Journal article 576 views 62 downloads
Soil erosion after fire in volcanic terrain: assessment and implications for post-fire soil losses
Journal of Hydrology, Volume: 625, Issue: A, Start page: 129923
Swansea University Authors: Jonay Neris Tome, Stefan Doerr
-
PDF | Version of Record
© 2023 The Author(s). Published by Elsevier B.V. Distributed under the terms of a Creative Commons Attribution 4.0 License (CC BY 4.0).
Download (4.38MB)
DOI (Published version): 10.1016/j.jhydrol.2023.129923
Abstract
Wildfires can dramatically modify the hydrologic and erosion response of ecosystems, increasing risks to population and assets downslope of fire affected hillslopes. This applies especially to volcanic areas in fire-prone regions which often exhibit steep terrain and high population densities. Howev...
Published in: | Journal of Hydrology |
---|---|
ISSN: | 0022-1694 |
Published: |
Elsevier BV
2023
|
Online Access: |
Check full text
|
URI: | https://cronfa.swan.ac.uk/Record/cronfa63914 |
first_indexed |
2023-07-19T10:46:55Z |
---|---|
last_indexed |
2024-11-25T14:13:06Z |
id |
cronfa63914 |
recordtype |
SURis |
fullrecord |
<?xml version="1.0"?><rfc1807><datestamp>2023-08-22T15:09:41.6261582</datestamp><bib-version>v2</bib-version><id>63914</id><entry>2023-07-19</entry><title>Soil erosion after fire in volcanic terrain: assessment and implications for post-fire soil losses</title><swanseaauthors><author><sid>bc8475d9297bd8441f68d13a94585ce1</sid><firstname>Jonay</firstname><surname>Neris Tome</surname><name>Jonay Neris Tome</name><active>true</active><ethesisStudent>false</ethesisStudent></author><author><sid>575eb5094f2328249328b3e43deb5088</sid><ORCID>0000-0002-8700-9002</ORCID><firstname>Stefan</firstname><surname>Doerr</surname><name>Stefan Doerr</name><active>true</active><ethesisStudent>false</ethesisStudent></author></swanseaauthors><date>2023-07-19</date><abstract>Wildfires can dramatically modify the hydrologic and erosion response of ecosystems, increasing risks to population and assets downslope of fire affected hillslopes. This applies especially to volcanic areas in fire-prone regions which often exhibit steep terrain and high population densities. However, the effects of fire on key hydrologic and erosion parameters, which are critical for modelling runoff-erosion processes, predicting related post-fire risks and for selecting effective mitigation measures, have not been extensively assessed in this terrain type. Here we evaluate water erosion processes of two contrasting volcanic soils in recently burned forest areas of Tenerife (Canary Islands, Spain) at hillslope scale using erosion plots monitoring and rill erosion simulation experiments. The results show that both the lithology and the degree of weathering of the volcanic material govern the post-fire water erosion by concentrated flow (rill erosion experiments) and by the combination of interrill and rill erosion (erosion plots). Mature volcanic soils showed less susceptibility to erosion than weakly weathered volcanic soils and soils with non-volcanic lithologies. The results also show that the availability of easily detachable and transportable soil particles swiftly decreases after the fire, leading to the exhaustion of sediments and a decrease of the erosion rates with cumulative runoff events. These findings have direct implications for the modelling of runoff-erosion processes in volcanic terrain.</abstract><type>Journal Article</type><journal>Journal of Hydrology</journal><volume>625</volume><journalNumber>A</journalNumber><paginationStart>129923</paginationStart><paginationEnd/><publisher>Elsevier BV</publisher><placeOfPublication/><isbnPrint/><isbnElectronic/><issnPrint>0022-1694</issnPrint><issnElectronic/><keywords>Wildfire, Runoff-erosion processes, Rill erosion, Sediment exhaustion, Andisols, Post-fire management</keywords><publishedDay>1</publishedDay><publishedMonth>10</publishedMonth><publishedYear>2023</publishedYear><publishedDate>2023-10-01</publishedDate><doi>10.1016/j.jhydrol.2023.129923</doi><url>http://dx.doi.org/10.1016/j.jhydrol.2023.129923</url><notes/><college>COLLEGE NANME</college><CollegeCode>COLLEGE CODE</CollegeCode><institution>Swansea University</institution><apcterm/><funders>During manuscript preparation J Neris and SH Doerr were supported by a Natural Environment Research Council grant (NE/R011125/1). J Neris, was also supported by a H2020 Marie Skłodowska‐Curie Individual Fellowship (655993) and SH Doerr was supported by a European Union Horizon 2020 research and innovation programme grant (FirEUrisk; 101003890.</funders><projectreference/><lastEdited>2023-08-22T15:09:41.6261582</lastEdited><Created>2023-07-19T11:44:04.0487867</Created><path><level id="1">Faculty of Science and Engineering</level><level id="2">School of Biosciences, Geography and Physics - Geography</level></path><authors><author><firstname>Jonay</firstname><surname>Neris Tome</surname><order>1</order></author><author><firstname>P.R.</firstname><surname>Robichaud</surname><orcid>0000-0002-2902-2401</orcid><order>2</order></author><author><firstname>J.W.</firstname><surname>Wagenbrenner</surname><orcid>0000-0003-3317-5141</orcid><order>3</order></author><author><firstname>R.E.</firstname><surname>Brown</surname><order>4</order></author><author><firstname>Stefan</firstname><surname>Doerr</surname><orcid>0000-0002-8700-9002</orcid><order>5</order></author></authors><documents><document><filename>63914__28196__6b869cfad74444cfbb31660e05d1127f.pdf</filename><originalFilename>63914.pdf</originalFilename><uploaded>2023-07-27T08:56:27.9718544</uploaded><type>Output</type><contentLength>4588810</contentLength><contentType>application/pdf</contentType><version>Version of Record</version><cronfaStatus>true</cronfaStatus><documentNotes>© 2023 The Author(s). Published by Elsevier B.V. Distributed under the terms of a Creative Commons Attribution 4.0 License (CC BY 4.0).</documentNotes><copyrightCorrect>true</copyrightCorrect><language>eng</language><licence>http://creativecommons.org/licenses/by/4.0/</licence></document></documents><OutputDurs/></rfc1807> |
spelling |
2023-08-22T15:09:41.6261582 v2 63914 2023-07-19 Soil erosion after fire in volcanic terrain: assessment and implications for post-fire soil losses bc8475d9297bd8441f68d13a94585ce1 Jonay Neris Tome Jonay Neris Tome true false 575eb5094f2328249328b3e43deb5088 0000-0002-8700-9002 Stefan Doerr Stefan Doerr true false 2023-07-19 Wildfires can dramatically modify the hydrologic and erosion response of ecosystems, increasing risks to population and assets downslope of fire affected hillslopes. This applies especially to volcanic areas in fire-prone regions which often exhibit steep terrain and high population densities. However, the effects of fire on key hydrologic and erosion parameters, which are critical for modelling runoff-erosion processes, predicting related post-fire risks and for selecting effective mitigation measures, have not been extensively assessed in this terrain type. Here we evaluate water erosion processes of two contrasting volcanic soils in recently burned forest areas of Tenerife (Canary Islands, Spain) at hillslope scale using erosion plots monitoring and rill erosion simulation experiments. The results show that both the lithology and the degree of weathering of the volcanic material govern the post-fire water erosion by concentrated flow (rill erosion experiments) and by the combination of interrill and rill erosion (erosion plots). Mature volcanic soils showed less susceptibility to erosion than weakly weathered volcanic soils and soils with non-volcanic lithologies. The results also show that the availability of easily detachable and transportable soil particles swiftly decreases after the fire, leading to the exhaustion of sediments and a decrease of the erosion rates with cumulative runoff events. These findings have direct implications for the modelling of runoff-erosion processes in volcanic terrain. Journal Article Journal of Hydrology 625 A 129923 Elsevier BV 0022-1694 Wildfire, Runoff-erosion processes, Rill erosion, Sediment exhaustion, Andisols, Post-fire management 1 10 2023 2023-10-01 10.1016/j.jhydrol.2023.129923 http://dx.doi.org/10.1016/j.jhydrol.2023.129923 COLLEGE NANME COLLEGE CODE Swansea University During manuscript preparation J Neris and SH Doerr were supported by a Natural Environment Research Council grant (NE/R011125/1). J Neris, was also supported by a H2020 Marie Skłodowska‐Curie Individual Fellowship (655993) and SH Doerr was supported by a European Union Horizon 2020 research and innovation programme grant (FirEUrisk; 101003890. 2023-08-22T15:09:41.6261582 2023-07-19T11:44:04.0487867 Faculty of Science and Engineering School of Biosciences, Geography and Physics - Geography Jonay Neris Tome 1 P.R. Robichaud 0000-0002-2902-2401 2 J.W. Wagenbrenner 0000-0003-3317-5141 3 R.E. Brown 4 Stefan Doerr 0000-0002-8700-9002 5 63914__28196__6b869cfad74444cfbb31660e05d1127f.pdf 63914.pdf 2023-07-27T08:56:27.9718544 Output 4588810 application/pdf Version of Record true © 2023 The Author(s). Published by Elsevier B.V. Distributed under the terms of a Creative Commons Attribution 4.0 License (CC BY 4.0). true eng http://creativecommons.org/licenses/by/4.0/ |
title |
Soil erosion after fire in volcanic terrain: assessment and implications for post-fire soil losses |
spellingShingle |
Soil erosion after fire in volcanic terrain: assessment and implications for post-fire soil losses Jonay Neris Tome Stefan Doerr |
title_short |
Soil erosion after fire in volcanic terrain: assessment and implications for post-fire soil losses |
title_full |
Soil erosion after fire in volcanic terrain: assessment and implications for post-fire soil losses |
title_fullStr |
Soil erosion after fire in volcanic terrain: assessment and implications for post-fire soil losses |
title_full_unstemmed |
Soil erosion after fire in volcanic terrain: assessment and implications for post-fire soil losses |
title_sort |
Soil erosion after fire in volcanic terrain: assessment and implications for post-fire soil losses |
author_id_str_mv |
bc8475d9297bd8441f68d13a94585ce1 575eb5094f2328249328b3e43deb5088 |
author_id_fullname_str_mv |
bc8475d9297bd8441f68d13a94585ce1_***_Jonay Neris Tome 575eb5094f2328249328b3e43deb5088_***_Stefan Doerr |
author |
Jonay Neris Tome Stefan Doerr |
author2 |
Jonay Neris Tome P.R. Robichaud J.W. Wagenbrenner R.E. Brown Stefan Doerr |
format |
Journal article |
container_title |
Journal of Hydrology |
container_volume |
625 |
container_issue |
A |
container_start_page |
129923 |
publishDate |
2023 |
institution |
Swansea University |
issn |
0022-1694 |
doi_str_mv |
10.1016/j.jhydrol.2023.129923 |
publisher |
Elsevier BV |
college_str |
Faculty of Science and Engineering |
hierarchytype |
|
hierarchy_top_id |
facultyofscienceandengineering |
hierarchy_top_title |
Faculty of Science and Engineering |
hierarchy_parent_id |
facultyofscienceandengineering |
hierarchy_parent_title |
Faculty of Science and Engineering |
department_str |
School of Biosciences, Geography and Physics - Geography{{{_:::_}}}Faculty of Science and Engineering{{{_:::_}}}School of Biosciences, Geography and Physics - Geography |
url |
http://dx.doi.org/10.1016/j.jhydrol.2023.129923 |
document_store_str |
1 |
active_str |
0 |
description |
Wildfires can dramatically modify the hydrologic and erosion response of ecosystems, increasing risks to population and assets downslope of fire affected hillslopes. This applies especially to volcanic areas in fire-prone regions which often exhibit steep terrain and high population densities. However, the effects of fire on key hydrologic and erosion parameters, which are critical for modelling runoff-erosion processes, predicting related post-fire risks and for selecting effective mitigation measures, have not been extensively assessed in this terrain type. Here we evaluate water erosion processes of two contrasting volcanic soils in recently burned forest areas of Tenerife (Canary Islands, Spain) at hillslope scale using erosion plots monitoring and rill erosion simulation experiments. The results show that both the lithology and the degree of weathering of the volcanic material govern the post-fire water erosion by concentrated flow (rill erosion experiments) and by the combination of interrill and rill erosion (erosion plots). Mature volcanic soils showed less susceptibility to erosion than weakly weathered volcanic soils and soils with non-volcanic lithologies. The results also show that the availability of easily detachable and transportable soil particles swiftly decreases after the fire, leading to the exhaustion of sediments and a decrease of the erosion rates with cumulative runoff events. These findings have direct implications for the modelling of runoff-erosion processes in volcanic terrain. |
published_date |
2023-10-01T08:23:03Z |
_version_ |
1821393062052495360 |
score |
11.047718 |