ライフサイエンスコーパス: aluminosilicate

1 a structure-directing agent for an inorganic aluminosilicate.

2 o make due to the strong inherent acidity of aluminosilicates.

3 preparation of MnFe2O4 and magnetic takovite-aluminosilicate adsorbent via precipitation methodology.

4 of NMR and ESI-MS spectra from the relevant aluminosilicate, aluminate, and silicate solutions revea

5 , we have applied the results to microporous aluminosilicates and aluminophosphates (zeolites).

6 Although aluminosilicates and metal phosphates can form porous op

7 le soil components (e.g., organic matter and aluminosilicates); and (ii) sorption at a specific sorbe

8 Despite the widespread use of amorphous aluminosilicates (ASA) in various industrial catalysts,

9 levitated droplets of a natural Fe2+-bearing aluminosilicate (basalt) melt occurs by chemical diffusi

10 With the aluminosilicate-based host (Al-MCM-41), the loading is f

11 e technologically important porous zeolites (aluminosilicates) because of their extensive use in petr

12 Phosphorus and microporous aluminosilicates, better known as zeolites, have a uniqu

13 s activity as compared to a more traditional aluminosilicate catalyst, further demonstrating the capa

14 Discoloration-resistant calcium aluminosilicate cement has been formulated to overcome t

15 ffect of the discoloration-resistant calcium aluminosilicate cement on osteogenesis by differentiated

16 Because binding to montmorillonite (an aluminosilicate clay mineral) or clay-enriched soils had

17 trimethylammonium, oxytetracycline) with two aluminosilicate clay minerals and one soil.

18 lysis shows that the fossils are composed of aluminosilicate clay minerals and some carbon, a composi

19 e to their ubiquity and chemical reactivity, aluminosilicate clays play an important role in actinide

20 al combustion byproduct with a predominantly aluminosilicate composition, is modified to develop an i

21 noted that production of abundant oligomeric aluminosilicates could be significantly increased by sub

22 This record shows that aluminosilicate dust deposition more than doubled during

23 D-XRF) allowed us to determine the use of an aluminosilicate enriched in Cu and Pb.

24 n diameter of 200-250 nm, composed of ~50-nm aluminosilicate flakes studded with Fe and Ti-rich clust

25 to 100 nm while short-range ordering of the aluminosilicate framework is significantly reduced-this

26 nd molecular modeling techniques, its porous aluminosilicate framework structure (R3m, a = 13.6373(1)

27 r the EFC (NATII) in closer proximity to the aluminosilicate framework.

28 tation of a secondary phase, likely a K-rich aluminosilicate gel.

29 done by first compressing a sodium-magnesium aluminosilicate glass at 1 GPa at Tg, followed by sub-Tg

30 to significant changes in the morphology of aluminosilicate glass, a dominant material in FA particl

31 paration of high-density, high-hardness bulk aluminosilicate glasses.

32 the dissolution kinetics of major weathering aluminosilicates, kaolinite and K-feldspar.

33 ge-sharing octahedral CuO6 layers and curved aluminosilicate layers and strings.

34 d as moderately dense silicates (SiO(2)) and aluminosilicates making their specific capacities for th

35 olymeric material, Sylgard-184 and a ceramic aluminosilicate material, Zircar RS-1200, at different t

36 Zeolites are aluminosilicate materials that contain regular three-dim

37 Zeolites are porous aluminosilicate materials that have found applications i

38 nt constraints on the solubility of argon in aluminosilicate melt compositions up to 25 GPa and 3,000

39 from inorganic and non-HA impurities (i.e., aluminosilicates, metals) and fractionated by a combinat

40 re determined for six homoionic forms of the aluminosilicate mineral, montmorillonite.

41 Albite (NaAlSi3O8) is an aluminosilicate mineral.

42 Iron-containing zeolites (microporous aluminosilicate minerals) are noteworthy in this regard,

43 curvature in the formation of single-walled aluminosilicate nanotubes.

44 ease, and finally form ordered single-walled aluminosilicate nanotubes.

45 The zeolite sodium aluminosilicate natrolite was recently shown to undergo

46 t with the high-pressure phase of the sodium aluminosilicate natrolite.

47 tions between metal precursors and incipient aluminosilicate nuclei during self-assembly of microporo

48 montmorillonite and illite, all of which are aluminosilicates of similar composition and surface char

49 titutes a useful tactic for generating large aluminosilicate oligomers for surface characterization a

50 A zeolite with structure type MFI is an aluminosilicate or silicate material that has a three-di

51 anion hydration suggest that H2O adds to the aluminosilicate oxyanions in a dissociative fashion, for

52 growth involving the attachment of amorphous aluminosilicate particles to crystal surfaces and classi

53 ly reported results on mineral dust, iron in aluminosilicate phases provides the predominant componen

54 f V(5+) species, possibly associated with Ca-aluminosilicate phases.

55 ety of monomeric and polymeric aluminate and aluminosilicate species (Al(1)Si(x)-Al(13)Si(x)), such a

56 porating the role of monomeric and polymeric aluminosilicate species as well as larger nanoparticles.

57 the rates at which aluminate, silicate, and aluminosilicate species hydrate, with important implicat

58 ly reveals the complexation of aluminate and aluminosilicate species with perchlorate species that mo

59 tage of their high affinity for silicate and aluminosilicate species.

60 erties on hydrating aluminate, silicate, and aluminosilicate surfaces that are shown to be due to the

61 igate uranyl(VI) adsorption onto two neutral aluminosilicate surfaces, namely, the orthoclase (001) s

62 adsorbs strongly as multilayers on hydrated aluminosilicate surfaces.

63 olymer-ceramic nanocomposites and mesoporous aluminosilicates that are derived by an amphiphilic dibl

64 Clay minerals are layer type aluminosilicates that figure in terrestrial biogeochemic

65 s contained in Fe oxides, whereas Fe-bearing aluminosilicates (vermiculite and Illite) accounted for

66 XRD revealed that soil clay aluminosilicates were hydroxy-interlayered vermiculite,

67 lying a similar association of Fe oxides and aluminosilicates with organic matter in organo-mineral a

68 orosilicates (with weak inherent acidity) to aluminosilicates (with much stronger acid strength) when

69 Catalytic fines (called cat fines) are aluminosilicate zeolite catalysts utilized in the oil cr

70 In this study, we discovered that the aluminosilicate zeolite structures with the highest CO(2

71 icability in identifying the best-performing aluminosilicate zeolite structures.

72 e the crystallization of SSZ-13, which is an aluminosilicate zeolite that possesses exceptional physi

73 A new aluminosilicate zeolite, ITQ-27, has been prepared using

74 t stable, three-dimensional extra-large pore aluminosilicate zeolite.

75 t new classes of zeolites (zeotypes)-such as aluminosilicate zeolites and zeolite analogues-together

76 e been invaluable in expanding the classical aluminosilicate zeolites to new unique framework types a

77 Large-scale simulations of aluminosilicate zeolites were conducted to identify stru

78 e, and beryllosilicate analogues of numerous aluminosilicate zeolites.

79 ures are based on the nets of seven distinct aluminosilicate zeolites: tetrahedral Si(Al) and the bri