“…The advective movement of gases through the substrate can be induced by variations on atmospheric pressure (AGHDAM et al, 2019;FJELSTED et al, 2019;XU et al, 2014), air temperature (ABICHOU et al, 2015;BOWDEN et al, 1998;XU et al, 2014), surface wind speed (AGHDAM et al, 2019;XIN et al, 2016), displacement of the water that infiltrates the substrate (ABICHOU et al, 2009;BAJAR et al, 2017;HANSON;HANSON, 1996;ROSLEV;KING, 1996;WHALEN et al, 1990), and differences in dump compaction KAUSHAL;SHARMA, 2016;RÖWER et al, 2011). CH 4 is less dense than the atmospheric air, and therefore tends to rise, while CO 2 and almost all of the vapors produced by volatile organic liquids are denser than air, tending to sink when released into the gaseous portion of the substrate (SEINFELD; PANDIS, 2006).…”