ライフサイエンスコーパス: alkaline-earth

1 2), where x, m, and n specify the amounts of alkaline earth, 6-coordinated silicon, and 4-coordinated

2 ctural and reaction chemistry of the heavier alkaline earth (Ae = Mg, Ca, Sr, Ba) elements.

3 c nonapeptide oxytocin (OT) with a number of alkaline earth and divalent transition metal ions (X(2+)

4 iodide perovskites centered around divalent alkaline earth and lanthanide elements, with the general

5 ecognition of Ag(+) among 20 various alkali, alkaline earth and transition metal ions.

6 and the nature and concentration of alkali, alkaline earth, and NH4+ ions in the test media.

7 With available alkaline, alkaline earth, and organic cations as partners, four se

8 t basic functionalities by utilizing alkali, alkaline earth, and transition metals (Na+, K+, Ca2+, Ba

9 yanine systems to selectively detect alkali, alkaline earth, and transition-metal cations.

10 ransition metals Co, Rh, and Ir, the alkali, alkaline-earth, and rare-earth elements, and Sb4 polyani

11 cluster exhibits properties analogous to an alkaline earth atom.

12 ity of two valence electrons within the same alkaline-earth atom, thereby providing insight into the

13 ds for observing Weyl quasiparticles in cold alkaline-earth-atom systems.

14 dances reaching about 10(-4) relative to the alkaline earth atomic ion abundances.

15 Exploring new atomic species, such as alkaline earth atoms(5-7), or combining multiple species

16 This study lays the groundwork for using alkaline-earth atoms as testbeds for important orbital m

17 erasure errors observed via fast imaging of alkaline-earth atoms(19-22), we achieve a Bell state fid

18 bon nanodots within crystalline particles of alkaline earth carbonates, sulphates and oxalates.

19 ble 2-naphthols and 2-oxo aldehydes using an alkaline earth catalyst [Ca(OTf)(2)].

20 ohols and alpha-acyl cyclic ketones using an alkaline earth catalyst under solvent-free conditions.

21 The divalent alkaline earth cations (Mg(2+), Ca(2+), and Ba(2+)) all

22 discrimination against higher charge density alkaline earth cations (Mg2+ and Ca2+) and smaller alkal

23 The divalent alkaline earth cations give aK(PLP) values approximately

24 Replacing Ca(2+) with larger alkaline-earth cations (Sr(2+), Ba(2+)) induces predicta

25 dent on the identity and amount of alkali or alkaline-earth cations present during crystallization.

26 what attributes engendered success in heavy alkaline earth complexation.

27 ation, which is found to be realized for the alkaline-earth complexes and, in a variant form, for the

28 The alkaline-earth complexes prefer a highly compact caged s

29 The hydration of some of the alkaline earth divalent metal cations and first row tran

30 charged helix than dsDNA, is precipitated by alkaline-earth divalent cations that are unable to conde

31 ORR on eight platinum (Pt)-lanthanide and Pt-alkaline earth electrodes, Pt5M, where M is lanthanum, c

32 The alkaline-earth element adopts the oxidation state +2, wh

33 The alkaline-earth element bis(trimethylsilyl)amides, [Ae{N(

34 from improved chelation strategies for heavy alkaline earth elements: Ra(2+), Ba(2+), and Sr(2+).

35 The alkaline-earth elements (Be, Mg, Ca, Sr, and Ba) strongl

36 Each alkaline earth exhibits different phase behavior in the

37 We synthesize 8 alkaline-earth host materials doped with Yb(3+) and Tm(3

38 The use of heavier alkaline earth hydride derivatives as pre-catalysts and

39 ting the long-known chemistry of the heavier Alkaline Earth hydrides.

40 Although the heavy alkaline-earth hydrides are of limited interest for thei

41 These results suggest that the alkaline-earth hydrides form an important new family of

42 ]) CNCs that were ionically crosslinked with alkaline-earth (i.e., [Formula: see text]) or transition

43 gether under ambient conditions, we examined alkaline earth ion substitution for two A, i.e., materia

44 only the primary ion, but also the secondary alkaline earth ion, based on the ion-exchange mechanism,

45 ge, and strongly reject all other alkali and alkaline earth ions.

46 PhePhe and for complexes of PhePhe with the alkaline-earth ions Ba(2+) and Ca(2+), the alkali-metal

47 m the transfer of electrons from alkaline or alkaline-earth ions to the C60 molecule, which is known

48 nounced effects observed among the series of alkaline-earth ions with Ca2+.

49 Upon the stimulation by alkaline-earth ions, the lipid layers appeared to underg

50 SrTiO(3) or BaTiO(3) templates to match the alkaline-earth layer in the Ba-122 with the alkaline-ear

51 Alkaline-earth Lewis acid sites yield increased benzene

52 icles has excellent selectivity over alkali, alkaline earth (Li(+), Na(+), K(+), Mg(2+), Ca(2+)), and

53 Hypermetallic alkaline earth (M) oxides of formula MOM have been studi

54 aterials doped with Yb(3+) and Tm(3+) , with alkaline-earth (M) spanning Ca, Sr, and Ba, MgSr, CaSr,

55 f the structure and electronic properties in alkaline earth metal acetylides with high-resolution mic

56 sitive ion mode CAD with/without alkaline or alkaline earth metal adduction, the ratio of product ion

57 s possessing disulfide bonds with sodium and alkaline earth metal are generated using electrospray io

58 rigid 7 K argon matrix containing alkali or alkaline earth metal atoms and NO(2) isolated from each

59 The oxide QC formation is forced by large alkaline earth metal atoms and the reduction of their mu

60 asis for analyzing the binding of alkali and alkaline earth metal atoms over a broad range of systems

61 designing and developing 1D architecture of alkaline earth metal carbonates by a simple method witho

62 ionophore-facilitated transfer of a smaller alkaline earth metal cation with higher hydrophilicity a

63 The structures of isolated alkaline earth metal cationized amino acids are investig

64 The behavior of alkaline earth metal cations (Mg2+ and Ca2+) and transit

65 In contrast to alkaline earth metal cations (Mg2+ and Ca2+), different

66 rference effects from other alkali metal and alkaline earth metal cations and has good stability and

67 est in free energy in complexes with smaller alkaline earth metal cations and that zwitterionic forms

68 The binding of alkali and alkaline earth metal cations by macrocyclic and diazamac

69 an indeed function as ligands for alkali and alkaline earth metal cations in a manner similar to that

70 the same conclusions are valid for divalent alkaline earth metal cations.

71 nce-dependent dsDNA condensation by divalent alkaline earth metal cations.

72 vation of singly charged cationic alkali and alkaline earth metal complexes, which results in the hig

73 Alkali and alkaline earth metal compounds in the dust dissolve in w

74 The approach, based on measuring alkali and alkaline earth metal content, revealed that adulterated

75 Divalent alkaline earth metal ions condensed triple-stranded (ts)

76 model systems for understanding the roles of alkaline earth metal ions in nucleic acid processing.

77 The effect of alkali and alkaline earth metal ions on the reactions of the cumylo

78 cated that Cd(II) and the heavier and larger alkaline earth metal ions Sr(II) and Ba(II) were effecti

79 ) among 14 different transition, alkali, and alkaline earth metal ions studied.

80 A series of alkaline earth metal ions was tested for the ability to

81 Similar to the alkaline earth metal ions, application of Cd(2+) elicite

82 sequence genomic DNA, AA-TT condenses in all alkaline earth metal ions.

83 clease that prefers transition metal ions to alkaline earth metal ions.

84 resence of transition metal ions compared to alkaline earth metal ions.

85 Herein, we present the alkaline earth metal nitridophosphate oxide Ba(3)[PN(3)]

86 daries in highly ionic materials such as the alkaline earth metal oxides and alkali halides.

87 ing solid CO(2) sorbents based on alkali and alkaline earth metal oxides operating at medium to high

88 infinite-layer compound ACuO2 (where A is an alkaline earth metal)-is an excellent way of investigati

89 e" structure of stoichiometry AeTiO(2) (AE = alkaline earth metal, Be, Mg, Ca, Sr, and Ba), we find s

90 own SHG active AMCO3F (A = alkali metal, M = alkaline earth metal, Zn, Cd, or Pb) materials indicates

91 The unique optical cycling efficiency of alkaline earth metal-ligand molecules has enabled signif

92 ntial clusters with a planar hypercoordinate alkaline-earth metal (phAe) as the lowest-energy form.

93 dy investigates the use of common alkali and alkaline-earth metal additives to enhance the mineraliza

94 Alkali- and alkaline-earth metal amidoboranes are a new class of com

95 lery-mode microlaser scheme, where ultracold alkaline-earth metal atoms, i.e., gain medium, are tight

96 Here, we report that alkaline-earth metal beryllium atoms react with OF(2) to

97 tions to compare the solvation of alkali and alkaline-earth metal cations in water and liquid CO(2) a

98 as optical molecular sensors for alkali and alkaline-earth metal cations.

99 Extra-framework alkaline-earth metal containing species and aluminum spe

100 cleavage was detected in the presence of the alkaline-earth metal ions Mg(2+), Ca(2+), Sr(2+), and Ba

101 also actively compensated by rare-earth and alkaline-earth metal ions of the interface.

102 Recently, alkaline-earth metal Sr intercalated Bi2Se3 has been rep

103 r chalcogen (Se, Te) of the type AFFeAs (A = alkaline-earth metal), AFe(2)As(2), AFeAs (A = alkali me

104 The calculations also predict that alkaline-earth metal-porphyrin COFs could catalyze the d

105 The FP-APW calculations show that alkaline-earth-metal and germanium orbitals, particularl

106 ctivity for lead over other alkali-metal and alkaline-earth-metal ions.

107 he strong binding affinity between U(IV) and alkaline earth metals (Ca(2+)/Mg(2+)/Sr(2+)/Ba(2+)), tra

108 , and all elements other than the alkali and alkaline earth metals (Ca, Mg, Sr, K, and Na) are positi

109 Doubly charged molecular ions of alkaline earth metals and argon could be identified as s

110 ed understanding of the interactions between alkaline earth metals and DOM under conditions that are

111 rgan and others is that fluxes of alkali and alkaline earth metals are required for signaling, but tr

112 Divalent cations of two alkaline earth metals Ca(2+) and Mg(2+) and the transiti

113 t actinides and rare earth metals as well as alkaline earth metals can be encapsulated within a varie

114 ular complexes of the terrestrially abundant alkaline earth metals have also demonstrated promise wit

115 tal amidoborane compounds of the alkali- and alkaline earth metals have in recent years found applica

116 ither a preferential accumulation of heavier alkaline earth metals nor core-shell structures in the c

117 Alloys of platinum with alkaline earth metals promise to be active and highly st

118 e gas wells generally yield HFFF enriched in alkaline earth metals such as Sr and Ba, known to cause

119 This indicated that fractionation between alkaline earth metals was not inherent to intracellularl

120 e to calcium(ii) (such as the lanthanides or alkaline earth metals), and in a few key cases this targ

121 al contained higher concentrations of salts, alkaline earth metals, and organic chemicals.

122 robe is selective for Hg(II) over alkali and alkaline earth metals, most divalent first-row transitio

123 ite general phenomenon: among the alkali and alkaline earth metals, Na and Mg generally have the weak

124 the presence of secondary metal ions, e.g., alkaline earth metals, transition metals, lanthanide met

125 up of cyclohexanol and phenol with alkali or alkaline earth metals.

126 lithium attracts interest in other alkali or alkaline earth metals.

127 ter by co-precipitation with barium or other alkaline earth metals.

128 ly relevant concentrations of the alkali and alkaline earth metals.

129 ormation using the d orbitals of the heavier alkaline-earth metals (Ae = Ca, Sr, Ba), the so-called "

130 Our model considers perovskites containing alkaline-earth metals (Ca, Sr, and Ba) and lanthanides (

131 The polymer does not interact with alkaline, alkaline-earth metals and transition metals.

132 clathrate type-I crystals containing alkali/alkaline-earth metals have been extensively studied, but

133 eolites, by incorporation of extra-framework alkaline-earth metals or by demetalation with dealuminat

134 as facilitated through the use of alkali and alkaline-earth metals, which selectively fill the availa

135 ed bonds catalyzed by alkali (Li, Na, K) and alkaline earth (Mg, Ca, Sr, Ba) metals, we provide a det

136 d in terms of the outer core orbitals of the alkaline earth mixing with the valence of the halogens a

137 ne, with and without added cations (Ce(IV) , alkaline earths, Mn(II) ), shows the metals' differentia

138 m intact in sharp contrast to the bonding in alkaline-earth monohydroxides and YbOH, where an electro

139 Alkaline-earth (most prominently barium) complexes of th

140 Replacing Mg(2+) with alkaline earths of increasing ionic radii (Ca(2+), Sr(2+

141 (2)](2) (Fp(2)) gave the isostructural heavy alkaline earth or divalent rare earth compounds [MFp(2)(

142 alkaline-earth layer in the Ba-122 with the alkaline-earth/oxygen layer in the templates opens new a

143 tic approach to the synthesis of fluorescent alkaline-earth perovskite oxide nanocrystals under ultra

144 ze of hydrocarbon ligands attached to single alkaline-earth phenoxides from -H to -C(14)H(19) while m

145 iamondoids and diamond surfaces suggest that alkaline-earth phenoxides may maintain their desirable s

146 scriminate the 57 species, including alkali, alkaline earth, post-transition, transition, and lanthan

147 the NIR-to-UV/visible emission of sub-15 nm alkaline-earth rare-earth fluoride UCNPs (M(1-x) Ln(x) F

148 c strontium isotopes ((87)Sr/(86)Sr) and the alkaline earth ratios (AERs) Sr/Ca and Ba/Ca in fossil d

149 ss OH(-) ions, mitigate Cl(-) corrosion, and alkaline earth salt precipitation.

150 ing fragments must be free from alkaline and alkaline earth salts as well as other contaminants for a

151 lly shown that in the presence of alkali and alkaline earth salts, oxidation of Cr(III) takes place,

152 neralization based on aqueous carbonation of alkaline earth silicate minerals is a promising route to

153 Recent syntheses of high-pressure alkali and alkaline earth silicates reveal a class of framework str

154 the favourable properties of tweezer-trapped alkaline-earth (strontium-88) atoms(8-10), and introduce

155 In particular, alkaline-earth sulfides are an important class of host m

156 f 13 new phases and crystal structures of 11 alkaline earth tartrates, including an unusual I(3)O(0)

157 ze the heterogeneous interactions of alkali, alkaline earth, transition and other metal ions and thei

158 r 23 elements from the categories of alkali, alkaline earth, transition, and poor metals.

159 ing of the outer core p(n-1) orbitals of the alkaline earth with the valence s and p orbitals of the