Soil Attributes and Their Interrelationships with Resistance to Root Penetration and Water Infiltration in Areas with Different Land Uses in the Apodi Plateau, Semiarid Region of Brazil

Author:

Dias Pollyana Mona Soares1,Portela Jeane Cruz1,Gondim Joaquim Emanuel Fernandes1,Batista Rafael Oliveira1ORCID,Rossi Leticia Sequinatto2,Medeiros Jonatan Levi Ferreira1,Farias Phâmella Kalliny Pereira1ORCID,Mota Paulo Jardel1ORCID,Bandeira Diego José da Costa1ORCID,Filho Luís Cesar de Aquino Lemos1,de Matos Geisiane Xavier1,Mesquita Francisco de Oliveira3ORCID,de Oliveira Felipe Ozias1,Araújo Antonio Genilson Rodrigues1,do Nascimento Claudeone Manoel1

Affiliation:

1. Department of Agronomic and Forest Science, Federal Rural University of the Semi-Arid-UFERSA, Mossoró 59625-900, RN, Brazil

2. Department of Soils and Nature Resources, State University of Santa Catarina-UDESC, Lages 88520-000, SC, Brazil

3. PPGEC Graduate Program in Ecology and Conservation, State University of Paraíba, Campina Grande 58429-500, PB, Brazil

Abstract

Studies on soils and their interrelationships with land use in the context of the semi-arid region of Brazil are still scarce, even though they have the potential to assist in understanding the use and management of soil and agricultural crops. From this perspective, this study investigated four land uses in different locations of the Apodi Plateau, an elevated area in semi-arid region of northeastern Brazil. The different soils were analyzed for their resistance to root penetration, water infiltration, inorganic fractions, soil density, total porosity, potential of hydrogen, electrical conductivity, total organic carbon, potential acidity, and sum of bases. The soil resistance to root penetration and water infiltration were determined in the field. The results obtained were interpreted using multivariate and geostatistical analysis. The resistance data were subjected to the Shapiro–Wilk test at 5% of probability and expressed in maps, whereas infiltration data curves were constructed to estimate the amount of infiltrated water at the different time intervals. The textural classification was an important factor for the analysis of soil resistance to root penetration (Q) and the infiltration rate, being evidenced in the cluster analysis and allowing the formation of two groups, one for the surface layers of the areas and another for the subsurface layers, with the inorganic sand and clay fractions standing out with the greatest dissimilarity. The establishment of conservation practices for soil management is suggested to correct the pore space problems and the degradation of agroecosystems in areas with soils whose conditions are similar to the ones of this study.

Funder

CAPES institutional

Publisher

MDPI AG

Subject

Plant Science,Agronomy and Crop Science,Food Science

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