絮体性质对纳滤膜污染的影响

混凝过程产生的絮体会对后续膜过滤性能产生一定的影响。实验中利用激光粒度仪研究2种混凝剂(AlCl3和PAC)在不同投加量下的絮体性质,混凝出水(不经过沉淀)直接进入纳滤膜(NF270)装置进行过滤实验。研究表明,投加量低(<0.20 mmol/L)的情况下,混凝出水反而使纳滤通量衰减发生恶化,随着投加量的增加,纳滤膜通量衰减得到有效的减缓。直接过滤腐殖酸(HA)的膜通量衰减(J/J0)为0.65,投加量为0.50 mmol/L时,AlCl3和PAC 2种混凝剂产生的通量衰减(J/J0)分别为0.78和0.75。滤饼层阻力受到絮体尺寸的影响较大,絮体尺寸越大,形成的滤饼层透水性更好。通过污染模型分析,混凝出水的纳滤膜污染机理主要是滤饼层阻力。     

Relating dissolved organic matter fluorescence and functional properties

The fluorescence excitation–emission matrix properties of 25 dissolved organic matter samples from three rivers and one lake are analysed. All sites are sampled in duplicate, and the 25 samples include ten taken from the lake site, and nine from one of the rivers, to cover variations in dissolved organic matter composition due to season and river flow. Fluorescence properties are compared to the functional properties of the dissolved organic matter; the functional assays provide quantitative information on photochemical fading, buffering capacity, copper binding, benzo[a]pyrene binding, hydrophilicity and adsorption to alumina. Optical (absorbance and fluorescence) characterization of the dissolved organic matter samples demonstrates that (1) peak C (excitation 300–350 nm; emission 400–460 nm) fluorescence emission wavelength; (2) the ratio of peak T (excitation 220–235 nm; emission 330–370 nm) to peak C fluorescence intensity; and (3) the peak C fluorescence intensity: absorbance at 340 nm ratio have strong correlations with many of the functional assays. Strongest correlations are with benzo[a]pyrene binding, alumina adsorption, hydrophilicity and buffering capacity, and in many cases linear regression equations with a correlation coefficient >0.8 are obtained. These optical properties are independent of freshwater dissolved organic carbon concentration (for concentrations <10 mg L⁻¹) and therefore hold the potential for laboratory, field and on-line monitoring and prediction of organic matter functional properties.     

Relating dissolved organic matter fluorescence and functional properties

The fluorescence excitation–emission matrix properties of 25 dissolved organic matter samples from three rivers and one lake are analysed. All sites are sampled in duplicate, and the 25 samples include ten taken from the lake site, and nine from one of the rivers, to cover variations in dissolved organic matter composition due to season and river flow. Fluorescence properties are compared to the functional properties of the dissolved organic matter; the functional assays provide quantitative information on photochemical fading, buffering capacity, copper binding, benzo[a]pyrene binding, hydrophilicity and adsorption to alumina. Optical (absorbance and fluorescence) characterization of the dissolved organic matter samples demonstrates that (1) peak C (excitation 300–350 nm; emission 400–460 nm) fluorescence emission wavelength; (2) the ratio of peak T (excitation 220–235 nm; emission 330–370 nm) to peak C fluorescence intensity; and (3) the peak C fluorescence intensity: absorbance at 340 nm ratio have strong correlations with many of the functional assays. Strongest correlations are with benzo[a]pyrene binding, alumina adsorption, hydrophilicity and buffering capacity, and in many cases linear regression equations with a correlation coefficient >0.8 are obtained. These optical properties are independent of freshwater dissolved organic carbon concentration (for concentrations <10 mg L⁻¹) and therefore hold the potential for laboratory, field and on-line monitoring and prediction of organic matter functional properties.     

Oxidative biodegradation of dissolved organic matter during composting

Dissolved organic matter (DOM) plays an important role in the microbial degradation of compost since it represents the most active organic fraction, both biologically and chemically. The detailed evaluation of the changes in the chemical and biochemical characteristics of DOM induced by oxidative biodegradation, presented in this work highlights the mechanisms involved in the degradation of soluble organic matter during composting. In fact, the results show that during the initial stages of composting, DOM is highly degradable under aerobic conditions, particularly due to the predominance of labile, hydrophilic compounds such as carbohydrates, amino acids and proteins. As such compounds are degraded more resistant aromatic moieties accumulate in solution resulting in a reduction in the degradability of DOM with composting time. This decrease in degradability was found to be highly correlated with microbial oxygen demand, and could have important implications in the evaluation of the composting process.     

Cosorption study of organic pollutants and dissolved organic matter in a soil

In this study we have evaluated the effects of dissolved organic matter (DOM) on sorption of imidacloprid, 3,4-dichloroaniline (3,4-DCA) and 4-bromoaniline (4-BA) on a typical calcareous soil (Luvic Xerosol) from south-eastern Spain. Two different types of DOM were used, that is to say, dissolved natural organic matter extracts from a commercial peat (DNOM) and a high-purity tannic acid (TA) solution. The experiments were carried out in a 0.01 M CaCl2 aqueous medium at 25 degrees C. The results indicated that the presence of both DNOM and TA, over a concentration range of 15-100 mg L(-1), produced an increase in the amount of 3,4-DCA and 4-BA sorbed and a decrease in the amount of imidacloprid retained on the soil studied. A modified distribution coefficient, K(doc), has been proposed as a safer parameter for soil sorption predictions of organic pollutants and it could be of help to model the fate of these in the environment.     

Relationships between colored dissolved organic matter and dissolved organic carbon in different coastal gradients of the Baltic Sea

Due to high terrestrial runoff, the Baltic Sea is rich in dissolved organic carbon (DOC), the light-absorbing fraction of which is referred to as colored dissolved organic matter (CDOM). Inputs of DOC and CDOM are predicted to increase with climate change, affecting coastal ecosystems. We found that the relationships between DOC, CDOM, salinity, and Secchi depth all differed between the two coastal areas studied; the W Gulf of Bothnia with high terrestrial input and the NW Baltic Proper with relatively little terrestrial input. The CDOM:DOC ratio was higher in the Gulf of Bothnia, where CDOM had a greater influence on the Secchi depth, which is used as an indicator of eutrophication and hence important for Baltic Sea management. Based on the results of this study, we recommend regular CDOM measurements in monitoring programmes, to increase the value of concurrent Secchi depth measurements.     

pH和溶解性有机质对磺胺甲恶唑光降解的影响

为了考察pH和溶解性有机质(DOM)对磺胺甲恶唑(SMX)自然光降解的影响,采用光化学反应器对SMX降解过程进行模拟实验,并利用傅里叶变换红外光谱(FT-IR)和三维荧光光谱(3DEEM)对腐殖酸进行表征。结果表明：SMX光解过程符合准一级反应动力学方程,在中等酸性条件下反应速率明显高于中性或碱性条件;添加不同浓度的Pahokee泥炭腐殖酸(PPHA)和Sigma-Aldrich腐殖酸(SigHA)时,均对SMX的光降解产生了不同程度的抑制作用;FT-IR检测发现,PPHA与SigHA均含有含氧官能团,具有一定的还原能力,3DEEM显示PPHA具有荧光特性,可能和SMX结合生成配合物。pH影响SMX的光解与物质本身的酸离解常数有关,对光子的竞争、淬灭作用和掩蔽效应可能是PPHA和SigHA对SMX光降解抑制作用的主要原因。     

Effect of organic fertilizers derived dissolved organic matter on pesticide sorption and leaching

Incorporation of organic fertilizers/amendments has been, and continues to be, a popular strategy for golf course turfgrass management. Dissolved organic matter (DOM) derived from these organic materials may, however, facilitate organic chemical movement through soils. A batch equilibrium technique was used to evaluate the effects of organic fertilizer-derived DOM on sorption of three organic chemicals (2,4-D, naphthalene and chlorpyrifos) in USGA (United States Golf Association) sand, a mixed soil (70% USGA sand and 30% native soil) and a silt loam soil (Typic Fragiochrept). DOM was extracted from two commercial organic fertilizers. Column leaching experiments were also performed using USGA sand. Sorption experiments showed that sorption capacity was significantly reduced with increasing DOM concentration in solution for all three chemicals. Column experimental results were consistent with batch equilibrium data. These results suggest that organic fertilizer-derived DOM might lead to enhanced transport of applied chemicals in turf soils.     

Chemical characteristics of chromophoric dissolved organic matter in rainwater

Proton nuclear magnetic resonance (¹H-NMR), UV absorbance and excitation-emission matrix (EEM) fluorescence spectroscopy were used to define the chemical characteristics of chromophoric dissolved organic matter (CDOM) in whole and C₁₈ extracted rainwater. The average total recovery of fluorescence determined from the sum of extract and filtrate fractions relative to the whole was 86% suggesting that 14% of fluorescent CDOM in rainwater is comprised of very hydrophobic material that cannot be eluted from the column. Half the fluorescence of rainwater was recovered in the filtrate fraction which is important because it suggests that 50% of the chromophoric material present in precipitation is relatively hydrophilic. The average spectral slope coefficient was smaller in extracted samples (16.3 ± 9.0 μm^?1) relative to whole samples (18.9 ± 2.8 μm^?1) suggesting that the extracted material contains larger molecular weight material. Approximately one-third of the total dissolved organic carbon (DOC) in rainwater exists in the extract fraction suggesting that a large percentage of the uncharacterized DOC in rainwater can be accounted for by these hydrophobic macromolecular species. The fluorescence of extracted samples is strongly correlated with total NMR integration and is most sensitive to aromatic protons suggesting that molecules in this region are the most important in controlling the optical properties of rainwater. The lower removal efficiency of CDOM in rainwater relative to surface waters or the water-soluble fraction of aerosols during solid phase extraction (SPE) suggests that rainwater contains significantly more hydrophilic chromophoric compounds which are compositionally different than found in these other aquatic matrices.     

Photochemical alteration of the molecular weight of dissolved organic matter

Molecular weight (MW) is a key control on the physical, chemical, and biological characteristics of dissolved organic mater (DOM). This study investigated the effect of photooxidation on the average MW of DOM by exposing DOM of diverse origins to simulated solar radiation at varying levels of dissolved oxygen and under different incident light wavelength regimes. During irradiation, high-molecular-weight fractions were destroyed and low-molecular-weight constituents were formed. The average MW decreased with irradiation time in all treatments in a manner that can be described by a quasi-exponential function, which suggests that solar radiation is incapable of completely mineralizing DOM even after prolonged exposure. Increasing the oxygen concentration accelerated the MW reduction while the removal of oxygen strongly suppressed this process. The fractional contributions from UV-B, UV-A, and visible radiations to full-spectrum photoinduced MW reduction varied considerably among the DOM samples examined, ranging from 19% to 60%, 17% to 36%, and 15% to 46%, respectively. The MW changes in time-series irradiations were inversely correlated with the ratio of the absorbance at 250 nm to that at 365 nm (i.e., the E₂/E₃ quotient). Photoinduced MW reduction was accompanied by a decrease of polydispersity, which is indicative of a reduced DOM heterogeneity.     

Environmental fate of amitrole: influence of dissolved organic matter

In this study the environmental fate of amitrole in terrestrial and aquatic model ecosystems was investigated. Under aerobic conditions mineralization of amitrole is the main degradation pathway. The experiments revealed that the leaching behaviour is low in the presence or the absence of dissolved organic matter (DOM) despite the high water solubility due to a strong binding of amitrole to soil constituents. Under anaerobic conditions the addition of DOM increases the transport of amitrole in soil columns. The tests with water/sediment model ecosystems showed that the mineralization of amitrole is lower in comparison to aerobic soil experiments. Up to 80.6% of the applied 14C-labelled amitrole transfer into the sediment and about 1/3 of this amount formed bound residues, which are not extractable.     

河道藻源胞内有机质光化学-生物降解机制

藻细胞破裂后会向水体释放大量的胞内有机质 (intracellular dissolved organic matter, I-DOM) 。I-DOM在河道中将经历复杂的光降解和生物降解过程,影响其在河道中的迁移转化和环境效应。为了探明光照和微生物对I-DOM的降解机制,开展了光降解、生物降解和光-生物降解实验。结果表明,I-DOM经7 d光降解和生物降解后,溶解性有机碳 (dissolved organic carbon, DOC) 的去除率分别为70%和81%;虽然光照1 d能去除38%的DOC,但后续生物降解 (光-生物降解) 与无光照生物降解对DOC的去除效率一致。进一步的研究表明,生物降解过程中的呼吸商 (respiratory quotient, RQ) 低于光-生物降解过程,说明相比于生物降解过程,光-生物降解过程中经光照后生物呼吸时所利用I-DOM的性质发生了改变,进而影响了生物呼吸时O₂的消耗和CO₂的产生。生物降解过程中微生物主要利用原始的I-DOM分子;而在光-生物降解过程中,生物降解过程的微生物主要利用经光降解转化后的I-DOM分子。光-生物降解过程中,光照消耗了I-DOM中可生物降解的脂质、蛋白质和木质素类组分,导致I-DOM的生物降解效率降低;同时,光照将I-DOM中的大分子物质分解成高O/C的小分子物质,使微生物代谢需要的O₂减少,小分子物质则更易被生物降解矿化生成CO₂,导致RQ升高。本研究结果可为河道水质调控提供参考。     

硅藻土预涂动态膜对海水中有机物的截留及膜污染特性

膜有机污染问题严重制约超滤在海水淡化预处理领域的推广应用。通过硅藻土预涂覆强化超滤膜对海水中有机物的截留,利用三维荧光光谱考察了硅藻土预涂动态膜对海水中典型有机污染物的净化作用,并对比分析了直接超滤和硅藻土预涂动态膜过滤海水过程中膜通量变化及污染特性。结果表明：硅藻土预涂动态膜对海水中DOC和UV254的去除率分别为65.25%和92.68%,较直接超滤分别提高了26.26%和31.10%。通过硅藻土预涂覆能够强化超滤膜对海水中蛋白质类有机物的截留,硅藻土预涂覆后超滤膜纯水通量略有降低。硅藻土在超滤膜表面形成的滤饼层结构避免了膜与有机污染物直接接触,在海水过滤过程中预涂动态膜的膜通量均高于直接超滤。硅藻土预涂动态膜更易清洗,膜通量更易恢复,能够有效减缓超滤膜的不可逆污染。     

Removal of dissolved organic matter in municipal effluent with ozonation, slow sand filtration and nanofiltration as high quality pre-treatment option for artificial groundwater recharge

In the paper the combination process of ozonation, slow sand filtration (SSF) and nanofiltration (NF) was investigated with respect to dissolved organic matter (DOM) removal as high quality pre-treatment option for artificial groundwater recharge. With the help of ozonation leading to breakdown of the large organic molecules, SSF preferentially removes soluble microbial by-product-like substances and DOM with molecular weight (MW) less than 1.0 kDa. NF, however, removes aromatic, humic acid-like and fulvic acid-like substances efficiently and specially removes DOM with MW above 1.0 kDa. The residual DOM of the membrane permeate is dominated by small organics with MW 500 Da, which can be further reduced by the aquifer treatment, despite of the very low concentration. Consequently, the O₃/SSF/NF system offers a complementary process in DOM removal. Dissolved organic carbon (DOC) and trihalomethane formation potential (THMFP) can be reduced from 6.5 ± 1.1 to 0.7 ± 0.3 mg L⁻¹ and from 267 ± 24 to 52 ± 6 μg L⁻¹, respectively. The very low DOC concentration of 0.6 ± 0.2 mg L⁻¹ and THMFP of 44 ± 4 μg L⁻¹ can be reached after the aquifer treatment.     

水体溶解性有机物的化学分级表征：原理与方法

综述了水体溶解性有机物（DOM）的化学分级表征法即树脂吸附分级法（RA）的研究与进展，同时基于该方法存在的一些问题结合我国典型水质体系，从树脂的选择、净化、分级的定义、水样过柱流速、水样树脂体积比的确定等方面进行了研究探讨，给出了完整的实验参数和操作方法。     

Column- and catchment-scale transport of cadmium: effect of dissolved organic matter

In the Ellen catchment on the Pinjarra Plain, NE of Perth in Western Australia, cadmium from fertilisers is starting to leach from soils. About 70% of surface soils in the Ellen catchment are sandy and often on top of a shallow ephemeral water table. Adsorption of Cd in the sandy soils of the Ellen catchment was studied by batch adsorption and by leaching small columns of soil. Adsorption of Cd increases linearly with increasing soil organic matter content and exponentially with increasing pH. Cadmium is significantly mobilised in the sandy soils by dissolved organic matter.The capacity of most of the sandy soils in the Ellen catchment to adsorb phosphate from fertiliser has been saturated. Resulting concentrations in Ellen Brook average 500 μg L⁻¹ P. Cadmium is adsorbed more strongly in the sandy soils than phosphate and is just starting to leach into Ellen Brook. From a comparison of Cd/P ratios in water, soils and fertiliser, cadmium concentrations in Ellen Brook are estimated to be at 10–30% of their maximum for complete breakthrough from soils. Present concentrations of Cd in Ellen Brook average 0.1 μg L⁻¹ and are estimated to approach the maximum for complete breakthrough in 100 yr. Maximum Cd concentrations in Ellen Brook could range from 0.6 to 2 μg L⁻¹, depending on rates of input with fertiliser and future increases in agricultural land use in the catchment.Breakthrough curves, resulting from leaching Cd through small columns of sandy soil, indicate that adsorption significantly increases the effective hydrodynamic dispersion of Cd. Longitudinal dispersivities, measured at pore-water velocities of 0.7–14 m day⁻¹, were 5 cm for Cd and 0.1–0.2 cm for chloride. The much greater dispersion of Cd in the sandy soils than of chloride is shown not to be caused by non-equilibrium adsorption.     

水体溶解性有机物的化学分级表征:原理与方法

综述了水体溶解性有机物(DOM)的化学分级表征法即树脂吸附分级法(RA)的研究与进展,同时基于该方法存在的一些问题结合我国典型水质体系,从树脂的选择、净化、分级的定义、水样过柱流速、水样树脂体积比的确定等方面进行了研究探讨,给出了完整的实验参数和操作方法.     

一体式光催化－膜分离三相流化床反应器膜污染特性

通过利用颗粒状 TiO2催化剂(平均粒径0.258/μm)对酸性红 B 模拟废水的催化降解实验,对一体式光催化氧化-膜分离三相流化床反应器的膜污染特性进行了研究.结果表明,TiO2是造成膜污染的主要污染物,且 TiO2浓度愈大,膜污染愈严重;本实验体系TiO2的适宜浓度为 2g/L.反应区曝气量在 3.6m3/h 时膜污染最小;膜组件底部曝气装置可大大减轻膜污染,且其曝气量以 0.6 m3/h 为宜.表面冲洗、气体反冲洗和碱洗均可有效地清除膜表面和膜孔内的污染物,使膜通量恢复至90%以上;"表面冲洗 碱洗"和"表面冲洗 碱洗 气体反冲"可进一步提高膜通量的恢复,但不十分明显.     

有机物性质对混凝-微滤-纳滤去除水中重金属的影响

为了探明有机物性质对混凝-微滤-纳滤去除水中重金属的影响,将腐殖酸和乙酸分别作为背景有机物,系统考察了组合工艺对镉(Cd)、铜(Cu)、镍(Ni)和锌(Zn)的去除效能及其膜通量变化过程,并通过物料衡算对4种重金属的去除行为进行了比较分析。结果表明,当原水中不含有机物时,Cu的截留率最高,达到97%以上,纳滤膜是去除其他3种重金属的主要步骤。随着原水中腐殖酸含量的增大,混凝-微滤阶段对重金属的截留能力显著增强,膜通量衰减速度加快。相反地,乙酸的存在对于组合工艺处理效能具有明显的负面效应。此时,重金属既不能被铝盐絮体有效吸附,也不能通过静电作用截留在NF膜表面。4种重金属在滤液和浓水中的回收率Rrec都超过了80%,膜通量的变化与处理无机重金属溶液时相近。     

生物炭中溶解性有机质光催化降解罗丹明B

为了区分生物炭对有机物降解的因素,通过控制光照条件、气体氛围、 · OH淬灭等实验对生物炭降解有机染料罗丹明B(rhodamine-B, RhB)的过程进行了考察;采用元素分析、电子顺磁共振、总有机碳分析仪对生物炭颗粒、持久性自由基(environmental persistent free radicals, EPFRs)及溶解性有机质(dissolved organic matter, DOM)进行了表征测定;研究了不同实验条件下,不同热解温度制备的水稻秸秆生物炭对RhB的吸附和降解效果。结果表明：在200 ℃和500 ℃下所制备的生物炭中检测到明显的EPFRs信号,但其强度与RhB的降解程度不匹配;200 ℃制备的生物炭中DOM含量显著高于其他温度条件下制备的生物炭;在光降解实验中,紫外光能明显促进200 ℃生物炭对RhB降解;气体氛围实验进一步证明紫外光可诱导DOM与生物炭颗粒中EPFRs相互作用形成大量的活性氧组分(主要为$ {\rm{O}}_2^{ \cdot - }$),进而促进了其对RhB的降解。