全文获取类型
收费全文 | 1460篇 |
免费 | 228篇 |
国内免费 | 245篇 |
专业分类
测绘学 | 423篇 |
大气科学 | 71篇 |
地球物理 | 312篇 |
地质学 | 668篇 |
海洋学 | 127篇 |
天文学 | 13篇 |
综合类 | 171篇 |
自然地理 | 148篇 |
出版年
2024年 | 8篇 |
2023年 | 19篇 |
2022年 | 50篇 |
2021年 | 63篇 |
2020年 | 62篇 |
2019年 | 63篇 |
2018年 | 48篇 |
2017年 | 68篇 |
2016年 | 82篇 |
2015年 | 90篇 |
2014年 | 92篇 |
2013年 | 96篇 |
2012年 | 93篇 |
2011年 | 90篇 |
2010年 | 83篇 |
2009年 | 97篇 |
2008年 | 80篇 |
2007年 | 89篇 |
2006年 | 84篇 |
2005年 | 58篇 |
2004年 | 70篇 |
2003年 | 49篇 |
2002年 | 50篇 |
2001年 | 40篇 |
2000年 | 34篇 |
1999年 | 36篇 |
1998年 | 31篇 |
1997年 | 32篇 |
1996年 | 27篇 |
1995年 | 26篇 |
1994年 | 12篇 |
1993年 | 32篇 |
1992年 | 11篇 |
1991年 | 13篇 |
1990年 | 12篇 |
1989年 | 16篇 |
1988年 | 8篇 |
1987年 | 9篇 |
1986年 | 4篇 |
1985年 | 2篇 |
1982年 | 1篇 |
1980年 | 2篇 |
1954年 | 1篇 |
排序方式: 共有1933条查询结果,搜索用时 15 毫秒
21.
引用了流体饱和两相多孔介质的动力控制方程分析半空间埋置动点源荷载问题的位移和变形。经过Laplace Hankel变换 ,控制方程化成常微分方程组。利用数学软件mathmatic对上述方程组求解 ,可以得到单层砂土的传递矩阵。分析过程中 ,假设在两层面上 ,位移与应力相互连续 ,可以借鉴有限元的思想进行耦合计算。这样就获得了在饱和砂土中施加竖向动荷载问题的Laplace Hankel变换解 ,其最终的解还需要通过Laplace Hankel逆变换得到 相似文献
22.
T. Masuda S. Nakayama N. Kimura K. Onodera A. Okamoto 《Journal of Structural Geology》2004,26(12):2203-2209
A rare metachert pebble containing amphibole grains with microboudin structures in a wide range of orientations provides an opportunity to perform stress analysis in two orthogonal orientations on the foliation surface. The sample was analysed by the microboudin method to infer the triaxial stress state during microboudinage. Stress parameters proportional to the far-field differential stress were determined for sodic amphibole grains in the two orientations. The ratio of the stresses in the two orthogonal orientations (σ1−σ2)/(σ1−σ3) was calculated to be 0.64, indicating that σ2 lies closer to the midpoint between σ1 and σ3 than to σ3. 相似文献
23.
Sandro Fadda 《Geostandards and Geoanalytical Research》2005,29(1):143-156
Major concentrations of Al2O3, Fe2O3, MgO, CaO, Na2O and K2O, minor levels of TiO2, P2O5 and thirty petrologically, geochemically and environmentally significant trace elements have been determined in microwave oven acid leachates of whole powdered coal samples by direct current plasma‐atomic emission spectrometry (DCP‐AES). A single sample preparation procedure was suitable for all the determinations with no additional dilution step for major elements solution. Dried samples (0.5 g) were treated in low‐pressure PFA digestion vessels with HF/HCl/HNO3/HClO4 acids to quantitatively extract the analytes from the bulk material, while leaving the major part of organic matrix as a residue. The major constituents of geological samples, in particular the easily ionised elements (EIEs) such as alkali and alkaline earths, may complicate the instrumental determinations in DCP‐AES because of differential enhancements of elemental emission intensities and stray light interferences. Taking account of these factors, the coal matrix is considered to have very low major oxide totals as compared to many other common geo‐environmental and related materials (rocks, sediments, soil, ashes etc.). The sample size employed here, while yielding a relatively concentrated solution to cover a wide range of elemental determinations, provided a sample matrix that significantly diminished interferences for DCP measurements. The need for closely matching the unknowns and calibrators was eliminated except for overall acidity and an excess quantity of caesium for EIE buffering. Calibration of the spectrometer was accomplished by simple aqueous single element solutions as high concentration calibrators in addition to a reagent blank as a low concentration calibrator. Two point working curves were established to allow for the maximum concentrations of each element expected in the unknowns. The precision of determinations under routine conditions as well as the reproducibility of the leaching and precision of instrumental measurements have been evaluated. Relative standard deviations (RSD) were of 1–2% for those elements whose concentrations in solid samples were well above the limits of quantification. Method detection limits in the buffered solutions were also evaluated. To evaluate the accuracy of the microwave oven‐DCP method a suite of eight certified coal reference materials of differing rank, were analysed with good agreement with the certified and/or available published data. Results are presented for the uncertified major oxides in the AR series reference materials. 相似文献
24.
25.
26.
27.
对薄壁金刚石钻头胎体进行了性能分析和配方设计探讨,尤其根据被钻切介质对钻头胎体性能的要求作了较详细的分析,从理论分析结合实践经验筛选出了钻切建筑石材和各种钢筋砼的钻头胎体配方,在生产中满足了钻头工作条件的要求。 相似文献
28.
收缩情境下城市用地结构时空格局演变及动力机制——以中国东北地区为例 总被引:2,自引:1,他引:2
构建城市用地结构时空格局演变分析框架,引入信息熵和偏移份额模型定量剖析2000-2017年中国东北地区城市用地结构时空格局演变特征,通过计量经济模型分阶段对比分析收缩情境下东北地区城市用地结构演变的动力机制.结果表明:东北地区城市用地总面积持续增长,用地结构信息熵整体呈现先上升、后下降的趋势.2011年以后,城市用地结... 相似文献
29.
盐岩在深部高温高压环境下具有很强的蠕变特性,在岩盐层钻井经常出现井眼缩径、卡钻等复杂事故。目前关于岩盐层井段安全钻进泥浆密度的计算方法主要适用于均匀地应力的情况,难以在非均匀地应力条件下应用。为此研究建立了三向地应力作用下盐岩和砂泥岩相互交错的复合岩盐层井眼蠕变缩径的三维有限元模型,并以塔里木油田羊塔克地区深井为例,研究了非均匀地应力条件下,复合岩盐层井眼随时间变化的蠕变缩径规律,得出了一定泥浆密度下岩盐层井眼在不同时刻的井径值。计算结果表明,安全泥浆密度有限元模拟值与羊塔克地区岩盐层井段实际采用的安全泥浆密度非常接近,验证了所建数值模型的合理性和计算结果的可靠性,研究成果为岩盐层井段的安全钻进提供了技术支撑。 相似文献
30.
Analysis of Sediments and Soils by X-Ray Fluorescence Spectrometry Using Matrix Corrections Based on Fundamental Parameters 总被引:2,自引:0,他引:2
Jacinta Enzweiler Maria Aparecida Vendemiatto 《Geostandards and Geoanalytical Research》2004,28(1):103-112
Wavelength dispersive X-ray fluorescence spectrometry (WD-XRF) is widely used for the analysis of soils and sediments using well characterised procedures. However, difficulties can occur with samples such as unknowns containing small amounts of ore materials and samples collected from contaminated sites where trace elemental concentrations can exceed the concentration range for routine analysis. We studied the performance of a commercially available method, based on fundamental parameters (FP) to correct matrix effects. The spectrometer was originally calibrated with elemental or simple compound calibrants. Samples were analysed as pressed powder pellets. Eighteen sediment and soil reference materials, three of them with certified values for some of their constituents, were used to evaluate accuracy, by comparing results with recommended values and their standard deviations (RV ± 2s) or certified values and their confidence intervals (CV ± Cl). When results fell systematically outside these intervals, calibrations were refined with geochemical reference materials. The best agreement of results with recommended and certified values was obtained when the contents of H2 O and C in each sample were included as matrix constituents during calculations. The detection limits of trace elements tended to be relatively high, because the measuring conditions employed were not maximised for sensitivity. The main advantage of the method tested was that it enabled the analysis of samples with high concentrations of trace elements and the determination of elements such as F, Bi, Sb and W, which are not commonly included in quantitative XRF analysis of geological samples. 相似文献