Inhibition of ferrous iron induced oxidation of arachidonic acid by indomethacin

The molecular mechanism by which indomethacin exerts its inhibitory effects on the prostaglandin endoperoxide synthetase enzyme is unknown. In the present study we have explored the possibility that indomethacin might interact with Fe⁺⁺ in the enzyme to produce its inhibitory effect. For this study we made use of the recent discovery that Fe⁺⁺ alone can oxidize arachidonic acid, and the interaction of this fatty acid with the metal can be detected by following reduction of nitroblue tetrazolium (NBT) or by conversion of the Fe⁺⁺ to Fe⁺⁺⁺. Indomethacin markedly inhibited NBT reduction in the presence of arachidonic acid and Fe⁺⁺ when the indomethacin had been preincubated with the Fe⁺⁺. Indomethacin also inhibited the conversion of Fe⁺⁺ to Fe⁺⁺⁺ by arachidonic acid. Results obtained by varying the concentrations of indomethacin and arachidonic acid and measuring inhibition of the conversion of Fe⁺⁺ to Fe⁺⁺⁺ by the indomethacin are consistent with a one to one complex forming between indomethacin and Fe⁺⁺. The complex between indomethacin and Fe⁺⁺ separates on prolonged incubation of the complex with arachidonic acid. The nature of the binding is suggested by a molecular model. Our results suggest that indomethacin may act to inhibit the prostaglandin endoperoxide synthetase enzyme by complexing Fe⁺⁺ in the enzyme. Ibuprofen and tolmetin, two other prostaglandin synthetase inhibitors, also inhibit the interaction of Fe⁺⁺ with arachidonic acid suggesting this may be a general mechanism for this type of drug.     

The role of iron in prostaglandin synthesis: Ferrous iron mediated oxidation of arachidonic acid

Arachidonic acid (AA) is the essential substrate for production of platelet endoperoxides and thromboxanes. Iron or heme is an essential cofactor for the peroxidase, lipoxygenase and cyclo-oxygenase enzymes involved in formation of these products. The present study has examined the direct interactions between iron and arachidonic acid. Iron caused the oxidation of AA into more polar products which could be detected by UV absorbtion at 232 nM or the thiobarbituric acid (TBA) reaction. High pressure liquid chromatography, chem-ionization and electron-impact mass spectrometry and nuclear magnetic resonance spectroscopy suggest that the major product was a hydroperoxide of AA. Ferrous iron (Fe⁺⁺) and oxygen were absolute requirements. Fe⁺⁺ was converted to the ferric iron (Fe⁺⁺⁺) state during oxidation of AA, but Fe⁺⁺⁺ could not substitute for Fe⁺⁺. No other enzymes, cofactors or ions were involved. Conversion of AA to a hydroperoxide by Fe⁺⁺ was inhibited by the antioxidant, 2, (3)-Tert-butyl-4-hydroxyanisole, the radical scavenger, nitroblue tetrazolium, and iron chelating agents, including EDTA, imidazole and dihydroxybenzoic acid. The reaction was not affected by superoxide dismutase, catalase or aspirin. These findings and preliminary studies of the Fe⁺⁺ induced oxidation product of AA as a substrate for prostaglandin synthesis and inhibitor of prostacyclin production indicate the critical role of Fe⁺⁺ in AA activation.     

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.     

Iron Autoxidation in Mops and Hepes Buffers

Iron autoxidation in Mops and Hepes buffers is characterized by a lag phase that becomes shorter with increasing FeCl₂ concentration and pH. During iron oxidation in these buffers a yellow colour develops in the solution. When the reaction is conducted in the presence of nitro blue tetrazolium (NBT), blue formazan is formed. Of the many OH' scavengers tested, mannitol and sorbitol are most effective in inhibiting Fe²⁺ oxidation, yellow colour development and NBT reduction. Some inhibition was also noted with catalase. The iron product of the oxidative reaction differs from Fe³⁺ in its absorption spectrum and its low reactivity with thiocyanate. Similar results are obtained when iron autoxidation is studied in unbuffered solutions brought to alkaline pH with NaOH. In phosphate buffer, no lag phase is evident and the absorption spectrum of the final solution is identical to that of Fe³⁺ in this buffer. The iron product reacts immediately with thiocyanate. When iron oxidation is conducted in the presence of NBT the formation of formazan is almost undetectable. Of the many compounds tested only catalase inhibits iron autoxidation in this buffer. The sequence of reactions leading to iron autoxidation in Good-type buffers¹ thus resembles that occurring in unbuffered solutions brought to alkaline pH with NaOH and greatly differs from that occurring in phosphate buffer. These results are in agreement with the observation that these buffers have very low affinity for iron.¹ The data presented define experimental conditions where Fe²⁺ is substantially stable for a considerable length of time in Mops buffer.     

Hydroxyl radical production from hydrogen peroxide and enzymatically generated paraquat radicals: Catalytic requirements and oxygen dependence

The ability of paraquat radicals (PQ^+.) generated by xanthine oxidase and glutathione reductase to give H₂O₂-dependent hydroxyl radical production was investigated. Under anaerobic conditions, paraquat radicals from each source caused chain oxidation of formate to CO₂, and oxidation of deoxyribose to thiobarbituric acid-reactive products that was inhibited by hydroxyl radical scavengers. This is in accordance with the following mechanism derived for radicals generated by γ-irradiation [H. C. Sutton and C. C. Winterbourn (1984) Arch. Biochem. Biophys.235, 106–115] PQ^+. + Fe³⁺ (chelate) → Fe²⁺ (chelate) + PQ⁺⁺ H₂O₂ + Fe²⁺ (chelate) → Fe³⁺ (chelate) + OH^? + OH.. Iron-(EDTA) and iron-(diethylenetriaminepentaacetic acid) (DTPA) were good catalysts of the reaction; iron complexed with desferrioxamine or transferrin was not. Extremely low concentrations of iron (0.03 μm) gave near-maximum yields of hydroxyl radicals. In the absence of added chelator, no formate oxidation occurred. Paraquat radicals generated from xanthine oxidase (but not by the other methods) caused H₂O₂-dependent deoxyribose oxidation. However, inhibition by scavengers was much less than expected for a reaction of hydroxyl radicals, and this deoxyribose oxidation with xanthine oxidase does not appear to be mediated by free hydroxyl radicals. With O₂ present, no hydroxyl radical production from H₂O₂ and paraquat radicals generated by radiation was detected. However, with paraquat radicals continuously generated by either enzyme, oxidation of both formate and deoxyribose was measured. Product yields decreased with increasing O₂ concentration and increased with increasing iron(DTPA). These results imply a major difference in reactivity between free and enzymatically generated paraquat radicals, and suggest that the latter could react as an enzyme-paraquat radical complex, for which the relative rate of reaction with Fe³⁺ (chelate) compared with O₂ is greater than is the case with free paraquat radicals.     

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.     

Chemical evolution 40. clay-mediated oxidation of diaminomaleonitrile

Summary The previously reported inhibition of the oligomerization of HCN by montmorillonite clays was investigated. The inhibition is due to the oxidation of diaminomaleonitrile (DAMN) by the Fe³⁺ in the clay lattice. Fe²⁺ and oxalic acid were shown to be the reaction products. From these reaction products and the previous report that two equivalents of HCN are formed per equivalent ofDAMN, it was established that diiminosuccinonitrile (DISN) is the initial reaction product, which is rapidly hydrolyzed to oxalic acid and HCN. The same oxidative transformations are effected by Fe³⁺ bound to Dowex 50, Fe³⁺ in solution and Ni(NH₃)₆ ²⁺. The rate of reaction of DAMN decreased in the order Fe³⁺ > Fe³⁺-Dowex > montmorillonite, indicating no catalytic role for the clay in the oxidation of DAMN. Little reaction of DAMN was observed with montmorillonite in which the bulk of the iron was in the Fe²⁺ oxidation state. The possible significance of these redox reactions to chemical evolution is discussed.For the previous papers in this series see Ferris JP, Alwis KW, Edelson EH, Mount N, Hagan Jr J (1980) Origin of Life Wolman Y (ed) Reidel, Dordrecht, p 125–128 Ferris JP, Edelson EH, Auyeung JM, Joshi PC (1981) J Mol Evol 17:69-77     

Dégradation du DNA par H2O2 en présence d'ions Cu++, Fe++ et Fe+++

The mechanism of degradation of calf thymus DNA by H₂O₂ in dark and light, and in the presence of either Cu⁺⁺, Fe⁺⁺, or Fe⁺⁺⁺ ions has been investigated by following the decrease of molecular weight M?_w by light scattering. Both in the dark and in light, the rate of degradation decreases in the following order: Cu⁺⁺>Fe⁺⁺>Fe⁺⁺⁺. In order to exploit quantitatively the variation of M?_w with time, we calculated the probability p(t) of rupture in a double stranded polymer as a function of the occurence at random of both breaks of the “first kind” (single hits) and of the “second kind” (double hits), when there are caused by any degrading agent. The value of p(t) can then be related to M?_w(t) for the present case of a randomly polydisperse sample of DNA molecules. In the dark, and in the presence of Cu⁺⁺ ions, a degradation of the first kind (which takes place through the simultaneous or successive splitting of both strands of DNA at the same level) is the only one so far observed. The number of degradation sites of the first kind is equivalent to the number of bound Cu⁺⁺ ions in inner sites of DNA. A model is set up to explain the successive breaks of the two strands of the DNA molecule through the formation of a complex (DNA site–Cu⁺⁺-H₂O₂) which exhibits peroxidative properties. The comparison of the degradation induced under these conditions in a native and a sonicated DNA, shows that the specific sites of attack of ultrasonic waves are not specific sites of H₂O₂ action in the presence of Cu⁺⁺ ions. In the dark and in the presence of Fe⁺⁺ or Fe⁺⁺⁺ ions, breaks of the first kind and second kind are superimposed, but the last are predominant. This is ascribed to the low binding of iron ions in inner sites of DNA under these conditions. A large increase in degradation rate of the second kind occurred in the presence of light (with or without added metallic ions and) is ascribed to the action of the free radicals HO^· (and HO₂^·) which arise from the photolysis of H₂O₂. These results are discussed in relation to those obtained by the action of ionizing radiations on aqueous solutions of DNA.     

Cation activation of desoxyribonuclease

The activation of desoxyribonuclease on desoxyribonucleate, known to occur with Mg⁺⁺ and Mn⁺⁺, has been shown to occur equally well with Co⁺⁺, to nearly the same extent with Fe⁺⁺, and to a lesser extent with Ca⁺⁺, Ba⁺⁺, Sr⁺⁺, Ni⁺⁺, Cd⁺⁺, and Zn⁺⁺. The conditions under which the optimal activation is revealed vary among these ions. Thus, Mg⁺⁺, Mn⁺⁺, and Co⁺⁺ may show marked activation under conditions in which Fe⁺⁺ is nearly ineffective. Since too high a concentration of an ion may be as ineffective as too little, concentration-activation curves were determined for each ion. Per micromole of nucleic acid phosphorus, the optimal effective amount of each ion in micromoles is as follows: Mg⁺⁺ 3, Mn⁺⁺ 3, Co⁺⁺ 3, Fe⁺⁺ 0.3, Ni⁺⁺ 0.3, Ba⁺⁺ 1.7, Ca⁺⁺ 3, Sr⁺⁺ 3, Zn⁺⁺ 0.3, and Cd⁺⁺ 0.3.The optimum pH for the activation with Mg⁺⁺, Co⁺⁺, and Ca⁺⁺ is about 6.5, that with Fe⁺⁺ is at 5.7, while Mn⁺⁺ shows two optima at pH 6.8 and 8.0.Experiments conducted in Pyrex and in quartz vessels showed the same results, and indicated that there was no activation of desoxy-ribonuclease in the absence of added salts.     

Possible role of a peroxidative system in melanin synthesis inVerticillium

Manometric tests demonstrated phenolase activity in potato and mushroom extracts but little in extracts from a microsclerotial isolate ofVerticillium albo-atrum. The purpurogallin test indicated the presence of peroxidase activity in theseVerticillium extracts. An assay for an enzyme system which produced dark pigment from catechol was developed. Mn⁺⁺ stimulated pigment synthesis about twice as much as Mg⁺⁺ or Ca⁺⁺. Other cations, Co⁺⁺, Ni⁺⁺, Zn⁺⁺, Cu⁺⁺ and Fe⁺⁺ had less effect. The cell-free enzyme system containing H₂O₂ and Mn⁺⁺ produced dark-colored products from catechol, dopa, andp-phenylenediamine. Pyrogallol yielded a bright yellow color. Chemicals which did not yield colored products as a result of enzyme action included aniline, ascorbic acid, chlorogenic acid,p-cresol, gallic acid, hydroquinone, phenol, phenylalanine, protocatechuic acid, resorcinol, shikimic acid, and tyrosine. In view of these results and the failure of others to demonstrate more than weak phenolase activity inVerticillium, we conclude that a peroxidation probably initiates most melanin synthesis inVerticillium.     

Interactions des ions métalliques avec le DNA. IV. Fixation de i'ion cuivrique sur le DNA

The binding of cupric ion (Cu⁺⁺) to DNA was followed by spectrophotometry, melting profiles, and hydrodynamic techniques, in 0. 1M NaClO₄ and at pH 5. 6. A small amount of Cu⁺⁺ is bound specifically to bases (about 1 Cu⁺⁺ per 20 nucleotides), in agreement with polarographic and EPR data. A preferential stabilization of G–C pairs and only a slight increase of the flexibility of the molecule were observed. In 5 × 10^?3M NaClO₄, a higher number of nonhomogeneous binding sites is found by spectrophotometry. It is concluded that at least two types of sites are available for Cu⁺⁺. The first one, where Cu⁺⁺ is chelating N₇ of purines to phosphate, is observed only at low ionic strength and destabilizes the double helix. The second exists mainly at 0, 1M or higher ionic strength. All the sites are identical and could be attributed to two successive guanine residues in the same strand. Similar behavior was found for other divalent cations, e. g., Fe⁺⁺, Mn⁺⁺, and Co⁺⁺.     

Kinetics of iron absorption by excised rice roots

Summary Studies on the rate of iron absorption by excised rice roots from solutions of different concentrations of FeSO₄ showed the presence of two patterns, one in the low (0.005–0.5 mM) and the other in the high (1–30 mM) concentration range. The presence of CaSO₄ or MnSO₄ at 0.5 mM enhanced Fe⁺⁺ absorption in the low concentration range, while CaSO₄ at 10 mM inhibited Fe absorption in the high concentration range in a competitive manner. Fe⁺⁺ absorption at both low and high concentrations was sensitive to metabolic inhibitors. The isotherm for Fe⁺⁺ absorption at O° exhibited an initial absorption shoulder in both low and high concentrations and was suggestive of a latent ion-transport capacity for Fe⁺⁺ in rice roots.     

Paraquat potentiates iron-induced microsomal lipid peroxidation: modulation by the diet lipid composition

SUMMARY

The study concerns the role of two combined factors—lipid composition of the microsomal membranes and the iron concentration in the incubation medium—in lipid peroxidation catalysed by paraquat (P⁺⁺). Rats were subjected to diets containing 5% lipids composed of either tripalmitin (T), peanut oil/rapeseed oil (v/v) (C) or fish oil (F). The level of polyunsaturated fatty acids in the microsomal membranes was higher in C and F than in T. The level of vitamin E was lowest in F. The activity of the system ‘Cyt P450-NADPH cyt c reductase’ increased in the order T<C<F. The iron concentrations initiating a basal NADPH-dependent lipid peroxidation have been established. p⁺⁺ potentiates this peroxidation due to additional reduction of Fe³⁺ by p^+., rather than by O₂^.- as is usually thought to occur. The sensitivity of the membranes to the potentiating effect of P^{+ +} is mainly determined by a high level of polyunsaturated fatty acids, but also by a low level of the antioxidant vitamin E.     

Lipid Peroxidation. Definition of Experimental Conditions for Selective Study of the Propagation and Termination Phases

To find experimental conditions to selectively study the propagation phase of lipoperoxidation we studied the lipoperoxidation, catalyzed by FeCl₂, of liposomes in a buffering condition where Fe²⁺ autoxidation and oxygen active species generation does not occur. Liposomes from egg yolk phosphatidylcholine. prepared by vortex mixing, do not oxidize Fe²⁺: on the contrary they oxidize Fe²⁺ when prepared by ultrasonic irradiation. Dimyristoyl phosphatidylcholine liposomes prepared by ultrasonic irradiation do not oxidize Fe²⁺. During sonication polyunsaturated fatty acid residues autoxidize and lipid hydroperoxides (LOOH) are generated. Only when LOOH are present in the liposimes Fe²⁺ oxidizes and its rate of oxidation depends on the amount of LOOH in the assay. The reaction results in the generation of both LOOH and thiobarbituric acid reactive material (TBAR): it is inhibited by butylated hydroxytoluene and has a acidic pH optimum; it is not inhibited by catalase and OH' scavengers. The reaction studied. thus, appears to be the chain branching and propagation phase of lipoperoxidation. When we studied the dependence of Fe²⁺ oxidation, LOOH and TBAR generation on FeCl₂ concentration, we observed that at high FeCl₂ concentrations the termination phase of lipoperoxidation was prevalent. Thus. by selecting the appropriate FeCl₂ concentration the proposed experimental system allows study of either the propagation or the termination phase of lipoperoxidation.     

Numbers of iron‐oxidizing bacteria and oxidation potential of sulfur and iron components in coal refuse amended with limestone and sewage sludge

Counts of acidophilic iron‐oxidizing bacteria, ratios of S₂O₃=—S/SO₄=—S and Fe⁺³/Fe⁺², and S₂O₃=—S oxidation potentials were examined over a two‐year period in coal refuse (acid gob) treated with limestone and/or sewage sludge. A non‐amended treatment was used as a control.

No significant difference in population counts of acidophilic iron‐oxidizing bacteria were observed between treatments in either year of the study. S₂O₃=—S/SO₄=—S and Fe⁺³/Fe⁺² ratios indicated active sulfur and iron oxidation suggesting that limestone and/or sewage sludge may be ineffective in suppressing pyrite oxidation. Under optimal conditions, S₂O₃=—S oxidation potentials (in vitro) showed a logarithmic increase in SO₄=—S formation for all four treatments over time. The final pH of the treatments following twenty days of perfusion ranged from 3.06 to 3.59.     

Studies on Proteinases from Gliocladium roseum

The alkaline proteinases of Gliocladium roseum (Link) Bainier were purified in crystalline forms by procedures of alcoholic precipitation, fuller’s earth- and acrinol-treatment, and isolated in two types. (Proteinases I and II). Both of these proteinases were homogeneous on zone electrophoresis with polyacrylamide gel (Gyanogum 41), and had the optimal pH values of 11 (Proteinase I) and 10 (Proteinase II), and the optimal temperature of 45°C.

The enzymatic reaction of proteinase I was remarkably promoted by Fe⁺⁺ and Co⁺⁺, and that of proteinase II was promoted by Fe⁺⁺, Go⁺⁺ and Ca⁺⁺, and both proteinases were protected from heat-inactivation by Ca⁺⁺ Proteinase II was activated remarkably by Cl^? under the existence of Fe⁺⁺, but proteinase I was unaffected by the anion.

The order of strength of proteolytic power of these proteinases and chymotrypsin on casein was as follows; proteinase I> proteinase II> chymotrypsin.     

Nuclear stains with soluble metachrome metal mordant dye lakes

Summary Following our study on the effect of deoxyribonucleic acid (DNA) extraction on nuclear staining with soluble metal mordant dye lakes covering 29 dye lakes we chose a series of lakes representing the three groups: (1) readily prevented by DNA removal, (2) weakened by DNA extraction but not prevented, (3) unaffected by DNA removal, for application of other endgroup blockade reactions. The lakes selected were alum and iron hematoxylins, iron alum and ferrous sulfate galleins, Fe²⁺ gallo blue E, iron alum celestin blue B, iron alum fluorone black and the phenocyanin TC-FeSO₄ sequence. Azure A with and without an eosin B neutral stain, was used as a simple cationic (and anionic) dye control.Methylation was less effective than with simple cationic dyes, but did weaken celestin blue, gallo blue E and phenocyanin Fe²⁺ nuclear stains. These dyes also demonstrate other acid groups: acid mucins, cartilage matrix, mast cells, central nervous corpora amylacea and artificially introduced carboxyl, sulfuric and sulfonic acid groups. Alum hematoxylin stained cartilage weakly and demonstrated sulfation and sulfonation sites. The iron galleins, iron fluorone black and acid iron hematoxylin do not. A pH 4 iron alum hematoxylin gave no staining of these sites; an alum hematoxylin acidified with 1% 12 N HCl gave weaker results.Deamination prevented eosin and orange G counterstains but did not impair nuclear stains with any of the mordant dye lakes. The simple acetylations likewise did not alter mordant dye nuclear staining, the Skraup reagent gave its usual sulfation effect on other tissue elements, but did not alter nuclear stains by mordant dyes.The mordant dyes do not bind to periodic acid engendered aldehyde sites and p-toluidine/acetic acid and borohydride aldehyde blockades did not alter mordant dye lake nuclear staining. Nitration by tetranitromethane, which blocks azo coupling of tyrosine residues, did not alter nuclear staining by the mordant dye lakes¹. Benzil at pH 13, which prevents the -naphthoquinone-4-Na sulfonate (NQS) arginine reaction and the Fullmer reaction of basic nucleoprotein, did not affect iron gallein, iron or alum hematoxylin stains of nuclei or lingual keratohyalin.Assisted by Contract Nol-CB-43912 National Cancer Institute     

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.     

Acceptor side effects on the electron transfer at cryogenic temperatures in intact photosystem II

In intact PSII, both the secondary electron donor (Tyr_Z) and side-path electron donors (Car/Chl_Z/Cyt_b559) can be oxidized by P₆₈₀⁺ at cryogenic temperatures. In this paper, the effects of acceptor side, especially the redox state of the non-heme iron, on the donor side electron transfer induced by visible light at cryogenic temperatures were studied by EPR spectroscopy. We found that the formation and decay of the S₁Tyr_Z EPR signal were independent of the treatment of K₃Fe(CN)₆, whereas formation and decay of the Car⁺/Chl_Z⁺ EPR signal correlated with the reduction and recovery of the Fe³⁺ EPR signal of the non-heme iron in K₃Fe(CN)₆ pre-treated PSII, respectively. Based on the observed correlation between Car/Chl_Z oxidation and Fe³⁺ reduction, the oxidation of non-heme iron by K₃Fe(CN)₆ at 0 °C was quantified, which showed that around 50-60% fractions of the reaction centers gave rise to the Fe³⁺ EPR signal. In addition, we found that the presence of phenyl-p-benzoquinone significantly enhanced the yield of Tyr_Z oxidation. These results indicate that the electron transfer at the donor side can be significantly modified by changes at the acceptor side, and indicate that two types of reaction centers are present in intact PSII, namely, one contains unoxidizable non-heme iron and another one contains oxidizable non-heme iron. Tyr_Z oxidation and side-path reaction occur separately in these two types of reaction centers, instead of competition with each other in the same reaction centers. In addition, our results show that the non-heme iron has different properties in active and inactive PSII. The oxidation of non-heme iron by K₃Fe(CN)₆ takes place only in inactive PSII, which implies that the Fe³⁺ state is probably not the intermediate species for the turnover of quinone reduction.     

Further Studies on the Roles of Sodium and Potassium in the Generation of the Electro-Olfactogram : Effects of mono-, di-, and trivalent cations

In the negative EOG-generating process a cation which can substitute for Na⁺ was sought among the monovalent ions, Li⁺, Rb⁺, Cs⁺, NH₄⁺, and TEA⁺, the divalent ions, Mg⁺⁺, Ca⁺⁺, Sr⁺⁺, Ba⁺⁺, Zn⁺⁺, Cd⁺⁺, Mn⁺⁺, Co⁺⁺, and Ni⁺⁺, and the trivalent ions, Al⁺⁺⁺ and Fe⁺⁺⁺. In Ringer solutions in which Na⁺ was replaced by one of these cations the negative EOG's decreased in amplitude and could not maintain the original amplitudes. In K⁺-Ringer solution in which Na⁺ was replaced by K⁺, the negative EOG's reversed their polarity. Recovery of these reversed potentials was examined in modified Ringer solutions in which Na⁺ was replaced by one of the above cations. Complete recovery was found only in the normal Ringer solution. Thus, it was clarified that Na⁺ plays an irreplaceable role in the generation of the negative EOG's. The sieve hypothesis which was valid for the positive EOG-generating membrane or IPSP was not found applicable in any form to the negative EOG-generating membrane. The reversal of the negative EOG's found in K⁺- , Rb⁺- , and Ba⁺⁺-Ringer solutions was attributed to the exit of the internal K⁺. It is, however, not known whether or not Cl^- permeability increases in these Na⁺-free solutions and contributes to the generation of the reversed EOG's.