全文获取类型
收费全文 | 2306篇 |
免费 | 453篇 |
国内免费 | 276篇 |
专业分类
测绘学 | 99篇 |
大气科学 | 54篇 |
地球物理 | 703篇 |
地质学 | 1206篇 |
海洋学 | 110篇 |
天文学 | 15篇 |
综合类 | 99篇 |
自然地理 | 749篇 |
出版年
2024年 | 13篇 |
2023年 | 43篇 |
2022年 | 83篇 |
2021年 | 95篇 |
2020年 | 103篇 |
2019年 | 92篇 |
2018年 | 69篇 |
2017年 | 82篇 |
2016年 | 103篇 |
2015年 | 86篇 |
2014年 | 111篇 |
2013年 | 123篇 |
2012年 | 116篇 |
2011年 | 116篇 |
2010年 | 104篇 |
2009年 | 135篇 |
2008年 | 158篇 |
2007年 | 131篇 |
2006年 | 116篇 |
2005年 | 100篇 |
2004年 | 128篇 |
2003年 | 114篇 |
2002年 | 89篇 |
2001年 | 86篇 |
2000年 | 107篇 |
1999年 | 72篇 |
1998年 | 76篇 |
1997年 | 67篇 |
1996年 | 49篇 |
1995年 | 45篇 |
1994年 | 46篇 |
1993年 | 40篇 |
1992年 | 44篇 |
1991年 | 34篇 |
1990年 | 24篇 |
1989年 | 17篇 |
1988年 | 10篇 |
1987年 | 1篇 |
1986年 | 4篇 |
1985年 | 1篇 |
1981年 | 1篇 |
1975年 | 1篇 |
排序方式: 共有3035条查询结果,搜索用时 109 毫秒
61.
介绍了当前湖泊水下地形测量的一般方法和作业过程。针对逐点插入构建不规则三角网算法,本文提出了效率改正算法和格网索引号快速计算算法。基于不规则三角网,给出了湖泊水下数字高程模型的一般应用模型——任意点高程计算、填挖方计算模型及等深线计算模型。 相似文献
62.
Multi-parameter studies (stable isotopes in carbonate and organic matter, pigment,organic carbon and nitrogen contents) from a 660-yr continuous sediment core from Lake Cheng-hai, a closed, eutropic lake in southern China, provide information on lake historical eutrophi-cation. During the last 660 years, great changes have taken place in productivity and eutrophi-cation of Lake Chenghai in response to human activities. In 1690, the productivity of the lakebegan to increase as Lake Chenghai became closed from agriculture in the lake‘‘ s watershed. In 1942, Lake Chenghai evolved to eutrophic state, marked by an increase in organic carbon, ni-trogen, CaC03, pigment contents and obvious negative values of stable isotopes, which is more or less simultaneous with the large-scale population immigration during the period. In 1984, in-tensive human activities induced modern lacustrine productivity and eutrophic level. Human-in-duced trophic changes during the past few decades have affected the Lake Chenghai ecosystem tosuch an extent that it has never experienced before in the last 660 years. 相似文献
63.
莱州湾南岸平原是指西起小清河口,东至胶莱河口的广大沿岸地区,这一地区近年来是我国工农业发展较快的地区,也是我国地下咸水入侵较为严重的地区。历史上,莱州湾南岸平原地区曾有一些湖泊存在,如巨淀湖、黑冢泊、别画湖,但现在早已荡然无存了。研究这些古湖泊的消亡原因对于恢复该区古地理环境以及确立湖迹区今后的发展方向具有十分重要的意义。本文运用查阅历史文献、地层剖面分析、地名考证、遥感解译等多种方法,对莱州湾南岸古湖泊的消亡原因进行了研究与分析,并指出该区古湖泊消亡的原因是气候变干、河流变迁、人类活动影响等,其中气候变化是古湖泊消亡的根本原因,河流变迁是古湖泊消亡的直接原因,而人类活动则加速了古湖泊消亡的进程。 相似文献
64.
65.
Following recent applications of numerical modelling and remote sensing to the thermal bar phenomenon, this paper seeks to review the current state of knowledge on the effect of its circulation on lacustrine plankton ecosystems. After summarising the literature on thermal bar hydrodynamics, a thorough review is made of all plankton observations taken in the presence of a thermal bar. Two distinct plankton growth regimes are found, one with production favoured throughout the inshore region and another with a maximum in plankton biomass near the position of the thermal bar. Possible explanations for the observed distributions are then discussed, with reference to numerical modelling studies, and the scope for future study of this interdisciplinary topic is outlined. 相似文献
66.
67.
The Franz Josef Glacier, Westland, New Zealand, has a history of catastrophic sediment‐laden outburst ?oods associated with extreme rainfall events when the glacier toe is advanced over its own sediments. Consideration of these events and inspection of recent sediment deposits suggest that there are three distinct modes of outburst. The ?rst is associated with fans fed by over?ow along the glacier margin. As the glacier has advanced across its own fore?eld gravels, it is inferred that the primary drainage conduit has developed a reach of negative slope. In high ?ows massive boulders can block the conduit, trapping lesser clasts. The resulting backup of water causes over?ows through marginal moulins, producing the fan type of deposit. The second type of outburst deposits massive imbricated boulders at a greater or lesser distance from the glacier portal. In this case, pressure buildup drives the blockage out of the portal where the boulders deposit. Smaller materials are generally carried away. The third type consists of very shallow ?ows, and produces massive gravel deposits of uncertain provenance. In this condition, the excess pressure in the conduit results in slight uplift of the glacier and widespread discharge of water and sediment below the glacier snout; gravels and smaller sediments are laid down in a massive deposit across the fore?eld. The massive, boulder‐veneered deposit from the December 1995 outburst is interpreted in the light of the above mechanisms as a hyperconcentrated ?ow deposit from hydraulic jacking, overlain by boulders emplaced by a subsequent conduit outburst. A possible association of outbursts with the present advanced position of the glacier is suggested. Copyright © 2003 John Wiley & Sons, Ltd. 相似文献
68.
By analysing a series of four successive thin‐sections from a ceramic clay that was subjected to uniaxial compression, we were able to monitor the development of microstructures in a fine‐grained sediment. The artificially induced microstructures, such as unidirectional clay reorientations and linear and circular grain arrangements, are identical to features that have been observed in thin‐sections of subglacially deformed tills, and therefore may be used as representative analogues. We argue that the structures, reflecting slip, planar shear displacements as well as rotational movements, can be explained by assuming a Coulomb‐plastic response to imposed shear. We conclude that sediments subjected to subglacial deformation behave as Coulomb materials, at least during the final stages of the deformation. The present study bridges the gap between field studies, experimental studies and theoretical modelling. The microscopic observations assist in visualising inferred subglacial processes and facilitate up‐ and downscaling between diverse methodological approaches. Copyright © 2003 John Wiley & Sons, Ltd. 相似文献
69.
根据西藏纳木错及邻区发现的多处湖岸阶地和高位湖相沉积,确定了藏北高原古大湖的存在。水准测量表明,在纳木错沿岸发育了6级湖岸阶地,以及拔湖48~139.2m的高位湖相沉积;在拔湖26m以下,发育有8~30条湖岸堤;一条明显的湖蚀凹槽则集中出现在拔湖17.5~19.8m的高度上,与纳木错和仁错的分水垭口的高度相当。纳木错沿岸和邻区湖相或湖滨相沉积物的铀系年龄测定表明,高位湖相沉积形成于115.9~71.8kaB.P.的晚更新世早期;第6至第2级阶地形成于53.7~28.2kaB.P.的晚更新世中晚期;与湖蚀凹槽相当的湖滨相沉积则稍早于29.3kaB.P.;第2至第1级阶地,14C测定结果为2350~10390aB.P.。 相似文献
70.
鄱阳湖地区土壤,植被光谱混合模型的研究 总被引:12,自引:1,他引:12
本文针对鄱阳湖地区的土壤、植被的特点设计了一套非线性混合光谱模型、较好了地预测了实际的混合光谱,从预测精度上看,要优于传统的线性混合光谱模型。 相似文献