Dust-mediated loading of trace and major elements to Wasatch Mountain snowpack
Dust-mediated loading of trace and major elements to Wasatch Mountain snowpack
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DOI:
10.1016/j.scitotenv.2012.05.077
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发表时间:
2012-08-15
影响因子:
9.8
通讯作者:
Johnson, William P.
中科院分区:
文献类型:
--
作者:
Carling, Gregory T.;Fernandez, Diego P.;Johnson, William P.
Depth-integrated snow columns were collected at 12 sites across the central Wasatch Mountains, Utah, during March and April 2010 to determine concentrations of trace elements, major anions and cations, and pH. Sample collection was conducted at or near maximum snow accumulation prior to the onset of melt, and included spring dust events driven by southerly pre-frontal winds. Snow samples were melted in the laboratory and subsampled for analyses on filtered (0.45 mu m) and unfiltered fractions. All measured elements (Al, As, Ba, Ca, Co, Cr, Cu, Fe, Hg, K, Li, Mg, Mn, Na, Ni, Pb, Sb, Sr, Ti, Tl, U, V. and Zn) and major anions (Cl, NO3, and SO4) displayed significant increases in concentration (for example, factor of 2 to 5 increases for As, Cr, Hg, and Pb) between the six sites sampled in March (prior to dust events) and the six sites sampled in April (after dust events). Acid neutralizing capacity and pH were also elevated in April relative to March snowpack. Comparison of elemental concentration in the particulate (>0.45 mu m; difference between unfiltered and filtered concentration) and soluble (0.45 mu m. The results suggest that the majority of trace element loading to the Wasatch snowpack occurs via dust deposition. The major elements were primarily loaded in the