全文获取类型
收费全文 | 36722篇 |
免费 | 6493篇 |
国内免费 | 8919篇 |
专业分类
测绘学 | 2100篇 |
大气科学 | 8105篇 |
地球物理 | 9000篇 |
地质学 | 18261篇 |
海洋学 | 4777篇 |
天文学 | 1810篇 |
综合类 | 3859篇 |
自然地理 | 4222篇 |
出版年
2024年 | 181篇 |
2023年 | 676篇 |
2022年 | 1545篇 |
2021年 | 1840篇 |
2020年 | 1614篇 |
2019年 | 1666篇 |
2018年 | 1959篇 |
2017年 | 1791篇 |
2016年 | 2092篇 |
2015年 | 1684篇 |
2014年 | 2219篇 |
2013年 | 2046篇 |
2012年 | 1980篇 |
2011年 | 2065篇 |
2010年 | 2129篇 |
2009年 | 2102篇 |
2008年 | 1829篇 |
2007年 | 1759篇 |
2006年 | 1493篇 |
2005年 | 1366篇 |
2004年 | 1106篇 |
2003年 | 1042篇 |
2002年 | 1065篇 |
2001年 | 1026篇 |
2000年 | 1212篇 |
1999年 | 1678篇 |
1998年 | 1418篇 |
1997年 | 1497篇 |
1996年 | 1272篇 |
1995年 | 1155篇 |
1994年 | 1050篇 |
1993年 | 909篇 |
1992年 | 767篇 |
1991年 | 576篇 |
1990年 | 396篇 |
1989年 | 419篇 |
1988年 | 340篇 |
1987年 | 243篇 |
1986年 | 191篇 |
1985年 | 145篇 |
1984年 | 120篇 |
1983年 | 95篇 |
1982年 | 101篇 |
1981年 | 67篇 |
1980年 | 56篇 |
1979年 | 40篇 |
1978年 | 18篇 |
1977年 | 12篇 |
1976年 | 14篇 |
1958年 | 26篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
21.
中国旅游资源开发模式与旅游区域可持续发展理念 总被引:38,自引:2,他引:38
从旅游资源开发与区域关系的角度,指出国内旅游资源在开发方面存在着不同的理念与方法论模式,导致不同的区域旅游开发效果;从旅游可持续发展的原则出发,旅游区域开发在理论上应该建立多元趋势分析旅游开发理论体系,在实践上应建立鞠域“大旅游”的结构系统,并提出区域旅游开发的一些理论。 相似文献
22.
23.
24.
25.
用于新生代定年的Ar-Ar法标准样品候选样品初测结果 总被引:5,自引:1,他引:5
Ar Ar法定年的特点是必须要有一套年龄从小到大的标准样。迄今用于新生代定年的国内标准样极少。为满足新生代矿物Ar Ar法定年的需要,初选了一个标准样候选者BT 1透长石。样品总重366g,粒级6080目,纯度100%,缩分为100瓶,每瓶3 66g。Ar Ar阶段加热法初测结果为:全部12个阶段给出的总气体年龄为30 8±0 9Ma,412阶段视年龄十分接近,年龄谱平坦,对应的39Ar析出量达96%,坪年龄为29 6±0 4Ma,等时年龄为29 6±0 6Ma,MSWD=1 01。40Ar/36Ar初始值为293 6±3 9,与尼尔值295 5相当。重复测定结果为:全部气体年龄为31 0±0 9Ma(全部9个阶段),坪年龄为29 5±0 4Ma,等时年龄为29 4±0 6Ma,MSWD=1 94,40Ar/36Ar初始值为282 2±6 3。这些结果表明,BT 1透长石不含过剩氩,作为新生代定年的Ar Ar法标准样品候选者是较为理想的。 相似文献
26.
An experimental study on reduction of U (Ⅵ) by anaerobic bacteria, Shewane//a putrefaciens, is first reported here in China. The experimental conditions were: 35℃ and pH =7.0-7.4, corresponding to a physicochemical environments in which the sandstone-hosted interlayer oxidation-zone type uranium deposit formed in Northwest China's Xinjiang. Bacteria adopted in the present experiment, Shewanella putrefaciens, occur extensively in natural environment. Our study shows that nano-crystal precipitates of uraninite quickly occurred on the surface of the cells within one week. It was found that the pitchblende was characterized by a random arrangement of uraninite nanocrystals (2-4 nm) in it, significantly different from natural pitchblende in which uraninite nanocrystals are arranged in order. Finally, a possible mechanism of uranium biomineralization by microorganisms in the deposits is discussed. Our investigation may supply a technical train of thoughts for bioremediation of nuclear-contaminated water environments and for underground dissolving extraction of the sandstone-hosted uranium ores. 相似文献
27.
LIU Jihua SHI Xuefa Chen Lirong HUANG Yongyang Wang Yinxi Cui Yingchun BU Wenrui 《中国科学D辑(英文版)》2005,48(5)
Clay fractions in the non-calcareous surface sediments from the eastern Pacific were analyzed for clay minerals, REE and 143Nd/144Nd. Montmorillonite/illite ratio (M/I ratio), total REE contents ((REE), LREE/HREE ratio and cerium anomaly (бCe) may effectively indicate the genesis of clay minerals. Clay fractions with M/I ratio >1, бCe (0.85, (REE (400 μg/g, LREE/HREE ratio (4, and REE patterns similar to those of pelagic sediments are terrigenous and autogenetic mixed clay fractions and contain more autogenetic montmorillonite. Clay fractions with M/I ratio <1, бCe=0.86 to 1.5, ΣREE=200 to 350 μg/g, LREE/HREE ratio (6 and REE distribution patterns similar to that of China loess are identified as terrigenous clay fraction. The 143Nd/144Nd ratios or (э)Nd values of clay fractions inherit the features of terrigenous sources of clay minerals. Clay fractions are divided into 4 types according to (э)Nd values. Terrigenous clay minerals of type I with the (э)Nd values of -8 to -6 originate mainly from North American fluvial deposits. Those of type II with the (э)Nd values of -9 to -7 are mainly from the East Asia and North American fluvial deposits. Those of type III with (э)Nd values of -6 to -3 could come from the central and eastern Pacific volcanic islands. Those of type IV with (э)Nd values of -13 to -12 may be from East Asia eolian. The terrigenous and autogenetic mixed clay fractions show patchy distributions, indicating that there are volcanic or hot-spot activities in the eastern Pacific plate, while the terrigenous clay fractions cover a large part of the study area, proving that the terrigenous clay minerals are dominant in the eastern Pacific. 相似文献
28.
SHA Liqing ZHENG Zheng TANG Jianwei Wang Yinghong ZHANG Yiping CAO Min WANG Rui Liu Guangren WANG Yuesi SUN Yang 《中国科学D辑(英文版)》2005,48(Z1)
With the static opaque chamber and gas chromatography technique, from January 2003 to January 2004 soil respiration was investigated in a tropical seasonal rain forest in Xishuangbanna, SW China. In this study three treatments were applied, each with three replicates: A (bare soil), B (soil+litter), and C (soil+litter+seedling). The results showed that soil respiration varied seasonally, low from December 2003 to February 2004, and high from June to July 2004. The annual average values of CO2 efflux from soil respiration differed among the treatments at 1% level, with the rank of C (14642 mgCO2· m-2. h-1)>B (12807 mgCO2· m-2. h-1)>A (9532 mgCO2· m-2. h-1). Diurnal variation in soil respiration was not apparent due to little diurnal temperate change in Xishuangbanna. There was a parabola relationship between soil respiration and soil moisture at 1% level. Soil respiration rates were higher when soil moisture ranged from 35% to 45%. There was an exponential relationship between soil respiration and soil temperature (at a depth of 5cm in mineral soil) at 1% level. The calculated Q1o values in this study,ranging from 2.03 to 2.36, were very near to those of tropical soil reported. The CO2 efflux in 2003was 5.34 kgCO2· m-2. a-1 from soil plus litter plus seedling, of them 3.48 kgCO2· m-2. a-1 from soil (accounting for 62.5%), 1.19 kgCO2· m-2. a-1 from litter (22.3%) and 0.67 kgCO2·m-2. a-1 from seedling (12.5%). 相似文献
29.
Science China Earth Sciences - Middle Permian palaeo-seamounts in the area of Bayan Har are generally composed of volcanic basement and carbonate cap. Basaltic lava, volcanic breecia and polymictic... 相似文献
30.