The interaction between the secondary and the common convective envelope in a contact binary

It has been suggested that a contact system almost certainly cannot exist in static equilibrium undergoing periodic thermal relaxation oscillation. The energy transfer in a common convective envelope (CCE) makes the secondary have a complex structure, so the interaction between the secondary and CCE may play an important role in the structure and evolution of the contact system. The present paper tests the TRO theory and investigates this interaction with polytropic stellar model from the observational datum of 22 contact systems directly. It shows that the A-type systems are expanding with a velocity of 25.04 m yr^–1, and the W-type systems are contracting at velocity of 3.10 m yr^–1 by the calculations about these contact systems. Also, we calculate the ratio of energy transfer and the interaction coefficient for them. The HS (hot secondary) model is supported by our calculations. These results may help to understand the TRO theory and the W-phenomenon.     

Re-Os Age of Cu-Ni Ores from the Huangshandong Cu-Ni Sulfide Deposit in the East Tianshan Mountains and Its Implication for Geodynamic Processes

An isochron age of 282±20 (95% conf. limit) Ma of the sulfide ores in the Huangshandong Cu-Ni sulfide deposit, the East Tianshan Mountains has been obtained through Re-Os isotopic measurement. The age implies that the Cu-Ni sulfide deposit and other related deposits in the same area occurred in a Permian extensional environment of post-collision instead of Devonian-Early Carboniferous ophiolite-related oceanic or island arc environments inferred before. It shares the same ages with the orogenic and epithermal gold deposit systems in the same area. An initial 187Os/188Os ratio of 0.25±0.04 (1σ) and a γos value of 99 on average display the participation of large quantities of crustal components into the rock-forming and ore-forming system during mineralization and magmatic emplacement.     

Cenozoic Tectonic Evolution of the Arcuate Structures in the Northeast Tibetan Plateau

<正>The northeast Tibetan plateau contains important information on the northeastward growth of the Tibetan plateau.It is bounded by the Ordos Block to the east,the Alxa Block to the north,and the Tibetan Plateau to thesouth(inset in Fig.1;Tapponnier et al.,2001),and has undergone complex intracontinental deformation during the Cenozoic.In this region,the northeast-convex arcuate structures developed northeastward,and are composed of     

《卫星水汽图像和位势涡度场在天气分析和预报中的应用》导读

最近科学出版社出版了译著<卫星水汽图像和位势涡度场在天气分析和预报中的应用>一书.此书的作者是法国的帕特里克·桑特里特和保加利亚的克里斯托·G·乔治夫.该书的特点是把动力气象的位势涡度理论、数值预报模式输出的物理量场和卫星遥感的水汽图像有机地结合起来,向天气预报人员介绍了一种可操作的预报思路,也为数值预报模式开发者提出了利用卫星水汽图像改进模式的潜在途径.在评述这本卫星气象新书的同时,简要地介绍了本书的结构,各章的主要内容和特点,希望能帮助中国的预报员更好地阅读和理解此书.     

贵州贞丰烂泥沟卡林型金矿床含砷黄铁矿Re-Os同位素测年及地质意义

贵州贞丰烂泥沟金矿(现称锦丰金矿)是滇黔桂“金三角”已知最大的卡林型金矿床,矿体赋存于断层破碎带内,最主要的载金矿物是具环带结构的含砷黄铁矿。本文运用Re-Os同位素法对该矿床的9个含砷黄铁矿样品进行了两次测试,成功获得10-9～10-12级Re-Os同位素数据:Re0.1257～1.233ng/g,Os6.75～33.50pg/g,等时线年龄为193±13Ma,反映其成矿时代为早侏罗世。等时线的初始n(187Os)/n(188Os)值为1.127±0.043,指示成矿物质来源于地壳而不是地幔。结合其他资料,初步建立其成矿模式为:盆地流体不断地从沉积物中萃取出包括金在内的成矿组分,形成含矿流体。印支期挤压造山期间,含矿流体沿不整合接触面和同生断层向上运动,造山后的伸展含矿流体进入减压扩容空间沉淀形成超大型金矿床。成矿作用发生在从印支期挤压造山向燕山期伸展转变的构造转换期。该模式与本文得到的成矿年龄和初始比值相吻合。     

浅谈地图模型雕刻技术

借助传统的雕刻技术和计算机雕刻软件,在雕刻软件中利用带高程的等高线数据进行地形建模,并通过输出雕刻指令控制雕刻机进行地形模型粗胚的雕刻;然后通过选材进行其他地图要素的雕刻;最后进行整饰,制作完成一幅按一定比例尺缩小的与实地相似的地形图。     

矿山边坡变形监测数据的高斯过程智能分析与预测

<正>矿产资源开采引发的地表塌陷、崩塌、地裂缝和地面沉降等矿山灾害给人类的生命财产安全造成严重的威胁,集成多传感器的自动化、智能化监测系统是矿山地面灾害监测的发展方向。以中煤平朔井工二矿边坡(简称二号井边坡)自动化监测系统作为研究案例,应用高斯过程(Gaussian process,GP)理论研究变形数据智能分析方法和预测模型,对矿山灾害进行防治提供科学依据。监测数据的可靠性是变形监测分析和预测的基础,针对原始观测数据可能存在的异常值,提出了完整搜索     

浮冰在规则波和双色波下的运动特性研究

为研究浮冰在波浪下的运动特性,以单个聚氯乙烯（PVC）塑料圆板模拟浮冰,进行了一系列波浪试验研究。在规则波试验基础上,同时研究了双色波条件下的浮冰运动特性。结果显示：规则波条件下浮冰运动幅频响应算子首先随无量纲波长的增大而增大,当无量纲波长大于4.0后,运动幅频响应算子随无量纲波长的变化不明显,且趋于一定值;在双色波条件下,对应频率组成成分的浮冰运动幅频响应算子与规则波条件下随波长的变化规律一致。根据部分规则波试验结果提出预测浮冰慢漂速度的经验公式,并用已有的试验和余下的规则波与双色波试验结果进行验证。结果表明,经验公式对规则波和双色波条件下的浮冰慢漂速度的误差在20%以内,预测结果吻合较好。     

Study on the Natural Mineral Water Resource Bearing Capacity and its Driving Factors in Fusong County,Changbai Mountain Area,Jilin Province of China

Water Resources - In order to maintain the sustainable exploitation of the natural mineral water resources in Changbai Mountain Area with the continuously increasing exploitation intensity,...