<abstract xmlns="http://www.w3.org/1999/xhtml">The layering of the soil profile can influence the accumulation of infiltrated water and the way in which subsurface runoff is formed. This paper examines a mountain podzol characterized by clearly developed soil horizons. After these horizons had been identified, distinct soil layers were defined (the eluvial horizon, the spodic horizon (undifferentiated), and weathered bedrock). Saturated hydraulic conductivity (Ks), particle size distribution and bulk density were measured in these layers. A visualization of the distribution of infiltrated water in the podzolic profile was performed using a dye tracer experiment. The accumulation of dyed water and a distinct lateral flow were detected in the eluvial layer. Only limited entry of water into the spodic layer was observed. These effects were caused by changes in soil hydraulic properties (SHP) among the investigated layers. For the spodic horizons, the measured Ks value (crucial SHP) was significantly lower than the Ks values for the other tested horizons. The probable reason for the lower Ks was an accumulation of fine particles and various substances in the spodic horizons, and corresponding changes in the porous system. The observed effects of layering indicate that water can be accumulated and subsurface runoff can be formed over the spodic layer during intensive rain or snow melting.</abstract>

The layering of the soil profile can influence the accumulation of infiltrated water and the way in which subsurface runoff is formed. This paper examines a mountain podzol characterized by clearly developed soil horizons. After these horizons had been identified, distinct soil layers were defined (the eluvial horizon, the spodic horizon (undifferentiated), and weathered bedrock). Saturated hydraulic conductivity (Ks), particle size distribution and bulk density were measured in these layers. A visualization of the distribution of infiltrated water in the podzolic profile was performed using a dye tracer experiment. The accumulation of dyed water and a distinct lateral flow were detected in the eluvial layer. Only limited entry of water into the spodic layer was observed. These effects were caused by changes in soil hydraulic properties (SHP) among the investigated layers. For the spodic horizons, the measured Ks value (crucial SHP) was significantly lower than the Ks values for the other tested horizons. The probable reason for the lower Ks was an accumulation of fine particles and various substances in the spodic horizons, and corresponding changes in the porous system. The observed effects of layering indicate that water can be accumulated and subsurface runoff can be formed over the spodic layer during intensive rain or snow melting.

The layering of a mountain podzol can strongly affect the distribution of infiltrated water in the soil profile

Journal of Hydrology and Hydromechanics

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 License.

The layering of the soil profile can influence the accumulation of infiltrated water and the way in which subsurface runoff is formed. This paper examines a...

The layering of a mountain podzol can strongly affect the distribution of infiltrated water in the soil profile

Publicado en línea: 14 ago 2018

Páginas: 348 - 356

Recibido: 03 jul 2017

Aceptado: 22 ene 2018

DOI: https://doi.org/10.2478/johh-2018-0014

Palabras clave
Brilliant blue, Guelph permeameter, Field saturated hydraulic conductivity, Infiltration into layered soil, Mountain forest

© 2018 Lukáš Jačka, published by Sciendo

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 License.

The layering of a mountain podzol can strongly affect the distribution of infiltrated water in the soil profile

Publicado en línea: 14 ago 2018

Páginas: 348 - 356

Recibido: 03 jul 2017

Aceptado: 22 ene 2018

DOI: https://doi.org/10.2478/johh-2018-0014

Palabras claveBrilliant blue, Guelph permeameter, Field saturated hydraulic conductivity, Infiltration into layered soil, Mountain forest

© 2018 Lukáš Jačka, published by Sciendo

This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 License.

Palabras clave
Brilliant blue, Guelph permeameter, Field saturated hydraulic conductivity, Infiltration into layered soil, Mountain forest