全文获取类型
收费全文 | 701篇 |
免费 | 88篇 |
国内免费 | 127篇 |
专业分类
测绘学 | 17篇 |
大气科学 | 63篇 |
地球物理 | 192篇 |
地质学 | 218篇 |
海洋学 | 225篇 |
天文学 | 37篇 |
综合类 | 45篇 |
自然地理 | 119篇 |
出版年
2024年 | 1篇 |
2023年 | 6篇 |
2022年 | 17篇 |
2021年 | 17篇 |
2020年 | 18篇 |
2019年 | 24篇 |
2018年 | 20篇 |
2017年 | 19篇 |
2016年 | 19篇 |
2015年 | 22篇 |
2014年 | 40篇 |
2013年 | 49篇 |
2012年 | 44篇 |
2011年 | 43篇 |
2010年 | 41篇 |
2009年 | 57篇 |
2008年 | 69篇 |
2007年 | 44篇 |
2006年 | 40篇 |
2005年 | 43篇 |
2004年 | 36篇 |
2003年 | 30篇 |
2002年 | 31篇 |
2001年 | 13篇 |
2000年 | 26篇 |
1999年 | 21篇 |
1998年 | 21篇 |
1997年 | 21篇 |
1996年 | 18篇 |
1995年 | 6篇 |
1994年 | 6篇 |
1993年 | 12篇 |
1992年 | 7篇 |
1991年 | 8篇 |
1990年 | 6篇 |
1989年 | 4篇 |
1988年 | 5篇 |
1987年 | 1篇 |
1986年 | 1篇 |
1985年 | 3篇 |
1983年 | 1篇 |
1980年 | 2篇 |
1979年 | 1篇 |
1978年 | 2篇 |
1977年 | 1篇 |
排序方式: 共有916条查询结果,搜索用时 15 毫秒
81.
82.
本文通过利用海南三亚站(1834°N, 10962°E)GPS闪烁/TEC接收机2004年8月到2005年7月间观测数据,在对三亚地区闪烁初步统计分析的基础上,比较分析了观测数据中S4(幅度闪烁指数)和C/N(载噪比),S4和ROTI(TEC变化率标准差)的关系,同时对2004年11月7日的闪烁事件进行了具体的分析. 通过比较分析得出:(1)三亚地区全年的闪烁强度具有明显的半年变化,在春秋季出现全年闪烁强度的最大值;(2)S4与C/N具有很好的负相关性;(3)ROTI可以作为由小尺度不规则结构引起闪烁出现的指示剂. 相似文献
83.
Jing Zhang 《Aquatic Geochemistry》1995,1(3):241-275
Water and suspended sediment samples from the Huanghe and its delta region were analyzed to determine arsenic concentrations. Comparison with the data of previous studies and other world pristine and less disturbed rivers reveals high levels of both dissolved and particulate As in this high turbidity river. Relatively stable distribution along the river course and in delta sediment cores shows that antrhopogenic activities have not altered As concentrations by any significant magnitude since the 1940s. Therefore, high levels of As in the Huanghe should be controlled by natural weathering and lithology. In the estuary, biological removal/regeneration and abiotic events (e.g. remobilization) have been identified to cause the active (non-conservative) As distributions. With the limited data set of the present study, the abiotic and biological contributions cannot be assessed accurately, however. 相似文献
84.
Fluxes of CO<Subscript>2</Subscript>, CH<Subscript>4</Subscript> and N<Subscript>2</Subscript>O from alpine grassland in the Tibetan Plateau 总被引:1,自引:0,他引:1
PEIZhiyong OUYANGHua ZHOUCaiping XUXingliang 《地理学报(英文版)》2003,13(1):27-34
Using static chamber technique,fluxes of CO2,CH4 and N2O were measured in the alpine grassland area from July 2000 to July 2001,determinations of mean fluxes showed that CO2 and N2O were generally released from the soil,while the alpine grassland accounted for a weak CH4 sink.Fluxes of CO2,CH4 and N2O ranged widely.The highest CO2 emission occurred in August,whereas almost 90?of the whole year emission occurred in the growing season.But the variations of CH4 and N2O fluxes did not show any clear patterns over the one-year-experiment.During a daily variation,the maximum CO2 emission occurred at 16:00,and then decreased to the minimum emission in the early morning.Daily pattern analyses indicated that the variation in CO2 fluxes was positively related to air temperatures(R^2=0.73)and soil temperatures at a depth of 5 cm(R^2=0.86),whereas daily variations in CH4 and N2O fluxes were poorly explained by soil temperatures and climatic variables.CO2 emissions in this area were much lower than other grasslands in plain areas. 相似文献
85.
嫩江组二段底部标志层岩石矿物学特征与成片套损因素新认识 总被引:1,自引:0,他引:1
大庆油田嫩江组二段底部与嫩江组一段顶部成片套损严重,从前一直认为泥岩吸水膨胀、蠕变是导致成片套损的主要因素。成片套损位置研究发现,嫩江组二段底部与嫩江组一段顶部成片套损实际集中于嫩江组二段底部标志层内,而嫩江组二段底部标志层岩石矿物学特征综合研究结果表明,其不含遇水膨胀的蒙脱石,且粘土矿物含量也低于其上下相邻岩石,表明其遇水膨胀与蠕变较弱,岩石遇水膨胀与蠕变不会构成成片套损的主要原因。嫩江组二段底部标志层岩石岩心观察描述、镜下鉴定、矿物成分综合测试和岩石强度性质研究发现,嫩江组二段底部标志层泥岩为富含长英质的质地坚硬岩石,含粘土矿物较少,不含蒙脱石,岩石吸水能力差、膨胀与蠕变能力弱;标志层中存在多个化石富集带,化石沿岩石层理分布形成沿层理方向的区域性力学薄弱面;沿化石层层理的抗张强度与抗剪强度远低于其他层位和垂直于层理方向的强度性质。因此,一旦注入水进入嫩江组二段底部标志层,富含化石的岩石沿岩石层理优先发生破坏,并迅速扩展,形成成片套损现象。 相似文献
86.
氮氧同位素在河流硝酸盐研究中的应用 总被引:9,自引:0,他引:9
多年来,世界各地河流普遍存在硝酸盐污染问题。为控制河流的硝酸盐污染,确定河水中硝酸盐的来源以及研究氮的循环过程就显得尤为重要。由于在不同成因下,硝酸盐的δ15N和δ18O存在着较大差异,因此利用氮、氧同位素方法研究河流硝酸盐问题正日益受到国内外研究人员的重视。综述了用硝酸盐中氮、氧同位素来研究河流硝酸盐的不同来源(大气沉降、化肥、牲畜粪、土壤硝酸盐等)和示踪其地球化学循环过程,特别是反硝化过程,这两方面的研究进展,并对我国河流硝酸盐研究现状进行了讨论及提出今后的研究方向。 相似文献
87.
用大功率5kWCO2激光器为能源,以六甲基二硅胺烷[(CH3)3Si]2NH(简称HMDS)和NH3为原料,合成纳米非晶Si/C/N复相粉体。研究了HMDS流量和NH3对纳米复相粉体组成的影响。NH3的加入可以大幅度降低纳米复相粉体的碳含量,提高氮含量。Si/C/N纳米复相粉体的粒径分布范围为10~50nm,为非晶态。 相似文献
88.
R. Swennen J. van der Sluys R. Hindel A. Brusselmans 《Journal of Geochemical Exploration》1998,62(1-3)
A geochemical survey of Belgium and Luxembourg was carried out as part of an international research project entitled ‘Regional geochemical mapping of Western Europe towards the year 2000'. The aim of this research was to map regional background geochemical patterns based on pristine or at least pre-industrial overbank samples and to deduce regional information on the degree of environmental pollution of floodplain and present-day river sediments. Over the entire study area (about 33,000 km2), 66 overbank sites have been sampled. Catchment areas range between 60 and 600 km2. At each site an overbank profile has been dug out in the immediate vicinity of the river and described in detail. A first composite sample was taken 5–25 cm below the surface. This sample is supposed to represent deposition over the last centuries. Human interferences in this interval are often inferable based on changed sedimentary characteristics and the presence of anthropogenic particles such as charcoal, slags and brick fragments. A second composite sample was taken at depth, usually >1.5 m below the surface over an interval of about 20 cm. In most sites, the profile characteristics allowed to assume pre-industrial or even pristine conditions for this lower overbank sample. In some profiles this was confirmed by 14C-dating and/or by the absence of anthropogenic particles. Finally, a present-day stream sediment was sampled on the site to infer the actual pollution status. After drying at 80°C, disaggregation and sieving, the <125 μm fractions of the three sediment samples were analysed by XRF for major elements and several trace elements. Lower overbank samples generally show a direct link with the geological substrate and allow to assess natural background concentrations. Results from the mapping exercise as well as from the statistical analyses display a clear contrast between the northern part of Belgium where Cenozoic unconsolidated sandy and silty formations dominate which are especially vulnerable for erosion, and the southern part of Belgium and Luxembourg where Paleozoic and Mesozoic sandstones, carbonates, marls and shales are the prevalent lithologies. Here the shales are the most intensively eroded lithologies. This is especially reflected in the element patterns of Al2O3, MgO, K2O, Ga, Ni, Rb, Sc and V which negatively correlate with SiO2. Despite the human related pollution, the geological contrast between north and south Belgium is still recognisable in the geochemical pattern of the upper overbank and present-day stream sediment samples for the above-mentioned elements. Furthermore there is a clear increase in heavy metal contents (Zn, Cd, Pb, Cu), As and in certain locations in Ba from the lower to the upper overbank sediment, as well as to the present-day stream sediment. The relative increase in element content allows to assess the degree of pollution and helps to define those drainage areas where more detailed research is needed. 相似文献
89.
Three provenances ofPappophorum caespitosum, a forage native grass from the temperate arid region of Argentina, were studied to gain a physiological knowledge of the seasonal organic N status in response to adequate water supply and water stress conditions; and to assess the extent to which variations in the N status between these provenances arise under different water regimes. Plant part samples were analysed for free and bound organic N fractions. Water shortage resulted in a significant depression of plant growth in all provenances. Total N concentration declined along the annual cycle in both water treatments, but it was higher under water stress. The size of the free N pool was very large, suggesting that it may act like an osmoticum. Nitrogen use efficiency increases along the growing period, while the rate of N intake and the specific leaf N content decrease. Variability was found between provenances in most of the physiological and biochemical traits examined under both water regimes. 相似文献
90.
氧化铬柱支撑蒙脱石的制备研究 总被引:4,自引:1,他引:3
以浙江和新疆的膨润土为原料合成了氧化铝柱支撑蒙脱石,成柱溶液以Na2CO3为碱水解铝盐溶液制得。因为制备含有大聚羟基铬阳离子的成柱溶液是获得具有大的基面间距的柱支撑粘土的关键,我们详细研究了CO32-/Cr3+值、水解温度和水解时间对所得柱支撑蒙脱石性质的影响。聚羟基铬阳离子通过阳离子交换引入蒙脱石,所得产物用X射线衍射分析和BET氮比表面等方法研究。所得氧化铝柱支撑蒙脱石(简称Cr-mont)的基面间距为2.55nm,BET氮比表面积为190~230m2/g。 相似文献