 |
大气科学 | 12篇 |
地球物理 | 59篇 |
地质学 | 61篇 |
海洋学 | 39篇 |
天文学 | 3篇 |
综合类 | 59篇 |
自然地理 | 91篇 |
出版年
2024年 | 2篇 |
2023年 | 1篇 |
2022年 | 9篇 |
2021年 | 8篇 |
2020年 | 5篇 |
2019年 | 13篇 |
2018年 | 5篇 |
2017年 | 15篇 |
2016年 | 21篇 |
2015年 | 14篇 |
2014年 | 23篇 |
2013年 | 29篇 |
2012年 | 20篇 |
2011年 | 20篇 |
2010年 | 11篇 |
2009年 | 29篇 |
2008年 | 32篇 |
2007年 | 33篇 |
2006年 | 34篇 |
2005年 | 23篇 |
2004年 | 20篇 |
2003年 | 27篇 |
2002年 | 19篇 |
2001年 | 18篇 |
2000年 | 20篇 |
1999年 | 10篇 |
1998年 | 11篇 |
1997年 | 12篇 |
1996年 | 14篇 |
1995年 | 5篇 |
1994年 | 7篇 |
1993年 | 10篇 |
1992年 | 5篇 |
1991年 | 5篇 |
1990年 | 1篇 |
1989年 | 7篇 |
1988年 | 5篇 |
1987年 | 3篇 |
1986年 | 3篇 |
1985年 | 1篇 |
排序方式: 共有550条查询结果,搜索用时 13 毫秒
51.
张赤军 《大地测量与地球动力学》2002,22(4):31-34
介绍当今确定天文大地垂偏差的新仪器-CCD自动天体测量仪和确定两点间高程异常差的新方法,该方法用单极坐标代替繁琐的双极坐标进行计算,讨论了天文重力水准的误差及垂线偏差非线性影响等问题,估计在不久的将来,用这一手段施测山区似大地水准面的精度可望达到厘米级。 相似文献
52.
作为主要的大气污染指标,PM2.5浓度常来源于固定环境监测站点的监测与遥感影像数据,但时空精度普遍不足,难以揭示微尺度下城市内部PM2.5时空分布情况。本文利用移动式监测方法,选择典型工作日(2017年11月27日),对广州市主城区道路以1 s和1 m为时空粒度进行PM2.5浓度数据采集,并以早、晚出行高峰时段为对象,通过机器学习方法模拟道路PM2.5精细化时空分布格局。结果表明,主城区早高峰道路PM2.5浓度值相近的平均范围为24 m,晚高峰为15 m,PM2.5浓度存在微尺度的时空异质性。利用多层感知器(MLP)构建的早、晚高峰PM2.5浓度模型,拟合度分别达到0.70和0.68,明显优于传统的普通最小二乘法(OLS)线性回归模型。模型揭示出早高峰主城区全路网PM2.5平均浓度为30.19μg/m3,晚高峰达到44.55μg/m3,部分高达94.82μg/m3,且“西高东低”的分布特征显著。本文提出的PM 相似文献
53.
Tobelite (NH4) Al2 [AlSi3O10] (OH)2, the ammonium analogue of muscovite, and its deuterated form ND4-tobelite (ND4) Al2 [AlSi3O10] (OD)2 have been synthesised at 600?°C and 200 and 500 Mpa using a well homogenised, stoichiometric SiO2-Al2O3 oxide mix with Al2O3 in excess of 5 mol% and a 25% NH3 solution whose relative abundance was such that the amount of NH4 + stoichiometrically available was in excess of 50%. Characterisation of both tobelite and ND4-tobelite using IR-spectroscopy, Rietveld refinement of X-ray powder diffraction data, and electron microprobe analysis indicate that, similar to K+ in muscovite, the NH4 + or ND4 + molecule occupies the interlayer site. IR absorption bands caused by NH4 + and ND4 + can be explained, to a very good approximation, on the basis of Td symmetry. Nevertheless, substantial line broadening and the occurrence of shoulders indicate a deviation from ideal Td symmetry. However, even at 77?K, no discrete splitting of the degenerate states could be confirmed. The OH stretching frequencies observed for synthetic tobelite are quite similar to those for muscovite, indicating that the replacement of K+ by NH4 + has no effect. The low FWHH of the OH bands indicate that the hydroxyl groups are well ordered within the structure. Rietveld refinement of tobelite and ND4-tobelite indicates that all samples synthesised consist of the 3 different mica polytypes which are typical of muscovite – namely 1M (C2/m), 2M 1 (C2/c) and 2M 2 (C2/c). Tobelite and ND4-tobelite synthesised at 500 Mpa principally contain the 1M polytype, whereas the principle polytype for ND4-tobelite synthesised at 200 Mpa, is 2M 2. Rietveld refinement of X-ray diffraction spectra for tobelite synthesised at 200 Mpa was problematic due to the very broad FWHH of the X-ray peaks indicating poor crystallinity. In comparision to synthetic muscovite, the cell dimensions observed for tobelite and its deuterated analogue are quite similar except for the lattice constant c. Due to the larger radius of NH4 + or ND4 + compared to K+ cation, the c-direction is expanded form 10.275 Å in muscovite to approximately 10.540 Å in tobelite and ND4-tobelite. 相似文献
54.
???????????????????BP?????緽????????????????????棬?????????????????????????????Ч???????????????????????????????????????????????????????????????????????????????????仯???????????????????????????y?????ж???????????п?????θ?????????£?PSO-BP??????????????÷???????Ч???? 相似文献
55.
The reduction of aliasing in gravity anomalies and geoid heights using digital terrain data 总被引:8,自引:0,他引:8
Observations of gravity can be aliased by virtue of the logistics involved in collecting these data in the field. For instance, gravity measurements are often made in more accessible lowland areas where there are roads and tracks, thus omitting areas of higher relief in between. The gravimetric determination of the geoid requires mean terrain-corrected free-air anomalies; however, anomalies based only on the observations in lowland regions are not necessarily representative of the true mean value over the topography. A five-stage approach is taken that uses a digital elevation model, which provides a more accurate representation of the topography than the gravity observation elevations, to reduce the unrepresentative sampling in the gravity observations. When using this approach with the Australian digital elevation model, the terrain-corrected free-air anomalies generated from the Australian gravity data base change by between 77.075 and −84.335 mgal (−0.193 mgal mean and 2.687 mgal standard deviation). Subsequent gravimetric geoid computations are used to illustrate the effect of aliasing in the Australian gravity data upon the geoid. The difference between 'aliased' and 'non-aliased' gravimetric geoid solutions varies by between 0.732 and −1.816 m (−0.058 m mean and 0.122 m standard deviation). Based on these conceptual arguments and numerical results, it is recommended that supplementary digital elevation information be included during the estimation of mean gravity anomalies prior to the computation of a gravimetric geoid model. 相似文献
56.
57.
田晋 《武汉大学学报(信息科学版)》2009,34(1):113-116
给出了局部大地水准面精化系统的总体结构以及各分系统的详细设计与实现方法,开发了旨在对相关重力测量数据实现自动化处理的局部大地水准面精化系统工具软件,并应用于某区域实际大地水准面的精确计算。实践证明,该系统能有效提高相关数据的处理效率,有助于局部大地水准面精化过程的规范化。 相似文献
58.
The atmospheric geoid effects in Stokes' formula 总被引:2,自引:0,他引:2
59.
60.
理论结合实际,用详实的数据说明了在两井贯通时,把水准面当作水平面处理的界限,避免了盲目应用而产生严重后果. 相似文献