Particle size characteristics of suspended sediments and subglacial hydrology of Dokriani Glacier, Garhwal Himalaya, India

Diurnal and seasonal variations in particle size characteristics of suspend ed sediments of Dokriani glacier meltwater were studied during the 1994 abl ation period (May-October). Diurnal suspended sediment concentration curves exhibit two prominent peaks from May to mid-August and only one peak durin g the rest of the ablation period. The first peak resulting from dominance of fine and medium sand contributed to the rising limb of the diurnal hydro graph, whereas the second peak was dominated by fine and medium silt which coincides with the diurnal discharge peak. The trends observed on the appea rance of silts and sand particles on diurnal scales at various stages of th e ablation period suggest that the subglacial drainage system comprises a d iurnally-reversing hydraulic gradient between the channels and distributed system along with translatory flow through the distributed system. This stu dy suggests that the subglacial zone is the major source of sediments in th e Dokriani glacier meltwaters. However, high intensity monsoonal rainfall h as contributed supraglacial sediments and resulted in bimodal distributions . Fines (clay to medium silt) are the dominant classes in the suspended sed iments except during the spring event; the supraglacial sediments had coars ely skewed distributions.