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- A complete laterite profile should be made up of laterite layer, parti-color clay layer and carbonate rock saprolite. 完整的紅土剖面應該由紅土層、雜色粘土層和碳酸鹽巖腐巖組成。
- Weathered rock is the predecessor of saprolite and is mainly made of corestones surrounded by saprolite crust. 土層可貯存上層滯水，風(fēng)化巖帶則可賦存潛水或承壓水。
- The porous nature of the saprolite is directly related to the high porosity of Andisols in this study area. 腐石之多孔性特性則直接與此研究區灰燼土之高孔隙率有關(guān)。
- Carbonate rock saprolite is formed in zones of alteration and made up of travertine and residual carbonate crystals. 碳酸鹽巖腐巖形成于包氣帶，由原巖中的碳酸鹽溶解后再次沉淀形成，主要由鈣華和殘馀碳酸鹽晶體組成。
- From the earth s surface to fresh bedrock the profile of slope may be divided into soil zone,saprolite zone and weathered rock zone. 從地表到新鮮巖體,隨著(zhù)水巖化學(xué)作用程度的逐漸減弱,斜坡剖面可依次劃分為土層、腐巖帶和風(fēng)化巖帶,各帶之間多是漸變過(guò)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. 從地表到新鮮巖體，隨著(zhù)水巖化學(xué)作用程度的逐漸減弱，斜坡剖面可依次劃分為土層、腐巖帶和風(fēng)化巖帶，各帶之間多是漸變過(guò)渡的。
- Principal Characteristics of Limestone Saprolite and Its Forming Mechanisms 石灰巖腐巖的基本特征及其形成機制
- saprolite of nickel laterite 常壓浸出
- saproliten. [地]腐泥土;殘余土
- sathrolith 殘余土
