Journal article 366 views 76 downloads
Best practice for upscaling soil organic carbon stocks in salt marshes
Geoderma, Volume: 428, Start page: 116188
Swansea University Author: Cai Ladd
-
PDF | Version of Record
Distributed under the terms of a Creative Commons Attribution 4.0 License (CC BY 4.0).
Download (13.93MB)
DOI (Published version): 10.1016/j.geoderma.2022.116188
Abstract
Calculating the amount of soil organic carbon (SOC) stored in coastal environments, including salt marshes, is needed to determine their role in mitigating the Climate Crisis. Several techniques exist to calculate the SOC content of a unit of land from the upscaling of soil cores. However, no compre...
Published in: | Geoderma |
---|---|
ISSN: | 0016-7061 |
Published: |
Elsevier BV
2022
|
Online Access: |
Check full text
|
URI: | https://cronfa.swan.ac.uk/Record/cronfa64484 |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
first_indexed |
2023-10-05T09:59:22Z |
---|---|
last_indexed |
2023-10-05T09:59:22Z |
id |
cronfa64484 |
recordtype |
SURis |
fullrecord |
<?xml version="1.0" encoding="utf-8"?><rfc1807 xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:xsd="http://www.w3.org/2001/XMLSchema"><bib-version>v2</bib-version><id>64484</id><entry>2023-09-08</entry><title>Best practice for upscaling soil organic carbon stocks in salt marshes</title><swanseaauthors><author><sid>134c870190db4c365e2ccc2d6c107462</sid><ORCID>0000-0001-5437-6474</ORCID><firstname>Cai</firstname><surname>Ladd</surname><name>Cai Ladd</name><active>true</active><ethesisStudent>false</ethesisStudent></author></swanseaauthors><date>2023-09-08</date><deptcode>SGE</deptcode><abstract>Calculating the amount of soil organic carbon (SOC) stored in coastal environments, including salt marshes, is needed to determine their role in mitigating the Climate Crisis. Several techniques exist to calculate the SOC content of a unit of land from the upscaling of soil cores. However, no comprehensive assessment has been made on the performance of commonly used SOC upscaling techniques until now. We measured the SOC content of soil cores gathered from two Scottish salt marshes. Two SOC values were used for upscaling; SOC content for a 1 m standardised depth (as recommended by the IPCC), and SOC content of the modern marsh deposit (identified in the stratigraphy as a transition from organic-rich (marsh) to mineral-rich (intertidal flat) soil. Twenty-two upscaling techniques were used (SOC content × area, interpolative, and regression-based extrapolative calculations). Leave-one-out cross-validation procedures and prediction interval widths were used to assess the accuracy of each technique. Digital Terrain Models and Normalized Difference Vegetation Indices were used as covariate surfaces in the regression models. We found that marsh-scale SOC stocks varied by as much as fifty-two times depending on which sampling depth and upscaling technique was used. The largest differences emerged when comparing SOC stocks upscaled from 1 m deep and modern marsh deposits. Using the IPCC recommended 1 m sampling depth inflated the SOC stocks of salt marshes, as intertidal flat environments were included in the calculation. Ensemble regression models from the weighted average of seven machine learning algorithm outputs produced the highest upscaling accuracies across marshes and sampling depths. Simple SOC content × area calculations produced marsh-scale SOC stocks that were comparable to stock values produced by more advanced ensemble regression models. However, regression models produced detailed maps of SOC distribution across a marsh, and the associated uncertainty in the SOC values. Our findings are broadly applicable for other environments where large-scale SOC stock assessments and uncertainty are needed.</abstract><type>Journal Article</type><journal>Geoderma</journal><volume>428</volume><journalNumber/><paginationStart>116188</paginationStart><paginationEnd/><publisher>Elsevier BV</publisher><placeOfPublication/><isbnPrint/><isbnElectronic/><issnPrint>0016-7061</issnPrint><issnElectronic/><keywords>Soil organic carbon, Salt marshes, Geostatistics, Upscaling, Soil coring, Pedometric mapping</keywords><publishedDay>15</publishedDay><publishedMonth>12</publishedMonth><publishedYear>2022</publishedYear><publishedDate>2022-12-15</publishedDate><doi>10.1016/j.geoderma.2022.116188</doi><url>http://dx.doi.org/10.1016/j.geoderma.2022.116188</url><notes/><college>COLLEGE NANME</college><department>Geography</department><CollegeCode>COLLEGE CODE</CollegeCode><DepartmentCode>SGE</DepartmentCode><institution>Swansea University</institution><apcterm>Another institution paid the OA fee</apcterm><funders/><projectreference/><lastEdited>2023-10-16T14:09:07.9727326</lastEdited><Created>2023-09-08T11:44:05.4050320</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>Cai</firstname><surname>Ladd</surname><orcid>0000-0001-5437-6474</orcid><order>1</order></author><author><firstname>Craig</firstname><surname>Smeaton</surname><orcid>0000-0003-4535-2555</orcid><order>2</order></author><author><firstname>Martin W.</firstname><surname>Skov</surname><orcid>0000-0002-7204-3865</orcid><order>3</order></author><author><firstname>William E.N.</firstname><surname>Austin</surname><order>4</order></author></authors><documents><document><filename>64484__28712__2c3a7a7b11ea4235aad0ba83bd24c931.pdf</filename><originalFilename>64484.VOR.pdf</originalFilename><uploaded>2023-10-05T11:03:47.8573931</uploaded><type>Output</type><contentLength>14607296</contentLength><contentType>application/pdf</contentType><version>Version of Record</version><cronfaStatus>true</cronfaStatus><documentNotes>Distributed under the terms of a Creative Commons Attribution 4.0 License (CC BY 4.0).</documentNotes><copyrightCorrect>true</copyrightCorrect><language>eng</language><licence>https://creativecommons.org/licenses/by/4.0/</licence></document></documents><OutputDurs/></rfc1807> |
spelling |
v2 64484 2023-09-08 Best practice for upscaling soil organic carbon stocks in salt marshes 134c870190db4c365e2ccc2d6c107462 0000-0001-5437-6474 Cai Ladd Cai Ladd true false 2023-09-08 SGE Calculating the amount of soil organic carbon (SOC) stored in coastal environments, including salt marshes, is needed to determine their role in mitigating the Climate Crisis. Several techniques exist to calculate the SOC content of a unit of land from the upscaling of soil cores. However, no comprehensive assessment has been made on the performance of commonly used SOC upscaling techniques until now. We measured the SOC content of soil cores gathered from two Scottish salt marshes. Two SOC values were used for upscaling; SOC content for a 1 m standardised depth (as recommended by the IPCC), and SOC content of the modern marsh deposit (identified in the stratigraphy as a transition from organic-rich (marsh) to mineral-rich (intertidal flat) soil. Twenty-two upscaling techniques were used (SOC content × area, interpolative, and regression-based extrapolative calculations). Leave-one-out cross-validation procedures and prediction interval widths were used to assess the accuracy of each technique. Digital Terrain Models and Normalized Difference Vegetation Indices were used as covariate surfaces in the regression models. We found that marsh-scale SOC stocks varied by as much as fifty-two times depending on which sampling depth and upscaling technique was used. The largest differences emerged when comparing SOC stocks upscaled from 1 m deep and modern marsh deposits. Using the IPCC recommended 1 m sampling depth inflated the SOC stocks of salt marshes, as intertidal flat environments were included in the calculation. Ensemble regression models from the weighted average of seven machine learning algorithm outputs produced the highest upscaling accuracies across marshes and sampling depths. Simple SOC content × area calculations produced marsh-scale SOC stocks that were comparable to stock values produced by more advanced ensemble regression models. However, regression models produced detailed maps of SOC distribution across a marsh, and the associated uncertainty in the SOC values. Our findings are broadly applicable for other environments where large-scale SOC stock assessments and uncertainty are needed. Journal Article Geoderma 428 116188 Elsevier BV 0016-7061 Soil organic carbon, Salt marshes, Geostatistics, Upscaling, Soil coring, Pedometric mapping 15 12 2022 2022-12-15 10.1016/j.geoderma.2022.116188 http://dx.doi.org/10.1016/j.geoderma.2022.116188 COLLEGE NANME Geography COLLEGE CODE SGE Swansea University Another institution paid the OA fee 2023-10-16T14:09:07.9727326 2023-09-08T11:44:05.4050320 Faculty of Science and Engineering School of Biosciences, Geography and Physics - Geography Cai Ladd 0000-0001-5437-6474 1 Craig Smeaton 0000-0003-4535-2555 2 Martin W. Skov 0000-0002-7204-3865 3 William E.N. Austin 4 64484__28712__2c3a7a7b11ea4235aad0ba83bd24c931.pdf 64484.VOR.pdf 2023-10-05T11:03:47.8573931 Output 14607296 application/pdf Version of Record true Distributed under the terms of a Creative Commons Attribution 4.0 License (CC BY 4.0). true eng https://creativecommons.org/licenses/by/4.0/ |
title |
Best practice for upscaling soil organic carbon stocks in salt marshes |
spellingShingle |
Best practice for upscaling soil organic carbon stocks in salt marshes Cai Ladd |
title_short |
Best practice for upscaling soil organic carbon stocks in salt marshes |
title_full |
Best practice for upscaling soil organic carbon stocks in salt marshes |
title_fullStr |
Best practice for upscaling soil organic carbon stocks in salt marshes |
title_full_unstemmed |
Best practice for upscaling soil organic carbon stocks in salt marshes |
title_sort |
Best practice for upscaling soil organic carbon stocks in salt marshes |
author_id_str_mv |
134c870190db4c365e2ccc2d6c107462 |
author_id_fullname_str_mv |
134c870190db4c365e2ccc2d6c107462_***_Cai Ladd |
author |
Cai Ladd |
author2 |
Cai Ladd Craig Smeaton Martin W. Skov William E.N. Austin |
format |
Journal article |
container_title |
Geoderma |
container_volume |
428 |
container_start_page |
116188 |
publishDate |
2022 |
institution |
Swansea University |
issn |
0016-7061 |
doi_str_mv |
10.1016/j.geoderma.2022.116188 |
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.geoderma.2022.116188 |
document_store_str |
1 |
active_str |
0 |
description |
Calculating the amount of soil organic carbon (SOC) stored in coastal environments, including salt marshes, is needed to determine their role in mitigating the Climate Crisis. Several techniques exist to calculate the SOC content of a unit of land from the upscaling of soil cores. However, no comprehensive assessment has been made on the performance of commonly used SOC upscaling techniques until now. We measured the SOC content of soil cores gathered from two Scottish salt marshes. Two SOC values were used for upscaling; SOC content for a 1 m standardised depth (as recommended by the IPCC), and SOC content of the modern marsh deposit (identified in the stratigraphy as a transition from organic-rich (marsh) to mineral-rich (intertidal flat) soil. Twenty-two upscaling techniques were used (SOC content × area, interpolative, and regression-based extrapolative calculations). Leave-one-out cross-validation procedures and prediction interval widths were used to assess the accuracy of each technique. Digital Terrain Models and Normalized Difference Vegetation Indices were used as covariate surfaces in the regression models. We found that marsh-scale SOC stocks varied by as much as fifty-two times depending on which sampling depth and upscaling technique was used. The largest differences emerged when comparing SOC stocks upscaled from 1 m deep and modern marsh deposits. Using the IPCC recommended 1 m sampling depth inflated the SOC stocks of salt marshes, as intertidal flat environments were included in the calculation. Ensemble regression models from the weighted average of seven machine learning algorithm outputs produced the highest upscaling accuracies across marshes and sampling depths. Simple SOC content × area calculations produced marsh-scale SOC stocks that were comparable to stock values produced by more advanced ensemble regression models. However, regression models produced detailed maps of SOC distribution across a marsh, and the associated uncertainty in the SOC values. Our findings are broadly applicable for other environments where large-scale SOC stock assessments and uncertainty are needed. |
published_date |
2022-12-15T14:09:09Z |
_version_ |
1779917651524452352 |
score |
11.035634 |