全文获取类型
收费全文 | 55389篇 |
免费 | 5959篇 |
国内免费 | 8588篇 |
专业分类
测绘学 | 3876篇 |
大气科学 | 8577篇 |
地球物理 | 12133篇 |
地质学 | 26972篇 |
海洋学 | 4858篇 |
天文学 | 2966篇 |
综合类 | 5269篇 |
自然地理 | 5285篇 |
出版年
2024年 | 179篇 |
2023年 | 576篇 |
2022年 | 1484篇 |
2021年 | 1764篇 |
2020年 | 1401篇 |
2019年 | 1658篇 |
2018年 | 6088篇 |
2017年 | 5259篇 |
2016年 | 4164篇 |
2015年 | 1897篇 |
2014年 | 2154篇 |
2013年 | 1956篇 |
2012年 | 2822篇 |
2011年 | 4526篇 |
2010年 | 3911篇 |
2009年 | 4077篇 |
2008年 | 3503篇 |
2007年 | 3834篇 |
2006年 | 1361篇 |
2005年 | 1413篇 |
2004年 | 1295篇 |
2003年 | 1299篇 |
2002年 | 1137篇 |
2001年 | 979篇 |
2000年 | 1124篇 |
1999年 | 1490篇 |
1998年 | 1205篇 |
1997年 | 1124篇 |
1996年 | 1037篇 |
1995年 | 909篇 |
1994年 | 787篇 |
1993年 | 714篇 |
1992年 | 563篇 |
1991年 | 451篇 |
1990年 | 330篇 |
1989年 | 310篇 |
1988年 | 270篇 |
1987年 | 150篇 |
1986年 | 143篇 |
1985年 | 95篇 |
1984年 | 99篇 |
1983年 | 75篇 |
1982年 | 65篇 |
1981年 | 79篇 |
1980年 | 60篇 |
1979年 | 34篇 |
1978年 | 11篇 |
1977年 | 11篇 |
1976年 | 12篇 |
1958年 | 30篇 |
排序方式: 共有10000条查询结果,搜索用时 10 毫秒
961.
我国钾盐资源的开发利用 总被引:14,自引:3,他引:14
本文以基础统计资料为主,首先叙述了我国钾盐资源的基本情况及其分布特点和勘查程度,介绍国内钾资源开发利用的现状,就如何开发利用我国钾资源,解决国内钾肥短缺问题提出了一些建议. 相似文献
962.
重庆吴家湾铝土矿产于中二叠统梁山组(P2l)之下,呈假整合覆于中志留统韩家店组粉砂质页岩或中石炭统黄龙组灰岩之上。矿体产状与地层产状基本致,铝土矿呈土状、豆(鲕状)、致密块状、砾屑状。一水硬铝石为主要矿石矿物。控制铝土矿形成的主要因素为古环境、地形地貌、构造位置和地层。 相似文献
963.
Syenogranitic dykes in the north of Egypt’s Eastern Desert are of geological and economic interest because of the presence of magmatic and supergene enrichment of radioactive mineralization. Zircon crystal morphology within the syenogranitic dykes allows precise definition of sub-alkaline series granites and crystallized at mean temperature of about 637 °C. The growth pattern of the zircons suggest magmatic and hydrothermal origins of radioactive mineralization. Hydrothermal processes are responsible for the formation of significant zircon overgrowth; high U-zircon margins might have occurred contemporaneously with the emplacement of syenogranitic dykes which show anomalous uranium (eU) and thorium (eTh) contents of up to 1386 and 7330 ppm, respectively. Zircon chemistry revealed a relative increase of Hf consistent with decreasing Zr content, suggesting the replacement of Zr by Hf during hydrothermal activity. Visible uranium mineralization is present and recognized by the presence of uranophane and autunite. 相似文献
964.
965.
966.
967.
Jie Feng Youbing Hu Zhijia Li Tao Yang Pengfei Shi 《Stochastic Environmental Research and Risk Assessment (SERRA)》2014,28(8):1973-1984
To maintaining a health ecological environment in Three Gorges Reservoir (TGR) area, ecological shelter zones (ESZ) need to be built in the TGR shore zone urgently. Based on the implication and function of ESZ, this study first analyzed the relationships amongst three subsystems of the TGR area, including the upstream production-living land, the downstream reservoir water body, and the ESZ. Then a simple and practical hydrological environment model for controlling the eutrophication of the TGR water body was constructed to determine ESZ range of TGR. Additionally, based on the pollutant degradation efficiency of ESZ and the assimilative capacity of reservoir water body, a raster reverse tracking method was proposed to determine the range of ESZ. Thirdly, take Yangdu town in Zhongxian county as a typical region, the ESZ range under three scenarios of different rainfall intensity, degradation efficiency and inflow water quality that corresponding to the three decisive factors of defining ESZ range were discussed. Finally, the statistical laws of the ESZ’s width at each boundary points were discussed to facilitate the ESZ construction projects, and selected standardized rate at 70, 90, and 99 % were labelled as “General”, “Good” and “Excellent” level to represent the performance of the width of the ESZ range. In conclusion, it suggest “Good” level width as basic width of ESZ, and additionally a special protection zone should be put on upstream environment for the extreme large width at the boundary points. 相似文献
968.
969.
Surface soil moisture has been extensively studied for various land uses and landforms. Although many studies have reported potential factors that control surface soil moisture over space or time, the findings have not always been consistent, indicating a need for identification of the main factors. This study focused on the static controls of topographic, soil, and vegetation features on surface soil moisture in a steep natural forested headwater catchment consisting of three hillslope units of a gully area, side slope, and valley‐head slope. Using a simple correlation analysis to investigate the effects of the static factors on surface soil moisture at depths of 0–20 cm at 470 points in 13 surveys, we addressed the characteristics of surface soil moisture and its main controlling factors. The results indicated that the mean of surface soil moisture was in the decreasing order of gully area > valley‐head slope > side slope. The relationship between the mean and standard deviation of surface soil moisture showed a convex‐upward shape in the headwater catchment, a negative curvilinear shape in the gully area, and positive curvilinear shapes at the side and valley‐head slopes. At the headwater catchment and valley‐head slope, positive contributions of soil porosity and negative contributions of slope gradient and saturated hydraulic conductivity were the main controlling factors of surface soil moisture under wetter conditions, whereas positive contributions of topographic wetness index and negative contributions of vegetation density were the main controlling factors of surface soil moisture under drier conditions. At the side slope underlain by fractured bedrocks, only saturated hydraulic conductivity and vegetation density were observed to be the controlling factors. Surface soil moisture in the gully area was mainly affected by runoff rather than were static features. Thus, using hillslope units is effective for approximately estimating the hydrological behaviours of surface moisture on a larger scale, whereas dependency between the main static factors and moisture conditions is helpful for estimating the spatial distributions of surface moisture on a smaller scale. 相似文献
970.
Using chlorofluorocarbons (CFCs) and tritium (3H) to estimate groundwater age and flow velocity in Hohhot Basin,China 下载免费PDF全文
Jun Liu Zongyu Chen Wen Wei Yilong Zhang Zhenghong Li Fuliang Liu Hualiang Guo 《水文研究》2014,28(3):1372-1382
The concentrations of chlorofluorocarbons (CFC‐11, CFC‐12 and CFC‐113) and tritium (3H) content in groundwater were used to date groundwater age, delineate groundwater flow systems and estimate flow velocity in the Hohhot basin. The estimated young groundwater age is fallen in the bracket of 21 ~ 50 a and indicates the presence of two different age profiles and flow systems in the shallow groundwater system. Older age waters occur under the topographically low areas, where the aquifer is double‐layer aquifer system consisting of shallow unconfined‐semi‐confined aquifer and deep confined aquifer. This reflects long flow paths associated with regional flow. Groundwater (range from 21 to 34 years) in the north piedmont and east hilly areas, where the aquifer is a single‐layer aquifer consisting of alluvial fans, are typically younger than those in the low areas. The combination of CFCs dating with hydrogeological information indicates that both local and regional flow systems are present at the basin. The regional groundwater flow mainly flows from the north and east to the southwest, the local groundwater flow system occurs nearby the Hohhot city. The mean regional groundwater flow velocity of the shallow groundwater is estimated about 0.73 km/a. These findings can aid in refining hydrogeological conceptual model of the study area. Copyright © 2012 John Wiley & Sons, Ltd. 相似文献