作者: M. Tranter , P. Brimblecombe , T.D. Davies , C.E. Vincent , P.W. Abrahams
DOI: 10.1016/0004-6981(86)90092-2
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摘要: Abstract Acidic snows in a small, remote, high-altitude snowpack the Cairngorms, Scotland, give rise to meltwaters which are proportionally rich sulphate and nitrate. As consequence, within-pack become chloride, even though depleted solute. Preferential elution appears be major process chemical evolution of snowfall snowpack.