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1 ter by co-precipitation with barium or other alkaline earth metals.
2 ly relevant concentrations of the alkali and alkaline earth metals.
3 up of cyclohexanol and phenol with alkali or alkaline earth metals.
4 lithium attracts interest in other alkali or alkaline earth metals.
5 f the structure and electronic properties in alkaline earth metal acetylides with high-resolution mic
6 dy investigates the use of common alkali and alkaline-earth metal additives to enhance the mineraliza
7 sitive ion mode CAD with/without alkaline or alkaline earth metal adduction, the ratio of product ion
8 ormation using the d orbitals of the heavier alkaline-earth metals (Ae = Ca, Sr, Ba), the so-called "
9 r chalcogen (Se, Te) of the type AFFeAs (A = alkaline-earth metal), AFe(2)As(2), AFeAs (A = alkali me
12 ed understanding of the interactions between alkaline earth metals and DOM under conditions that are
15 e to calcium(ii) (such as the lanthanides or alkaline earth metals), and in a few key cases this targ
17 s possessing disulfide bonds with sodium and alkaline earth metal are generated using electrospray io
18 rgan and others is that fluxes of alkali and alkaline earth metals are required for signaling, but tr
19 rigid 7 K argon matrix containing alkali or alkaline earth metal atoms and NO(2) isolated from each
20 The oxide QC formation is forced by large alkaline earth metal atoms and the reduction of their mu
21 asis for analyzing the binding of alkali and alkaline earth metal atoms over a broad range of systems
22 lery-mode microlaser scheme, where ultracold alkaline-earth metal atoms, i.e., gain medium, are tight
23 e" structure of stoichiometry AeTiO(2) (AE = alkaline earth metal, Be, Mg, Ca, Sr, and Ba), we find s
26 he strong binding affinity between U(IV) and alkaline earth metals (Ca(2+)/Mg(2+)/Sr(2+)/Ba(2+)), tra
27 , and all elements other than the alkali and alkaline earth metals (Ca, Mg, Sr, K, and Na) are positi
28 Our model considers perovskites containing alkaline-earth metals (Ca, Sr, and Ba) and lanthanides (
29 t actinides and rare earth metals as well as alkaline earth metals can be encapsulated within a varie
30 designing and developing 1D architecture of alkaline earth metal carbonates by a simple method witho
31 ionophore-facilitated transfer of a smaller alkaline earth metal cation with higher hydrophilicity a
35 rference effects from other alkali metal and alkaline earth metal cations and has good stability and
36 est in free energy in complexes with smaller alkaline earth metal cations and that zwitterionic forms
38 an indeed function as ligands for alkali and alkaline earth metal cations in a manner similar to that
41 tions to compare the solvation of alkali and alkaline-earth metal cations in water and liquid CO(2) a
43 vation of singly charged cationic alkali and alkaline earth metal complexes, which results in the hig
46 The approach, based on measuring alkali and alkaline earth metal content, revealed that adulterated
47 ular complexes of the terrestrially abundant alkaline earth metals have also demonstrated promise wit
48 tal amidoborane compounds of the alkali- and alkaline earth metals have in recent years found applica
49 clathrate type-I crystals containing alkali/alkaline-earth metals have been extensively studied, but
51 model systems for understanding the roles of alkaline earth metal ions in nucleic acid processing.
53 cated that Cd(II) and the heavier and larger alkaline earth metal ions Sr(II) and Ba(II) were effecti
60 cleavage was detected in the presence of the alkaline-earth metal ions Mg(2+), Ca(2+), Sr(2+), and Ba
63 infinite-layer compound ACuO2 (where A is an alkaline earth metal)-is an excellent way of investigati
64 The unique optical cycling efficiency of alkaline earth metal-ligand molecules has enabled signif
65 robe is selective for Hg(II) over alkali and alkaline earth metals, most divalent first-row transitio
66 ite general phenomenon: among the alkali and alkaline earth metals, Na and Mg generally have the weak
68 ither a preferential accumulation of heavier alkaline earth metals nor core-shell structures in the c
69 eolites, by incorporation of extra-framework alkaline-earth metals or by demetalation with dealuminat
71 ing solid CO(2) sorbents based on alkali and alkaline earth metal oxides operating at medium to high
72 ntial clusters with a planar hypercoordinate alkaline-earth metal (phAe) as the lowest-energy form.
76 e gas wells generally yield HFFF enriched in alkaline earth metals such as Sr and Ba, known to cause
77 the presence of secondary metal ions, e.g., alkaline earth metals, transition metals, lanthanide met
78 This indicated that fractionation between alkaline earth metals was not inherent to intracellularl
79 as facilitated through the use of alkali and alkaline-earth metals, which selectively fill the availa
80 own SHG active AMCO3F (A = alkali metal, M = alkaline earth metal, Zn, Cd, or Pb) materials indicates