“…In soils, Modelli et al (2008), demonstrated that at the end of a 180-day respirometric experiment, none of the four imidazolium-based ILs was mineralized completely, and the amount of evolved CO 2 depended on both the type of cation and the type of anion. Primary biodegradation, defined as an "alteration in the chemical structure of a substance, brought about by biological action, resulting in the loss of a specific property of that substance" (OECD, 301, 1992) of imidazolium-, morpholinium-, piperidinium-, pyridinium-and pyrrolidiniumbased ILs, has been studied Neumann et al, 2014) and formation of biotransformation products of some imidazolium-and pyridinium-based ILs documented Pham et al, 2009;Docherty et al, 2010). Sorption of ILs onto the soil matrix can occur, depending on soil parameters (such as organic carbon content or cation exchange capacity), which can lead to a decrease of their bioavailability and biodegradability and contribute to the potential persistence (Stepnowski, 2005;Studzi nska et al, 2008;Mrozik et al, 2012).…”