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  <rdf:Description rdf:about="https://doi.org/10.1590/s0100-06832008000200031">
    <dct:isReferencedBy>IMPACT4SOIL</dct:isReferencedBy>
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    <dct:isReferencedBy>LAReferencia - Red Federada de Repositorios Institucionales de Publicaciones Cient&#237;ficas Latinoamericanas</dct:isReferencedBy>
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    <dct:isReferencedBy>Microsoft Academic Graph</dct:isReferencedBy>
    <dct:isPartOf>Revista Brasileira de Ci&#234;ncia do Solo</dct:isPartOf>
    <dct:license>Open Access</dct:license>
    <dct:created>2008-07-04</dct:created>
    <dc:description>&lt;p&gt;Maize root growth is negatively affected by compacted layers in the surface (e.g. agricultural traffic) and subsoil layers (e.g. claypans). Both kinds of soil mechanical impedances often coexist in maize fields, but the combined effects on root growth have seldom been studied. Soil physical properties and maize root abundance were determined in three different soils of the Rolling Pampa of Argentina, in conventionally-tilled (CT) and zero-tilled (ZT) fields cultivated with maize. In the soil with a light Bt horizon (loamy Typic Argiudoll, Chivilcoy site), induced plough pans were detected in CT plots at a depth of 0-0.12 m through significant increases in bulk density (1.15 to 1.27 Mg m-3) and cone (tip angle of 60 &#65474;&#65466;) penetrometer resistance (7.18 to 9.37 MPa in summer from ZT to CT, respectively). This caused a reduction in maize root abundance of 40-80 % in CT compared to ZT plots below the induced pans. Two of the studied soils had hard-structured Bt horizons (clay pans), but in only one of them (silty clay loam Abruptic Argiudoll, Villa L&#65475;&#65453;a site) the expected penetrometer resistance increases (up to 9 MPa) were observed with depth. In the other clay pan soil (silty clay loam Vertic Argiudoll, P&#65475;&#65449;rez Mill&#65475;&#65441;n site), penetrometer resistance did not increase with depth but reached 14.5 MPa at 0.075 and 0.2 m depth in CT and ZT plots, respectively. However, maize root abundance was stratified in the first 0.2 m at the Villa L&#65475;&#65453;a and P&#65475;&#65449;rez Mill&#65475;&#65441;n sites. There, the hard Bt horizons did not represent an absolute but a relative mechanical impedance to maize roots, by the observed root clumping through desiccation cracks.&lt;/p&gt;</dc:description>
    <dc:subject>soil compaction</dc:subject>
    <dc:subject>plantio direto</dc:subject>
    <dc:subject>plantio convencional</dc:subject>
    <dc:subject>root growth</dc:subject>
    <dc:subject>ra&#237;zes</dc:subject>
    <dc:subject>conventional tillage</dc:subject>
    <dc:subject>0401 agriculture, forestry, and fisheries</dc:subject>
    <dc:subject>04 agricultural and veterinary sciences</dc:subject>
    <dc:subject>zero tillage</dc:subject>
    <dc:subject>camadas compactadas</dc:subject>
    <dc:creator>Taboada, Miguel Angel, Alvarez, Carina Rosa, </dc:creator>
    <dc:date>2008-04-01</dc:date>
    <dc:type>journalpaper</dc:type>
    <dct:abstract>&lt;p&gt;Maize root growth is negatively affected by compacted layers in the surface (e.g. agricultural traffic) and subsoil layers (e.g. claypans). Both kinds of soil mechanical impedances often coexist in maize fields, but the combined effects on root growth have seldom been studied. Soil physical properties and maize root abundance were determined in three different soils of the Rolling Pampa of Argentina, in conventionally-tilled (CT) and zero-tilled (ZT) fields cultivated with maize. In the soil with a light Bt horizon (loamy Typic Argiudoll, Chivilcoy site), induced plough pans were detected in CT plots at a depth of 0-0.12 m through significant increases in bulk density (1.15 to 1.27 Mg m-3) and cone (tip angle of 60 &#65474;&#65466;) penetrometer resistance (7.18 to 9.37 MPa in summer from ZT to CT, respectively). This caused a reduction in maize root abundance of 40-80 % in CT compared to ZT plots below the induced pans. Two of the studied soils had hard-structured Bt horizons (clay pans), but in only one of them (silty clay loam Abruptic Argiudoll, Villa L&#65475;&#65453;a site) the expected penetrometer resistance increases (up to 9 MPa) were observed with depth. In the other clay pan soil (silty clay loam Vertic Argiudoll, P&#65475;&#65449;rez Mill&#65475;&#65441;n site), penetrometer resistance did not increase with depth but reached 14.5 MPa at 0.075 and 0.2 m depth in CT and ZT plots, respectively. However, maize root abundance was stratified in the first 0.2 m at the Villa L&#65475;&#65453;a and P&#65475;&#65449;rez Mill&#65475;&#65441;n sites. There, the hard Bt horizons did not represent an absolute but a relative mechanical impedance to maize roots, by the observed root clumping through desiccation cracks.&lt;/p&gt;</dct:abstract>
    <dc:title>Root Abundance Of Maize In Conventionally-Tilled And Zero-Tilled Soils Of Argentina</dc:title>
    <dc:identifier>10.1590/s0100-06832008000200031</dc:identifier>
    <dct:references>https://doi.org/10.1590/s0100-06832008000200031</dct:references>
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