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P. Tematio, E. Fritsch, M. E. Hodson, Y. Lucas, D. Bitom and P. Bilong, “Mineral and Geochemical Characteriza- tion of a Leptic Aluandic Soil and a Thapto Aluandic-Fer- ralsol Developed on Trachytes in Mount Bambouto (Ca- meroon Volcanic Line),” Geoderma, Vol. 152, No. 3-4, 2009, pp. 314-323. doi:10.1016/j.geoderma.2009.05.029

has been cited by the following article:

• TITLE: Andosolization of Soils on a Strombolian Cone at Mount Bambouto, Cameroon

  AUTHORS: Pierre S. Tsopjio Jiomeneck, Paul Tematio, Mike A. Wilson, Martin Yemefack

  KEYWORDS: Soil Morphology, Mineralogy, Geochemistry, Andosolization, Strombolian Cone, Cameroon Volcanic Line

  JOURNAL NAME: Open Journal of Soil Science, Vol.1 No.3, December 28, 2011

  ABSTRACT: Morphology, mineral and geochemical investigations were carried out on two selected soil pedons (ZA and TO) developed on a late Quaternary-aged strombolian cone to better understand andosolization processes in Mount Bambouto, Cameroon. Both pedons have A-BC-C horizonation. They have thick surface (A) horizon with bulk density -3, Alo + 0.5Feo about 2% and P retention >90%. Mineral association consists predominantly of kaolinite, gibbsite, goe- thite, organometal complexes and trace amount of ferrihydrite and allophane. The Ki values between 1.1 and 1.6, the low TRB (45 to 67 mg kg-1), the important IMob (20% to 24%), the CIA between 60% and 70% and the EFs above 1.16 for Al and Fe, and below 0.6 for Si indicate sparingly hydrolysis process in subsoil during which released Al, Fe and Si form allophanic or ferrihydrite minerals undergo crystallization into kaolinite, gibbsite and goethite, respectively. At topsoil, part of released Al (and Fe) is organically bounded with organic acids to form organometal complexes.