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1 creased, indicating preferential sorption to chlorite.
2 tite and 0.15 mmol/g ( approximately 20%) in chlorite.
3 e surface U(VI) species on quartz and two on chlorite.
4 ain highly active in subsequent additions of chlorite.
5 rnovers with peroxide and <10 turnovers with chlorite.
6 ich is formed in situ by reduction of sodium chlorite.
7 nsistent with dehydration of antigorite than chlorite.
8 eact by electron transfer and form above 80% chlorite.
9 inside cells in response to externally added chlorite.
10 0% of the total U) and to a lesser extent to chlorite (30-40% of the total U).
11 chanism and specificity of the reaction with chlorite and alternate oxidants were investigated.
12 ent step for the overall reaction, producing chlorite and an intermediate that further forms chlorate
13 sproportionation with equimolar formation of chlorite and chlorate, (2) reaction to chlorite and oxyg
14 NOM) significantly enhanced the formation of chlorite and decreased the ClO2 disproportionation in th
15 ralogy with the identification of kaolinite, chlorite and illite or muscovite, and a new class of hyd
16  the upper limit of stability of the mineral chlorite and in particular, that the arc fronts lie dire
17 on of chlorite and chlorate, (2) reaction to chlorite and oxygen, and (3) oxidation of a metal in a r
18                Instead, minor phases such as chlorite and prehnite control the Eu(III) distribution,
19        These concentrations of the inhibitor chlorite and the activator iodide are shown in the form
20 eading to the concentration of the inhibitor chlorite and the activator iodide, respectively.
21 icrobial reduction of Fe(III) in biotite and chlorite and the role that this has in enhancing mineral
22 pO2, and U(IV) formed nanoparticulate UO2 in chlorite and was associated with silica in biotite.
23 esented that successfully determines iodate, chlorite, and bromate in drinking water at practical qua
24 ibition, MFP is synergistic with nitrite and chlorite, and could enhance the efficacy of nitrate or p
25 I intermediate via oxygen atom transfer from chlorite, and subsequent recombination of the resulting
26 scence quenching by both structural Fe/Cr in chlorite, and trace amounts of solubilized and reprecipi
27 ronite and saponite are the most common, but chlorites are also present in some locations.
28 xed-layer chlorite/smectite, corrensite, and chlorite) are the dominant clays through the lower 80 m
29                             Cld does not use chlorite as an oxidant for oxygen atom transfer and halo
30 d oxidation of benzylic centers using sodium chlorite as the stoichiometric oxidant is reported.
31 te, quartz, hematite, anatase, goethite, and chlorite at varying degrees was observed in the pedons d
32 ions, the addition of bioreduced biotite and chlorite caused removal of Cr(VI) from solution, and sur
33  the possible ClO2 loss and the formation of chlorite/chlorate should be carefully considered in drin
34 -O bond forming enzyme that transforms toxic chlorite (ClO(2)(-)) into innocuous chloride and molecul
35 lorite O(2)-lyase (Cld) enzymes that convert chlorite (ClO(2)(-)) into molecular oxygen (O(2)) and ch
36 ne used to generate ClO(2) via reaction with chlorite (ClO(2)(-)) or chlorine that forms when ClO(2)
37 FAC) could form as another byproduct next to chlorite (ClO(2)(-)).
38     The steady-state profile for the rate of chlorite decomposition is characterized by these same pK
39 tified the terminal reductase ClrABC and the chlorite detoxifying enzyme Cld.
40                                              Chlorite dismutase (Cld) is a heme b-dependent, O-O bond
41                                              Chlorite dismutase carries out the heme-catalyzed decomp
42                                              Chlorite dismutase catalyzes O(2) release from chlorite
43                                          The chlorite dismutase family of hemoproteins received its n
44 ing affinities, and steady-state kinetics of chlorite dismutase from Dechloromonas aromatica were exa
45 ng O2 in situ from chlorite using the enzyme chlorite dismutase to prepare X at ~2.0 mM, more than 2.
46 a beta-sheet motif typical for DyPs and Cld (chlorite dismutase)-related structures and includes the
47                                These include chlorite dismutase, arsenate reductase, V-type ATPase an
48 ing microorganisms employ a separate enzyme, chlorite dismutase, to prevent accumulation of the destr
49                                          The chlorite dismutases (C-family proteins) are a widespread
50 ctroscopic and physicochemical features with chlorite dismutases previously isolated from three organ
51 its sequence is highly similar to functional chlorite dismutases, the HemQ protein has no steady stat
52     We hypothesized this was enabled through chlorite dismutation by the community, as most strains i
53                 U(VI) adsorbed on quartz and chlorite displayed characteristic individual luminescenc
54 aused by surface modifications stemming from chlorite dissolution; The largest deviation occurred whe
55 esponding unsaturated allylamide with sodium chlorite followed by (ii) epoxidation of the allylamide
56  intensities of U(VI) adsorbed on quartz and chlorite followed the same trend of fractional adsorbed
57 own of antigorite to olivine, enstatite, and chlorite generates fluids with high oxygen fugacities, c
58 s steadily increased as the mass fraction of chlorite increased, indicating preferential sorption to
59 ylic oxocarbenium intermediate is trapped by chlorite ion to form a carbonyl group, we name this reac
60                                              Chlorite irreversibly inactivates the enzyme after appro
61 idation/double bond epoxidation using sodium chlorite is reported.
62                                              Chlorite is the sole source of dioxygen as determined by
63 (VI) concentration increased with increasing chlorite mass fraction-likely due to ill-defined lumines
64 latively low-temperature microdomains of the chlorite matrix.
65 ed alteration minerals including serpentine, chlorite, Mg-carbonate in fractured bedrock, veins, and
66 py investigation of U(VI) adsorbed on quartz-chlorite mixtures with variable mass ratios have been pe
67                     The acid form decomposes chlorite most efficiently when the distal Arg is protona
68 beta-unsaturated delta-lactones using sodium chlorite (NaClO(2)) as a cheap and environmentally frien
69 n in living cells, by harnessing prokaryotic chlorite O(2)-lyase (Cld) enzymes that convert chlorite
70 cyclobutene-1-carboxylate followed by sodium chlorite oxidation afforded the 1-monooctyl 2-ketoglutar
71 rresponding Delta(8)-THCs followed by sodium chlorite oxidation to give the 9-carboxy-Delta(8)-THC de
72  Sensitivity improved fourfold for PLP using chlorite postcolumn derivatization over traditional bisu
73                                              Chlorite postcolumn derivatization was used to oxidize P
74 n of the Fe(III) associated with biotite and chlorite primed the minerals for reductive scavenging of
75      When reacted with unaltered biotite and chlorite, significant sorption of U(VI) occurred in low
76 ring phases (i.e., two types of serpentines, chlorite, smectite, goethite, and hematite) the isotopic
77 te) and its diagenetic products (mixed-layer chlorite/smectite, corrensite, and chlorite) are the dom
78 ic system, SupplemeNtal Oxygen Released from ChLorite (SNORCL), for on-demand local generation of mol
79 from their experiments is that the limits of chlorite stability cannot explain the global systematics
80              The reduction of perchlorate to chlorite, the first enzymatic step in the bacterial redu
81  with growth of porosity from dissolution of chlorite, the most reactive of the abundant minerals in
82 roscale compositional mapping, combined with chlorite thermodynamic modeling, reveals that the titani
83 c disinfection byproduct (e.g., chlorate and chlorite) through photoactivated transformations.
84 ton coupled electron-transfer) reaction with chlorite to afford chlorine dioxide.
85 aining phyllosilicates including biotite and chlorite to alter the speciation, and thus the mobility,
86 ld is highly specific for the dismutation of chlorite to chloride and dioxygen with no other side pro
87 dria of human cells, and that coexpressing a chlorite transporter results in molecular oxygen product
88 creased significantly following an acidified chlorite treatment.
89 lulase treatment and decreased antigen after chlorite treatment.
90 halomethanes, haloacetic acids, bromate, and chlorite typically remained below current regulatory lev
91 catalytic formation of chlorine dioxide from chlorite under ambient temperature at pH 5.00.
92 veloped method of generating O2 in situ from chlorite using the enzyme chlorite dismutase to prepare
93  protein has no steady state reactivity with chlorite, very modest reactivity with H2O2 or peracetic
94 lorite dismutase catalyzes O(2) release from chlorite with exquisite efficiency and specificity.
95  illite, mixed layers of illite/smectite and chlorite, with minor kaolinite and smectite.