摘要
本文通过实验论证了三价铁和二价硫无论在酸性或碱性条件下只发生氧化还原反应,不发生成三硫化二铁的沉定反应。沉淀中含有的少量三价铁是由于共沉淀所致。
The article provides proof that when ferric iron and divalent sulfide are in acidity or bacicity, it results in oxidation-reduction, reaction but not in precipitating reaction of ironic trisulfide, and the snail amount of ferric iron in the sediment is the result of the cosediment.
出处
《曲靖师范学院学报》
1990年第1期57-58,共2页
Journal of Qujing Normal University
关键词
三硫化二铁
氧化还原反应
沉淀反应
Ironic trisulfide, Oxidation-reduction reaction, Precipitating reaction