2011
DOI: 10.1016/j.geoderma.2011.04.023
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Changes in soil structure following passage of a tracked heavy machine

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Cited by 8 publications
(3 citation statements)
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“…At the column scale, the dispersivity of the water was generally correlated with pore structure characteristics (Hou, Hu, Qi, & Yang, 2018). Soil compaction often leads to changes in the volume, size, and continuity of soil pores and thus in the water transport of soils (Gayoso & Iroume, 1991;Alaoui & Diserens, 2011;Costa, Albuquerque, Costa, Warmling, & Magro, 2016). Frey, Niklaus, Kremer, Luescher, and Zimmermann (2011) found that compaction resulting from machine passes mainly decreased the macropore volume and lowered the hydraulic conductivities of the soil.…”
Section: Mechanism Of the Effects Of Compaction On Water Transportmentioning
confidence: 99%
“…At the column scale, the dispersivity of the water was generally correlated with pore structure characteristics (Hou, Hu, Qi, & Yang, 2018). Soil compaction often leads to changes in the volume, size, and continuity of soil pores and thus in the water transport of soils (Gayoso & Iroume, 1991;Alaoui & Diserens, 2011;Costa, Albuquerque, Costa, Warmling, & Magro, 2016). Frey, Niklaus, Kremer, Luescher, and Zimmermann (2011) found that compaction resulting from machine passes mainly decreased the macropore volume and lowered the hydraulic conductivities of the soil.…”
Section: Mechanism Of the Effects Of Compaction On Water Transportmentioning
confidence: 99%
“…The soil with higher water content increases with the increase of shear rate, and it is easier to reach a stable state. The green curve in Figure 6 indicates the water content of 10 % soil, as the shear rate increases, its shear strength changes quickly to level and increases no longer [8][9][10][11].…”
Section: Janosi Shear Model For Classic Ground Soilmentioning
confidence: 99%
“…These soil properties include soil texture, pore size distribution, mineralogical composition, soil structure and aggregation, infiltration, bulk density ( ρ b ), and soil organic matter (SOM) content [ 3 , 4 ]. These properties can be influenced by various factors, including land uses [ 5 , 6 ], root biomass [ 7 ], soil fauna [ 8 ], shrinking and swelling properties of clay soils [ 9 ], freezing and thawing [ 10 , 11 ], and agricultural activities such as tillage [ 12 ], wheel-traffic compaction [ 13 ], and animal trampling [ 14 ].…”
Section: Introductionmentioning
confidence: 99%