Magnetic Properties of Plant Ashes and Their Influence on Magnetic Signatures of Fire in Soils
Fires are an integral part of many terrestrial ecosystems and have a strong impact on soil properties. While reports of topsoil magnetic enhancement after fires vary widely, recent evidence suggests that plant ashes provide the most significant source of magnetic enhancement after burning. To invest...
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crfrontiers:10.3389/feart.2020.592659 2024-09-15T18:14:27+00:00 Magnetic Properties of Plant Ashes and Their Influence on Magnetic Signatures of Fire in Soils Till, Jessica L. Moskowitz, Bruce Poulton, Simon W. Icelandic Centre for Research 2021 http://dx.doi.org/10.3389/feart.2020.592659 https://www.frontiersin.org/articles/10.3389/feart.2020.592659/full unknown Frontiers Media SA https://creativecommons.org/licenses/by/4.0/ Frontiers in Earth Science volume 8 ISSN 2296-6463 journal-article 2021 crfrontiers https://doi.org/10.3389/feart.2020.592659 2024-09-03T04:05:14Z Fires are an integral part of many terrestrial ecosystems and have a strong impact on soil properties. While reports of topsoil magnetic enhancement after fires vary widely, recent evidence suggests that plant ashes provide the most significant source of magnetic enhancement after burning. To investigate the magnetic properties of burnt plant material, samples of individual plant species from Iceland and Germany were cleaned and combusted at various temperatures prior to rock magnetic and geochemical characterization. Mass-normalized saturation magnetization values for burnt plant residues increase with the extent of burning in nearly all samples. However, when normalized to the loss on ignition, fewer than half of ash and charcoal samples display magnetic enhancement relative to intact plant material. Thus, while magnetic mineral concentrations generally increase, changes in the total amount of magnetic material are much more variable. Elemental analyses of Icelandic samples reveal that both total plant Fe and saturation magnetization are strongly correlated with Ti and Al, indicating that most of the Fe-bearing magnetic phases originate from inorganic material such as soil and atmospheric dust. Electron microscopy confirmed that inorganic particulate matter remains on most plant surfaces after cleaning. Plants with more textured leaf surfaces retain more dust, and ash from these samples tend to exhibit higher saturation magnetization and metal concentrations. Magnetic properties of plant ash therefore result from the thermal transformation of Fe in both organic compounds and inorganic particulate matter, which become concentrated on a mass basis when organic matter is combusted. These results indicate that the soil magnetic response to burning will vary among sites and regions as a function of 1) fire intensity, 2) the local composition of dust and soil particles on leaf surfaces, and 3) vegetation type and consequent differences in leaf morphologies. Article in Journal/Newspaper Iceland Frontiers (Publisher) Frontiers in Earth Science 8 |
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Fires are an integral part of many terrestrial ecosystems and have a strong impact on soil properties. While reports of topsoil magnetic enhancement after fires vary widely, recent evidence suggests that plant ashes provide the most significant source of magnetic enhancement after burning. To investigate the magnetic properties of burnt plant material, samples of individual plant species from Iceland and Germany were cleaned and combusted at various temperatures prior to rock magnetic and geochemical characterization. Mass-normalized saturation magnetization values for burnt plant residues increase with the extent of burning in nearly all samples. However, when normalized to the loss on ignition, fewer than half of ash and charcoal samples display magnetic enhancement relative to intact plant material. Thus, while magnetic mineral concentrations generally increase, changes in the total amount of magnetic material are much more variable. Elemental analyses of Icelandic samples reveal that both total plant Fe and saturation magnetization are strongly correlated with Ti and Al, indicating that most of the Fe-bearing magnetic phases originate from inorganic material such as soil and atmospheric dust. Electron microscopy confirmed that inorganic particulate matter remains on most plant surfaces after cleaning. Plants with more textured leaf surfaces retain more dust, and ash from these samples tend to exhibit higher saturation magnetization and metal concentrations. Magnetic properties of plant ash therefore result from the thermal transformation of Fe in both organic compounds and inorganic particulate matter, which become concentrated on a mass basis when organic matter is combusted. These results indicate that the soil magnetic response to burning will vary among sites and regions as a function of 1) fire intensity, 2) the local composition of dust and soil particles on leaf surfaces, and 3) vegetation type and consequent differences in leaf morphologies. |
author2 |
Icelandic Centre for Research |
format |
Article in Journal/Newspaper |
author |
Till, Jessica L. Moskowitz, Bruce Poulton, Simon W. |
spellingShingle |
Till, Jessica L. Moskowitz, Bruce Poulton, Simon W. Magnetic Properties of Plant Ashes and Their Influence on Magnetic Signatures of Fire in Soils |
author_facet |
Till, Jessica L. Moskowitz, Bruce Poulton, Simon W. |
author_sort |
Till, Jessica L. |
title |
Magnetic Properties of Plant Ashes and Their Influence on Magnetic Signatures of Fire in Soils |
title_short |
Magnetic Properties of Plant Ashes and Their Influence on Magnetic Signatures of Fire in Soils |
title_full |
Magnetic Properties of Plant Ashes and Their Influence on Magnetic Signatures of Fire in Soils |
title_fullStr |
Magnetic Properties of Plant Ashes and Their Influence on Magnetic Signatures of Fire in Soils |
title_full_unstemmed |
Magnetic Properties of Plant Ashes and Their Influence on Magnetic Signatures of Fire in Soils |
title_sort |
magnetic properties of plant ashes and their influence on magnetic signatures of fire in soils |
publisher |
Frontiers Media SA |
publishDate |
2021 |
url |
http://dx.doi.org/10.3389/feart.2020.592659 https://www.frontiersin.org/articles/10.3389/feart.2020.592659/full |
genre |
Iceland |
genre_facet |
Iceland |
op_source |
Frontiers in Earth Science volume 8 ISSN 2296-6463 |
op_rights |
https://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.3389/feart.2020.592659 |
container_title |
Frontiers in Earth Science |
container_volume |
8 |
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1810452210070323200 |