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Oxygen can be combined with various cations to form a large number of ionically bonded solids.
Sulfur reacts with different organic molecules to form a large number of different organic-S compounds [7], though for simplicity we will consider only inorganic S chemistry here.
The main feature of these alloys is their particular phase structure, which tends to be a continuous solid solution in spite of the large number of constituents which would otherwise form a large number of intermetallic phases.
This result indicated that Au-30@TiO2 has the most excellent SERS performance, implying that Au nanoparticles contacted with TiO2 nanoparticles may form a large number of hot spots, which can facilitate to effective SERS enhancement [55].
Herein, sulfur-rich side chains are anchored onto Schiff-base copolymer of thiourea aldehyde resin (cp (S-TAR)) nanosheets via inverse vulcanization to form a large number of intermolecular crosslinkers as well as mesopores.
This may be due to the large number of free functional groups available for silver binding, which facilitated higher number of silver ions to bind and subsequently form a large number of NPs with smaller diameters (λ max 417 nm) [33].
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Ni2+ forms a large number of complexes, encompassing coordination numbers 4, 5, and 6 and all of the main structural types e.g., octahedral, trigonal bipyramidal, tetrahedral, and square.
This is particularly apparent for substitutions in the region of residues 56 64, which forms a large number of electrostatic and hydrophobic interactions with thrombin in the crystal structure of the complex.
In the dissolution recrystallization process, many cubic structural units tended to change to hexagonal phase in the CdS crystals, resulting in forming a large number of stacking fault structures.
Detailed subsurface, and surface, studies indicate that the Miocene and post-Miocene extension in northern Egypt, due to the rift of Arabia away from Africa, formed a large number of NW-SE-oriented normal faults and rejuvenated the ENE-oriented faults in the Cairo-Suez district by dextral transtension (Moustafa et al., 1998).
This element forms a large number of organometallic compounds, such as tetraethylgermane, which are useful in organometallic chemistry.
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