Plant and Soil · 2014
Root induced changes of effective 1D hydraulic properties in a soil column
Scholl, P., Leitner, D., Kammerer, G., Loiskandl, W., Kaul, H., Bodner, G.
Export
Root induced changes of effective 1D hydraulic properties in…
Abstract
Aims Roots are essential drivers of soil structure and pore formation. This study aimed at quantifying root induced changes ofthe pore size distribution (PSD). The focus was on the extent of clogging vs. formation of pores during active root growth. Methods Parameters ofKosugi’s lognormal PSDmodel were determined by inverse estimation in a column experiment with two cover crops (mustard, rye) and an unplanted control. Pore dynamics were described using aconvection–dispersion like pore evolution model. Results Rooted treatments showed a wider range of pore radii with increasing volumes of large macropores >500 μm and micropores <2.5 μm, while fine macropores, mesopores and larger micropores decreased. The non-rooted control showed narrowing of the PSD and reduced porosity over all radius classes. The pore evolution model accurately described root induced changes, while structure degradation in the non-rooted control was not captured properly. Our study demonstrated significant short term root effects with heterogenization ofthe pore system as dominant process of root induced structure formation. Conclusions Pore clogging is suggested as a partial cause for reduced pore volume. The important change in micro- and large macropores however indicates that multiple mechanic and biochemical processes are involved in root-pore interactions.
Show all
Aims Roots are essential drivers of soil structure and pore formation. This study aimed at quantifying root induced changes ofthe pore size distribution (PSD). The focus was on the extent of clogging vs. formation of pores during active root growth. Methods Parameters ofKosugi’s lognormal PSDmodel were determined by inverse estimation in a column experiment with two cover crops (mustard, rye) and an unplanted control. Pore dynamics were described using aconvection–dispersion like pore evolution model. Results Rooted treatments showed a wider range of pore radii with increasing volumes of large macropores >500 μm and micropores <2.5 μm, while fine macropores, mesopores and larger micropores decreased. The non-rooted control showed narrowing of the PSD and reduced porosity over all radius classes. The pore evolution model accurately described root induced changes, while structure degradation in the non-rooted control was not captured properly. Our study demonstrated significant short term root effects with heterogenization ofthe pore system as dominant process of root induced structure formation. Conclusions Pore clogging is suggested as a partial cause for reduced pore volume. The important change in micro- and large macropores however indicates that multiple mechanic and biochemical processes are involved in root-pore interactions.
Aims Roots are essential drivers of soil structure and pore formation. This study aimed at quantifying root induced changes ofthe pore size distribution (PSD). The focus was on the extent of clogging vs. formation of pores during active root growth. Methods Parameters ofKosugi’s lognormal PSDmodel were determined by inverse estimation in a column experiment with two cover crops (mustard, rye) and an unplanted control. Pore dynamics were described using aconvection–dispersion like pore evolution model. Results Rooted treatments showed a wider range of pore radii with increasing volumes of large macropores >500 μm and micropores <2.5 μm, while fine macropores, mesopores and larger micropores decreased. The non-rooted control showed narrowing of the PSD and reduced porosity over all radius classes. The pore evolution model accurately described root induced changes, while structure degradation in the non-rooted control was not captured properly. Our study demonstrated significant short term root effects with heterogenization ofthe pore system as dominant process of root induced structure formation. Conclusions Pore clogging is suggested as a partial cause for reduced pore volume. The important change in micro- and large macropores however indicates that multiple mechanic and biochemical processes are involved in root-pore interactions.
Similar papers
Effect of root density of wheat and okra on hydraulic properties of an unsaturated compacted loam
Chen et al. · 2019 · European Journal of Soil Science
6 shared concepts
10 findings1 site
Environmental and management influences on temporal variability of near saturated soil hydraulic properties
Bodner et al. · 2013 · Geoderma
6 shared concepts
8 findings1 site
Coarse and fine root plants affect pore size distributions differently
Bodner, Leitner & Kaul · 2014 · Plant and Soil
5 shared concepts
4 findings
