Reference soil China 16: Regosol
Regosols are found in areas where soil has been eroded to the extent that the underlying unconsolidated materials come near to the surface, or where soil formation has not played an important role, e.g. in desert regions. The name comes from the greek 'rhegos' :blanket meaning young soils on weathering materials.
Characteristics
Soils in medium and fine textured materials, having no distinctive horizons other than an ochric horizon at the surface.
Reference soil CN016: Regosols
PROFILE DESCRIPTION : Very deep, excessively drained, gravel with a thin brown, slightly gravelly sandy loam topsoil. A desert pavement is present at the surface. Notes on profile description: the A horizon consists of 3 thin layers. The first layer (top 1.5 cm) sometimes has a "foam or gasbubble" structure. The second layer is formed by a 4 cm clear loose laminated layer. The third or bottom part of the A horizon shows some crumb structure. The 24 cm boundary is not fixed, sometimes this boundary is at 15 cm or 20 cm depth. The C2 horizon may be devided into: 24-60 cm (coarse gravel) and 60-120 cm (fine gravel). The C2 is a dark coloured gravel layer. CLIMATE: somewhat in between Urumqi and Changyi / SURFACE CHARACTERISTICS: very shallow broad "run-off" channels or streamlines are visible (mainly through a denser vegetation cover) / VEGETATION: the Gobi or gravel/stone desert has an irregular vegetational cover; about 10% consists mainly of Reaumaria, Zljinia regelii, Ephedra and Zygo phyllum / Slide nos. of the ISRIC collection: 7609-7626 (profile, landscape/vegetation, monolith sampling). Thin section nos. of the ISRIC collection: none.