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951.
Emma L. Bredesen Darren G. Bos Kathleen R. Laird Brian F. Cumming 《Journal of Paleolimnology》2002,28(4):389-402
To investigate the impact of forest harvesting on lake ecosystems, six lakes (four impact, two reference) from central British Columbia, Canada were assessed using cladoceran remains preserved in the lake sediment cores. Two temporal resolutions were analyzed: a decadal scale for the past 70 years, and a high-resolution scale (2 year intervals for ten years before and after harvesting). Three lakes which experienced forestry activity in their watersheds in the early 1960s, and one lake which experienced forestry activityin the mid 1970s, showed subtle but statistically significant changes in cladoceran species composition following forest harvesting (analysis of similarity tests) at the decadal scale, whereas only two of these lakes showed significant changes at the higher resolution. These changes may be due to increased nutrient levels that might be associated with forest harvesting. The two reference lakes, which had not experienced any known large-scale anthropogenic watershed disturbances in the past century, showed no significant shifts in the cladoceran species assemblages at either temporal scale. 相似文献
952.
The influence of petrophysical properties on the salt weathering of porous building rocks 总被引:1,自引:0,他引:1
D. Benavente N. Cueto J. Martínez-Martínez M. A. García del Cura J. C. Cañaveras 《Environmental Geology》2007,52(2):215-224
The influence of pore structure, water transport properties and rock strength on salt weathering is evaluated by means of
a thorough rock characterisation and a statistical analysis. The pore structure was described in terms of its porosity, pore
size distribution (quantified by mean pore radius) and specific surface area, density and water transport was characterised
by means of water permeability (saturated flow) and capillary imbibition (unsaturated flow); whilst the rock strength test
was carried out using uniaxial compressive strength, compressional and shear wave velocities, dynamic elastic constants and
waveform energy and attenuation were obtained from the digital analysis of the transmitted signal. A principal component analysis
and a stepwise multiple regression model was carried out in order to examine the direct relationships between salt weathering
and petrophysical properties. From the principal component analysis, two main components were obtained and assigned a petrophysical
meaning. The first component is mostly linked to mechanical properties, porosity and density whereas the second component
is associated with the water transport and pore structure. Salt weathering, quantified by the percentage of weight loss after
salt crystallisation, was included in both principal components, showing its dependence on their petrophysical properties.
The stepwise multiple regression analysis found that rock strength has a predominant statistical weight in the prediction
of salt weathering, with a minor contribution of water transport and pore structure parameters. 相似文献
953.
煤中全硫测定是煤质分析的一项重要指标。本文从煤样的粒度和均匀性,载气流量,电解液的使用,电解池和电极片的处理,库仑测硫仪的校正等方面对应用库仑法测定煤中全硫应注意的问题及原因进行分析,以确保测定结果的准确性。 相似文献
954.
Based on a consistent interpretation of earthquake occurrence as a stochastic process I demonstrate that the mathematical model of Probabilistic Seismic Hazard Analysis (PSHA) as it is in use today is inaccurate and leads to systematic errors in the calculation process. These mathematical errors may be regarded as an important contributor to the unrealistic results obtained by traditional PSHA for low probabilities of exceedance in recent projects. 相似文献
955.
区域开发累积环境影响及其全幕景分析法评价 总被引:3,自引:0,他引:3
在分析区域开发活动及其特点的基础上,论述了区域开发累积环境影响及其累积效应.通过总结常用的累积环境影响评价方法的实质,考察传统幕景分析法评价累积环境影响的工作方法,提出广义的幕景分析法--"全幕景分析法",阐述其用于区域开发累积环境影响分析评价的工作程序与优势."全幕景分析法"可在区域开发累积环境影响评价中起到综合、优化、直观的作用. 相似文献
956.
957.
喀什地磁台数字与模拟记录K指数对比分析 总被引:1,自引:0,他引:1
介绍了喀什地磁台地磁数字记录K指数的计算机FM I测定方法和传统的模拟测定K指数方法,分析比较了数字和模拟测定K指数存在的差异和原因。与国家地磁台网2005年统计的平均数据进行了比较,数字记录测定比模拟测定的值更好,数字记录更真实、更准确地反映出地磁场活动状态,因此在实际量算K指数时应以数字测定为准。 相似文献
958.
959.
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
960.