温度对好氧颗粒污泥处理纤维素乙醇废水脱氮效能的影响

采用SBR反应器,考察了温度对好氧颗粒污泥处理纤维素乙醇废水脱氮性能的影响.研究结果表明,当进水为纤维素乙醇废水原水时,稳定阶段不同温度(10、20、30℃)条件下体系对COD的去除率分别为10.2%、12.7%、13.7%;总无机氮的去除率分别为42.8%、53.6%、70.5%,温度的升高明显地提高了硝化菌的活性和生长速率,进而促进了脱氮效果.当进水为纤维素乙醇废水经IC工艺处理后的厌氧出水时,3个温度条件下系统对废水中有机物的去除效果无较大差异,去除率均低于15%,主要因为纤维素乙醇废水的厌氧处理出水中的有机物很难被微生物利用;而温度对脱氮效果影响较大,30℃下NH_4~+-N去除率达到60.9%,分别是10℃和20℃时的2.0和1.3倍,并且,随着温度的升高总无机氮的去除率增强,NO_3~--N的去除量增加.由于体系COD去除率低说明反硝化可利用的碳源不足,因此,系统内可能存在内碳源反硝化作用,而且内碳源反硝化作用也随着温度的升高而增强.通过氮平衡计算可知,3个温度条件下氮损失分别为37.6%、45.0%、53.6%,说明温度的升高不仅提高了硝化菌活性,还促进了内碳源反硝化,进而提高了对氮素的去除.     

羊粪生物炭对水体中诺氟沙星的吸附特性

以羊粪为原料分别在350、450、550、650℃条件下制备生物炭,通过元素分析、BET-N_2、电镜扫描及FTIR表征了不同热解温度下羊粪生物炭的结构特征,并采用序批实验研究了pH、生物炭投加量、热解温度、初始浓度等因素对羊粪生物炭吸附水体中诺氟沙星(NOR)的影响及吸附机制.结果表明,随着热解温度的升高,生物炭的比表面积、总孔容、平均孔径增大,芳香性和稳定性也有所提高.羊粪生物炭吸附NOR的最佳初始pH为6.0,吸附在180 min左右达到平衡,采用准二级动力学模型能更好地拟合动力学数据(R~20.96),吸附速率由表面吸附和颗粒内扩散共同控制.等温吸附拟合发现,Langmuir模型能较好地描述NOR在羊粪生物炭上的吸附行为(R~20.93),吸附过程均为有利吸附,且可能与氢键和π-π键作用密切相关,4种热解温度下生物炭的吸附能力大小为:650℃550℃450℃350℃.吸附过程中ΔGθ0、ΔHθ0、ΔSθ0,表明羊粪生物炭对NOR的吸附是自发、吸热及熵增加的过程.650℃和550℃条件下制备的羊粪生物炭可作为水体中NOR的优势吸附材料.     

佛山地区干季边界层垂直风温结构对空气质量的影响

利用佛山地区2013年12月大气边界层观测试验得到的垂直风温资料和相应逐日AQI资料、逐时PM_(2.5)浓度资料,研究了佛山地区大气边界层垂直风温结构对空气质量的影响.结果表明:佛山地区干季持续存在的逆温结构是导致PM_(2.5)污染较重的重要原因.干季污染日近60%的最低逆温层高度低于1000 m,而非污染日低于1000 m的最低逆温层仅占36%,污染日佛山贴地逆温频率高达31.2%.逆温层出现高度较低,将污染物压缩积累在贴地层大气中导致污染较重.在大陆冷高压控制下,佛山地区的边界层结构演化非常典型,最大边界层高度和最大边界层通风量表现出了显著相关,污染日日平均边界层高度始终维持在较低的水平,多数时候不足500 m,最大边界层高度则大部分小于1000 m,日平均边界层通风量主要分布在500~1500 m~2·s~(-1)之间,在极端情况下甚至不足300 m~2·s~(-1),最大边界层通风量大部分处于1500~5000 m~2·s~(-1)之间,导致污染物始终聚集在较低的大气边界层内,使得PM_(2.5)浓度长时间维持在较高的污染水平.佛山地区风场存在显著的3层结构,较小的底层风速意味着大气的输送和扩散能力较弱,高度较低的中层使得污染物进一步被压缩累积在大气底层,垂直风场的不稳定性使得污染日佛山地区局地回流活跃,回流(RF)指数极小值多分布在0.2~0.4之间,污染日RF指数普遍小于非污染日,垂直风场的有效输送能力被显著削弱.     

Estimating Plecoglossus altivelis altivelis migration using a mass balance model expressed by hydrological distribution parameters in a major limpid river basin in Japan

We examined the influence of several hydrological and meteorological parameters on the migratory movements of ayu Plecoglossus altivelis altivelis in central Japan. When comprehensively evaluating rivers and ayu behaviour on a catchment scale, the subjects of analysis typically include human activities and hydrological and meteorological phenomena. However, limiting analyses to such factors may be too restrictive when human activities are being conducted. Accordingly, we incorporated a biological viewpoint into the evaluation method, analysing hydrological data (river discharge, river water temperature, sea water temperature) to determine watershed characteristics and examining the relationship between these characteristics and the habitat conditions of ayu. Then we constructed a numerical model for ayu migratory runs that incorporated ayu ecology and watershed characteristics. Analyses of ayu movements from a lower estuarine dam demonstrated that downstream displacements were associated with high water flows of more than 200 m³ s⁻¹ at the beginning of summer. We conclude that it is important to consider the effects of environmental parameters on the movements of different fish species to understand the causes of spatial variation in fish distribution in lowland rivers.     

气候试验箱内部条件不确定度计算(下)

提供了对温度和湿度气候试验箱内部环境条件进行不确定度分析的方法。首先介绍了测量的不确定度概念,然后讨论容差的意义。考虑到湿度和温度测量是采用确定和合成不确定度。结合校准空载试验箱和有负载试验箱的条件测量的案例。最后,逐条整理成为范本用于分析结果以给出规范的不确定度评估依据。     

三叶鬼针草生物量分配与化感作用对大气温度升高的响应

全球气候变暖已经成为不容置疑的事实,同时外来入侵植物对入侵地的生态环境造成严重的危害,外来入侵植物可能对温度升高做出积极地响应。文章研究了不同温度(22、26和30℃)处理对入侵植物三叶鬼针草(Bidens pilosa L.)种子萌发、幼苗生物量分配及化感作用的影响,探讨三叶鬼针草对全球气候变暖的响应策略。结果表明;温度为22和26℃比30℃有利于三叶鬼针草种子的萌发。温度升高显著增加三叶鬼针草的株高、生物量和叶面积,三叶鬼针草幼苗增加对茎和叶的生物量投资。同时相同浓度的三叶鬼针草水浸提液对马唐(Digitaria sanguinalis(L.)Scop)和牛筋草(Eleusine indica(L.)Gaertn)的化感作用随着温度升高而增强。研究表明:温度升高促进了三叶鬼针草的生长,改变生物量分配模式同时增强了对受体植物的化感作用。温度升高可能是促进三叶鬼针草入侵的生态环境因子之一,未来全球气温变暖可能使其入侵加剧。     

成都市城市效应对大气环境的影响

本文利用1979—1981年气象资料用统计方法分析了城市热岛效应对主要气象要素时空分布特征的影响(例如:温度、无霜期、风速、日照、云量、降水量、雷暴、雨日、雾日和土壤温度),结果表明:城市效应对市区大气环境的影响是明显的。     

THE SENSITWITY OF NORTHERN SIERRA NEVADA STREAMFLOW TO CLIMATE CHANGE1

ABSTRACT: The sensitivity of streamflow to climate change was investigated in the American, Carson, and Truckee River Basins, California and Nevada. Nine gaging stations were used to represent streamflow in the basins. Annual models were developed by regressing 1961–1991 streamflow data on temperature and precipitation. Climate-change scenarios were used as inputs to the models to determine streamflow sensitivities. Climate-change scenarios were generated from historical time series by modifying mean temperatures by a range of +4°C to—4°C and total precipitation by a range of +25 percent to -25 percent. Results show that streamflow on the warmer, lower west side of the Sierra Nevada generally is more sensitive to temperature and precipitation changes than is streamflow on the colder, higher east side. A 2°C rise in temperature and a 25-percent decrease in precipitation results in stream-flow decreases of 56 percent on the American River and 25 percent on the Carson River. A 2°C decline in temperature and a 25-percent increase in precipitation results in streamflow increases of 102 percent on the American River and 22 percent on the Carson River.     

INVESTIGATION OF TURBIDITY MAXIMUM IN A MESOTIDAL ESTUARY,TAIWAN1

ABSTRACT: To comprehend the distributions of salinity, temperature, and suspended sediment in the Danshuei River estuary in Taiwan, monthly field surveys were conducted in 2003. These included several high and low slackwater surveys and intensive surveys. The results show that the Danshuei River estuary is predominately a partially mixed estuary. The highest concentration of suspended sediment is typically observed at the Chung‐Hsin Bridge, the most upstream sampling station. The suspended sediment concentration exhibits a general decreasing trend in the downstream direction. It may be concluded that the sediments mostly come from the upstream reach. A locally high concentration of suspended sediment is found at the Kuan‐Du station because of the local deep channel bathymetry and two‐layered estuarine circulation. A vertical two‐dimensional hydrodynamic and sediment transport model is applied to investigate the tidally averaged salinity distribution, residual circulation, and suspended sediment concentration. The modeling results reveal that, under the Q₇₅ flow condition (i.e., low flow), a turbidity maximum occurs at the Kuan‐Du station due to the strong estuarine circulation. The model simulation with a much higher river flow condition results in a weaker residual circulation and weaker turbidity maximum.     

Comprehensive temperature monitoring in an in-vessel forced-aeration static-bed composting process

Comprehensive temperature monitoring was done in an in-vessel forced-aeration static-bed composting process using sewage sludge. The three layers that divided the compost pile horizontally showed different temperature distributions. The temperature of the top layer appeared not to be influenced by the ambient temperature. The temperature of the center area of the top layer was taken to be the representative temperature for evaluating composting start-up performance. The temperature of the bottom layer was strongly influenced by the ambient temperature, and the temperature of the center area of the bottom layer was taken to be the representative temperature for pathogen control as it was the minimum temperature in the reactor. Composting start-up performance was influenced by several factors when the ambient temperature was either below or above 20°C. When the ambient temperature was below 20°C, the time taken to reach 65°C (T ₆₅) was influenced by the temperature of inflowing air, but when the temperature was higher than 20°C, it was influenced by the ratio of sewage sludge to seed compost (F/S). T ₆₅ was least when F/S was 1–2. Received: January 9, 2001 / Accepted: October 10, 2001