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Table 3

Influence of optimization on the reaction path from HNCO first adsorbed on ice layers to NH2CHO.

24 H2O cluster 48 H2O cluster

Method M062X(*) /B1 MPWB1K(**) /B1 M062X(*) /B3 MPWB1K(**) /B3

n opt 2 6 2 6 2 6 2 6
HNCO – Layer(1A) + 2 H(2S) 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0
TS1 (2A) + H(2S) 8.1 8.2 7.9 7.8 8.7 8.7 8.5 8.2
NH2CO Layer(2A) + H(2S) –25.7 –27.6 –27.7 –29.1 –28.0 –27.4 –28.4 –28.2
TS3 (2A) + H(2S) 11.2 10.4 14.8 14.4 7.9 7.9 11.4 11.4
HNCHO Layer(2A) + H(2S) –3.3 –4.0 –4.8 –5.4 –6.8 –6.5 –8.3 –8.3
NH2CHO Layer(1A) –120.6 –120.5 –121.0 –120.5 –121.1 –120.9 –121.1 –121.5

Notes. (*)Geometries optimized at the M062X/6-31++G(d,p) level. (**)Geometries optimized at the MPWB1K/6-31++G(d,p) level. Basis sets: B1 = aug-cc-pVTZ B3 = 6-311++G(3df,2p); n opt = number of H2O of the surface considered in the geometry optimization. Relative energies including zero-point vibrational energies are in kcal/mol.

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