<rdf:RDF xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:dct="http://purl.org/dc/terms/" xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#">
  <rdf:Description rdf:about="https://doi.org/10.1016/j.iswcr.2022.12.002">
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    <dct:isReferencedBy>Recolector de Ciencia Abierta, RECOLECTA</dct:isReferencedBy>
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    <dct:isPartOf>International Soil and Water Conservation Research</dct:isPartOf>
    <dct:license>Open Access</dct:license>
    <dct:created>2022-12-29</dct:created>
    <dc:description>Open AccessPeer reviewed </dc:description>
    <dc:description>Open AccessPeer reviewed Orchards have a high potential for carbon sequestration. However, little research is available on the spatial variability at catchment scale and on the difference between the tree area and the lanes. We analyzed theik spatial variability of soil organic carbon stock, SOCstock at 90 cm depth in an 8-ha catchment in Southern Spain with olives on a vertic soil. Results showed higher soil organic carbon concentration, SOC, in the tree area as compared to the lane up to 60 cm depth, but its impact on SOCstock was negligible since it was compensated by the higher soil bulk density in the lane. SOC at different depths was correlated with that in the top 0&#8211;5 cm. The overall SOCstock of the orchard was 4.14 kg m&#8722;2, ranging between 1.8 and 6.0 kg m&#8722;2. This SOCstock is in the mid-lower range of values reported for olive orchards, measured at smaller scale, and similar to those other intensive field crops and agroforestry under comparable rainfall conditions. The spatial variability in SOCstock was correlated to several geomorphological variables: elevation, cumulative upstream area, topographic wetness index, sediment transport index, and tillage erosion. Differences in SOC and SOCstock are driven by the sediment redistribution downslope, mainly by tillage erosion, and higher soil water availability in lower areas allowing higher biomass production. These topographic indexes and the correlation between SOC in the topsoil and SOCstock up to 90 cm should be further explored in other typology of olive orchards for facilitating the mapping of SOCstock. </dc:description>
    <dc:description>Open AccessPeer reviewed Orchards have a high potential for carbon sequestration. However, little research is available on the spatial variability at catchment scale and on the difference between the tree area and the lanes. We analyzed theik spatial variability of soil organic carbon stock, SOCstock at 90 cm depth in an 8-ha catchment in Southern Spain with olives on a vertic soil. Results showed higher soil organic carbon concentration, SOC, in the tree area as compared to the lane up to 60 cm depth, but its impact on SOCstock was negligible since it was compensated by the higher soil bulk density in the lane. SOC at different depths was correlated with that in the top 0&#8211;5 cm. The overall SOCstock of the orchard was 4.14 kg m&#8722;2, ranging between 1.8 and 6.0 kg m&#8722;2. This SOCstock is in the mid-lower range of values reported for olive orchards, measured at smaller scale, and similar to those other intensive field crops and agroforestry under comparable rainfall conditions. The spatial variability in SOCstock was correlated to several geomorphological variables: elevation, cumulative upstream area, topographic wetness index, sediment transport index, and tillage erosion. Differences in SOC and SOCstock are driven by the sediment redistribution downslope, mainly by tillage erosion, and higher soil water availability in lower areas allowing higher biomass production. These topographic indexes and the correlation between SOC in the topsoil and SOCstock up to 90 cm should be further explored in other typology of olive orchards for facilitating the mapping of SOCstock. This work was supported by projects AGL 2009-12936-C03-01, AGL2009-12936-C03-03 (Spanish Government), SHui (European Commission Grant Agreement number: 773903). TUdi (European Commission Grant Agreement number: 101000224) and EU-FEDER funds. T. Vanwalleghem thanks financial support from the Spanish Ministry of Science and Innovation, the Spanish State Research Agency, through the Severo Ochoa and Mar&#237;a de Maeztu Program for Centers and Units of Excellence in R&amp;D (Ref. CEX2019-000968-M). All this support is gratefully acknowledged. </dc:description>
    <dc:description>Open AccessPeer reviewed Orchards have a high potential for carbon sequestration. However, little research is available on the spatial variability at catchment scale and on the difference between the tree area and the lanes. We analyzed theik spatial variability of soil organic carbon stock, SOCstock at 90 cm depth in an 8-ha catchment in Southern Spain with olives on a vertic soil. Results showed higher soil organic carbon concentration, SOC, in the tree area as compared to the lane up to 60 cm depth, but its impact on SOCstock was negligible since it was compensated by the higher soil bulk density in the lane. SOC at different depths was correlated with that in the top 0&#8211;5 cm. The overall SOCstock of the orchard was 4.14 kg m&#8722;2, ranging between 1.8 and 6.0 kg m&#8722;2. This SOCstock is in the mid-lower range of values reported for olive orchards, measured at smaller scale, and similar to those other intensive field crops and agroforestry under comparable rainfall conditions. The spatial variability in SOCstock was correlated to several geomorphological variables: elevation, cumulative upstream area, topographic wetness index, sediment transport index, and tillage erosion. Differences in SOC and SOCstock are driven by the sediment redistribution downslope, mainly by tillage erosion, and higher soil water availability in lower areas allowing higher biomass production. These topographic indexes and the correlation between SOC in the topsoil and SOCstock up to 90 cm should be further explored in other typology of olive orchards for facilitating the mapping of SOCstock. This work was supported by projects AGL 2009-12936-C03-01, AGL2009-12936-C03-03 (Spanish Government), SHui (European Commission Grant Agreement number: 773903). TUdi (European Commission Grant Agreement number: 101000224) and EU-FEDER funds. T. Vanwalleghem thanks financial support from the Spanish Ministry of Science and Innovation, the Spanish State Research Agency, through the Severo Ochoa and Mar&#237;a de Maeztu Program for Centers and Units of Excellence in R&amp;D (Ref. CEX2019-000968-M). All this support is gratefully acknowledged. With funding from the Spanish government through the 'Severo Ochoa Centre of Excellence' accreditation (CEX2019-000968-M). </dc:description>
    <dc:subject>Carbon sequestration</dc:subject>
    <dc:subject>2. Zero hunger</dc:subject>
    <dc:subject>Vertic soils</dc:subject>
    <dc:subject>Mediterranean crops</dc:subject>
    <dc:subject>Catchments</dc:subject>
    <dc:subject>0401 agriculture, forestry, and fisheries</dc:subject>
    <dc:subject>04 agricultural and veterinary sciences</dc:subject>
    <dc:subject>TA1-2040</dc:subject>
    <dc:subject>15. Life on land</dc:subject>
    <dc:subject>Engineering (General). Civil engineering (General)</dc:subject>
    <dc:subject>Catchment</dc:subject>
    <dc:subject>Spatial variability</dc:subject>
    <dc:creator rdf:resource="https://orcid.org/0000-0002-6616-5815"/>
    <dc:creator rdf:resource="https://orcid.org/0000-0002-1023-9387"/>
    <dc:creator rdf:resource="https://orcid.org/0000-0002-2396-7965"/>
    <dc:creator>G&#243;mez, Jose A., Guzm&#225;n, Gema, Vanwalleghem, Tom, Vanderlinden, Karl, </dc:creator>
    <dc:date>2023-06-01</dc:date>
    <dc:type>journalpaper</dc:type>
    <dct:abstract>Open AccessPeer reviewed </dct:abstract>
    <dct:abstract>Open AccessPeer reviewed Orchards have a high potential for carbon sequestration. However, little research is available on the spatial variability at catchment scale and on the difference between the tree area and the lanes. We analyzed theik spatial variability of soil organic carbon stock, SOCstock at 90 cm depth in an 8-ha catchment in Southern Spain with olives on a vertic soil. Results showed higher soil organic carbon concentration, SOC, in the tree area as compared to the lane up to 60 cm depth, but its impact on SOCstock was negligible since it was compensated by the higher soil bulk density in the lane. SOC at different depths was correlated with that in the top 0&#8211;5 cm. The overall SOCstock of the orchard was 4.14 kg m&#8722;2, ranging between 1.8 and 6.0 kg m&#8722;2. This SOCstock is in the mid-lower range of values reported for olive orchards, measured at smaller scale, and similar to those other intensive field crops and agroforestry under comparable rainfall conditions. The spatial variability in SOCstock was correlated to several geomorphological variables: elevation, cumulative upstream area, topographic wetness index, sediment transport index, and tillage erosion. Differences in SOC and SOCstock are driven by the sediment redistribution downslope, mainly by tillage erosion, and higher soil water availability in lower areas allowing higher biomass production. These topographic indexes and the correlation between SOC in the topsoil and SOCstock up to 90 cm should be further explored in other typology of olive orchards for facilitating the mapping of SOCstock. </dct:abstract>
    <dct:abstract>Open AccessPeer reviewed Orchards have a high potential for carbon sequestration. However, little research is available on the spatial variability at catchment scale and on the difference between the tree area and the lanes. We analyzed theik spatial variability of soil organic carbon stock, SOCstock at 90 cm depth in an 8-ha catchment in Southern Spain with olives on a vertic soil. Results showed higher soil organic carbon concentration, SOC, in the tree area as compared to the lane up to 60 cm depth, but its impact on SOCstock was negligible since it was compensated by the higher soil bulk density in the lane. SOC at different depths was correlated with that in the top 0&#8211;5 cm. The overall SOCstock of the orchard was 4.14 kg m&#8722;2, ranging between 1.8 and 6.0 kg m&#8722;2. This SOCstock is in the mid-lower range of values reported for olive orchards, measured at smaller scale, and similar to those other intensive field crops and agroforestry under comparable rainfall conditions. The spatial variability in SOCstock was correlated to several geomorphological variables: elevation, cumulative upstream area, topographic wetness index, sediment transport index, and tillage erosion. Differences in SOC and SOCstock are driven by the sediment redistribution downslope, mainly by tillage erosion, and higher soil water availability in lower areas allowing higher biomass production. These topographic indexes and the correlation between SOC in the topsoil and SOCstock up to 90 cm should be further explored in other typology of olive orchards for facilitating the mapping of SOCstock. This work was supported by projects AGL 2009-12936-C03-01, AGL2009-12936-C03-03 (Spanish Government), SHui (European Commission Grant Agreement number: 773903). TUdi (European Commission Grant Agreement number: 101000224) and EU-FEDER funds. T. Vanwalleghem thanks financial support from the Spanish Ministry of Science and Innovation, the Spanish State Research Agency, through the Severo Ochoa and Mar&#237;a de Maeztu Program for Centers and Units of Excellence in R&amp;D (Ref. CEX2019-000968-M). All this support is gratefully acknowledged. </dct:abstract>
    <dct:abstract>Open AccessPeer reviewed Orchards have a high potential for carbon sequestration. However, little research is available on the spatial variability at catchment scale and on the difference between the tree area and the lanes. We analyzed theik spatial variability of soil organic carbon stock, SOCstock at 90 cm depth in an 8-ha catchment in Southern Spain with olives on a vertic soil. Results showed higher soil organic carbon concentration, SOC, in the tree area as compared to the lane up to 60 cm depth, but its impact on SOCstock was negligible since it was compensated by the higher soil bulk density in the lane. SOC at different depths was correlated with that in the top 0&#8211;5 cm. The overall SOCstock of the orchard was 4.14 kg m&#8722;2, ranging between 1.8 and 6.0 kg m&#8722;2. This SOCstock is in the mid-lower range of values reported for olive orchards, measured at smaller scale, and similar to those other intensive field crops and agroforestry under comparable rainfall conditions. The spatial variability in SOCstock was correlated to several geomorphological variables: elevation, cumulative upstream area, topographic wetness index, sediment transport index, and tillage erosion. Differences in SOC and SOCstock are driven by the sediment redistribution downslope, mainly by tillage erosion, and higher soil water availability in lower areas allowing higher biomass production. These topographic indexes and the correlation between SOC in the topsoil and SOCstock up to 90 cm should be further explored in other typology of olive orchards for facilitating the mapping of SOCstock. This work was supported by projects AGL 2009-12936-C03-01, AGL2009-12936-C03-03 (Spanish Government), SHui (European Commission Grant Agreement number: 773903). TUdi (European Commission Grant Agreement number: 101000224) and EU-FEDER funds. T. Vanwalleghem thanks financial support from the Spanish Ministry of Science and Innovation, the Spanish State Research Agency, through the Severo Ochoa and Mar&#237;a de Maeztu Program for Centers and Units of Excellence in R&amp;D (Ref. CEX2019-000968-M). All this support is gratefully acknowledged. With funding from the Spanish government through the 'Severo Ochoa Centre of Excellence' accreditation (CEX2019-000968-M). </dct:abstract>
    <dc:title>Spatial variability of soil organic carbon stock in an olive orchard at catchment scale in Southern Spain</dc:title>
    <dc:identifier>10.1016/j.iswcr.2022.12.002</dc:identifier>
    <dct:references>https://doi.org/10.1016/j.iswcr.2022.12.002</dct:references>
    <dct:relation>773903</dct:relation>
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