“…The catalytic performance of heterogeneous catalysts is generally determined by the structure of active sites. − The reaction atmosphere is capable of dynamically regulating the structure of active sites and forming active multinuclear species at low temperatures, thereby realizing quasi-homogeneous reactions over Cu-SSZ-13 zeolites in the selective catalytic reduction of NO x with NH 3 (NH 3 -SCR). − The chabazite ( CHA ) structure of Cu-SSZ-13 is composed of double six-membered rings ( d6r ) that form larger cha cages in three-dimensional channel structures with eight-membered rings (8-ring) of 3.8 Å × 3.8 Å dimensions . Si 4+ is replaced by Al 3+ in the framework, and a H + ion is introduced to the Al–O site to maintain framework charge equilibrium, thus generating a Brønsted acid site. − By exchanging H + ions, Cu 2+ and Cu(OH) + cations are anchored at d6r and 8-rings, respectively, to form active Cu sites. , Under the reduction atmospheres (i.e., NH 3 or NO + NH 3 ) or the standard SCR condition (i.e., NO + NH 3 + O 2 ), a large number of linear [Cu I (NH 3 ) 2 ] + complexes are generated through the coordination with NH 3 . , Due to the solvation effect of NH 3 , the electrostatic interaction between Cu species and the negatively charged zeolite framework is weakened, leading to a high mobility of [Cu I (NH 3 ) 2 ] + within the zeolite and even allowing its intercage migration. − The Cu-NH 3 species enable the occurrence of the NH 3 -SCR reaction within cha cages in a locally homogeneous manner, hence effectively promoting the low-temperature SCR reaction. , Thus, the formation process of active dinuclear species in the channels via dynamic [Cu I (NH 3 ) 2 ] + ions is a crucial step for low-temperature SCR reactions, and enhancing the formation efficiency of dimer-Cu species is essential for the promotion of SCR activity.…”