Dehydration of clay sediments 粘土矿物的脱水作用
The sediments are rich in clay, which forms when water weathers rocks into fine-grained particles.
这些沉积物富含粘土,粘土是由水流将岩石侵蚀成细小的微粒所形成的。
Then something strange happened: the loess in the terraces wasn't on top of crushed rock anymore - it was on top of very finely laminated clay-rich sediments.
然后一些很奇怪的事儿发生了:梯田里的黄土不再在碎岩石上-在非常完美层压的黏土丰富的沉积物上。
Elements are mainly terrigenous, clay (or fine muddy matter) is the major factor controlling the concentrations of heavy metals in sediments.
大多数元素以陆源为主,粘土(或细颗粒沉积物)是控制底质金属含量的主要因素。
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