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Physical Quality Indicators and Mechanical Behavior of Agricultural Soils of Argentina
Author(s) -
Sílvia Imhoff,
Álvaro Pires da Silva,
Pablo Javier Ghiberto,
Cássio Antônio Tormena,
Miguel Ángel Pilatti,
Paulo Leonel Libardi
Publication year - 2016
Publication title -
plos one
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.99
H-Index - 332
ISSN - 1932-6203
DOI - 10.1371/journal.pone.0153827
Subject(s) - pedotransfer function , bulk density , soil water , soil science , water content , water retention curve , environmental science , soil texture , soil organic matter , field capacity , organic matter , soil structure , silt , consolidation (business) , hydraulic conductivity , geotechnical engineering , chemistry , geology , accounting , business , paleontology , organic chemistry
Mollisols of Santa Fe have different tilth and load support capacity. Despite the importance of these attributes to achieve a sustainable crop production, few information is available. The objectives of this study are i) to assess soil physical indicators related to plant growth and to soil mechanical behavior; and ii) to establish relationships to estimate the impact of soil loading on the soil quality to plant growth. The study was carried out on Argiudolls and Hapludolls of Santa Fe. Soil samples were collected to determine texture, organic matter content, bulk density, water retention curve, soil resistance to penetration, least limiting water range, critical bulk density for plant growth, compression index, pre-consolidation pressure and soil compressibility. Water retention curve and soil resistance to penetration were linearly and significantly related to clay and organic matter (R 2 = 0.91 and R 2 = 0.84). The pedotransfer functions of water retention curve and soil resistance to penetration allowed the estimation of the least limiting water range and critical bulk density for plant growth. A significant nonlinear relationship was found between critical bulk density for plant growth and clay content (R 2 = 0.98). Compression index was significantly related to bulk density, water content, organic matter and clay plus silt content (R 2 = 0.77). Pre-consolidation pressure was significantly related to organic matter, clay and water content (R 2 = 0.77). Soil compressibility was significantly related to initial soil bulk density, clay and water content. A nonlinear and significantly pedotransfer function (R 2 = 0.88) was developed to predict the maximum acceptable pressure to be applied during tillage operations by introducing critical bulk density for plant growth in the compression model. The developed pedotransfer function provides a useful tool to link the mechanical behavior and tilth of the soils studied.

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