red rare earth compound红色稀土化合物
REd-Earth嫣妮
red d earth红壤
red yellow earth红黄壤
hilly red-earth region红壤丘陵
Red-Earth-Hilly area in humid subtropics中国亚热带东部丘陵区
THE RED EARTH红地球
podzolized red earth灰化红壤
Old red earth老红壤
The difference of CIA between plinthitic and typical red earth in homogeneous red earth. denotes that the weathering intensity of the plinthitic red earth are stronger than typical red earth,which indicates more warm and humid environment.
均质类红土网纹红土层CIA值大于均质红土层,表明该类红土网纹红土风化强度大于均质红土层,指示网纹红土经历了比均质红土风化作用更强的气候环境。
参考来源 - 期刊学术社区N（名词） a clayey zonal soil of tropical savanna lands, formed by extensive chemical weathering, coloured by iron compounds, and less strongly leached than laterite 热带草原的红土