2013
DOI: 10.1016/j.still.2013.08.009
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Ca-amendment and tillage: Medium term synergies for improving key soil properties of acid soils

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Cited by 28 publications
(30 citation statements)
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References 79 publications
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“…In our case the population of earthworms (Eisenia foetida) was significantly higher in the uppermost 0-10 cm soil layer of NT plots (data not shown). In addition, the 11% higher content in water-stable aggregates (1-2 mm) found under NT in a previous study (Gómez-Paccard et al, 2013), together with a 64% higher mean weight diameter of the size distribution of water stable aggregates under NT (data not published) probably contribute to explain our results. It should also be considered that, as suggested by Douglas et al (1986) in our case NT better preserves the pore continuity and functional macroporosity that presumably developed under the grassland that was present after the cultivation and successive abandonment of our experimental site in the 1990s (Gómez-Paccard et al, 2013).…”
Section: Water Infiltration and Saturated Hydraulic Conductivitymentioning
confidence: 45%
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“…In our case the population of earthworms (Eisenia foetida) was significantly higher in the uppermost 0-10 cm soil layer of NT plots (data not shown). In addition, the 11% higher content in water-stable aggregates (1-2 mm) found under NT in a previous study (Gómez-Paccard et al, 2013), together with a 64% higher mean weight diameter of the size distribution of water stable aggregates under NT (data not published) probably contribute to explain our results. It should also be considered that, as suggested by Douglas et al (1986) in our case NT better preserves the pore continuity and functional macroporosity that presumably developed under the grassland that was present after the cultivation and successive abandonment of our experimental site in the 1990s (Gómez-Paccard et al, 2013).…”
Section: Water Infiltration and Saturated Hydraulic Conductivitymentioning
confidence: 45%
“…In addition, the 11% higher content in water-stable aggregates (1-2 mm) found under NT in a previous study (Gómez-Paccard et al, 2013), together with a 64% higher mean weight diameter of the size distribution of water stable aggregates under NT (data not published) probably contribute to explain our results. It should also be considered that, as suggested by Douglas et al (1986) in our case NT better preserves the pore continuity and functional macroporosity that presumably developed under the grassland that was present after the cultivation and successive abandonment of our experimental site in the 1990s (Gómez-Paccard et al, 2013). Although at the beginning of our experiment, the natural vegetation was cleared using a cultivator (two passes) to 20 cm depth and a power tiller (one pass) to 5-7 cm depth, these tillage operations were probably not sufficient to destroy the soil structure developed under the grassland from a depth of 5 cm to deeper layers.…”
Section: Water Infiltration and Saturated Hydraulic Conductivitymentioning
confidence: 45%
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“…Thus, there is an initial limited effect of surface liming, which is, however, compensated for by its long-term effect under NT, especially in the deeper layers. The depth effect of liming under NT is caused by the translocation of thin particles of limestone through soil channels, by the formation of complexes among water-soluble organic compounds and Ca and Mg at the soil surface and the subsequent exchange of these cations by Al at deeper layers, as well as the production of non-toxic stable complexes formed by the soil OM and the aluminum (Ernani et al, 2004;Gómez-Paccard et al, 2013;Miyazawa et al, 2002;Oliveira and Pavan, 1996;Roth and Pavan, 1991). In the case of poultry litter, similar mechanisms of translocation of particles and reaction products are expected to occur, since this residue is rich in calcium carbonates and phosphates, in addition to allowing for the formation of water-soluble organic because of the tendency of the lime and the products of its reaction to stay close to the soil surface because alkalinity must be transported from the surface by mass flow to lower layers (Wyngaard et al, 2012).…”
Section: Soil Phmentioning
confidence: 99%