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1 nine) in addition to some selenocysteine and selenate.
2 atile Se compounds when they were exposed to selenate.
3 erexpressors, both on media with and without selenate.
4 robably by an inability to chemically reduce selenate.
5 plants supplied with selenite compared with selenate.
6 whereas selenate-supplied plants accumulated selenate.
7 e from T. selenatis grown anaerobically with selenate.
8 cystine, methaneseleninic acid, selenite and selenate.
9 th myrosinase activity below 3.5-mmol sodium selenate.
10 ata) exposed to either 20 microM selenite or selenate.
11 ironmentally relevant mineral reductants for selenate.
12 o environmentally relevant concentrations of selenate.
13 y (88-95%) organic C-Se-C; the remainder was selenate.
14 the grain more efficiently than selenite and selenate.
16 o or supranutritional amounts of selenium as selenate (200 or 400 mug/d) or as selenomethionine (200
17 orms was higher for selenite (100%) than for selenate (26%), the absolute concentration of organosele
18 than that measured from plants supplied with selenate, 38 times higher than from selenite, and six ti
20 (-1)DM) and the concentration (2-mmol sodium selenate) above which the content of phenolic compounds
21 cation of Se reduction and assimilation from selenate accumulated in the cladode tips into the two LC
23 ontent was lower in plants supplemented with selenate and accumulated mainly in the leaves compared w
25 ke step caused by diffusive exchange between selenate and chloride followed by a slower, high-fractio
29 ested for their ability to adsorb and remove selenate and selenite anions from aqueous solutions.
31 products, two foliar Se fertilisers (sodium selenate and selenite) were tested at four rates (0-10-2
32 capacity, and fastest uptake rates for both selenate and selenite, of all zirconium-based MOFs studi
34 ate-limiting steps in Se volatilization from selenate and selenite, time- and concentration-dependent
36 from the elements, DeltaH(f,el), for Al(13) selenate and sulfate are -19,656.35 ( +/- 67.30) kJ.mol(
37 degrees C in 5 N HCl for the epsilon-Al(13) selenate and sulfate are -924.57 (+/- 3.83) and -944.30
38 affinity of the epsilon-Keggin clusters for selenate and sulfate, the enthalpy associated with two S
39 slow rate of oxygen isotope exchange between selenate and water under most environmental conditions d
40 The rate of oxygen isotope exchange between selenate and water was investigated at conditions of 10
41 sures, we examined the toxicity of selenite, selenate, and amorphous selenium nanoparticles (SeNPs).
42 rtant implications for the fate of chromate, selenate, and sulfate in subsurface environments and off
43 rized the adsorption mechanisms of chromate, selenate, and sulfate on Al-substituted ferrihydrite (0,
46 selectivity for the tetrahedral sulfate and selenate anions observed in competitive crystallization
49 e to dimethyl selenide (DMSe): (a) uptake of selenate, (b) activation of selenate by ATP sulfurylase,
50 4 mm or more behind the apex when exposed to selenate but in the meristem (approximately 1 mm from th
51 nificantly up-regulated in plants exposed to selenate but were low in plants supplied with selenite.
52 ): (a) uptake of selenate, (b) activation of selenate by ATP sulfurylase, and (b) conversion of selen
53 experiments were performed with selenite or selenate by equilibrating suspensions containing the nan
56 m jarosite, TlFe3(OH)6(SO4)2, along with the selenate-capped jarosite analogues of potassium, KFe3(OH
64 t environmental conditions demonstrates that selenate-delta(18)O signatures produced by biogeochemica
65 that it will be possible to use the value of selenate-delta(18)O to investigate the biogeochemical be
68 the kinetic isotope effects for (18)O within selenate during abiotic reactions with iron-bearing hydr
71 and for selenate on schwertmannite, whereas selenate forms outer-sphere complexes in the aluminum oc
72 rpose of this study was to determine whether selenate fortification of infant formula would improve t
74 (n = 7, mean body weight = 1312 g) received selenate-fortified preterm and full-term infant formulas
75 lenium (Se), occurring as oxidized inorganic selenate from hypersalinized agricultural drainage water
80 selenate for 28 days contained predominantly selenate in the mature leaf tissue at a concentration of
81 o investigate the biogeochemical behavior of selenate, in an analogous fashion to the use of sulfate-
84 luminite and schwertmannite for arsenate and selenate is compared, and the coordination geometries of
85 indicating that the ability to biotransform selenate is either inducible or developmentally specific
86 Our data suggest that Se volatilization from selenate is limited by the rate of selenate reduction, a
87 Root transcriptome changes in response to selenate mimicked the effects observed under sulfur star
88 num centered epsilon-Keggin clusters, Al(13) selenate, (Na(AlO(4))Al(12)(OH)(24)(SeO(4))(4)*12H(2)O)
89 The enzyme is specific for the reduction of selenate; nitrate, nitrite, chlorate, and sulfate were n
90 f ligand for arsenate on both phases and for selenate on schwertmannite, whereas selenate forms outer
93 um compared with plants supplied with SeMet, selenate, or selenite; they also accumulated more Se in
95 (approximately 5 microM), sulfate, chromate, selenate, phosphate, and chlorate did not bind even when
96 d classes of oxo compounds (i.e., vanadates, selenate, phosphate, sulfate, acetate, nitrate, and nitr
99 after the initial uptake step, the extent of selenate reaction is well correlated with delta(18)O val
107 eta-subunits of microbial nitrate reductase, selenate reductase, dimethyl sulfide dehydrogenase, ethy
108 on of selenate to selenite is catalyzed by a selenate reductase, previously shown to be located in th
109 tudies constitute the first description of a selenate reductase, which represents a new class of enzy
110 These results also indicate that sulfate and selenate reduction are developmentally correlated, and t
111 TPS and APR had a significant enhancement of selenate reduction as a proportion of total Se, whereas
114 ntribute to Se isotope forensics to identify selenate reduction within field sites and to possibly di
115 APR2 is a key enzyme in both sulfate and selenate reduction, and its reduced activity in the loss
116 tion from selenate is limited by the rate of selenate reduction, as well as by the availability of Se
117 h other and to the previously isolated sel1 (selenate-resistant) mutants, and have been designated se
121 nt selenium oxyanions, selenite (Se(IV)) and selenate (Se(VI)), can be quantified down to 7.3 and 8.3
122 e, were optimised for five selenium species; selenate (Se(VI)), Selenite (se(IV)), selenocysteine (Se
124 ith selenocompounds (sodium selenite, sodium selenate, Se-Met, MeSeCys) or SeB [high-Se (H-SeB) or lo
125 amino acids" and related oxidation products, selenate, selenite, and other species relatable to the q
126 ous inorganic or organic species of Se (e.g. selenate, selenite, and Se-methionine [Met]) into gaseou
127 ession and SeMSC accumulation in response to selenate, selenite, and sulfate treatments showed that t
128 edium and amended with the selenium oxyanion selenate, selenite, or selenocyanate, produces volatile
129 d several SRM selective inhibitors including selenate, selenite, tellurate, tellurite, nitrate, nitri
132 n selenium oxoanions selenite (SeO3(2-)) and selenate (SeO4(2-)) are toxic at intake levels slightly
133 onsumers of dissolved selenite (SeO3) versus selenate (SeO4) uptake into aquatic primary producer com
135 e- or SeMet-supplied wild-type plants and in selenate-supplied ATP-sulfurylase transgenic plants.
137 increased Se accumulation, whereas increased selenate supply increased sulfate accumulation in both r
139 activity was increased more by both doses of selenate than by the placebo in C-P class B patients.
140 selenium was increased more by 400 mug Se as selenate than by the placebo in C-P class C patients.
143 s for the assimilation and volatilization of selenate to dimethyl selenide (DMSe): (a) uptake of sele
146 CpNifS overexpression significantly enhanced selenate tolerance (1.9-fold) and Se accumulation (2.2-f
147 The present study showed that shoots of selenate-treated plants accumulated very low concentrati
153 nvolve constitutive up-regulation of sulfate/selenate uptake and assimilation, associated with elevat
154 , 5 mM, 3 d) were also tested for effects on selenate uptake and sulfate transporters' expression.
156 ed by 100-fold excess sulfate, which reduced selenate uptake by 100% in S. elata and 40% in B. juncea
157 entrations, apparently due to suppression of selenate uptake by sulfate, and insufficient nitrogen co
158 ccumulators S. elata and Brassica juncea for selenate uptake in long- (9 d) and short-term (1 h) assa
161 addition, high levels of sulfate suppressed selenate uptake, resulting in a dramatic reduction of Bo
162 sorption capacity but had a strong impact on selenate uptake, suggesting some kind of specific intera
165 ulfur, plants readily take up and assimilate selenate via sulfur transporters and enzymes and can eve
166 Based upon bulk solution concentrations, selenate was 9-fold more toxic to the roots than selenit
179 ulfate was the main mechanism for removal of selenate, whereas arsenate was removed by a combination
181 6-fold more Se and was tolerant to 20 microm selenate, while S. albescens suffered reduced growth, ch
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