“…Larger organic particles tend to be deposited as a mat over the soil surface, particularly over finer textured soils (DeTar, 1979;Houston et al, 1999), while smaller organic particles (relative to the sizes of soil pores in the lining) pass through or are trapped in the upper few centimeters of the soil lining (Chang et al, 1974;Barrington and Madramootoo, 1989). DeTar (1979) and Cihan et al (2006) found that seal efficacy was more sensitive to the amount of organic solids present than to the saturated hydraulic conductivity of the untreated soil lining. Rowsell et al (1985) reported that coarser soil textures were I 1249 sealed less rapidly with the organics than fine soils.…”