Drivers of the variability of soil phosphorus fractions in boreal forested watersheds

In the boreal forest, phosphorus (P) is tightly cycled and can be heterogenous in its distribution across the landscape. Characterizing chemical, physical, and landscape-scale drivers of variability in both concentration and forms of soil P can help us understand how P dynamics will respond to envir...

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Main Authors: Nora J. Casson, Chammi P. Attanayake, Geethani Amarawansha, Mauli Gamhewage, Darshani Kumaragamage, Jeremy G. Leathers, U.W.A. Vitharana
Format: Article
Language:English
Published: Canadian Science Publishing 2025-01-01
Series:FACETS
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Online Access:https://facetsjournal.com/doi/10.1139/facets-2025-0086
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author Nora J. Casson
Chammi P. Attanayake
Geethani Amarawansha
Mauli Gamhewage
Darshani Kumaragamage
Jeremy G. Leathers
U.W.A. Vitharana
author_facet Nora J. Casson
Chammi P. Attanayake
Geethani Amarawansha
Mauli Gamhewage
Darshani Kumaragamage
Jeremy G. Leathers
U.W.A. Vitharana
author_sort Nora J. Casson
collection DOAJ
description In the boreal forest, phosphorus (P) is tightly cycled and can be heterogenous in its distribution across the landscape. Characterizing chemical, physical, and landscape-scale drivers of variability in both concentration and forms of soil P can help us understand how P dynamics will respond to environmental change; however, data on forms of soil P in boreal forests are sparse. The goal of this study was to assess the variability of soil P across a boreal forested watershed. Seventy-four surface soil samples from a boreal forested catchment were analyzed for a suite of chemical and physical characteristics, and were paired with geospatial data to develop predictive models of forms of soil P. Water-extractable P concentrations were low, while total P (65.7–2197 mg kg−1) and plant-available (Mehlich-3-extractable) P (0.63–193 mg kg−1) concentrations varied widely across the study area. Partial least squares regression results indicated that plant-available P was strongly related to soil Mn and Ca content, while total P was more strongly related to organic C and wetness index. These results suggest that soil P can vary widely, even in nutrient-poor boreal ecosystems, and site-specific characteristics may play an important role in predicting variability.
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spelling doaj-art-6bc9df627eab4280a31a6e3bb0cecd682025-08-20T02:34:55ZengCanadian Science PublishingFACETS2371-16712025-01-011011110.1139/facets-2025-0086Drivers of the variability of soil phosphorus fractions in boreal forested watershedsNora J. Casson0Chammi P. Attanayake1Geethani Amarawansha2Mauli Gamhewage3Darshani Kumaragamage4Jeremy G. Leathers5U.W.A. Vitharana6Department of Geography, The University of Winnipeg, Winnipeg, MB R3B 2E9, CanadaDepartment of Environmental Studies and Sciences, The University of Winnipeg, Winnipeg, MB R3B 2E9, CanadaDepartment of Geography, The University of Winnipeg, Winnipeg, MB R3B 2E9, CanadaDepartment of Geography, The University of Winnipeg, Winnipeg, MB R3B 2E9, CanadaDepartment of Environmental Studies and Sciences, The University of Winnipeg, Winnipeg, MB R3B 2E9, CanadaDepartment of Geography, The University of Winnipeg, Winnipeg, MB R3B 2E9, CanadaDepartment of Soil Science, Faculty of Agriculture, University of Peradeniya, Sri LankaIn the boreal forest, phosphorus (P) is tightly cycled and can be heterogenous in its distribution across the landscape. Characterizing chemical, physical, and landscape-scale drivers of variability in both concentration and forms of soil P can help us understand how P dynamics will respond to environmental change; however, data on forms of soil P in boreal forests are sparse. The goal of this study was to assess the variability of soil P across a boreal forested watershed. Seventy-four surface soil samples from a boreal forested catchment were analyzed for a suite of chemical and physical characteristics, and were paired with geospatial data to develop predictive models of forms of soil P. Water-extractable P concentrations were low, while total P (65.7–2197 mg kg−1) and plant-available (Mehlich-3-extractable) P (0.63–193 mg kg−1) concentrations varied widely across the study area. Partial least squares regression results indicated that plant-available P was strongly related to soil Mn and Ca content, while total P was more strongly related to organic C and wetness index. These results suggest that soil P can vary widely, even in nutrient-poor boreal ecosystems, and site-specific characteristics may play an important role in predicting variability.https://facetsjournal.com/doi/10.1139/facets-2025-0086phosphorussoilborealMehlich-3nutrient
spellingShingle Nora J. Casson
Chammi P. Attanayake
Geethani Amarawansha
Mauli Gamhewage
Darshani Kumaragamage
Jeremy G. Leathers
U.W.A. Vitharana
Drivers of the variability of soil phosphorus fractions in boreal forested watersheds
FACETS
phosphorus
soil
boreal
Mehlich-3
nutrient
title Drivers of the variability of soil phosphorus fractions in boreal forested watersheds
title_full Drivers of the variability of soil phosphorus fractions in boreal forested watersheds
title_fullStr Drivers of the variability of soil phosphorus fractions in boreal forested watersheds
title_full_unstemmed Drivers of the variability of soil phosphorus fractions in boreal forested watersheds
title_short Drivers of the variability of soil phosphorus fractions in boreal forested watersheds
title_sort drivers of the variability of soil phosphorus fractions in boreal forested watersheds
topic phosphorus
soil
boreal
Mehlich-3
nutrient
url https://facetsjournal.com/doi/10.1139/facets-2025-0086
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