光催化氧化（UV+TiO2）法处理印染废水生化出水及其各类有机物去除

采用UV+TiO2光催化氧化法处理印染废水生化出水,考察了反应时间、TiO2投加量以及初始pH对反应的影响,结果表明,TiO2投加量800 mg·L-1,反应时间8 h,反应pH为原水pH(6.5～8.0),在此操作条件下,ADMI7.6、DOC和COD的去除率分别为86%、20%及46%;选取两组反应条件,对其进出水采用XAD-8/XAD-4树脂联用技术,分析疏水酸、非酸疏水物质、弱疏水物质及亲水物质4类有机物的去除情况,结果表明,UV+TiO2光催化氧化处理工艺都能够长期有效去除印染废水生化出水中的弱疏水物质、疏水物质和非酸疏水物质引起的色度.     

印染废水生化出水中有机污染物特性及在硫酸镁混凝过程中的去除行为

以某印染废水二级生化出水为研究对象,考察了生化出水中有机污染物中各组分含量、分子量分布特点等特性,以及各类有机物在硫酸镁混凝处理过程中的去除行为.实验结果表明,该印染废水的生化出水溶解性有机物的主要成分是疏水性物质,以溶解性有机碳（DOC）表征时占总DOC的78%,其中非酸疏水物质约占46%,而以UV254表征时约占总55%,以美国染料生产协会色度值（ADMI7.6）表征时为97%,其中以非酸疏水物质的贡献最大,达到66%,并且非酸疏水物质中不饱和双键或芳香环有机物的含量较高.生化出水中的DOC主要集中在小于1000 D的有机物上,占37%.在硫酸镁的最佳混凝条件下,可以有效地去除由大分子量的非酸疏水物质引起的色度,而对小分子量的有机物也有一定的去除效果.     

Ca(OH)_2絮凝沉淀-臭氧氧化垃圾渗滤液生化出水提高反渗透性能

为了提高生化出水的反渗透性能,本文提出采用Ca(OH)_2絮凝沉淀预处理生化出水,再经O_3氧化后,用于反渗透膜的深度处理工艺.研究表明,Ca(OH)_2絮凝沉淀可以有效地去除垃圾渗滤液生化出水中的大分子有机物及Ca~(2+)、Mg~(2+)离子.当废水絮凝沉淀出水的电导率最低时,废水中的Ca~(2+)和Mg~(2+)离子浓度降到最低,同时也去除了较大比例的COD.对电导率最低条件下的Ca(OH)_2絮凝沉淀出水再经O_3处理后,废水中的Ca~(2+)和Mg~(2+)离子浓度和COD进一步降低,其反渗透膜通量比MBR出水的通量增高25%—35%,膜污染明显减轻,可延长膜清洗周期.臭氧氧化Ca(OH)_2絮凝沉淀出水涉及到臭氧分子直接氧化和氢氧根催化臭氧氧化两种机理,但前者起主导作用.臭氧氧化处理进一步降低了废水中的COD和Ca~(2+)、Mg~(2+)离子浓度,是提高反渗透膜通量的主要原因.     

印染废水生化出水高锰酸钾强化混凝深度处理溶解性有机物的去除特性

采用高锰酸钾预氧化,强化某印染废水生化出水铁盐混凝深度处理溶解性有机物(DOM),考察了高锰酸钾强化混凝对印染废水生化出水中DOM的去除特性并为优化混凝深度处理工艺提供理论参考.在最优投加条件下,高锰酸钾强化混凝处理提高了DOM色度的去除效果,以美国染料生产协会色度值(ADMI7.6)表征时为84%,出水ADMI7.6值较单独混凝处理降低了43%.但以溶解性有机碳(DOC)表征时去除率基本保持不变,为55%.通过XAD-8/XAD-4吸附树脂分离技术和分子量分布分析发现,高锰酸钾强化混凝处理通过有效去除疏水性和弱疏水性DOM色度降低了出水的色度.同时,出水中亲水性和小分子DOM(MW<1 kDa)较单独混凝处理分别增加了34%和15%,导致了DOM去除率以DOC表征时无显著改善.采用三维荧光光谱技术定性分析表明,引起色度的可见类富里酸和类腐殖酸物质被进一步去除使出水色度降低,此时出水中增多的小分子亲水性DOM主要为类蛋白质和富里酸物质.因此,高锰酸钾强化混凝处理过程仍需与其它能去除亲水性、小分子量DOM(MW<1 kDa)的处理工艺结合,以提高总体去除效率.     

活性炭吸附对印染废水生化出水中不同种类有机物的去除效果

染料废水是含有一定量有毒物质的有机废水,具有高COD和高色度.传统的生化方法能够去除纺织印染废水中的大部分有机物,然而出水仍有相当大的色度,因此后续处理是必要的.活性炭是使用最广泛和最有效的吸附剂,能很好地去除色度.本文以印染废水生化出水中的溶解性有机物为研究对象,     

电化学氧化垃圾渗滤液生化出水过程中溶解性有机物形态及可生化性

以垃圾渗滤液生化出水为研究对象,利用Ti/RuO_2阳极和Cu-Zn阴极进行电化学氧化去除溶解性有机物机理研究.应用三维荧光光谱对垃圾渗滤液生化出水溶解性有机物组成、结构变化和官能团变化进行分析,并对反应过程中垃圾渗滤液生化出水可生化性变化进行研究.结果表明,垃圾渗滤液生化出水中溶解性有机物主要由类富里酸类物质、类胡敏酸类物质和可溶性微生物降解产物为主,类色氨酸类物质和类酪氨酸类物质含量较低;反应过程中溶解性有机物的腐殖化程度降低,芳香性减弱,苯环上连接的极性基团率先被氧化去除;Ti/RuO_2-Cu/Zn电化学氧化体系降解垃圾渗滤液生化出水有机物,主要依赖生成次氯酸的间接氧化作用.电化学氧化过程中垃圾渗滤液生化出水可生化性增强.     

还原铁法处理印染废水生化出水及原理

采用还原铁粉处理印染废水生化出水,以ADMI7.6作为主要测试指标,考察铁粉投加量、反应时间以及进水pH对出水水质的影响,并研究在此过程中铁粉还原作用和混凝絮凝作用对整体效果的贡献比.结果表明,条件1:铁粉投加量=1.0 g.L-1,反应时间150 min,进水pH 2;条件2:铁粉投加量1.0 g.L-1,反应时间150 min,进水pH 3.条件1时,ADMI7.6去除率达到80%,但铁泥量大,酸碱消耗大,在此反应条件下,铁粉还原去除40%,混凝絮凝去除60%;条件2时,ADMI7.6去除率达到50%左右,产铁泥量小,经济合理;在此反应条件下,铁粉还原去除55%—63%左右,混凝絮凝去除37%—45%左右.经XAD8/XAD4树脂联用,分析疏水酸、非酸疏水物质、弱疏水物质及亲水物质4类有机物的去除情况表明,条件1时,能够高效去除非酸疏水物质,去除率为95%,对于疏水酸以及弱疏水物质也有一定的去除效果;条件2时,对4类有机物去除均有一定作用,但对于非酸疏水物质以及疏水酸的去除效果要略差于条件1.     

ZnO-MgO/Al2O3吸附-臭氧催化氧化处理难降解有机废水

以活性氧化铝为载体,采用浸渍法制备催化剂,对甲基橙及草酸模拟废水进行处理.在中性条件下,臭氧催化氧化比单独臭氧氧化能提前30 min使得甲基橙溶液褪色,反应105 min时,臭氧催化氧化对TOC的去除率高达96.53%,比单独使用臭氧氧化对甲基橙TOC去除率提高了47.19%,在处理草酸废水时臭氧催化氧化对TOC去除率高达80.59%,比单独使用臭氧氧化对草酸TOC去除率提高了59.14%.在处理甲基橙及草酸的小试实验中催化剂对有机污染物的吸附作用起到了加快反应进行的作用.在对垃圾渗滤液超滤出水时,O₃与COD质量比为1:1时,臭氧催化氧化对COD去除率为49.09%,比单独使用臭氧氧化提高36.37%,臭氧催化氧化对TOC的去除率是单独使用臭氧氧化的2.54倍,在处理垃圾渗滤液纳滤浓水时,臭氧催化氧化对COD去除率高达88.72%,比单独使用臭氧氧化提高37.60%,并且臭氧催化氧化对TOC的去除率是单独臭氧氧化的1.6倍.臭氧催化氧化反应过程中产生的羟基自由基对有机物更快的反应速率.     

Fenton试剂预处理提高钻井废水可生化性

采用Fenton试剂预处理钻井废水,研究了Fenton反应中各影响因子对废水COD去除率、 BOD5/COD值的影响并分析其作用机制,确定了最佳条件,即初始pH为4.0, H2O2/Fe2 (摩尔浓度比, c∶c)＝20, H2O2/COD (质量浓度比, w∶w)＝1,反应时间为2 h.在该条件下,废水的COD去除率约为40%, BOD5/COD值从0.002～0.003提高至0.15～0.2,可生化性得到很大提高,为后续生物处理创造了条件.紫外-可见吸收光谱分析表明,可生化性的改善主要是由于有机物的分子结构发生了变化.     

臭氧深度处理垃圾焚烧厂沥滤液时溶解性有机质（DOM）特性分析

采用荧光光谱、红外光谱和紫外-可见光谱技术分析了臭氧氧化深度处理沥滤液生化处理水过程中废水中DOM组成及结构变化.同步荧光光谱显示,反应过程中340—370 nm处的特征峰强度明显下降,小于270 nm的短波长范围内荧光强度有一个从高到低再升高的变化过程.三维荧光光谱表明,沥滤液生化处理水中含有两个类富里酸荧光峰（UV-FA：Ex/Em=250—255/410—450 nm;Vis-FA：Ex/Em=315—320/400—405 nm）,反应过程中荧光峰强度不断降低,其中UV-FA荧光峰的发射波长存在明显的蓝移现象,最大蓝移量40 nm.红外光谱表明,沥滤液生化处理水中含有多种芳香性特征峰,臭氧氧化过程中峰强度逐渐降低,部分特征峰消失,并有过氧化合物的CO伸缩振动峰生成.沥滤液生化处理水经臭氧氧化深度处理60 min后,其SUVA254值由3.01 L.mg-.1m-1降低到1.16 L.mg-.1m-1,A3/A4值由4.06上升到8.43.综合分析表明,臭氧氧化能够有效将沥滤液生化处理水中结构复杂的大分子芳香族化合物降解为芳构化程度较低、分子量较小的有机物.     

Removal of organic matter and disinfection by-products precursors in a hybrid process combining ozonation with ceramic membrane ultrafiltration

The performance of an integrated process including coagulation, ozonation, ceramic ultrafiltration (UF) and biologic activated carbon (BAC) filtration was investigated for the removal of organic matter and disinfection by-products (DBPs) precursors from micro-polluted surface water. A pilot scale plant with the capacity of 120 m³ per day was set up and operated for the treatment of drinking water. Ceramic membranes were used with the filtration area of 50 m² and a pore size of 60 nm. Dissolved organic matter was divided into five fractions including hydrophobic acid (HoA), base (HoB) and neutral (HoN), weakly hydrophobic acid (WHoA) and hydrophilic matter (HiM) by DAX-8 and XAD-4 resins. The experiment results showed that the removal of organic matter was significantly improved with ozonation in advance. In sum, the integrated process removed 73% of dissolved organic carbon (DOC), 87% of UV₂₅₄, 77% of trihalomethane (THMs) precursors, 76% of haloacetic acid (HAAs) precursors, 83%of trichloracetic aldehyde (CH) precursor, 77% of dichloroacetonitrile (DCAN) precursor, 51% of trichloroacetonitrile (TCAN) precursor, 96% of 1,1,1-trichloroacetone (TCP) precursor and 63% of trichloronitromethane (TCNM) precursor. Hydrophobic organic matter was converted into hydrophilic organic matter during ozonation/UF, while the organic matter with molecular weight of 1000–3000 Da was remarkably decreased and converted into lower molecular weight organic matter ranged from 200–500 Da. DOC had a close linear relationship with the formation potential of DBPs.     

Using respirometer in biodegradation phenomenon of natural organic matters

This study conducted in monitoring respirometer oxygen consumption of aerobic microorganism during biodegradation processes of ozonated organic matters, which can estimate both biodegraded efficiency and coefficient of natural organic matters (NOMs) in water source. It can be proposed that different ozone dosage might change biodegradation characteristics of organic matters. The result reveals that higher ozone dosage may cause higher biomass yield coefficient of microorganism, and cultured microorganism may easily utilize biodegradation organic matters (BOMs) produced by ozonation, finally increasing overall removal efficiency. Therefore, using respirometer to evaluate the production of BOMs by ozonation before the biological treatment is effective for controling ozone dosage and enhancement of NOMs removal by biological processes.     

Do microbial processes regulate the stability of a coral atoll's enclosed pelagic ecosystem?

Complex marine ecosystems contain multiple feedback cycles that can cause unexpected responses to perturbations. To better predict these responses, complicated models are increasingly being developed to enable the study of feedback cycles. However, the sparseness of ecological data often limits the direct empirical parameterization of all model parameters. Here we use a Bayesian inverse analysis approach to synthesize empirical data and ecological theory derived from published studies of a coral atoll's enclosed pelagic ecosystem (Takapoto Atoll, French Polynesia). We then use the estimates of flux magnitudes to parameterize probabilistic compartment models with two forms of heterotrophic consumption: (1) “bottom-up” donor-controlled heterotrophic consumption and (2) “top-down” mass-action heterotrophic consumption. We explore how the flux magnitudes affect the ecosystem's stability properties of resilience, reactivity, and resistance under both assumptions for heterotrophic consumption. The models suggest that the microbial uptake of dissolved organic carbon (DOC) regulates the long term rate of return to steady state following a temporary or pulse perturbation (resilience), and the cycling of carbon between abiotic pools and heterotrophic compartments regulates the short-term response (reactivity). In the bottom-up process model, the sensitivity of steady state masses following a sustained or press perturbation (resistance) is highest for the DOC pool following a sustained change to the microbial uptake rate of DOC. Further, a change in the microbial uptake of DOC propagates through the ecosystem and affects the steady state values of zooplankton. The analysis suggests that the food web is highly dependent on the recycling between the abiotic and biotic carbon pools, particularly as mediated by the microbial consumption of DOC, and this recycling determines how the ecosystem responds to perturbations.     

Molecular weight fractionation of dissolved organic matter in coastal seawater by ultrafiltration

Fractionation of molecular weight of dissolved organic matter (DOM) in coastal seawater of Tokyo Bay (Japan) was performed by ultrafiltration. Ultrafiltration membranes Diaflo UM-05, UM-10 and XM-100 were used for DOM fractionation, and dissolved organic carbon (DOC) was determined for ultrafiltrates of each membrane. In surface water of Station 1, near the center of Tokyo Bay, low-molecular weight DOM (molecular weight less than 500) which passed through a Diaflo UM-05 membrane was 0.3 to 2.6 mgC/l (24 to 42% of the total DOC) during August, 1971 to September, 1972. The macromolecular DOM (molecular weight greater than 100,000) retained on an XM-100 membrane, ranged from 0.1 to 1.0 mgC/l. These fractions accounted for 8 to 23% of the total DOC. The precision of the method was within ± 0.1 mgC/l, and therefore may be employed for coastal seawater of high DOC content.     

岩溶山区不同土地利用方式对土壤活性有机碳动态的影响

对贵州茂兰自然保护区内三种典型土地利用方式(林地、草地和耕地)下土壤活性有机碳组分(土壤溶解有机碳和土壤微生物量碳)的月变化及其对环境因子的响应进行了研究,结果表明在不同的土地利用方式下上覆植被类型不同,其凋落物数量、质量及分解行为不同,有机质的输入量及质量也不相同,从而形成不同的土壤溶解有机碳含量差异,土壤有机碳的大小也存在较大差别。研究结果显示:从全年平均值来看,林地土壤溶解有机碳分别比草地和耕地高25%、48%;从3月到8月,三者均随气温的上升呈增加的趋势,林地和耕地在8月均达到最大值,而草地则在10月达到最大值;林地和草地土壤微生物量碳分别高于耕地81%和45%,林地和草地在10月达到最大值。不同的土地利用方式导致土壤活性有机碳的差异较大,这说明岩溶生态系统中土地利用方式对土壤碳库的大小有较大影响。不同土地利用方式下土壤活性有机碳对环境因子的响应也各不相同,这表明土壤活性碳受众多因素的制约而呈现出一种动态平衡关系,进一步的机理仍需要进行深入研究。     

给水深度处理中臭氧副产物的产生及控制

就给水深度处理中臭氧副产物的产生及其化学过程、控制臭氧副产物生成的技术措施等问题进行了探讨。采用臭氧深度处理时,会产生以甲醛为代表的有机副产物,以溴酸根为代表的无机副产物。副产物的形成与溴离子浓度、水中有机物种类和浓度、pH值、臭氧投加量、温度和碱度等因素有关。在应用臭氧进行深度处理时,应根据不同条件,采取适宜的措施,以减少臭氧副产物的生成。     

Catalytic activity of cerium-doped Ru/AlO during ozonation of dimethyl phthalate

In this paper, factors influencing the mineralization of dimethyl phthalate (DMP) during catalytic ozonation with a cerium-doped Ru/Al₂O₃ catalyst were studied. The catalytic contribution was calculated through the results of a comparison experiment. It showed that doping cerium significantly enhanced catalytic activity. The total organic carbon (TOC) removal over the doped catalyst at 100 min reached 75.1%, 61.3% using Ru/Al₂O₃ catalyst and only 14.0% using ozone alone. Catalytic activity reached the maximum when 0.2% of ruthenium and 1.0% of cerium were simultaneously loaded onto Al₂O₃ support. Results of experiments on oxidation by ozone alone, adsorption of the catalyst, Ce ion’s and heterogeneous catalytic ozonation confirmed that the contribution of heterogeneous catalytic ozonation was about 50%, which showed the obvious effect of Ru–Ce/Al₂O₃ on catalytic activity.     

河流有机质生物地球化学研究进展

探讨了近年来河流中有机质的生物地球化学研究状况。大多数河流有机质的来源主要是外源即流域侵蚀而来的,经过河流的新陈代谢过程,把河流中的悬浮物分解为不同类型的有机质。在有机质分解过程中由于外部条件的差异,形成粒径大小不同的颗粒物和溶解有机质、无机质等。河流水体中的溶解有机碳(DOC)在全球不同纬度、不同区域,其含量差异较大,但目前对其生物地球化学控制的量级缺乏足够的理解和认识。另外碳氮同位素及其比值在当前的河流有机质生物地球化学研究中仍起着非常重要的示踪作用。     

Effects of rising temperature on pelagic biogeochemistry in mesocosm systems: a comparative analysis of the AQUASHIFT Kiel experiments

A comparative analysis of data, obtained during four indoor-mesocosm experiments with natural spring plankton communities from the Baltic Sea, was conducted to investigate whether biogeochemical cycling is affected by an increase in water temperature of up to 6?°C above present-day conditions. In all experiments, warming stimulated in particular heterotrophic bacterial processes and had an accelerating effect on the temporal development of phytoplankton blooms. This was also mirrored in the build-up and partitioning of organic matter between particulate and dissolved phases. Thus, warming increased both the magnitude and rate of dissolved organic carbon (DOC) build-up, whereas the accumulation of particulate organic carbon (POC) and phosphorus (POP) decreased with rising temperature. In concert, the observed temperature-mediated changes in biogeochemical components suggest strong shifts in the functioning of marine pelagic food webs and the ocean’s biological carbon pump, hence providing potential feedback mechanisms to Earth’s climate system.     

Reassessment of the Ocean-To-Atmosphere Flux of Carbon Monoxide

Carbon monoxide (CO) in the surface sea waters is produced predominantly by photochemical processes, oxidized by micro-organisms and outgassed to the atmosphere. to assess carbon monoxide flux from the oceans to the atmosphere, the photochemical production and microbial oxidation of carbon monoxide in the oceanic mixed-layer was investigated during several oeanographic cruises and in the laboratory. the photoproduction rate of carbon monoxide was found to be well correlated to the concentration of dissolved organic carbon (DOC) in coastal and open ocean surface waters. Taking a global average carbon monoxide production rate of 10 ± 2 nmole litre^-1 (mg DOC hr)^-1 in the surface open ocean water, and 25 ± 7 nmole litre^-1 (mg DOC hr)^-1 in coastal sea water, at cloud-free summer solar noon, the photochemical production of carbon monoxide in the global oceans is estimated to be at a rate of 1200 ± 200 Tg CO y^-1. the microbial carbon monoxide turnover time in the mixed-layer was observed to range from hours in a coastal estuary to 16 days in the Pacific along 1057deg; W in dark incubations. Natural sunlight can largely inhibit the microbial consumption of carbon monoxide in surface water. On a global scale, microbial consumption is responsible for the loss of less than 10% of photochemical produced carbon monoxide in the surface ocean. Field measurements have shown that the net transport of carbon monoxide from the euphotic zone to the underlying deeper ocean water is limited and that the overall life time in surface sea waters is less than 3-4 hours. When combined, these field measurements with the photoproduction and microbial consumption rates obtained, we estimate the oceanic flux to the atmosphere is about 1000 ± 200 Tg CO y^-1, which represents the largest single source of atmospheric carbon monoxide.