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141.
This paper describes certain procedures for deriving from the apparent resistivity data as measured by the Wenner electrode configuration two functions, known as the kernel and the associated kernel respectively, both of which are functions dependent on the layer resistivities and thicknesses. It is shown that the solution of the integral equation for the Wenner electrode configuration leads directly to the associated kernel, from which an integral expression expressing the kernel explicitly in terms of the apparent resistivity function can be derived. The kernel is related to the associated kernel by a simple functional equation where K1(λ) is the kernel and B1(λ) the associated kernel. Composite numerical quadrature formulas and also integration formulas based on partial approximation of the integrand by a parabolic arc within a small interval are developed for the calculation of the kernel and the associated kernel from apparent resistivity data. Both techniques of integration require knowledge of the values of the apparent resistivity function at points lying between the input data points. It is shown that such unknown values of the apparent resistivity function can satisfactorily be obtained by interpolation using the least-squares method. The least-squares method involves the approximation of the observed set of apparent resistivity data by orthogonal polynomials generated by Forsythe's method (Forsythe 1956). Values of the kernel and of the associated kernel obtained by numerical integration compare favourably with the corresponding theoretical values of these functions.  相似文献   
142.
淮北地区是皖北重要的铁铜成矿区,为系统总结该区矽卡岩型矿床成矿系列及成矿规律,基于近年来在该地区取得的找矿成果,通过系统研究已知矿床地质特征和成矿地质条件,结合成岩、成矿年代学特征,认为该区有3个成矿系列: 与高钾钙碱性侵入岩有关的矽卡岩型铁铜金成矿系列、与高钾钙碱性侵入岩有关的矽卡岩型铁-石膏成矿系列和与二长花岗岩有关的矽卡岩型铁-轻稀土成矿系列。分别论述了该区4个典型矿床的地质特征及成矿规律,认为该区为两阶段成矿,成矿空间受深断裂、弧形构造和岩浆岩带的共同控制。最终建立了该区早白垩世早期“前常式”、“杨桥孜式”和“王场式”铁多金属矿床和早白垩世晚期“旗杆楼式”铁-轻稀土矿床的区域成矿模式。  相似文献   
143.
Two families of symmetric periodic orbits of the planar, general, three-body problem are presented. The masses of the three bodies include ratios equal to the Sun-Jupiter-Saturn system and the periods of the orbits of Jupiter and Saturn are in a 25 resonance. The (linear) stability of the orbits are studied in relation to eccentricity and mass variations. The generation of the two families of periodic orbits follows a systematic approach and employs (numerical) continuation from periodic orbits of the first and second kind in the circular restricted problem to the elliptic restricted problem and from the circular and elliptic problems to the general problem through bifurcation phenomena relating the three dynamical systems. The approach also provides insight into the evolutionary process of periodic orbits continued from the restricted problems to the general problem.  相似文献   
144.
Mainly.three methods have been developed to calculate turbulence heat flux.They are eddy covariance method,Bowen ratio/energy balance method and aerodynamic method.In this paper, all the three methods have been used to calculate sensible heat flux,latent heat flux and imbalance energy near the surface with the experiment data of EBEX-2000.Then comparisons of the three methods and some possible explanations of the surface imbalance energy are given.  相似文献   
145.
位于松辽盆地南部某油气田边缘一个油气显示井的磁性测量结果表明,岩石具有明显的磁性变异结构特征.以磁化率(κ)为例,在低缓的背景磁性上主要呈现高强度与中等强度的2类异常:大于400×10-5为强磁性,100×10-5~150×10-5为中等强度磁性.结合录井资料与地球化学分析解释可知,强磁性异常主要位于取样间隔的底部干层区,少数样品位于浅部油气显示层;中等强度异常主要位于2 700 m附近的油气显示层.岩石磁性与地球化学成分对应分析表明,油气显示层岩石的C1和C2成分与磁化率 (κ)、饱和磁化强度 (Js) 和饱和等温剩余磁化强度(SIRM)之间呈明显的正相关,与内禀矫顽力(Hc)为逆相关,而干层岩石相关性不明显.矿物成分分析显示,岩石中主要含铁矿物为磁铁矿、磁赤铁矿、赤铁矿、黄铁矿和菱铁矿.其中磁赤铁矿主要分布在具有中等磁性强度的油气显示层,而高含量(最高含量达12.5%)的磁铁矿主要位于底部干层.磁赤铁矿与赤铁矿、黄铁矿及菱铁矿含量之间相关特征初步表明,自生磁赤铁矿可能主要来源于原地赤铁矿与黄铁矿.推测油气显示层岩石中磁性偏软的磁赤铁矿属于烃蚀变的产物,为烃微渗漏效应(或烟筒效应)的全空间形成机理提供了新证据.  相似文献   
146.
在全桥三维有限元模型基础上 ,进行了车载响应分析 ,得到全桥的动力响应 ,并与实测结果进行了分析对比 ;对疲劳危险部位建立局部有限元模型 ,并进行了局部应力分析。在结构健康安全监测系统实测数据基础上 ,得到应变循环标准块 ,用基于热点应力疲劳评估方法对危险部位进行了疲劳寿命评估。  相似文献   
147.
Nomograms for solving equations in multilayer and dipping layer cases are presented. The nomograms constructed are used to solve the following equations: I. Intercept-time formula. 2. Critical distance formula. 3. Critical angle formula. 4. Critical angle and dip angle formula. 5. Vertical depth formula.  相似文献   
148.
The South China Sea is a hotspot for regional climate research. Over the past 40 years, considerable im provement has been made in the development and utilization of the islands in the South China Sea, leading to a substantialchange in the land-use of the islands. However, research on the impact of human development on the local climate of theseislands is lacking. This study analyzed the characteristics of local climate changes on the islands in the South China Seabased on data from the Yongxing Island Observation Station and ERA5 re-analysis. Furthermore, the influence of urba nization on the local climate of the South China Sea islands was explored in this study. The findings revealed that the 10-year average temperature in Yongxing Island increased by approximately 1.11 °C from 1961 to 2020, and the contributionof island development and urbanization to the local warming rate over 60 years was approximately 36.2%. The linearincreasing trend of the annual hot days from 1961–2020 was approximately 14.84 days per decade. The diurnal tem perature range exhibited an increasing trend of 0.05 °C per decade, whereas the number of cold days decreased by 1.06days per decade. The rapid increase in construction on Yongxing Island from 2005 to 2021 led to a decrease in observedsurface wind speed by 0.32 m s –1 per decade. Consequently, the number of days with strong winds decreased, whereas thenumber of days with weak winds increased. Additionally, relative humidity exhibited a rapid decline from 2001 to 2016and then rebounded. The study also found substantial differences between the ERA5 re-analysis and observation data,particularly in wind speed and relative humidity, indicating that the use of re-analysis data for climate resource assessmentand climate change evaluation on island areas may not be feasible.  相似文献   
149.
The greater Agulhas Current is one of the most energetic current systems in the global ocean. It plays a fundamental role in determining the mean state and variability of the regional marine environment, affecting its resources and ecosystem, the regional weather and the global climate on a broad range of temporal and spatial scales. In the absence of a coherent in-situ and satellite-based observing system in the region, modelling and data assimilation techniques play a crucial role in both furthering the quantitative understanding and providing better forecasts of this complicated western boundary current system. In this study, we use a regional implementation of the Hybrid Coordinate Ocean Model and assimilate along-track satellite sea level anomaly (SLA) data using the Ensemble Optimal Interpolation (EnOI) data assimilation scheme. This study lays the foundation towards the development of a regional prediction system for the greater Agulhas Current system. Comparisons to independent in-situ drifter observations show that data assimilation reduces the error compared to a free model run over a 2-year period. Mesoscale features are placed in more consistent agreement with the drifter trajectories and surface velocity errors are reduced. While the model-based forecasts of surface velocities are not as accurate as persistence forecasts derived from satellite altimeter observations, the error calculated from the drifter measurements for eddy kinetic energy is significantly lower in the assimilation system compared to the persistence forecast. While the assimilation of along-track SLA data introduces a small bias in sea surface temperatures, the representation of water mass properties and deep current velocities in the Agulhas system is improved.  相似文献   
150.
Water is our most precious and arguably most undervalued natural resource. It is essential for life on our planet, for food production and economic development. Moreover, water plays a fundamental role in shaping weather and climate. However, with the growing global population, the planet’s water resources are constantly under threat from overuse and pollution. In addition, the effects of a changing climate are thought to be leading to an increased frequency of extreme weather causing floods, landslides and drought. The need to understand and monitor our environment and its resources, including advancing our knowledge of the hydrological cycle, has never been more important and apparent. The best approach to do so on a global scale is from space. This paper provides an overview of the major components of the hydrological cycle, the status of their observations from space and related data products and models for hydrological variable retrievals. It also lists the current and planned satellite missions contributing to advancing our understanding of the hydrological cycle on a global scale. Further details of the hydrological cycle are substantiated in several of the other papers in this Special Issue.  相似文献   
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