“…Indeed, the GCMC method has successfully been used to simulate the adsorption of various small molecules at the surface of, among others, clay minerals (e.g., kaolinite), 48,49 zeolites, 50-56 various metal oxides, 57-60 crystalline 26,61-69 as well as amorphous ice, 70 various carbonaceous materials, [71][72][73][74][75][76][77] self-assembled aerosol monolayers, 78,79 and covalent organic frameworks, [80][81][82] as well as inside protein crystals 83 and clathrate cages. [84][85][86][87][88][89][90][91] In this paper, we investigate in detail the adsorption of formamide both at the surface of Ih ice (at 200 K) and at the surface of LDA ice (at 200 K, 100 K, and 50 K). Although the adsorption on LDA at 200 K has relevance neither in atmospheric chemistry nor in astrochemistry, we included this system in the present investigation for reference purposes.…”