全文获取类型
收费全文 | 5494篇 |
免费 | 1208篇 |
国内免费 | 1752篇 |
专业分类
测绘学 | 952篇 |
大气科学 | 680篇 |
地球物理 | 1110篇 |
地质学 | 3562篇 |
海洋学 | 777篇 |
天文学 | 247篇 |
综合类 | 393篇 |
自然地理 | 733篇 |
出版年
2024年 | 54篇 |
2023年 | 111篇 |
2022年 | 318篇 |
2021年 | 422篇 |
2020年 | 328篇 |
2019年 | 381篇 |
2018年 | 364篇 |
2017年 | 345篇 |
2016年 | 349篇 |
2015年 | 373篇 |
2014年 | 383篇 |
2013年 | 455篇 |
2012年 | 449篇 |
2011年 | 486篇 |
2010年 | 451篇 |
2009年 | 439篇 |
2008年 | 423篇 |
2007年 | 394篇 |
2006年 | 368篇 |
2005年 | 342篇 |
2004年 | 273篇 |
2003年 | 197篇 |
2002年 | 182篇 |
2001年 | 143篇 |
2000年 | 116篇 |
1999年 | 70篇 |
1998年 | 27篇 |
1997年 | 29篇 |
1996年 | 21篇 |
1995年 | 20篇 |
1994年 | 16篇 |
1993年 | 10篇 |
1992年 | 14篇 |
1991年 | 13篇 |
1990年 | 16篇 |
1988年 | 3篇 |
1987年 | 4篇 |
1986年 | 5篇 |
1985年 | 5篇 |
1984年 | 5篇 |
1983年 | 6篇 |
1982年 | 4篇 |
1981年 | 6篇 |
1980年 | 4篇 |
1979年 | 6篇 |
1976年 | 4篇 |
1971年 | 2篇 |
1970年 | 2篇 |
1957年 | 3篇 |
1954年 | 2篇 |
排序方式: 共有8454条查询结果,搜索用时 31 毫秒
71.
72.
四阶△-∑过抽样电路原理及其在微弱地学信号检测中的应用 总被引:4,自引:0,他引:4
传统的测量电路无法解决诸如海底大地电磁场这样微弱地学信号的检测问题。近几年诞生了一种称之为△-∑的电路理论以及相应的硬件芯片,给微伏级的弱信号检测开辟一条新的技术路径。文章介绍与地学探测有关的一种△-∑电路类型,该类型以低频段微弱信号为检测对象。采用系统理论和电路分析方法对△-∑原理作了较深入的讨论,阐明这种电路技术对提高微弱信号观测的分辨率是有效的。结合海底大地电磁探测中的信号采集问题,介绍了在仪器中把多路的被测模拟量变为数字量的技术过程。经对实际采集的海底信息的频谱曲线进行分析,证实所采用的△-∑技术以及多路信号采集的电路方案是合理的。 相似文献
73.
74.
为探讨高原牌70kN和进口120,210kN瓷绝缘子的成分和结构性能,中采用原子吸收光谱(AAS)和X射线衍射(XRD)方法,对三类产品进行了检测。结果表明,有效成分除K2O外,70kN和210kN的SiO2,Al2O3,Fe2O3含量接近,主晶相基本相同,有刚玉,莫来石、石英和长石等;结晶相总量:70kN35%,120kN40%,210kN48%,这表明机械强度愈大,结晶相含量愈高,只需调整70kN原样的部分成分,粒度和工艺,即生产出高等级(如210kN)瓷绝缘子。 相似文献
75.
重点论述高峰锡矿 10 0号矿体的矿床数学经济模型的建立 ,分析模型在采矿、选矿等矿山生产动态管理中的作用及意义 相似文献
76.
本文以 1∶5万里庄幅为例 ,阐述了运用GIS系统对区调过程中各种资料的处理与编辑方法 ,并介绍了数字制图方法及工艺流程 ,提出了GIS系统在 1∶5万区调工作中的应用前景 相似文献
77.
78.
Chlorine- and sulphur-bearing compounds in fumarole discharges of the La Fossa crater at Vulcano Island (Italy) can be modelled by a mixing process between magmatic gases and vapour from a boiling hydrothermal system. This allows estimating the compounds in both endmembers. Magma degassing cannot explain the time variation of sulphur and HCl concentrations in the deep endmember, which are more probably linked to reactions of solid phases at depth, before mixing with the hydrothermal vapours. Based on the P–T conditions and speciation of the boiling hydrothermal system below La Fossa, the HCl and Stot contents in the hydrothermal vapours were used to compute the redox conditions and pH of the aqueous solution. The results suggest that the haematite–magnetite buffer controls the hydrothermal fO2 values, while the pH has increased since the end of the 1970s. The main processes affecting pH values may be linked to Na–Ca exchanges between evolved seawater, feeding the boiling hydrothermal system, and local rocks. While Na is removed from water, calcium enters the solution, undergoes hydrolysis and produces HCl, lowering the pH of the water. The increasing water–rock ratio within the hydrothermal system lowers the Ca availability, so the aqueous solution becomes less acidic. Seawater flowing towards the boiling hydrothermal brine dissolves a large quantity of pyrite along its path. In the boiling hydrothermal system, dissolved sulphur precipitates as pyrite and anhydrite, and becomes partitioned in vapour phase as H2S and SO2. These results are in agreement with the paragenesis of hydrothermal alteration minerals recovered in drilled wells at Vulcano and are also in agreement with the isotopic composition of sulphur emitted by the crater fumaroles. 相似文献
79.
Jean‐Jacques Macaire Saïda Bellemlih Christian Di‐Giovanni Patrick De Luca Lionel Visset Jacques Bernard 《地球表面变化过程与地形》2002,27(9):991-1009
In the Négron River catchment area (162 km2), surface‐sediment stores are composed of periglacial calcareous ‘grèze’ (5 × 106 t) and loess (21 × 106 t), and Holocene alluvium (12·6 × 106 t), peat (0·6 × 106 t) and colluvium (18·5 × 106 t). Seventy‐five per cent of the Holocene sediments is stored along the thalwegs. Present net sediment yield, calculated from solid discharge at the Négron outlet, is low (0·6 t km?2 a?1) due to the dominance of carbonate rocks in the catchment. Mean sediment yield during the Holocene period is 7·0 t km?2 a?1 from alluvium stores and 7·6 t km?2 a?1 from colluvium stores. Thus, the gross sediment yield during the Holocene period is about 18·7 t km?2 a?1 and the sediment delivery ratio 3 per cent. The yield considerably varies from one sub‐basin to another (3·9 to 24·5 t km?2 a?1) according to lithology: about 25 per cent and 50 per cent of initial stores of periglacial grèze and loess respectively were reworked during the Holocene period. Sediment yield has increased by a factor of 6 in the last 1000 years, due to the development of agriculture. The very high rate of sediment storage on the slope during that period (88 per cent of the yield) can be accounted for by the formation of cultivation steps (‘rideaux’). It is predicted that the current destruction of these steps will result in a sediment wave reaching the valley floors in the coming decades. Subboreal and Subatlantic sediments and pollen assemblages in the Taligny marsh, where one‐third of the alluvium is stored, show the predominant influence of human activity during these periods in the Négron catchment. Copyright © 2002 John Wiley & Sons, Ltd. 相似文献
80.