2019
DOI: 10.1016/j.still.2019.05.014
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Quantification of soil pore dynamics during a winter wheat cropping cycle under different tillage regimes

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Cited by 31 publications
(44 citation statements)
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“…Similar BD values found in the wheeled sub-area in contrast to the agricultural field suggest that the machinery compaction under SRC might not affect the topsoil properties as crop rotation practices. The BD found in the agricultural field was comparable to that described by Kreiselmeier et al [22] indicating that the influence of soil management (ploughing and seedbed preparation) can still be noticed at the beginning of the growing season for winter wheat.…”
Section: Influence Of Src On Total Soil Cn and Bdsupporting
confidence: 85%
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“…Similar BD values found in the wheeled sub-area in contrast to the agricultural field suggest that the machinery compaction under SRC might not affect the topsoil properties as crop rotation practices. The BD found in the agricultural field was comparable to that described by Kreiselmeier et al [22] indicating that the influence of soil management (ploughing and seedbed preparation) can still be noticed at the beginning of the growing season for winter wheat.…”
Section: Influence Of Src On Total Soil Cn and Bdsupporting
confidence: 85%
“…Sampling was conducted in the end of March 2019. Since variations in soil structure are expected to be larger in the topsoil [22], we collected undisturbed soil cores (250 cm 3 ) from a depth of 0 to 5 cm. Undisturbed samples were taken, four in the agricultural site and nine in each SRC sites, by thoroughly removing the litter layer and small herbaceous vegetation.…”
Section: Sampling and Analysis For Soil Hydraulic Propertiesmentioning
confidence: 99%
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“…While in the present study, tillage and crop stage only produced significant effects on soil capillary porosity but not on bulk density and penetration resistance (Tables 2 and 3). Under CT, pores over 50 μm in diameter decrease over time in the growth season, while under conservation tillage, enhanced biological activities (such as the growth and exudation of plant roots, soil animals and microorganisms) contribute to the formation and stabilisation of rounded pores (usually 30–500 μm in diameter) (Kautz, 2015; Kreiselmeier et al, 2019; Pagliai & De Nobili, 1993; Reichert et al, 2016). These effects may explain why the soil capillary porosity at the sowing stage was higher under CT than under conservation tillage but reverse result was observed at the harvest stage.…”
Section: Discussionmentioning
confidence: 99%
“…Furthermore, soil water retention data from saturation to wilting point can be used to derive variables important to crop growth and that are influenced by variations in soil structure. In particular, the parameters of the Kosugi (1996) model defining the geometric mean ( r m ) and SD (σ) of the pore size distribution are sensitive to soil management in response to changes in the seasonal cycle (Kreiselmeier et al., 2019), as well as characteristics of the rooting system (Scholl et al., 2014).…”
Section: Discussionmentioning
confidence: 99%