“…To understand the effects of grain size and mineralogy in the hydrate formation process seafloor sediments composed of sand, kaolinite/sand mix, and bentonite/sand mix from the Gulf of Mexico, where gas hydrates are more prone to fine-grained sediments, were placed in segregated compartments of a test cell in the study of Rogers et al (2007). Based on the evidence of these tests, dirty sand can be considered as an ideal host medium for gas hydrate.…”