3 results

Pedogenic Iron Oxides in Iron-Rich Oxisols Developed from Mafic Rocks

Danilo de Lima Camêlo, João Carlos Ker, Maurício Paulo Ferreira Fontes, Marcelo Metri Corrêa, Antonio Carlos Saraiva da Costa, Vander Freitas Melo

21/Mar/2017

ABSTRACT Despite the considerable amount of information on the mineralogical characteristics of pedogenic Fe oxides in Brazilian soils, there are few studies on Fe-rich soils developed from mafic rocks with taxonomic identities at lower categorical levels. This study evaluated the mineralogical characteristics of pedogenic Fe oxides in B horizons (Bw) of Fe-rich Oxisols developed from several mafic rocks in the state of Minas Gerais, Brazil. The Bw horizons were sampled at a 0.8-1.0 m depth in 13 Ferric and Perferric […]

Chemical and mineralogical characterization of the different structure size classes of Red-Yellow and Dusky Red Latosols in Paraná, Brazil

Vander de Freitas Melo, Fernando Henrique Toledo, Rodrigo de Moura, Valmiqui Costa Lima, André Ademir Ghidin

01/Feb/2008

The content and shap of clay minerals are important in the definition of soil structure morphology. To evaluate the clay mineralogy and chemical properties of different aggregate size-classes of Latosols (Red-Yellow – LBd and Dusky Red – LVdf) derived from basalt in the state of Paraná, Brazil, soil samples of the Bw1 and Bw2 horizons were collected in four LBd and three LVdf profiles, distributed across two distinct toposequences. Dried and undisturbed soil samples were separated into six size-classes (2-4; […]

Oxisol toposequences developed from basaltic rocks in Paraná State, Brazil. I – clay fraction mineralogy

André Ademir Ghidin, Vander de Freitas Melo, Valmiqui Costa Lima, Jane Maria Jonasson Costa Lima

01/Apr/2006

Two Oxisol (Red-Yellow Latosol LBw and Dusky Red Latosol LVdf) toposequences in Paraná State, Brazil, were evaluated regarding the effect of different relief positions and parent material on mineralogical characteristics of the soil clay fraction. The clay fraction was investigated by X-ray diffraction, differential thermal analysis, thermogravimetry, and chemical analysis. Total Si, Al and Fe contents were determined after clay sample digestion with a 3:1 mixture of 36% HCl and 68% HNO3 acids. The Fe and Al contents were determined […]