首页 | 本学科首页   官方微博 | 高级检索  
文章检索
  按 检索   检索词:      
出版年份:   被引次数:   他引次数: 提示:输入*表示无穷大
  收费全文   753篇
  免费   61篇
  国内免费   4篇
测绘学   16篇
大气科学   101篇
地球物理   160篇
地质学   295篇
海洋学   40篇
天文学   143篇
综合类   14篇
自然地理   49篇
  2023年   3篇
  2021年   8篇
  2020年   16篇
  2019年   16篇
  2018年   37篇
  2017年   21篇
  2016年   36篇
  2015年   30篇
  2014年   32篇
  2013年   49篇
  2012年   41篇
  2011年   40篇
  2010年   39篇
  2009年   43篇
  2008年   47篇
  2007年   35篇
  2006年   29篇
  2005年   37篇
  2004年   23篇
  2003年   26篇
  2002年   12篇
  2001年   17篇
  2000年   12篇
  1999年   8篇
  1998年   13篇
  1997年   12篇
  1996年   11篇
  1995年   9篇
  1994年   10篇
  1993年   6篇
  1991年   10篇
  1990年   4篇
  1989年   7篇
  1988年   12篇
  1987年   5篇
  1986年   7篇
  1984年   7篇
  1982年   4篇
  1981年   3篇
  1980年   3篇
  1978年   2篇
  1977年   2篇
  1974年   3篇
  1973年   3篇
  1971年   2篇
  1970年   2篇
  1969年   2篇
  1967年   3篇
  1960年   2篇
  1955年   2篇
排序方式: 共有818条查询结果,搜索用时 234 毫秒
1.
2.
地下水资源可持续利用的一个急待解决的重要问题,是对地下水补给和更新能力的评价.利用环境同位素技术研究地下水的补给和可更新性是当前较为新颖的方法之一.在西北干旱、半干旱的隐伏岩溶地区,地下水埋藏条件复杂,常规的地质勘探方法所能提供的水文地质信息有限,环境同位素方法在研究地下水的补给及可更新能力方面发挥了优势,可对传统方法进行补充和验证.其结果表明,研究区隐伏岩溶水形成较早,且有大量现代水的混入,平均混入量为54%.说明区内隐伏岩溶水的补给和更新能力较好.环境同位素分析结果还显示,大岔河隐伏岩溶水为一相对独立、半开放的水文地质单元,其补给来源部分为流域内大气降水、地表水的补给,部分为东南部三道沟岩溶地下水的补给;根据环境同位素EPM模型计算,地下水的滞留时间为36 a.地下水储存量为1.314×108 m3; 储水系数为7.29×10-3.这一结果与传统勘探方法的计算结果基本吻合,说明环境同位素方法的实用性.  相似文献   
3.
4.
The Triana PlasMag Faraday Cup (FC) will be able to determine speed, flow angles, temperature, and density of the main solar wind ion species with a time resolution of better than one second. Thus, the Triana PlasMag FC will enable resolution of spatial structures as small as a few hundred kilometers as the structures convect past the spacecraft. Under typical solar wind conditions, that size is comparable to a few proton gyroradii. This revised version was published online in July 2006 with corrections to the Cover Date.  相似文献   
5.
Using political ecology as its conceptual framework, this paper focuses on the changes in forest utilisation and management of South Kyrgyzstan's walnut-fruit forests over the last century The aim of this study on human-environment interactions is to investigate the relationship between actors on the one side, their interests and demands, and the forests and forested lands on the other. Forest resource utilisation and management - and even the recognition of different forest products as resources - are connected with political and socioeconomic conditions that change with time. The walnut-fruit forests of South Kyrgyzstan are unique, characterised by high biodiversity and a multiplicity of usable products; and they have been utilised for a long time. Centralised and formal management of the forests started with the Russian occupation and was strengthened under Soviet rule, when the region became a part of the USSR. During this era, a state forest administration that was structured from Moscow all the way down to the local level drew up detailed plans and developed procedures for utilising the different forest products. Since the collapse of the Soviet Union, the socio-political and economic frame conditions have changed significantly, which has brought not only the sweeping changes in the managing institutions, but also the access rights and interests in the forest resources. At present, the region is suffering from a high unemployment rate, which has resulted in the forests' gaining considerable importance in the livelihood strategies of the local population. Political and economic liberalization, increased communication and transregional exchange relations have opened the door for international companies and agents interested in the valuable forest products. Today, walnut wood and burls, walnuts, wild apples and mushrooms are all exported to various countries in the world. Scientists and members of various international organisations stress the ecological value of the forests and are trying to establish nature conservation areas. Nevertheless, it is to fear that a multiplicity of interrelated factors - the present transformation and globalization processes, the appearance of new actors, the local population's insecure economic situation and the erosion of managing institutions - are all leading to an intensified and unregulated exploitation of the forests, resulting in their degradation.  相似文献   
6.
Between June 2004 and September 2004 a temporary seismic network was installed on the northern insular shelf of Iceland and onshore in north Iceland. The seismic setup aimed at resolving the subsurface structure and, thus, the geodynamical transition from Icelandic crust to typical oceanic crust along Kolbeinsey Ridge. The experiment recorded about 1,000 earthquakes. The region encloses the Tjörnes Fracture Zone containing the Husavik–Flatey strike-slip fault and the extensional seismic Grimsey Lineament. Most of the seismicity occurs in swarms offshore. Preliminary results reveal typical mid-ocean crust north of Grimsey and a heterogeneous structure with major velocity anomalies along the seismic lineaments and north–south trending subsurface features. Complementary bathymetric mapping highlight numerous extrusion features along the Grimsey Lineament and Kolbeinsey Ridge. The seismic dataset promises to deliver new insights into the tectonic framework for earthquakes in an extensional transform zone along the global mid-ocean ridge system.  相似文献   
7.
Variation in glycogen concentration, condition index (CI) and filtration activity were measured in the bivalve Macoma balthica buried in sediment and experimentally exposed to cadmium (Cd). The stress due to elevated but sub-lethal concentrations (300 ppb Cd) affected the overall fitness of the organism as all parameters monitored responded significantly. Lower concentrations tested (10, 30 and 100 ppb) only induced a significant decrease in filtration activity, which may play a protective role, enabling the organism to slow down its metabolic activity and preserving the integrity of its reserves (reflected by stable CI and glycogen levels). Hence, the various endpoints selected show different thresholds. Our results also demonstrate that under high exposure, small individuals loose proportionally more glycogen per unit of weight than larger ones, thus confirming the higher sensitivity of small individuals to metal contamination. Furthermore, exposure to intermediate concentration (30 ppb) seems to be beneficial to the small individuals as indicated by their high CI values compared to the control. These results showed thus that non-sigmoidal concentration-response relationship and sizes of individuals should be considered in monitoring programmes and risk assessment.  相似文献   
8.
Multi-parameter mixing analysis is applied to 26 stations of Auftrieb 75, a joint expedition of R.R.S. Discovery and FS Meteor. North Atlantic Central Water (NACW) and South Atlantic Central Water (SACW) are represented by two water types each, and phosphate, silicate and nitrate are all used as an additional parameter with temperature and salinity, yielding three sets of independent solutions. Solutions from different parameters show similar vertical distributions but can differ considerably in absolute terms. This is believed to be caused by insufficient knowledge of nutrient values of pure NACW and SACW and by low range/precision ratios of nutrient determination.It is shown that isopycnal mixing analysis correctly describes the water mass distribution to lowest order, i.e. there is agreement between results from isopycnal and multi-parameter analysis at most stations within the error bounds which are inherent in the method and which are presently very high. Significant non-isopycnal mixing could be confirmed for only one station, situated on the continental slope in the area of the undercurrent of the Canary Current upwelling regime, and may be caused by active upwelling, increased lateral and vertical shear in the under-current, or internal waves interacting with the bottom. Five stations do not yield oceanographically acceptable solutions, and an attempt is made to include a coastal water mass in the analysis in order to improve the result for these stations, i.e. three-parameter analysis for NACW and SACW is replaced by four-parameter analysis for NACW, SACW and coastal water by combining temperature and salinity with phosphate and silicate or with nitrate and silicate simultaneously (the combination phosphate and nitrate is degenerate because both nutrients are linearly correlated). This indeed improves the results, indicating the presence of coastal water at those stations, but accumulation of errors inhibits quantitative conclusions.  相似文献   
9.
Vitrinite reflectance (Rr), proximate analysis and carbon isotope composition (δ13C) have been used to characterise coal samples from two zones of Late Carboniferous sediments (Gastern and Ferden) in the Aar massif where they are penetrated by the Lötschberg base tunnel (constructed between 1999 and 2005). Samples are characterised by variable ash yields (21.7–93.9%; dry basis); those with ash yields of less than ~50% and with volatile matter content (V;dry ash-free basis) within the limits 2 < V% ≤ 8 are anthracite. Values of Rr range from 3.89% to 5.17% and indicate coalification to the rank of anthracite and meta-anthracite in both Gastern and Ferden Carboniferous zones. Samples of anthracite and shale from the Gastern Carboniferous exhibit a relatively small range in δ13C values (–24.52‰ to –23.38‰; mean: –23.86‰) and are lighter than anthracite samples from the Ferden Carboniferous (mean: –22.20‰). The degree of coalification in the Gastern and Ferden Carboniferous zones primarily depends on the maximum rock temperature (T) attained as a result of burial heating. Vitrinite reflectance based estimates of T range from ~290° –360 °C. For a proposed palaeogeothemal gradient of 25 ° C/km at the time of maximum coalification the required overburden is attributable to relatively thin autochtonous Mesozoic/Cenozoic sedimentary cover of the Aar massif and Gastern granite and deep tectonic burial beneath advancing Helvetic, Ultrahelvetic and Prealpine (Penninic) nappes in Early Oligocene to Miocene.  相似文献   
10.
This paper deals with the derivation of the convective mixing height and the characteristic convective velocity w * from profiles of w measured by sodar. The parameters were obtained by fitting an analytical profile to the observed data. Results were compared with values obtained by the meteorological preprocessor of a dispersion model and from noon radiosoundings. In addition, a Monte Carlo method was applied to study the influence of measurement errors. It turned out that it is inherently difficult to determine the depth of deep mixed layers from sodar measurements with a limited range, although the determination of w * should be possible. However, a significant underestimation of w , and thus w *, was found, which is probably due to disproportional sampling of updrafts and downdrafts.  相似文献   
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号