ICSTD反应器处理污泥的启动试验研究

新型内循环污泥浓缩消化反应器（ICSTD）处理污泥的启动运行试验采用某污水处理厂二沉池好氧活性污泥进行驯化培养,使反应器正常启动运行。在日处理量为50 L/d,进泥含水率为99.23％～99.46％,进泥VS/TS为0.65～0.73,进泥COD为4 115～5 780 mg/L,反应器容积负荷为1.31 kg COD/(m³·d)时,排泥含水率在96.2％～97.3％,排泥VS/TS为0.48～0.57,COD去除率在95％以上,出水pH在6.6～7.1,且上清液澄清。试验结果表明： ICSTD反应器处理污泥的启动试验,采用直接培养污泥启动的方式培养厌氧污泥历时66 d,能较快地培养厌氧污泥且运行稳定,对污泥的浓缩消化起到较好的作用,同时对反应器后续运行的消化效果提供了一个良好的条件。     

10%丁醚脲微乳剂在甘蓝和土壤中的残留及消解动态研究

建立了丁醚脲在甘蓝及土壤中残留量的高效液相色谱检测方法,并采用田间试验方法对丁醚脲在甘蓝及土壤中的残留消解动态进行研究,开展了最终残留试验.结果表明,在0.05～5.0 mg/kg添加水平范围内,丁醚脲在甘蓝和土壤中的平均添加回收率为82.5%～100.9%,相对标准偏差为4.5%～7.5%.残留消解动态研究表明,丁醚脲在甘蓝和土壤中的降解符合方程式Ct=C0e-kt;10%丁醚脲微乳剂在甘蓝和土壤中的半衰期分别为2.87～2.99 d和3.37～3.57 d.最终残留试验研究表明,在施用有效成分约为0.02～0.04 g/m2,施药1～2次,每次施药间隔期为7 d的情况下,北京市试验地内,10%丁醚脲微乳剂在甘蓝中的残留量为ND～0.18 mg/kg,土壤中的残留量为0.09～0.37 mg/kg;湖南冷水江市试验地内,10%丁醚脲微乳剂在甘蓝中的残留量为ND～0.24 mg/kg;土壤中的残留量为0.11～0.46mg/kg.对照日本的最大残留限量标准,产品符合我国及日本规定的质量安全要求.     

中国海岸带灾害地质查询及风险评价系统的设计与实现

介绍了"中国海岸带灾害地质查询及风险评价系统"开发研制的GIS平台,VB为二次开发工具,利用OLE技术集成开发.系统实现了对中国海岸带灾害地质的可视化查询、空间分析和综合评价,并为实施海岸带灾害地质综合管理和决策提供了科学依据.     

气候变化对长江源地区高寒草甸生态系统的影响

近十几年来,长江源区气候暖干化趋势明显,冰川退缩、湖泊萎缩、草场退化、土地沙漠化、水土流失等环境问题日益严重。高寒草甸是长江源地区主要的植被类型之一,在全球变化影响下,以耐低温寒冷的嵩草属（Kobresia）植物为建群种的高寒草甸将面临更严重的生态胁迫。以长江源地区高寒草甸生态系统为研究对象,采用国际通用的生物地球化学模型模拟高寒草甸生物量、生产力和土壤有机质等的动态变化,并综合考虑人类活动对生态系统生产力和营养元素生物地球化学循环的影响,探讨了全球气候变化对高寒草甸生态系统可能造成的影响。     

碱性氧化焙烧回收含铬污泥中的铬

采用碱性氧化焙烧工艺回收含铬污泥中的铬,以浸出渣作为焙烧填料,最佳工艺条件为：含铬污泥加入量10g,浸出渣加入量8g,焙烧温度700℃,焙烧时间40min,n（Cr2O3）：n（NaNO3）：n（Na2CO3）：n（NaOH）=1：2：3．5：10。在此条件下,碱性氧化焙烧工艺铬浸出率高达98％以上。     

生态环境脆弱地区油气田开发生态保护措施探讨

我国许多油气田处于生态环境脆弱地区,石油开采以及油气集输、储运等工程对生态环境的影响非常突出。文章依据生态保护的原则提出了油气田开发规划、设计、施工以及施工后几个阶段应当采取的生态保护措施,同时还提出了施工结束后的一些生态恢复措施,以供借鉴。     

崂山水库上游区生态环境需水量的计算

本文建立了崂山水库上游区生态环境需水量的计算方法,并计算了该区域的生态环境需水量.结果表明崂山水库上游区生态环境需水量为3089.78×104m3,其中植被生态环境需水量为2792.7×104m3,河流生态环境需水量为291.95×104m3,水库生态环境需水量为5.13×104m3.崂山水库上游区生产生活用水总量为63.67×104m3,多年平均水资源总量为4032.7×104m3,说明从全年来看该区域生态环境需水能够得到基本满足.但径流量年内分配极不均匀,大部分集中于丰水期,枯水期的生态环境需水可能无法保障.     

Water‐Yield Reduction After Afforestation and Related Processes in the Semiarid Liupan Mountains,Northwest China1

Abstract: The increase of coverage of forest/vegetation is imperative to improve the environment in dry‐land areas of China, especially for protecting soil against serious erosion and sandstorms. However, inherent severe water shortages, drought stresses, and increasing water use competition greatly restrict the reforestation. Notably, the water‐yield reduction after afforestation generates intense debate about the correct approach to afforestation and forest management in dry‐land areas. However, most studies on water‐yield reduction of forests have been at catchment scales, and there are few studies of the response of total evapotranspiration (ET) and its partitioning to vegetation structure change. This motivates us to learn the linkage between hydrological processes and vegetation structure in slope ecosystems. Therefore, an ecohydrological study was carried out by measuring the individual items of water balance on sloping plots covered by different vegetation types in the semiarid Liupan Mountains of northwest China. The ratio of precipitation consumed as ET was about 60% for grassland, 93% for shrubs, and >95% for forestland. Thus, the water yield was very low, site‐specific, and sensitive to vegetation change. Conversion of grassland to forest decreased the annual water yield from slope by 50‐100 mm. In certain periods, the plantations at lower slopes even consumed the runon from upper slopes. Reducing the density of forests and shrubs by thinning was not an efficient approach to minimize water use. Leaf area index was a better indicator than plant density to relate ET to vegetation structure and to evaluate the soil water carrying capacity for vegetation (i.e., the maximum amount of vegetation that can be supported by the available soil water for an extended time). Selecting proper vegetation types and plant species, based on site soil water condition, may be more effective than the forest density regulation to minimize water‐yield reduction by vegetation coverage increase and notably by reforestation. Finally, the focuses in future research to improve the forest‐water relations in dry‐land areas are recommended as follows: vegetation growth dynamics driven by environment especially water conditions, coupling of ecological and hydrological processes, further development of distributed ecohydrological models, quantitative relation of eco‐water quota of ecosystems with vegetation structures, multi‐scaled evaluation of soil water carrying capacity for vegetation, and the development of widely applicable decision support tools.     

庚烷与二氧化硫的光化学反应研究

研究了庚烷与二氧化硫的光化学反应,利用GC/MS对气相产物及气溶胶产物进行了定性分析,确定了部分产物：醇、酮、呋喃衍生物、有机酸、三氧化硫、一氧化碳、二氧化碳等,探讨了反应机理和反应动力学,考察了NO,NO2,O2对反应的影响。     

Effect of submergence-emergence sequence and organic matter or aluminosilicate amendment on metal uptake by woody wetland plant species from contaminated sediments

Site-specific hydrological conditions affect the availability of trace metals for vegetation. In a greenhouse experiment, the effect of submersion on the metal uptake by the wetland plant species Salix cinerea and Populus nigra grown on a contaminated dredged sediment-derived soil and on an uncontaminated soil was evaluated. An upland hydrological regime for the polluted sediment caused elevated Cd concentrations in leaves and cuttings for both species. Emergence and soil oxidation after initial submersion of a polluted sediment resulted in comparable foliar Cd and Zn concentrations for S. cinerea as for the constant upland treatment. The foliar Cd and Zn concentrations were clearly higher than for submerged soils after initial upland conditions. These results point at the importance of submergence-emergence sequence for plant metal availability. The addition of foliar-based organic matter or aluminosilicates to the polluted sediment-derived soil in upland conditions did not decrease Cd and Zn uptake by S. cinerea.