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

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

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

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

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

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

10 cluster exhibits properties analogous to an alkaline earth atom.

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

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

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

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

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

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

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

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

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

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

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

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

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

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

25 Each alkaline earth exhibits different phase behavior in the

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

92 (2)](2) (Fp(2)) gave the isostructural heavy alkaline earth or divalent rare earth compounds [MFp(2)(

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

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

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

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

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

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

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

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

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