Temporal trends in chemical parameters of upland forest soils in southern Finland

Changes in chemical soil properties during periods of 12 to 28 years were studied in 54 stands in southern Finland. Relative slopes (%/year) were calculated for the changes in soil variables in order to utilise all the sampling occasions (2â6) covered by the study period. Only the res...

Full description

Bibliographic Details
Main Authors: Tamminen, Pekka, Derome, John
Format: Article
Language:English
Published: Finnish Society of Forest Science 2005-01-01
Series:Silva Fennica
Online Access:https://www.silvafennica.fi/article/370
id doaj-66ceeec5fd624d82ae7da006d3a08735
record_format Article
spelling doaj-66ceeec5fd624d82ae7da006d3a087352020-11-25T02:01:15ZengFinnish Society of Forest ScienceSilva Fennica2242-40752005-01-0139310.14214/sf.370Temporal trends in chemical parameters of upland forest soils in southern FinlandTamminen, PekkaDerome, John Changes in chemical soil properties during periods of 12 to 28 years were studied in 54 stands in southern Finland. Relative slopes (%/year) were calculated for the changes in soil variables in order to utilise all the sampling occasions (2â6) covered by the study period. Only the results of new analyses made on the soil samples could be used owing to unpredictable differences between the results of the original and new analyses. During the study period the acidity (pH, exchangeable acidity) of the organic layer had decreased, and the mineral soil had become more acidic only in terms of increased exchangeable aluminium concentrations. An increasing trend in the amount of soil organic matter best explained the acidity variables: it lowered acidity in the organic layer, but increased it in the mineral soil. Acid ammonium acetate extractable nutrients showed decreasing trends over time, apart from an increasing trend for sulphur in the 0â30 cm mineral soil layer. Total concentrations of most elements in the organic layer, including nitrogen and sulphur, also showed a decreasing trend. Changes in the soil variables could not be firmly connected to deposition, wood production or the amount of nutrients accumulated in woody tissues. However, the decrease in sulphur concentrations in the organic layer was clearly linked with the decrease in sulphur deposition in recent years.https://www.silvafennica.fi/article/370
collection DOAJ
language English
format Article
sources DOAJ
author Tamminen, Pekka
Derome, John
spellingShingle Tamminen, Pekka
Derome, John
Temporal trends in chemical parameters of upland forest soils in southern Finland
Silva Fennica
author_facet Tamminen, Pekka
Derome, John
author_sort Tamminen, Pekka
title Temporal trends in chemical parameters of upland forest soils in southern Finland
title_short Temporal trends in chemical parameters of upland forest soils in southern Finland
title_full Temporal trends in chemical parameters of upland forest soils in southern Finland
title_fullStr Temporal trends in chemical parameters of upland forest soils in southern Finland
title_full_unstemmed Temporal trends in chemical parameters of upland forest soils in southern Finland
title_sort temporal trends in chemical parameters of upland forest soils in southern finland
publisher Finnish Society of Forest Science
series Silva Fennica
issn 2242-4075
publishDate 2005-01-01
description Changes in chemical soil properties during periods of 12 to 28 years were studied in 54 stands in southern Finland. Relative slopes (%/year) were calculated for the changes in soil variables in order to utilise all the sampling occasions (2â6) covered by the study period. Only the results of new analyses made on the soil samples could be used owing to unpredictable differences between the results of the original and new analyses. During the study period the acidity (pH, exchangeable acidity) of the organic layer had decreased, and the mineral soil had become more acidic only in terms of increased exchangeable aluminium concentrations. An increasing trend in the amount of soil organic matter best explained the acidity variables: it lowered acidity in the organic layer, but increased it in the mineral soil. Acid ammonium acetate extractable nutrients showed decreasing trends over time, apart from an increasing trend for sulphur in the 0â30 cm mineral soil layer. Total concentrations of most elements in the organic layer, including nitrogen and sulphur, also showed a decreasing trend. Changes in the soil variables could not be firmly connected to deposition, wood production or the amount of nutrients accumulated in woody tissues. However, the decrease in sulphur concentrations in the organic layer was clearly linked with the decrease in sulphur deposition in recent years.
url https://www.silvafennica.fi/article/370
work_keys_str_mv AT tamminenpekka temporaltrendsinchemicalparametersofuplandforestsoilsinsouthernfinland
AT deromejohn temporaltrendsinchemicalparametersofuplandforestsoilsinsouthernfinland
_version_ 1724957915634204672