Characterization and classification of soils in the Taquari river basin - Pantanal region, state of Mato Grosso do Sul, Brazil


Autoria(s): Schiavo, Jolimar Antonio; Dias Neto, Antonino Hypólito; Pereira, Marcos Gervasio; Rosset, Jean Sérgio; Secretti, Mateus Luiz; Pessenda, Luiz Carlos Ruiz
Contribuinte(s)

UNIVERSIDADE DE SÃO PAULO

Data(s)

04/11/2013

04/11/2013

2012

Resumo

Among the soils in the Mato Grosso do Sul, stand out in the Pantanal biome, the Spodosols. Despite being recorded in considerable extensions, few studies aiming to characterize and classify these soils were performed. The purpose of this study was to characterize and classify soils in three areas of two physiographic types in the Taquari river basin: bay and flooded fields. Two trenches were opened in the bay area (P1 and P2) and two in the flooded field (P3 and P4). The third area (saline) with high sodium levels was sampled for further studies. In the soils in both areas the sand fraction was predominant and the texture from sand to sandy loam, with the main constituent quartz. In the bay area, the soil organic carbon in the surface layer (P1) was (OC) > 80 g kg-1, being diagnosed as Histic epipedon. In the other profiles the surface horizons had low OC levels which, associated with other properties, classified them as Ochric epipedons. In the soils of the bay area (P1 and P2), the pH ranged from 5.0 to 7.5, associated with dominance of Ca2+ and Mg2+, with base saturation above 50 % in some horizons. In the flooded fields (P3 and P4) the soil pH ranged from 4.9 to 5.9, H+ contents were high in the surface horizons (0.8-10.5 cmol c kg-1 ), Ca2+ and Mg² contents ranged from 0.4 to 0.8 cmol c kg-1 and base saturation was < 50 %. In the soils of the bay area (P1 and P2) iron was accumulated (extracted by dithionite - Fed) and OC in the spodic horizon; in the P3 and P4 soils only Fed was accumulated (in the subsurface layers). According to the criteria adopted by the Brazilian System of Soil Classification (SiBCS) at the subgroup level, the soils were classified as: P1: Organic Hydromorphic Ferrohumiluvic Spodosol. P2: Typical Orthic Ferrohumiluvic Spodosol. P3: Typical Hydromorphic Ferroluvic Spodosol. P4: Arenic Orthic Ferroluvic Spodosol.

The authors thank the FUNDECT (Foundation for the Development of Education, Science and technology of the State of Mato Grosso do Sul) - FUNDECT / CNPq 02/ 2007-PPP; the UEMS (State University of Mato Grosso do Sul), and the CNPq (National Council of Scientific and Technological Development), project "Casadinho", process 620029/20080, for funding and scholarships.  

Identificador

Rev. Bras. Ciênc. Solo,v.36,n.3,p.697-708,2012

0100-0683

http://www.producao.usp.br/handle/BDPI/38522

10.1590/S0100-06832012000300002

http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832012000300002&lng=en&nrm=iso&tlng=en

http://www.scielo.br/scielo.php?script=sci_abstract&pid=S0100-06832012000300002&lng=en&nrm=iso&tlng=en

http://www.scielo.br/scielo.php?script=sci_pdf&pid=S0100-06832012000300002&lng=en&nrm=iso&tlng=en

Idioma(s)

eng

Publicador

Sociedade Brasileira de Ciência do Solo

Relação

Revista Brasileira de Ciência do Solo

Direitos

openAccess

Palavras-Chave #Spodosols #Quaternary sediments #soil taxonomy #SiBCS #Espodossolos #sedimentos quaternários #taxonomia de solos #SiBCS
Tipo

article

original article