ライフサイエンスコーパス: Sr

1 Sr(2) Fe(2) O(6-delta) also has the highest electrical c

2 Sr(2)RuO(4) is an extremely clean layered perovskite and

3 Sr(3) Sn(2) O(7) :Nd(3+) (SSN) with polar A2(1) am struc

4 Sr-bearing marine barite [(Ba (x) , Sr(1-x) )SO(4)] cycl

5 Here, the perovskite oxide Bi(0.15) Sr(0.85) Co(0.8) Fe(0.2) O(3-) (delta) (BiSCF) is shown

6 harge- and spin-stripe-ordered La(1.7)Eu(0.2)Sr(0.1)CuO(4) and La(1.48)Nd(0.4)Sr(0.12)CuO(4) in perpe

7 s, two prospective perovskite oxides, La(0.2)Sr(0.8)Co(1- x)Fe (x)O(3-delta) and Ba(0.5)Sr(0.5)Co(1-

8 rnating one-unit-cell of SrIrO(3) and La(0.2)Sr(0.8)MnO(3), we find a reversible phase transformation

9 La(1.6-x)Nd(0.4)Sr(x)CuO(4), La(1.8-x)Eu(0.2)Sr(x)CuO(4), La(2-x)Sr(x)CuO(4) and Bi(2)Sr(2-x)La(x)CuO

10 states N(r) within the halo surrounding Bi(2)Sr(2)CaCu(2)O(8) vortex cores.

11 of the high-temperature superconductor Bi(2)Sr(2)CaCu(2)O(8+delta) (Bi-2212; here, a monolayer refer

12 )Sr(2)CuO(6+delta) (Bi2201) and bilayer Bi(2)Sr(2)CaCu(2)O(8+delta) (Bi2212) to beyond the maximum T(

13 s of scanning tunneling spectroscopy in Bi(2)Sr(2)CaCu(2)O(8+delta) and conduct the analysis of phase

14 toemission spectroscopy measurements of Bi(2)Sr(2)CaCu(2)O(8+delta) over a wide range of doping level

15 r) modulations in the canonical cuprate Bi(2)Sr(2)CaCu(2)O(8+delta) that have eight-unit-cell periodi

16 including WTe(2), WSe(2), TiSe(2), and Bi(2)Sr(2)CaCu(2)O(8+delta).

17 te coexisting with superconductivity in Bi(2)Sr(2)CaCu(2)O(8+delta).

18 n temperatures (T(c)s) of the monolayer Bi(2)Sr(2)CuO(6+delta) (Bi2201) and bilayer Bi(2)Sr(2)CaCu(2)

19 0.2)Sr(x)CuO(4), La(2-x)Sr(x)CuO(4) and Bi(2)Sr(2-x)La(x)CuO(6+delta).

20 has also been reported in the trilayer Br(2)Sr(2)Ca(2)Cu(3)O(10+delta) (Bi2223).

21 from other cations (Cd(2+), Ni(2+), Co(2+), Sr(2+), Mg(2+), Fe(3+), K(+), Sm(3+), Ag(+), Na(+), Ba(2

22 eate a spinel Co(3) O(4) /perovskite La(0.3) Sr(0.7) CoO(3) interface by in situ reconstruction of th

23 Interestingly, the Nd(0.3)Sr(0.7)MnO(3) content has the highest degradation rate o

24 ehavior in photocatalytic activity of Nd(0.3)Sr(0.7)MnO(3) nanocomposite emerges from large surface a

25 The photocatalytic efficiency of Nd(0.3)Sr(0.7)MnO(3) nanocomposite was 95% of the initial AO dy

26 ort intriguing magnetic phenomena for La(2/3)Sr(1/3)MnO(3) films on an SrTiO(3) (001) substrate (LSMO

27 hin films were deposited on {(LaAlO(3))(0.3)(Sr(2)AlTaO(6))(0.7)} (LSAT) substrates in oxygen atmosph

28 dence of the proximity effect in Au/SrRuO(3)/Sr(2)RuO(4) junctions.

29 onovalent metal ions, Cr(3+), Mg(2+), Y(3+), Sr(2+) or Ba(2+).

30 sisting of one honeycomb-like network, Ba(4) Sr(4) (Co(0.8) Fe(0.2) )(4) O(15) (hex-BSCF), is reporte

31 (1.7)Eu(0.2)Sr(0.1)CuO(4) and La(1.48)Nd(0.4)Sr(0.12)CuO(4) in perpendicular magnetic fields (H( )),

32 e of four different cuprates-La(1.6-x)Nd(0.4)Sr(x)CuO(4), La(1.8-x)Eu(0.2)Sr(x)CuO(4), La(2-x)Sr(x)Cu

33 ple, the well-known perovskite oxide Ba(0.5) Sr(0.5) Co(0.8) Fe(0.2) O(3-) (delta) (BSCF) exhibits ex

34 current state of the art catalysts, Ba(0.5) Sr(0.5) Co(0.8) Fe(0.2) O(3-delta) and RuO(2) .

35 the oxygen evolution reaction (OER), Ba(0.5)Sr(0.5)Co(0.8)Fe(0.2)O(3-delta) (BSCF) exhibits excellen

36 2)Sr(0.8)Co(1- x)Fe (x)O(3-delta) and Ba(0.5)Sr(0.5)Co(1- x)Fe (x)O(3-delta) with x = 0 and 0.2, were

37 rk, we take double perovskite oxide PrBa(0.5)Sr(0.5)Co(1.5)Fe(0.5)O(5+delta) (PBSCF) as a model syste

38 in a representative cathode material, La(0.5)Sr(0.5)CoO(3-delta), and predict that under operating co

39 a(2+) is exchanged with Sr(2+); the Mn(4)O(5)Sr cofactor remains active, but the S(2)-S(3) and S(3)-S

40 oir consisting of a perovskite phase (La(0.6)Sr(0.4)FeO(3-delta)).

41 gated for the BiFeO(3) films grown on La(0.6)Sr(0.4)MnO(3)/SrTiO(3) and YAlO(3) substrates.

42 smatch found in the BiFeO(3) grown on La(0.6)Sr(0.4)MnO(3)/SrTiO(3) is exerted as biaxial in-plane co

43 sed organic spin valves (OSVs) using La(0.67)Sr(0.33)MnO(3) as a magnetic electrode.

44 nneling current from a ferromagnetic La(0.67)Sr(0.33)MnO(3) electrode.

45 upward and downward magnetization in La(0.67)Sr(0.33)MnO(3) thin films.

46 terostructures of BiFeO(3) (BFO) and La(0.7) Sr(0.3) MnO(3) (LSMO).

47 the spin dynamics in a half-metallic La(0.7) Sr(0.3) MnO(3) film by ultrafast pump-probe technique.

48 and other physical functionalities of La(0.7)Sr(0.3)MnO(3) (LSMO) films, here we report detailed inve

49 measurements carried out on Pt/PbPdT/La(0.7)Sr(0.3)MnO(3) (LSMO) metal-dielectric-metal capacitors s

50 lm of epitaxially grown ferromagnetic La(0.7)Sr(0.3)MnO(3) and an electroactive substrate of ferroele

51 La(0.7)Sr(0.3)MnO(3), a strong semi-metallic ferromagnet having

52 (0.1) Ce(0.9) O(1.95) and perovskite La(0.8) Sr(0.2) Ga(0.8) Mg(0.2) O(2.55) ) with a high concentrat

53 ensity and magnetic-field response of Nd(0.8)Sr(0.2)NiO(2) indicate a superconducting transition temp

54 tactic reduction(14-20), NdNiO(2) and Nd(0.8)Sr(0.2)NiO(2) single-crystal thin films are synthesized

55 Here we prepared a PEO/perovskite Li(3/8)Sr(7/16)Ta(3/4)Zr(1/4)O(3) composite electrolyte with a

56 harge localization in optimal-doped La(1.85) Sr(0.15) CuO(4) thin-film on SrTiO(3) substrate (LSCO/ST

57 hemical fingerprinting methods, namely n((86)Sr)/n((87)Sr) isotope amount ratios, multi-elemental and

58 2.9 +/- 3.5 per thousand) and Sr ((87)Sr/(86)Sr = 0.70923 +/- 0.00024) isotope ratios were not consis

59 The (87)Sr/(86)Sr age determinations have high accuracy, even in cases

60 dback on seawater composition and (87)Sr/(86)Sr changes.

61 ern Uttar Pradesh contains higher (87)Sr/(86)Sr compared to other region of Indo-Gangetic Plain due t

62 Indo-Gangetic Plain due to higher (87)Sr/(86)Sr of the Ganga compared to other rivers.

63 ans of variabilities observed for (87)Sr/(86)Sr ratio and Sr concentrations in authentic Bordeaux win

64 The (87)Sr/(86)Sr ratio and Sr concentrations of 43 authentic Bordeaux

65 The results imply that the (87)Sr/(86)Sr ratio of isolated spherical carbonate concretions can

66 of individuals exhibit different (87)Sr/(86)Sr ratios and, while the Gravettians are similar to the

67 ntium isotopic stratigraphy using (87)Sr/(86)Sr ratios of all concretions indicates an age of 17.02 +

68 Here we use (87)Sr/(86)Sr ratios to determine the ages of these spherical concr

69 (18)O, delta(13)C, delta(34)S and (87)Sr/(86)Sr) at periods >200 Myr, when they are broadly in phase

70 This study uses a multi-isotope ((87)Sr/(86)Sr, delta(34)S, delta(13)C, delta(15)N) approach to iden

71 res (delta(30)Si, delta(11)B, and (87)Sr/(86)Sr, respectively) to study serpentinization in the mantl

72 g with previous determinations of (87)Sr/(86)Sr.

73 ive feedback on seawater composition and (87)Sr/(86)Sr changes.

74 , delta(18)O, delta(13)C, delta(34)S and (87)Sr/(86)Sr) at periods >200 Myr, when they are broadly in

75 signatures (delta(30)Si, delta(11)B, and (87)Sr/(86)Sr, respectively) to study serpentinization in th

76 groups of individuals exhibit different (87)Sr/(86)Sr ratios and, while the Gravettians are similar

77 rrow spans of variabilities observed for (87)Sr/(86)Sr ratio and Sr concentrations in authentic Borde

78 n southern Uttar Pradesh contains higher (87)Sr/(86)Sr compared to other region of Indo-Gangetic Plai

79 ion of Indo-Gangetic Plain due to higher (87)Sr/(86)Sr of the Ganga compared to other rivers.

80 This study uses a multi-isotope ((87)Sr/(86)Sr, delta(34)S, delta(13)C, delta(15)N) approach

81 ngerprinting methods, namely n((86)Sr)/n((87)Sr) isotope amount ratios, multi-elemental and metabolom

82 repare 2 x 10(4) spin-polarized atoms of (87)Sr in the optical lattice within 500 ms; we observe a va

83 ovarying with previous determinations of (87)Sr/(86)Sr.

84 1)B = 22.9 +/- 3.5 per thousand) and Sr ((87)Sr/(86)Sr = 0.70923 +/- 0.00024) isotope ratios were not

85 The (87)Sr/(86)Sr age determinations have high accuracy, even in

86 The (87)Sr/(86)Sr ratio and Sr concentrations of 43 authentic Bo

87 The results imply that the (87)Sr/(86)Sr ratio of isolated spherical carbonate concreti

88 Here we use (87)Sr/(86)Sr ratios to determine the ages of these spherica

89 Strontium isotopic stratigraphy using (87)Sr/(86)Sr ratios of all concretions indicates an age of

90 We interrogate a (88)Sr(+) ion with our stimulated Brillouin scattering laser

91 ples followed by determination of (90)Sr/(88)Sr abundance sensitivity (2.1 x 10(-10)).

92 nd 2.5 +/- 0.1 ug g(-1) while the (90)Sr/(88)Sr isotope ratios were 6.47 +/- 0.17 x 10(-8) and 9.04 +

93 ionic conductivity is delineated in La(0.9) Sr(0.1) Ga(0.95) Mg(0.05) O(3-) (delta) .

94 Strontium-90 ((90)Sr) is the major long-lived radionuclide derived from th

95 , removed only 14 and 25% of (226)Ra and (90)Sr, respectively.

96 ed for its ability to uptake (226)Ra and (90)Sr.

97 at there is a clear relationship between (90)Sr and Q.

98 In contrast, (90)Sr is a radionuclide of sole anthropogenic origin, produ

99 rent radionuclides ((131)I, (134,137)Cs, (90)Sr-(90)Y, (103)Ru and (239,240)Pu) in terms of the radia

100 tration and the concentration-discharge ((90)Sr-Q) relationship in stream water since the accident.

101 For (90)Sr analysis, the method makes use of stable strontium as

102 For (90)Sr determination, tap water and milk powder samples were

103 We show that the slow decline in (90)Sr follows a double-exponential function, and that there

104 ackground media solution did not inhibit (90)Sr and (226)Ra uptake by G. lithophora.

105 r the determination of ultra-trace level (90)Sr has been recently developed applying thermal ionizati

106 tudy is the first to reveal that the log((90)Sr)-log(Q) slope has been gradually decreasing since the

107 This suggested that sequestration of (90)Sr and (226)Ra was not intrinsic to all cyanobacteria bu

108 t is not caused by the physical decay of (90)Sr and environmental diffusion, but implies that the con

109 226)Ra within 144 h and 47.9 ng g(-1) of (90)Sr within 1 h, corresponding to ~99% removal of trace ra

110 ug g(-1) of (226)Ra and 8.87 ng g(-1) of (90)Sr.

111 the samples followed by determination of (90)Sr/(88)Sr abundance sensitivity (2.1 x 10(-10)).

112 ong-term decrease in the dissolved-phase (90)Sr concentration and the concentration-discharge ((90)Sr

113 history of inorganic mass-spectrometry, (90)Sr analysis using a TIMS instrument is confirmed by an i

114 accurately represents both the long-term (90)Sr trend in stream water and the time-dependency of the

115 el to explain the time-dependency of the (90)Sr-Q relationship.

116 eam water and the time-dependency of the (90)Sr-Q relationship.

117 g(-1) and 2.5 +/- 0.1 ug g(-1) while the (90)Sr/(88)Sr isotope ratios were 6.47 +/- 0.17 x 10(-8) and

118 nique ability of G. lithophora to uptake (90)Sr and (226)Ra at high rates makes it an attractive cand

119 NIST SRM 987 Sr was used as an internal standard, and the reproducibi

120 arch for an expected 'split' transition in a Sr(2)RuO(4) crystal under in-plane uniaxial pressure, wh

121 halcogenides A(2) Ni(II) O(2) Ag(2) Se(2) (A=Sr, Ba) with the S=1 NiO(2) square lattice are now repor

122 % in a simple resistor structure made of AFM Sr(2)IrO(4) without auxiliary reference layer.

123 ted particles of eight elements (Na, Al, Ag, Sr, Ca, Mg, Fe, and Be) were injected into the conical t

124 3)La(0.7)NiO(3), SrNi(0.75)Co(0.25)O(3), and Sr(0.25)Ba(0.75)NiO(3), are among the oxide perovskite c

125 n 366 were investigated for their Si, B, and Sr isotope signatures (delta(30)Si, delta(11)B, and (87)

126 Ba + Sr + SO(4) and the proportion of Ba and Sr in Ba(x)Sr(1-x)SO(4) depended upon the Ba/Sr ratio in

127 V, Eu(III) at 114 BV, Ce(III) at 126 BV, and Sr(II) at 100.

128 OFs to degrade and release osteogenic Ca and Sr ions was investigated.

129 eous medium, and capable of releasing Ca and Sr ions.

130 generated by choosing osteoinductive Ca and Sr metals, and an organic ligand 1,3,5 tricarboxylicbenz

131 mal fluids are not typical due to low Ca and Sr relative to Mg and SO4 in modern seawater.

132 compositions, major- and trace elements, and Sr-Nd-Pb-O isotope ratios, supporting that the two outcr

133 to 2016, based on paired oxygen isotope and Sr/Ca measurements.

134 In this study, Ba, Ca, Mg, Mn and Sr contents were determined in 215 wines from several We

135 f seven elements (Ba, Ca, Fe, Mg, Mn, Na and Sr).

136 Nd and Sr isotopic measurements suggest that a distinct source

137 ices possessing both anion-vacancy order and Sr and Ca chemical order at the subnanometer scale, conf

138 We used regional daily secretion rates and Sr marker-lines to reconstruct tooth growth along the en

139 ilities observed for (87)Sr/(86)Sr ratio and Sr concentrations in authentic Bordeaux wines, which can

140 The (87)Sr/(86)Sr ratio and Sr concentrations of 43 authentic Bordeaux wines from th

141 Al, As, Ba Cd, Co, Ni, P, Pb, Sb, Sn and Sr showed values below the LOD.

142 (delta(11)B = 22.9 +/- 3.5 per thousand) and Sr ((87)Sr/(86)Sr = 0.70923 +/- 0.00024) isotope ratios

143 the two waters can precipitate HFFF-Ba and -Sr with AMD-SO(4), therefore removing them from solution

144 FF enriched in alkaline earth metals such as Sr and Ba, known to cause scaling issues in oil and gas

145 rtilization and artificial reagents, such as Sr(2+), which also leads to CaMKII activation.

146 the best optical clocks using neutral atoms (Sr, Yb, Hg) and is competitive with that of ion optical

147 cidic solution as the solution can etch away Sr atoms.

148 at maximize total removal efficiencies (Ba + Sr + SO(4)) for reuse in O&G development.

149 Total removal efficiencies of Ba + Sr + SO(4) and the proportion of Ba and Sr in Ba(x)Sr(1-

150 Ba, Sr, and cyclic hydrocarbons indicated the potential to a

151 alose, arabinose and raffinose, elements Ba, Sr, P, Cd and Se, and delta(13)C values of honey, have d

152 Increasing Ba/Sr ratios can enhance total removal efficiency but decre

153 Sr in Ba(x)Sr(1-x)SO(4) depended upon the Ba/Sr ratio in the initial HFFF.

154 ersaturated solution with respect to barite, Sr-rich barite nanoparticles formed on organics, while m

155 sides (no internal electric field) for both Sr-rich and stoichiometric interfaces, while the DFT-cal

156 ution catalyst in neutral pH, Brownmillerite Sr(2)GaCoO(5), with the specific activity about one orde

157 s holes introduced via substitution of La by Sr segregate into lines to form boundaries between magne

158 principles predictions that the AMX (A = Ca, Sr, Ba; M = Cu, Ag, Au; X = P, As, Sb) compounds consist

159 (+) (A=Li, Na, K, Rb and Cs), AE(2+) (AE=Ca, Sr, Ba) and Mn(2+) demonstrate that the dimensionality o

160 yers being more susceptible to loss, and Ca, Sr and Zn are more sensitive to the parboiling hydrother

161 libration linearity for tested elements (Ca, Sr, and K), quick data collection times, and Limits of D

162 transition metals); phase transitions in Ca, Sr, and Ba correlating well with s->d transitions; spin-

163 Adding elements Mg, Ca, Sr and Li into Zn can improve the cytocompatibility, ost

164 The alkaline-earth elements (Be, Mg, Ca, Sr, and Ba) strongly favor the formation of diamagnetic

165 tal clusters [M(mu-OH)(2)M](2+) (M = Mg, Ca, Sr, Ba, and HOAl).

166 ary Zn alloys with alloying elements Mg, Ca, Sr, Li, Mn, Fe, Cu, and Ag respectively, are screened sy

167 ional markers: Playa (Mg, SO(4)(2-), Na, Ca, Sr), Colorado Alluvium (U, Ca), Local Alluvium (Al, Fe,

168 recently characterized octacarbonyls of Ca, Sr, and Ba mimic the classical Dewar-Chatt-Duncanson bon

169 RAs(3) where R = Ca, Sr, thus, offers a unique opportunity to realize an arch

170 m(3+) , with alkaline-earth (M) spanning Ca, Sr, and Ba, MgSr, CaSr, CaBa, SrBa, and CaSrBa.

171 he type of TDS (i.e., Na only vs Na-Mg-Ba-Ca-Sr) influenced self-attenuation in well-detector gamma s

172 Ca-, Sr-, and Ba-doped LaMnO(3) are selected as model systems

173 ation technique) was obtained using combined Sr isotope amount ratios and multi-elemental data.

174 ts using water-soluble and growth-compatible Sr(3)Al(2)O(6) hard masks.

175 As was expected, the scaffolds containing Sr(2+)-doped fluorapatite, presented high osteoconductiv

176 and trace elements (Li, Mg, Mn, Ni, Co, Cu, Sr, Ba, Pb) via chemometric evaluation facilitated class

177 cting pairing in the M(x)Bi(2)Se(3) (M = Cu, Sr, Nb) superconductor family.

178 average, took up 8 to 18% more rock-derived Sr than five co-occurring nonfixing tree species, includ

179 ynthesized using sol gel method at different Sr content x = 0.3, 0.5, 0.7, and 0.9.

180 In contrast, divalent Sr(II) forms an ion-extractant complex with DHDP that le

181 e band structure of hole- and electron-doped Sr(2)IrO(4) are striking given the different internal st

182 (2)) and surface-electron-doped Sr(2)IrO(4), which exhibits spectroscopic signatures con

183 re, we synthesize and investigate hole-doped Sr(2-x)K(x)IrO(4) utilizing a combination of reactive ox

184 l experiments using glassy carbon electrode, Sr(2) Fe(2) O(6-delta) shows better OER activity than th

185 sotopic compositions of lithophile elements (Sr, Nd, Hf) in these lavas require derivation from a man

186 he adsorption-controlled growth of epitaxial Sr(3) SnO single-crystal films by molecular-beam epitaxy

187 nonstoichiometry of a model perovskite film, Sr(Ti,Fe)O(3-) (y) , is reported and the lattice vibrati

188 oss the forest, and only N fixers had foliar Sr isotopes that differed significantly from soil exchan

189 element and ranged between 0.1 mg kg(-1) for Sr and 42 mg kg(-1) for P.

190 study provides a mechanistic explanation for Sr-rich marine barite formation and offers insights for

191 t of imitated Bordeaux wines was studied for Sr isotopic and elemental compositions.

192 strength of the Lewis acid sites (Mg > Ca > Sr > Ba) was characterized by a blue shift of characteri

193 We measured He-Sr-Pb isotope ratios in superdeep diamond fluid inclusio

194 ver, the reason for the occurrence of higher Sr content in marine barites than expected for classical

195 heric) with anomalous (182)W and examine how Sr-Nd-Hf-Pb isotopic variations-useful for tracing subdu

196 In Sr(2)RuO(4) films deposited on tetragonal substrates the

197 the magnetic moments for the bilayer, as in Sr(3)Ir(2)O(7).

198 ified interlayer coupling by 1% Ga-doping in Sr(2)IrO(4).

199 lds and non-zero electric field gradients in Sr(2)IrO(4) have been detected and attributed to the str

200 ffects of NTCP inhibition were maintained in Sr-b1(-/-) mice, eliminating the possibility that the in

201 actual or incipient electronic nematicity in Sr(2)RuO(4).

202 to probe the nature of superconductivity in Sr(2)RuO(4) and its evolution under strain.

203 n field of spin-orbit-coupled Mott insulator Sr(2) IrO(4) can be in situ modulated by almost 300%.

204 of reverse micelles formed from interfacial Sr(II) ion-extractant complexes could transport Sr(II) a

205 ratios (15.5-15.6) and relatively invariant Sr, Nd, and Hf isotopes, the data suggest that this sour

206 , RE resin, and again Ln resin for isolating Sr and Pb, LREE then La-Ce-Nd-Sm, Lu(Yb), and Hf, Th, an

207 an the rate limiting step on the Sr-rich (La,Sr)O termination.

208 tentially be obtained by suppressing the (La,Sr)O termination and stabilizing highly active CoO(2) te

209 a(2) Fe(2) O(6-delta) <CaSrFe(2) O(6-delta) <Sr(2) Fe(2) O(6-delta) .

210 ds M(15)Tr(22)As(32) and M(3)Ga(6)As(8) (M = Sr, Eu; Tr = Ga, In) were synthesized by heating the ele

211 2) N}M{B(NDippCH)(2) }(thf)(n) (M=Ca, n=2; M=Sr, n=3), through the reactions of the corresponding bis

212 um in the antiperovskite-type Dirac material Sr(3)SnO.

213 compounds, but several elements (Ba, Ca, Mg, Sr, Mn, Al, Co, Ni, Se) were marked as characteristic of

214 further determination of Al, Cr, Cu, Fe, Mn, Sr, and Zn.

215 We show that elements such as Na, Sr, and S dissolved readily and therefore were fully rec

216 ent cuprates, yet the intrinsic behaviour of Sr(2)IrO(4) upon hole doping remains enigmatic.

217 ncentrations and increased concentrations of Sr.

218 ments on a superconducting single crystal of Sr(0.1)Bi(2)Se(3), a prime candidate for realizing topol

219 d quantum state preparation and detection of Sr(+) qubits.

220 The evolution of Sr(2)IrO(4) upon carrier doping has been a subject of in

221 The successful realization of thin films of Sr(3) SnO opens opportunities to manipulate topological

222 n our samples as a result of the increase of Sr contents from 0.3 to 0.7wt %.

223 Elevated levels of Sr validate the assumed heavy vegetative diets of poor a

224 ve for wine authenticity control by means of Sr isotopic and elemental composition.

225 ffer an enhanced discriminating potential of Sr.

226 osed for samples requiring the separation of Sr, Pb, Nd, and Hf only.

227 We find that substitution of Sr in the A-site drives the system into a metallic state

228 similar to the local macro-fauna in terms of Sr isotopic signal, the Epigravettians are shifted towar

229 We propose that coupled use of Sr/Y and La/Yb is a feasible method for reconstructing c

230 ttributed to the rotation of the d-vector of Sr(2)RuO(4).

231 the prediction that the antiperovskite oxide Sr(3) SnO is a topological crystalline insulator, a new

232 We found extreme He-C-Pb-Sr isotope variability, with high (3)He/(4)He ratios rel

233 le precipitates, discordant Ag atoms, and Pb/Sr, Pb/Ba point defects in the PbSe matrix work together

234 The bilayer perovskite Sr(3)Ru(2)O(7) has been widely studied as a canonical st

235 mensional and strongly correlated perovskite Sr(2)RuO(4) is considered to be the only solid-state ana

236 two B-site cations in the double perovskite Sr(2) Fe(1+) (x) Re(1-) (x) O(6) (-0.2 <= x <= 0.2) are

237 m noncentrosymmetric and ferroelectric-phase Sr(3) Sn(2) O(7) doped with rare earth Nd(3+) ions.

238 ontium removal, specifically for radioactive Sr(90).

239 ttians are shifted towards higher radiogenic Sr ratios.

240 , Ca, V, Cr, Mn, Fe, Co, Cu, Zn, Se, Br, Rb, Sr, Mo, I, Cs, and Ba) in 10 muL of serum and 12 element

241 P, S, K, Ca, Cl, Mn, Fe, Ni, Cu, Zn, Br, Rb, Sr.

242 nts were chosen: Ti, Mn, Fe, Cu, Zn, Br, Rb, Sr.

243 ariables (Na, Mg, Al, V, Co, Ni, As, Se, Rb, Sr, Mo, Hg, delta(2)H, delta(18)O, delta(13)C and K/Rb).

244 se commercially available extraction resins (Sr resin, TRU resin, Ln resin, RE resin, and again Ln re

245 es formed on organics, while micrometer-size Sr-poor barites formed in bulk solutions.

246 , Fe, K, Mg, Mn, Mo, Na, Ni, Pb, Sb, Se, Sn, Sr, V, Tl and Zn, presenting the differences and migrati

247 ntly developed method based on water-soluble Sr(3)Al(2)O(6) as the sacrificial buffer layer(13,14) we

248 The mobility of stable Sr and Cs (as analogs for their radioactive counterparts

249 The stable Sr concentrations were 39.4 +/- 0.9 ng g(-1) and 2.5 +/-

250 he known FM metallic phase in stoichiometric Sr(2) FeReO(6) , an FMI state with a high Curie temperat

251 the anomalous transport observed in strained Sr(2)RuO(4).

252 properties of lanthanum (La) and strontium (Sr) doped rhombohedral bismuth ferrite within density fu

253 Here we use strontium (Sr) isotopes as a tracer of nutrient sources in a mixed-

254 ctural examples include bulk superconducting Sr(2)RuO(4) (ref.

255 y deposited on a spin-triplet superconductor Sr(2)RuO(4), without any electronic spin-flip scattering

256 n films of the unconventional superconductor Sr(2)RuO(4) grown on various substrates.

257 ace by in situ reconstruction of the surface Sr enrichment region in perovskite LSC to activate surfa

258 spectroscopy studies of Bi[Formula: see text]Sr[Formula: see text]CaCu[Formula: see text]O[Formula: s

259 Our findings indicate that Sr(3)CrN(3) is the first known electride with a partiall

260 bined with geochemical analyses, reveal that Sr was incorporated into the CaCO(3) concretions during

261 d X-ray and neutron diffraction to show that Sr(3)CrN(3) is indeed an electride despite its partial d

262 The Sr and Ba atoms diminish the contribution of Pb 6s(2) st

263 The Sr enrichment in barites formed on organic films was fou

264 Here, we present temporal variations in the Sr isotope composition of 14 human deciduous teeth and t

265 olid-solution nucleation rates; instead, the Sr-poor barite formation in bulk solution was found to b

266 report on optical spectroscopic study of the Sr(3)(Ir(1-x)Ru(x))(2)O(7) system over a wide doping reg

267 s resolved by employing a compilation of the Sr, Nd, and Hf isotope composition of kimberlites-volcan

268 es faster than the rate limiting step on the Sr-rich (La,Sr)O termination.

269 esent better antibacterial response than the Sr(2+) doped material.

270 graphical zones were classified according to Sr, Ba, Ni, and Cu.

271 II) ion-extractant complexes could transport Sr(II) across the interface.

272 mplies that a second process that transports Sr(II) across the interface has yet to be observed.

273 layered metal oxide, Ruddlesden-Popper-type Sr(2)RuO(4) with alternative perovskite layer and rock-s

274 The unique Sr binary signature may detect imitated wines and trace

275 Using Sr(2)GaCoO(5) to catalyze oxygen evolution, the integrat

276 Acidic solutions containing U(VI), Sr(II), Eu(III), and Ce(III) were used to determine the

277 n voltage of 1.65 V, and a radiance of 2.7 W Sr(-1) m(-2) when driven at 4.5 V.

278 iate wines from studied grape varieties were Sr, Ca, Mg and Mn.

279 despite spatial variation in community-wide Sr sources across the forest, and only N fixers had foli

280 fluorapatite was synthesised and doped with Sr(2+) and Ce(3+) ions in order to tailor its properties

281 cofactors in which Ca(2+) is exchanged with Sr(2+); the Mn(4)O(5)Sr cofactor remains active, but the

282 ynamics of the hydroxyl free-radical OH with Sr atoms leading to quenching of OH hyperfine states.

283 ical cycling, a surface reconstruction, with Sr and Co leaching, over SrCo(0.9)Ir(0.1)O(3-delta) occu

284 orthy as the (Ni/Ru)H(2) sheets in the La(x) Sr(4-x) NiRuO(4) H(4) phases are structurally analogous

285 then converting into the corresponding La(x) Sr(4-x) NiRuO(4) H(4) phases.

286 irst preparing precursors in the range La(x) Sr(4-x) NiRuO(8) 0.5<x<1.4 and then converting into the

287 Sr-bearing marine barite [(Ba (x) , Sr(1-x) )SO(4)] cycling has been widely used to reconstr

288 The photocatalytic performance of the Nd(1-x)Sr(x)MnO(3) nanocomposites for photodegradation of Acrid

289 Nd(1-x)Sr(x)MnO(3) nanocomposites perovskites were synthesized

290 The Energy gap of the Nd(1-x)Sr(x)MnO(3) nanocomposites were estimated for all concen

291 findings shows convincingly that the Nd(1-x)Sr(x)MnO(3) photocatalysts possess great promise for vis

292 films of the infinite-layer nickelate Nd(1-x)Sr(x)NiO(2) (x = 0.12-0.25) which is believed to have th

293 ring, we study the archetypal cuprate La(2-x)Sr(x)CuO(4) (LSCO) over a broad doping range.

294 uality La(2-x)Sr(x)CuO(4)/La(2)CuO(4)/La(2-x)Sr(x)CuO(4) (LSCO/LCO/LSCO) heterostructures fabricated

295 )CuO(4), La(1.8-x)Eu(0.2)Sr(x)CuO(4), La(2-x)Sr(x)CuO(4) and Bi(2)Sr(2-x)La(x)CuO(6+delta).

296 By contrast for La(2-x)Sr(x)CuO(4) thin films, such substrates are sub-optimal

297 of tunnelling current in high-quality La(2-x)Sr(x)CuO(4)/La(2)CuO(4)/La(2-x)Sr(x)CuO(4) (LSCO/LCO/LSC

298 found in single-layer nickelates like La(2-x)Sr(x)NiO(4).

299 tion within 1 day of mixing in the form Ba(x)Sr(1-x)SO(4) and no further significant precipitation oc

300 O(4) and the proportion of Ba and Sr in Ba(x)Sr(1-x)SO(4) depended upon the Ba/Sr ratio in the initia