Typic Endoaqualf CN
A Typic Endoaqualf (PRC-12) from Guangdong Province China.
Endoaqualfs are the Aqualfs that have an epipedon that rests on an argillic horizon without an abrupt textural change if the argillic horizon has moderately low or lower saturated hydraulic conductivity. The soil temperature regime is frigid, isomesic, mesic, or warmer.
Endoaqualfs are characterized by endoaquic saturation. The ground water fluctuates from a level near the soil surface to below the argillic horizon and is sometimes below a depth of 200 cm. Before cultivation, most Endoaqualfs supported either a deciduous broadleaf or a coniferous forest. Generally, Endoaqualfs are nearly level, and their parent materials are typically late-Pleistocene sediments.
For additional information about soil classification, visit:
sites.google.com/site/dinpuithai/Home/taxonomy/j-alfisols...
Typic Endoaqualf CN
A Typic Endoaqualf (PRC-12) from Guangdong Province China.
Endoaqualfs are the Aqualfs that have an epipedon that rests on an argillic horizon without an abrupt textural change if the argillic horizon has moderately low or lower saturated hydraulic conductivity. The soil temperature regime is frigid, isomesic, mesic, or warmer.
Endoaqualfs are characterized by endoaquic saturation. The ground water fluctuates from a level near the soil surface to below the argillic horizon and is sometimes below a depth of 200 cm. Before cultivation, most Endoaqualfs supported either a deciduous broadleaf or a coniferous forest. Generally, Endoaqualfs are nearly level, and their parent materials are typically late-Pleistocene sediments.
For additional information about soil classification, visit:
sites.google.com/site/dinpuithai/Home/taxonomy/j-alfisols...