Physical Quality and Porosity Aspects of Amazon Anthropogenic Soils under Different Management Systems

Author:

Soares Marcelo Dayron Rodrigues1,Souza Zigomar Menezes de2ORCID,Campos Milton César Costa3ORCID,Cooper Miguel4ORCID,Tavares Rose Luiza Moraes5ORCID,Lovera Lenon Henrique2ORCID,Farhate Camila Viana Vieira2ORCID,Cunha José Maurício da1ORCID

Affiliation:

1. University of Amazonas, Institute of Education Agriculture and Environment, 69800-000 Humaitá, Amazonas, Brazil

2. University of Campinas, School of Agricultural Engineering–Av. Cândido Rondon, 501 Barão Geraldo, Campinas, São Paulo 13083-875, Brazil

3. Federal University of Paraíba, Rodovia BR 079—km 12, Areia, Paraíba 58397-000, Brazil

4. University of São Paulo, “Luiz de Queiroz” College of Agriculture, Department of Soil Science–Av. Pádua Dias Avenue 11, Piracicaba, São Paulo 13418-900, Brazil

5. Universidade de Rio Verde, Fazenda Fontes do Saber, Caixa Postal 104, Rio Verde, Goiás 75901-970, Brazil

Abstract

Archaeological Dark Earth (ADE) soils are rich in organic matter and highly fertile, but when used for farming or grazing activities, they generally lose chemical and physical quality, becoming more susceptible to erosion. In this context, this study aimed to evaluate the changes in physical properties of the soil in different management systems adopted in ADE areas of the Amazon. The study area is located in the municipality of Novo Aripuanã, in the mesoregion of Madeira, south of the state of Amazonas. Three ADE areas were selected: 1—native forest (Amazon forest fragment); 2—area covered with Brachiaria (Urochloa brizantha cv. Marandu), without the addition of fertilizers or soil improvers; and 3—area covered with pigeon pea (Cajanus cajan) and other commercial crops (corn, beans, and watermelon). The following soil characteristics were evaluated: soil resistance to penetration, soil bulk density, macroporosity and microporosity, and total soil porosity in the 0–0.20 m and 0.20–0.40 m layers. The results showed that the pasture area presented a smaller amount of total pores and complex pores, which are important for water flow in the soil. The areas analyzed in this study presented no critical obstacle to plant root development with the low value of resistance to penetration (<2.00 MPa) in all areas.

Funder

Fundação de Amparo à Pesquisa do Estado de São Paulo

Publisher

Hindawi Limited

Subject

Earth-Surface Processes,Soil Science

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