Structural changes in latosols of the cerrado region: I - relationships between soil physical properties and least limiting water range

Revista Brasileira de Ciência do Solo

Eduardo Da Costa Severiano²  Geraldo César De Oliveira¹  Moacir De Souza Dias Júnior¹  Katia Aparecida De Pinho Costa¹  Fabiano Guimarães Silva¹  Silvio Marcos Ferreira Filho¹ 

[1] ,Federal Institute of Education, Science and Technology GoianoRio Verde Goiás ,Brazil

关键词: soil compaction;    degradation of agricultural soils;    soil penetration resistance;    water availability;    soil texture;    compactação do solo;    degradação estrutural;    resistência do solo à penetração;    disponibilidade hídrica;    textura do solo;   

DOI  :  10.1590/S0100-06832011000300013

来源: SciELO

【 摘 要 】

The agricultural potential of Latosols of the Brazilian Cerrado region is high, but when intensively cultivated under inappropriate management systems, the porosity can be seriously reduced, leading to rapid soil degradation. Consequently, accelerated erosion and sedimentation of springs and creeks have been observed. Therefore, the objective of this study was to evaluate structural changes of Latosols in Rio Verde, Goiás, based on the Least Limiting Water Range (LLWR), and relationships between LLWR and other physical properties. Soil samples were collected from the B horizons of five oxidic Latosols representing the textural variability of the Latosols of the Cerrado biome. LLWR and other soil physical properties were determined at various soil compaction degrees induced by uniaxial compression. Soil compaction caused effects varying from enhanced plant growth due to higher water retention, to severe restriction of edaphic functions. Also, inverse relationships were observed between clay content and bulk density values (Bd) under different structural conditions. Bd values corresponding to critical soil macroporosity (BdcMAC) were more restrictive to a sustainable use of the studied Latosols than the critical Bd corresponding to LLWR (BdcLLWR). The high tolerable compression potential of these oxidic Latosols was related to the high aeration porosity associated to the granular structure.

【 授权许可】

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