1976Soil Science Society of America JournalRequires access

Soil Compaction After Tree‐Length Skidding in Northern Mississippi

B. P. Dickerson

Open publisher page 133 citations

Abstract

Abstract After skidding with a rubber‐tired skidder, bulk densities of wheel‐rutted soils increased an average of 20% to 1.55 g/cm 3 ; the increase was 10% for the soils between the ruts which were compacted by the movement of logs. Macropores were reduced 68% for wheel‐rutted soils and 38% for log‐disturbed soils; micropore space of both increased about 7%. Percolation rates decreased initially but recovered gradually. Wheel‐rutted soils require about 12 years to recover and log‐disturbed soils about 8 years.

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What this paper is about

Abstract After skidding with a rubber‐tired skidder, bulk densities of wheel‐rutted soils increased an average of 20% to 1.55 g/cm 3 ; the increase was 10% for the soils between the ruts which were compacted by the movement of logs. Macropores were reduced 68% for wheel‐rutted soils and 38% for log‐disturbed soils; micropore space of both increased about 7%. Percolation rates decreased initially but recovered gradually. Wheel‐rutted soils require about 12 years to recover and log‐disturbed soils about 8 years.

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Available abstract

Abstract After skidding with a rubber‐tired skidder, bulk densities of wheel‐rutted soils increased an average of 20% to 1.55 g/cm 3 ; the increase was 10% for the soils between the ruts which were compacted by the movement of logs. Macropores were reduced 68% for wheel‐rutted soils and 38% for log‐disturbed soils; micropore space of both increased about 7%. Percolation rates decreased initially but recovered gradually. Wheel‐rutted soils require about 12 years to recover and log‐disturbed soils about 8 years.

Key concepts: Soil water, Macropore, Characterisation of pore space in soil, Environmental science, Compaction, Soil science, Percolation (cognitive psychology), Soil compaction

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