Degradation of organic contaminants found in organic waste

In recent years, great interest has arisen in recycling of the waste created by modern society. A common way of recycling the organic fraction is amendment on farmland. However, these wastes may contain possible hazardous components in small amounts, which may prevent their use in farming. The objective of our study has been to develop biological methods by which selected organic xenobiotic compounds can be biotransformed by anaerobic or aerobic treatment. Screening tests assessed the capability of various inocula to degrade two phthalates di-n-butylphthalate, and di(2-ethylhexyl)phthalate, five polycyclic aromatic hydrocarbons, linear alkylbenzene sulfonates and three nonylphenol ethoxylates under aerobic and anaerobic conditions. Under aerobic conditions, by selecting the appropriate inoculum most of the selected xenobiotics could be degraded. Aerobic degradation of di(2-ethylhexyl)phthalate was only possible with leachate from a landfill as inoculum. Anaerobic degradation of some of the compounds was also detected. Leachate showed capability of degrading phthalates, and anaerobic sludge showed potential for degrading, polycyclic aromatic hydrocarbons, linear alkylbenzene sulfonates and nonyl phenol ethoxylates. The results are promising as they indicate that a great potential for biological degradation is present, though the inoculum containing the microorganisms capable of transforming the recalcitrant xenobiotics has to be chosen carefully.     

Acidity controls on dissolved organic carbon mobility in organic soils

Dissolved organic carbon (DOC) concentrations in surface waters have increased across much of Europe and North America, with implications for the terrestrial carbon balance, aquatic ecosystem functioning, water treatment costs and human health. Over the past decade, many hypotheses have been put forward to explain this phenomenon, from changing climate and land management to eutrophication and acid deposition. Resolution of this debate has been hindered by a reliance on correlative analyses of time series data, and a lack of robust experimental testing of proposed mechanisms. In a 4 year, four‐site replicated field experiment involving both acidifying and deacidifying treatments, we tested the hypothesis that DOC leaching was previously suppressed by high levels of soil acidity in peat and organo‐mineral soils, and therefore that observed DOC increases a consequence of decreasing soil acidity. We observed a consistent, positive relationship between DOC and acidity change at all sites. Responses were described by similar hyperbolic relationships between standardized changes in DOC and hydrogen ion concentrations at all sites, suggesting potentially general applicability. These relationships explained a substantial proportion of observed changes in peak DOC concentrations in nearby monitoring streams, and application to a UK‐wide upland soil pH dataset suggests that recovery from acidification alone could have led to soil solution DOC increases in the range 46–126% by habitat type since 1978. Our findings raise the possibility that changing soil acidity may have wider impacts on ecosystem carbon balances. Decreasing sulphur deposition may be accelerating terrestrial carbon loss, and returning surface waters to a natural, high‐DOC condition.     

Incubation studies on mineralization of organic sulphur and organic nitrogen

Summary Incubation studies were carried out to investigate the release of sulphur and nitrogen in West Indian soils. Sulphur and nitrogen released or fixed were estimated at 10 days intervals up to 60 days incubation period.All the soils released sulphate when incubated at 30°C. A rapid initial flush of mineralization of both sulphur and nitrogen took place in Cocal fine sand and Montreal sandy loam. In Piarco sandy clay loam and Mayaro sandy loam sulphur mineralization was not accompanied by a concomitant mineralization of nitrogen. An inconsistent pattern of release of sulphur and nitrogen was noticed in Montserrat clay, Akers sandy clay loam, Bellevue sandy clay loam and Soufriere cindery gravelly loamy sand.The release of sulphur does not appear to be related to the total amount of carbon, nitrogen or sulphur. Nitrogen mineralized was significantly correlated with total nitrogen and total sulphur. The correlation between organic matter and nitrogen mineralized was highly significant (r=0.87^**) whereas with sulphur mineralized it did not reach significance. This suggests that nitrogen and sulphur are not mineralized at the same rate in these soils.     

Alternative explanations for rising dissolved organic carbon export from organic soils

Since 1988, there has been, on average, a 91% increase in dissolved organic carbon (DOC) concentrations of UK lakes and streams in the Acid Waters Monitoring Network (AWMN). Similar DOC increases have been observed in surface waters across much of Europe and North America. Much of the debate about the causes of rising DOC has, as in other studies relating to the carbon cycle, focused on factors related to climate change. Data from our peat‐core experiments support an influence of climate on DOC, notably an increase in production with temperature under aerobic, and to a lesser extent anaerobic, conditions. However, we argue that climatic factors may not be the dominant drivers of DOC change. DOC solubility is suppressed by high soil water acidity and ionic strength, both of which have decreased as a result of declining sulphur deposition since the 1980s, augmented during the 1990s in the United Kingdom by a cyclical decline in sea‐salt deposition. Our observational and experimental data demonstrate a clear, inverse and quantitatively important link between DOC and sulphate concentrations in soil solution. Statistical analysis of 11 AWMN lakes suggests that rising temperature, declining sulphur deposition and changing sea‐salt loading can account for the majority of the observed DOC trend. This combination of evidence points to the changing chemical composition of atmospheric deposition, particularly the substantial reduction in anthropogenic sulphur emissions during the last 20 years, as a key cause of rising DOC. The implications of rising DOC export for the carbon cycle will be very different if linked primarily to decreasing acid deposition, rather than to changes in climate, suggesting that these systems may be recovering rather than destabilising.     

Orbitally magnetized organic solids

The preparation is discussed of polymeric organic solids in which large ring-like delocalized electronic orbitals can be made to enclose or trap magnetic flux. The situation is analogous to snapping shut a loop of superconductor while it is in a magnetic field. The operation of the Meissner effect acts to retain the trapped flux and create remant magnetization.     

Investigations on organic fungicides

Antonie van Leeuwenhoek - The antimicrobial spectrum of the antifungal substance tetramethylthiuram disulphide (t.m.t.d.) was determined. The substance in general possessed antifungal rather than...     

Biocatalysis in organic media

The potentials of using organic reaction media in biotechnological conversions have already been demonstrated in several experimental studies. Examples of possible advantages are: possibility of higher substrate and/or product concentrations, favorable shift of reaction equilibria, reduced substrate and/or product inhibition, and facilitated product recovery. Especially water/organic solvent two-phase systems seem to possess several of these advantages. The solvent type will highly affect kinetics and stability of the (immobilized) biocatalyst, solubility and partitioning of reactants/products, and product recovery. Therefore the solvent choice can have a large influence on the economics of the two-liquid-phase biocatalytic process. Immobilization of the biocatalyst may be useful to provide protection against denaturating solvent effects. The polarity of the employed support material will also be decisive for the partitioning of substrates and products among the various phases.

A classification of biphasic systems, which is based on the possible types of theoretical concentration profiles and aqueous phase configurations, is discussed. Reversed micelles and aqueous two-liquid-phase systems can be considered as special cases. The design of two-liquid-phase bioreactors is dependent on the state of the biocatalyst, free or immobilized, and on the necessity for emulsification of one of the two liquid phases in the other. Many mass-transfer resistances, e.g. across the liquid/liquid interface, in the aqueous phase, across the liquid/solid interface, and in the biocatalyst phase, can limit the overall reaction rate. The epoxidation of alkenes in water/solvent two-phase systems is discussed to give an example of the scope of biotechnological processes that is obtained by using organic media. Finally, a design calculation of a packed-bed organic-liquid-phasel immobilized-biocatalyst reactor for the epoxidation of propene is given to illustrate some of the above aspects.     

Complexity in organic evolution

The present state of knowledge of the formation of the Compounds I of peroxidases and catalases is discussed in terms of the restrictions which must be placed upon a valid mechanism. It is likely that all Compounds I contain one oxygen atom bound to the heme-iron as in the Compound I of chloroperoxidase. Thus the formation of Compound I, obtained after molecular hydrogen peroxide and the enzyme diffuse together, involves a minimum of two bond ruptures and the formation of two new bonds. Yet this amazing reaction proceeds with an activation energy equal to or less than that for the fluidity of water. This result can only be accounted for by including at least one reversible step. Since Compound I formation requires the formation of an “inner sphere” complex, the presence or absence of water in the sixth co-ordination position of the heme-iron is of crucial importance. A comparison of the rates of ligand binding with the rate of Compound I formation indicate that the inner sphere complex leading to Compound I formation is formed by an excellent nucleophile, probably the peroxide anion, formed by a proton transfer from hydrogen peroxide. This proton cannot equilibrate with the bulk solvent. A proton derived from the active site would appear to be added to the hydroxide ion which permits a molecule of water to depart upon oxygen atom addition (or substitution) to (or at) the heme-iron. It is tentatively suggested that Compound I of catalase has a single active site per subunit molecule and that Compound I of peroxidase normally has two reactive sites.     

Polyoxovanadates with organic ligands

Polyoxovanadates are inhibitors to various phosphate-metabolizing enzymes. The question arises of how the cluster is bound to the protein matrix. This paper describes oxovanadates with carboxylate and hydroxide ligands in the periphery of the cluster, which may be considered to model oxovanadate binding to carboxylic and alcoholic side-chain functions of the protein. Examples for complexes carrying alkoxo ligands dealt with in this article are dinuclear vanadate(V) esters, and hexa-, octa- and decanuclear, mixed-valence (V^V/V^IV) clusters, the latter related to decavanadate. The possible role of dimeric vanadate esters as transition state anologues in enzymatic phosphoester cleavage is addressed. Examples for carboxylate complexes are the mononuclear, seven-coordinate mixed anhydride between orthovanadic acid and pivalic acid, containing the carboxylate in the bidentate mode, tetra-, penta- and hexanuclear V^IV/V^V clusters with bridging carboxylate, and trinuclear V^IV and V^II/V^III clusters, bridged by carboxylates and trebly bridged by O^2–. Special attention is given to a comparison of the bowls containing a V₄(-O)₃(-OH)(O₂CR)₄ and V₄(-O₄(O₂CR)₄ core, respectively, which can accomodate a K⁺ or a NO ₃ ^– .⁵¹V NMR spectroscopy is shown to be a useful tool, in many cases, for the vanadium speciation of complex systems.     

Investigations on organic fungicides

Summary The antimicrobial spectrum of the antifungal substance tetramethylthiuram disulphide (t.m.t.d.) was determined. The substance in general possessed antifungal rather than antibacterial properties. The bacteria as well as the moulds varied considerably with regard to their sensitivity towards t.m.t.d. Among the moulds the parasitic species were in general more sensitive to t.m.t.d. than the saprophytic fungi.The mode of action of t.m.t.d. was briefly discussed. It was concluded that this substance probably acts by interference with the anabolic part of mould metabolism.     

Proteins in organic solvents

Catalysis in organic solvents and the mapping of protein surfaces using multiple solvent crystal structures are two rapidly developing areas of research. Recent advances include the study of protein folding and stability in different solvents, and the demonstration that it is possible to qualitatively rank the affinities of protein binding sites for a given organic solvent using the multiple solvent crystal structures method.     

Phytodegradation of organic compounds

The phytodegradation of organic compounds can take place inside the plant or within the rhizosphere of the plant. Many different compounds and classes of compounds can be removed from the environment by this method, including solvents in groundwater, petroleum and aromatic compounds in soils, and volatile compounds in the air. Although still a relatively new area of research, there are many laboratories studying the underlying science necessary for a wide range of applications for plant-based remediation of organic contaminants.