Pyrite oxidation by Thiobacillus ferrooxidans with special reference to the sulphur moiety of the mineral

Available cultures of Thiobacillus ferrooxidans were found to be contaminated with bacteria very similar to Thiobacillus acidophilus. The experiments described were performed with a homogeneous culture of Thiobacillus ferrooxidans.Pyrite (FeS₂) was oxidized by Thiobacillus ferrooxidans grown on iron (Fe²⁺), elemental sulphur (S^o) or FeS₂.Evidence for the direct utilization of the sulphur moiety of pyrite by Thiobacillus ferrooxidans was derived from the following observations: a. Known inhibitors of Fe²⁺ and S^o oxidation, NaN₃ and NEM, respectively, partially abolished FeS₂ oxidation. b. A b-type cytochrome was detectable in FeS₂-and S^o-grown cells but not in Fe²⁺-grown cells. c. FeS₂ and S^o reduced b-type cytochromes in whole cells grown on S^o. d. CO₂ fixation at pH 4.0 per mole of oxygen consumed was the highest with S^o, lowest with Fe²⁺ and medium with FeS₂ as substrate. e. Bacterial Fe²⁺ oxidation was found to be negligible at pH 5.0 whereas both FeS₂ and S^o oxidation was still appreciable above this pH. f. Separation of pyrite and bacteria by means of a dialysis bag caused a pronounced drop of the oxidation rate which was similar to the reduction of pyrite oxidation by NEM; indirect oxidation of the sulphur moiety by Fe³⁺ was not affected by separation of pyrite and bacteria.Bacterial oxidation and utilization of the sulphur moiety of pyrite were relatively more important with increasing pH.     

Process for biological oxidation and control of dissolved iron in bioleach liquors

Iron has a central role in bioleaching and biooxidation processes. Fe²⁺ produced in the dissolution of sulfidic minerals is re-oxidized to Fe³⁺ mostly by biological action in acid bioleaching processes. To control the concentration of iron in solution, it is important to precipitate the excess as part of the process circuit. In this study, a bioprocess was developed based on a fluidized-bed reactor (FBR) for Fe²⁺ oxidation coupled with a gravity settler for precipitative removal of ferric iron. Biological iron oxidation and partial removal of iron by precipitation from a barren heap leaching solution was optimized in relation to the performance and retention time (τ_FBR) of the FBR. The biofilm in the FBR was dominated by Leptospirillum ferriphilum and “Ferromicrobium acidiphilum.” The FBR was operated at pH 2.0 ± 0.2 and at 37 °C. The feed was a barren leach solution following metal recovery, with all iron in the ferrous form. 98–99% of the Fe²⁺ in the barren heap leaching solution was oxidized in the FBR at loading rates below 10 g Fe²⁺/L h (τ_FBR of 1 h). The optimal performance with the oxidation rate of 8.2 g Fe²⁺/L h was achieved at τ_FBR of 1 h. Below the τ_FBR of 1 h the oxygen mass transfer from air to liquid limited the iron oxidation rate. The precipitation of ferric iron ranged from 5% to 40%. The concurrent Fe²⁺ oxidation and partial precipitative iron removal was maximized at τ_FBR of 1.5 h, with Fe²⁺ oxidation rate of 5.1 g Fe²⁺/L h and Fe³⁺ precipitation rate of 25 mg Fe³⁺/L h, which corresponded to 37% iron removal. The precipitates had good settling properties as indicated by the sludge volume indices of 3–15 mL/g but this step needs additional characterization of the properties of the solids and optimization to maximize the precipitation and to manage sludge disposal.     

Effect of chloride on ferrous iron oxidation by a Leptospirillum ferriphilum‐dominated chemostat culture

Biomining is the use of microorganisms to catalyze metal extraction from sulfide ores. However, the available water in some biomining environments has high chloride concentrations and therefore, chloride toxicity to ferrous oxidizing microorganisms has been investigated. Batch biooxidation of Fe²⁺ by a Leptospirillum ferriphilum‐dominated culture was completely inhibited by 12 g L^?1 chloride. In addition, the effects of chloride on oxidation kinetics in a Fe²⁺ limited chemostat were studied. Results from the chemostat modeling suggest that the chloride toxicity was attributed to affects on the Fe²⁺ oxidation system, pH homeostasis, and lowering of the proton motive force. Modeling showed a decrease in the maximum specific growth rate (µ_max) and an increase in the substrate constant (K_s) with increasing chloride concentrations, indicating an effect on the Fe²⁺ oxidation system. The model proposes a lowered maintenance activity when the media was fed with 2–3 g L^?1 chloride with a concomitant drastic decrease in the true yield (Y_true). This model helps to understand the influence of chloride on Fe²⁺ biooxidation kinetics. Biotechnol. Bioeng. 2010; 106: 422–431. © 2010 Wiley Periodicals, Inc.     

Effects of protease inhibitors on liver regeneration

The oxidation of Fe²⁺ to Fe³⁺ by oxygen at pH 7.45 is a first order reaction with a 25 minute half life. In the presence of apotransferrin the oxidation rate is greatly enhanced and Fe³⁺-transferrin is formed. The apotransferrin mediated reaction reaches 50% completion in one minute; it does not follow simple first order kinetics. Iron-saturated transferrin does not exhibit the rate enhancement effect suggesting that the specific metal binding sites are the loci of the iron oxidation. Addition of H₂O₂, an agent which rapidly oxidizes Fe²⁺ to Fe³⁺, during the reaction of Fe²⁺ with apotransferrin greatly decreases the yield of Fe³⁺-transferrin. It is postulated that the basis of the rate enhancement effect is the binding of Fe²⁺ to the metal binding site of the transferrin molecule, followed by a rapid oxidation of the iron to the trivalent form.     

Biooxidation of ferrous iron by immobilized Acidithiobacillus ferrooxidans in poly(vinyl alcohol) cryogel carriers

PVA-cryogels entrapping about 10⁹ cells of Acidithiobacillus ferrooxidans per ml of gel were prepared by freezing-thawing procedure, and the biooxidation of Fe²⁺ by immobilized cells was investigated in a 0.365 l packed-bed bioreactor. Fe²⁺ oxidation fits a plug-flow reaction model well. A maximum oxidation rate of 3.1 g Fe²⁺ l^–1 h^–1 was achieved at the dilution rate of 0.4 h^–1 or higher, while no obvious precipitate was determined at this time. In addition, cell-immobilized PVA-cryogels packed in bioreactor maintained their oxidative ability for more than two months under non-sterile conditions. Nomenclature: C _A0 – Concentration of Fe²⁺ in feed stream (g l^–1) C _A – Concentration of Fe^{2 +} in outlet stream (g l^{– 1}) D – Dilution rate of the packed-bed bioreactor (h^–1) F – Volumetric flow rate of iron solution (l h^–1) F _A0 – Mass flow rate of Fe²⁺ in the feed stream (g h^–1) K – Kinetic constant (l l^–1 h^–1) r _A – Oxidation rate of Fe²⁺ (g l^–1 h^–1) V – Volume of packed-bed bioreactor (l) X _A – Conversion ratio of Fe²⁺ (%)     

Studies on the growth ofThiobacillus ferrooxidans

Summary Uranyl sulphate (0.2–0.9 mM) inhibited ferrous iron oxidation by growing cultures ofThiobacillus ferrooxidans. The addition of 5–100 mM uranium to the cultures caused immediate cessation of carbon dioxide fixation, rapid loss of viability and gradual depression of ferrous iron oxidation. Virtually no uranium was found in washed cells grown in the presence of subtoxic to toxic amounts of uranyl sulphate. Uranium-poisoned organisms appeared plasmolyzed in electron micrographs. Cultures tolerant to 5 mM UO₂ ²⁺ were develoepd by successive subculturing in increased uranium concentrations. The tolerance was maintained during subculturing in uranium-free medium. Frequency of mutants resistant to 1.0 and 1.5 mM UO₂ ²⁺ was 1 per 1.3×10⁶ and 1 per 9.0×10⁸, respectively. The frequency was increased in the presence of 15–150 mM nickel, zinc and manganese. In liquid cultures, bivalent cations and EDTA alleviated the toxicity of 2 mM uranyl sulphate.     

Modelling of Fe2 + oxidation by Thiobacillus ferrooxidans

Summary The kinetics of oxidation of aqueous acidic ferrous sulphate by Thiobacillus ferrooxidans has been studied in a batch reactor. The contribution of cell wall envelopes to the oxidation rate has been shown to be negligible. A model which accounts for the oxidation of Fe^{2 +}, death of bacteria due to Fe^{3 +} poisoning, existence of an optimal pH and precipitation of Fe^{3 +} has been proposed. The model is able to predict the concentration of Fe^{2 +} and pH quite satisfactorily. The predictions of Fe^{3 +} are not so accurate because of simplifying assumptions made about its precipitation. Offprint requests to: R. Kumar     

Biogeochemical Properties of Bacteriogenic Iron Oxides

Bacteriogenic iron oxides (BIOS) are composite materials that consist of intact and partly degraded remains of bacterial cells intermixed with variable amounts of poorly ordered hydrous ferric oxide (HFO) minerals. They form in response to chemical or bacterial oxidation of Fe²⁺, which gives rise to Fe³⁺. Once formed, Fe³⁺ tends to undergo hydrolysis to precipitate in association with bacterial cells. In acidic systems where the chemical oxidation of Fe²⁺ is slow, bacteria are capable of accelerating the reaction by several orders of magnitude. At circumneutral pH, the chemical oxidation of Fe²⁺ is fast. This requires Fe²⁺ oxidizing bacteria to exploit steep redox gradients where low pO₂ slows the abiotic reaction enough to allow the bacteria to compete kinetically. Because of their reactive surface properties, BIOS behave as potent sorbents of dissolved metal ions. Strong enrichments of Al, Cu, Cr, Mn, Sr, and Zn in the solid versus aqueous phase (log 10 K_d values range from 1.9 to 4.2) are common; however, the metal sorption properties of BIOS are not additive owing to surface chemical interactions between the constituent HFO and bacteria. These interactions have been investigated using acid-base tritrations, which show that the concentration of high pK_a sites is reduced in BIOS compared to HFO. At the same time, hydroxylamine insoluble material (i.e., residual bacterial fraction) is enriched in low pK_a sites relative to both BIOS and HFO. These differences indicate that low pK_a or acidic sites associated with bacteria in BIOS interact specifically with high pK_a or basic sites on intermixed HFO.     

FORMATION AND MORPHOLOGY OF AN IRON PLAQUE ON THE ROOTS OF TYPHA LATIFOLIA L. GROWN IN SOLUTION CULTURE

Roots of Typha latifolia L. exposed to Fe²⁺ under reduced conditions in solution culture developed visible coatings (plaques) of an oxidized Fe compound that extended as much as 15-17 μm into the rhizosphere. Iron concentrations were significantly less and discoloration was not apparent on the surface of roots exposed to Fe-(BPDS)₃, Fe³⁺, Fe-EDDHA, and Fe-EDTA. The extent of plaque formation increased with the concentration of Fe²⁺ in solution and with pH of the solution in the range of 3.0 to 4.6. Above pH 4.6, oxidation of Fe²⁺ in the culture solution may have reduced precipitation of Fe on the root surface. Plaque development was most extensive approximately 1.0 cm from the root tip, but all root surfaces showed some Fe staining. Scanning electron micrographs of plaqued roots, grown both in solution culture and in the field, provided support for a model of cast formation by oxidation and precipitation of Fe on external cell surfaces.     

The influence of pH on OH scavenger inhibition of damage to deoxyribose by Fenton reaction

Summary Hydroxyl radicals (OH') can be formed in aqueous solution by direct reaction of hydrogen peroxide (H₂O₂) with ferrous salt (Fenton reaction). OH' damage to deoxyribose, measured as formation of thiobarbituric acid-reactive material, was evaluated at different pHs to study the mechanism of action of classical OH' scavengers. OH' scavenger effect on Fe²⁺ oxidation was also evaluated in the same experimental conditions. In the absence of OH' scavengers, OH' damage to deoxyribose is higher at acidic compared to neutral and moderately basic pH. At acidic pH deoxiribose is per se able to inhibit Fe²⁺ oxidation by H₂0₂. Most of OH' scavengers tested inhibit deoxyribose damage and Fe²⁺ oxidation in a similar manner: both inhibitions are most relevant at acidic pH and decrease by increasing the pH. These results are not due to OH' scavenger inhibition of Fenton reaction. The influence of pH on the parameters studied appears to be due to the competition of deoxyribose and OH' scavengers for iron. These results suggest the prominent role of iron binding in the degradation of deoxyribose and in the OH' scavenging ability of different compounds. Results obtained with triethylenetetramine, a iron chelator with a low rate constant with OH', confirm that both deoxyribose and the OH' scavengers interact with iron bringing about a site specific Fenton reaction; that the OH' formed at these sites oxidize these molecules to their radical forms which in turn reduce the Fe^3– produced by Fenton reaction. The results presented indicate that most of classical OH' scavengers exert their effect predominantly by preventing the site specific reaction between Fe²⁺ and H₂0₂ on the deoxyribose molecule.     

Iron (III) Stimulation of Lipid Hydroperoxide-Dependent Lipid Peroxidation

In an experimental system where both Fe²⁺ autoxidation and generation of reactive oxygen species is negligible, the effect of FeCl₂ and FeCl₃ on the peroxidation of phosphatidylcholine (PC) liposomes containing different amounts of lipid hydroperoxides (LOOH) was studied; Fe²⁺ oxidation, oxygen consumption and oxidation index of the liposomes were measured. No peroxidation was observed at variable FeCl₂/FeCl₃ ratio when PC liposomes deprived of LOOH by triphenyl-phosphine treatment were utilized. By contrast, LOOH containing liposomes were peroxidized by FeCl₂. The FeCl₂ concentration at which Fe²⁺ oxidation was maximal, defined as critical Fe²⁺ concentration [Fe²⁺]*, depended on the LOOH concentration and not on the amount of PC liposomes in the assay. The LOOH-dependent lipid peroxidation was stimulated by FeCl₃, addition; the oxidized form of the metal increased the average length of radical chains, shifted to higher values the [Fe²⁺]* and shortened the latent period. The iron chelator KSCN exerted effects opposite to those exerted by FeCl₃ addition. The experimental data obtained indicate that the kinetics of LOOH-dependent lipid peroxidation depends on the Fe²⁺/Fe³⁺ ratio at each moment during the time course of lipid peroxidation. The results confirm that exogenously added FeCl₃ does not affect the LOOH-independent but the LOOH-deendent lipid peroxidation; and suggest that the Feg, endogenously generated exerts a major role in the control of the LOOH-dependent lipid peroxidation.     

Structural similarity and functional diversity in diiron-oxo proteins

 Diiron-oxo proteins currently represent one of the most rapidly developing areas of bioinorganic chemistry. All of these proteins contain a four-helix bundle protein fold surrounding a (μ-carboxylato)diiron core, and most, if not all, of the diiron(II) sites appear to react with O₂ as part of their functional processes. Despite these common characteristics, an emerging functional diversity is one of the most striking aspects of this class of proteins. X-ray crystal structures of diiron(II) sites are now available for four of these proteins: hemerythrin (Hr), the hydroxylase protein of methane monooxygenase (MMOH), the R2 protein of Escherichia coli ribonucleotide reductase (RNR-R2), and a plant acyl-carrier protein Δ⁹-desaturase. The structure of the diiron(II) site in Hr, the sole O₂ carrier in the group, is clearly distinct from the other three, whose function is oxygen activation. The Hr diiron site is more histidine rich, and the oxygen-activating diiron sites contain a pair of (D/E)X_30–37EX₂H ligand sequence motifs, which is clearly not found in Hr. The Hr diiron site apparently permits only terminal O₂ coordination to a single iron, whereas the oxygen-activating diiron(II) centers present open or labile coordination sites on both irons of the center, and show a much greater coordinative flexibility upon oxidation to the diiron(III) state. Intermediates at the formal Fe^IIIFe^III and Fe^IVFe^IV oxidation levels for MMOH and formal Fe^IIIFe^IV oxidation level for RNR-R2 have been identified during reactions of the diiron(II) sites with O₂. An [Fe₂(μ-O)₂]^4+, 3+ "diamond core" structure has been proposed for the latter two oxidation levels. The intermediate at the Fe^IIIFe^IV oxidation level in RNR-R2 is kinetically competent to generate a stable, functionally essential tyrosyl radical. The Fe^IVFe^IV oxidation level is presumed to effect hydroxylation of hydrocarbons in MMOH, but the mechanism of this hydroxylation, particularly the involvement of discrete radicals, is currently controversial. The biological function of diiron sites in three members of this class, rubrerythrin, ferritin and bacterioferritin, remains enigmatic. Received: 31 July 1996 / Accepted: 4 October 1996     

Ferrous Iron and Sulfur Oxidation and Ferric Iron Reduction Activities of Thiobacillus ferrooxidans Are Affected by Growth on Ferrous Iron, Sulfur, or a Sulfide Ore

Eight strains of Thiobacillus ferrooxidans (laboratory strains Tf-1 [= ATCC 13661] and Tf-2 [= ATCC 19859] and mine isolates SM-1, SM-2, SM-3, SM-4, SM-5, and SM-8) and three strains of Thiobacillus thiooxidans (laboratory strain Tt [= ATCC 8085] and mine isolates SM-6 and SM-7) were grown on ferrous iron (Fe²⁺), elemental sulfur (S⁰), or sulfide ore (Fe, Cu, and Zn). The cells were studied for their aerobic Fe²⁺ - and S⁰-oxidizing activities (O₂ consumption) and anaerobic S⁰-oxidizing activity with ferric iron (Fe³⁺) (Fe²⁺ formation). Fe²⁺-grown T. ferrooxidans cells oxidized S⁰ aerobically at a rate of 2 to 4% of the Fe²⁺ oxidation rate. The rate of anaerobic S⁰ oxidation with Fe³⁺ was equal to the aerobic oxidation rate in SM-1, SM-3, SM-4, and SM-5, but was only one-half or less that in Tf-1, Tf-2, SM-2, and SM-8. Transition from growth on Fe²⁺ to that on S⁰ produced cells with relatively undiminished Fe²⁺ oxidation activities and increased S⁰ oxidation (both aerobic and anaerobic) activities in Tf-2, SM-4, and SM-5, whereas it produced cells with dramatically reduced Fe²⁺ oxidation and anaerobic S⁰ oxidation activities in Tf-1, SM-1, SM-2, SM-3, and SM-8. Growth on ore 1 of metal-leaching Fe²⁺-grown strains and on ore 2 of all Fe²⁺-grown strains resulted in very high yields of cells with high Fe²⁺ and S⁰ oxidation (both aerobic and anaerobic) activities with similar ratios of various activities. Sulfur-grown Tf-2, SM-1, SM-4, SM-6, SM-7, and SM-8 cultures leached metals from ore 3, and Tf-2 and SM-4 cells recovered showed activity ratios similar to those of other ore-grown cells. It is concluded that all the T. ferrooxidans strains studied have the ability to produce cells with Fe²⁺ and S⁰ oxidation and Fe³⁺ reduction activities, but their levels are influenced by growth substrates and strain differences.     

Rate Equations and Kinetic Parameters of the Reactions Involved in Pyrite Oxidation by Thiobacillus ferrooxidans

Rate equations and kinetic parameters were obtained for various reactions involved in the bacterial oxidation of pyrite. The rate constants were 3.5 μM Fe²⁺ per min per FeS₂ percent pulp density for the spontaneous pyrite dissolution, 10 μM Fe²⁺ per min per mM Fe³⁺ for the indirect leaching with Fe³⁺, 90 μM O₂ per min per mg of wet cells per ml for the Thiobacillus ferrooxidans oxidation of washed pyrite, and 250 μM O₂ per min per mg of wet cells per ml for the T. ferrooxidans oxidation of unwashed pyrite. The K_m values for pyrite concentration were similar and were 1.9, 2.5, and 2.75% pulp density for indirect leaching, washed pyrite oxidation by T. ferrooxidans, and unwashed pyrite oxidation by T. ferrooxidans, respectively. The last reaction was competitively inhibited by increasing concentrations of cells, with a K_i value of 0.13 mg of wet cells per ml. T. ferrooxidans cells also increased the rate of Fe²⁺ production from Fe³⁺ plus pyrite.     

Mechanisms of Saccharomyces Cerevisiae PMA1 H+-ATPase inactivation by Fe2+, H2O2 and Fenton reagents

Although considerably more oxidation-resistant than other P-type ATPases, the yeast PMA1 H⁺-ATPase of Saccharomyces cerevisiae SY4 secretory vesicles was inactivated by H₂O₂, Fe²⁺, Fe- and Cu-Fenton reagents. Inactivation by Fe²⁺ required the presence of oxygen and hence involved auto-oxidation of Fe²⁺ to Fe³⁺. The highest Fe^2- (100 μM) and H₂O₂ (100 mM) concentrations used produced about the same effect. Inactivation by the Fenton reagent depended more on Fe²⁺ content than on H₂O₂ concentration, occurred only when Fe²⁺ was added to the vesicles first and was only slightly reduced by scavengers (mannitol, Tris, NaN₃, DMSO) and by chelators (EDTA, EGTA, DTPA, BPDs, bipyridine, 1, 10-phenanthroline). Inactivation by Fe- and Cu- Fenton reagent was the same; the identical inactivation pattern found for both reagents under anaerobic conditions showed that both reagents act via OH^·. The lipid peroxidation blocker BHT prevented Fenton-induced rise in lipid peroxidation in both whole cells and in isolated membrane lipids but did not protect the H⁺-ATPase in secretory vesicles against inactivation. ATP partially protected the enzyme against peroxide and the Fenton reagent in a way resembling the protection it afforded against SH-specific agents. The results indicate that Fe²⁺ and the Fenton reagent act via metal-catalyzed oxidation at specific metal-binding sites, very probably SH-containing amino acid residues. Deferrioxamine, which prevents the redox cycling of Fe²⁺, blocked H⁺-ATPase inactivation by Fe²⁺ and the Fenton reagent but not that caused by H₂O₂, which therefore seems to involve a direct non-radical attack. Fe-Fenton reagent caused fragmentation of the H⁺-ATPase molecule, which, in Western blots, did not give rise to defined fragments bands but merely to smears.     

Predicting the disruption by of a protein-ligand interaction

The uranyl cation (UO₂²⁺) can be suspected to interfere with the binding of essential metal cations to proteins, underlying some mechanisms of toxicity. A dedicated computational screen was used to identify UO₂²⁺ binding sites within a set of nonredundant protein structures. The list of potential targets was compared to data from a small molecules interaction database to pinpoint specific examples where UO₂²⁺ should be able to bind in the vicinity of an essential cation, and would be likely to affect the function of the corresponding protein. The C‐reactive protein appeared as an interesting hit since its structure involves critical calcium ions in the binding of phosphorylcholine. Biochemical experiments confirmed the predicted binding site for UO₂²⁺ and it was demonstrated by surface plasmon resonance assays that UO₂²⁺ binding to CRP prevents the calcium‐mediated binding of phosphorylcholine. Strikingly, the apparent affinity of UO₂²⁺ for native CRP was almost 100‐fold higher than that of Ca²⁺. This result exemplifies in the case of CRP the capability of our computational tool to predict effective binding sites for UO₂²⁺ in proteins and is a first evidence of calcium substitution by the uranyl cation in a native protein.     

Interactions of uranyl ion with cytochrome <Emphasis Type="Italic">b</Emphasis><Subscript>5</Subscript> and its His39Ser variant as revealed by molecular simulation in combination with experimental methods

The biological toxicity of uranyl ion (UO₂²⁺) lies in interacting with proteins and disrupting their native functions. The structural and functional consequences of UO₂²⁺ interacting with cytochrome b ₅ (cyt b ₅), a small membrane heme protein, and its heme axial ligand His39Ser variant, cyt b ₅ H39S, were investigated both experimentally and theoretically. In experiments, although cyt b ₅ was only slightly affected, UO₂²⁺ binding to cyt b ₅ H39S with a K _D of 2.5 μM resulted in obvious alteration of the heme active site, and led to a decrease in peroxidase activity. Theoretically, molecular simulation proposed a uranyl ion binding site for cyt b ₅ at surface residues of Glu37 and Glu43, revealing both coordination and hydrogen bonding interactions. The information gained in this study provides insights into the mechanism of uranyl toxicity toward membrane protein at an atomic level.     

Spin trapping nitric oxide from neuronal nitric oxide synthase: A look at several iron–dithiocarbamate complexes

The free radical, nitric oxide (√NO), is responsible for a myriad of physiological functions. The ability to verify and study √NO in vivo is required to provide insight into the events taking place upon its generation and in particular the flux of √NO at relevant cellular sites. With this in mind, several iron-chelates (Fe²⁺(L)₂) have been developed, which have provided a useful tool for the study and identification of √NO through spin-trapping and electron paramagnetic resonance (EPR) spectroscopy. However, the effectiveness of √NO detection is dependent on the Fe²⁺(L)₂ complex. The development of more efficient and stable Fe²⁺(L)₂ chelates may help to better understand the role of √NO in vivo. In this paper, we present data comparing several proline derived iron–dithiocarbamate complexes with the more commonly used spin traps for √NO, Fe²⁺-di(N-methyl-D-glutamine-dithiocarbamate) (Fe²⁺(MGD)₂) and Fe²⁺-di(N-(dithiocarboxy)sarcosine) (Fe²⁺(DTCS)₂). We evaluate the apparent rate constant (k_app) for the reaction of √NO with these Fe²⁺(L)₂ complexes and the stability of the corresponding Fe²⁺(NO)(L)₂ in presence of NOS I.     

Oxidative Inactivation of Brain Alkaline Phosphatase Responsible for Hydrolysis of Phosphocholine

Abstract : Alkaline phosphatase, one of the enzymes responsible for the conversion of phosphocholine into choline, was purified from bovine brain membrane, where the phosphatase is bound as glycosylphosphatidylinositollinked protein, and subjected to oxidative inactivation. The phosphatase activity, based on the hydrolysis of p-nitrophenyl phosphate and phosphocholine, decreased slightly after the exposure to H₂O₂. Inclusion of Cu²⁺ in the incubation with 1 mM H₂O₂ led to a rapid decrease of activity in a time- and concentration-dependent manner. In comparison, the H₂O₂/Cu²⁺ system was much more effective than the H₂O₂/Fe²⁺ system in inactivating brain phosphatase. In a further study, it was observed that the hydroxy radical scavengers mannitol, ethanol, or benzoate failed to prevent against H₂O₂/Cu²⁺-induced inactivation of the phosphatase, excluding the involvement of extraneous hydroxy radicals in metalcatalyzed oxidation. In addition, it was found that both substrates, p-nitrophenyl phosphate and phosphocholine, and an inhibitor, phosphate ion, at their saturating concentrations exhibited a remarkable, although incomplete, protection against the inactivating action of H₂O₂/Cu²⁺. A similar protection was also expressed by divalent metal ions such as Mg²⁺ or Mn²⁺. Separately, it was found that H₂O₂/Fe²⁺-induced inactivation was prevented by p-nitrophenyl phosphate or Mg²⁺ but not phosphate ions. Thus, it is implied that phosphocholine-hydrolyzing alkaline phosphatase in brain membrane might be one of enzymes susceptible to metal-catalyzed oxidation.     

Competitive Inhibition of Ferrous Iron Oxidation by Thiobacillus ferrooxidans by Increasing Concentrations of Cells

The oxidation of ferrous iron (Fe²⁺) to ferric iron (Fe³⁺) with dioxygen (O₂) by various strains of Thiobacillus ferrooxidans was studied by measuring the rate of O₂ consumption at various Fe²⁺ concentrations and cell concentrations. The apparent K_m values for Fe²⁺ remained constant at different cell concentrations of laboratory strains ATCC 13661 and ATCC 19859 but increased with increasing cell concentrations of mine isolates SM-4 and SM-5. The latter results are explained by the competitive inhibition of the Fe²⁺-binding site of a cell by other cells in the reaction mixture. Possible mechanisms involving cell surface properties are discussed.