Abstract
Field and laboratory observations have indicated that the “fractionation” mechanism, whereby the bulk of the solute in seasonal snowcover is removed in the early meltwater fractions, is a differential process. Some soluble ions may be removed at faster rates than others. This process is known as “preferential elution”. Since the process is not yet universally accepted amongst scientists who engage in research into snowmelt chemistry, in this chapter we review the pertinent experimental work. Varying experimental conditions in real snowpacks often militate against reproducible elution sequences, although sodium and chloride are consistently found to be the least mobile ions upon melt. Laboratory experiments have provided more controlled conditions under which to examine the relative removal rates of soluble ions in meltwater. Those ions which are more soluble in ice are seen to be less mobile upon melt, whereas the ions which are eluted more rapidly may be regarded as being more strongly partitioned into the solute-rich surficial liquid, or quasi-liquid, layer. In real melting snowpacks, preferential elution of some ions by the meltwater can be masked by snowpack-scale hydrology.
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Davies, T.D. et al. (1987). The Removal of Soluble Ions from Melting Snowpacks. In: Jones, H.G., Orville-Thomas, W.J. (eds) Seasonal Snowcovers: Physics, Chemistry, Hydrology. NATO ASI Series, vol 211. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-3947-9_20
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DOI: https://doi.org/10.1007/978-94-009-3947-9_20
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