Investigations into the thermal non-equilibrium of W UMa-type contact binaries

Traditionally, some physical details(e.g., magnetic braking, energy transfer, angular momentum loss, etc.) have to be taken into consideration during investigations into the evolution of contact binaries. However, the real evolutionary processes which usually contain several of these physical mechanisms are very complicated as a result of strong interaction between components. To avoid dealing with these factors, a linear relationship is applied to the temperatures of components. It is found that the higher the mass ratio(M_2/M_1) of a contact system, the weaker the deviation from thermal equilibrium.On this basis, a variation trend of fill-out factor(f) changing with mass ratio can be inferred, which is consistent with observations. Moreover, if we stick to this point of view, it should be natural that the number of semi-detached binaries in the predicted broken-contact phase of relaxation oscillations is less than the number in the contact phase.     

面向作战任务的战场环境仿真过程对象模型

针对目前战场环境仿真系统与指控系统之间互操作性还不完善,需要构建一种面向作战任务的战场环境仿真过程模型来有效解析指控系统的关键信息需求。分析了仿真过程结构化特征,采用面向对象的方法构建仿真过程概念模型;分析GeoBML的数据模型和形式化语法,使用形式化语言建立仿真过程的逻辑语义模型;定义仿真过程对象数据结构,构建任务驱动下的仿真过程数据映射模型。最后,基于该模型设计战场环境仿真平台组件并应用,验证其合理性与可扩展性。     

A terrain openness index for the extraction of karst Fenglin and Fengcong landform units from DEMs

The Fenglin and Fengcong landform units are considered to be an important representation for defining the degree of development of Karst landforms. However, these terrain features have been proven difficult to delineate and extract automatically because of their complex morphology. In this paper, a new method for identifying the Fenglin and Fengcong landform units is proposed. This method consists of two steps: (1) terrain openness calculation and (2) toe line extraction. The proposed method is applied and validated in the Karst case area of Guilin by using ASTER GDEM with one arc-second resolution. The openness of both the positive and negative terrain and a threshold were used to extract toe lines for segmenting depressions and pinnacles in Fenglin and Fengcong landforms. A comparison between the extracted Fenglin and Fengcong landform units and their real units from high resolution images was carried out to evaluate the capability of the proposed method. Results show the proposed method can effectively extract the Fenglin and Fengcong landform units, and has an overall accuracy of 93.28%. The proposed method is simple and easy to implement and is expected to play an important role in the automatic extraction of similar landform units in the Karst area.     

近50年华南沿海SST热事件变化的时空特征

根据华南沿海10个海洋站1960-2009年实测海表温度(SST)资料统计分析了近50年华南沿海SST热事件时空变化特点,得出如下结论:华南沿海SST热事件主要出现在6-8月份,SST热事件出现的频率以北部湾东北部海域最高,粤东沿海最低;导致SST热事件海区差异的原因是上升流及热带气旋存在海区差异;受全球气候变暖的影响,华南沿海年均SST有上升趋势,近50年来气候变化可划分为冷、暖两个时期,其相对暖期SST热事件的年频数、累计天数、每次SST热事件持续天数较相对冷期均有增加趋势.     

商丘近40 a蒸发量变化特征及原因分析

利用商丘1961-2000年小型蒸发皿蒸发量资料,分析了商丘蒸发量的变化趋势及引起蒸发量变化的因子,结果表明,商丘年、季和月蒸发量均存在明显的下降趋势,影响蒸发量变化的因子主要有风速、日照、相对湿度、水汽压等.     

Seismic reflection evidence of crustal duplexing and lithospheric underthrusting beneath the western Qilian Mountains,northeastern margin of the Tibetan Plateau

The geological processes responsible for outward growth of the Tibetan Plateau are debated.The Qilian Mountains on the northeastern margin of the plateau comprise one of the youngest structural components of the plateau whose understanding is key to deciphering the broader geological evolution of the region.Here,based on a reprocessed deep seismic profile which was originally collected during the 1990 s across the northeast margin of the western Qilian Mountains and previous geological and geophysical data,we find evidence for decoupled crustal deformation that was partitioned by a decollement,in which lowercrustal deformation featured by local duplexing preceded upper-crustal deformation featured by imbricate thrusts.Furthermore,we propose that the Asian lithospheric mantle is being underthrust beneath the western Qilian Mountains,as inferred from patterns of lower crustal deformation which is marked by the Moho geometry.Integrating these results yields a better understanding of lithospheric deformation of western Qilian Mountains,northeastern margin of the plateau during the Cenozoic.     

钇铝石榴石晶体高压相变研究

采用金刚石压砧高压设备,对立方结构掺钕钇铝榴石多晶进行高温高压相变研究。实验分同时加温加压、独立加压、独立加温三类。对压力温度作用后相变产物进行了 X 射线衍射研究,对相变前后样品的配位数、晶体结构、晶胞参数、体积、密度进行了对比。     

铼－锇同位素体系在基性—超基性岩中应用现状的综述

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     

热流测量中垂向地下水运动干扰的校正方法

本文提出了一种地表热流测量中垂向地下水干扰的校正方法。并以江西萍乡和福建安溪的二个钻孔为例,说明了热流校正的具体过程。由于地下水对流传热的影响,垂向地下水渗透层内温度和热流随深度均呈指数分布。通过对钻孔测温数据的一维垂向Peclet数分析,可以确定渗透层内传导和对流热流分量以及热流的构成,从而得到未受地下水对流干扰的区域背景热流。这一方法不仅适用于渗透率结构均一的介质,也可用于水平层状介质。     

佳木斯市地下水水量水质模型

佳木斯市是一个以开采地下水为主要供水水源的城市.本文根据当地的水文地质条件,建立了佳木斯市的地下水的水量水质模型.用有限元法求解水量模型进行地下水资源评价.用特征有限元法求解水质模型进行地下水污染预测,该方法在求解对流一弥散方程时能有效地消除数值弥散和数值振荡,精度较高.为使该方法付诸实施,文中也提出了当利用特征有限元法求解时确定运动水质点所属单元的方法.