凝聚作用 coacervation,指亲水胶体的粒子集聚而变成浓厚的溶胶(Sol),是作为显微镜下的小液滴或肉眼可见的“相”而被分离出来的现象,为H.G.Bungenberg deJong(1929)所命名。
经常用凝聚作用来解释这种变化。
它们是由F心的凝聚作用而形成的缔合中心。
They are F aggregates formed by the association of F centers.
有人提出用差异凝聚作用的机理来解释所观察到的沉降速度随盐度变化的原因。
Differential flocculation was proposed as the mechanism to explain these observed variations in setting rates with salinity.
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