Surface chemical properties and pedogenesis of tropical soils derived from basalts with different ages in Hainan, China

• Published in: Catena (Giessen) Vol. 87; no. 3; pp. 334 - 340
• Main Authors: Jiang, Jun, Xu, Ren-kou, Zhao, An-zhen
• Format: Journal Article
• Language: English
• Published: Cremlingen-Destedt Elsevier B.V 01.12.2011; Catena
• Subjects: Bgi / Prodig; Clay minerals; IEP; Pedogenetic processes; Pedology; Physical geography; PZNC; Surface charge; Tropical soil; Zeta potential; Guangdong; Hainandao; China; China, People's Rep., Hainan; China, People's Rep., Hainan Prov; Tropical soil; Clay minerals; Surface charge; PZNC; Zeta potential; IEP; Pedogenesis; Soil properties; Clay mineral; Tropical zone; Geophysics; Weathering; Basalt
• ISSN: 0341-8162; 1872-6887
• DOI: 10.1016/j.catena.2011.06.016

Limited information is available on the changes of surface chemical properties of tropical soils with time during the pedogenesis. Soil samples of three profiles derived from basalts of 10, 1330 and 2290 kilo annum (ka) in age were collected from adjacent locations in a tropical region of Hainan Province, China. The changes in soil surface chemical properties and the mineralogy of the soil clay fraction with time were investigated using ion adsorption, micro-electrophoresis, and X-ray diffraction analysis. The content of 2:1-type clay minerals decreased, while those of kaolinite and gibbsite increased with increasing basalt age and degree of soil development. The content of pedogenic free iron (Fe) oxides and the ratio of free Fe oxides/total Fe oxides increased with soil development stage, while soil poorly crystalline Fe and aluminum (Al) oxides had an opposite trend. The positive surface charge of the soils increased with increasing basalt age and degree of soil development; this was consistent with the change in their contents of free Fe/Al oxides. However, the value of negative surface charge had an opposite behavior. The soil derived from 10-ka-basalt had much more negative charge than soils derived from 1330- and 2290-ka-basalt. Soil net surface charge and zeta potential of the soil clay-fraction decreased with the increase in basalt age. Both net charge–pH curves and zeta potential–pH curves shifted to positive values with increased basalt age and degree of soil development. Increasing age also elevated the point of zero net charge of the soil and the isoelectric point of soil colloids. ► Content of kaolinite and gibbsite increased with increasing basalt age and degree of soil development ► Increase of free Fe 2O 3 led to the increase in positive charge of the tropical soils ► Increase in soil development elevated PZC and IEP and made negative surface charge less negative