全文获取类型
收费全文 | 1494篇 |
免费 | 258篇 |
国内免费 | 390篇 |
专业分类
测绘学 | 62篇 |
大气科学 | 318篇 |
地球物理 | 351篇 |
地质学 | 787篇 |
海洋学 | 250篇 |
天文学 | 74篇 |
综合类 | 157篇 |
自然地理 | 143篇 |
出版年
2024年 | 13篇 |
2023年 | 22篇 |
2022年 | 58篇 |
2021年 | 85篇 |
2020年 | 75篇 |
2019年 | 63篇 |
2018年 | 57篇 |
2017年 | 69篇 |
2016年 | 81篇 |
2015年 | 60篇 |
2014年 | 89篇 |
2013年 | 74篇 |
2012年 | 63篇 |
2011年 | 84篇 |
2010年 | 75篇 |
2009年 | 85篇 |
2008年 | 73篇 |
2007年 | 60篇 |
2006年 | 47篇 |
2005年 | 51篇 |
2004年 | 47篇 |
2003年 | 47篇 |
2002年 | 56篇 |
2001年 | 56篇 |
2000年 | 53篇 |
1999年 | 82篇 |
1998年 | 64篇 |
1997年 | 67篇 |
1996年 | 60篇 |
1995年 | 46篇 |
1994年 | 49篇 |
1993年 | 34篇 |
1992年 | 55篇 |
1991年 | 26篇 |
1990年 | 19篇 |
1989年 | 23篇 |
1988年 | 22篇 |
1987年 | 13篇 |
1986年 | 13篇 |
1985年 | 9篇 |
1984年 | 8篇 |
1983年 | 5篇 |
1982年 | 1篇 |
1981年 | 1篇 |
1979年 | 1篇 |
1954年 | 1篇 |
排序方式: 共有2142条查询结果,搜索用时 15 毫秒
1.
Based on energy balance equation and mass transfer equation, a general model to estimate actual evaporation from non-saturated
surfaces was derived. Making use of two concepts, “relative evaporation” and “relative drying power”, a relationship was established
to account for the departure from saturated conditions. Using this model, the actual evaporation (evapotranspiration) can
be calculated without the need of potential evaporation estimation. Furthermore, the model requires only a few meteorological
parameters that are readily and routinely obtainable at standard weather stations. Based on nearly 30 years data of 432 meteorological
stations and 512 hydrological stations in China, in combined with GIS, nine typical river basins were selected. Using the
data of the selected river basins, the model was tested. The results show that the actual evaporation rate can be estimated
with an error of less than 10% in most areas of China, except few years in the Yellow River Basin. 相似文献
2.
3.
“Elementary bursts” refer to fine time structures on scales of tens of milli-second to a few seconds in flare radiations.
In this paper, we investigate temporal and spatial properties of elementary bursts by exploiting high-cadence Hα (100 ms)
and hard X-ray (125 – 500 ms) observations of an impulsive flare on March 16, 2000. We find that the time scale of 2 – 3 s
is likely an upper limit of the elementary bursts in this event, at which hard X-ray emissions observed by different instruments
correlate, low energy (≤30 keV) hard X-rays and Hα flux correlate, and Hα emissions at conjugate flare kernels correlate.
From our methods, and also largely limited by instrument resolutions, there is a weak indication of existence of sub-second
structures. With the high-resolution Hα data, we also attempt to explore the spatial structure of “elementary bursts” by determining
the average spatial displacement of Hα peak emission between successive “elementary bursts” defined from hard X-ray light
curves. We find that, at the time scale of 3 s, the smallest spatial scale, as limited by the imaging resolution, is about
0.4″. We discuss these results with respect to mechanisms of fragmented magnetic energy release. 相似文献
4.
Spatial pattern and regional types of rural settlements in Xuzhou City, Jiangsu Province, China 总被引:3,自引:1,他引:3
This paper principally focuses on the morphological differences,spatial pattern and regional types of rural settlements in Xuzhou City of Jiangsu Province in China.Using satellite images of Xuzhou City taken in 2007 and 2008 and models of exploratory spatial data analysis(ESDA) and spatial metrics,the paper conducts a quantitative analysis of the morphological pattern of rural settlements,and finds significant characteristics.First,rural settlements in Xuzhou City are significantly agglomerated in terms of their spatial distribution;meanwhile,there is significant variation in the geographical density distribution.Second,the scale of rural settlements in Xuzhou City is larger than the average in Jiangsu Province,and the histogram of the scale data is more even and more like a gamma distribution.There are a significant high-value cluster in the scale distribution,and local negative correlation between the scale and density distribution of rural settlements in Xuzhou City.Third,the morphology of rural settlements in Xuzhou City shows relative regularity with good connection and integrity,but the spatial variation of the morphology is anisotropic.Finally,according to the characteristics of density,scale,and form of rural settlements,the rural settlements of Xuzhou City are divided into three types:A high-density and point-scattered type,a low-density and cluster-like type and a mass-like and sparse type.The research findings could be used as the scientific foundation for rural planning and community rebuilding,particularly in less-developed areas. 相似文献
5.
Sedimentary evolution of the Holocene subaqueous clinoform off the southern Shandong Peninsula in the Western South Yellow Sea 总被引:1,自引:0,他引:1
Jiandong Qiu Jian Liu Yoshiki Saito Zigeng Yang Baojing Yue Hong Wang Xianghuai Kong 《中国海洋大学学报(英文版)》2014,13(5):747-760
Based on the stratigraphic sequence formed since the last glaciation and revealed by 3000 km long high-resolution shallow seismic profiles and the core QDZ03 acquired recently off the southern Shandong Peninsula, we addressed the sedimentary characteristics of a Holocene subaqueous clinoform in this paper. Integrated analyses were made on the core QDZ03, including sedimentary facies, sediment grain sizes, clay minerals, geochemistry, micro paleontology, and AMS 14 C dating. The result indicates that there exists a Holocene subaqueous clinoform, whose bottom boundary generally lies at 15–40 m below the present sea level with its depth contours roughly parallel to the coast and getting deeper seawards. The maximum thickness of the clinoform is up to 22.5 m on the coast side, and the thickness contours generally spread in a banded way along the coastline and becomes thinner towards the sea. At the mouths of some bays along the coast, the clinoform stretches in the shape of a fan and its thickness is evidently larger than that of the surrounding sediments. This clinoform came into being in the early Holocene(about 11.2 cal kyr BP) and can be divided into the lower and upper depositional units(DU 2 and DU 1, respectively). The unit DU 2, being usually less than 3 m in thickness and formed under a low sedimentation rate, is located between the bottom boundary and the Holocene maximum flooding surface(MFS), and represents the sediment of a post-glacial transgressive systems tract; whereas the unit DU 1, the main body of the clinoform, sits on the MFS, belonging to the sediment of a highstand systems tract from middle Holocene(about 7–6 cal kyr BP) to the present. The provenance of the clinoform differs from that of the typical sediments of the Yellow River and can be considered as the results of the joint contribution from both the Yellow River and the proximal coastal sediments of the Shandong Peninsula, as evidenced by the sediment geochemistry of the core. As is controlled mainly by coactions of multiple factors such as the Holocene sea-level changes, sediment supplies and coastal dynamic conditions, the development of the clinoform is genetically related with the synchronous clinoform or subaqueous deltas around the northeastern Shandong Peninsula and in the northern South Yellow Sea in the spatial distribution and sediment provenance, as previously reported, with all of them being formed from the initial stage of the Holocene up to the present. 相似文献
6.
吴秋凤 《广东海洋大学学报》2003,23(5):94-98
在阐述西部大开发中科技主导地位的基础上 ,从科技应用成效二重性的视角 ,探讨了关注西部科技伦理的必要性 ,并初步提出了西部大开发战略的科技伦理调控机制 相似文献
7.
1 IntroductionBacteriaandtheiractivitiesplayanimportantroleintheelementalbiogeochemicalcyclesandenergytransformingintheocean (Zhenetal.1 997) .DortchandPackard(1 989) proposedthatfoodwebsintheeutrophicwatersaredominatedbythebiomassofprimaryproducerswhilefoodwebsintheoligotrophicwatersaredominatedbythebiomassofmicrobes.Heterotrophicbacteriahadbeenshowntoplayanimportantroleinthedecompositionoflarge ,rapidlysinkingorganicparticleswithinandbelowtheeuphot iczone ,andfurthertoaffecttheelementaldyn… 相似文献
8.
Based on TM image data and other survey materials, this paper analyzed the spatiotemporal patterns of land use change in the
Bohai Rim during 1985–2005. The findings of this study are summarized as follows: (1) Land use pattern changed dramatically
during 1985–2005. Industrial and residential land in urban and rural areas increased by 643,946 hm2, of which urban construction land had the largest and fastest increase of 294,953 hm2 at an annual rate of 3.72%. (2) The outward migration of rural population did not prevent the expansion of residential land
in rural areas by 184,869 hm2. This increase reveals that construction of rural residences makes seriously wasteful and inefficient use of land. (3) Arable
land, woodland and grassland decreased at a rate of −0.02%, −0.12% and −1.32% annually, while unused land shrank by 157,444
hm2 at an annual rate of −1.69%. (4) The change of land use types showed marked fluctuations over the two stages (1985–1995 and
1995–2005). In particular, arable land, woodland and unused land experienced an inversed trend of change. (5) There was a
significant interaction between arable land and woodland. Industrial construction land in urban and rural areas showed a net
trend of increase during the earlier period, but only adjustment to its internal structure during the second period. The loss
of arable land to the construction of factories, mines and residences took place mainly in the fringe areas of large and medium-sized
cities, along the routes of major roads, as well as in the economically developed coastal areas in the east. Such changes
are closely related to the spatial differentiation of the level of urbanization and industrialization in the region. 相似文献
9.
全球主要河流流域碳酸盐岩风化碳汇评估 总被引:7,自引:0,他引:7
碳酸盐岩风化吸收的大气CO2主要以HCO3 -形式连续地经由河流从大陆输送到海洋,成为陆地生态系统的重要碳汇。目前主要河流流域的碳酸盐岩风化碳汇估算存在不确定性,分布格局尚不清晰。基于GEMS-GLORI全球河流数据库提供的全球10万km 2以上主要河流流域多年平均监测数据,利用水化学径流法估算出全球主要河流流域碳酸盐岩对CO2的吸收速率为0.43±0.15 Pg CO2 yr -1,平均CO2吸收通量为7.93±2.8 t km -2 yr -1。CO2吸收通量在不同气候带下差异显著,热带和暖温带CO2年吸收速率占全球主要河流流域年吸收速率的62.95%。冷温带CO2年吸收速率占全球主要河流流域的33.05%,仅次于热带地区。本文划分出全球CO2吸收通量的9个关键带,关键带的交汇处CO2吸收通量较高。喀斯特出露流域碳酸盐岩对CO2吸收通量的均值为8.50 t km -2 yr -1,约为非喀斯特流域的3倍。全球喀斯特出露流域碳酸盐岩风化碳汇在全球碳循环、水循环及碳收支平衡估算研究方面占据重要地位。 相似文献
10.
以闽江上游地区为例,在分析三明市2007—2016年森林碳密度时空动态的基础上,采用常规的以及改进后的道路网络测度指标,应用缓冲区分析方法和地理加权回归(Geographically Weighted Regression,GWR)模型,从线上和面上分别探讨道路网络对森林碳密度干扰的地理变异规律。结果表明:① 碳密度受到道路网络的较大影响,路网影响域内外碳密度的大小排序为:路网影响域内<整个研究区<路网影响域外;多条道路影响域重叠区的碳密度(26.330 Mg/hm2)明显低于单条道路影响域的碳密度(37.406 Mg/hm2);不同等级道路影响域的碳密度由大到小依次为县道>高速>省道>其它道路>国道>乡道。道路网络对2007—2016年碳密度的降低也有明显影响。② GWR模型的分析结果表明,路网对碳密度的影响程度随着样点的变化而变化,具有“空间非平稳性”。碳密度随着路网密度的增加而降低,而随着离道路距离的增加而增加。③ 研究区西北部和中部,GWR的回归系数及相关系数均较大,表明这2个区域道路对碳密度影响大且解释力皆较强。 相似文献