水质对UV/H_2O_2降解2,4-二氯酚的影响

研究了UV/H2O2工艺对2,4-二氯酚(2,4-DCP)的去除效果和水中阴离子、腐殖酸对该工艺降解2,4-DCP的影响。结果表明:UV/H2O2工艺可以有效的去除水中2,4-DCP,光降解过程符合一级反应动力学模型;在H2O2投加量为8mg/L,1个30W低压汞灯照射下,2,4-DCP在蒸馏水和自来水中光降解速率常数分别为0.0232/min和0.0162/min;NO3-、Cl-、HCO3-对2,4-DCP光降解有抑制作用;当3种离子浓度为0.5mmol/L、10mmol/L、20mmol/L时,对2,4-DCP光降解的抑制程度为HCO3->NO3->Cl-;随着离子浓度增大,抑制作用增强;自来水中的光降解速率常数低于蒸馏水中的光降解速率常数是由于水中多种离子影响的结果;腐殖酸在低浓度时,促进光降解反应的进行,在高浓度时,2,4-DCP的光降解氧化受到抑制。     

以有机农业为载体推进循环经济建设

分析了有机农业与循环经济的理论联系,论述了发展有机农业的必要性,提出了宝应应从有机食品基地、有机产业园、科学规划、市场化运作等方面来发展有机农业,并在此基础上,建设西湖、运西、东荡、中部四大循环经济示范园区,继而推进循环经济建设.     

气单胞菌SH10吸附银离子机制的研究

以气单胞菌SH10为生物吸附材料,从静电吸附作用、离子交换作用、络合作用、沉淀作用几方面研究了SH10吸附Ag 过程可能存在的作用机制.结果表明,气单胞菌SH10吸附银离子依赖于静电吸附作用;吸附Ag 前后溶液中Na 、K 、Mg2 浓度的变化较小,说明吸附过程中离子交换不明显;SH10表面的羧基、氨基和脂类基团经化学屏蔽后,对Ag 的吸附量明显下降,结合红外光谱分析结果,确定酰胺基CO-NH为SH10与银离子发生络合作用的主要官能团;电镜扫描结果表明,SH10在吸附过程中可以和Ag 形成沉淀沉积在细胞表面.     

二苯并噻吩降解菌筛选及16S rDNA序列分析

以DBT(dibenzothiophene,二苯并噻吩)为模型化合物,分离得到了一株能降解DBT的微生物HB2,应用HPLC对其脱硫特性进行了检测。应用PCR技术克隆到16SrDNA片段,核苷酸序列分析结果表明,该菌的16SrDNA全序列与假单胞菌存在98%的同源性,初步确定该菌在微生物系统发育学上的地位。     

上海市南汇区水环境污染成因及防治对策

根据南汇区环境监测站对区域内8条主要河流中24个监测断面的水质监测资料（2001-2005年），分析了南汇区水环境污染现状，并利用水质综合指数法对水质年际变化进行了评价。从主要污染源，环境保护基础设施和工业结构等方面，分析了南汇区域内水环境污染的成因，结合第3轮“环保三年行动计划”提出了水环境污染防治对策。     

催化CODcr快速测法的精密度与准确度实验

化学需氧量标准分析方法测定时间长、操作繁琐。本实验采用CTL—BX3C型便携式COD快速测定仪能在20分钟获得COD数据，同时耗能低、省时省力、减少污染。催化CODcr快速法的精密度与准确度均能达到要求。     

环境监测技术培训需求分析——应用OTP模型

简述了环境监测技术培训需求分析的重要性及OTP模型的概念.针对环境监测技术培训的现状和特点,设计了符合环境监测技术培训特点的OTP模型,提出了系统分析环境监测技术培训需求的方法,以及根据实际情况科学设置输入项的不同权重,充分考虑影响模型输出的各种因素,加强研究模型输入项的量化表征,动态调整模型的输入项的建议.     

盲样考核浓度预判及稀释方法——以原子荧光法测定水中砷为例

以原子荧光法测定水中砷为例,探讨了实验室盲样考核浓度预判及稀释方法.分析了3个砷盲样考核实例,归纳了“直接稀释法”“系列稀释法”“最大稀释法”3种方法,分别适用于盲样浓度范围窄、适中、宽3种情况,检测人员可根据考核机构给定的浓度范围合理选用.     

Estimation of phosphorus flux in rivers during flooding

Reservoirs in Taiwan are inundated with nutrients that result in algal growth, and thus also reservoir eutrophication. Controlling the phosphorus load has always been the most crucial issue for maintaining reservoir water quality. Numerous agricultural activities, especially the production of tea in riparian areas, are conducted in watersheds in Taiwan. Nutrients from such activities, including phosphorus, are typically flushed into rivers during flooding, when over 90 % of the yearly total amount of phosphorous enters reservoirs. Excessive or enhanced soil erosion from rainstorms can dramatically increase the river sediment load and the amount of particulate phosphorus flushed into rivers. When flow rates are high, particulate phosphorus is the dominant form of phosphorus, but sediment and discharge measurements are difficult during flooding, which makes estimating phosphorus flux in rivers difficult. This study determines total amounts of phosphorus transport by measuring flood discharge and phosphorous levels during flooding. Changes in particulate phosphorus, dissolved phosphorus, and their adsorption behavior during a 24-h period are analyzed owing to the fact that the time for particulate phosphorus adsorption and desorption approaching equilibrium is about 16 h. Erosion of the reservoir watershed was caused by adsorption and desorption of suspended solids in the river, a process which can be summarily described using the Lagmuir isotherm. A method for estimating the phosphorus flux in the Daiyujay Creek during Typhoon Bilis in 2006 is presented in this study. Both sediment and phosphorus are affected by the drastic discharge during flooding. Water quality data were collected during two flood events, flood in June 9, 2006 and Typhoon Bilis, to show the concentrations of suspended solids and total phosphorus during floods are much higher than normal stages. Therefore, the drastic changes of total phosphorus, particulate phosphorus, and dissolved phosphorus in rivers during flooding should be monitored to evaluate the loading of phosphorus more precisely. The results show that monitoring and controlling phosphorus transport during flooding can help prevent the eutrophication of a reservoir.     

基于Sentinel-2与随机森林算法的太湖水生植被分布监测

基于2018—2021年太湖地区哨兵2号（Sentinel-2）卫星遥感影像和随机森林算法,结合植被敏感指数,开展太湖水生植被分布监测,综合分析了水生植被的时空变化特征,初步揭示了太湖水生植被的动态变化。结果表明,太湖水生植被分布面积有逐年上升的趋势,且年间变化具有明显的单峰型特征,表现为春季沉寂,夏季快速增长,秋季达到暴发期,冬季面积开始减退;太湖水生植被主要分布于东太湖、东部沿岸和贡湖,类型以沉水植被为主,其中浮叶植被主要分布于东太湖,挺水植被主要分布于东太湖沿岸的浅水区域;沉水植被主要分布于东部沿岸和贡湖;水生植被主要分布的东太湖水域,其水质总体优于太湖其他水域。