Pavlov Sergey Kh, Chudnenko Konstantin V
a Institute of the Earth Crust , Siberian Branch , Russian Academy of Sciences , Irkutsk , Russia.
J Environ Sci Health A Tox Hazard Subst Environ Eng. 2015;50(7):719-27. doi: 10.1080/10934529.2015.1011969.
The hydrogeochemical conditions of a large flatland-type ash dump (Eastern Siberia, Russia) were studied. High-alkalinity sulphate water with high calcium content was found to infiltrate into the aquifer from the ash dump. The water was transformed into neutral bicarbonate solutions. Simulation of physicochemical interactions of the clarified water with ash, sandstone, and soil demonstrated that the composition of the resulting simulated solutions is similar to composition of the transformed clarified water leaking into the aquifer, and moving at various distances from their place of infiltration towards the discharge area.
对俄罗斯东西伯利亚一个大型平地型灰渣场的水文地球化学条件进行了研究。发现高碱度、高钙含量的硫酸盐型水从灰渣场渗入含水层。这些水转变为中性碳酸氢盐溶液。对澄清水与灰、砂岩和土壤的物理化学相互作用进行模拟表明，所得模拟溶液的成分与渗入含水层并从渗入点向排泄区不同距离处流动的转变后的澄清水的成分相似。
