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Chemistry-transport coupled modelling of the Aespoe groundwater system (Sweden) since the last glaciation

机译:自上次冰期以来,Aespoe地下水系统(瑞典)的化学-运输耦合模型

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Based on the specific coupled modelling approach developed at BRGM, a reaction-transport model of the Aspo groundwater system (Sweden) has been developed; it simulates a continuous scenario from 12.000 BP to the natural modern situation. Examples of the results (evolution of Na, ~(18)O, calcite) are presented. Na, Ca, Cl and stable isotopes are mainly related to mixing between the different mixing endmembers subsequently entering the system (glacial meltwater, Baltic Sea stages, meteoric water), calcite contents, pH and silica are determined by water rock interaction.
机译:根据BRGM开发的特定耦合建模方法,开发了Aspo地下水系统(瑞典)的反应-运输模型;它模拟了从12.000 BP到自然自然状况的连续情景。给出了结果的示例(Na的演化,〜(18)O,方解石)。 Na,Ca,Cl和稳定同位素主要与随后进入系统的不同混合末端成员之间的混合有关(冰融水,波罗的海阶段,陨石水),方解石含量,pH和二氧化硅是由水岩相互作用确定的。

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