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701.
以许厂煤矿的应用为例,介绍了小波变换和二维分形技术的基本理论以及预测奥灰裂隙发育带的方法、步骤及效果。理论与实际分析表明,在预测奥灰裂隙发育带中,小波变换可以提高地震资料的分辨率和信噪比,二维分形参数有很高的参考价值,二者的结合为预测奥灰裂隙发育提供了一种有效的方法。 相似文献
702.
703.
本文从信息时代国家经济建设、社会发展和人民生活对测绘工作的需求出发,提出了精确测绘保障模式,论述了构建该模式的三大要素:地理空间信息、测绘信息技术装备、测绘科技人才,讨论了建立该模式的技术途径,旨在推进测绘信息化建设. 相似文献
704.
In this study, we determined pH, phosphorus content and the number of P-dis- solving/decomposing bacteria in relation to the depth in the sediment of Guanting reservoir in Beijing. The pH value was slightly increased from 8.0 in the surface to 8.5 in the bottle (69 cm in depth) of sediment. The highest P content, 1269 mg/kg, was detected in the 35 cm layer, followed by the 5 cm (993 mg/kg) and 69 cm (580 mg/kg) layers. The number of inorganic P-dissolving bacteria varied from 6(102 to 8(104 and the organic P-discomposing bacteria were from 1.9(103 to 6.3(104 per gram sediment in different depths, which were counted under 28℃ and 20℃ ( pH7.5 and 8.5. The number of P-dissolving/discomposing bacteria was directly correlated to the P content in each layer of sediments. The analysis of P-dissolving/decomposing ability of bacteria showed that some of these bacteria were also capable of accumulating P intracellularly. The intracellular P-accumulation was more efficient at lower temperature; in contrast, the activity of P-dissolving/decomposing was stronger at higher temperature. So the content of dissolved P in water body, or quality of water, could be affected by the change of temperature via the regulation of bacterial activity. On the basis of 16S rDNA sequencing, the 13 efficient P-dis- solving/decomposing bacteria were identified as Bacillus spp., Bacterium sp., Microbacterium sp., Paenibacillus sp. and Pseudomonas sp. 相似文献
705.
GIS支持下的新疆平原区地下水资源评价模型 总被引:1,自引:1,他引:1
在阐述地下水资源系统特征的基础上,采用水均衡的基本原理,在MAPGIS、RS、数据库和VBA面向对象开发技术支持下,构建地下水资源评价模型,评价模型主要应用了遥感信息、水文地质调查、水位水质观测及其他试验资料多源信息,综合考虑了影响地下水系统的多种因素,如含水层特征、水质、植被覆盖情况以及地下水开发利用状况.该评价方法同传统方法相比,具有速度快、精度高的优点.另外,基于GIS的评价模型更大的优势是数据更新时,便于模型重新评价,最终为水资源统一规划提供可靠的决策依据. 相似文献
706.
707.
In application to numerical analysis of geotechnical problems, the limit-state surface is usually not known in any closed form. The probability of failure can be assessed via the so-called reliability index. A minimization problem can naturally be formed with an implicit equality constraint defined as the limit-state function and optimization methods can be used for such problems. In this paper, a genetic algorithm is proposed and incorporated into a displacement finite element method to find the Hasofer–Lind reliability index. The probabilistic finite element method is then used to analyse the reliability of classical geotechnical systems. The performance of the genetic algorithm (GA) is compared with simpler probability methods such as the first-order-second-moment Taylor series method. The comparison shows that the GA can produce the results fairly quickly and is applicable to evaluation of the failure performance of geotechnical problems involving a large number of decision variables. 相似文献
708.
在研究了水文相关中利用最小二乘原理进行回归分析方法的基础上,指出了传统水文回归分析方法的使用条件、局限性和存在的问题。提出了不同性质的变量在回归分析时应区别对待的概念。结合水文观测的实际情况,研究了相关变量观测值均存在误差情况下,以变量的观测误差作权进行回归分析的概念,提出了建立基于最小二乘原理基础上的双加权回归模型,并研究了该模型的解算方法。同时推导了估计参数和预测值的误差估计公式,通过估计参数和模型误差的研究,有助于提高水文变量回归的精度和误差估计水平。 相似文献
709.
Recent tectonic stress field zoning in Sichuan-Yunnan region and its dynamic interest 总被引:7,自引:0,他引:7
In this paper, we have carefully determined the stress zones in the Sichuan-Yunnan region with reference to the in-situ stress data of hydraulic fracturing and the inverted fault slip data by using the step-by-step convergence method for stress zoning based on focal mechanism solutions. The results indicate that the tectonic stress field in the Sichuan-Yunnan region is divided into 3 stress zones by 2 approximately parallel NNW-trending stress transition belts. The area between the 2 belts is the Sichuan-Yunnan stress zone where the maximum principal stress σ1 is just in the NNW direction. The eastern boundary of Sichuan-Yunnan stress zone (the eastern stress transition belt) is basically consistent with the eastern boundary of Sichuan-Yunnan rhombic block. The western boundary of Sichuan-Yunnan stress zone (the western stress transition belt) is not totally consistent with the western boundary of Sichuan-Yunnan rhombic block. The northern segment of the western stress transition belt extends basically along the Jinshajiang fault and accords with the western boundary of Sichuan-Yunnan rhombic block, while its southern segment does not extend along the southwestern boundary of the rhombic block, i.e., Honghe fault and converge with the eastern stress transition belt, but stretches continuously in the NNW direction and accords with the Yingpanshan fault. We therefore consider that under the combined influence from the northward motion of India Plate, the southeastward shift of east Qinghai-Xizang Plateau and the strong obstruction of South China block, the tectonic stress field in the Sichuan-Yunnan region might not be totally controlled by the previous tectonic frame and new stress transition belt may have possibly formed. 相似文献
710.
NWP产品在强对流天气诊断分析中的应用 总被引:7,自引:2,他引:7
利用ECMWF、T213、T106数值预报产品及各物理量场,对已知中尺度系统发生发展的大尺度条件,预报中尺度环流出现的统计概率进行探讨:首先将武汉中心气象台过去总结的强对流天气模型与数值预报产品中的环流形势进行对比分析,当所预报的环流形势满足强对流天气模型时,认为大尺度条件将会促进中尺度天气的发生发展。再对数值预报产品中的有关物理要素场和值进行诊断分析,当所诊断的结果反映出有中尺度次级环流出现或有利中尺度对流天气发生时,最后对强对流天气落区、落点及降水性质进行诊断分析。同时,还利用AREM中尺度数值模式对2002年7月21~24日过程进行诊断分析,预报效果较好。,通过诊断分析,得出了强对流天气落区、落点及降水性质与各要素之间预报场和值的关系,同时也为今后精细化预报提供了启示和参考。 相似文献