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dc.contributor.authorObour, Peter
dc.contributor.authorKolberg, Dorothée
dc.contributor.authorLamandé, Mathieu
dc.contributor.authorBørresen, Trond
dc.contributor.authorEdwards, Gareth
dc.contributor.authorSørensen, Claus Gron
dc.contributor.authorMunkholm, Lars J
dc.date.accessioned2020-12-01T15:45:58Z
dc.date.available2020-12-01T15:45:58Z
dc.date.created2018-08-10T15:23:38Z
dc.date.issued2018
dc.identifier.citationSoil & Tillage Research. 2018, 184, 153-163.en_US
dc.identifier.issn0167-1987
dc.identifier.urihttps://hdl.handle.net/11250/2711297
dc.description.abstractTiming of tillage operations is of utmost importance in arable farming because tillage performed under inappropriate soil water conditions results in soil structural damage and creation of undesirable seedbeds for crop establishment and growth. In a field experiment on a loamy soil in Ås, Norway, we investigated the effect of compaction and sowing dates on (i) seedbed physical properties, (ii) crop yield, and (iii) the range of water contents for tillage. The experiment was established in 2014 and the same experimental treatments were repeated in 2015, 2016 and 2017. The sowing dates included early (A1), normal/timely (A2) and late (A3) sowing dates. The compaction treatments applied each year were done wheel-by-wheel by a MF 4225 tractor weighing 4.5 Mg with a single pass (B1) and compared with a control treatment (B0). This study reported soil physical properties for only 2016 and small grain cereal yield for the four years. The soil pore characteristics determined were soil bulk density (ρb), volumetric water content (θ), air-filled porosity (εa), air permeability (ka) and pore organization indices (PO1= ka/εa and PO2= ka/εa2); strength properties measured were tensile strength (Y), soil penetration resistance (PR), degree of soil fragmentation by drop-shatter test, and water contents for tillage by calculating the range of water content for tillage (ΔθRANGE). The interaction of compaction with sowing date, generally affected soil pore characteristics, particularly at 1–5 cm depth. The A1 treatment significantly affected the strength characteristics of seedbed by decreasing soil friability and increasing Y at 1–10 cm depth, and PR down to 27 cm depth. The A3 treatment decreased yield of spring-sown small grain cereal crops, but this may be ascribed to a shorter growing season rather than an influence of soil physical properties. The A1 and A3 decreased the range of water contents for tillage compared to the A2, although the difference was not significant at any of the depths studied. Findings of the study have practical implications for cropping regimes in colder climates where farmers can be faced with a short growing period by showing that cultivation in wet soil conditions such as early spring can adversely affect seedbed physical properties and soil workability for subsequent tillage operations.en_US
dc.language.isoengen_US
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/deed.no*
dc.titleCompaction and sowing date change soil physical properties and crop yield in a loamy temperate soilen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionacceptedVersionen_US
dc.source.pagenumber153-163en_US
dc.source.volume184en_US
dc.source.journalSoil & Tillage Researchen_US
dc.identifier.doi10.1016/j.still.2018.07.014
dc.identifier.cristin1601073
cristin.unitcode192,14,0,0
cristin.unitnameMiljøvitenskap og naturforvaltning
cristin.ispublishedtrue
cristin.fulltextpostprint
cristin.qualitycode1


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Attribution-NonCommercial-NoDerivatives 4.0 Internasjonal
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