鄂北地区推覆构造重磁异常特征

利用区域重磁资料,对鄂北推覆构造的空间分布特征进行了定性、半定量的分析与研究,解决了鄂北复杂地质问题,拓宽了区域重力调查的研究领域.     

计算机视觉中摄像机标定精度评估方法

介绍了两种经典的摄像机标定精度评估方法:Tsai提出的测量3维世界精确程度的准则和Weng提出的NSCE、NCE准则.在此基础上,提出了一种基于棋盘格长度的标定精度评估方法.该方法通过交会测量得到的多个棋盘格的边长与实际边长的误差量来衡量摄像机标定的精度,能够比较形象地描述标定结果的精度.     

基于信息扩散理论的云南省地震风险评估及管理研究

利用信息扩散的方法,从破坏性地震次数风险和震级风险的角度对云南各地区进行了风险评价,并提出相应的风险管理策略。     

The influence of different underlying surface on sand-dust storm in northern China

In this paper, a quantitative research on the relationship between different underlying surface and sand-dust storm has been made by using 40 years meteorological data of five different types of underlying surface in northern China, which include farmland, grassland, sandland, gobi and salt crust. These metrological data comprise sand-dust storm days and strong wind days. By analyzing, we can find that there are certain correlations between the days of sand-dust storm and strong wind for different underlying surface, which has great influence on sand-dust storm. But there are pronounced differences in different types of underlying surface. The sand-dust storm days of grassland, gobi and salt crust, with smaller interannual variation are obviously less than strong wind days. On the other hand, the sand-dust storm days of farmland and sandland increase evidently, even in many years, are much more than strong wind days. The differences are mainly induced by the influencing mechanism of different underlying surface on sand-dust storm. Grassland, gobi and salt crust with stable underlying surface are not prone to sand-dust storm under strong wind condition. Whereas, the underlying surface of farmland and sandland is unstable, that is easy to induce sand-dust storm under strong wind condition.     

湖南省主要稀有稀土金属矿床特征

湖南省主要有铌、钽、铷、铯、锂、铍、锆等稀有金属及稀土金属矿床．矿床类型以岩浆晚期分异交代型、气成热液型、佛晶岩型、风化壳型和砂矿型为主．稀有稀土金属矿床在空间分布与成因上，与东山期花岗岩体密切相关，往往具有水平分带和垂向分带规律．     

青藏铁路可调式通风管路基的数值仿真分析

Finite Element Method has been used to operate the numerical analysis and comparison between the traditional ventilated embankment and the adjustable ventilated embankment adopted in Qinghai-Tibet Railway construction. The numerical results show that: 1) The adjustable ventilated embankments can prevent the thermal entry from air into ducts during summer from thawing the permafrost beneath the embankments; 2) The cooling effects of the adjustable ventilated embankments on permafrost is much better than the traditional ventilated embankments although two kinds of embankments can generate the thawing bulbs at the beginning of finishing construction; 3) The drop of the mean temperature of permafrost under the adjustable ventilated embankments keeps faster than that of the mean temperature of permafrost under the traditional ventilated embankments. It is clear that the adjustable ventilated embankments can keep the embankment more stable than the traditional ventilated embankments.     

青藏铁路通风路基边界条件研究

In permafrost regions, many methods about active cooling embankment are put forward, one of these representations is ventilated embankment, its cooling effect is the result of the air convection in the duct, and this leads to reducing the annual average ground temperature. The present work in this article is to determine the boundary conditions of the ventilated embankment and natural ground in numerical work. There are several effects which influence boundary conditions, they are: radiation, evaporation,phase change, convection and embankment material etc. Radiation and convection are the main effects in those. We mainly consider sun radiation in this article. The added-surface effect in ventilated embankment lowers its temperature, so the temperature on the wall of the ventilated embankment is different from the temperature in atmosphere. There are two methods in determining the surface temperature, experimental method and experiential method. Detailed research is discussed in the article.     

四川南江桥亭、流坝剖面裂缝特征研究

川东北及川北是未来几年中国油气勘探开发的重点地区,这个地区的储层类型主要以裂缝-孔隙型为主。通过对南江桥亭、流坝剖面野外地质调查,认为南江地区裂缝可分为成岩缝与构造缝两大类,其中成岩缝有成岩收缩缝和压溶缝合线两种类型;构造缝主要有与岩层面垂直、与水平面垂直、与岩层面低角度相交、与水平面低角度相交的剪切缝及纵张缝、顺层缝和共轭剪切带雁列张裂缝等七种类型。     

土壤盐分特征对内陆盐沼盐生植物群落的影响

为研究内陆盐沼植物群落的分布对土壤盐分的响应特征,选取鄂尔多斯盐湖盐沼区作为研究区,筛选了肉质耐盐植物群落,苔草植物群落和禾草植物群落3类典型植物群落,开展了土壤含水量、pH、电导率以及Na_⁺,K_⁺,Mg2_⁺,Ca_{^{2 +}},Cl_^-、SO_4^2-、CO_3^2-和HCO_3^-的测定,分析了区内典型植物群落对土壤水盐因子的响应规律。探讨了3类植物群落之间土壤因子含量的差异性;采用相关性分析和CCA分析,评价了3类植物群落多样性及物种分布随土壤因子的变化规律。结果表明,区内3类植物群落中,土壤盐分含量表现为肉质耐盐植物群落最高,苔草植物群落最低,禾草植物群落居中;植物多样性与土壤中含量最高的Na_⁺和SO_4^2-的相关性最显著;植物分布同时受到土壤盐分、水分和pH的显著影响。研究结果可为鄂尔多斯盐湖区土壤盐渍化改良和植被恢复提供理论支撑。     

中原经济区城市体系空间组织

新型城镇化是引领中原经济区“三化”协调发展的重要切入点,而城市体系空间组织又是支撑新型城镇化的主要载体。依据空间组织的基本理论,采用多种空间分析手段,分析了中原经济区城市体系的空间组织路径,结论如下：① 通过规模实力、综合实力评价模型计算中原经济区30个省辖市的空间组织等级,结合空间组织的均衡原则,确定以郑州为核心城市,洛阳、邯郸、信阳和商丘为区域中心城市,晋城、安阳、南阳、淮北为区域性次中心城市的等级体系;② 应用分形理论、圈层分析、缓冲区分析、城市相互作用模型等方法分析发现,中原经济区具备以郑州为核心的圈层式、轴带状、核心板块网络化、组团分区的组织基础;③ 结合空间组织的等级层次和现实基础,提出中原经济区空间组织的“中心带动、圈层推动、轴带组织、核心板块网络化、组团分片”的模式选择与路径取向。