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101.
地下水开采—地面沉降模型研究 总被引:27,自引:5,他引:22
本文建立三维流支--一维非线性固结地面沉降模型,在混合井流,降雨滞后补给,初始水头形成,人为边界刻画,水流-固结耦合及软土层固结滞后于地下水开采层水头变化等方面有所改进,所建模型用于苏州市,模拟出若干地面沉降重要特征,地面沉降中心偏离地下水漏斗中心,地面沉降动态滞后于地下水的水头动态,软土层渗透系数随固结过程的变化及头在软土层中的传递特征。 相似文献
102.
平扭耦联隔震体系的简化模型及有关参数变化的计算分析 总被引:5,自引:1,他引:5
李向真 《地震工程与工程振动》2005,25(3):163-166
本文根据隔震结构的动力学特点,提出了空间平扭耦联隔震结构简化计算模型,该模型仅有四个自由度,做定性分析和近似计算十分方便,力学概念明确可靠,文中并对这种体系的动力特性和反应,采用反应谱方法进行分析计算。还对平扭耦联隔震结构的重要特征参数对结构的动力特性和动力反应的影响,进行了较为全面的分析研究。 相似文献
103.
云南民族地区城市化与产业集群关系的研究 总被引:1,自引:0,他引:1
云南民族地区作为欠发达地区,在发展的过程中面临着很多的问题,这些问题无一不与城市化密切相关,而产业集群作为一种新的经济发展模式,显现出了它独特的优势,所以正确认识产业集群与城市化的互动关系,是云南民族区域要实现区域的协调发展的关键.产业集群与城市化是耦合发展的,在分析云南民族地区产业集群与城市化互动发展现状的基础上,云南必须选择符合自身发展的互动发展模式,最后提出云南城市化发展与产业集群互动发展的政策建议. 相似文献
104.
Data of neutral meridional wind obtained by the meteor radar at Esrange and data of temperature and pressure measured by the Sounding of the Atmosphere using Broadband Emission Radiometry (SABER) instrument on board the Thermosphere–Ionosphere–Mesosphere Energetics and Dynamics (TIMED) spacecraft were studied with respect to a day-to-day atmospheric variability with periods ranging from 1.5 to 5 days. The detailed analysis was carried out for February 2004. Perturbations of the atmospheric parameters at the examined periods appeared mainly as eastward-propagating waves of zonal wavenumbers 1 and 2. We suggested that these waves excited by the jet instability on both flanks of the polar-night jet in the upper stratosphere and mesosphere interact nonlinearly with each other, and this interaction generates secondary waves. The radar observed both primary and secondary waves at mesospheric heights. The data analysis supports this suggestion. Under conditions of weaker instability observed in February 2003 the perturbations of atmospheric parameters of periods ranging from 1.5 to 5 days had smaller amplitudes at heights of the mesosphere than those in February 2004. It was found that the Eliassen-Palm fluxes calculated for the waves generated by the jet instability were mainly downward directed. This result suggests a possible dynamical influence of the mesospheric layers on the lower atmospheric levels. 相似文献
105.
A probabilistic fog forecast system was designed based on two high resolution numerical 1-D models called COBEL and PAFOG.
The 1-D models are coupled to several 3-D numerical weather prediction models and thus are able to consider the effects of
advection. To deal with the large uncertainty inherent to fog forecasts, a whole ensemble of 1-D runs is computed using the
two different numerical models and a set of different initial conditions in combination with distinct boundary conditions.
Initial conditions are obtained from variational data assimilation, which optimally combines observations with a first guess
taken from operational 3-D models. The design of the ensemble scheme computes members that should fairly well represent the
uncertainty of the current meteorological regime. Verification for an entire fog season reveals the importance of advection
in complex terrain. The skill of 1-D fog forecasts is significantly improved if advection is considered. Thus the probabilistic
forecast system has the potential to support the forecaster and therefore to provide more accurate fog forecasts. 相似文献
106.
相位激电法(偶极-偶极)单频电磁耦合校正方法 总被引:2,自引:2,他引:2
主要介绍一种相位激电法(偶极—偶极,以下简称偶极)电磁耦合校正方法,其原理是将视电阻率近似视为均匀大地电阻率,利用均匀大地条件下偶极装置电磁感应响应的正演计算方法,算出电磁感应响应,再将其从观测的总响应中去除,从而达到电磁耦合校正的目的。 相似文献
107.
108.
《地理学报(英文版)》1996,(3)
I.IntroductionTherearealotofstudiesdealingwithhydrodwiaAncsoflakes,numericalsimulationoflakecurrentsystemst5,7,lO,l31,andwiti1windsystemsoverlakesandnumericalsimulationontheland-lake/seaormountain-valleybreeze[4,6,8].Usually,ti1emodelsinti1eatmosphericboundarylayerandinlakewaterweresimulatedseParately.InfaCt,theprocessesintheatmosphericboundarylayeroverlakesandti1eprocessesinthelakewaterareinteraCtedstronglyeachoti1er.Collecteddatashow,thatalmoStalllargelakes,marginalseas,estuariesandlagoon… 相似文献
109.
T. W. Dawson 《Geophysical Journal International》1996,124(2):577-590
The mode-matching method is used to obtain an exact analytical solution to the problem of B -polarization induction in two adjacent thin half-sheets, lying on a conducting layer that is terminated by a perfect conductor at finite depth. These components of the model represent, respectively, the Earth's conducting surface layers, crust, and mantle. In dimensionless variables, the model has three independent parameters, these being the two thin-sheet conductances and the layer thickness. The mode-matching solution obtained in this paper is shown to be identical lo that derived via the Wiener-Hopf method in a companion paper (Dawson 1996), and so provides additional verification of that solution. As was shown in the companion paper, the solution for the present model contains, as special limiting cases, those for three models considered earlier by various authors. The second part of the present paper addresses the solutions for the electric fields in the non-conducting half-space above the conductors, which represents the atmosphere. In the final part, sample numerical calculations are presented to illustrate the solution. 相似文献
110.