Glacially abraded rock flour from Greenland: Potential for macronutrient supply to plants

Abstract Rock flour (RF) is a fine‐grained material produced naturally by glacial movement and resulting bedrock abrasion. In Greenland fluvial transported RF from the inland ice sheet sediments in riverbeds and marine outflows. This fine‐sized RF (50% < 9.8 µm) has a high reactivity and may ther...

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Published in:Journal of Plant Nutrition and Soil Science
Main Authors: Gunnarsen, Klara Cecilia, Jensen, Lars Stoumann, Gómez-Muñoz, Beatriz, Rosing, Minik Thorleif, de Neergaard, Andreas
Other Authors: Novo Nordisk UK Research Foundation
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2019
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Online Access:http://dx.doi.org/10.1002/jpln.201800647
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spelling crwiley:10.1002/jpln.201800647 2024-09-15T18:09:00+00:00 Glacially abraded rock flour from Greenland: Potential for macronutrient supply to plants Gunnarsen, Klara Cecilia Jensen, Lars Stoumann Gómez-Muñoz, Beatriz Rosing, Minik Thorleif de Neergaard, Andreas Novo Nordisk UK Research Foundation 2019 http://dx.doi.org/10.1002/jpln.201800647 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjpln.201800647 https://onlinelibrary.wiley.com/doi/pdf/10.1002/jpln.201800647 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/jpln.201800647 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Journal of Plant Nutrition and Soil Science volume 182, issue 5, page 846-856 ISSN 1436-8730 1522-2624 journal-article 2019 crwiley https://doi.org/10.1002/jpln.201800647 2024-08-30T04:11:32Z Abstract Rock flour (RF) is a fine‐grained material produced naturally by glacial movement and resulting bedrock abrasion. In Greenland fluvial transported RF from the inland ice sheet sediments in riverbeds and marine outflows. This fine‐sized RF (50% < 9.8 µm) has a high reactivity and may therefore potentially be used to rejuvenate nutrient poor soils and provide nutrients to plants. The aim of this study was to evaluate the ability of a RF from Greenland to supply P, K, Mg, and S to plants. A double‐pot system was used, in which ryegrass ( Lolium perenne L .) could take up nutrients from both a hydroponic solution and a soil‐compartment with or without RF amendment; a soil mixture or pure sand was used in the soil‐compartment to estimate RF‐soil interaction effects. Omission of single nutrients from the hydroponic solution allowed assessment of which nutrients the RF in the soil‐compartment was able to supply. Ryegrass biomass was harvested four times during 62 days. We found that RF could supply K continuously to plants grown in soil or sand, but insufficient to fully circumvent K deficiency. During 62 days 5.8% and 4.3% of the applied K from RF was accumulated in the aboveground plant tissue in soil and sand, respectively. Mg was supplied from RF to plants in sand, but no significant effects were observed in soil, possibly due to background soil Mg availability. The amounts of P and S supplied to plants were insignificant. These results indicate the potential of Greenland RF to act as a slow release K and Mg fertilizer. Article in Journal/Newspaper Greenland Ice Sheet Wiley Online Library Journal of Plant Nutrition and Soil Science 182 5 846 856
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description Abstract Rock flour (RF) is a fine‐grained material produced naturally by glacial movement and resulting bedrock abrasion. In Greenland fluvial transported RF from the inland ice sheet sediments in riverbeds and marine outflows. This fine‐sized RF (50% < 9.8 µm) has a high reactivity and may therefore potentially be used to rejuvenate nutrient poor soils and provide nutrients to plants. The aim of this study was to evaluate the ability of a RF from Greenland to supply P, K, Mg, and S to plants. A double‐pot system was used, in which ryegrass ( Lolium perenne L .) could take up nutrients from both a hydroponic solution and a soil‐compartment with or without RF amendment; a soil mixture or pure sand was used in the soil‐compartment to estimate RF‐soil interaction effects. Omission of single nutrients from the hydroponic solution allowed assessment of which nutrients the RF in the soil‐compartment was able to supply. Ryegrass biomass was harvested four times during 62 days. We found that RF could supply K continuously to plants grown in soil or sand, but insufficient to fully circumvent K deficiency. During 62 days 5.8% and 4.3% of the applied K from RF was accumulated in the aboveground plant tissue in soil and sand, respectively. Mg was supplied from RF to plants in sand, but no significant effects were observed in soil, possibly due to background soil Mg availability. The amounts of P and S supplied to plants were insignificant. These results indicate the potential of Greenland RF to act as a slow release K and Mg fertilizer.
author2 Novo Nordisk UK Research Foundation
format Article in Journal/Newspaper
author Gunnarsen, Klara Cecilia
Jensen, Lars Stoumann
Gómez-Muñoz, Beatriz
Rosing, Minik Thorleif
de Neergaard, Andreas
spellingShingle Gunnarsen, Klara Cecilia
Jensen, Lars Stoumann
Gómez-Muñoz, Beatriz
Rosing, Minik Thorleif
de Neergaard, Andreas
Glacially abraded rock flour from Greenland: Potential for macronutrient supply to plants
author_facet Gunnarsen, Klara Cecilia
Jensen, Lars Stoumann
Gómez-Muñoz, Beatriz
Rosing, Minik Thorleif
de Neergaard, Andreas
author_sort Gunnarsen, Klara Cecilia
title Glacially abraded rock flour from Greenland: Potential for macronutrient supply to plants
title_short Glacially abraded rock flour from Greenland: Potential for macronutrient supply to plants
title_full Glacially abraded rock flour from Greenland: Potential for macronutrient supply to plants
title_fullStr Glacially abraded rock flour from Greenland: Potential for macronutrient supply to plants
title_full_unstemmed Glacially abraded rock flour from Greenland: Potential for macronutrient supply to plants
title_sort glacially abraded rock flour from greenland: potential for macronutrient supply to plants
publisher Wiley
publishDate 2019
url http://dx.doi.org/10.1002/jpln.201800647
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https://onlinelibrary.wiley.com/doi/full-xml/10.1002/jpln.201800647
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op_source Journal of Plant Nutrition and Soil Science
volume 182, issue 5, page 846-856
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