SEMIAUTOMATIC BUILDING EXTRACTION FROM STEREO IMAGE PAIR BASED ON LINES GROUPING AND LEAST SQUARES MATCHING

1　ＩｎｔｒｏｄｕｃｔｉｏｎＡｔｐｒｅｓｅｎｔ,ｍａｎｙｃｏｍｍｅｒｃｉａｌｄｉｇｉｔａｌｐｈｏｔｏｇｒａｍ ｍｅｔｒｉｃｗｏｒｋｓｔａｔｉｏｎｓ (ＤＰＷ )ｈａｖｅｂｅｅｎｄｅｖｅｌｏｐｅｄａｎｄａｐｐｌｉｅｄｉｎｔｏｐｒａｃｔｉｃａｌｐｒｏｄｕｃｔｉｏｎ .Ｍｏｓｔｏｆｔｈｅｍｃａｎａｕｔｏｍａｔｉｃａｌｌｙ ｇｅｎｅｒａｔｅｄｉｇｉｔａｌｔｅｒｒａｉｎｍｏｄｅｌ(ＤＴＭ)ａｎｄｄｉｇｉｔａｌｏｒｔｈｏ＿ｉｍａｇｅ (ＤＯＭ ) ,ｂｕｔｔｈｅｒｅａｒｅｎｏｔａｎｙｓｙｓｔｅｍｓｗｈｉｃｈｃａｎａｕｔｏｍａ…     

计算机仿真模型的灵敏度分析

计算机仿真模型的灵敏度分析，是仿真建模中的重要研究内容，对实际系统的建立和优化具有重要意义。本文主要研究了在用蒙特卡洛方法仿真随机系统时，其仿真模型（输出）的灵敏度（导数、梯度、Ｈｅｓｓｉａｎ矩阵等），对系统性能函数和灵敏度的参数估计进行了探讨，并结合实际应用系统，对结论进行了分析比较。     

爆震观测及爆震效应的工程评价

本文介绍了有关爆破地震效应工程评价方法及其标准,汇报了观测仪器和得到的不同地区的经验传递系数,同时还介绍了部分振速及爆破地震烈度标准。     

预应力锚索在滑坡治理中的应用

介绍了国内外用于边坡，滑坡加固的预应力锚索的主要类型及结构，并例举了锚索在滑坡治理中的实际应用。     

PDCA循环法用于专业硕士产教融合培养模式研究

为满足新时代对卓越工程技术人才的需求,本文在分析专业硕士培养现状基础上,从人才培养方案入手,提出了PDCA理念用于产教深度融合培养模式,讨论了产教深度融合培养的目标制定、计划落实、课程体系开发、导师团队优化及实践基地的质量保障建设等方面的模式与对策,论述了专业硕士研究生培养的质量监控体系,总结出教育教学各环节的计划、执行、考查、处理的持续改进和提高的螺旋式上升过程,为专业硕士高水平培养与管理提供参考与借鉴。     

德清县自然生态系统质量量化评估方法探究

针对县域自然生态系统质量量化评估方法的选择和优化问题,该文以德清县为例,选择物种多样性、生态承载力和生态系统服务价值量化评估模型和方法对其2010年和2018年的自然生态系统质量进行评估分析.结果显示,德清县林地物种多样性的Shannon-Wiener指数和Simpson指数均优于草地.2010-2018年的生态承载力和生态系统服务价值呈上升趋势,生态系统服务价值能够有效评估地区自然资源的资本价值.生态系统服务价值结合物种多样性具有较高的实践价值.进一步拓展了地理国情和国土数据的实践应用,研究结果可用于县域土地利用规划、自然资产统计和自然保护地监测和评估等.     

一种利用机载激光点云的河流横纵断面自动提取方法

传统的河流断面测量方法具有周期长、成本高、外业多等不足,为此提出一种基于机载激光点云的河流横纵断面自动提取方法.首先,使用渐进三角网滤波器从机载点云中分离出地面点,用以构建三角网模型,并将其转化成数字高程模型数据.接着,利用洼地填充、流向分析、流量分析、河流栅格提取、矢量化等水文分析模块,从数字高程模型数据中自动提取出河流中心线.然后,修正河流中心线并生成纵断面,沿着纵断面按固定间距自动提取横断面,并自动填充属性.最后,利用断面线进行缓冲区分析,根据缓冲区范围从正射影像中裁剪出河流影像,并将河流影像与数字高程模型、横纵断面数据打包成完整成果.项目应用证明,该方法具有数据精度高、更新周期短、生产成本低等优势,适用于大范围的河流断面数据生产.     

Review on physical models of lunar brightness temperature

Brightness temperature is a main index to reflect the energy of microwave radiation of an object. Using lunar brightness temperature data, physical properties of lunar regolith, such as thickness, heat flow and dielectric permittivity, could be interpreted. There are two methods to study brightness temperature distribution of the moon: the first is used to measure lunar brightness temperature by radio observation or spaceborne microwave radiometers, and the second is used to simulate calculation by the physical model. On the basis of the measurements of lunar brightness temperature in the history, this study analyzed the main physical model of lunar brightness temperature, also including its theory and influence factors. The authors concluded that surface and subsurface temperatures of the moon, dielectric properties and layered structure of lunar regolith were the main factors affecting the global brightness temperature of the moon. These factors should be quantified in detail in the future research.     

Ore-forming Fluid Characteristics of the Saishitang Cu-polymetallic Deposit in Qinghai Province, China

Saishitang Cu-polymetallic deposit is located in the southeast section of Late Paleozoic arcfold in the southeastern margin of Qaidam platform. Accoring to the geological process of the deposit,four mineralization episodes were identified: melt/fluid coexisting period(O),skarn period(A),first sulfide period(B) and second sulfide period(C),and 10 stages were finally subdivided. Three types of inclusions were classified in seven stages,namely crystal bearing inclusions(type I),aqueous inclusions(type II) and pure liquid inclusions(type III). Type I and II inclusions were observed in stage O1,having homogenization temperature from 252 to 431°C,and salinities ranging from 24.3% to 48.0%. Type I inclusion was present in stage A1,having homogenization temperature from 506 to 548°C,and salinities ranging from 39.4% to 44.6%. In stage B1,type II and III inclusions were observed,with homogenization temperature concentrating between 300–400°C,and salinities from 0.4% to 4.3%. Type II inclusions were present in stage B2,with homogenization temperature varying from 403 to 550°C. In stage C1,type I and II inclusion commonly coexisted,and constituted a boiling inclusion group,having homogenization temperatures at 187–463°C,and salinities in a range of 29.4%–46.8% and 2.2%–11.0%. Type II and III inclusions were developed in stage C2,having homogenization temperature at 124–350°C,and salinities ranging between 1.6% and 15.4%. In stage C3,type II and III inclusions were presented,with a homogenization temperature range of 164–360°C,and salinities varying from 4.0% to 11.0%. The results of micro-thermal analysis show that fluids are characterized by high temperature and high salinity in stage O1 and A1,and experienced slight decrease in temperature and dramatic decrease in salinity in stage B1 and B2. In stage C1,the salinity of fluid increased greatly and a further decrease of temperature and salinity occurred in stage C2 and C3. Fluids boiled in stage C1. With calculated pressure of 22 MPa from the trapping temperature of 284–289°C,a mineralization depth of 2.2 km was inferred. Results of Laser Raman Spectroscopy show high density of H2 O,CH4 and CO2 were found as gas composition. H-O isotope study indicates the oreforming fluids were the mixture of magmatic water and meteoric water. Physicochemical parameters of fluids show oxygen and sulfur fugacity experienced a decrease,and redox state is weakly reducing. Along with fluid evolution,oxidation has increased slightly. Comprehensive analysis shows that melt exsolution occurred during the formation of quartz diorite and that metal elements existed and migrated in the form of chlorine complex. Immiscible fluid separation and boiling widely occurred after addition of new fluids,bringing about dissociation of chlorine-complex,resulting in a great deal of copper precipitation. In conclusion,Saishitang deposit,controlled by regional tectonics,is formed by metasomatism between highly fractionated mineralization rock body and wall rock,and belongs to banded skarn Cu-polymetallic deposit.