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431.
胡晓娟 《测绘与空间地理信息》2016,(3)
兰州新区地理国情监测三维展示系统以兰州新区地理国情普查综合统计成果为基础,基于Skyline软件建立三维场景。在所建成的三维场景中叠加地理国情监测各类专题信息并设计展示效果,最后将三维场景封装入所开发的展示系统中,用以展示兰州新区的区位优势、地形地貌、总体规划、地理国情监测成果等内容。 相似文献
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本文以PDR—2记录仪构成的小型数字化地震观测系统为基础,从理论上对该系统的群延迟进行了分析,同时还进行了实际测算,发现在这种具有不太复杂电子线路的短周期地震观测系统中,群延迟的数值也是可观的。文章分析了它的特性及从中发现的信息还谈到了有关测试方法。 相似文献
434.
在“九五”科技重点项目“中国若干近代火山潜在喷发危险及其监测研究”项目起动之际,作者对于火山喷发危险的监测研究中的CT技术者进行调研,本文总结了这方面的研究3方法和思路,并介绍了中国在这方面的部分成果,展望今后的研究动向。 相似文献
435.
Data collected by monitoring suggest that the movement of mudslides essentially develops through alternating stages of undrained–drained
deformation. Undrained conditions are established as a consequence of landslide mobilisation or reactivation. Every acceleration
phase is followed by progressive deceleration associated with dissipation of excess pore pressure. This paper reports the
results of some simple numerical analyses performed to investigate the role of pore pressure on mudslide behaviour. 相似文献
436.
Measurement of effusion rate is a primary objective for studies that model lava flow and magma system dynamics, as well as
for monitoring efforts during on-going eruptions. However, its exact definition remains a source of confusion, and problems
occur when comparing volume flux values that are averaged over different time periods or spatial scales, or measured using
different approaches. Thus our aims are to: (1) define effusion rate terminology; and (2) assess the various measurement methods
and their results. We first distinguish between instantaneous effusion rate, and time-averaged discharge rate. Eruption rate
is next defined as the total volume of lava emplaced since the beginning of the eruption divided by the time since the eruption
began. The ultimate extension of this is mean output rate, this being the final volume of erupted lava divided by total eruption
duration. Whether these values are total values, i.e. the flux feeding all flow units across the entire flow field, or local,
i.e. the flux feeding a single active unit within a flow field across which many units are active, also needs to be specified.
No approach is without its problems, and all can have large error (up to ∼50%). However, good agreement between diverse approaches
shows that reliable estimates can be made if each approach is applied carefully and takes into account the caveats we detail
here. There are three important factors to consider and state when measuring, giving or using an effusion rate. First, the
time-period over which the value was averaged; second, whether the measurement applies to the entire active flow field, or
a single lava flow within that field; and third, the measurement technique and its accompanying assumptions. 相似文献
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438.
Evanthia Lekka Ifigenia Kagalou Maria Lazaridou‐Dimitriadou Triantafilos Albanis Vasileios Dakos Dimitra Lambropoulou Vasilis Sakkas 《洁净——土壤、空气、水》2004,32(3):175-188
In the present study, the water quality of Kalamas river (NW Greece) was evaluated using physicochemical and hydromorphological parameters and benthic macroinvertebrates. Statistical analyses (Cluster and FUZZY analyses) were performed and two biotic scores (BMWP' and HS) were used in order to classify the sites according to water quality. Kalamas river appeared to have excellent tomoderate water quality at all sampling sites except one (close to the delta area) which was ”fairly or significantly polluted”. During the low flow season water quality appeared poorer than during the high flow season. The ecological parameters (hydromorphological, chemical, and biological) used for this integrated approach are the ones proposed by the New Water Directive 2000/60 EC for an efficient surveying monitoring of running waters. 相似文献
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