利用HJ-1A/1BCCD数据进行黄河凌汛监测     

刘良明  徐琪  周正  叶沅鑫 《武汉大学学报(信息科学版)》2012,37(2):141-144,124

利用HJ-1A/1B卫星CCD数据进行黄河凌汛监测,提出了基于主成分分析和决策树的冰凌提取方法。实验结果显示,利用HJ-1A/1B卫星CCD数据能有效地提取出黄河的冰凌范围,对黄河凌汛监测具有较大的应用潜力。  相似文献   

B/S党务信息管理系统方案研究与设计     

李娜  李琦  刘波  高桂棠  张照杰 《测绘与空间地理信息》2012,(7):150-152,155

电子党务信息管理系统是实现党务管理信息化、规划化的有效途径,能够辅助完成党务管理中的各项工作,本文在分析当前党务信息管理的前提下,给出了建设党务信息管理系统的总体结构框架设计及具体功能设计方案,为党务信息管理系统的建设提供思路。  相似文献   

IS影像3维扫描全站仪在矿山开采中的应用     

刘喜  潘勋  任恒星 《测绘与空间地理信息》2012,(8):108-110

介绍了基于拓普康IS影像3维扫描全站仪获取的点云数据,构造不规则三角网(TIN)计算土石方的功能和特点,并对该系统在齐齐哈尔市碾子山区东海采石场的应用情况进行了详细地介绍和分析。实际应用表明,影像全自动扫描全站仪在矿山开采中具有操作流程更简单,系统效率高,作业时间短,测量结果精度高等特点。  相似文献   

区域延迟模型在CORS站反演水汽中的应用     

文鸿雁  何美琳  潘元进  康晋明 《测绘科学技术学报》2012,(6):406-409

系统地论述了利用CORS系统观测数据反演大气水汽含量的基本原理和方法,分析其反演大气水汽含量过程。基于探空资料建立了广西区域干延迟的延迟模型和加权平均温度模型,利用广西地区CORS站及国内IGS站的观测数据进行解算得出天顶方向对流层延迟量。经过比较区域模型与经验模型得出区域模型具有可用性,且反演出的大气水汽含量与探空水汽含量精度相当,从而验证了区域模型具有可靠性。  相似文献   

GPS/BD静态相对定位解算研究与实现     

袁本银  鲍志雄  潘国富 《测绘》2012,(6):247-250

BD系统的投入使用改变了传统的单星座静态相对定位解算方法,使GPS/BD双星座相对定位解算成为可能,本文论述了GPS/BD静态相对定位解算的数学模型,对载波相位频率不同的双星座整周模糊度固定方法进行了阐述;利用中海达新版后处理软件HGO软件来实现相关算法,并用通过实测数据进行了多项试验,证明了GPS/BD静态相对定位解算的正确性和可靠性。  相似文献   

诠释地球生命力报告:1998—2010     

梁艳  张琦  余国培 《世界地理研究》2012,(2):35-40

《地球生命力报告》应用地球生命力指数、生态足迹和水足迹3个指标描绘了全球自然生态系统的状况与变化趋势,以及在经济发展过程中可再生资源可持续利用的程度。本文在简要解读1998年至2010年的全部8期报告核心内容的基础上,认为人类对生态系统的衰退尚没有给予足够的重视,人们的生活方式应有所改变。只有认识到保护自然是为了人类自身的健康、财富和福祉,而不是维护生物多样性本身和只有意识到自然在维护人类健康和生活中所起的核心作用时,人类才能更好地维护我们生活的这个星球,因为我们只有一个地球。  相似文献   

基于共生理论的河南省城乡统筹空间差异研究   总被引：1，自引：0，他引：1  

刘荣增  王淑华  齐建文 《地域研究与开发》2012,31(4):19-22,28

城市和乡村作为区域经济系统的2个共生单元,既存在相互依赖与合作,又存在相互冲突与竞争。从共生理论的视角出发,选择城乡之间共生界面、共生关联度和共生协调作为城乡统筹的一级指标并细分为22个二级指标,对河南省18个地市城乡统筹情况进行了客观综合的评价,并对其统筹水平进行5个等级的划分,揭示了河南省城乡统筹空间分布上西北高东南低的态势。最后,从工业化水平、城镇化水平、区域基础设施、资源条件以及政策导向等方面探讨了河南省城乡统筹水平差异的原因,旨在为中原经济区建设和"三化"协调战略的制订提供依据。  相似文献   

基于GIS的社区环境信息管理系统研究     

江晓岚  潘文斌 《福建地理》2012,(3):62-66

在GIS技术支持下,以福州市鼓楼区铜盘河沿岸社区作为研究对象,通过收集社区的自然环境、社会环境以及污染源等相关信息,同时结合遥感影像,运用相关软件进行空间信息的矢量化,建立起社区级环境信息管理系统.该系统包括4个模块：地图显示、数据输入、信息查询和专题图制作.本研究在建立数据库的基础上,对数据进行分析.该数据库对于社区环境信息管理系统的建设具有一定的指导意义和参考价值.  相似文献   

开垦对内蒙古温带草地土壤不同有机碳组分的影响(英文)   总被引：3，自引：2，他引：1  

齐玉春  董云社  彭琴  肖胜生  何亚婷  刘欣超  孙良杰  贾军强  杨智杰 《地理学报(英文版)》2012,22(2):315-328

Cultivation is one of the most important human activities affecting the grassland ecosystem besides grazing, but its impacts on soil total organic carbon (C), especially on the liable organic C fractions have not been fully understood yet. In this paper, the role of cropping in soil organic C pool of different fractions was investigated in a meadow steppe region in Inner Mongolia of China, and the relationships between different C fractions were also discussed. The results indicated that the concentrations of different C fractions at steppe and cultivated land all decreased progressively with soil depth. After the conversion from steppe to spring wheat field for 36 years, total organic carbon (TOC) concentration at the 0 to 100 cm soil depth has decreased by 12.3% to 28.2%, and TOC of the surface soil horizon, especially those of 0-30 cm decreased more significantly (p<0.01). The dissolved organic carbon (DOC) and microbial biomass carbon (MBC) at the depth of 0-40 cm were found to have decreased by 66.7% to 77.1% and 36.5% to 42.4%, respectively. In the S.baicalensis steppe, the ratios of soil DOC to TOC varied between 0.52% and 0.60%, and those in the spring wheat field were only in the range of 0.18%-0.20%. The microbial quotients (qMBs) in the spring wheat field, varying from 1.11% to 1.40%, were also lower than those in the S. baicalensis steppe, which were in the range of 1.50%-1.63%. The change of DOC was much more sensitive to cultivation disturbance. Soil TOC, DOC, and MBC were significantly positive correlated with each other in the S. baicalensis steppe, but in the spring wheat field, the correlativity between DOC and TOC and that between DOC and MBC did not reach the significance level of 0.05.  相似文献   

巴丹吉林沙漠湖泊与地下水的补给来源及化学组成(英文)   总被引：1，自引：0，他引：1  

邵天杰  赵景波  周旗  董治宝  马延东 《地理学报(英文版)》2012,22(3):479-496

Based on the analysis of ion chemical composition of lake water and shallow groundwater in the Badain Jaran Desert, this paper discussed the characteristics of ion chemical composition, spatial variation of lake water, and possible supply sources of lake water and groundwater in the desert areas. The results show that the pH, salinity, TDS and electrical conductivity of the lake water are greater than those of groundwater. The ion con-tents of water samples are dominated by Na+ and Cl?. Most of the higher salinity lakes are Na (K)-Cl-(SO4) type, and a few of low salinity lakes belong to the Na-(Mg)-(Ca)-Cl-(SO4)-(HCO3) type. Most of the groundwater is Na-(Ca)-(Mg)-Cl-(SO4)-(HCO3) type, attributed to subsaline lake, and only a few present the Na-Cl-SO4 type, flowing under saline lake. The pH, salinity, TDS and electrical conductivity in the southeastern lakes are relatively low, and there are slightly alkaline lakes. The pH, salinity, TDS and electrical conductivity in the northern lakes are much greater than those of the southeastern lakes, and the northern lakes are moderately alkaline and saline ones. In the southeastern part of the Badain Jaran Desert, the ion chemical characteristics of the lake water from south to north show a changing trend of sub-saline →saline→hypersaline. The changing trend of chemical compositions of ions in recent 9 years indicates that most of the ion contents have a shade of reduction in Boritaolegai, Badain, Nuoertu and Huhejilin lakes, which state clearly that the amount of fresh water supply is increasing in the 9-year period. The ion chemical composition of the lake water reveals that the flow direction of lake water is from southeast to northwest in the Badain Jaran Desert. The ion chemical composition, moisture content of sand layer water level height and hierarchical cluster analysis of the lake water and groundwater demonstrate that the lake water is mainly supplied by local rainfall and infiltration of precipitation in Yabulai Mountains and Heishantou Mountain, and the supply from the Qilian Mountains is almost impossible.  相似文献