白龟山水库富营养化与热污染研究（Ⅰ）

对平原浅水型大型水库的富营养化特征和水平作了深入研究,特别对标志富营养化的浮游藻类、浮游动物及底栖动物等作了模拟试验和现场验证,对加速白龟山水库富营养化的诱导因素作了详细探讨。     

"九五"期间昆明市盘龙区酸雨状况分析

本文通过对盘龙区‘‘九五"期间降水监测结果进行评价,得出昆明市中心区酸雨的变化趋势,并加以分析,提出对策建议.     

生态系统健康评价的研究进展

回顾了生态系统健康的概念,阐述了水生态系统健康评价的三种指标体系:指示物种指标体系、结构功能指标体系、V-O-R指标体系.其中,结构功能指标体系从选取指标和指标分类两方面进行了方法归纳,分析了生态系统健康的几种评价方法,以及讨论了生态系统健康研究中存在的问题和发展趋势.     

兖州矿区采煤塌陷地状况与综合治理途径研究

通过对兖州矿区采煤塌陷地状况进行现状分析和趋势预测,结果表明,至2000年底,已累计塌陷土地5389.40hm2;预计到21世纪中叶,兖州、济东2个煤田最终将形成两个塌陷中心,面积达4.4×104hm2。这不仅使大面积农田被毁,造成生态失衡,而且给当地工农业生产以及社会和生态环境等方面带来一系列严重问题,应该彻底进行采煤塌陷地的综合治理。据此,根据矿区工农业持续协调发展的需要,从宏观和微观的角度,全方位提出了采煤塌陷地的综合治理途径。     

东北平原西部沙地的气候变异与土地荒漠化

东北平原西部沙地位于欧亚大陆中纬度巨型沙带的东部边缘 ,为我国荒漠化土地的东缘。随着经济的发展 ,生态环境遭到严重破坏 ,荒漠化景观日益明显 ,前景令人堪忧。气候因素是荒漠化发展的一个基本因素 ,东北平原西部沙地是我国北方气候条件最好的沙区 ,但目前对于区域荒漠化驱动因子的气候因素影响方面的研究未开展系统的工作。论文系统分析了东北平原西部沙地影响荒漠化的现代气候因素特点 ,探讨了在较好气候条件下气候变异、人类活动与荒漠化之间的关系 ,并根据气候发展趋势预测了未来在自然因素作用下沙地的可能发展趋势。     

浑河抚顺市区段污染趋势分析

采用各种模型，对2010年浑河抚顺市区段污染趋势预测分析。结果表明，经济社会增长的同时入河污染物量大副增加，水环境也严重超标，必须采取相应防治对策。     

沈阳市和平区环境空气质量现状及变化趋势

本文通过对和平区近几年环境空气监测数据的分析,评价了和平区“八·五”期间的环境空气质量状况及变化趋势。     

煤与瓦斯突出预测研究动态及展望

笔者总结了以突出敏感性指标预测为基础的接触式煤与瓦斯突出预测技术的发展现状 ;阐述了瓦斯地质理论研究进展情况 ;对统计学方法、计算机模拟、模糊数学、灰色系统理论、神经网络技术、专家系统、分形理论、流变与突变理论等数学物理理论在煤与瓦斯突出预测领域中的应用情况作了系统的描述 ;对GIS技术、无线电波透视探测技术及以地震波为主的弹性波技术为煤与瓦斯突出预测技术的发展前景作了必要的分析。     

DIFFERENT TYPES OF DISASTERS IN RECENT 10 YEARS IN ANHUI AND THEIR TREND

TheconditionsofdisastersinAnhuiinrecent 1 0 years　Thenaturaldisastersandman madeaccidentsinAnhuiProvincecanbedividedintothefollowingtypes:Meteorologicaldisasters　Inthemovementofatmosphereandsynopticsystemoccurabnormality,whichcausestotheearthandhumansocialandeconomicactivitieseffectsanddamages,thatarecalledmeteo rologicaldisaster.AnhuiProvinceislocatedbetween 2 9°4 1′～ 34° 38′Nand 1 1 4°54′～ 1 1 9°37′E,theretheeastis 1 6 0kmapartfromtheYellowSea,andthenorthisthebroadHuang Huai …     

Analysis and Case Study of Duststorms in the Beijing Area

Dust weather conditions with strong wind often occur in Beijing during spring. The number of duststorms in Beijing has declined since 1954. In the last two years, however, the number of duststorms in Beijing has increased drastically due to frequent cold air movements and the deteriorated ecological environment. The heaviest duststorm in the last decade in Beijing occurred on 6 April 2000. It was caused by the development of a high-level small trough along with strong northwest wind behind a large trough that moved eastward and developed a strong cold air system. A non-hydrostatic meso-scale numerical model (MM5) gave a good forecast to the duststorm's major features and movement. Simulated results showed that there was a strong vertical ascending motion with a strong positive vorticity center in mid and low level. The mesoscale structure's formation and development and movement were consistent with the passage and moving direction of the duststorm. At the same time, the trajectories of air particles during this duststorm event and another case (on 27 March 2000) were estimated and analyzed, which had the comparable results with the real situation and the trajectory monitored by meteorological satellite. The trajectories analysis could help us study the transport track and sand source to some extent.