Reconstructing historic bog iron ore deposits in the Bourtangermoor, a former raised bog in the Netherlands

Bog iron ores are well-known lumps of Fe-(oxy)hydroxides (goethite, limonite) found along streams and in seasonally flooded, low-lying areas. Historic literature of the Bourtangermoor, a former raised bog in the north of the Netherlands and adjacent Germany, however, revealed a second, rare type of bog iron ores, exclusively composed of siderite (Fe-carbonate) with accessory vivianite (Fe-phosphate), minerals only stable under anaerobic conditions. In this research we compared historic literature and maps mainly from the first half of the 20th century, when parts of the bog were still intact, with present-day seepage data to allow analysis whether recent seepage could be used to reconstruct the location of historic bog iron ores in the Bourtangermoor. Our results showed two distinctly different present-day seepage patterns: one related to shallow aquifers, one to deeper aquifers. Present-day seepage from deeper aquifers was related to historic siderite bog iron ore deposits (deposits exclusively limited to the lower, early formed, still groundwater-fed part of the raised bog). Present-day seepage – deep or shallow – did not show a clear relation to historic classic-type bog iron ores (lumps of goethite and limonite). We conclude that present-day seepage patterns from deep aquifers can be used to reconstruct historic siderite bog iron ores in the Bourtangermoor. Present-day seepage patterns – deep or shallow – are however not representative for historic bog iron ores deposited along streams. Our results could be useful for wetland restoration projects as iron can contribute to nutrient-poor conditions by capturing phosphate in bog iron ores and for archaeological research regarding the potential use of bog iron ores by past societies.

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Main Authors: Nauta, Aukjen A., Dijksma, Roel, Candel, Jasper H.J., Stoof, Cathelijne R.
Format: Article/Letter to editor biblioteca
Language:English
Subjects:Bog iron ores, Historic data, Raised bog, Seepage, Siderite,
Online Access:https://research.wur.nl/en/publications/reconstructing-historic-bog-iron-ore-deposits-in-the-bourtangermo
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spelling dig-wur-nl-wurpubs-6280642025-01-14 Nauta, Aukjen A. Dijksma, Roel Candel, Jasper H.J. Stoof, Cathelijne R. Article/Letter to editor Catena 239 (2024) ISSN: 0341-8162 Reconstructing historic bog iron ore deposits in the Bourtangermoor, a former raised bog in the Netherlands 2024 Bog iron ores are well-known lumps of Fe-(oxy)hydroxides (goethite, limonite) found along streams and in seasonally flooded, low-lying areas. Historic literature of the Bourtangermoor, a former raised bog in the north of the Netherlands and adjacent Germany, however, revealed a second, rare type of bog iron ores, exclusively composed of siderite (Fe-carbonate) with accessory vivianite (Fe-phosphate), minerals only stable under anaerobic conditions. In this research we compared historic literature and maps mainly from the first half of the 20th century, when parts of the bog were still intact, with present-day seepage data to allow analysis whether recent seepage could be used to reconstruct the location of historic bog iron ores in the Bourtangermoor. Our results showed two distinctly different present-day seepage patterns: one related to shallow aquifers, one to deeper aquifers. Present-day seepage from deeper aquifers was related to historic siderite bog iron ore deposits (deposits exclusively limited to the lower, early formed, still groundwater-fed part of the raised bog). Present-day seepage – deep or shallow – did not show a clear relation to historic classic-type bog iron ores (lumps of goethite and limonite). We conclude that present-day seepage patterns from deep aquifers can be used to reconstruct historic siderite bog iron ores in the Bourtangermoor. Present-day seepage patterns – deep or shallow – are however not representative for historic bog iron ores deposited along streams. Our results could be useful for wetland restoration projects as iron can contribute to nutrient-poor conditions by capturing phosphate in bog iron ores and for archaeological research regarding the potential use of bog iron ores by past societies. en application/pdf https://research.wur.nl/en/publications/reconstructing-historic-bog-iron-ore-deposits-in-the-bourtangermo 10.1016/j.catena.2024.107847 https://edepot.wur.nl/652800 Bog iron ores Historic data Raised bog Seepage Siderite https://creativecommons.org/licenses/by/4.0/ https://creativecommons.org/licenses/by/4.0/ Wageningen University & Research
institution WUR NL
collection DSpace
country Países bajos
countrycode NL
component Bibliográfico
access En linea
databasecode dig-wur-nl
tag biblioteca
region Europa del Oeste
libraryname WUR Library Netherlands
language English
topic Bog iron ores
Historic data
Raised bog
Seepage
Siderite
Bog iron ores
Historic data
Raised bog
Seepage
Siderite
spellingShingle Bog iron ores
Historic data
Raised bog
Seepage
Siderite
Bog iron ores
Historic data
Raised bog
Seepage
Siderite
Nauta, Aukjen A.
Dijksma, Roel
Candel, Jasper H.J.
Stoof, Cathelijne R.
Reconstructing historic bog iron ore deposits in the Bourtangermoor, a former raised bog in the Netherlands
description Bog iron ores are well-known lumps of Fe-(oxy)hydroxides (goethite, limonite) found along streams and in seasonally flooded, low-lying areas. Historic literature of the Bourtangermoor, a former raised bog in the north of the Netherlands and adjacent Germany, however, revealed a second, rare type of bog iron ores, exclusively composed of siderite (Fe-carbonate) with accessory vivianite (Fe-phosphate), minerals only stable under anaerobic conditions. In this research we compared historic literature and maps mainly from the first half of the 20th century, when parts of the bog were still intact, with present-day seepage data to allow analysis whether recent seepage could be used to reconstruct the location of historic bog iron ores in the Bourtangermoor. Our results showed two distinctly different present-day seepage patterns: one related to shallow aquifers, one to deeper aquifers. Present-day seepage from deeper aquifers was related to historic siderite bog iron ore deposits (deposits exclusively limited to the lower, early formed, still groundwater-fed part of the raised bog). Present-day seepage – deep or shallow – did not show a clear relation to historic classic-type bog iron ores (lumps of goethite and limonite). We conclude that present-day seepage patterns from deep aquifers can be used to reconstruct historic siderite bog iron ores in the Bourtangermoor. Present-day seepage patterns – deep or shallow – are however not representative for historic bog iron ores deposited along streams. Our results could be useful for wetland restoration projects as iron can contribute to nutrient-poor conditions by capturing phosphate in bog iron ores and for archaeological research regarding the potential use of bog iron ores by past societies.
format Article/Letter to editor
topic_facet Bog iron ores
Historic data
Raised bog
Seepage
Siderite
author Nauta, Aukjen A.
Dijksma, Roel
Candel, Jasper H.J.
Stoof, Cathelijne R.
author_facet Nauta, Aukjen A.
Dijksma, Roel
Candel, Jasper H.J.
Stoof, Cathelijne R.
author_sort Nauta, Aukjen A.
title Reconstructing historic bog iron ore deposits in the Bourtangermoor, a former raised bog in the Netherlands
title_short Reconstructing historic bog iron ore deposits in the Bourtangermoor, a former raised bog in the Netherlands
title_full Reconstructing historic bog iron ore deposits in the Bourtangermoor, a former raised bog in the Netherlands
title_fullStr Reconstructing historic bog iron ore deposits in the Bourtangermoor, a former raised bog in the Netherlands
title_full_unstemmed Reconstructing historic bog iron ore deposits in the Bourtangermoor, a former raised bog in the Netherlands
title_sort reconstructing historic bog iron ore deposits in the bourtangermoor, a former raised bog in the netherlands
url https://research.wur.nl/en/publications/reconstructing-historic-bog-iron-ore-deposits-in-the-bourtangermo
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