全文获取类型
收费全文 | 1696篇 |
免费 | 203篇 |
国内免费 | 284篇 |
专业分类
测绘学 | 249篇 |
大气科学 | 47篇 |
地球物理 | 374篇 |
地质学 | 667篇 |
海洋学 | 436篇 |
天文学 | 34篇 |
综合类 | 96篇 |
自然地理 | 280篇 |
出版年
2024年 | 10篇 |
2023年 | 26篇 |
2022年 | 50篇 |
2021年 | 69篇 |
2020年 | 79篇 |
2019年 | 63篇 |
2018年 | 54篇 |
2017年 | 58篇 |
2016年 | 59篇 |
2015年 | 65篇 |
2014年 | 74篇 |
2013年 | 154篇 |
2012年 | 83篇 |
2011年 | 84篇 |
2010年 | 79篇 |
2009年 | 105篇 |
2008年 | 103篇 |
2007年 | 99篇 |
2006年 | 85篇 |
2005年 | 69篇 |
2004年 | 65篇 |
2003年 | 70篇 |
2002年 | 66篇 |
2001年 | 62篇 |
2000年 | 50篇 |
1999年 | 54篇 |
1998年 | 48篇 |
1997年 | 53篇 |
1996年 | 29篇 |
1995年 | 41篇 |
1994年 | 31篇 |
1993年 | 30篇 |
1992年 | 20篇 |
1991年 | 11篇 |
1990年 | 15篇 |
1989年 | 16篇 |
1988年 | 10篇 |
1987年 | 15篇 |
1986年 | 6篇 |
1985年 | 6篇 |
1984年 | 3篇 |
1983年 | 5篇 |
1982年 | 1篇 |
1981年 | 2篇 |
1980年 | 1篇 |
1979年 | 3篇 |
1978年 | 1篇 |
1971年 | 1篇 |
排序方式: 共有2183条查询结果,搜索用时 31 毫秒
121.
利用水化学找铀,有成本低、效率高、速度快等特点,在寻找可地浸砂岩型铀矿也有明显的效果,但是在找铀过程中仅用水化学成份、氡含量、酸碱度和氧化还原电位等数值进行描述,说明它们与铀矿化的关系,这种单一因素不能综合反映与铀矿化的联系程度,以定量评价铀矿化与上述因素的关系,从而影响了水化学找矿的效果,通过模糊数学方法建立数学模型处理水化学数据,巳知可地浸砂岩型铀矿的特征值为参数进行定量评价未知区铀成矿的前景,使该方法成为今后铀矿预测中一种可靠有效的水文地质方法。 相似文献
122.
Large woody debris (LWD) is an integral component of forested streams of the Pacific Northwest and elsewhere, yet little is known about how far wood is transported and where it is deposited in streams. In this paper, we report the results of flume experiments that examine interactions among hydraulics, channel geometry, transport distance and deposition of floating wood. These experiments were carried out in a 1.22-m-wide×9.14-m-long gravel bed flume using wooden dowels of various sizes as surrogate logs. Channel planforms were either self-formed or created by hand, and ranged from meanders to alternate bars. Floating pieces tended to orient with long axes parallel to flow in the center of the channel. Pieces were deposited where channel depth was less than buoyant depth, typically at the head of mid-channel bars, in shallow zones where flow expanded, and on the outside of bends. We hypothesize that the distance logs travel may be a function of the channel's debris roughness, a dimensionless index incorporating ratios of piece length and diameter to channel width, depth and sinuosity. Travel distance decreased as the ratio of piece length to both channel width and radius of curvature increased, but the relative importance of these variables changed with channel planform. Large pieces can move further than our debris roughness models predict if greater than 50% of the active channel area is deeper than the buoyant depth of the piece, or if momentum is high enough to carry pieces across shallows. Our debris roughness model allows first-order prediction of the amount of wood transport under various channel geometries. 相似文献
123.
A New Coastal Marine Ecosystem Model Study Coupled with Hydrodynamics and Tidal Flat Ecosystem Effect 总被引:3,自引:0,他引:3
Akio Sohma Yasuyuki Sekiguchi Hiroshi Yamada Tatsuaki Sato Kisaburo Nakata 《Marine pollution bulletin》2001,43(7-12):187-208
A new coastal marine ecosystem model was developed, which was composed of pelagic and benthic ecosystems, and was applied to Mikawa Bay, Japan. This model deals with variations of biochemical and physical interactions among dissolved oxygen and C–N–P species (composition formed out of carbon, nitrogen and phosphorus elements) so that it resolves the flux dynamics of carbon, nitrogen, phosphorus and oxygen elements. The physical and biochemical mechanism figured in this model is constructed for the purpose of simulating the estuarine lower trophic ecosystem, in areas where the sea was too deep for light to reach the sea-bottom. As a result of coupling the benthic with pelagic system, the effect of process of sedimentation and nutrient diffusion back to the pelagic system could be indicated. In addition, by implementing the tidal flat ecosystem model's calculation result, the integrated model can include the effect of water purification in tidal flats where the light can reach the sea-bottom, and where sea-weed, sea grass and benthic algae exist. In this study, the model indicates that oxygen-depleted water exists at the sea-bottom especially in summer mainly caused by an increase of oxygen consumption in the benthic system and a decrease of the vertical mixing water process. Furthermore, by comparing the case – with the tidal flat ecosystem model and the case without it, the effect of water purification of tidal flat estuaries was indicated. From the viewpoint of a short time scale, the tidal flat has the potential to restrict red tide (rapid increase of phytoplankton), and from the viewpoint of a long time scale, it restricts the sedimentation of detritus. Restricting the sedimentation prevents oxygen-depleted water occurring in the coastal marine system of Mikawa Bay. 相似文献
124.
Pollani Annika Triantafyllou George Petihakis George Nittis Konstantinos Dounas Costas Christoforos Koutitas 《Marine pollution bulletin》2001,43(7-12):270-278
In this work the development and the application of an operational management tool for the Greek Seas is described. This tool consists of a three-dimensional floating pollutant prediction model coupled with a weather, a hydrodynamic and a wave model in order to track the movements and the spreading of the pollutants and indicate those coastal areas which might be affected. The tool is part of the Poseidon system which has been designed to provide real time data and forecasts for marine environmental conditions in the Greek Seas. In this paper, we present four case studies based on realistic scenarios that show the value of the application for long-term strategic planning and short-term decision making in oil spill accidents. 相似文献
125.
南水北调西线雅砻江调水工程温波引水枢纽坝址径流计算的研究 总被引:1,自引:2,他引:1
南水北调西线雅砻江调水工程(简称西线调水)是从长江的一级支流雅砻江上游区引水至黄河源头地区的跨流域调水工程,是补充黄河水资源不足与解决我国西北和华北部分地区干旱缺水的重大战略措施,由于引水枢纽坝址缺乏实测水文资料,我们依据附近孜水文站实测资料,采用一些非确定性的数理统计模型来计算温波引水坝址的设计年径流量,并对计算成果进行了合理性分析,结果表明,上述计算成果基本反映了温波引水坝址径流变化的客观情况,从而为南水北调西线雅砻江调水工程缺乏实测水文资料地区的水文计算提供了科学依据。 相似文献
126.
127.
Previous studies devoted to the morphology and hydrodynamics of ridge and runnel beaches highlight characteristics that deviate from those initially postulated by King and Williams (Geographical Journal, 1949, vol. 113, 70–85) and King (Beaches and Coasts, 1972, Edward Arnold). Disagreements on the morphodynamics of these macrotidal beaches include the position of the ridges relative to the mean neap and spring tide levels, the variation in the height of the ridges across the intertidal profile and, most importantly, whether the ridges are formed by swash or surf zone processes. The morphological characteristics of ridge and runnel beaches from three locations with varying wave, tidal and geomorphic settings were investigated to address these disagreements. Beach profiles from each site were analysed together with water‐level data collected from neighbouring ports. It was found that the ridges occur over the entire intertidal zone. On one site (north Lincolnshire, east England), the ridges are uniformly distributed over the intertidal beach, whereas on the two other sites (Blackpool beach, northwest England, and Leffrinckoucke beach, north France) there is some indication that the ridges appear to occur at preferential locations. Most significantly, the locations of the ridge crests were found to be unrelated to the positions on the intertidal profile where the water level is stationary for the longest time. It was further found that the highest ridges generally occur just above mid‐tide level where tidal non‐stationarity is greatest. These findings argue against the hypothesis that the ridges are formed by swash processes acting at stationary tide levels. It is tentatively suggested that the ridges are the result of a combination of swash and surf zone processes acting across the intertidal zone. Elucidation of the morphodynamic roles of these two types of processes, and other processes such as strong current flows in the runnels, requires further comprehensive field measurements complemented by numerical modelling. Copyright © 2001 John Wiley & Sons, Ltd. 相似文献
128.
129.
130.
Sea ice thickness measurement and its underside morphology analysis using radar penetration in the Arctic Ocean 总被引:5,自引:0,他引:5
Sea ice, as an important component of the Arctic climate system, has drawn significant sci-entific interest. Sea ice thickness and its morphology have dramatic impacts on ocean-atmos- phere-ice interactions[1—4], which directly affect the exchange proces… 相似文献