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Evaluation of ~32Si as a tracer for measuring silica production rates in marine waters

机译:评估〜32Si作为示踪剂以测量海水中的二氧化硅生产率

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摘要

the radioisotope ~32Si was evaluated as a tracer for measuring silica production rates in marine waters. ~32Si is a weak β-emitter that decays to ~32p allowing the isotope to be used to determine simultaneously the production rate of biogenic silica and organic phosphorus. High specific activity ~32Si, 42-000-52,000 Bq (μg Si)~1, was produced by the proton spallation of DCI. Reasonable tracer additions result in only nanomolar increases in the ambient silicic acid and orthophosphate concentrations during production rate experiments.
机译:放射性同位素〜32Si被用作示踪剂,用于测量海水中的二氧化硅产率。 〜32Si是一种弱的β-发射极,其衰减至〜32p,从而可用于同位素同时确定生物硅和有机磷的生产率。 DCI的质子散裂产生了高比活〜32Si,42-000-52,000 Bq(μgSi)〜1。合理添加示踪剂只会导致生产率实验中环境硅酸和正磷酸盐浓度的纳摩尔增加。

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