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- W2013513152 abstract "The natural regeneration of soil structure following compaction was studied on a stagnogleyic paleoargillic brown earth (Albaquic Paleudalf) at Rothamsted Experimental Station. The compaction treatment was produced by wheelings, and the area between the wheelings was used as the control. The wheeled and unwheeled areas were sampled 4 times, in spring and after harvest in 1979 and 1980 The following techniques were used to monitor regeneration: measuring the profile of the soil surface in the field and laboratory measurements of air-filled pore space, water retention, shrinkage and clod density, micromorphometry and mercury intrusion. Compaction decreased the macroporosity (pores >60 μm diameter) by over a half. Pores <6 μm diameter were unaffected by compaction. Natural regeneration of porosity in the top 5 cm was achieved within 18 months, but the soil below remained compacted for longer. The regenerated structure consisted mainly of planar voids induced by physical processes unlike the unwheeled soil which was characterised by packing voids and biopores." @default.
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- W2013513152 date "1985-08-01" @default.
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- W2013513152 title "Porosity aspects of the regeneration of soil structure after compaction" @default.
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- W2013513152 doi "https://doi.org/10.1016/s0167-1987(85)80001-5" @default.
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