西部生态脆弱区矿山不同开采强度下生态系统服务时空变化——以神府矿区为例

以神府矿区为例,选取土地利用、植被覆盖、土壤、气象等生态环境与统计数据指标,利用RS和GIS技术构建生态系统服务遥感测量评估指标体系,评估研究区2005-2015年生态系统服务变化及时空分布特征,进一步探究神府矿区不同开采强度对生态系统服务的影响并进行驱动力分析。研究结果表明：（1）2005年、2010年、2015年研究区的总生态系统服务分别为1.598×10¹⁰元、1.905×10¹⁰元、2.134×10¹⁰元,呈现逐年递增的趋势;（2）生态系统服务功能中水土保持价值比例最大,草地的单位面积生态系统服务价值最高,耕地、草地生态系统为该地区贡献了最多的生态系统服务价值;（3）研究区生态系统服务分布表现为由东北向西南逐渐降低的趋势,不同开采强度下的生态系统服务增长变化较为相似,煤炭开采区域生态系统服务未显著下降,整体较为平稳。对生态系统服务变化的驱动分析表明在近年来相对改善的气候环境与人工修复共同作用下,神府矿区生态系统服务未发生明显的缩减。此类半干旱生态脆弱矿区国土空间生态修复适宜通过主动的“保护性开发”以及“人工诱导+自然修复”为主的方式,避免大范围与高强度的水土扰动型治理,通过适度的人为干预保证与维持区域内生态系统服务的功能。研究成果不但揭示高强度煤矿开采下的生态环境变化,也对西部生态脆弱区环境做了定量评估;同时,为将来的矿区重建提供了重要的依据。     

浙江城镇空间扩展与经济发展的遥感研究

近年来。浙江省经济飞速发展。城镇规模迅速扩大。但有关全省城镇建成区扩展面积的具体数量和扩展速度的客观数据还很缺乏。利用多时相的Landsat卫星遥感图像数据。采用目视解译与计算机自动分类方法，对1998～2001年浙江省城镇时空扩展进行了调查。调查结果显示，1998年和2001年浙江省县级以上城市建成区面积分别为977．85km^2和1499．06km^。3年内全省县级以上城市建成区面积扩展了521．21km^2，年增长速率达15．31％。在此基础上，根据区域社会经济统计数据，对城镇经济发展与城市空间扩展的相关性进行了分析。     

气象卫星遥感在干旱监测中的应用

本文根据ＮＯＡＡ极轨气象卫星ＡＶＨＲＲ资料计算生成植被指数相对距平图用于旱情监测，并在江苏省１９９４年特大干旱中进行了应用服务     

遥感技术在小城镇发展规划中的应用

对卫星遥感技术在小城镇发展规划中的应用进行了分析，包括小城镇空间布局信息分析、小城镇区位分析和小城镇环境污染分析，介绍了遥感技术在小城镇变化监测中的应用。分析表明，遥感技术能为小城镇发展规划提供众多基础数据，具有广阔的应用前景，但不能完全取代地面调查。     

农业旱灾监测中土壤水分遥感反演研究进展

土壤水分是农业干旱监测最重要的指标之一。文章全面回顾了光学遥感和微波遥感土壤水分遥感反演进展，重点讨论了符种反演方法的优点和不足。光学遥感中，热惯量法和作物缺水指数法可分别较好地应用于裸露地和作物覆盖地的土壤水分监测；距平植被指数、植被条件指数采用了植被指数因子实现农业旱情监测，温度植被指数、植被供水指数和条件植被温度指数同时考虑了作物植被指数和地表温度。微波遥感被认为是当前土壤水分监测中最有效的方法。主动微波遥感空间分辨率较高，但对土壤粗糙度和植被敏感；被动微波遥感空间分辨率低，重访周期短，对大尺度农业旱灾监测具有较大潜力。为提高农业旱灾监测巾土壤水分遥感反演的精度和效率，采用光学遥感和微波遥感的结合可能是较为实际的方法。     

三峡库区地质灾害监测技术及展望

笔者综述了三峡库区地质灾害监测技术的应用现状。在论述当前地质灾害监测技术存在的问题的基础上,提出了新型的基于Internet的地质灾害远程、集中监测系统,并详细讨论了该技术的原理、结构、应用前景以及功能完善和发展方向。新型安全监测系统的使用可有效防止库区地质灾害的发生,控制其潜在危害;提高库区整体预警管理水平,有效增强防灾减灾能力;显著降低库区安全监测系统运行成本。     

基于GPRS技术的地质灾害无线遥测系统

将通用分组无线业务(GPRS)技术应用于地质灾害监测系统,可实现监测数据的无线传输和Internet的无线接入,因而实现地质灾害监测数据互联网共享和预警、救灾指挥联网.详细介绍了在三峡工程万州库区运行的基于GPRS技术的地质灾害无线遥测台网的体系结构、功能实现以及运行效果.该系统的建成与可靠运行使三峡库区地质灾害的监测预警系统走向数字化、自动化、网络化.     

高分辨率遥感影像的土地利用分类

高分辨率遥感影像在我国土地利用动态监测中展现出良好的应用前景,但与此相关的关键技术问题亟待解决.结合Ikonos影像,分析高分辨率遥感影像的特点,并在我国土地利用现状类型划分的基础上,针对高分辨遥感影像土地利用分类这一关键技术问题,概述常规分类方法,提出一套适宜高分辨率遥感影像土地利用分类的技术路线.     

MODELING THE DISTRIBUTION OF DIFFUSE NITROGEN SOURCES AND SINKS IN THE NEUSE RIVER BASIN OF NORTH CAROLINA,USA1

This study quantified nonpoint source nitrogen (NPS‐N) sources and sinks across the 14,582 km² Neuse River Basin (NRB) located in North Carolina, to provide tabular data summaries and graphic overlay products to support the development of management approaches to best achieve established N reduction goals. First, a remote sensor derived, land cover classification was performed to support modeling needs. Modeling efforts included the development of a mass balance model to quantify potential N sources and sinks, followed by a precipitation event driven hydrologic model to effectively transport excess N across the landscape to individual stream reaches to support subsequent labeling of transported N values corresponding to source origin. Results indicated that agricultural land contributed 55 percent of the total annual NPS‐N loadings, followed by forested land at 23 percent (background), and urban areas at 21 percent. Average annual N source contributions were quantified for agricultural (1.4 kg/ha), urban (1.2 kg/ha), and forested cover types (0.5 kg/ha). Nonpoint source‐N contributions were greatest during the winter (40 percent), followed by spring (32 percent), summer (28 percent), and fall (0.3 percent). Seasonal total N loadings shifted from urban dominated and forest dominated sources during the winter, to agricultural sources in the spring and summer. A quantitative assessment of the significant NRB land use activities indicated that high (greater than 70 percent impervious) and medium (greater than 35 percent impervious) density urban development were the greatest contributors of NPS‐N on a unit area basis (1.9 and 1.6 kg/ha/yr, respectively), followed by row crops and pasture/hay cover types (1.4 kg/ha/yr).     

ACCURACY OF LAKE AND STREAM TEMPERATURES ESTIMATED FROM THERMAL INFRARED IMAGES1

Emitted thermal infrared radiation (TIR, λ= 8 to 14 μm) can be used to measure surface water temperatures (top approximately 100 μm). This study evaluates the accuracy of stream (50 to 500 m wide) and lake (300 to 5,000 m wide) radiant temperatures (15 to 22°C) derived from airborne (MASTER, 5 to 15 m) and satellite (ASTER 90 m, Landsat ETM+ 60 m) TIR images. Applied atmospheric compensations changed water temperatures by ?0.2 to +2.0°C. Atmospheric compensation depended primarily on atmospheric water vapor and temperature, sensor viewing geometry, and water temperature. Agreement between multiple TIR bands (MASTER ‐ 10 bands, ASTER ‐ 5 bands) provided an independent check on recovered temperatures. Compensations improved agreement between image and in situ surface temperatures (from 2.0 to 1.1°C average deviation); however, compensations did not improve agreement between river image temperatures and loggers installed at the stream bed (from 0.6 to 1.6°C average deviation). Analysis of field temperatures suggests that vertical thermal stratification may have caused a systematic difference between instream gage temperatures and corrected image temperatures. As a result, agreement between image temperatures and instream temperatures did not imply that accurate TIR temperatures were recovered. Based on these analyses, practical accuracies for corrected TIR lake and stream surface temperatures are around 1°C.