活化方式对过硫酸盐强化剩余污泥发酵的影响

对比考察了二价铁（Fe²⁺）、零价铁（ZVI）、超声波（US）3种活化方式对过硫酸盐（S₂O₈^2-）预处理剩余污泥的溶胞性能,并研究其对污泥厌氧发酵产酸进程的促进效能.结果表明,相对比未预处理污泥,S₂O₈^2-能够明显促进剩余污泥溶胞和发酵产酸进程;同时,活化后的S₂O₈^2-预处理效果明显优于未活化预处理实验组,其中S₂O₈^2-+Fe²⁺预处理体系的促进作用最为明显.Fe²⁺、ZVI和US活化S₂O₈^2-的3组溶胞率分别为42.6%、36.5%和32.9%,相比未活化实验组（22.3%）提高了10.6%～20.3%;3组活化体系最大挥发酸浓度分别为8052,6613,4996mg COD/L,而未活化组仅为3296mg COD/L.此外,不同方式活化S₂O₈^2-预处理对溶解性有机物溶出及挥发酸组分分布也有一定影响.从环境和经济角度来看,S₂O₈^2-+Fe²⁺体系对促进污泥发酵进程具有更大意义.     

全氟和多氟烷基化合物微生物降解与转化研究进展

全氟和多氟烷基化合物(PFASs)因其持久性、长距离迁移性、生物积累性和生物毒性而受到广泛关注.目前世界上对环境中PFASs的监测和管控主要针对全氟烷基酸(PFAAs).而大部分多氟烷基化合物在环境中能够被微生物降解为PFAAs,也被称为前体物.因此,探究前体物在环境中的微生物转化行为有助于综合评价PFASs的环境风险,以及制定相关的管控和修复措施.虽然PFAAs一直被认为是环境中的“永久化合物”,但近年来,PFAAs的厌氧微生物还原脱氟作为一项极具潜力且充满挑战的修复技术,成为研究的一个前沿热点.系统总结了前体物(氟调化合物和全氟辛烷磺胺衍生物)、 PFAAs和新型PFASs在微生物作用下的降解规律和转化路径,并讨论了PFASs微生物降解的影响因素,最后提出未来的研究方向.     

Modeling and verifying chlorine decay and chloroacetic acid formation in drinking water chlorination

This study presents a phenomenological model that can be used by the water professionals to quantify chlorine decay and disinfection byproduct (DBP) formation in water. The kinetic model was developed by introducing the concept of limiting chlorine demand and extending an established reactive species approach. The limiting chlorine demand, which quantifies chlorine reactive natural organic matter (NOM) on an equivalent basis, was mathematically defined by the relation between ultimate chlorine residue and initial chlorine dose. It was found experimentally that NOM in water has limiting chlorine demand that increases with chlorine dose once the ultimate residue is established. These results indicated that the complex NOM has a unique ability to adjust chemically to the change in redox condition caused by the free chlorine. It is attributed mainly to the redundant functional groups that persist in heterogeneous NOM molecules. The results also demonstrated that the effect of chlorine dose on the rate of chlorine decay can be quantitatively interpreted with the limiting chlorine demand. The kinetic model developed was validated for chlorine decay and chloroacetic acid formation in finished drinking water.     

Organic matter composition in sediments of the Oman Margin

The quantity and biochemical composition of organic matter (OM) in the sediments underlying and below oxygen minimum zone (OMZ) in the Arabian Sea were studied to provide information on the diagenetic processes of organic carbon under different environmental conditions. Concentrations of total organic carbon (TOC), total nitrogen (TN) and total hydrolysable amino acids (THAA) were significantly higher in sediments within rather than below OMZ, while those of total carbohydrates (TCHO) were slightly lower in the latter, suggesting the presence of a larger supply of labile compounds into the sea bottom at the shallower site (i.e. within OMZ). Hydrolysable amino acid and carbohydrate contribution to TOC were even lower (about 10% in surficial sediments) than the values obtained from the abyssal oligotrophic North Pacific, suggesting that OM food availability in the Oman Margin sediments within OMZ was lower than that observed at abyssal depths. The presence of the highest THAA and TCHO concentrations in the top 40?mm of the sediment core at both sites reflected the presence of bioturbation processes. In contrast with the general view of the deep sea as a stable and constant system, below OMZ in the Arabian Sea sediments, some differences were observed in the two investigated cores indicating the presence of a certain spatial variability in OM content and diagenesis.     

Compartmental systems. An appealing class for kinetic modeling and identification of metabolic processes

Problems which arise in quantitative studies on the kinetics of exogenous and endogenous chemical substances within the organism are examined together with approaches for their resolution. Linear and nonlinear compartmental mathematical models are presented and their relevant role for interpreting stimulus‐response experimental data is outlined. Available approaches are then discussed for the resolution of the system identification problem, including a priori and a posteriori identifiability, parameter estimation from test measurement data and optimum design of kinetic experiments. Finally, approaches to the problem of validation are reviewed.     

Microbial community variation in phytoremediation of triazophos by Canna indica Linn. in a hydroponic system

Phytoremediation of triazophos (O,O-diethyl-O-(1-phenyl-1,2,4-triazole-3-base) sulfur phosphate, TAP) pollution by Canna indica Linn. in a hydroponic system has been well studied, whereas the microbial mechanism on TAP degradation is still unknown. The variation in microbial community compositions was investigated by analyzing phospholipid fatty acids (PLFAs) profiles in microbes under TAP exposure. The TAP exposure resulted in an increase in proportions of fatty acid 16:0 and decrease in fatty acid 18:2ω9,12c, indicating that TAP may stimulate the reproduction of microorganisms and inhibit the growth of fungi to some degree. Significant correlation was found between the ratio of fungi to bacteria and TAP removal (r 2 = 0.840, p 0.01). In addition, the microbial community in the phytoremediation system with C. indica was dominated by Gram negative bacteria, which possibly contributed to the degradation of TAP. These results indicated that TAP might induce the colonization of bacteria in the hydroponic system planted with C. indica, and lead to a discrimination of microbial community, which might be one of the mechanisms on TAP dissipation in phytoremediation system.     

Effects of Lime and Ash Treatments on DOC Fractions and Low Molecular Weight Organic Acids in Soil Solutions of Acidified Podzolic Soils

Dissolved organic carbon (DOC) fractions and different low molecular weight organic acids (LMWOAs) were determined in soil solutions from two lime or ash treated Norway spruce sites in the south of Sweden. At Hasslöv, 3.45 t ha^-1 or 8.75 t ha^-1 dolomite were applied 15 years before sampling. Horröd was treated with 4.28 t ha^-1 ash and 3.25 t ha^-1 dolomite and sampled four years later. Propionate (7–268 M) and malonate (2–34 M) were the LMWOAsfound in the highest concentrations at Hasslöv. Two other LMWOAs dominated at Horröd, namely citrate (18–64 M)and fumarate (5–31 M). The differences in concentration of most of the determined LMWOAs at Hasslöv were significantly increased due to treatment. The LMWOAs comprised between 1.1–6.3% of the DOC at Hasslöv and 4.5–17.6% at Horröd. At Hasslöv normally 3–10% of the total acidity (TA) was due to LMWOAs and the average specific buffer capacity was 74 ± 22 mmol mol^-1C.The total DOC concentration in the mor layer solution was 16 mM for the dolomite treated plots compared to 10 mM at the untreated plot. A major part of the increase in DOC at the treated plots apparently had a hydrophobic character and was of high molecular weight corresponding to 3–10 kDa. The concentration of DOC < 1 kDa in the control and treated plots was similar.     

环境友好新型聚乳酸复合材料的研究及应用

聚乳酸(PLA)复合材料是一类重要的环境友好新型可降解材料。该材料通常是以PLA高分子为基体,以无机钙质成分(如羟基磷灰石、磷酸钙、珊瑚、珍珠层)、碳纤维、生物活性成分、有机物等为增强材料复合而成。概述了近年来国内外通过共聚、共混、复合等改性方法获得PLA复合材料的研究进展;论述了PLA复合材料的制备方法、生物相容性、力学性能、开发现状及应用等;指出使用新型的复合工艺、采用超细的无机粒子或纳米增强材料或加入特殊填料,同时开发新型增强物质是PLA复合材料的发展趋势;展望了PLA复合材料的应用前景。     

五种海洋微藻脂肪酸存在形式的初步研究

对五种海洋微藻的脂类组成进行了测定,微藻在确定的条件下生长,分别于指数生长前期和稳定期收获,采用超声波萃取法提取脂肪酸,应用GC及GC-MS技术进行定量和定性分析。结果表明,在两个时期取得的同种藻体中,各主要脂类化合物的量存在明显变化。由此可以看出,实验藻体中多数脂肪酸都参与组成储能物质;多不饱和脂肪酸主要是以储能物质形式存在,在细胞膜中存在较少。     

Characteristics and distribution of low molecular weight organic acids in the sediment porewaters in Bosten Lake, China

The composition and vertical profiles of low molecular-weight organic acids (LMWOAs) and the contribution of them to dissolved organic matter (DOM) in sediment porewaters in Bosten Lake, Xinjiang, China were investigated. The results showed that total concentration of LMWOAs was up to 94.5 μmol/L and their proportion in DOM was 5.6%, suggesting that LMWOAs were important chemical components in DOM in lake sediment porewaters. Among the seven LMWOAs, pyruvic and acetic acid had the highest concentrations with 26.30 and 8.31 μmol/L, accounting for 51.4% and 14.92% of LMWOAs, respectively. Trifluoroacetic and sorbic acid had the lowest concentrations, indicating that the compositions of LMWOAs in relative reducing environments were largely different from those reported in glacier, atmosphere and soils. The concentrations of lactic, acetic, formic, sorbic and oxalic acid decreased with increasing depth, probably relating to stronger microbial activities in the initial stage of early diagenesis. Trifluoroacetic acid was mainly anthropogenic with its concentration, showing a diusive trend from the surface to bottom sediments. The concentrations of lactic acid and nitrate generally showed a consistent profile. The increasing concentration of pyruvic acid in the vertical profile was just opposite to that of sulfate, revealing a significant negative relationship between them. Oxalic acid remained constant except for an obvious peak at 6 cm depth. The results indicated the diversities in sources and behaviors for various LMWOAs during early diagenesis in sediments.