There is a remarkable tendency for the hydrogen ion concentration in snowmelt water in the early spring to be higher than that in the late spring. Falling fresh snow catches atmospheric acid substances in the atmosphere. The fresh fallen snow on the ground is compressed by repeated dissolution and crystallization and forms icy granular snow. The repetition causes sulfate, nitrate and chloride ions to be concentrated near the surface of the icy granular snow. Some laboratory experiments were performed to examine this concentration phenomenon by the formation of spherical ice crystallized from sulfate-containing water and by dissolution of the formed ice crystals.
On dissolution, the inclusion amount and the distribution of sulfate ions in ice crystals were measured. The distribution of sulfate in the crystals was found to be biased; the sulfate amount near the surface was larger than that around the center, when each crystal was melted from the surface to the center in organic solvent. It was also found that the higher initial concentration of sulfate tended to create a uniform distribution of sulfate.
When the ice crystals were packed in a column (2.0cm inner diameter, 30cm length) and dissolved at room temperature, a higher concentration of sulfate was observed in the first effluent. The concentration ratio was higher than the estimated value at the surface using the organic solvent method. With the dissolution of the natural granular snow, similar results were obtained; higher concentrations of sulfate ions were observed in the first effluent and lower con-centrations in the later effluent.
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