The impacts of cover crop mixes on the penetration resistance model of an Oxisol under no-tillage

被引:0
|
作者
de Moraes, Moacir Tuzzin [1 ]
Olbermann, Flavio Jose Rohden [2 ]
Bonetti, Joao de Andrade [3 ]
Pilegi, Luan Roberto [2 ]
Costa, Marcos Vinicius Rampi [2 ]
Pacheco, Vacilania [2 ]
Rogers, Craig David [2 ]
Guimaraes, Rachel Muylaert Locks [2 ]
机构
[1] Univ Sao Paulo, Luiz de Queiroz Coll Agr, Dept Soil Sci, 11 Padua Dias Ave, BR-13418900 Piracicaba, SP, Brazil
[2] Univ Tecnol Fed Parana, Dept Ciencias Agr, Via Conhecimento,Km 1, BR-85503390 Pato Branco, PR, Brazil
[3] Sao Paulo State Univ, Coll Agron Sci, Dept Forest Sci Soil & Environm, 3780 Univ Ave, BR-18610034 Botucatu, SP, Brazil
来源
SOIL & TILLAGE RESEARCH | 2024年 / 242卷
关键词
Cropping system; Soil strength; Soil compaction; Root system; Oxisol; HYDRAULIC CONDUCTIVITY; PENETROMETER RESISTANCE; MECHANICAL IMPEDANCE; PHYSICAL-PROPERTIES; ROOT ELONGATION; DECADES; SOIL; GROWTH; COMPACTION; MANAGEMENT;
D O I
10.1016/j.still.2024.106138
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Soil penetration resistance is used as an indicator of mechanical resistance to root growth into the soil matrix. However, penetration resistance measured only under wet soil conditions may not identify the effects of cover crops on soil structure. We aimed to determine the impact of individual and mixes of cover crops on soil penetration resistance as a function of water content and bulk density in an Oxisol under no-tillage in southern Brazil. Six treatments of individual and mixed cover crops were tested: (i) black oat; (ii) ryegrass; (iii) forage radish; (iv) wheat; (v) Fibrous-rooted crop mix: with 80 % fibrous-rooted and 20 % tap-rooted plants; and (vi) Tap-rooted crop mix: 40 % fibrous-rooted and 60 % tap-rooted plants. Soil cores were collected from a depth of 0-0.10 and 0.10-0.20 m and soil penetration resistance was evaluated under four soil water matric potentials (-6, -33, -100, and -500 kPa). Soil penetration resistance (Q) data for each treatment were fitted as a function of bulk density (rho) and water content (0) [Q=f(rho, 0)]. The soil penetration resistance model was a non-linear equation (i.e., a double power function, with a negative exponent for water content and a positive exponent for bulk density). Under a given combination of bulk density and water content values, soil penetration resistance was higher after single crops than crop mixes, indicating a crop-mediated soil strengthening process. The cover crop mixes increased the macroporosity, resulting in an adequate soil physical quality for successional crops such as soybean, although no differences were observed for cover crops at soil water matric potentials of -60 hPa and -330 hPa when soil penetration resistance was used as a static measurement. The modelling of the soil resistance to penetration, as a function of soil bulk density and soil water content, showed that cover crops changed soil cohesion and reduced the impact of drying on soil strength when compared to the single cropping systems, indicating that soil penetration resistance should be modelled under a broad range of water contents, instead of only under a specific soil water content, to quantify the impacts of cover crops on soil strength.
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页数:8
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