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CONCENTRATION CHARACTERISTICS OF SOLUBLE IMPURITIES IN THE SURFACE SNOW OF COLLINS ICE CAP, KING GEORGE ISLAND, ANTARCTICA

机译:南极洲国王乔治岛凝灰岩冰帽溶于杂质浓度特征

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摘要

Measurements carried out for the upper 10m firn/ice obtained at the main dome of Collins Ice Cap, King George Island, Antarctica revealed the direct relation of soluble impurities of snow mass to the composition of atmosphere aerosols. It was indicated that sea salt source dominates the atmosphere aerosol around Collins Ice Cap. The simultaneous variation shown by the concentration profiles of Na+, K+, Mg2+, Ca2+, SO42-, CI-, Br- and very close EF values (≈1) suggested their common marine source and similar deposition process. Besides the possible surface contamination,NH4+varied uniformly along deeper part of the core in concentration, which could be considered as background value of ammonium. A satisfactory explanation for NO3- concentration profile has not reached at present.
机译:南极洲国王乔治岛主圆顶上获得的10M FiRN /冰上的测量揭示了雪地质量溶解杂质与大气气溶胶组成的直接关系。结果表明,海盐源在柯林斯冰帽周围的气氛气溶胶中占主导地位。 Na + / sup>,k + ,mg 2 + ,ca 2 + 的同时变化。 ,所以 4 2 - ,ci - ,br - 和非常关闭的EF值(≈1)建议它们常见的海洋源和类似的沉积过程。除了可能的表面污染之外,NH 4 + 均匀地沿浓度的深层部分均匀地变化,这可以被认为是铵的背景值。目前尚未达到对NO 3 - 浓度曲线的令人满意的解释。

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