全文获取类型
收费全文 | 1894篇 |
免费 | 134篇 |
国内免费 | 110篇 |
专业分类
测绘学 | 212篇 |
大气科学 | 22篇 |
地球物理 | 239篇 |
地质学 | 366篇 |
海洋学 | 71篇 |
天文学 | 2篇 |
综合类 | 166篇 |
自然地理 | 1060篇 |
出版年
2024年 | 6篇 |
2023年 | 15篇 |
2022年 | 46篇 |
2021年 | 86篇 |
2020年 | 77篇 |
2019年 | 74篇 |
2018年 | 58篇 |
2017年 | 91篇 |
2016年 | 72篇 |
2015年 | 70篇 |
2014年 | 90篇 |
2013年 | 138篇 |
2012年 | 119篇 |
2011年 | 122篇 |
2010年 | 67篇 |
2009年 | 112篇 |
2008年 | 106篇 |
2007年 | 108篇 |
2006年 | 112篇 |
2005年 | 110篇 |
2004年 | 68篇 |
2003年 | 86篇 |
2002年 | 71篇 |
2001年 | 53篇 |
2000年 | 37篇 |
1999年 | 34篇 |
1998年 | 23篇 |
1997年 | 20篇 |
1996年 | 9篇 |
1995年 | 13篇 |
1994年 | 7篇 |
1993年 | 7篇 |
1992年 | 4篇 |
1991年 | 1篇 |
1990年 | 3篇 |
1989年 | 1篇 |
1988年 | 4篇 |
1987年 | 4篇 |
1986年 | 4篇 |
1985年 | 3篇 |
1984年 | 2篇 |
1983年 | 2篇 |
1982年 | 2篇 |
1976年 | 1篇 |
排序方式: 共有2138条查询结果,搜索用时 15 毫秒
911.
Mette V.ODGAARD Peder K.BФCHER Tommy DALGAARD Jesper E.MOESLUND Jens-Christian SVENNING 《地理学报(英文版)》2014,(1)
Complex topography buffers forests against deforestation in mountainous regions.However,it is unknown if terrain also shapes forest distribution in lowlands where human impacts are likely to be less constrained by terrain.In such regions,if important at all,topographic effects will depend on cultural-historical factors and thus be human-driven(anthropogenic) rather than natural,except in regions where the general climate or extreme soils limit the occurrence of forests.We used spatial regression modeling to assess the extent to which topographic factors explain forest distribution(presence-absence at a 48×48 m resolution) in a lowland agricultural region(Denmark,43,075 km2) at regional and landscape scales(whole study area and 10×10 km grid cells,respectively),how landscape-scale forest-topography relationships vary geographically,and which potential drivers(topographic heterogeneity,forest cover,clay content,coastal/inland location) determine this geographic heterogeneity.Given a moist temperate climate and non-extreme soils all landscapes in Denmark would naturally be largely forest covered,and any topographic relationships will be totally or primarily human-driven.At regional scale,topographic predictors explained only 5% of the distribution of forest.In contrast,the explanatory power of topography varied from 0%–61% at landscape scale,with clear geographic patterning.Explanatory power of topography at landscape scale was moderately dependent on the potential drivers,with topographic control being strongest in areas with high topographic heterogeneity and little forest cover.However,these conditioning effects were themselves geographically variable.Our findings show that topography by shaping human land-use can affect forest distribution even in flat,lowland regions,but especially via localized,geographically variable effects. 相似文献
912.
随着土地利用向立体化、复杂化发展,不动产登记管理迫切需要向立体化模式转变。将三维景观构建技术用于不动产登记管理,能够立体直观地表现地、楼、房之间的空间关系。本文研究了将二维GIS数据用于查询分析、关联三维模型用于显示的二维向三维扩展的方式,具有一定的实践意义。 相似文献
913.
914.
渤海海岸带地区土地利用时空演变及景观格局响应 总被引:9,自引:0,他引:9
综合利用RS、GIS和景观生态学方法,以渤海海岸带地区1995、2000、2005和2008年土地利用分布图为基础,
分析了渤海海岸带地区近13年间的土地利用时空演变及其景观响应,得到以下结论:(1)渤海海岸带地区土地利用
年动态变化率在2000年—2005年间最大,为0.40%;2005年—2008年段次之;1995年—2000年间最小;(2)下辽河平
原、海河平原以及黄河三角洲地区为土地利用动态发生的主要区域;(3)监测期内,城乡、工矿、居民用地的面积扩
展明显,且主要来源于其周边的优质耕地,但在耕地流向城乡、工矿、居民用地的同时,有较大面积的林地和草地转
向耕地,因此监测期内耕地的总面积变化不大,海域向陆地土地利用类型的转化(即填海造陆)是该区域一种特殊的
土地利用动态类型,并随着时间推移速度越来越快;(4)整个区域在监测期内表现出多种土地利用类型(未利用地、
水域等)的小型斑块被整合,而优势土地利用类型(主要是耕地和城乡、工矿、居民用地)的大型斑块则积极向外扩
展的发展态势,整个景观表现出多样性和均匀度减小而优势度增加的趋势。 相似文献
915.
以曲阜市为研究区,利用2005年TM遥感影像,经过校正、人机交互目视解译得到该研究区空间景观结构矢量图,提取居民点斑块,然后利用景观生态学数量方法分析研究区农村居民点空间景观分布特征.研究表明,研究区农村居民点规模较小,分布零散,平原地区农村居民点平均面积为15.67 hm2,山区居民点平均面积为7.94hm2.这样的... 相似文献
916.
Francesc Ordines Gabriel JordàAntoni Quetglas Mar FlexasJoan Moranta Enric Massutí 《Continental Shelf Research》2011,31(17):1835-1844
Linking the abiotic and biotic traits of ecosystems is a critical step towards understanding their structure and functioning. Here we attempt to determine the connections between the hydrodynamics, benthic landscape and the associated fish communities on the coastal continental shelf off the Balearic Islands (western Mediterranean). Specifically we investigate the role the hydrodynamics play in shaping the benthic landscape, and whether the hydrodynamics affect the composition and structure of demersal fish communities. A realistic numerical model was used to establish the hydrodynamic characteristics of the area. The study area showed high hydrodynamic variability on a medium spatial scale (tens of km) in terms of mean water velocity (ū). Principal component analysis was used to determine the main gradients of macro-epibenthic variability. Redundancy analysis (RDA) was used to model the effect of the hydrodynamics on macro-epibenthic species. RDA was also used to model the effect of the hydrodynamics and macro-epibenthos on the abundance of the associated fish fauna, and on its biomass at a community level using biomass spectra classes. The results showed that the hydrodynamics had a significant influence on the distribution of both macro-epibenthic species and the associated fish species. The latter was also influenced by the macro-epibenthos. Fish size appeared to be a key attribute for the distribution of species across gradients of ū and macro-epibenthic change. Our findings can be applied in ecosystem-based fisheries management, as they show that it is necessary to take into account both the biotic and abiotic traits of the habitats when the habitat use and requirements of the associated species are defined. 相似文献
917.
采用时空相结合的分类方法来获取多时相土地利用/覆盖,有效减少了多时相遥感的时空不一致性。为探测时空不一致性对景观指标取值及其变化轨迹的影响,将时相独立分类方法和时空相结合分类方法进行了对比,四种常用的景观指标——斑块数(NP)、边缘密度(ED)、平均斑块大小(MPS)和平均形状指数(MSI)用来探测两种方法的差异。结果表明,时空不一致性不仅影响到景观指标取值,而且改变了景观指标的变化轨迹。 相似文献
918.
919.
920.
S. M. Hill 《Australian Journal of Earth Sciences》2013,60(2):217-232
The long‐term survival of regolith and landscape features of Mesozoic origins in southeastern Australia is supported by the sedimentary record, pre‐volcanic remnants, oxygen‐isotope signatures of secondary minerals, and the associated geomorphological context. The recognition of these ancient landscape remnants reflects the establishment of a major paradigm in Australian landscape studies after early interpretations emphasised a predominantly Late Cenozoic landscape history. The Mesozoic regolith and landscape remnants constrain interpretations of the evolution of the highlands in this region, indicating that Late Mesozoic and Cenozoic denudation did not extend beyond the complete removal of Mesozoic landscape features. Apatite fission track thermochronology interpretations invoke kilometre‐scale denudation levels across the southeastern highlands during the mid‐Cretaceous, which at first may appear contradictory to the geomorphological evidence of restricted denudation. Rather than necessarily being mutually exclusive interpretations, possible scenarios allowing for the preservation of Mesozoic palaeosurfaces along with kilometre‐scale denudation in the mid‐Cretaceous include: (i) exhumation of palaeosurfaces from beneath a thick sedimentary cover; (ii) truncation of formerly more extensive weathering profiles; and (iii) local‐scale variations in denudation. Local‐scale variations in denudation may not have been detected in previous studies due to dangers associated with overextending regional extrapolations and interpretations, as well as a tendency for the field basis of the different denudation models to emphasise different parts of the landscape. Field studies from areas where there has been localised deep incision into Mesozoic landscape remnants highlight the problem. Geomorphological studies have tended to emphasise areas of relative stability, featuring the preservation of regolith materials and the associated long‐term landscape record. In contrast, apatite fission track thermochronology interpretations may tend to emphasise a regional thermal history related to maximum denudation. Local variations in denudation leading to the preservation of Mesozoic palaeosurfaces have mainly been facilitated by localised lithological and structural controls on stream base‐levels and knickpoints, tectonic setting, and sedimentary and volcanic burial. When palaeolandscape interpretations are considered at the local scale, arguments proposing long‐term stability based on palaeolandscape remnants and apatite fission track thermochronology interpretations of large‐scale denudation may therefore not necessarily be contradictory. 相似文献