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Relationship in chemical composition between mother solution and allophane-like aluminosilicate precipitate through neutralization of acid hydrothermal water by seawater

机译:海水中和酸性热热水时母液与脲基烷样硅铝酸盐沉淀物化学成分的关系

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A series of experiments on the formation of allophane-like aluminosilicate precipitates were carried out through neutralization of acid solutions in variety of relative proportions of Si, Fe and Al by seawater. The retrieval and decomposition procedures were available for precise determination of those components in the precipitates. Iron in the mother solutions was completely precipitated and Al was mostly precipitated, however, Si was partly co-precipitated with iron and aluminum. Iron and/or Al coexisting with Si caused a remarkable rise of the precipitated proportion of Si. This was ascribed to co-precipitation of these components on the formation of the precipitates. Difference in effect on the precipitated proportion of Si between Fe and Al was not noticeable. This result indicated equivalence of Fe to Al on the formation of the precipitates through neutralization. The correlations in the (Fe + Al)/Si and the Fe/Al molar ratios between the mother solution and the precipitates strongly designated that the relative proportions of Si, Fe and Al in hydrothermal water discharged from submarine volcanoes were able to be determined uniquely through chemical analysis of the precipitates causing discolored seawater.
机译:通过用海水中和各种相对比例的硅,铁和铝的酸溶液,进行了一系列形成脲基甲烷铝硅酸盐沉淀的实验。提取和分解程序可用于精确测定沉淀物中的那些成分。母液中的铁完全沉淀,而Al大部分沉淀,但是,Si与铁和铝部分共沉淀。与Si共存的铁和/或Al引起Si沉淀比例的显着增加。这归因于这些组分在沉淀物形成时的共沉淀。 Fe和Al之间对Si的沉淀比例的影响差异不明显。该结果表明,在通过中和形成沉淀物中,Fe与Al相当。母液与沉淀物之间的(Fe + Al)/ Si与Fe / Al摩尔比的相关性强烈表明,可以唯一确定从海底火山喷出的热水中Si,Fe和Al的相对比例通过对导致海水变色的沉淀物的化学分析。

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