全文获取类型
收费全文 | 1370篇 |
免费 | 220篇 |
国内免费 | 424篇 |
专业分类
测绘学 | 157篇 |
大气科学 | 60篇 |
地球物理 | 388篇 |
地质学 | 1014篇 |
海洋学 | 158篇 |
天文学 | 88篇 |
综合类 | 75篇 |
自然地理 | 74篇 |
出版年
2024年 | 6篇 |
2023年 | 9篇 |
2022年 | 26篇 |
2021年 | 36篇 |
2020年 | 53篇 |
2019年 | 49篇 |
2018年 | 37篇 |
2017年 | 48篇 |
2016年 | 56篇 |
2015年 | 74篇 |
2014年 | 99篇 |
2013年 | 106篇 |
2012年 | 81篇 |
2011年 | 90篇 |
2010年 | 103篇 |
2009年 | 107篇 |
2008年 | 108篇 |
2007年 | 106篇 |
2006年 | 101篇 |
2005年 | 71篇 |
2004年 | 66篇 |
2003年 | 83篇 |
2002年 | 60篇 |
2001年 | 57篇 |
2000年 | 56篇 |
1999年 | 57篇 |
1998年 | 57篇 |
1997年 | 43篇 |
1996年 | 37篇 |
1995年 | 17篇 |
1994年 | 29篇 |
1993年 | 16篇 |
1992年 | 11篇 |
1991年 | 15篇 |
1990年 | 8篇 |
1989年 | 6篇 |
1988年 | 11篇 |
1987年 | 4篇 |
1986年 | 4篇 |
1985年 | 3篇 |
1984年 | 3篇 |
1983年 | 3篇 |
1982年 | 1篇 |
1971年 | 1篇 |
排序方式: 共有2014条查询结果,搜索用时 15 毫秒
101.
102.
形变反演模型的非线性平差 总被引:1,自引:0,他引:1
陶本藻 《武汉大学学报(信息科学版)》2001,26(6):504-508
阐述了反演问题参数估计的质量要求,将反演理论中的分辨率和精度与平差中的良好统计性质作了对比分析,为使反演参数得到良好估计,提出平差处理对策。针对反演问题经常是非线性模型,提出了非线性平差的几种方法,最后给出参数筛选的原则和相应的统计检验方法。 相似文献
103.
远场和超远场前兆的模拟实验研究 总被引:7,自引:0,他引:7
在岩石试件、传压块体(包括岩石和钢块)和压机架上布设应变观测点,观测研究它们在岩石试样破裂孕育过程中的变化特征。结果发现,岩样临破坏前除岩样上各个测点都出现异常变化外,同时较远处的测力元件、传压块体和压机架上的应变也出现了突变或扰动前兆异常。岩石试样外部测点的应变特征变化在极临近主破裂时才有反映。而岩样上的测点除极临近主破裂时有突变和扰动外在离主破裂较早时已有反映。岩石试样外的测点距岩样约25-90cm,约为破裂尺度的3-10(多)倍。这表明在孕震区以外很远的地方都可能出现前兆异常。并初步探讨了形成远场前兆的原因。 相似文献
104.
105.
106.
电感耦合等离子体质谱法同时测定地质样品中痕量碘溴硒砷的研究:Ⅱ.土壤及沉积物标准物质分析 总被引:11,自引:8,他引:11
样品用碳酸钠和氧化锌混合熔剂半熔,热水提取,然后用强酸性阳离子交换树脂将阴离子形式存在的分析元素与溶液中大量钠、锌等阳离子分离,采用电感耦合等离子体质谱法直接同时测定溶液中的碘、溴、硒、砷。用0.07mol/L的氨水溶液清洗进样系统,有效减少了碘等元素的记忆效应和清洗时间。方法检出限(10σ,DF=100)溴、碘分别为0.15和0.028μg/g,砷、硒分别为0.04和0.004μg/g。用土壤和沉积物等地质标准物质分析验证了方法的准确度和精密度,绝大多数分析结果在标准值的允许误差范围之内。样品10次测定的RSD为0.8%~2.8%。 相似文献
107.
108.
The need for full‐scale dynamic tests, which are recognized as the most reliable method to evaluate a structure's vibration properties, is increasing as new analysis techniques are developed that take into account the complex interaction phenomenons that occur in dam–reservoir–foundation systems. They are extremely useful to obtain reliable data for the calibration of newly developed numerical methods. The Earthquake Engineering and Structural Dynamics Research Center (CRGP) at the University of Sherbrooke has been developing and applying dynamic testing methods for large structures in the past 10 years. This paper presents the experimental evaluation of the effects of the varying water level on the dynamic response of the 180 m Emosson arch dam in Switzerland. Repeated forced‐vibration tests were carried out on the dam during four different periods of the reservoir's filling cycle during a one‐year span. Acceleration and hydrodynamic pressure frequency responses were obtained at several locations while the dam was subjected to horizontal harmonic loading. The variation of the resonant frequencies as a function of the reservoir level is investigated. A summary of the ongoing numerical correlation phase with a three‐dimensional finite element model for the dam–reservoir–foundation system is also presented. Copyright © 2001 John Wiley & Sons, Ltd. 相似文献
109.
This study integrated surface and subsurface stratigraphic data with geophysical logs and hydrogeologic data in order to
characterize the hydraulic properties of the Silurian dolomite in northeastern Wisconsin. Silurian stratigraphy consists of
predictable alternations of characteristic facies associations. A vertical profile of hydraulic conductivity, obtained from
short-interval packer tests in a core hole that penetrates a majority of the Silurian section, indicates that hydraulic conductivity
ranges over five orders of magnitude (10–1 to 10–6 cm/s). Matrix conductivity is generally low and varies with texture; the finer-grained restricted-marine and transitional
facies being less permeable than the coarser-grained open-marine facies. High-conductivity values are generally associated
with bedding-plane fractures, and fracture frequency is greater in the restricted-marine facies.
High-flow features in 16 wells were identified using fluid-temperature/resistivity and heat-pulse flowmeter logs. Natural-gamma
logs were used to identify the stratigraphic position of flow features in each well and to correlate flow features to specific
stratigraphic horizons. By combining stratigraphic, geophysical, and hydrogeologic data, 14 high-permeability zones within
the Silurian aquifer have been identified and correlated in wells more than 16 km apart. These zones parallel bedding, appear
most pronounced at contacts between contrasting lithologies, and are most abundant in restricted-marine lithologies.
Electronic Publication 相似文献
110.