Details
Original language | English |
---|---|
Article number | 106672 |
Number of pages | 14 |
Journal | Soil and Tillage Research |
Volume | 253 |
Early online date | 22 May 2025 |
Publication status | E-pub ahead of print - 22 May 2025 |
Abstract
Soil compaction primarily stems from compression and shear stresses due to field wheeling processes. Laboratory studies have revealed the effects of these two types of stresses on soil structure and pore functions, but their consequences for soil properties and crop under field conditions need to be quantified. In this study, the temporal changes of soil physical conditions and maize growth under repeated wheeling were studied on a Mollisol. At field capacity, wheeling plots were created by a 10.4 Mg harvester with 1, 3, 5, and 21 wheeling passes (C1, C3, C5, and C21). Soil volume water content (θv) and matric potential (Ψ) were monitored during a maize growing season. The results showed that field soil deformed progressively with the increase of wheeling frequency: After 1, 3, 5, and 21 wheeling passes, the rut depths were 6.4 cm, 8.0 cm, 9.5 cm, and 13.7 cm, respectively. In response to soil compaction, the wheeling plots exhibited significant changes in soil water status with increased θv, less negative Ψ, greater water retention, but decreased water availability for plants, which lasted for the whole growing season. The C5 and C21 treatments frequently experienced waterlogging during the wet season and more severe cracking during the dry season. Compared to the control, the above-ground biomass of maize in the C1, C3, C5, and C21 treatments decreased by 14.5 %, 36.9 %, 37.0 %, and 56.4 %, respectively, and crop yield reduced by 9.7 %, 30.7 %, 38.4 %, and 59.7 %, respectively. At a load of 10.4 Mg, a threshold wheeling pass of two was recommended in the study area.
Keywords
- Maize growth, Mollisol, Repeated wheeling, Soil compaction, Soil structure
ASJC Scopus subject areas
- Agricultural and Biological Sciences(all)
- Agronomy and Crop Science
- Agricultural and Biological Sciences(all)
- Soil Science
- Earth and Planetary Sciences(all)
- Earth-Surface Processes
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In: Soil and Tillage Research, Vol. 253, 106672, 11.2025.
Research output: Contribution to journal › Article › Research › peer review
}
TY - JOUR
T1 - Quantifying the effects of repeated wheeling on soil physical conditions and maize growth in a Mollisol
AU - Huang, Xinjun
AU - Wang, Hengfei
AU - Horn, Rainer
AU - Ren, Tusheng
N1 - Publisher Copyright: © 2025 Elsevier B.V.
PY - 2025/5/22
Y1 - 2025/5/22
N2 - Soil compaction primarily stems from compression and shear stresses due to field wheeling processes. Laboratory studies have revealed the effects of these two types of stresses on soil structure and pore functions, but their consequences for soil properties and crop under field conditions need to be quantified. In this study, the temporal changes of soil physical conditions and maize growth under repeated wheeling were studied on a Mollisol. At field capacity, wheeling plots were created by a 10.4 Mg harvester with 1, 3, 5, and 21 wheeling passes (C1, C3, C5, and C21). Soil volume water content (θv) and matric potential (Ψ) were monitored during a maize growing season. The results showed that field soil deformed progressively with the increase of wheeling frequency: After 1, 3, 5, and 21 wheeling passes, the rut depths were 6.4 cm, 8.0 cm, 9.5 cm, and 13.7 cm, respectively. In response to soil compaction, the wheeling plots exhibited significant changes in soil water status with increased θv, less negative Ψ, greater water retention, but decreased water availability for plants, which lasted for the whole growing season. The C5 and C21 treatments frequently experienced waterlogging during the wet season and more severe cracking during the dry season. Compared to the control, the above-ground biomass of maize in the C1, C3, C5, and C21 treatments decreased by 14.5 %, 36.9 %, 37.0 %, and 56.4 %, respectively, and crop yield reduced by 9.7 %, 30.7 %, 38.4 %, and 59.7 %, respectively. At a load of 10.4 Mg, a threshold wheeling pass of two was recommended in the study area.
AB - Soil compaction primarily stems from compression and shear stresses due to field wheeling processes. Laboratory studies have revealed the effects of these two types of stresses on soil structure and pore functions, but their consequences for soil properties and crop under field conditions need to be quantified. In this study, the temporal changes of soil physical conditions and maize growth under repeated wheeling were studied on a Mollisol. At field capacity, wheeling plots were created by a 10.4 Mg harvester with 1, 3, 5, and 21 wheeling passes (C1, C3, C5, and C21). Soil volume water content (θv) and matric potential (Ψ) were monitored during a maize growing season. The results showed that field soil deformed progressively with the increase of wheeling frequency: After 1, 3, 5, and 21 wheeling passes, the rut depths were 6.4 cm, 8.0 cm, 9.5 cm, and 13.7 cm, respectively. In response to soil compaction, the wheeling plots exhibited significant changes in soil water status with increased θv, less negative Ψ, greater water retention, but decreased water availability for plants, which lasted for the whole growing season. The C5 and C21 treatments frequently experienced waterlogging during the wet season and more severe cracking during the dry season. Compared to the control, the above-ground biomass of maize in the C1, C3, C5, and C21 treatments decreased by 14.5 %, 36.9 %, 37.0 %, and 56.4 %, respectively, and crop yield reduced by 9.7 %, 30.7 %, 38.4 %, and 59.7 %, respectively. At a load of 10.4 Mg, a threshold wheeling pass of two was recommended in the study area.
KW - Maize growth
KW - Mollisol
KW - Repeated wheeling
KW - Soil compaction
KW - Soil structure
UR - http://www.scopus.com/inward/record.url?scp=105005600912&partnerID=8YFLogxK
U2 - 10.1016/j.still.2025.106672
DO - 10.1016/j.still.2025.106672
M3 - Article
AN - SCOPUS:105005600912
VL - 253
JO - Soil and Tillage Research
JF - Soil and Tillage Research
SN - 0167-1987
M1 - 106672
ER -