甘肃崆峒站新旧址对比观测资料分析     

王丽娜 《沙漠与绿洲气象(新疆气象)》2019,13(1):117-121

为了解甘肃崆峒国家基本气象站新旧址气象要素对比观测数据差异,选用2016年1～12月新站和旧站气温、气压、相对湿度、风向风速、降水量等要素资料进行对比分析,重点利用均值差异、相关与回归、显著性检验等统计方法分析了新旧测站气温差异及产生原因,结果表明：新址气温、气压均低于旧址,风速高于旧址,降水量、相对湿度差异大,变化无规律,其产生的主要原因是地理位置、海拔高度及观测场周边环境的不同造成;新址与旧址气温存在高度正相关,两站气温差异不显著,可以合并计算,研究结果可为资料使用者提供订正的依据。  相似文献   

Direct observation of complex Tóthian groundwater flow systems in the laboratory     

Xing Liang  Yu Liu  Menggui Jin  Xingchen Lu  Renquan Zhang 《水文研究》2010,24(24):3568-3573

Based on the theory of gravity‐driven groundwater flow systems, we have developed a complex Flow System Sand‐Box Model (FSM). It enables the visual observations of the development and characteristics and temporal evolution of complex Tóthian flow systems in the laboratory. The configuration of the regional, intermediate and local flow systems can be controlled and observed; hydraulic head, flow direction and travel time can be measured; and the scale and shape of the sub‐flow systems as well as the path lines and flow lines can be observed directly. The experiments demonstrate the Tóthian flow systems in a small basin with multiple sources and sinks. Greater local topographic (water table) undulation will lead to larger local flow systems. Greater regional and less local topographic undulation will enhance the development of intermediate and regional flow systems. In homogeneous media, increasing fluid‐potential differences between source and sink increase the spatial scale of the generated flow systems. The FSM is a useful teaching aid and experimental device to study and develop an intuitive insight into gravity‐driven groundwater flow systems. It helps to visualize and understand the hydraulic properties and controlling factors of Tóthian flow systems and may be used to study problems related to the chemical and temperature characteristics of the flow systems as well. Copyright © 2010 John Wiley & Sons, Ltd.  相似文献   

新安含镍基性岩体的岩石学,岩石化学及地球化学初步研究     

傅德彬 《吉林地质》1990,9(3):50-60

通过对新安含镍基性岩侵入体的岩石学、岩石化学与地球化学研究,认为它与赤柏松含镍基性岩体是同源、同期、产于不同部位的孪生岩体,一旦有暗色橄榄辉长苏长岩相大量出现,则具找矿远景。  相似文献   

Areal extent of the 1988 flood in Bangladesh: How much did the satellite imagery show?     

Harun Rasid  M. A. H. Pramanik 《Natural Hazards》1993,8(2):189-200

This paper presents the methods and results of visual interpretation of satellite imagery for estimating areal extent of the 1988 flood in Bangladesh. The main limitation of this method was that cloud-free images were not available for the peak flood period in the first week of September. Relatively cloud-free images on three selected dates in the last three weeks of September showed that areas of inundation on those dates ranged from 44000 to 60000 km² ± 5% (31 to 42% of Bangladesh). The Government of Bangladesh official estimates of the areal extent of flooding were tentative in nature, since these were based on a choropleth map of relative proportions (percentages) of flooding in different parts of the country. The official estimate of the maximum extent of flooding was 82000 km² (57% of Bangladesh), i.e. 15 to 26% larger than the area shown on satellite imagery. The actual extent of flooding was certainly larger than the estimates from satellite imagery but, perhaps, smaller than the official estimates, since a reduction of 15 to 26% of flood area in one to three weeks seemed unlikely. An alternative method of mapping flood-affected areas by using newspaper-interpreted data was attempted, but the method had limited values because of reporting bias.  相似文献   

钽钼杂多酸—碱性染料多元缔合物体系的研究   总被引：1，自引：0，他引：1  

李祖碧  王加林 《岩矿测试》1993,12(1):38-42

在PVA、OP或Tween-60存在下,采用平衡移动法确定了碱性染料亚甲基蓝、耐尔蓝(NB)、罗丹明B(RB)、丁基罗丹明B(BRB)、结晶紫(CV)、乙基紫(EV)与Ta的摩尔比是1:1至7:1;考察了NB(或BRB)-钽钼杂多酸缔合物的红外光谱,初步探讨了反应机理:比较了几个碱性染料-钽钼杂多酸缔合物体系的光度特性,筛选出两个摩尔吸光系数>2×10~6的分析体系,并用于合金钢和地质标样中痕量Ta的测定,方法可行。  相似文献   

铼－锇同位素体系在基性—超基性岩中应用现状的综述     

熊永良  翟裕生 《地质科技情报》1994,(3)

综述了该同位素体系晚侏罗世以来，尤其是现代地幔岩石的研究成表明，地幔在晚侏罗世以来在１８７Ｏｓ／１８６Ｏｓ比值方面显示出非均一性，其比值从０．９０～１．２６，但此类岩石的１８７Ｏｓ／１８６Ｏｓ比值分别与各个不同研究者所确定的地幔演化线相一致；来自较古老正常地幔或贫化地幔的岩石，在锇同位素方面体现为１８７Ｏｓ／１８６Ｏｓ初始比值接近或低于Ｒｅ－Ｏｓ同位素体系地幔演化线值。在此类岩石中，Ｒｅ－Ｏｓ同位素体系与Ｓｍ－Ｎｄ同位素体系之间存在着三种可能的关系：①正相关关系；②负相关关系；③无相关关系。据认为，第一种关系是由羽状地幔端元和富集亲石元素而且贫铼之次大陆型岩石圈地幔端元混合而成；第二种关系则是由羽状地幔端元与地壳物质混合而成；第三种关系则是锇同位素成分相同但钕同位素成分明显不同的两端元物质混合而成。在第三方面，有古老俯冲大洋壳物质参与之基性－超基性岩石具有高于地幔演化线的初始１８７Ｏｓ／１８６Ｏｓ比值。具有此种锇同位素成分特征的岩石包括大洋岛弧玄武岩（ＯＩＢ）、洋中脊玄武岩（ＭＯＲＢ）以及榴辉岩。①  相似文献   

南极长城站至莫斯科和伊尔库茨克路径上时延的测量与传播路径研究          下载免费PDF全文

孙宪儒  王聚杰  杜军虎  杨维富 《极地研究》1994,6(1):61-65

本文介绍了利用在南极长城站接收来自ＲＷＭ（莫斯科）和ＲＩＤ（伊尔库茨克）台的授时信号的无线电波时延的测量方法，并依据１９９１年４月至１９９１年９月所测量的传播时延数据分析了电波传播路径。说明了沿长、短大圆路径的传播时段。判定存在着非大圆路径传播并阐明了关于非大圆路径传播的一些变化规律。对非大圆路径发生的条件进行了探讨  相似文献   

纬向切变基流中的非线性Rossby波     

何建中  郭品文 《高原气象》1993,12(4):361-366

本文在半地转近似下讨论了纬向切变基流中的非线性正压Ｒｏｓｓｂｙ波，给出了存在波解的切变基流条件。  相似文献   

内蒙古呼盟地区地震活动的基本特征     

徐建德  杨毅  张建中 《东北地震研究》1993,(1)

通过对内蒙古呼盟地区地震活动的研究,认为呼盟地区震中分布较稳定;存在20年左右地震活动周期;震源机制两节面分布相对比较稳定,P、T轴近水平向;地震破裂是以水平滑动为主。将来呼盟地区的地震活动主体地区为博克图、满洲里一带,震级为5级左右。  相似文献   

视景地形仿真及其应用   总被引：2，自引：0，他引：2  

张华军 《测绘学院学报》1994,(3)

本文主要讨论了视景地形仿真的特点、数据基础及其实现的整个过程，列举了视景地形仿真在军事上和其它领域的应用实例。实验表明，本文所介绍的视景地形仿真过程简单而容易实现，仿真的地形景观具有良好的视觉效果。  相似文献