Impact of a moderate/high-severity prescribed eucalypt forest fire on soil phosphorous stocks and partitioning
This study examines the direct impact of a moderate/high-severity prescribed fire on phosphorous (P) stocks and partitioning in oligotrophic soils of a dry eucalypt forest within Sydney's water supply catchments, Australia. We also quantify and characterize the P present in the ash produced in...
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Published in | The Science of the total environment Vol. 621; pp. 1103 - 1114 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
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Netherlands
Elsevier B.V
15.04.2018
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Abstract | This study examines the direct impact of a moderate/high-severity prescribed fire on phosphorous (P) stocks and partitioning in oligotrophic soils of a dry eucalypt forest within Sydney's water supply catchments, Australia. We also quantify and characterize the P present in the ash produced in this fire, and explore its relationships with the maximum temperatures recorded in the litter layer during the burn.
In these oligotrophic soils, P concentrations were already relatively low before the fire (<130mgkg−1, mainly in organic forms). The fire consumed the entire litter layer and the thin Oa soil horizon, creating 6.3±3.1tha−1 of ash, and resulted into direct net P losses of ~7kgha−1. The P lost was mostly organic and there was a moderate net gain of inorganic and non-reactive P forms. Importantly, only a small proportion of the post-fire P was bioavailable (equivalent to ~3% of the total P lost during fire). Higher total P concentrations in ash corresponded with higher maximum temperatures (>650°C) recorded in the burning litter layer, but effects of fire temperature on ash P partitioning were not significant.
Fire not only transformed P chemically, but also physically. Our results show that, immediately after fire, up to 2kgha−1 of P was present in the ash layer and, therefore, highly erodible and susceptible to be transported off-site by wind- and water erosion. Even if most of this P was, initially, of low bioavailability, its transfer to depositional environments with different geochemical conditions (e.g. anoxic sediments in water reservoirs) can alter its geochemical forms and availability. Further investigation of potential P transformations off-site is therefore essential, particularly given that SE-Australian water supply catchments are subject to recurrent perturbation by prescribed fire and wildfires. The latter have already resulted in major algal blooms in water supply reservoirs.
[Display omitted]
•A moderate/high-severity prescribed fire in dry eucalypt forest was investigated.•Fire led to net phosphorous losses of ~7kgha−1 from litter and surface soil.•Fire increased inorganic P stocks, but only a minor proportion was bioavailable.•~2kg total Pha−1 was transferred from litter and soil to the highly-erodible ash.•T>650°C in the burning litter layer related to higher ash total P concentrations |
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AbstractList | This study examines the direct impact of a moderate/high-severity prescribed fire on phosphorous (P) stocks and partitioning in oligotrophic soils of a dry eucalypt forest within Sydney's water supply catchments, Australia. We also quantify and characterize the P present in the ash produced in this fire, and explore its relationships with the maximum temperatures recorded in the litter layer during the burn.In these oligotrophic soils, P concentrations were already relatively low before the fire (<130mgkg⁻¹, mainly in organic forms). The fire consumed the entire litter layer and the thin Oa soil horizon, creating 6.3±3.1tha⁻¹ of ash, and resulted into direct net P losses of ~7kgha⁻¹. The P lost was mostly organic and there was a moderate net gain of inorganic and non-reactive P forms. Importantly, only a small proportion of the post-fire P was bioavailable (equivalent to ~3% of the total P lost during fire). Higher total P concentrations in ash corresponded with higher maximum temperatures (>650°C) recorded in the burning litter layer, but effects of fire temperature on ash P partitioning were not significant.Fire not only transformed P chemically, but also physically. Our results show that, immediately after fire, up to 2kgha⁻¹ of P was present in the ash layer and, therefore, highly erodible and susceptible to be transported off-site by wind- and water erosion. Even if most of this P was, initially, of low bioavailability, its transfer to depositional environments with different geochemical conditions (e.g. anoxic sediments in water reservoirs) can alter its geochemical forms and availability. Further investigation of potential P transformations off-site is therefore essential, particularly given that SE-Australian water supply catchments are subject to recurrent perturbation by prescribed fire and wildfires. The latter have already resulted in major algal blooms in water supply reservoirs. This study examines the direct impact of a moderate/high-severity prescribed fire on phosphorous (P) stocks and partitioning in oligotrophic soils of a dry eucalypt forest within Sydney's water supply catchments, Australia. We also quantify and characterize the P present in the ash produced in this fire, and explore its relationships with the maximum temperatures recorded in the litter layer during the burn. In these oligotrophic soils, P concentrations were already relatively low before the fire (<130mgkg-1, mainly in organic forms). The fire consumed the entire litter layer and the thin Oa soil horizon, creating 6.3±3.1tha-1 of ash, and resulted into direct net P losses of ~7kgha-1. The P lost was mostly organic and there was a moderate net gain of inorganic and non-reactive P forms. Importantly, only a small proportion of the post-fire P was bioavailable (equivalent to ~3% of the total P lost during fire). Higher total P concentrations in ash corresponded with higher maximum temperatures (>650°C) recorded in the burning litter layer, but effects of fire temperature on ash P partitioning were not significant. Fire not only transformed P chemically, but also physically. Our results show that, immediately after fire, up to 2kgha-1 of P was present in the ash layer and, therefore, highly erodible and susceptible to be transported off-site by wind- and water erosion. Even if most of this P was, initially, of low bioavailability, its transfer to depositional environments with different geochemical conditions (e.g. anoxic sediments in water reservoirs) can alter its geochemical forms and availability. Further investigation of potential P transformations off-site is therefore essential, particularly given that SE-Australian water supply catchments are subject to recurrent perturbation by prescribed fire and wildfires. The latter have already resulted in major algal blooms in water supply reservoirs.This study examines the direct impact of a moderate/high-severity prescribed fire on phosphorous (P) stocks and partitioning in oligotrophic soils of a dry eucalypt forest within Sydney's water supply catchments, Australia. We also quantify and characterize the P present in the ash produced in this fire, and explore its relationships with the maximum temperatures recorded in the litter layer during the burn. In these oligotrophic soils, P concentrations were already relatively low before the fire (<130mgkg-1, mainly in organic forms). The fire consumed the entire litter layer and the thin Oa soil horizon, creating 6.3±3.1tha-1 of ash, and resulted into direct net P losses of ~7kgha-1. The P lost was mostly organic and there was a moderate net gain of inorganic and non-reactive P forms. Importantly, only a small proportion of the post-fire P was bioavailable (equivalent to ~3% of the total P lost during fire). Higher total P concentrations in ash corresponded with higher maximum temperatures (>650°C) recorded in the burning litter layer, but effects of fire temperature on ash P partitioning were not significant. Fire not only transformed P chemically, but also physically. Our results show that, immediately after fire, up to 2kgha-1 of P was present in the ash layer and, therefore, highly erodible and susceptible to be transported off-site by wind- and water erosion. Even if most of this P was, initially, of low bioavailability, its transfer to depositional environments with different geochemical conditions (e.g. anoxic sediments in water reservoirs) can alter its geochemical forms and availability. Further investigation of potential P transformations off-site is therefore essential, particularly given that SE-Australian water supply catchments are subject to recurrent perturbation by prescribed fire and wildfires. The latter have already resulted in major algal blooms in water supply reservoirs. This study examines the direct impact of a moderate/high-severity prescribed fire on phosphorous (P) stocks and partitioning in oligotrophic soils of a dry eucalypt forest within Sydney's water supply catchments, Australia. We also quantify and characterize the P present in the ash produced in this fire, and explore its relationships with the maximum temperatures recorded in the litter layer during the burn. In these oligotrophic soils, P concentrations were already relatively low before the fire (<130mgkg−1, mainly in organic forms). The fire consumed the entire litter layer and the thin Oa soil horizon, creating 6.3±3.1tha−1 of ash, and resulted into direct net P losses of ~7kgha−1. The P lost was mostly organic and there was a moderate net gain of inorganic and non-reactive P forms. Importantly, only a small proportion of the post-fire P was bioavailable (equivalent to ~3% of the total P lost during fire). Higher total P concentrations in ash corresponded with higher maximum temperatures (>650°C) recorded in the burning litter layer, but effects of fire temperature on ash P partitioning were not significant. Fire not only transformed P chemically, but also physically. Our results show that, immediately after fire, up to 2kgha−1 of P was present in the ash layer and, therefore, highly erodible and susceptible to be transported off-site by wind- and water erosion. Even if most of this P was, initially, of low bioavailability, its transfer to depositional environments with different geochemical conditions (e.g. anoxic sediments in water reservoirs) can alter its geochemical forms and availability. Further investigation of potential P transformations off-site is therefore essential, particularly given that SE-Australian water supply catchments are subject to recurrent perturbation by prescribed fire and wildfires. The latter have already resulted in major algal blooms in water supply reservoirs. [Display omitted] •A moderate/high-severity prescribed fire in dry eucalypt forest was investigated.•Fire led to net phosphorous losses of ~7kgha−1 from litter and surface soil.•Fire increased inorganic P stocks, but only a minor proportion was bioavailable.•~2kg total Pha−1 was transferred from litter and soil to the highly-erodible ash.•T>650°C in the burning litter layer related to higher ash total P concentrations This study examines the direct impact of a moderate/high-severity prescribed fire on phosphorous (P) stocks and partitioning in oligotrophic soils of a dry eucalypt forest within Sydney's water supply catchments, Australia. We also quantify and characterize the P present in the ash produced in this fire, and explore its relationships with the maximum temperatures recorded in the litter layer during the burn. In these oligotrophic soils, P concentrations were already relatively low before the fire (<130mgkg , mainly in organic forms). The fire consumed the entire litter layer and the thin Oa soil horizon, creating 6.3±3.1tha of ash, and resulted into direct net P losses of ~7kgha . The P lost was mostly organic and there was a moderate net gain of inorganic and non-reactive P forms. Importantly, only a small proportion of the post-fire P was bioavailable (equivalent to ~3% of the total P lost during fire). Higher total P concentrations in ash corresponded with higher maximum temperatures (>650°C) recorded in the burning litter layer, but effects of fire temperature on ash P partitioning were not significant. Fire not only transformed P chemically, but also physically. Our results show that, immediately after fire, up to 2kgha of P was present in the ash layer and, therefore, highly erodible and susceptible to be transported off-site by wind- and water erosion. Even if most of this P was, initially, of low bioavailability, its transfer to depositional environments with different geochemical conditions (e.g. anoxic sediments in water reservoirs) can alter its geochemical forms and availability. Further investigation of potential P transformations off-site is therefore essential, particularly given that SE-Australian water supply catchments are subject to recurrent perturbation by prescribed fire and wildfires. The latter have already resulted in major algal blooms in water supply reservoirs. |
Author | Doerr, Stefan H. Otero, Xose L. Santín, Cristina Chafer, Chris J. |
Author_xml | – sequence: 1 givenname: Cristina orcidid: 0000-0001-9901-2658 surname: Santín fullname: Santín, Cristina email: c.santin@swansea.ac.uk organization: Department of Geography, College of Science, Swansea University, Singleton Park, Swansea SA2 8PP, UK – sequence: 2 givenname: Xose L. surname: Otero fullname: Otero, Xose L. organization: Department of Edaphology and Agricultural Chemistry, University of Santiago de Compostela, Santiago de Compostela, Spain – sequence: 3 givenname: Stefan H. surname: Doerr fullname: Doerr, Stefan H. organization: Department of Geography, College of Science, Swansea University, Singleton Park, Swansea SA2 8PP, UK – sequence: 4 givenname: Chris J. surname: Chafer fullname: Chafer, Chris J. organization: Water New South Wales, 2–6 Station Street, Penrith, NSW 2751, Australia |
BackLink | https://www.ncbi.nlm.nih.gov/pubmed/29103642$$D View this record in MEDLINE/PubMed |
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Keywords | Organic phosphorus Bioavailable phosphorus Algal blooms Fuel reduction burn Ash 31P NMR P NMR |
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Snippet | This study examines the direct impact of a moderate/high-severity prescribed fire on phosphorous (P) stocks and partitioning in oligotrophic soils of a dry... |
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SubjectTerms | 31P NMR Algal blooms Ash Australia bioavailability Bioavailable phosphorus Eucalyptus forest fires forests Fuel reduction burn Organic phosphorus phosphorus prescribed burning sediments soil horizons temperature water erosion water reservoirs water supply watersheds |
Title | Impact of a moderate/high-severity prescribed eucalypt forest fire on soil phosphorous stocks and partitioning |
URI | https://dx.doi.org/10.1016/j.scitotenv.2017.10.116 https://www.ncbi.nlm.nih.gov/pubmed/29103642 https://www.proquest.com/docview/1961034812 https://www.proquest.com/docview/2000544990 |
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