ライフサイエンスコーパス: alkaline earth metal

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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