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2010
DOI: 10.1007/s11104-010-0405-3
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Influence of grazing on hydraulic and mechanical properties of semiarid steppe soils under different vegetation type in Inner Mongolia, China

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Cited by 62 publications
(44 citation statements)
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“…This was demonstrated by Carminati and Vetterlein (2013) and Carminati et al (2010) who found that hydraulic conductivity and water uptake were enhanced by exudates after multiple cycles of wetting and drying. One driver is enhanced pore structure, which Reszkowska et al (2011) found helped to recover hydraulic conductivity of rhizosphere soil in a degraded pasture field under wet conditions. Exudates can therefore decrease plant water stress by regulating water content dynamics and aiding capture of water in the rhizosphere Ahmed et al 2014).…”
Section: Introductionmentioning
confidence: 99%
“…This was demonstrated by Carminati and Vetterlein (2013) and Carminati et al (2010) who found that hydraulic conductivity and water uptake were enhanced by exudates after multiple cycles of wetting and drying. One driver is enhanced pore structure, which Reszkowska et al (2011) found helped to recover hydraulic conductivity of rhizosphere soil in a degraded pasture field under wet conditions. Exudates can therefore decrease plant water stress by regulating water content dynamics and aiding capture of water in the rhizosphere Ahmed et al 2014).…”
Section: Introductionmentioning
confidence: 99%
“…On the other hand, animal trampling during grazing causes external stresses on the soil altering its structure and pore functions (Reszkowska et al, 2011). Thus, the physical quality of soils can be studied based on two concepts: the soil's physical resistance and its resilience (Gregory et al, 2009).…”
Section: A)mentioning
confidence: 99%
“…This is relevant in soils derived from volcanic ashes in southern Chile, since livestock production systems are based on pastures, which are grazed throughout the year, leaving the soil exposed to the effect of external pressures caused by grazing animals, and internal stresses due to wetting and drying cycles . While the first type of stress (animal trampling) can cause compaction, negatively affecting soil structure and its physical functions like hydraulic conductivity (Reszkowska et al, 2011), the internal stress allows the soil to recover its functions like air conductivity due to crack formation (Dörner et al, 2011.…”
Section: A)mentioning
confidence: 99%
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“…Summarizing and integrating current knowledge and recent experimental findings Kölbl et al (2011, this issue) show that intensive grazing clearly decreased soil aggregation and the amount of fresh, litter-like particulate organic matter. As a consequence of weak aggregation in combination with animal trampling, soil organic matter mineralization is enhanced, whereas topsoil bulk densities were increased and infiltration rates, saturated hydraulic and air conductivities (Reszkowka et al, 2011, this issue) were found to be decreased. The effects of soil structure disruption due to grazing was further amplified by the degradation of vegetation patches and resulted in a texture controlled wettability of the soil surface (Kölbl et al, 2011, this issue).…”
mentioning
confidence: 96%