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...

Full description

Bibliographic Details
Main Authors: Brogowski Zygmunt, Chojnicki Józef
Format: Article
Language:English
Published: Soil Science Society of Poland 2019-06-01
Series:Soil Science Annual
Subjects:
Online Access:http://www.degruyter.com/view/j/ssa.2019.70.issue-2/ssa-2019-0013/ssa-2019-0013.xml?format=INT
_version_ 1818539841663533056
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.
first_indexed 2024-12-11T21:47:26Z
format Article
id doaj.art-ef2cd6415d974b7091fc2dc629865920
institution Directory Open Access Journal
issn 2300-4975
language English
last_indexed 2024-12-11T21:47:26Z
publishDate 2019-06-01
publisher Soil Science Society of Poland
record_format Article
series Soil Science Annual
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