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.     

NMR spectroscopy of dissolved organic matter: a review

Environmental Chemistry Letters - The presence of liquid water makes our planet habitable. Water in soils, sediments, lakes, rivers and the ocean forms the largest habitat for life on Earth. During...     

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.     

Characterization and variation of dissolved organic matter in composting: a critical review

● Effect of composting approaches on dissolved organic matter (DOM). ● Effect of composting conditions on the properties of DOM. ● Character indexes of DOM varied in composting. ● The size, hydrophobicity, humification, and electron transfer capacity increased. ● The hydrophilicity, protein-like materials, and aliphatic components reduced. As the most motive organic fraction in composting, dissolved organic matter (DOM) can contribute to the transfer and dispersal of pollutants and facilitate the global carbon cycle in aquatic ecosystems. However, it is still unclear how composting approaches and conditions influence the properties of compost-derived DOM. Further details on the shift of DOM character indexes are required. In this study, the change in properties of compost-derived DOM at different composting approaches and the effect of composting conditions on the DOM characteristics are summarized. Thereafter, the change in DOM character indexes’ in composting was comprehensively reviewed. Along with composting, the elements and spectral properties (chromophoric DOM (CDOM) and fluorescent DOM (FDOM)) were altered, size and hydrophobicity increased, and aromatic-C and electron transfer capacity were promoted. Finally, some prospects to improve this study were put forward. This paper should facilitate the people who have an interest in tracing the fate of DOM in composting.     

Release of dissolved organic matter from natural populations of marine phytoplankton

A new method is presented for measuring the rate of release of dissolved organic matter (DOM) produced by natural populations of marine phytoplankton. The method has been field-tested using natural populations of estuarine, coastal, and oceanic phytoplankton. Problems associated with the necessity for long incubation times, high initial activity of the inorganic ¹⁴C added to the sample, and self-absorption are overcome. Improved sensitivity is obtained by utilizing a large portion of the sample filtrate, Results from sampling at different times of day and for different lengths of incubation suggest that these problems should be reexamined in terms of both the percent and rate of relase of DOM from natural populations of phytoplankton. The rate of release of DOM from natural populations of marine phytoplankton decreases seaward. Phytoplankton in Georgia (USA) estuaries release <1 to 40 mg C m^-3 day^-1, in southeastern USA coastal waters from 0 to 19 mg C m^-3 day^-1, and in the westernmost Sargasso Sea from 0 to 2 mg C m^-3 day^-1. The percent of photoassimilated carbon released as DOM increases seaward. The percents are less than 7% in the Georgia estuaries, generally less than 13% in southeastern USA surface coastal waters, generally less than 21% for these coastal waters below the surface, and less than 44% for the westernmost Sargasso Sea. The results of this study and of other studies suggest that the measurement of primary productivity in estuarine and nearshore coastal waters is not seriously in error because of the absence of measurements on the rate of release of DOM from such phytoplankton. However, the estimation of primary-productivity values for oceanic waters is underestimated in some cases by about 50%.Contribution No. 595 from the Department of Oceanography, University of Washington, Seattle, Washington, USA and Contribution No. 224 from the University of Georgia Marine Institute, Sapelo Island, Georgia, USA.Extracted in part from a dissertation submitted to the Graduate Faculty of the University of Georgia in partial fulfillment of the requirements for the degree of Doctor of Philosophy.     

Soil organic matter dynamics in Portuguese natural and sown rainfed grasslands

Soil organic matter (SOM) is a particularly important parameter in soil management, especially in mineral soils in Mediterranean and semi-arid countries where its concentration is low. In these conditions, increasing SOM concentration has several agronomic and environmental benefits, ranging from increase in water holding capacity to soil protection and carbon sequestration. We develop a model to express the short-term trend of SOM increase in grasslands as the balance between input and mineralization. This model is calibrated using five years of soil analyses from eight locations. In each location there were either two or three plots with the different grassland systems considered: sown biodiverse permanent pastures rich in legumes (SBPPRLs), fertilized natural grasslands (FNGs), and (un-improved) natural grasslands (NGs). SBPPRL are a new system consisting in the use of plant biodiversity to increase pasture productivity and resilience. So far, they exist mostly in Portugal.We use statistical calibration to adjust an asymptotic curve to the data and obtain the model parameters. Under the assumption of equal mineralization rates across grassland systems, we find that the expected steady-state long term SOM concentration in undisturbed SBPPRL is higher than in NG and FNG. Fertilization does not significantly increase SOM input, and so the trend in SOM is equal for NG and FNG. In 10 years, there is an average increase of 0.21 percentage points per year in SBPPRL. In turn, SOM increases in FNG and NG are 0.08 percentage points per year.     

Effects of a dynamic membrane formed with polyethylene glycol on the ultrafiltration of natural organic matter

The formation of a dynamic membrane (DM) was investigated using polyethylene glycol (PEG) (molecular weight of 35000 g/mol, concentration of 1 g/L). Two natural organic matters (NOM), Dongbok Lake NOM (DLNOM) and Suwannee River NOM (SRNOM) were used in the ultrafiltration experiments along with PEG. To evaluate the effects of the DM with PEG on ultrafiltration, various transport experiments were conducted, and the analyses of the NOM in the membrane feed and permeate were performed using high performance size exclusion chromatography, and the effective pore size distribution (effective PSD) and effective molecular weight cut off (effective MWCO) were determined. The advantages of DM formed with PEG can be summarized as follows: (1) PEG interferes with NOM transmission through the ultrafiltration membrane pores by increasing the retention coefficient of NOM in UF membranes, and (2) low removal of NOM by the DM is affected by external factors, such as pressure increases during UF membrane filtration, which decreases the effective PSD and effective MWCO of UF membranes. However, a disadvantage of the DM with PEG was severe flux decline; thus, one must be mindful of both the positive and negative influences of the DM when optimizing the UF performance of the membrane.     

Ingestion of natural particulate organic matter and subsequent assimilation,respiration and growth by tropical lagoon zooplankton

Rates of ingestion of natural particulate organic matter and subsequent assimilation and respiration by zooplankton at Enewetak Atoll lagoon (Marshall Islands) were measured using a flow-through system. Maximum daily ingestion rates of carbon and nitrogen, expressed as a percentage of the body content, were 79 and 37%, respectively, for the large copepod Undinula vulgaris; 112 and 65%, respectively, for a group of mixed small copepods; and 61 and 34%, respectively, for the pteropod Creseis acicula. Daily metabolic carbon losses, expressed as above, were 63% for U. vulgaris, 88% for the small copepods, and 50% for C. acicula. Assimilation efficiences of carbon and nitrogen ranged from about 86 to 91%. The above rates are generally higher than in previous reports for similar sized zooplankton in temperate waters, while the daily growth increments, expressed as a percentage of the body carbon content (4.8% for U. vulgaris, 8.6% for the small copepods, and 2.6% for C. acicula), are comparable. It appears that the high rates of ingestion and assimilation of organic matter are compensated by high metabolic losses. These results indicate that at least for carbon, tropical zooplankton may have low growth efficiencies ranging from 4 to 9%.     

Bactericidal properties of natural and synthetic sea water as influenced by addition of low amounts of organic matter

The influence of added organic nutrients on the bactericidal capacity of natural and synthetic sea water was investigated, with special reference to levels below the normal concentration of orgnnic matter in natural sea water. Resting cells of Escherichia coli, Staphylococcus aureus and Serratia marinorubra were used as test organisms. The inactivation of test bacteria in synthetic and filter-sterilized natural sea water could be increased by addition of ZoBell's 2216E-broth (containing peptone and yeast extract), peptone or glucose. This effect of the nutrients depended on chemical nature and concentration as well as on specific properties of the test strains. In regard to peptone, less than 10^-4 mg/ml must be added to induce bacterial kill exceeding that observed with unsupplemented controls. With raw sea water, no fundamentally different results were obtained; however, the influence of marine bacteria was clearly discernible. All findings support a previously offered hypothesis of nutrient-dependent antibacterial activity of sea water which is discussed in detail.     

Metal ion-induced enhanced oxidation of organic contaminants by ferrate: a review

Environmental Chemistry Letters - The global contamination of water resources by organic contaminants such as pharmaceuticals and pesticides is calling for advanced remediation techniques, yet...     

UV light induces Ag nanoparticle formation: roles of natural organic matter,iron, and oxygen

Nanoparticles occurring in the environment originate either from engineered, synthetically produced nanoparticles, or from naturally produced nanoparticles. The latter can be formed in natural media by light-induced reduction of metal ions in presence of natural organic matter, such as humic substances occurring widely in waters, soils and sediments. There is actually few knowledge on the effect of sunlight and of the nature of organic matter on nanoparticle formation. Therefore, we studied here the photoreduction of silver(I) ion to silver nanoparticles with and without ferrous ion under oxic and anoxic conditions, using humic and fulvic acids as proxies of natural organic matter. UV light-induced formation of silver nanoparticles was monitored up to 60 min by measuring surface plasmon resonance in air-saturated mixture and nitrogen-saturated mixture of silver(I) ion–organic matter. Results show that the surface plasmon resonance intensity was about 2.5 times higher in the nitrogen-purged solution mixture than the air-saturated solution. This finding suggests the oxygen-containing species had no major role in forming silver nanoparticles. Therefore, photo-driven formation of silver nanoparticles most likely involved photoactivation of silver(I) ion and natural organic matter complexes. We observed also that both iron(II) and iron(III) ions highly modified the surface plasmon resonance spectra of the particles with broader features. Results also reveal that in the presence of humic acid, the intensity of the surface plasmon resonance peak decreased by at least 50 %, while almost no change in the intensity was seen when fulvic acid was used. Overall, our findings demonstrate that the ligand–metal charge transfer process, affected by the nature of organic matter, i.e., humic acid versus fulvic acid, was influenced by redox iron species.     

Unlocked disinfection by-product formation potential upon exposure of swimming pool water to additional stimulants

• Swimming pool water was studied for DBPs upon exposure to additional stimulants. • DBP formation could be induced by residual chlorine and extended incubation. • Urine led to a massive formation of chloroform with additional stimulants. • Reactions between chlorine and anthropogenic organics were slow and long-lasting. • Urine control and air ventilation should be on the priority list for pool management. Anthropogenic organics are known to be responsible for the formation of harmful disinfection by-products (DBPs) in swimming pool water (SPW). The research explored an important scenario of SPW with no additional anthropogenic organic input. With stimulations by residual chlorine or additional chlorine and extended incubation, the formation of DBPs, especially chloroform, was significantly induced. Similar observations were found by investigating synthetic SPW made with sweat and urine. The presence of urine led to a massive formation of chloroform, as noted by an approximate 19-fold increase after 165-day incubation with a shock chlorine dose. The research suggests that consistent residual chlorine and long water retention as two typical features of SPW could unlock the DBP formation potential of anthropogenic organics. Thus, limiting the introduction of anthropogenic organics may not have an immediate effect on reducing DBP levels, because their reactions with chlorine can be slow and long-lasting. Pool management should prioritize on control of urine and improving air ventilation. This work is useful to deepen understandings about DBP formation in SPW and provide implications for pool management and prospective legislation.     

Effect of natural organic matter on arsenic release from soils and sediments into groundwater

Arsenic (As) contamination in groundwater has received significant attention recently. Natural and anthropogenic sources contribute to the worldwide occurrence of As contamination. As speciation is an important factor related to its toxic and mobile behavior. The release of As from soils and sediments into groundwater is governed by several geophysicochemical processes, of which, As sorption behavior is of principle significance. This review paper summarizes existing information regarding the effects of natural organic matter (NOM) on the fate and mobility of As species in the environment. NOM may enhance the release of As from soils and sediments into the soil solution, thereby facilitating As leaching into the groundwater. The main influencing mechanisms include competition for available adsorption sites, formation of aqueous complexes, and/or changes in the redox potential of site surfaces and As redox speciation. NOM may also serve as binding agents, thereby reducing As mobility. However, comparably little research has been performed on this aspect. Since most investigations have been done on purified minerals under laboratory conditions, further research involving various geological materials under natural environmental conditions is required. Development of proper geochemical conceptual models may provide means of predicting the role of NOM in arsenic leaching and/or immobilization.     

Transformation of some dissolved organic compounds by a natural heterotrophic population

Uptake of radioactively labeled glycolic acid, arginine, glutamic acid, and glycine by natural marine bacterial population was rapid and approached a maximum value which was over 90% of the total substrate. Uptake of glucose was rapid, but had a maximum uptake of less than 80%. All substrates except glycolic acid were assimilated to a similar degree (a maximum of more than 30% of the total given substrate). Glycolic acid had a maximum assimilation of less than 10%. The presence of glycolic acid resulted in no extracellular metabolites detectable on a gel permeation column. Between 5 and 10% of the other substrates were transformed and excreted within 72 h by the bacteria. These exudates were both nominally larger and smaller than the given substrates.NORDA publication number: JA 330:008:80     

垃圾填埋场渗滤液溶解性有机质特性及其去除技术综述

垃圾填埋场渗滤液所含物质种类繁多,理化特性复杂,且随填埋时间等条件而变化.本文综合分析了垃圾渗滤液溶解性有机质的组成特征、结构特征及随年代变化特征.针对垃圾渗滤液难降解有机质的特性而研发的处理技术包括物化法、高级氧化法和微电解法等,并在实际工程中得到应用.随着越来越严格的渗滤液排放要求,溶解性有机质的去除应充分考虑投资的经济、运行的稳定性和可靠性.     

Release of dissolved organic matter by some marine macrophytes

The amount of photoassimilated carbon released as dissolved organic carbon was investigated for 5 species of benthic marine macrophytes (Thalassia testudinum, Diplanthera wrightii, Acanthophora spicifera, Chondria dasyphylla, and Dictyota dichotoma) and 1 species of pelagic marine macrophyte (Sargassum natans). Release rates ranged between 0.006 and 0.053 mg C g^-1 h^-1. Percent release values ranged from 1.1 to 3.8%. Spermatophytes had slightly lower percent release values than algae. Investigations performed on the ability of release products to be utilized by heterotrophic organisms showed that 20 to 30% of the released organic carbon was assimilated within a 2-h period.     

Suspended particulate organic matter in a Mediterranean submarine cave

Submarine caves display a paucity of benthic density and biomass that may be related to low trophic resources. Analysis of organic carbon, organic nitrogen, carbohydrate, protein and lipid content of suspended particulate matter was made during the period July 1985–July 1987 in a Mediterranean cave (Marseille, France) in order to determine any differences in the particulate organic matter composition along an horizontal transect. Particulate organic matter content clearly declined from the entrance of the cave to the dark inner area. This impoverishment could not be explained by a simple decrease in a few organic compounds, but appeared to be related to the combination of a decrease in both the amount and the composition of the suspended particles. Three progressive levels of impoverishment were identified towards the dark inner area of the cave: (i) decreasing amounts of seston; (ii) decreasing organic content of particles; (iii) increasing proportions of the geopolymeric (i.e., humic) components in the remaining organic matter, indicating increased degradation. The cave appeared to be sharply divided into two distinct sections — a twilight outer section whose waters contained slightly lower amounts of particulate organic matter than the open sea, and a dark inner section, 8 to 10 m higher, separated from the outer section by a steep rise and with waters of low organic matter content. The water in the twilight section appeared to be in thermal equilibrium with the open sea, and that in the dark inner section displayed thermal stratification. These differences indicated the presence of two distinct water bodies with contrasting average residence times, estimated as 1 d in the outer twilight section and 8 d in the dark inner section. The joint action of sedimentation and degradation resulted in an abrupt depletion of particulate organic matter in the dark inner section accompanied by a decrease in the benthic fauna. The decline in benthic heterotroph populations is probably related to the abrupt transition to oligotrophic conditions.     

Methods for the assessment of health risk induced by contaminants in atmospheric particulate matter: a review

Environmental Chemistry Letters - Air pollution is a major issue for human health with more than 7 million premature deaths per year due to indoor and outdoor air pollution. Exposure to particulate...