ライフサイエンスコーパス: Cs

1 Cs and Li ions were added as integrated ISTDs to the BGE

2 Cs sorption isotherms were carried out with Illite previ

3 Cs uses outer core 5s and 5p orbitals to bind the oxygen

4 Cs(+) acts as a soft Lewis acid to polarize the carbon-c

5 o 80,000 counts per second for a 1 ng/L (133)Cs solution, providing a detection limit of 1 pg/L.

6 We use (133)Cs, (87)Rb, (39)K, (13)C, and (14)N solid-state MAS NMR

7 7)Cs (234-824 mBq/kg of wet weight) and (134)Cs (18.2-356 mBq/kg of wet weight).

8 activity concentrations of (137)Cs and (134)Cs in the same samples were also analyzed by gamma spect

9 migration-aged fish did not exhibit any (134)Cs, suggesting that they had not recently migrated near

10 ed for (137)Cs and Fukushima-attributed (134)Cs.

11 In contrast to the effectively constant (134)Cs/(137)Cs activity ratios (1.04 +/- 0.04) and (129)I/(1

12 termination of the presence of (137)Cs, (134)Cs, (131)I, and other gamma-emitting radionuclides in th

13 Bq/kg of wet weight) with no detectable (134)Cs activity.

14 for (137)Cs, and 54 +/- 1 Bq.m(-3) for (134)Cs, appear to be influenced by ongoing releases from the

15 5.34 TBq for (137)Cs, and 4.74 TBq for (134)Cs, corresponding to 1.13% of the total estimated radioc

16 Most (134)Cs and (137)Cs were bound in organic matter (53-91%) and

17 both the presence and concentration of (134)Cs (p < 0.001).

18 Here, time series measurements of (134)Cs and (137)Cs in seawater on Line P and on the CLIVAR-P

19 Time series measurements of (134)Cs and (137)Cs in seawater revealed the initial arrival

20 dionuclides other than (131)I, (132)Te, (134)Cs, (136)Cs, and (137)Cs.

21 ma, Japan have become contaminated with (134)Cs and (137)Cs released in March 2011 from the damaged F

22 ission product radionuclides of cesium ((135)Cs and (137)Cs) at concentrations found in environmental

23 The ability to reliably measure (135)Cs/(137)Cs using a high specification laboratory ICP-SFM

24 CP-SFMS enables reliable measurement of (135)Cs/(137)Cs ratios, which can be used as a forensic tool

25 (137)Cs distribution patterns, (135)Cs/(137)Cs isotope ratios, known Cs chemistry at this si

26 FMS are the high yield fission products (135)Cs and (137)Cs that have entered the environment as a re

27 ate limitations to the information that (135)Cs/(137)Cs ratios alone can provide is presented and inc

28 This in turn enables measurement of the (135)Cs/(137)Cs ratio, which varies with the source of nuclea

29 es other than (131)I, (132)Te, (134)Cs, (136)Cs, and (137)Cs.

30 (137)Cs distribution patterns, (135)Cs/(137)Cs isotope ratios

31 (137)Cs resulted <0.10Bqkg(-1) in all samples.

32 (134/137)Cs poisoning, and use for (131/137)Cs radiotherapy (brachytherapy).

33 Dose rates from (134,137)Cs were highest in demersal species with sediment-associ

34 In addition to (134,137)Cs, the radionuclide (90)Sr was estimated to contribute

35 , administration as an antidote for (134/137)Cs poisoning, and use for (131/137)Cs radiotherapy (brac

36 ential applications as an effective (134/137)Cs remover from nuclear waste solutions, administration

37 luenced by freshwater inputs carrying a (137)Cs/(90)Sr activity ratio closer to that of the FDNPP fal

38 time series measurements of (134)Cs and (137)Cs in seawater on Line P and on the CLIVAR-P16N 152 degr

39 Time series measurements of (134)Cs and (137)Cs in seawater revealed the initial arrival of the Fukus

40 Natural radionuclides and (137)Cs in twenty seven honeys produced in a region of the Ce

41 ve become contaminated with (134)Cs and (137)Cs released in March 2011 from the damaged Fukushima Dai

42 high yield fission products (135)Cs and (137)Cs that have entered the environment as a result of anth

43 Most (134)Cs and (137)Cs were bound in organic matter (53-91%) and some in wat

44 ct radionuclides of cesium ((135)Cs and (137)Cs) at concentrations found in environmental and low lev

45 lyzed for (236)U (as well as (238)U and (137)Cs).

46 (131)I, (132)Te, (134)Cs, (136)Cs, and (137)Cs.

47 ating, were confirmed using (210)Pb and (137)Cs: these show that the top 2 m of Sphagnum-peat has acc

48 s from the FDNPP, with a characteristic (137)Cs/(90)Sr activity ratio of 3.5 +/- 0.2.

49 ast to the effectively constant (134)Cs/(137)Cs activity ratios (1.04 +/- 0.04) and (129)I/(131)I ato

50 (137)Cs distribution patterns, (135)Cs/(137)Cs isotope ratios, known Cs chemistry at this site, and

51 turn enables measurement of the (135)Cs/(137)Cs ratio, which varies with the source of nuclear contam

52 tations to the information that (135)Cs/(137)Cs ratios alone can provide is presented and includes (1

53 enables reliable measurement of (135)Cs/(137)Cs ratios, which can be used as a forensic tool in deter

54 The ability to reliably measure (135)Cs/(137)Cs using a high specification laboratory ICP-SFMS now en

55 A distinguishable (137)Cs energy spectrum with comparable or better resolution

56 adiation doses and follow environmental (137)Cs behavior.

57 (137)Cs (Fukushima-derived plus fallout (137)Cs) off the North American coast will likely attain maxi

58 between 2008 and 2012 were analyzed for (137)Cs and Fukushima-attributed (134)Cs.

59 asin area 5,172 km(2)) was 5.34 TBq for (137)Cs, and 4.74 TBq for (134)Cs, corresponding to 1.13% of

60 (-3) for (90)Sr, 124 +/- 3 Bq.m(-3) for (137)Cs, and 54 +/- 1 Bq.m(-3) for (134)Cs, appear to be infl

61 Pre-Fukushima (137)Cs and (90)Sr levels (resulting from atmospheric nuclear

62 e time series measurements of Fukushima (137)Cs indicate that the 2015-2016 results represent maximum

63 The current elevated Fukushima (137)Cs levels in seawater in the eastern North Pacific are e

64 groundwater collected in Sendai Bay had (137)Cs concentrations of up to 43 +/- 1 Bq.m(-3), while (90)

65 and seawater samples, an initial (129)I/(137)Cs activity ratio of approximately 4 x 10(-7) was obtain

66 tomic ratios (16.0 +/- 2.2), the (129)I/(137)Cs activity ratios scattered from 3.5 x 10(-7) to 5 x 10

67 011-2015 was calculated from the (129)I/(137)Cs ratio of the ongoing (137)Cs releases and estimated t

68 g, whereby meat was typically higher in (137)Cs and vegetarian produce was usually higher in (90)Sr.

69 The increase in (137)Cs levels in the eastern North Pacific from Fukushima in

70 grated effective dose from incorporated (137)Cs of about 18 mSv.

71 ima (2008-2009) samples possessed lower (137)Cs activity concentrations (103-272 mBq/kg of wet weight

72 ed increased activity concentrations of (137)Cs (234-824 mBq/kg of wet weight) and (134)Cs (18.2-356

73 es indicate that future total levels of (137)Cs (Fukushima-derived plus fallout (137)Cs) off the Nort

74 ol compared to radiometric detection of (137)Cs alone.

75 The activity concentrations of (137)Cs and (134)Cs in the same samples were also analyzed by

76 Annual studies of (137)Cs in reindeer herders in Kautokeino, Norway, were initi

77 ion could be expected from the decay of (137)Cs produced by the US nuclear testing program there from

78 ivalent to fallout background levels of (137)Cs that prevailed during the 1970s and do not represent

79 ted that the assimilation efficiency of (137)Cs was 16% in polychaetes ingesting Fukushima sediment,

80 to the determination of the presence of (137)Cs, (134)Cs, (131)I, and other gamma-emitting radionucli

81 About 10.9 TBq of (137)Cs, 1.5 TBq of (90)Sr, 7.8 GBq of (238)Pu, 6.3 GBq of (2

82 indings confirm that (129)I, instead of (137)Cs, should be considered as a proxy for (131)I reconstru

83 s estimated from vertical abundances of (137)Cs.

84 the (129)I/(137)Cs ratio of the ongoing (137)Cs releases and estimated to be about 100 g (which adds

85 response with low LET gamma-radiation ((137)Cs; 0.5 Gy/min; 2 Gy).

86 progeny) and artificial radionuclides ((137)Cs) in various honey samples, as well as to compile a da

87 f and by 2015 and early 2016 it reached (137)Cs values of 6-8 Bq/m(3) in surface water along Line P.

88 y of (90)Sr being 10% of the respective (137)Cs concentrations may soon be at risk, as the (90)Sr/(13

89 Th and (228)Th) and gamma spectrometry ((137)Cs, (40)K, (226)Ra and (228)Ra).

90 ions may soon be at risk, as the (90)Sr/(137)Cs ratio increases with time.

91 The (137)Cs concentrations declined from the peak in 1965 with ef

92 accident, and we compare the results to (137)Cs collected at the same stations and depths.

93 been retained in the Hythe marsh, with (137)Cs and Cu depth profiles showing retention of input maxi

94 se to an unprecedented 16-coordinate (CN 16) Cs(+) cation in a likewise unprecedented tetracosahedral

95 t the intermediate solidification rate of 30 Cs(-1).

96 solidified in the cooling rate range of 1-50 Cs(-1).

97 onally photostable material, [HC(NH2)2](0.83)Cs(0.17)Pb(I(0.6)Br(0.4))3, with an optical band gap of

98 ment was also isolated by encapsulation of a Cs(+) counterion with 2.2.2-cryptand.

99 tribution is explained by the formation of a Cs-symmetric intermediate (dpms)Pt(IV)Me(OH)2 (8), a goo

100 ew cycloparaphenylene derivative possesses a Cs point group symmetry.

101 t distal stereocontrol is achieved through a Cs-bridged interaction between the Lewis-basic C-termina

102 the muscle oxidative capacity (Cpt1, Acox1, Cs, Cycs, Ucp3) and glucose metabolism (Glut1, Glut4, Hk

103 In addition, all animals acquired Cs directly from the aqueous phase, but this accounted f

104 We intentionally added Cs(+) ions to show that the Au329(SR)84 is the base mole

105 Although Cs (II) and (IV) are not energetically favoured, the int

106 Cesium bis(perfluoro-triphenylborane)amide, Cs[H2NB2(C6F5)6] (1), has been prepared by the reaction

107 adsorbent to remove toxic Sr(2+), Ba(2+) and Cs(+) cations from wastewater.

108 l that covalently modifies accessible As and Cs, than regions that encode protein domain junctions.

109 hat serves to enhance Ba decontamination and Cs recovery.

110 ith incompatible elements (S, As, Mo, F, and Cs) in water samples within granitic intrusions.

111 n be optimized in the same way as by Ga+ and Cs+ bombardment.

112 ch water clusters attached to the H3O(+) and Cs(+) ions into structures that yield well-resolved vibr

113 d Pt(II) complex compounds and Li, Na, K and Cs atoms.

114 l network are ion-exchangeable with K(+) and Cs(+) ions.

115 and Na(+) over larger ones such as K(+) and Cs(+).

116 l ion cationization (Li(+), Na(+), K(+), and Cs(+)).

117 onic adducts (H(+), NH4(+), Na(+), K(+), and Cs(+)).

118 cation, [M + X](+) where X = Li, Na, K, and Cs, versus the topologically similar structures of the p

119 Although Li and Cs only form alloys at ambient conditions, we demonstrat

120 e ligands, in positive and negative mode and Cs(+) adduction, leads to a conclusive composition of Au

121 The controlled reaction of Na and Cs, two alkali metals of different ionic sizes and bindi

122 pS channel was permeable to K(+), Na(+) and Cs(+) but not to Cl(-) or Ca(2+).

123 A than the NATII materials containing Rb and Cs as EFC.

124 ctroscopy on a mixture of interacting Rb and Cs vapors.

125 tion by several alkali metals (Li, K, Rb and Cs) and alkali-earth Ca.

126 r 25 and 20 GPa long-range ordered Rb-Rb and Cs-Cs correlations continue to be present over length sc

127 icients between those reported for Rb(+) and Cs(+).

128 the occludable ions Na(+), K(+), Rb(+), and Cs(+) cause a drop in RH421 fluorescence.

129 addition of alkali cations (K(+), Rb(+), and Cs(+)) led to the aggregation of Mn(IV)-OH-PFOM as analy

130 s, is examined; of these, certain K, Rb, and Cs compounds are predicted to be thermodynamically stabl

131 t of AAuH2 compounds, A = Li, Na, K, Rb, and Cs, is examined; of these, certain K, Rb, and Cs compoun

132 measured for metallic fluid H, N, O, Rb, and Cs.

133 These species have C1 (unsym) and Cs (sym) symmetries, respectively, depending on the ster

134 onuclides of the elements Kr, Te, I, Xe, and Cs.

135 maroon [K(crypt)](+) , [K(18-c-6)](+) , and [Cs(crypt)](+) salts of the [Sc(NR2 )3 ](-) anion are for

136 cent experiments show that direct, anhydrous Cs(+)-K(+) exchange is kinetically viable and leads to t

137 econstitution and analysis of vertebrate APC/Cs under physiological conditions, we show how cyclin-de

138 e polyhedral structure having an approximate Cs symmetry and featuring a four-atom trapezoidal face.

139 amounts in strong-acid extracts decreased as Cs > Rb > Ba > K approximately Sr.

140 e tunnel dimension was found to increases as Cs substitution in the tunnel increased.

141 eding polychaetes, and macrofauna assimilate Cs from these polychaetes to account for >90% of their b

142 The elements B, Ba, Cs, Cu, Mg, Rb, Sr, Tl and Zn were identified as suitabl

143 some heavy stable elements (Rb, Sr, Zr, Ba, Cs, Ba, La, Ce, Nd, Sm, Dy, Lu, U, Th) in glassy fallout

144 Using the integrated ISTDs, both Cs and Li improved the Na peak area reproducibility appr

145 Overall, sediment-bound Cs is sufficiently bioavailable to deposit-feeding polyc

146 -aniline were not systematically affected by Cs(+).

147 nd Na(+) ions, and is selectively blocked by Cs(+) and ZD7288.

148 r reversed when the h-current was blocked by Cs(+).

149 e (AMA), and N,N-diallyl acrylamide (DAA) by Cs-ligated zirconocenium ester enolate catalysts under a

150 nted in silicon and then sputter profiled by Cs bombardment.

151 ow-threshold harmonic generation of caesium (Cs) atoms in an intense 3,600-nm mid-infrared laser fiel

152 age and lower BMI compared with Caucasians (Cs).

153 ight alkali metals such as Li to Cs, causing Cs to become anionic with a formal charge much beyond -1

154 r shell 5p electrons of Cs reactive, causing Cs to expand beyond the +1 oxidation state.

155 form when an ultracold ground-state cesium (Cs) atom becomes bound within the electronic cloud of an

156 ignificantly more stable isomer, a classical Cs(+) complex of F5 (-) .

157 ion of twenty-nine elements (Ag, As, Ce, Co, Cs, Cu, Eu, Fe, Ga, Gd, La, Lu, Mn, Mo, Nb, Nd, Ni, Pr,

158 of the nitride-bridged diuranium(IV) complex Cs[{U(OSi(OtBu)3)3}2(mu-N)]affords the first example of

159 ces (fs) and monovalent salt concentrations (Cs).

160 ibits a complex crystal structure containing Cs(+) cations, Pt(2-) and H(-) anions.

161 32 elements, Al, As, Ba, Ca, Cd, Ce, Co, Cr, Cs, Cu, Dy, Fe, Ga, La, Li, Mg, Mn, Na, Nd, Ni, Pb, Pr,

162 THP-1 cells by treatment with cyclosporine (Cs) or its nonimmunosuppressive analogue SDZ-NIM811, ind

163 (2) possibility of mixing between different Cs source terms (including nuclear weapons fallout and a

164 layer spacing ( approximately 0.7 A) during Cs(+) exchange is an example of "chemical-mechanical cou

165 apabilities and limitations to environmental Cs analyses.

166 hat may facilitate cation uptake--especially Cs(+), which is a highly selective cation.

167 d within the electronic cloud of an extended Cs electronic orbit.

168 f exchange materials can effectively extract Cs; however, non-quantitative elution of Cs makes subseq

169 Significantly fast Cs+ transport rate along with high selectivity is an int

170 The Td -symmetric [CsO4 ](+) ion, featuring Cs in an oxidation state of 9, is computed to be a minim

171 ns interlayer K(+) and has high affinity for Cs(+).

172 The current efficiency for Cs+ transport has been found to be approximately 100%.

173 High decontamination factor for Cs+ over Na+ has been obtained in all the cases.

174 tructure is a promising crystalline host for Cs immobilization.

175 Although exchange of interlayer K(+) for Cs(+) is nearly thermodynamically nonselective, recent e

176 motion and by extension, the propensity for Cs release from hollandite.

177 because this clay is especially relevant for Cs migration-retention in the environment.

178 become active, with growing tendency to form Cs (III) and (V) valence states at fluorine-rich conditi

179 demembranated sucrose gradient fractionated (Cs/Tx) sperm heads.

180 ng for Illite decollapse especially for high Cs loadings, because of the potential prediction errors

181 The procedure developed shows high Cs selectivity and Ba decontamination from digests of co

182 on transport together with the use of highly Cs+ selective hexachlorinated derivative of cobalt bis d

183 he objective of this study is to analyze how Cs adsorption onto Illite is affected by structural chan

184 ion by two bowl-shaped sumanenyl anions in [Cs(C21 H11(-) )2 ](-) was revealed crystallographically.

185 ials with cage-like structures incorporating Cs and Ba guest atoms, are reported as a means of alteri

186 Comparison of its Cs(+) cation exchange properties at pH 8 and pH 13 unexp

187 nt moieties, the [Nb6O19](8-) polyanion, its Cs(+) counterions, and the DMMP substrate, were tracked

188 alkali metal cations (Li(+) , Na(+) , K(+) , Cs(+) ) on the non-Nernstian pH shift of the step-relate

189 on from latency; they include protein kinase Cs(PKCs), mitogen activated protein kinase/extracellular

190 terns, (135)Cs/(137)Cs isotope ratios, known Cs chemistry at this site, and historical records enable

191 On the contrary, large Cs(+) ions blocked the WT channels, while displayed larg

192 ck mechanism in which exchange of the larger Cs(+) for the smaller K(+) significantly lowers the migr

193 dimers [{U(Tren(TIPS))(mu-N[H]M)}2] [M = Li-Cs (2a-e)].

194 It was proposed that group I elements like Cs can be oxidized further under high pressure.

195 In the presence of 1 M Cs(+), we found a marked increase of apparent (13)C-kine

196 + Na)(+), (M + K)(+), (M + Rb)(+), and (M + Cs)(+), were successfully detected on the FAPCI mass spe

197 Their intensity order was as follows: (M + Cs)(+) > (M + Rb)(+) > (M + K)(+) > (M + Na)(+) > (M + L

198 healthy, young lean male SAs and 12 matched Cs underwent a two-step hyperinsulinemic-euglycemic clam

199 d scanning transmission electron microscopy (Cs -corrected STEM).

200 d scanning transmission electron microscopy (Cs-STEM), nano-beam electron diffraction, electron holog

201 rmation space of AITC contains three minima, Cs-M1 and enantiomers M2 and M2'; the exchange between c

202 iety of monovalent cations, including Na(+), Cs(+), and dimethylammonium (DMA(+)), the side chain of

203 metal reagents MR (M = Li, R = Bu(t); M = Na-Cs, R = CH2C6H5) afforded the imido-bridged dimers [{U(T

204 Single cells with Na-Cs alloy anodes exhibit great improvement in cycling lif

205 The retention of natural Cs by these three soils, which developed over many thous

206 ted elements, Li, B, Na, Ga, Rb, Sr, Zr, Nb, Cs, Ba, Sm, and Hf, allows more than 80% of correct pred

207 Here, blue-emission ( approximately 470 nm) Cs-based perovskite NCs are derived by directly mixing s

208 that the UO(NO)Cl2(-) complex has nonplanar Cs symmetry and a singlet ground state.

209 lates with the size of the alkali cation: NS/Cs(+)/NS > NS/Rb(+)/NS > NS/K(+)/NS > NS/Na(+)/NS > NS/L

210 R correlates with the interlayer spacing; NS/Cs(+)/NS has the lowest eta (0.45 V), while NS/Li(+)/NS

211 ers (eta and Tafel slope) associated with NS/Cs(+)/NS for the OER were superior to that of the bulk b

212 , and 6% d(-1) for fish after acquisition of Cs from water; rate constants following dietary uptake w

213 Only the UCC-normalized amount of Cs was greater than unity.

214 diometric and mass spectrometric analyses of Cs contamination in the environment can reveal the locat

215 prediction of sorption/migration behavior of Cs, and possibly other contaminants, in the environment.

216 d for nearly all of the total body burden of Cs in these animals.

217 nd organic matter may be the main carrier of Cs-bearing particles.

218 thesis and spectroscopic characterization of Cs-symmetric tris- and C2v-symmetric tetra-adducts of C7

219 MAS NMR to probe microscopic composition of Cs-, Rb-, K-, MA-, and FA-containing phases in double-,

220 Rate constants of Cs loss from animal tissues were 20% d(-1) for polychaet

221 ion channels due to the internal dialysis of Cs(+) , which increased the bleach-induced desensitizati

222 hich is eliminated upon internal dialysis of Cs(+) .

223 conductances during the internal dialysis of Cs(+) further desensitizes the photovoltage thereby elim

224 Under pressure, 5p electrons of Cs atoms become active, with growing tendency to form Cs

225 ure may make the inner shell 5p electrons of Cs reactive, causing Cs to expand beyond the +1 oxidatio

226 act Cs; however, non-quantitative elution of Cs makes subsequent ICP-SFMS quantification challenging.

227 Consequently, the relative enrichment of Cs and Rb is largely controlled by selective sorption to

228 The enrichment of Cs and Rb relative to Ba, Sr, and K in three soils repre

229 model indicated that the transfer factors of Cs from sediments and the trophic transfer factors from

230 in bonding of the formally core 5p levels of Cs.

231 n the environment can reveal the location of Cs emission sources, release mechanisms, modes of transp

232 ould be considered in the migration model of Cs and radionuclides in the current environment surround

233 th experimental evidence and the modeling of Cs sorption onto Illite supported the hypothesis of deco

234 ere, we elucidate the atomic-level nature of Cs and Rb incorporation into the perovskite lattice of F

235 t O2 formation is fastest in the presence of Cs(+) and approximately fourth order in Mn(IV)-OH-PFOM s

236 nge 2.0 to 9.0 as well as in the presence of Cs(+) as a quencher of excited singlet 4-Cl-aniline at p

237 ge 2.0 to 7.0 in the absence and presence of Cs(+) used as an excited singlet state quencher.

238 of 2-Cl-aniline decreased in the presence of Cs(+), whereas those for 3-Cl-aniline were not systemati

239 anoparticles associated with a wide range of Cs concentrations (1.1-19 wt% Cs as Cs2O).

240 his helps to explain the longer retention of Cs in bottom-dwelling fish near Fukushima.

241 f 1 allows nearly quantitative separation of Cs(+) from water, which suggests potential applications

242 e, allows to achieve selective separation of Cs+ from high concentration of Na+ and other fission pro

243 s the effect of the unusual anionic state of Cs on the transition temperature.

244 work function of 2.07 eV (lower than that of Cs) while remaining chemically inert, two properties usu

245 les in a SiO2 glass matrix (up to 30 wt% of Cs and 1 wt% of U mainly associated with Zn-Fe-oxide).

246 Only Cs- and Rb-NAT reveal a phase separation into a dense fo

247 sults indicate that grain size and optimized Cs stoichiometry control cation motion and by extension,

248 exes in solution with Na(+), K(+), Rb(+), or Cs(+) counterions, we mathematically decompose the scatt

249 ntinental crust (UCC) decreased in the order Cs > Rb > Ba > K > Sr in the soil fine fractions.

250 s model predicts that Na(+) would outcompete Cs(+) by 1.8-2.1-fold; i.e., with Cs(+) in 2-fold excess

251 is no significant preference for Na(+) over Cs(+).

252 te the binary caesium salts of phenanthrene, Cs(C14H10) and Cs2(C14H10), to show that they are multio

253 diamagnetic because of orbital polarization, Cs(C14H10) is a Heisenberg antiferromagnet with a gapped

254 chanisms (polyfluoride anions and polyvalent Cs cations) allows CsF2 and CsF4 compounds to be stable

255 The enol tautomer possesses Cs symmetry with a planar ring and strongly asymmetric h

256 urthermore, we showed that 2-APB potentiated Cs(+) current on constitutively active Orai1-V102C/A/G m

257 usly reported data on Pu, U, and radioactive Cs, we concluded that Pu and non-natural U from the FDNP

258 ork cations (EFC) Li(+), Na(+), K(+), Rb(+), Cs(+) allow us to assess the role of two different EFC-H

259 However, in the case of AxFe2Se2 (A = K, Rb, Cs), the presence of an intergrown antiferromagnetic ins

260 rent alkali metals as reductants (Na, K, Rb, Cs).

261 iple bonds, [M]2[U(NR)4] (M = Li, Na, K, Rb, Cs).

262 alated FeSe system (A1-xFe2-ySe2, A = K, Rb, Cs, Tl).

263 neN(3,5-(CF3)2C6H3)(TriNOx)] (M = Li, K, Rb, Cs; solv = TMEDA, THF, Et2O, or DME), was isolated and f

264 which has been studied by atomic-resolution Cs -corrected STEM.

265 rds a novel type of organometallic sandwich [Cs(C21 H11(-) )2 ](-) , which crystallized as a solvent-

266 ullerene containing a heptagonal ring, Sc2C2@Cs(hept)-C88, was isolated from the raw soot obtained by

267 The Sc2C2@Cs(hept)-C88 was purified by multistage high-performance

268 In this sense, Cs(+) resembles hypervalent Xe.

269 R)84 is the base molecular ion, with several Cs(+) adducts.

270 In the presence of Ca, the maximum sorbed Cs was unexpectedly high (900 mequiv . kg(-1)) given the

271 We examine the electron donor species Cs, Rb, K, Na, Li, Ca and for each we determine the full

272 f the following four ("allowed") symmetries, Cs, C2v, D2d and S4.

273 bled the number of disease-associated target Cs able to be corrected preferentially over nearby non-t

274 rected preferentially over nearby non-target Cs.

275 ne, SAs had higher insulin clamp levels than Cs, indicating reduced insulin clearance rate.

276 n having K(+) as the permeant ion; (ii) that Cs(+) or Rb(+), known to halt C-inactivation, prevented

277 ressive analogue SDZ-NIM811, indicating that Cs-sensitive host cell cyclophilins other than CypA cont

278 The Cs-X-U-Si-O (X = F, Cl) pentanary phase space is used as

279 In addition, a new band for the Cs(+) [F3 ](-) complex in neon is reported.

280 ay diffraction studies were conducted in the Cs/Sn/P/Se system.

281 The presence of two or three Cs+ cations binding the nitride group is key for the iso

282 ltiply bound to two uranium and two or three Cs+ cations, these complexes transfer the nitride group

283 ed by conformational switching from a C3h to Cs symmetry of mTBPB via rotation of m-phenylene units.

284 nsfer from light alkali metals such as Li to Cs, causing Cs to become anionic with a formal charge mu

285 Group 1 of the periodic table from Li(+) to Cs(+), PFL-AE activity sharply maximizes at K(+), with N

286 n of 3 M HNO3, shows high selectivity toward Cs, which is effectively eluted in 0.05 M HNO3.

287 The high conformational selectivity toward Cs-conformers is templated by the twofold coordination t

288 U, Cs, Ba, Rb, K, and Ca isotopic ratios were determined on

289 a zigzag Sc2C2 unit inside an unprecedented Cs(hept)-C88 carbon cage containing 13 pentagons, 32 hex

290 trend: they show no octahedral tilting upon Cs-substitution but only a contraction of the lattice, l

291 sions of our previous publication which used Cs and Li as traditional ISTDs.

292 Using Cs(+) as a benchmark element, this study aims to assess

293 The valence Cs 6s orbital lies too high to be involved in bonding, a

294 _clus complex forms intermediate with a weak Cs-heteroatom(azole) bond, the existence of which increa

295 and (crypt) and 18-crown-6 (18-c-6) and with Cs in the presence of crypt.

296 outcompete Cs(+) by 1.8-2.1-fold; i.e., with Cs(+) in 2-fold excess of Na(+) the ion atmosphere would

297 chalcogenides, CPM-120-ZnGeS (exchanged with Cs(+) ions) also shows reversible adsorption with high c

298 Reduction of the unstable red solid with Cs metal produces the dianion of the title compound, fro

299 In contrast (to previous work), Cs as a traditional ISTD resulted in final RSDs of 2.5-8

300 wide range of Cs concentrations (1.1-19 wt% Cs as Cs2O).