Influence of edaphic and management factors on soils aggregates stability under no - tillage in mollisols and vertisols of the Pampa Region, Argentina

In the highly fertile and productive soils of the Pampa Region of Argentina, constraints on soil water regime as a consequence of the decline in aggregates stability and the development of platy structures, are observed. Most of agricultural plots in this region, even under no tillage, are subject...

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Otros Autores: Behrends Kraemer, Filipe, Morrás, Héctor José María, Fernández, Patricia Lilia, Duvall, Matías Ezequiel, Galantini, Juan Alberto, Garibaldi, Lucas Alejandro
Formato: Artículo
Lenguaje:Inglés
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Acceso en línea:http://ri.agro.uba.ar/files/intranet/articulo/2021behrends.pdf
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Aporte de:Registro referencial: Solicitar el recurso aquí
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024 |a 10.1016/j.still.2020.104901 
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245 |a Influence of edaphic and management factors on soils aggregates stability under no - tillage in mollisols and vertisols of the Pampa Region, Argentina 
520 |a In the highly fertile and productive soils of the Pampa Region of Argentina, constraints on soil water regime as a consequence of the decline in aggregates stability and the development of platy structures, are observed. Most of agricultural plots in this region, even under no tillage, are subjected to simplification of crop sequences (low cropping intensity) with predominance of soybean. On the contrary, some farmers are intensifying the crops sequence to avoid soil degradation and equilibrate economical incomes. The aim of this work was to evaluate the effects of intrinsic soil factors and of cropping intensity on aggregates stability in the surface horizon of the main soils in this region. Three Mollisols (an Entic Haplustoll and two Typic Argiudolls) and a Vertisol (Hapludert) located across a west-east transect in the northern part of the Argentinean Pampas were selected for this study. In each site two management treatments under no-till (GAP: Good Agricultural Practices – high cropping intensityand PAP: Poor Agricultural Practices – low cropping intensity-) and a soil without cultivation as a reference (NE: Natural Environment) were compared. In each treatment, aggregates destruction mechanisms were assessed by Le Bissonnais (1996) tests: slaking, microcraking and cohesion loss. Mollisols showed higher aggregates stability than the Vertisol. Differences on aggregates stability depended on management variables and on organic carbon contents in the Mollisols and on both clay content-clay type in the Vertisol, revealing a strong relationship of aggregation mechanisms with soils taxonomic order. In the Mollisols, the labile coarse particulate organic carbon fraction (POCc) determined the shifts on slaking and overall aggregates stability rather than other carbon fractions. In the soils studied, aggregates stability was linked mainly to management variables, best reflected by the cropping intensity index (CI). More intensive agricultural managements (GAP treatments) in Mollisols and Vertisol, resulted in an enhancement of aggregates stability; however, this relationship was stronger in the Mollisols. Surface horizons from both soil orders evidenced a high soil fragility related to slaking process (FW10s and FW tests). Thus, FW test was the best test to discriminate between management treatments. The results obtained in this work allow, on the one hand, to understand the stabilization mechanisms of the structure in the surface horizon of the main Pampas soils and, on the other hand, to highlight the effect of different NT management practice on soil aggregate stability, which highly affects soil health and the sustainability of agricultural systems. 
650 |2 Agrovoc  |9 26 
653 |a AGGREGATES STABILITY 
653 |a ORGANIC CARBON FRACTIONS 
653 |a LE BISSONNAIS TESTS 
653 |a CROPPING INTENSITY 
653 |a SOIL CLASSIFICATION 
653 |a SOIL TAXONOMY 
653 |a MOLLISOLS AND VERTISOL 
700 1 |a Behrends Kraemer, Filipe  |u Universidad de Buenos Aires. Facultad de Agronomía. Departamento de Ingeniería Agrícola y Uso de la Tierra. Cátedra de Manejo y Conservación de Suelos. Buenos Aires, Argentina.  |u Instituto Nacional de Tecnología Agropecuaria. Investigación de Recursos Naturales. Instituto de Suelos (INTA - CIRN). Argentina.  |u CONICET. Buenos Aires, Argentina.  |9 22849 
700 1 |a Morrás, Héctor José María  |u Instituto Nacional de Tecnología Agropecuaria. Investigación de Recursos Naturales. Instituto de Suelos (INTA - CIRN). Argentina.  |9 19698 
700 1 |a Fernández, Patricia Lilia  |u CONICET. Buenos Aires, Argentina.  |u Universidad de Buenos Aires. Facultad de Agronomía. Departamento de Ingeniería Agrícola y Uso de la Tierra. Cátedra de Fertilidad y Fertilizantes. Buenos Aires, Argentina.  |9 33912 
700 1 |a Duvall, Matías Ezequiel  |u Universidad Nacional del Sur. Departamento de Agronomía. Centro de Recursos Naturales Renovables de la Zona Semiárida (CONICET - CERZOS). Bahía Blanca, Argentina.  |9 50608 
700 1 |a Galantini, Juan Alberto  |u Comisión de investigaciones científicas (CIC). Argentina.  |u Universidad Nacional del Sur. Departamento de Agronomía. Centro de Recursos Naturales Renovables de la Zona Semiárida (CONICET - CERZOS). Bahía Blanca, Argentina.  |9 16073 
700 1 |a Garibaldi, Lucas Alejandro  |u Universidad Nacional de Río Negro. Instituto de Investigaciones en Recursos Naturales, Agroecología y Desarrollo Rural. Río Negro, Argentina  |u CONICET - Universidad Nacional de Río Negro. Instituto de Investigaciones en Recursos Naturales, Agroecología y Desarrollo Rural. Río Negro, Argentina.  |9 31177 
773 0 |t Soil and tillage research  |w SECS000167  |g Vol.209 (2021), art.104901, 12 p., tbls., grafs. 
856 |f 2021behrends  |i en intranet  |q application/pdf  |u http://ri.agro.uba.ar/files/intranet/articulo/2021behrends.pdf  |x ARTI202204 
856 |u http://www.elsevier.com/  |z LINK AL EDITOR 
942 |c ARTICULO 
942 |c ENLINEA 
976 |a AAG