Sorption properties of granulometric fractions in Haplic Cambisol developed from boulder loam
The aim of the paper was to investigate the sorption properties of granulometric fractions separated from the genetic horizons of arable Haplic Cambisol developed from boulder loams of the Middle-Polish (Riss) Glaciation, Wartanian Stadial (central Poland). Separation of granulometric fractions was...
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Soil Science Society of Poland
2019-06-01
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Series: | Soil Science Annual |
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Online Access: | http://www.degruyter.com/view/j/ssa.2019.70.issue-2/ssa-2019-0013/ssa-2019-0013.xml?format=INT |
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author | Brogowski Zygmunt Chojnicki Józef |
author_facet | Brogowski Zygmunt Chojnicki Józef |
author_sort | Brogowski Zygmunt |
collection | DOAJ |
description | The aim of the paper was to investigate the sorption properties of granulometric fractions separated from the genetic horizons of arable Haplic Cambisol developed from boulder loams of the Middle-Polish (Riss) Glaciation, Wartanian Stadial (central Poland). Separation of granulometric fractions was made with application of the Atterberg method without the use of centrifuging and dispersing agents. The cation exchange capacity average value in cmol(+)kg−1 and % contribution in particular fractions reached: 1–0.1 mm – 2.1 (1.6%), 0.1–0.05 mm – 5.5 (4.0%), 0.05–0.02 mm – 8.5 (6.1%), 0.02–0.01 mm – 13.0 (10.1%), 0.01–0.005 mm – 16.1 (12.8%), 0.005–0.002 mm – 28.6 (20.5%) and fraction <0.002 mm – 48.7 (44.9%). Leaching of the total exchangeable bases was the largest in the 0.1–0.05 mm fraction and decreased successively with decreasing grain diameter. Sorption properties of the tested soil determine its high agricultural value and buffer properties. The cation exchange capacity of the recognised granulometric fractions successively increased with decrease of their diameter while leaching process intensity in individual fractions decreased gradually as their dimensions decreased. Calcium was the most leached cation, followed by magnesium and sodium, whereas potassium was not leached at all. Significant increase of the cation exchange capacity in fractions from carbonate horizons was mostly caused by the increased contribution of calcium, which could be released from carbonates during extraction of bases. |
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language | English |
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publishDate | 2019-06-01 |
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spelling | doaj.art-ef2cd6415d974b7091fc2dc6298659202022-12-22T00:49:34ZengSoil Science Society of PolandSoil Science Annual2300-49752019-06-0170214715710.2478/ssa-2019-0013ssa-2019-0013Sorption properties of granulometric fractions in Haplic Cambisol developed from boulder loamBrogowski Zygmunt0Chojnicki Józef1Warsaw University of Life Sciences-SGGW, Faculty of Agriculture and Biology, Department of Soil Environment Sciences, 159 Nowoursynowska Str., 02-776Warszawa, PolandWarsaw University of Life Sciences-SGGW, Faculty of Agriculture and Biology, Department of Soil Environment Sciences, 159 Nowoursynowska Str., 02-776Warszawa, PolandThe aim of the paper was to investigate the sorption properties of granulometric fractions separated from the genetic horizons of arable Haplic Cambisol developed from boulder loams of the Middle-Polish (Riss) Glaciation, Wartanian Stadial (central Poland). Separation of granulometric fractions was made with application of the Atterberg method without the use of centrifuging and dispersing agents. The cation exchange capacity average value in cmol(+)kg−1 and % contribution in particular fractions reached: 1–0.1 mm – 2.1 (1.6%), 0.1–0.05 mm – 5.5 (4.0%), 0.05–0.02 mm – 8.5 (6.1%), 0.02–0.01 mm – 13.0 (10.1%), 0.01–0.005 mm – 16.1 (12.8%), 0.005–0.002 mm – 28.6 (20.5%) and fraction <0.002 mm – 48.7 (44.9%). Leaching of the total exchangeable bases was the largest in the 0.1–0.05 mm fraction and decreased successively with decreasing grain diameter. Sorption properties of the tested soil determine its high agricultural value and buffer properties. The cation exchange capacity of the recognised granulometric fractions successively increased with decrease of their diameter while leaching process intensity in individual fractions decreased gradually as their dimensions decreased. Calcium was the most leached cation, followed by magnesium and sodium, whereas potassium was not leached at all. Significant increase of the cation exchange capacity in fractions from carbonate horizons was mostly caused by the increased contribution of calcium, which could be released from carbonates during extraction of bases.http://www.degruyter.com/view/j/ssa.2019.70.issue-2/ssa-2019-0013/ssa-2019-0013.xml?format=INTgranulometric fractionscation exchange capacityleaching process |
spellingShingle | Brogowski Zygmunt Chojnicki Józef Sorption properties of granulometric fractions in Haplic Cambisol developed from boulder loam Soil Science Annual granulometric fractions cation exchange capacity leaching process |
title | Sorption properties of granulometric fractions in Haplic Cambisol developed from boulder loam |
title_full | Sorption properties of granulometric fractions in Haplic Cambisol developed from boulder loam |
title_fullStr | Sorption properties of granulometric fractions in Haplic Cambisol developed from boulder loam |
title_full_unstemmed | Sorption properties of granulometric fractions in Haplic Cambisol developed from boulder loam |
title_short | Sorption properties of granulometric fractions in Haplic Cambisol developed from boulder loam |
title_sort | sorption properties of granulometric fractions in haplic cambisol developed from boulder loam |
topic | granulometric fractions cation exchange capacity leaching process |
url | http://www.degruyter.com/view/j/ssa.2019.70.issue-2/ssa-2019-0013/ssa-2019-0013.xml?format=INT |
work_keys_str_mv | AT brogowskizygmunt sorptionpropertiesofgranulometricfractionsinhapliccambisoldevelopedfromboulderloam AT chojnickijozef sorptionpropertiesofgranulometricfractionsinhapliccambisoldevelopedfromboulderloam |