The use of carbonatite rock powder as a liming agent
Abstract Carbonatite rock powder, originating from the Lillebukt Alkaline Complex at Stjernøy in northern Norway, can potentially be used as a slow‐releasing lime and potassium (K) and magnesium (Mg) fertilizer due to a high concentration of the easily weathered minerals calcite (42%) and biotite (3...
Published in: | Journal of Plant Nutrition and Soil Science |
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crwiley:10.1002/jpln.201600455 2024-06-02T08:12:06+00:00 The use of carbonatite rock powder as a liming agent Myrvang, Mona Bakke Heim, Michael Krogstad, Tore Almås, Åsgeir R. Gjengedal, Elin 2017 http://dx.doi.org/10.1002/jpln.201600455 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjpln.201600455 https://onlinelibrary.wiley.com/doi/pdf/10.1002/jpln.201600455 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/jpln.201600455 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Journal of Plant Nutrition and Soil Science volume 180, issue 3, page 326-335 ISSN 1436-8730 1522-2624 journal-article 2017 crwiley https://doi.org/10.1002/jpln.201600455 2024-05-03T11:25:23Z Abstract Carbonatite rock powder, originating from the Lillebukt Alkaline Complex at Stjernøy in northern Norway, can potentially be used as a slow‐releasing lime and potassium (K) and magnesium (Mg) fertilizer due to a high concentration of the easily weathered minerals calcite (42%) and biotite (30%). However, the enrichment of barium (Ba) and strontium (Sr) may cause an undesired uptake to plants when carbonatite is applied to agroecosystems. A pot experiment was designed to investigate the liming and fertilization effects of carbonatite and the potential mobilization of Ba and Sr compared to a dolomite lime commonly used in Norwegian agriculture. These liming agents were mixed with a sandy soil applied to different amounts of peat, and the uptake of Ba, Sr, calcium (Ca), Mg, and K by Festuca arundinácea Schreb. Kora (tall fescue) and Trifolium repens L. Milkanova (white clover) was evaluated. The liming agents were generally incapable of buffering the acidifying effect from increased applications of peat, while the plant dry mass was unaffected. Compared to pots given dolomite and soluble K, the availability of K from carbonatite to plants was equally high or higher, and no difference in the K:(Ca + Mg) ratio in plants was observed. Carbonatite was a significant source to plant Ba and Sr, and the uptake seemed to follow the Ca uptake. Addition of peat amplified the uptake of Ba, Sr, Ca, Mg, and K to plants, probably an effect of organic acid‐induced weathering of carbonatite. White clover took up Ba, Sr, and Ca more effectively than tall fescue, but the Ba and Sr concentrations in plants were relatively moderate compared to concentrations reported from field investigations. Article in Journal/Newspaper Northern Norway Wiley Online Library Lillebukt ENVELOPE(22.107,22.107,70.257,70.257) Norway Journal of Plant Nutrition and Soil Science 180 3 326 335 |
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Wiley Online Library |
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English |
description |
Abstract Carbonatite rock powder, originating from the Lillebukt Alkaline Complex at Stjernøy in northern Norway, can potentially be used as a slow‐releasing lime and potassium (K) and magnesium (Mg) fertilizer due to a high concentration of the easily weathered minerals calcite (42%) and biotite (30%). However, the enrichment of barium (Ba) and strontium (Sr) may cause an undesired uptake to plants when carbonatite is applied to agroecosystems. A pot experiment was designed to investigate the liming and fertilization effects of carbonatite and the potential mobilization of Ba and Sr compared to a dolomite lime commonly used in Norwegian agriculture. These liming agents were mixed with a sandy soil applied to different amounts of peat, and the uptake of Ba, Sr, calcium (Ca), Mg, and K by Festuca arundinácea Schreb. Kora (tall fescue) and Trifolium repens L. Milkanova (white clover) was evaluated. The liming agents were generally incapable of buffering the acidifying effect from increased applications of peat, while the plant dry mass was unaffected. Compared to pots given dolomite and soluble K, the availability of K from carbonatite to plants was equally high or higher, and no difference in the K:(Ca + Mg) ratio in plants was observed. Carbonatite was a significant source to plant Ba and Sr, and the uptake seemed to follow the Ca uptake. Addition of peat amplified the uptake of Ba, Sr, Ca, Mg, and K to plants, probably an effect of organic acid‐induced weathering of carbonatite. White clover took up Ba, Sr, and Ca more effectively than tall fescue, but the Ba and Sr concentrations in plants were relatively moderate compared to concentrations reported from field investigations. |
format |
Article in Journal/Newspaper |
author |
Myrvang, Mona Bakke Heim, Michael Krogstad, Tore Almås, Åsgeir R. Gjengedal, Elin |
spellingShingle |
Myrvang, Mona Bakke Heim, Michael Krogstad, Tore Almås, Åsgeir R. Gjengedal, Elin The use of carbonatite rock powder as a liming agent |
author_facet |
Myrvang, Mona Bakke Heim, Michael Krogstad, Tore Almås, Åsgeir R. Gjengedal, Elin |
author_sort |
Myrvang, Mona Bakke |
title |
The use of carbonatite rock powder as a liming agent |
title_short |
The use of carbonatite rock powder as a liming agent |
title_full |
The use of carbonatite rock powder as a liming agent |
title_fullStr |
The use of carbonatite rock powder as a liming agent |
title_full_unstemmed |
The use of carbonatite rock powder as a liming agent |
title_sort |
use of carbonatite rock powder as a liming agent |
publisher |
Wiley |
publishDate |
2017 |
url |
http://dx.doi.org/10.1002/jpln.201600455 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjpln.201600455 https://onlinelibrary.wiley.com/doi/pdf/10.1002/jpln.201600455 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/jpln.201600455 |
long_lat |
ENVELOPE(22.107,22.107,70.257,70.257) |
geographic |
Lillebukt Norway |
geographic_facet |
Lillebukt Norway |
genre |
Northern Norway |
genre_facet |
Northern Norway |
op_source |
Journal of Plant Nutrition and Soil Science volume 180, issue 3, page 326-335 ISSN 1436-8730 1522-2624 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/jpln.201600455 |
container_title |
Journal of Plant Nutrition and Soil Science |
container_volume |
180 |
container_issue |
3 |
container_start_page |
326 |
op_container_end_page |
335 |
_version_ |
1800758438433652736 |