Solvent Hydrogen Isotope Effects Research Articles

Proton Availability at the Air/Water Interface

The acidity of the water surface sensed by a colliding gas is determined in experiments in which the protonation of gaseous trimethylamine (TMA) on aqueous microjets is monitored by online electrospray mass spectrometry as a function of the pH of the bulk liquid (pH_(BLK)). TMAH^+ signal intensities describe a titration curve whose equivalence point at pH_(BLK) 3.8 is dramatically smaller than the acidity constant of trimethylammonium in bulk solution, pK_A(TMAH^+) = 9.8. Notably, the degree of TMA protonation above pH_(BLK) 4 is enhanced hundred-fold by submillimolar LiCl or NaCl and weakly inhibited at larger concentrations. Protonation enhancements are associated with the onset of significant direct kinetic solvent hydrogen isotope effects. Since TMA(g) can be protonated by H_2O itself only upon extensive solvent participation, we infer that H3O^+ emerges at the surface of neat water below pH_(BLK) 4.

Solvent Hydrogen Isotope Effects in Catalysis by Carbonic Anhydrase: Proton Transfer Through Intervening Water Molecules

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Proton transfer in a Thr200His mutant of human carbonic anhydrase II

Human carbonic anhydrase II (HCA II) has a histidine at position 64 (His64) that donates a proton to the zinc-bound hydroxide in catalysis of the dehydration of bicarbonate. To examine the effect of the histidine location on proton shuttling, His64 was replaced with Ala and Thr200 replaced with histidine (H64A-T200H HCAII), effectively relocating the proton shuttle residue 2 A closer to the zinc-bound hydroxide compared to wild type HCA II. The crystal structure of H64A-T200H HCA II at 1.8 A resolution shows the side chain of His200 directly hydrogen-bonded with the zinc-bound solvent. Different proton transfer processes were observed at pH 6 and at pH 8 during the catalytic hydration-dehydration cycle, measured by mass spectrometry as the depletion of 18O from C18O2 by H64A-T200H HCA II. The process at pH 6.0 is attributed to proton transfer between the side chain of His200 and the zinc-bound hydroxide, in analogy with proton transfer involving His64 in wild-type HCA II. At pH 8.0 it is attributed to proton transfer between bicarbonate and the zinc-bound hydroxide, as supported by the dependence of the rate of proton transfer on bicarbonate concentration and on solvent hydrogen isotope effects. This study establishes that a histidine directly hydrogen-bonded to the zinc-bound hydroxide, can adopt the correct distance geometry to support proton transfer

Activation of the Proton Transfer Pathway in Catalysis by Iron Superoxide Dismutase

Catalysis by Escherichia coli and Porphyromonas gingivalis iron superoxide dismutase was activated by addition of primary amines, as measured by pulse radiolysis and stopped-flow spectrophotometry. This activation was saturable for most amines investigated, and a free energy plot of the apparent second-order rate constant of activation was linear as a function of the pK(a) of the amine, indicating activation by proton transfer. Amines provide an alternate rather than the only pathway for proton transfer, and catalysis was appreciable in the absence of amines. Solvent hydrogen isotope effects were near unity for amine activation, which is consistent with rate-contributing proton transfer if the pK(a) of the proton acceptor on the enzyme is not in the region of the pK(a) values of the amines studied, from 7.8 to 10.6. The activation of catalysis by these amines was uncompetitive with respect to superoxide, interpreted as proton transfer in a ternary complex of amine with the enzyme-bound peroxide dianion.

6] Catalytic pathway of manganese superoxide dismutase by direct observation of superoxide

Measurement of catalysis by MnSOD using direct observation of the UV absorbance of superoxide allows determination of steady-state catalytic constants. Stabilizing superoxide in aprotic solvents such as dimethyl sulfoxide permits the use of stopped-flow spectrophotometry, although significant information is lost in the 2- to 4-msec mixing time; generating superoxide by pulse radiolysis requires no mixing time. Studies show that kcat/Km for the decay of superoxide catalyzed by MnSOD proceeds at diffusion control. Investigations using solvent hydrogen isotope effects and enhancement of catalysis by exogenous proton donors show that kcat near 10(4) sec-1 contains a significant contribution from proton transfer steps. The active site of MnSOD is dominated by a hydrogen bond network comprising the manganese-bound aqueous ligand, the side chains of four residues (Gln-143, Tyr-34, His-30, and Tyr-166 from an adjacent subunit), as well as other water molecules. Interrupting this hydrogen bond network by conservative replacement of residues 30, 34, and 166 causes a 10- to 40-fold decrease in maximal velocity, interpreted as an effect on proton transport to the active site, with smaller effects on kcat/Km. Replacement of Gln-143 causes a much greater decrease in catalytic activity, by two to three orders of magnitude, and causes significant changes to the redox potential as well. During catalysis, MnSOD is inhibited by a peroxide complex of the metal in the active site, different from the inhibition of FeSOD and Cu,ZnSOD by Fenton chemistry. Site-specific mutagenesis of active-site residues alters the extent of product inhibition of MnSOD as well, indicating that this is not only a property of the metal. The replacement of Trp-161 with phenylalanine results in a variant that is completely blocked in catalysis by product inhibition.

Kinetic analysis of product inhibition in human manganese superoxide dismutase.

Manganese superoxide dismutase (MnSOD) cycles between the Mn(II) and Mn(III) states during the catalyzed disproportionation of O(2)(*-), a catalysis that is limited at micromolar levels of superoxide by a peroxide-inhibited complex with the metal. We have investigated the role in catalysis and inhibition of the conserved residue Trp161 which forms a hydrophobic side of the active site cavity of MnSOD. Crystal structures of mutants of human MnSOD in which Trp161 was replaced with Ala or Phe showed significant conformational changes on adjacent residues near the active site, particularly Gln143 and Tyr34 which in wild-type MnSOD participate in a hydrogen bond network believed to support proton transfer during catalysis. Using pulse radiolysis and observing the UV absorbance of superoxide, we have determined rate constants for the catalytic dismutation of superoxide. In addition, the rates of formation and dissociation of the product-inhibited complex of these mutants were determined by direct observation of the characteristic visible absorption of the oxidized and inhibited states. Catalysis by W161A and W161F MnSOD was associated with a decrease of at least 100-fold in the catalytic rate of reduction of superoxide, which then promotes a competing pathway leading to product inhibition. The structural changes caused by the mutations at position 161 led to small changes, at most a 6-fold decrease, in the rate constant for formation of the inhibited complex. Solvent hydrogen isotope effects support a mechanism in which formation of this complex, presumably the peroxide dianion bound to the manganese, involves no rate-contributing proton transfer; however, the dissociation of the complex requires proton transfer to generate HO(2)(-) or H2O2.

Bicarbonate as a proton donor in catalysis by Zn(II)- and Co(II)-containing carbonic anhydrases.

Catalysis of (18)O exchange between CO(2) and water catalyzed by a Co(II)-substituted mutant of human carbonic anhydrase II is analyzed to show the rate of release of H(2)(18)O from the active site. This rate, measured by mass spectrometry, is dependent on proton transfer to the metal-bound (18)O-labeled hydroxide, and was observed in a site-specific mutant of carbonic anhydrase II in which a prominent proton shuttle residue His64 was replaced by alanine, which does not support proton transport. Upon increasing the concentration of bicarbonate, the rate of release of H(2)(18)O increased in a saturable manner to a maximum of 4 x 10(5) s(-)(1), consistent with proton transfer from bicarbonate to the Co(II)-bound hydroxide. The same mutant of carbonic anhydrase containing Zn(II) had the rate of release of H(2)(18)O smaller by 10-fold, but rate of interconversion of CO(2) and HCO(3)(-) about the same as the Co(II)-containing enzyme. These data as well as solvent hydrogen isotope effects suggest that the bicarbonate transferring the proton is bound to the cobalt in the enzyme. The enhancement of (18)O exchange caused by increasing bicarbonate concentration during catalysis by the Zn(II)-containing carbonic anhydrase from the archaeon Methanosarcina thermophila suggests that a very similar mechanism for proton donation by bicarbonate occurs with this wild-type enzyme.

Structural and kinetic characterization of an archaeal beta-class carbonic anhydrase.

The beta-class carbonic anhydrase from the archaeon Methanobacterium thermoautotrophicum (Cab) was structurally and kinetically characterized. Analytical ultracentrifugation experiments show that Cab is a tetramer. Circular dichroism studies of Cab and the Spinacia oleracea (spinach) beta-class carbonic anhydrase indicate that the secondary structure of the beta-class enzymes is predominantly alpha-helical, unlike that of the alpha- or gamma-class enzymes. Extended X-ray absorption fine structure results indicate the active zinc site of Cab is coordinated by two sulfur and two O/N ligands, with the possibility that one of the O/N ligands is derived from histidine and the other from water. Both the steady-state parameters k(cat) and k(cat)/K(m) for CO(2) hydration are pH dependent. The steady-state parameter k(cat) is buffer-dependent in a saturable manner at both pH 8.5 and 6.5, and the analysis suggested a ping-pong mechanism in which buffer is the second substrate. At saturating buffer conditions and pH 8.5, k(cat) is 2.1-fold higher in H(2)O than in D(2)O, consistent with an intramolecular proton transfer step being rate contributing. The steady-state parameter k(cat)/K(m) is not dependent on buffer, and no solvent hydrogen isotope effect was observed. The results suggest a zinc hydroxide mechanism for Cab. The overall results indicate that prokaryotic beta-class carbonic anhydrases have fundamental characteristics similar to the eukaryotic beta-class enzymes and firmly establish that the alpha-, beta-, and gamma-classes are convergently evolved enzymes that, although structurally distinct, are functionally equivalent.

Kinetic and spectroscopic characterization of the gamma-carbonic anhydrase from the methanoarchaeon Methanosarcina thermophila.

The zinc and cobalt forms of the prototypic gamma-carbonic anhydrase from Methanosarcina thermophila were characterized by extended X-ray absorption fine structure (EXAFS) and the kinetics were investigated using steady-state spectrophotometric and (18)O exchange equilibrium assays. EXAFS results indicate that cobalt isomorphously replaces zinc and that the metals coordinate three histidines and two or three water molecules. The efficiency of either Zn-Cam or Co-Cam for CO(2) hydration (k(cat)/K(m)) was severalfold greater than HCO(3-) dehydration at physiological pH values, a result consistent with the proposed physiological function for Cam during growth on acetate. For both Zn- and Co-Cam, the steady-state parameter k(cat) for CO(2) hydration was pH-dependent with a pK(a) of 6.5-6.8, whereas k(cat)/K(m) was dependent on two ionizations with pK(a) values of 6.7-6.9 and 8.2-8.4. The (18)O exchange assay also identified two ionizable groups in the pH profile of k(cat)/K(m) with apparent pK(a) values of 6.0 and 8.1. The steady-state parameter k(cat) (CO(2) hydration) is buffer-dependent in a saturable manner at pH 8. 2, and the kinetic analysis suggested a ping-pong mechanism in which buffer is the second substrate. The calculated rate constant for intermolecular proton transfer is 3 x 10(7) M(-1) s(-1). At saturating buffer concentrations and pH 8.5, k(cat) is 2.6-fold higher in H(2)O than in D(2)O, suggesting that an intramolecular proton transfer step is at least partially rate-determining. At high pH (pH > 8), k(cat)/K(m) is not dependent on buffer and no solvent hydrogen isotope effect was observed, consistent with a zinc hydroxide mechanism. Therefore, at high pH the catalytic mechanism of Cam appears to resemble that of human CAII, despite significant structural differences in the active sites of these two unrelated enzymes.

Probing the active site of human manganese superoxide dismutase: the role of glutamine 143.

Structural and biochemical characterization of the nonliganding residue glutamine 143 near the manganese of human Mn superoxide dismutase (hMnSOD), a homotetramer of 22 kDa, reveals a functional role for this residue. In the wild-type protein, the side-chain amide group of Gln 143 is about 5 A from the metal and is hydrogen-bonded to Tyr 34, which is a second prominent side chain adjacent to the metal. We have prepared the site-specific mutant of hMnSOD with the conservative replacement of Gln 143 --> Asn (Q143N). The crystal structure of Q143N shows that the side-chain amide nitrogen of residue 143 is 1.7 A more distant from the manganese than in the wild-type enzyme. The Tyr 34 side-chain hydroxyl in Q143N is also moved to become 0.6 A more distant from the metal due to an additional water molecule. Differential scanning calorimetry showed that Q143N is slightly more stable than the wild-type enzyme with Tm for the main unfolding transition increased by 2 degrees C to 90.7 degrees C. Pulse radiolysis and stopped-flow spectrophotometry reveal that unlike wild-type hMnSOD, which is strongly inhibited by peroxide, Q143N MnSOD exhibits no product inhibition even at concentrations of O2. - in the millimolar range, and its catalysis follows Michaelis kinetics with no evidence of cooperativity. However, the overall catalytic activity of this mutant was decreased 2-3 orders of magnitude compared with the wild-type MnSOD, which can account for its lack of product inhibition. Q143N MnSOD lacked the visible absorption spectrum typical of wild-type Mn(III)SOD. Also, unlike the wild-type Mn(III)SOD, which is electron paramagnetic resonance (EPR) silent, Q143N MnSOD has a complex EPR spectrum with many resonances in the region below 2250 G. We conclude that the Gln 143 --> Asn mutation has increased the reduction potential of manganese to stabilize Mn(II), indicating that Gln 143 has a substantial role in maintaining a reduction potential favorable for the oxidation and reduction cycles in the catalytic disproportionation of superoxide. A solvent hydrogen isotope effect near 2 for kcat in catalysis by Q143N hMnSOD indicates rate-contributing proton transfers to form product hydroperoxide anion or hydrogen peroxide. The data demonstrate a prominent role for Gln 143 in maintaining the microenvironment of the manganese and in efficient catalysis of superoxide dismutation to oxygen and hydrogen peroxide.

Solvent hydrogen isotope effects and anion inhibition of CO2 hydration catalysed by carbonic anhydrase from Pisum sativum.

Chloroplast carbonic anhydrase from Pisum sativum has been studied to elucidate the catalytic mechanism and to test if the mechanism proposed for human carbonic anhydrase II is also valid for pea carbonic anhydrase. The catalytic activity was found to depend on the chemical nature of the buffer. Barbital buffer gives the highest turnover number at infinite buffer concentration and the lowest Km value with respect to the buffer, while the kinetic parameters obtained in the imidazole-type buffer, 1-methylimidazole, do not differ from those obtained using the biological-type buffer Mops. The anion inhibition of CO2 hydration was investigated using SCN- at pH 6-9. The binding of the anion was found to be pH dependent with the strongest interaction at low pH. We obtained an uncompetitive inhibition pattern at high pH and noncompetitive inhibition patterns at pH 7 and low pH. The catalytic mechanism was further tested by measurements of the solvent hydrogen isotope effects on the kinetic parameters for CO2 hydration. The observed effects were comparatively small with a kcat value of approximately 2 irrespective of the pH. The effect on kcat/Km and on Km changes when going from high pH to pH 7 and low pH. At high pH, the solvent isotope effect in Km is at least 3, giving a value below 1 for kcat/Km, while at pH 7 and low pH the major effect is found in kcat/Km with values of 2.6 and 2.9. The dependence of the CO2-hydration activity on the buffer concentration is in agreement with a ping-pong mechanism with buffer acting as a second substrate. This is analogous to the behaviour of human carbonic anhydrase II. The inhibition patterns and the observed isotope effects at high pH can also be explained within the framework of the catalytic mechanism for human carbonic anhydrase II, with a rate-determining and buffer-dependent part. The results are consistent with a mechanism involving a proton transfer that contributes to rate limitation. However, the isotope effects found at pH 7 and low pH indicate that some part of the mechanism has changed. Moreover, we cannot decide whether the mechanism for pea carbonic anhydrase involves an internal proton-shuttle group, or if the buffer molecule acts in a direct proton transfer from the zinc-coordinated water.

Comparison of intra- and intermolecular proton transfer in human carbonic anhydrase II.

The catalysis of the hydration of CO2 by human carbonic anhydrase II (HCA II) includes the transfer of a proton from zinc-bound water to histidine 64 utilizing a network of intervening hydrogen-bonded water molecules, then the proton is transferred to buffer in solution. We used stopped-flow spectrophotometry and 18O exchange between CO2 and water measured by mass spectrometry to compare catalytic constants dependent on proton transfer in HCA II and in the mutant H64A HCA II containing the replacement His64-->Ala. Maximal velocities and oxygen-18 exchange catalyzed by H64A HCA II showed that nearly all of the proton transfer with this mutant proceeded through the imidazole buffer. The following parameters were very similar or identical in catalysis by H64A HCA II compared with catalysis by wild-type HCA II both in the presence of large concentrations of imidazole (100 mM): the maximal rate of initial velocity and of exchange of 18O between CO2 and water, solvent hydrogen isotope effects on the maximal velocity, and the dependence of these isotope effects on the atom fraction of deuterium in solvent water. These results indicate that the proton transfer involving the zinc-bound water in catalysis is not significantly affected by the difference between the mobility of the free imidazole buffer and the side chain of His 64. Moreover, data for both the wild-type and mutant enzymes are consistent with proton transfer through intervening hydrogen-bonded water bridges in the active sites. These features of the proton transfer are discussed in terms of a model in which the first proton transfer from the zinc-bound water to an adjacent water is rate limiting.

A comparison of the kinetic properties of native bovine muscle carbonic anhydrase and an activated derivative with modified thiol groups

Steady-state and equilibrium kinetic properties of native bovine carbonic anhydrase III (carbonate hydrolyase, EC 4.2.1.1) and a derivative modified with methyl methanethiosulfonate were investigated. The modified enzyme has a markedly increased CO 2 hydration activity compared to the native form with a 3-times higher value of k cat and a 6–10-times higher value of k cat K m . Qualitatively, the activated enzyme shows the same kinetic behavior as native isoenzyme III. This is reflected in similar pH dependences of the kinetic parameters for CO 2 hydration, similar solvent hydrogen isotope effects on these parameters, similar deviations from Michaelis-Menten kinetics for the HCO 3 − dehydration reaction, and similar behavior of the kinetics of CO 2 HCO 3 − exchange at chemical equilibrium as measured by a 13C-NMR magnetization transfer technique. It is concluded that the conversion of -SH groups to -S-S-CH 3 moieties does not change the catalytic mechanism, but leads to an increased rate of CO 2 HCO 3 − interconversion as well as to an increased rate of proton transfer between the active site and the reaction medium.

Oxidation in H 2O and D 2O of 6-ethyl-5H-dibenz( c,e)azepine and 1-methylnicotinamide by aldehyde oxidase from rabbit liver

We report the solvent hydrogen isotope effects associated with the oxidation of 6-ethyl-5H-dibenz( c,e)azepine (6-ED) and 1-methylnicotinamide (1-MN) catalyzed by aldehyde oxidase from rabbit liver using two assay methods. The first uses 2,6-dichlorophenolindophenol (DCI) as electron acceptor in an indirect assay in which the bleaching of DCI is measured as the substrate is oxidized. The second uses molecular oxygen as electron acceptor in a direct assay in which the oxidation of 1-MN to its pyridones is accompanied by an increase in absorbance at 300 nm and the oxidation of 6-ED to its lactam product is accompanied by a decrease in absorbance at 335 nm. We have found a solvent hydrogen isotope effect close to unity in the turnover number for each substrate and for each assay method. The solvent hydrogen isotope effects on k cat K m ranged from 0.4 to 1.1. We conclude that changes in bonding of hydrogen in solvent water, including hydrolysis of or general base attack on an enzyme-intermediate complex, do not play a rate-contributing role in the maximal velocity of oxidation of 1-MN and 6-ED catalyzed by aldehyde oxidase from rabbit liver.

Solvent hydrogen isotope effects on the catalysis of CO 2 hydration by three isozymes of mammalian carbonic anhydrase

The exchange of 18O between CO 2 and H 2O catalyzed by three isozymes of mammalian carbonic anhydrase has been used to determine the rate constants for two steps in the catalytic pathway. That for the inter-conversion of CO 2 and HCO 3 − at chemical equilibrium has a solvent hydrogen isotope effect of unity for all three isozymes indicating no rate-contributing proton transfer steps. That for the release of 18O from the enzyme has a solvent hydrogen isotope effect between 2.4 and 8.0 for these three isozymes indicating a change in bonding to hydrogen accompanying this process in each isozyme.

The rate of exchange of water between the active site of carbonic anhydrase and solvent

In the dehydration of HCO − 3 to form CO 2, carbonic anhydrase catalyzes the removal of an oxygen from substrate. Using an 18O labeling technique, we have determined the rate at which this oxygen is released from the enzyme and appears in solvent as H 18 2O [1]. In this technique, the isotopic content of CO 2 in solution is measured with a mass spectrometer From the rate of depletion of 18O in CO 2 and from the rate of exchange of 18O between 12C- and 13C-containing species of CO 2, the rate of release from the enzyme of substrate oxygen is calculated. This is described by the rate constant k H 2O : rate of release = k H 2O [E tot]. Although there is no proof from this technique that the site from which oxygen is released is the metal, such an interpretation is the most consistent with current ideas of the mechanism and the metal as the binding site of HCO − 3 [2]. We have observed k H 2O in the absence of buffer for human carbonic anhydrases I and II obtained from red cells and from cat carbonic anhydrase III obtained from the skeletal muscle of the hindlimb. In the range of pH from 5.7 to 8.2, k H 2O = 1.5 × 10 3 sec −1 for isozyme III and is independent of pH. For isozyme I, k H 2O = 3 × 10 4 sec −1, and is independent of pH from 5.7 to 7.5; data at higher pH are too uncertain to evaluate. In both of these cases the solvent hydrogen isotope effect, k H 2O /k D 2O , is 2.5 ± 20%. In contrast, we have observed a strong pH dependence of k H 2O for isozyme II which reaches a maximum plateau of 5 × 10 5 sec −1 at pH 6.6 and decreases as pH is increased. The solvent hydrogen isotope effect at this maximum plateau is k H 2O / k D 2O = 8.0 ± 10%. We interpret the data for isozyme II to be consistent with an itramolecular proton transfer as the step which determines the rate of oxygen release from the active site. This proton transfer occurs with a rate constant of 10 6 sec −1 and is likely the same step that determines the steady-state turnover rate. On the other hand, the pH independence of k H 2 O for isozyme III indicates no rate-limiting proton transfer for oxygen release with k H 2O /k D 2O determined by secondary isotope effects or solvation changes. The case for isozyme I is less certain because of the smaller pH range of observation: but isozyme I clearly behaves in a manner more similar to isozyme III than to isozyme II.

Transition-state structure in the yeast alcohol dehydrogenase reaction: the magnitude of solvent and alpha-secondary hydrogen isotope effects.

Solvent and alpha-secondary isotope effects have been measured in the yeast alcohol dehydrogenase reaction, under conditions of a rate-limiting transfer of hydrogen between coenzyme and substrate. Determination of catalytic constants (at saturating concentrations of substrate and coenzyme) in H2O and D2O as a function of pH(D) has allowed the separation of solvent effects on pKa from kcat: delta pKa = pKD--pKH = 0.02--0.21, kH2O/kD2O = 1.20 +/- 0.09 in the direction of p-methoxybenzyl alcohol oxidation, and kH2O/kD2O = 0.50 +/- 0.05 and 0.58 +/- 0.06 for p-methoxybenzaldehyde reducation by NADH and [4-2H]NADH. The small effect of D2O on pKa, which contrasts with the common observation that delta pKa congruent to 0.4--0.6, is tentatively assigned to ionization of an active-site ZnOH2. The near absence of an isotope effect on kcat in the direction of alcohol oxidation rules out a mechanism involving concerted catalysis by an active-site base of hydride transfer. In the direction of aldehyde reduction, the observation of inverse isotope effects on kcat is concluded to reflect displacement of zinc-bound water by substrate to form an inner-sphere complex, subsequent to the E.S complex. Equilibrium alpha-secondary isotope effects, measured as a frame of reference for kinetic values, indicate KH/KT = 1.33 +/- 0.05 and 1.34 +/- 0.09 for the oxidation of [1(S)-3H]benzyl alcohol and p-methoxy[1(S)-3H]benzyl alcohol, respectively. Kinetic alpha-secondary isotope effects are within experimental error of equilibrium values, kH/kT = 1.34 +/- 0.07 and 1.38 +/- 0.02 for [1(S)-3H]benzyl alcohol and p-methoxy[1(S)-3H]benzyl alcohol oxidation, respectively. The near identity of kinetic and equilibrium alpha-secondary isotope effects in the direction of alcohol oxidation implicates a transition-state structure which resembles aldehyde with regard to bond hybridization properties. This result contrasts sharply with previously reported structure--reactivity correlations, which implicate a transition-state structure resembling alcohol with regard to charge properties. The significance of these findings to the mechanism of NAD(P)H-dependent redox reactions is discussed.

The kinetics and mechanism of the protodeboronation of ferroceneboronic acid in moderately concentrated sulfuric acid

Ferroceneboronic acid has been characterized by its UV and NMR spectrum and its dissociation constant in water/ethanol solvents has been determined. The kinetics of protodeboronation have been studied in the same solvents containing moderate concentrations of sulfuric acid; the H 0 acidity function has been evaluated throughout the range of the reaction media used. The log of the rate of reaction of ferroceneboronic acid depends linearly with unit slope on H 0. The solvent hydrogen isotope effect, the temperature dependence and the nature of acid catalysis have also been investigated. The reaction probably proceeds by an A- S E2-type mechanism.

Substrate and solvent hydrogen isotope effects in the pyridine- and 2,6-lutidine-catalysed iodination of diethyl ketone (pentan-3-one)

The relative rates of base-catalysed iodination of pentan-3-one and [2,2,4,4-2H4]pentan-3-one are 4·0 : 1 for pyridine catalysis and 6·8 : 1 for 2,6-lutidine catalysis in ordinary water at 25°. The exaltation of the isotope effect for the sterically hindered base parallels previous observations of hydrogen isotope effects with nitroalkanes and shows that it is confined neither to one class of substrates nor to proton transfers between bases of similar strength.