用土壤法进行生活污水的深度处理

土壤是物质生产的场所,也是物质降解的中心。利用土壤法进行生活污水的深度处理,具有成本低,能耗低,不需要维护等特点,并且可以循环利用土壤和水资源,实现水环境的再生。土壤法的推广利用符合中国循环经济的发展要求,促进新农村运动的开展。本文着重介绍了如何利用和加强土壤的净化功能来进行生活污水的处理,并且回顾了土壤处理法的发展历史和研究现状。     

An integrated assessment method of urban drainage system:A case study in Shenzhen City,China

In recent years, the urban drainage system in China is facing the dual pressure of renovation and construction. This requires that the integrated assessment for the planning and operation of the urban drainage system is obligatory. To evaluate the urban drainage system, an integrated assessment methodology based on the analytic hierarchy process (AHP), integrated simulation, and fuzzy assessment is established. This method is a multi-criteria decision adding app roach to the assessment of the urban drainage system comprehensively. Through the integration of the Storm Water Management Model (SWMM), a simple wastewater treatment plant model, and a surface water quality model, an integrated modelling system for the urban drainage system is developed and applied as a key tool for assessment. Using the established method, a case study in Shenzhen City has been implemented to evaluate and compare two urban drainage system reno vation plans, the distributed plan and the centralized plan. Because of the particularity of this case study, the established method is not applied entirely. Considering the water environ mental impact, ecological impact, technological feasibility, and economic cost, the integrated performance of the distri buted plan is better. As shown in this case study, the proposed method is found to be both effective and practical.     

生物陶粒——硅藻土联合工艺脱氮除磷

试验采用硅藻土和生物接触氧化组合工艺处理污水处理厂出水,氨氮从10mg／L下降到0．5mg／L以下,去除率70～95％;硅藻土澄清池对总磷的去除率高于95％;且对浊度、色度均有良好的去除效果。     

云南腾冲地区大气降水中氢氧稳定同位素特征

为了揭示腾冲地区降水中氢氧稳定同位素特征,利用2009年1月～2011年12月腾冲地区339个降水样品资料,对降水中的氢、氧同位素组成及其影响因素进行了分析和研究。结果表明：腾冲地区大气降水中δ18O值变化范围为-2678‰～405‰,δD值变化范围为-20095‰～3689‰,均处于全球降水δ18O与δD值变化范围内。天气尺度下,腾冲地区降水中δ18O的变化具有显著的降水量效应以及反温度效应。但是,在季风降水期间,如果相邻两天都有降水发生时,腾冲地区降水中δ18O值变化并不一定遵循“降水量效应”。利用ECMWF（European Centre for Medium Range Weather Forecasts）提供的TCWV（Total Column Water Vapour）再分析资料,发现TCWV与δ18O的日变化存在明显的反位相对应关系。腾冲地区的大气降水线为：δD=818δ18O+1172,斜率与截距均比全球和全国的大气降水线偏大,说明该地区气候湿润多雨。d值分布具有季节差异,在雨季（4～9月）,腾冲地区降水的水汽主要来源于低纬度海洋,空气湿度大,降水中d值较小;在干季（10～3月）,由于受大陆性气团控制,腾冲地区降水的水汽主要来源于西风带的输送以及局地再蒸发水汽的补充,空气湿度小,降水中d值较大     

Spatial-temporal analysis of wetland landscape pattern under the influence of artificial dykes in the Yellow River delta

The influence of anthropogenic activities,especially artificial dykes,on the coastal wetland landscape is now considered as a serious problem to the coastal ecosystem.It is important and necessary to analyze changes of coastal landscape pattern under the influence of artificial dykes for the protection and management of coastal wetland.Our study aimed to reveal the quantitative characteristics of the coastal wetland landscape and its spatial-temporal dynamics under the influence of artificial dykes in the Yellow River delta(YRD).It was analyzed by the methods of the statistical analysis of landscape structure,five selected landscape indices and the changes of spatial centroids of three typical wetland types,including reed marshes,tidal fiats and aquaculture-salt fields.The results showed that:(1)Reduction of wetland area,especially the degradation of natural wetlands,had been the principal problem since the dykes were constructed in the YRD.The dykes created conditions for the development of artificial wetlands.However,the new born artificial wetlands were still less than the vanished natural wetlands.(2)Compared with the open area,the building of artificial dykes significantly speeded up the changes of landscape patterns and the aggravation of the landscape fragmentation in the closed area.(3)The changes of area-weighted centroids of three typical wetland landscapes were greatly affected by dykes,and the movement of the centroid of the aquaculture-salt field was very sensitive to the dykes constructed in the corresponding period.     

Application of Tradable Emission Permits in Europe

Abstract

The purpose of this study is merely to review the current situation in the designing and implementation of the emission trading programs in Europe. Historical data show that although there is a series of shortcomings in their current functioning, employing such instruments for GHG reduction policy making is strongly expected to be efficient and effective. The European Union Emission Trading Scheme (EU ETS), Clean Development Mechanism (CDM) and Joint Implementation (JI) are just a few examples of the ambitious EU initiative that heavily relies on such instruments. We dwell on their operations and achievements by far and all the content in this article is expected to convince the Chinese government and regional public authorities to take positive actions and attitudes in promoting these instruments.     

皖江城市带农田生态系统碳排放动态研究

基于化肥、农药、农膜、农业灌溉、农地翻耕、农机运用、农作物收割后残留根系分解 7个主要碳源,测算皖江城市带1991~2010年农业碳排放量。结果表明：研究区农业碳排放总量从1991年的273万t增加到2010年的535万t,年均增长率为1035%,同时2010年其排放量约占安徽省碳总排放量的443%。1991~2010年研究区人均农业碳排放年均增幅26%,农业碳排放密度年均增幅584%,碳排放强度年均降幅3769 t/亿元。研究区农业碳排放以农作物收割后残留根系分解为主(占总排放量的5987% ),且化肥碳排放比重年均增长最快达1618%。各市农业碳排放量六安最大,安庆较大,铜陵最小,其中平均增幅最大为六安298万t/a,最小为铜陵009万t/a;碳排放强度最大为六安,较大为滁州,最小为铜陵,平均降幅最大为滁州64774 t/（亿元·a）,最小为铜陵19760 t/（亿元·a）;人均农业碳排放量最大为滁州,最小为铜陵,人均增加量最大为六安460 kg/a,最小为合肥039 kg/a;碳排放密度年均增幅最大为芜湖836%,最小为马鞍山345%。最后根据该区农业碳源的构成特点和动态特征,为其降低农业碳排放提出一些建议     

铁氮共掺杂生物炭对二级水溶解性有机物的吸附特性与长效性评价

为经济高效地去除污水厂二级水中溶解性有机物(DOM),采用铁氮共掺杂生物炭材料(Fe-N-C)作为新型吸附剂,系统分析了该新型碳材料对于二级水DOM的吸附性能、动力学过程、选择性和作用机制.此外,通过固定床吸附装置深入考察了该吸附材料的长效性和重复利用性.结果表明,Fe-N-C对于二级水DOM具有突出的吸附性能,投加量...     

可见光促有机物诱导铁还原的多相类芬顿体系强化效能与机制

近年来,亚铁离子活化过硫酸盐的类芬顿(Fe²⁺-PMS/PS)高级氧化技术发展日趋成熟,但因Fe³⁺无法还原导致反应停止的问题仍制约其大规模应用.结果发现,当把以双酚A（BPA）为代表的某些有机物与Fe³⁺和TiO₂混合,所形成的某种络合物可以拓宽TiO₂光响应范围捕获可见光,通过TiO₂将光生电子传递给Fe³⁺进行还原,从而实现Fe³⁺/Fe²⁺的无限循环.依据上述原理,构建了可见光下BPA-TiO₂-Fe³⁺-PS复合体系来降解BPA,并对其催化性能、催化机制和影响因素进行探讨.结果表明,该体系具有突出的催化性能,60 min内BPA(50 mg·L^-1)降解率达到93.1%,矿化度达到70%.同时验证该体系可以通过双酚A自生光电子还原Fe³⁺, 60 min还原得到的Fe²⁺稳...     

外源输入对底泥疏浚新生表层磷恢复及迁移的影响

外源输入对底泥疏浚新生表层磷恢复及迁移转化的影响尚不清楚,阐明该问题对于底泥疏浚实施后流域尺度上的外源控制及管理具有重要的意义.本研究以太湖梅梁湾沉积物为研究对象,采用野外原位模拟疏浚的方法研究在有无外源颗粒物输入条件下,疏浚前后新生泥水界面磷的迁移转化过程,并探讨疏浚对内源磷释放的控制效果.结果表明,疏浚后阻止外源颗粒物输入对沉积物总磷(TP)和总氮(TN)的控制产生着积极的影响;疏浚显著降低了表层沉积物潜在可移动磷的含量,有外源颗粒物输入组潜在可移动态磷(Mobile-P)含量显著高于无外源组,变化的Mobile-P以铁结合态磷(Fe-P)为主,有机磷(Org-P)次之,弱结合态磷(Lb-P)含量较低不足总磷的1‰;实验210d后,有外源颗粒物输入疏浚组间隙水PO_4~(3-)-P浓度低于未疏浚组,无外源疏浚组显著低于未疏浚组(P 0. 05);无外源疏浚组间隙水PO_4~(3-)-P浓度保持着较低的水平,其余组间隙水中PO_4~(3-)-P浓度呈现先增加后减小的趋势,间隙水PO_4~(3-)-P浓度与其对应分层沉积物中Fe-P含量显著正相关;冬春季间沉积物的源-汇功能发生了转变,沉积物对上覆水由汇转变成为源;疏浚措施降低了底泥内源磷释放速率,可有效控制其内源磷释放,阻止外源颗粒物输入对疏浚控制内源磷负荷起到了较好的促进作用.