Genesis and micropedology of soils at Serra do Divisor and Moa river floodplain, northwestern Acre, Brazilian Amazonia.

The northwestern part of the Acre State (Brazil) possesses singular soils in Brazilian Amazonia, but have been very little studied. This study aimed to discuss the genesis and some micropedological aspects of the soils from Serra do Divisor and adjacent floodplain soils of the Moa river, to enhance the knowledge on their formation. A toposequence of soils ranging from the uppermost part of sub-Andean Serra do Divisor to the Alluvial soils of Moa river floodplain was studied, regarding chemical, physical, mineralogical, and micromorphological attributes. The parent material of the Serra do Divisor is basically quartzose sandstone, and the soils along the toposequence were classified as Typic Haplorthods (P1), Spodic Quartzipsamment (P2), Lithic Quartzipsamment (P3), and Lithic Quartzipsamment (P4). Along the Moa river floodplain, we also identified and collected, Typic Udifluvent (P5), Typic Kandiudult (P6), Typic Kandiudalf (P7), and Arenic Plinthic Kandiudult (P8). The Serra do Divisor soils have very low fertility, high acidity, and low cation exchange capacities, presenting a coarse sandy texture, even shallow pedons. The X-ray diffraction analysis of these soils indicates the predominance of kaolinite, with traces of quartz and gibbsite. The shallow mountain Podzols on sandstone have an expressive accumulation of organic material in surface horizons, with evidence of ferrihydrite and imogolite in the subsurface. At the Moa river floodplain, all soils are originated from recent sediments (Cenozoic), which have a geological source upstream. Varying sedimentary layers are key aspects influencing soil genesis. Those soils have evidence of 2:1 clays with hydroxyl-Al interlayers in subsurface horizons. The Serra do Divisor steep landforms and the coarse texture of the soils promote good drainage and favor leaching and chemical impoverishment. Kaolinite and gibbsite were formed by severe leaching and there are evidences of in situ neoformation of gibbsite by extreme Si losses. All studied soils have some peculiarities such as high accumulation of organic material or 2:1 clay minerals. Most investigated soils were affected by colluvial, reworking, mass movements or a strong variation on sedimentation.

Bibliographic Details

Main Authors:	MENDONÇA, B. A. F. de, SCHAEFER, C. E. G. R., FERNANDES-FILHO, E. I., SIMAS, F. N. B., AMARAL, E. F. do
Other Authors:	Bruno Araujo Furtado de Mendonça, Universidade Federal Rural do Rio de Janeiro; Carlos Ernesto Gonçalves Reynaud Schaefer, Universidade Federal de Viçosa; Elpídio Inácio Fernandes-Filho, Universidade Federal de Viçosa; Felipe Nogueira Bello Simas, Universidade Federal de Viçosa; EUFRAN FERREIRA DO AMARAL, CPAF-AC.
Format:	Artigo de periódico biblioteca
Language:	Ingles English
Published:	2020-08-31
Subjects:	Serra do Divisor (AC), Micropedologia, Micropedology, Planície de inundação, Formación del suelo, Mineralogía del suelo, Materia orgánica del suelo, Llanuras sujetas a inundaciones, Rio Moa (AC), Northwestern Acre, Amazônia Ocidental, Western Amazon, Amazonia Occidental., Gênese do Solo, Várzea., Mineralogia, Matéria Orgânica, Floodplains., Soil formation, Soil mineralogy, Soil organic matter,
Online Access:	http://www.alice.cnptia.embrapa.br/alice/handle/doc/1124663
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