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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Frontiers Media S.A.
2021-01-01
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| Series: | Frontiers in Earth Science |
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| Online Access: | https://www.frontiersin.org/articles/10.3389/feart.2020.592659/full |
| _version_ | 1818573503911165952 |
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| author | Jessica L. Till Jessica L. Till Bruce Moskowitz Simon W. Poulton |
| author_facet | Jessica L. Till Jessica L. Till Bruce Moskowitz Simon W. Poulton |
| author_sort | Jessica L. Till |
| collection | DOAJ |
| description | 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. |
| first_indexed | 2024-12-15T00:12:13Z |
| format | Article |
| id | doaj.art-f71d24b2bf934f0b91b1dcd21f6e1f03 |
| institution | Directory Open Access Journal |
| issn | 2296-6463 |
| language | English |
| last_indexed | 2024-12-15T00:12:13Z |
| publishDate | 2021-01-01 |
| publisher | Frontiers Media S.A. |
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| series | Frontiers in Earth Science |
| spelling | doaj.art-f71d24b2bf934f0b91b1dcd21f6e1f032022-12-21T22:42:33ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632021-01-01810.3389/feart.2020.592659592659Magnetic Properties of Plant Ashes and Their Influence on Magnetic Signatures of Fire in SoilsJessica L. Till0Jessica L. Till1Bruce Moskowitz2Simon W. Poulton3Institute of Earth Sciences and Institute of Life and Environmental Sciences, University of Iceland, Reykjavik, IcelandInstitute for Rock Magnetism, University of Minnesota, Minneapolis, MN, United StatesInstitute for Rock Magnetism, University of Minnesota, Minneapolis, MN, United StatesSchool of Earth and Environment, University of Leeds, Leeds, United KingdomFires 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.https://www.frontiersin.org/articles/10.3389/feart.2020.592659/fullsoilsrock magnetismvegetationsoil magnetismfire |
| spellingShingle | Jessica L. Till Jessica L. Till Bruce Moskowitz Simon W. Poulton Magnetic Properties of Plant Ashes and Their Influence on Magnetic Signatures of Fire in Soils Frontiers in Earth Science soils rock magnetism vegetation soil magnetism fire |
| title | 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_short | 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 |
| topic | soils rock magnetism vegetation soil magnetism fire |
| url | https://www.frontiersin.org/articles/10.3389/feart.2020.592659/full |
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