An Optimization Method for Estimating Constituent Mean Concentrations in Base Flow‐Dominated Flow

Pollutant coefficients have been widely used to assess runoff nonpoint source pollution from individual land uses (e.g., agricultural, residential) of a watershed. Pollutant coefficients, known as event mean concentrations (EMCs), were developed by the U.S. Environmental Protection Agency's Nationwide Urban Runoff Program (NURP) to serve as a national measure for characterizing pollutant loading in a receiving water body. The term “baseflow pollutant coefficient (BPC)” is used in this study as a surrogate for EMC to describe mean concentration of pollutants in base flow‐dominated flow. A method for characterizing base flow quantity and quality for different land uses was explored using inverse modeling with two optimization techniques (a least square method and a genetic algorithm [GA] optimization), land use information, and streamflow quantity and quality data. The inverse model was formulated as a constrained minimization problem and demonstrated with data for 15 watersheds in Indiana. Results showed that estimated pollutant coefficients are comparable to the published literature. This indicates that the proposed method has the potential to effectively estimate constituent mean concentrations for pollutant load determination in gauged and ungauged watersheds, albeit more analysis with larger and more robust datasets is desirable to further refine and validate the accuracy of the approach.     

滇西北农村生活能源使用现状及生物质能源开发利用研究——以兰坪县和香格里拉县为例

少数民族地区农村能源建设是中国能源可持续发展的一个特殊领域,是资源节约型社会和社会主义新农村建设的重要内容。论文以滇西北的兰坪县和香格里拉县的能源使用情况作为研究对象,通过实地调查,分析了在经济仍处于贫困状态的少数民族聚居的西南山区生活能源利用的特点:兰坪县和香格里拉薪柴的使用分别达85%和98%,而以太阳能、沼气、水能为代表的可再生能源的使用仅有7.0%和1.8%,由此产生了一系列的环境问题。论文对促进现代生物质能源的开发利用提出建议:制定农村能源资源开发利用规划,健全能源政策体系,争取国际经济和技术支持等。     

能值分析理论在耕地可持续利用评价中的应用研究——以南京市为例

评价指标体系是耕地可持续利用评价研究的难点,正确选择评价理论与方法,构建科学、合理的评价指标体系,为正确认识耕地利用的可持续性及制定相应政策提供理论与实践依据。文章引入能值理论,在传统评价方法基础上对耕地利用中物流、能流等以太阳能值为统一衡量标准,建立新的指标体系,并对南京市1995~2004年的耕地利用进行评价。结果表明,研究时段内南京市耕地利用是向可持续方向发展的,且其可持续利用经历了两个阶段:①1995~1998年可持续性下降阶段,综合系数从1995年的1逐渐下降到1998年的0.9570;②1998~2004年可持续性上升阶段,综合系数逐年上升到2004年的1.1123。与传统评价方法相比,引入能值理论后的评价结果更能全面、客观地反映耕地利用的可持续状况。     

贵州土地复垦发展现状及其对策研究

详细分析了贵州省土地复垦的发展现状以及近年来所做的工作及成效,研究了矿山开采等活动对贵州省土地资源造成的破坏及生态危害,提出了具体的土地复垦的技术措施。为了实现能源、环境、社会、人口和经济的可持续发展,土地复垦是必然选择。     

纸浆模塑缓冲材的技术研究

聚苯乙烯发泡塑料（EPS）作为缓冲包装的内衬件广泛用于电子产品的内包装,但其所带来的白色污染问题也日益严峻。研究以再生资源（废纸）为原料,生产产品内衬包装物——纸浆模塑缓冲材,并使其产业化,以替代发泡塑料包装物,改变发泡塑料包装物难降解所带来的污染和危害,并实现“废弃物—产品”的资源循环利用。     

浑善达克沙地退化草地的封育效果调查

封育保护是促进退化草地自然恢复的有效方法之一,为了研究实施京津风沙源工程措施以来浑善达克沙地沙质草场的围封效果,我们特对浑善达克沙地南缘地段的围封草场进行了调查,并取得了一些结果。     

西安市LUCC预测生态系统服务价值损失

人类活动作用于土地资源,使LUCC（土地利用／土地覆被变化）在全球环境变化过程中起主导作用,随着国际LUCC研究计划的进展,各国依据本国的实际情况开展研究。对西安市以往五年（2000-2004年）的土地利用基础数据开展调查统计分析,建立灰色系统动态GM（1,1）模型,预测2005—2010年西安市土地利用结构变化状况,尝试计算西安市土地生态系统服务价值损失（简称生态损失）,用一种直观经济指标-货币来反映这种生态损失。预测2010年西安市生态损失为331、84×10^6元。     

浅论林业生产与生态环境建设

森林是陆地生态系统的主体。林业是一项重要的公益事业和基础产业,承担着生态建设和林产品供给的重要任务,做好林业工作意义十分重大。目前在林业生产中,环境没有得到应有的保护,造成生态环境恶化,反之又影响了林业生产,因此林业生产应当是在保护环境的前提下,采取多种办法解决问题,例如采取生态采伐、建立自然保护区、退耕还林、分类经营、林业体制改革等手段,既保护了生态环境又能使林业生产可持续发展。     

鞍山市铁矿景观格局变化的遥感调查

采用1997和2007年2个时相的卫星遥感数据,对鞍山市城区周边铁矿典型景观类型的面积及其10年来的变化进行了遥感调查和分析。结果表明,国有矿山采矿场的面积相对稳定,边界无明显变化,民营矿山采矿场面积增加明显。采矿场面积变化与开采方式有关,国有矿山采用深凹露天开采,对地表破坏较轻,民营矿山采用山坡露天开采,对地表破坏较严重。排岩场的总面积有所增加,个别矿区增加明显。复垦绿地有大幅度增加,但仍低于排岩场扩张的速度。     

Effect of soil crust on evaporation and dew deposition in Mu Us sandy land, China

The development of soil crust on sandy land may affect the surface hydrological process. This paper investigates the process of evaporation and dew deposition influenced by different soil surface types which were dominated by sand, primitive biotic crust, and advanced biotic crust, respectively, in the south fringe of Mu Us sandy land in Northwest China from July to September of 2006. The experimental results indicate that the advanced biotic crust could increase evaporation and dew deposition compared to the primitive biotic crust and bare sand although the differences between them were not significant. The average evaporation from advanced biotic crust, primitive biotic crust and sand was 6.8, 6.6, and 6.5 mm/d, respectively, and water content is around 16.2 % in the condition of initially identical soil. The average dew amount on advanced biotic crust was 0.116 mm/d with extreme 0.05 and 0.24 mm/d. The average values on primitive biotic crust and sand were 0.105 and 0.101 mm/d, respectively, with extreme 0.04 and 0.21 mm/d for both treatments. Also, the dew deposition on advanced biotic crust seemed stable and might rest for a longer time than that on primitive biotic crust and sand. The results suggest that the advanced biotic crust possibly facilitates evaporation and dew deposition. Therefore, the development of biotic crust may potentially enhance the hydrological circulation in the upper sand layer in sandy land.