CARACTERIZAÇÃO HIDRODINÂMICA E HIDRODISPERSIVA DE UM CAMBISSOLO FLÚVICO NA REGIÃO DO NORDESTE DO BRASIL

Albedson Miranda Palácio Filho; André  Maciel Netto; Marcus Metri Corrêa; Fernando Cartaxo Rolim Neto; Lívia Previatello da Silva; Sanderson Hudson da Silva Malta

doi:10.1590/1983-21252020v33n118rc

Authors

Albedson Miranda Palácio Filho Department of Rural Technology, Universidade Federal Rural de Pernambuco, Recife, PE https://orcid.org/0000-0001-7164-8996
André Maciel Netto Department of Nuclear Energy, Universidade Federal de Pernambuco, Recife, PE https://orcid.org/0000-0002-1341-5171
Marcus Metri Corrêa Department of Rural Technology, Universidade Federal Rural de Pernambuco, Recife, PE https://orcid.org/0000-0002-9506-8969
Fernando Cartaxo Rolim Neto Department of Rural Technology, Universidade Federal Rural de Pernambuco, Recife, PE https://orcid.org/0000-0002-6411-2058
Lívia Previatello da Silva Department of Nuclear Energy, Universidade Federal de Pernambuco, Recife, PE https://orcid.org/0000-0001-7157-451X
Sanderson Hudson da Silva Malta Laboratory Co-ordination, Instituto Federal de Educação, Ciência e Tecnologia de Pernambuco, Vitória de Santo Antão, PE https://orcid.org/0000-0001-6038-2600

DOI:

https://doi.org/10.1590/1983-21252020v33n118rc

Keywords:

Soil hydraulic properties. Solute transport. Semi-arid.

Abstract

The determination of the hydraulic and hydrodispersive properties of soil is necessary for the understanding of water dynamics and soil solute transport, and they are used as input data in several models. Determinations of soil hydraulic and hydrodispersive parameters are usually obtained by separate methodologies. Axisymmetric infiltration tests using a single ring infiltrometer with a conservative tracer (KBr) in the field (Beerkan-Solute) lead to the determination of the most realistic hydraulic and hydrodispersive properties of the study area. The objective of this work was the hydrodynamic and hydrodispersive characterization of an irrigated soil, classified as Fluvic Cambisol, from the lowland areas of the northeastern semi-arid region, located in the backwoods of the state of Pernambuco, in the municipality of Serra Talhada-PE. The hydrodispersive parameters were determined with the CXTFIT 2.0 program, using the CDE and MIM models. The studied soil presented hydrodynamic characteristics with high values of sorptivity (S) that were associated with high values of saturated hydraulic conductivity (K_s), indicating that the soil has good permeability and resistance to surface crumbling caused by rain drops or soil management. It was observed the predominance of the convective process, being the CDE model the one that presented the best performance in the transport of the KBr tracer under field conditions, indicating the absence of two water regions mobile and immobile in the studied soil.

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