saprolites

与saprolites相关的网络例句 [注：此内容来源于网络，仅供参考]

The color difference between saprolite blocks and their parent rocks is obvious and the texture and structure of the parent rock can be preserved in saprolites.

发育于斜坡非饱和带的结晶岩与碎屑岩腐岩多夹于残坡积土层和风化岩带之间，保留有裂隙及层理等构造，但质地松软。

The major driving force promoting the formation of iron nodules is in situ weathering from saprolites by frequently alternating wetting/drying cycles, while illuviated iron only played a minor role in this formation.

本研究中生成铁瘤的主要机制乃是腐石在原处经频繁变动的乾湿交替作用后，崩解风化而化育生成，而洗入型的氧化铁则为生成铁瘤的次要力量。

Secondary clay minerals, quartz and ferrohydrite are most common in saprolites.

腐岩结构体与母岩色差显著，保留原岩结构和构造特征，矿物成分以次生粘土矿物、次生石英及褐铁矿最为常见。

Saprolites have spongy microtexture and are characterized by high porosity, high intrinsic permeability, high specific water capacity, low specific yield and low density.

腐岩次生微孔隙发育，具有低密度、高孔隙度、高渗透率、高容水度及高持水度特征。