导流明沟人工湿地治理橡胶废水实践

运用人工湿地原理，采用明沟导流治理橡胶生产废水，其工程投资低，占地面积小，运行稳定，易于管理，去除率高，处理后废水达到国家标准。     

Enhancing treatment efficiency of swine wastewater by effluent recirculation in vertical-flow constructed wetland

Introduction Livestock w astew ater contains highly concen- trated pollutants, including suspended solids (SS), organics, nutrients and bacteria. In C hina, w astew ater generated by concentrated farm s is com m only stored in anaerobic lagoons and partia…     

碳酸盐岩地表岩溶与红粘土

从红粘土的分布特征、土体构造特征及土性特征入手,系统研究红粘土的成因,包括研究碳酸盐岩地表岩溶与红粘土的相互作用、红粘土的物质来源、土中矿物的种类和形成条件;着重分析碳酸盐岩地表岩溶的作用、特点对红粘土形成的重要影响;认为碳酸盐岩地表岩溶作用和红土化作用是红粘土特殊成因中的两种最重要的地质作用,而前者不仅是控制红粘土性质的主要因素,还影响成土后期的土质演化过程。红粘土特殊性的本质源于特殊的成因。     

神头泉域人类活动的水资源-环境效应

神头泉是山西省朔州市的重要供水水源，泉域内的岩溶水开采引发了一系列环境地质问题。本文介绍了神头泉域岩溶水资源的开发利用历史及现状，对水资源开发导致的泉流量衰减、地下水位下降、地下水污染等水资源-环境效应进行了评述，并在此基础上提出了相应的岩溶水资源保护措施，为该地区岩溶水资源的可持续利用提供了理论依据。     

人工湿地基质除磷影响因素研究进展

基质除磷被认为是人工湿地中磷去除的主要方式。人工湿地基质除磷不仅受其自身化学特性的影响,还受到废水磷负荷、水力条件、运行方式、温度、溶解氧、pH、竞争性离子等的影响,结合国内外的最新研究进展较全面地论述了上述因素对基质除磷效果的影响。最后对吸附饱和基质的去向进行了一定的探讨。     

云南砚平高速公路岩溶的勘察与处治研究

文章叙述了砚平高速公路岩溶勘察情况,分析了砚平高速公路岩溶的工程地质特征及工程地质问题,提出了砚平高速公路岩溶的工程地质分类及处治原则,对岩溶地区公路的建设具有一定的参考和指导作用。     

不同进水方式人工湿地除污效率对比分析

研究了人工湿地在间歇流、连续流进水方式下处理生活污水的效率．并进行了对比分析。在平均水力负荷4.8cm／d时，间歇流和连续流人工湿地COD平均去除率分别为78％和64％；NH3-N平均去除率分别为60％和44％；TP平均去除率均为53％。结果表明，间歇流进水能够提高床体内的含氧量，缓解植物根系放氧不足．提高了污染物去除率。     

天津市湿地资源开发的累积环境影响评价初探

历史上天津市自然湿地资源十分丰富,几十年来湿地大面积萎缩和生态功能急剧退化。天津湿地生态系统存在的主要问题是湿地生态系统如何恢复、重建和功能修复。文章在对天津市湿地生态环境建设的现状与湿地景观变化发展主要问题进行分析的基础上,探讨了湿地生态建设的目标、任务和对策,论述了湿地资源开发利用过程中累积影响评价(CIA)在政策、规划、计划及项目的各个层次都应得到充分考虑,建议明确将累积影响评价纳入到资源开发利用的体系,推动环境影响评价实践的进一步深入开展。     

中外大河河口湿地保护与利用初探

在分析研究河口湿地形成与演变、河口湿地生态系统特征的基础上 ,对中外大河河口湿地保护与利用现状进行了初步研究 ,以期为中国河口湿地保护与利用提供一定的借鉴和启示     

Nitrogen cycling of atmosphere-plant-soft system in the typical Calamagrostis angustifolia wetland in the Sanjiang Plain,Northeast China

The nitrogen(N)distribution and cycling of atmosphere-plant-soil system in the typical meadow Calamagrostis angustifolia wetland (TMCW)and marsh meadow Calamagrostis angustifolia wetland(MMCW)in the Sanjiang plain were studied by a compartment model.The results showed that the N wet deposition amount was 0.757 gN/(m~2.a),and total inorganic N(TIN)was the main body (0.640 gN/(m~2.a)).The ammonia volatilization amounts of TMCW and MMCW soils in growing season were 0.635 and 0.687 gN/m~2, and the denitrification gaseous lost amounts were 0.617 and 0.405 gN/m~2,respectively.In plant subsystem,the N was mainly stored in root and litter.Soil organic N was the main N storage of the two plant-soil systems and the proportions of it were 93.98% and 92.16%, respectively.The calculation results of N turnovers among compartments of TMCW and MMCW showed that the uptake amounts of root were 23.02 and 28.18 gN/(m~2.a)and the values of aboveground were 11.31 and 6.08 gN/(m~2.a),the re-translocation amounts from aboveground to root were 5.96 and 2.70 gN/(m~2.a),the translocation amounts from aboveground living body to litter were 5.35 and 3.38 gN/(m~2.a),the translocation amounts from litter to soil were larger than 1.55 and 3.01 gN/(m~2.a),the translocation amounts from root to soil were 14.90 and 13.17 gN/(m~2.a),and the soil(0-15 cm)N net mineralization amounts were 1.94 and 0.55 gN/(m~2.a), respectively.The study of N balance indicated that the two plant-soil systems might be situated in the status of lacking N,and the status might induce the degradation of C.angustifolia wetland.