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921.
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924.
分布式时变增益流域水循环模拟 总被引:55,自引:0,他引:55
针对分布式水文模拟的问题,结合河西走廊黑河流域实际资料条件,提出将水文循环空间数字化信息与水文系统理论相结合的分布式时变增益水循环模型 (DTVGM)。DTVGM将单元时变增益水文非线性模型(TVGM)拓广到由DEM划分的流域单元网格上建立非线性地表水产流模型,基于水量平衡方程和蓄泄方程建立土壤水产流模型,并应用运动波方法建立分级网格汇流模型。最后,以黑河干流山区流域为例应用DTVGM开展了实例研究,设计开发了模型系统。研究区域被划分为38 277个网格单元 (网格大小为500 m×500 m),在此基础上将流域划分为456级带状汇流区域。考虑到黑河干流山区的寒区特点,模型耦合了融雪径流模型。模拟结果表明,DTVGM既有分布式水文概念性模拟的特征,同时具有水文系统分析适应能力强的优点,能够在水文资料信息不完全或者有不确定性干扰条件获得比较好的分布式水文模拟效率,在黑河干流山区的应用能够较好地满足水资源管理的要求。 相似文献
925.
In this study, long‐term discharge data and climate records, such as temperature and precipitation during 1977–2006, have been used to define basin climatic and hydrologic regimes and changes. Discharge analyses at four key gauging stations (Eagle, Stevens Village, Nenana, and Pilot Station) in the Yukon River Basin show that the runoff in the cold season (November to April) is low with small variations, whereas it is high (28 500–177 000 ft3/s; 810–5000 m3/s) with high fluctuations in the warm season (May to October). The Stevens Village Station is in the upper basin and has similar changes with the flow near basin outlet. Flow increases in May (61 074 ft3/s; 1729 m3/s) and September (23 325 ft3/s; 660 m3/s); and decreases in July (35 174 ft3/s; 996 m3/s) and August (6809 ft3/s; 193 m3/s). Discharge in May at the Pilot Station (near the basin outlet) shows a positive trend (177 000 ft3/s; 5010 m3/s). Daily flow analyses show high fluctuation during the warm season and very low flow during the cold season; the 10‐year average analyses of daily flow at Pilot Station show a small increase in the peak and its timing shifted to a little earlier date. The annual flow, average of 227 900 ft3/s (6450 m3/s) with high inter‐annual fluctuations, has increased by 18 200 ft3/s (or 8%; 520 m3/s) during 1977–2006. From 1977 to 2006, basin air temperature in June has increased by 3.9 °F (2.2 °C) and decreased by 10.5 °F (5.8 °C) in January. A strong and positive correlation exists between air temperature in April and discharge in May, whereas a strong and negative correlation relates August temperature and September discharge. Negative trend during 1977–2006 is observed for precipitation in June (0.6 in.; 15 mm) with a confidence over 93%. Precipitation in August and September has strong and positive correlations with discharge in September and October at basin outlet; the precipitation in other months has weak correlation with the discharge. The mean annual precipitation during 1977–2006 increased by 1.1 in. (or 8%; 28 mm), which contributes to the annual flow increase during the study period. Copyright © 2012 John Wiley & Sons, Ltd. 相似文献
926.
我对白云鄂博铁铌稀土矿床的研究过程及往见新识 总被引:1,自引:1,他引:0
80年前,丁道衡先生奉命去西北进行古生物考查研究工作,取道乌蒙草原,突然看到荒漠大地上有一座高耸美丽的神山,作了旅游参观之举.走到山脚下,就看到很多黑黑的滚石,到山上,更见有大块致密的磁铁矿石和红绿条带相间的赤铁矿石,就这样偶然发现了白云鄂博大型铁矿床. 相似文献
927.
基于等价分析法评估溢油事故的自然资源损害 总被引:2,自引:0,他引:2
尽管国际公约和许多国家立法已将海上溢油事故导致的自然资源损失列入索赔范围,然而,在量化和货币化损害以及确定索赔和修复范围等方面尚未建立被广泛接受的计算方法。生境等价分析(Habitat Equivalency Analysis,HEA)和资源等价分析(Resource Equivalency Analysis,REA)是美国和欧盟应用于评估自然资源损害的理论方法,二者的关键假设是受损的生态服务损失和修复计划的服务收益应当相等。HEA结果依赖于生态服务价值标尺选择、服务价值水平、恢复曲线形状、修复计划时长以及贴现率等;REA结果受死亡生物数量和年龄组成的影响。HEA和REA的非货币形式结果补偿的并非生态环境,而是人类社会福祉。目前,一些货币化损失的方法已被提出,然而传统经济学家和生态经济学家之间存在争议。美国部分法庭承认HEA和REA方法,其结果为法庭索赔提供数据支持。如果将生态学和经济学原理结合考虑,将能够促进等价分析法的深入发展,推动索赔工作更加有理有据。 相似文献
928.
Quartz sandstone peak forest landforms of Zhangjiajie Geopark, northwest Hunan Province, China: pattern, constraints and comparison 总被引:1,自引:1,他引:0
Guifang Yang Mingzhong Tian Xujiao Zhang Zhenghong Chen Robert A. L. Wray Zhiliang Ge Yamin Ping Zhiyun Ni Zhen Yang 《Environmental Earth Sciences》2012,65(6):1877-1894
The Zhangjiajie Sandstone Peak Forest Geopark in northwest Hunan Province, China, is a comprehensive geopark containing many
spectacular quartz sandstone landforms, limestone karst landscapes and various other important geoheritage resources. It is
listed as a UNESCO World Geopark and is also part of the World Heritage Wulingyuan Scenic and Historic Interest Area for its
important landscape features. Many of the sandstone landforms, particularly the vast number of thin pillars or spires, are
very unusual and serve as the core landscapes of the geopark. But Zhangjiajie displays a diverse range of landform types,
exhibiting spectacular patterns and regular distributions. In this paper, the geomorphic traits, distribution pattern and
constraints of the sandstone landforms of the Zhangjiajie Geopark are examined. Our study indicates that in the outcropping
areas, the sandstones display four distinctive levels from 300 to 1,000 m above sea level, and these extend clearly from the
highest sandstone plateau platform to the center of the valleys. The high sandstone platforms developed close to a flat high-level
erosional surface, and subsequent erosion into this plateau has resulted in successively lower levels of landforms that transition
gradually from peak walls, peak clusters, peak forests and peak pillars to remnant peaks in the lower valley bottoms. The
form and distribution of the Zhangjiajie sandstone landforms are primarily dominated by the geological setting, particularly
the presence of brittle structures (fractures and joint sets) trending NNW, ENE and NE. Triggered by the episodic tectonic
movements, major streams and escarpments frequently occur along these structural directions, while some of the peak walls,
peak clusters and peak forests have their longer elongated axes corresponding to NE or NNW directions, with an increased density
of peak forms at the intersection of these fractures and joints. The geometry of the diverse sandstone landforms is also influenced
to a certain degree by the climatic, water system distribution, lithologic properties, biological process, meteorological
features and denudation processes. The suite of quartz sandstone landforms in Zhangjiajie can be compared with other sandstone
landscapes regionally, and our interpretation of the sandstone peak forest formation processes offers a significant contribution
to the study of topographic features and the geomorphic evolution of sandstone landscapes. 相似文献
929.
Jianqiang Zhang Peng Cui Yonggang Ge Lingzhi Xiang 《Environmental Earth Sciences》2012,65(4):1037-1047
Generally, pixels are the basic unit for assessment of landslide susceptibility. However, even if the results facilitate the
comparison, a pixel-based analysis does not clearly illustrate the distribution relationships. To eliminate this deficiency,
the concept of the Landslide Response Unit (LRU) is proposed in this study, for which adjacent pixels that have similar properties
are combined as a basic unit for susceptibility assessment. The Subao River basin, seriously impacted by the Wenchuan Earthquake,
was selected as the study area, and three factors including slope gradient, slope aspect, and slope shape, which have a significant
impact on landslides, were chosen to divide the basin into 25,984 LRUs. Then topographic, geologic, and distance factors were
applied for the landslide susceptibility evaluation. The logistic regression method was used to establish the susceptibility
assessing model by analyzing 2,000 susceptible LRUs and 2,000 un-susceptible LRUs. The model accuracy was defined in terms
of the ROC curve value and the κ value, 0.531 and 0.84, respectively. The susceptibility of landslides was divided into low,
moderate, high, and very high in Subao River basin, and 73% of historical landslides and all four new landslides are in the
highly susceptible zone and very highly susceptible zones. Finally, the LRUs with houses, farmlands, and roads prone to sliding
and burial hazard were assessed separately. On the basis of considering the potential movement directions of the LRUs, the
result found that 1,001 and 835 LRUs probably would be destroyed by slope sliding and landslide burial, respectively. 相似文献
930.