A series of solvates based on a dinuclear
Fe(II) complex [(TPA)2Fe2(μ-DHBQ)][BF4]2·S
[S = CH3OH (1·CH
3
OH), 2CH3OH (2·2CH
3
OH), 4DMF (3·4DMF), 2Et2O (4·2Et
2
O), Et2O·MeCN (5·Et
2
O·MeCN), and 2CH2Cl2 (6·2CH
2
Cl
2
)] were synthesized. Upon solvent
removal, single-crystal-to-single-crystal (SC-to-SC) transitions could
occur for the first four solvates to give 1, 2, 3, and 4·0.5Et
2
O. Within the temperature range of 400–10
K, these compounds exhibited abundant variations in their spin crossover
(SCO) properties. 2,5·Et
2
O·MeCN and 6·2CH
2
Cl
2
displayed half high-spin (HS) to low-spin (LS) transitions, and 4·2Et
2
O underwent
incomplete LS-to-HS conversion, whereas other solvatomorphs showed
complete SCO. As all these solvatomorphs possessed the identical [(TPA)2Fe2(μ-DHBQ)][BF4]2 core,
these variations in SCO behavior emphasized the critical role of the
crystal lattice contributions. With the aim of deciphering their origin,
periodic DFT+U+D3 computations were performed on these solvatomorphs
to quantify the importance of all possible intramolecular and intermolecular
effects on their spin-state energetics. Computationally, the isolated
[(TPA)2Fe2(μ-DHBQ)]2– molecule in the gas phase would undergo SCO around 350 K in one
step intrinsically. However, distinctive roles of the crystal-lattice
effects in the solid state resulted in varying SCO behaviors. Different
reasons were discovered for the incomplete spin transitions of different
solvatomorphs. For 2, although serious volume shrinkage
of the LS state caused efficient packing of the overall crystal-lattice
organization, the originally close-packing SCO cations got loose and
thus strongly destabilized its LS state. For 5·Et
2
O·MeCN and 6·2CH
2
Cl
2
, severe molecular distortions kinetically trapped their LS state. These computationally magneto-structural studies on dinuclear
solvatomorphs have great importance for designing SCO compounds with
selected properties, which is critical for their actual application.