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- A complete laterite profile should be made up of laterite layer, parti-color clay layer and carbonate rock saprolite. 完整的红土剖面应该由红土层、杂色粘土层和碳酸盐岩腐岩组成。
- Weathered rock is the predecessor of saprolite and is mainly made of corestones surrounded by saprolite crust. 土层可贮存上层滞水，风化岩带则可赋存潜水或承压水。
- The porous nature of the saprolite is directly related to the high porosity of Andisols in this study area. 腐石之多孔性特性则直接与此研究区灰烬土之高孔隙率有关。
- Carbonate rock saprolite is formed in zones of alteration and made up of travertine and residual carbonate crystals. 碳酸盐岩腐岩形成于包气带，由原岩中的碳酸盐溶解后再次沉淀形成，主要由钙华和残馀碳酸盐晶体组成。
- From the earth s surface to fresh bedrock the profile of slope may be divided into soil zone,saprolite zone and weathered rock zone. 从地表到新鲜岩体,随着水岩化学作用程度的逐渐减弱,斜坡剖面可依次划分为土层、腐岩带和风化岩带,各带之间多是渐变过渡的。
- From the earth's surface to fresh bedrock the profile of slope may be divided into soil zone, saprolite zone and weathered rock zone. 从地表到新鲜岩体，随着水岩化学作用程度的逐渐减弱，斜坡剖面可依次划分为土层、腐岩带和风化岩带，各带之间多是渐变过渡的。
- Principal Characteristics of Limestone Saprolite and Its Forming Mechanisms 石灰岩腐岩的基本特征及其形成机制
- saprolite of nickel laterite 常压浸出
- saproliten. [地]腐泥土;残余土
- sathrolith 残余土
