Co-variation relations of physical soil properties and site characteristics of Finnish upland forests

Physical soil properties have a marked influence on the quality of forest sites and on the preconditions for forest growth and management. In this study, water retention characteristics (WRC) and related physical soil properties in addition to vegetation coverage and tree stand data were...

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Main Authors: Heiskanen, Juha, Hallikainen, Ville, Uusitalo, Jori, Ilvesniemi, Hannu
Format: Article
Language:English
Published: Finnish Society of Forest Science 2018-01-01
Series:Silva Fennica
Online Access:https://www.silvafennica.fi/article/9948
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spelling doaj-ca8e98495d194ba1a555838b0675f6712020-11-25T02:06:28ZengFinnish Society of Forest ScienceSilva Fennica2242-40752018-01-0152310.14214/sf.9948Co-variation relations of physical soil properties and site characteristics of Finnish upland forestsHeiskanen, JuhaHallikainen, VilleUusitalo, JoriIlvesniemi, Hannu Physical soil properties have a marked influence on the quality of forest sites and on the preconditions for forest growth and management. In this study, water retention characteristics (WRC) and related physical soil properties in addition to vegetation coverage and tree stand data were studied at upland forest sites in Finland. Fixed and mixed models between soil and site characteristics were formed to estimate physical and hydrologic soil characteristics and the site quality with indirect co-varying variables. In the present data, the site quality index (H100) shows a high coefficient of determination in respect to the temperature sum. It is also related to soil fine fraction content, topsoil pH and water retention at field capacity. The thickness of the humus layer is predictable from the pH and cover of xeric and mesic plant species. The soil fine fraction content (clay + silt) is closely related to water retention at field capacity, the soil layer and site type, and without WRC to the temperature sum and site index and type, as well as the slope angle. The soil bulk density is related to organic matter, depth (layer) or alternatively to organic matter, slope and field estimated textural class (fine, medium, coarse). Water retention characteristics were found to be best determinable by the fine fraction content, depth and bulk density. Water content and air-filled porosity at field capacity are closely related to the fine fraction. This study provides novel models for further investigations that aim at improved prediction models for forest growth, hydrology and trafficability.https://www.silvafennica.fi/article/9948
collection DOAJ
language English
format Article
sources DOAJ
author Heiskanen, Juha
Hallikainen, Ville
Uusitalo, Jori
Ilvesniemi, Hannu
spellingShingle Heiskanen, Juha
Hallikainen, Ville
Uusitalo, Jori
Ilvesniemi, Hannu
Co-variation relations of physical soil properties and site characteristics of Finnish upland forests
Silva Fennica
author_facet Heiskanen, Juha
Hallikainen, Ville
Uusitalo, Jori
Ilvesniemi, Hannu
author_sort Heiskanen, Juha
title Co-variation relations of physical soil properties and site characteristics of Finnish upland forests
title_short Co-variation relations of physical soil properties and site characteristics of Finnish upland forests
title_full Co-variation relations of physical soil properties and site characteristics of Finnish upland forests
title_fullStr Co-variation relations of physical soil properties and site characteristics of Finnish upland forests
title_full_unstemmed Co-variation relations of physical soil properties and site characteristics of Finnish upland forests
title_sort co-variation relations of physical soil properties and site characteristics of finnish upland forests
publisher Finnish Society of Forest Science
series Silva Fennica
issn 2242-4075
publishDate 2018-01-01
description Physical soil properties have a marked influence on the quality of forest sites and on the preconditions for forest growth and management. In this study, water retention characteristics (WRC) and related physical soil properties in addition to vegetation coverage and tree stand data were studied at upland forest sites in Finland. Fixed and mixed models between soil and site characteristics were formed to estimate physical and hydrologic soil characteristics and the site quality with indirect co-varying variables. In the present data, the site quality index (H100) shows a high coefficient of determination in respect to the temperature sum. It is also related to soil fine fraction content, topsoil pH and water retention at field capacity. The thickness of the humus layer is predictable from the pH and cover of xeric and mesic plant species. The soil fine fraction content (clay + silt) is closely related to water retention at field capacity, the soil layer and site type, and without WRC to the temperature sum and site index and type, as well as the slope angle. The soil bulk density is related to organic matter, depth (layer) or alternatively to organic matter, slope and field estimated textural class (fine, medium, coarse). Water retention characteristics were found to be best determinable by the fine fraction content, depth and bulk density. Water content and air-filled porosity at field capacity are closely related to the fine fraction. This study provides novel models for further investigations that aim at improved prediction models for forest growth, hydrology and trafficability.
url https://www.silvafennica.fi/article/9948
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