Soil organic matter transformation influenced by silver birch (Betula pendula Roth) succession on abandoned from agricultural production sandy soil

Abstract A chronosequence approach was applied to evaluate the effects of silver birch succession on soil organic matter (SOM). The studies covered five plots (arable field [AF], fallow [FA] and three birch stands aged 8, 33 and 40 years), and all located in the same complex of Brunic Arenosols in c...
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Autor*in:	Jonczak, Jerzy [verfasserIn] Oktaba, Lidia Pawłowicz, Edyta Chojnacka, Aleksandra Regulska, Edyta Słowińska, Sandra Olejniczak, Izabella Oktaba, Jarosław Kruczkowska, Bogusława Kondras, Marek Jankiewicz, Urszula Wójcik-Gront, Elżbieta

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2022

Schlagwörter:	Silver birch Soil organic matter Ecological succession Post-arable soils Soil quality

Anmerkung:	© The Author(s) 2022

Übergeordnetes Werk:	Enthalten in: European journal of forest research - Berlin : Springer, 2004, 142(2022), 2 vom: 24. Dez., Seite 367-379
Übergeordnetes Werk:	volume:142 ; year:2022 ; number:2 ; day:24 ; month:12 ; pages:367-379

Links:	Volltext

DOI / URN:	10.1007/s10342-022-01527-8

Katalog-ID:	SPR04999431X

Internformat


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100	1		\|a Jonczak, Jerzy \|e verfasserin \|0 (orcid)0000-0002-9577-5292 \|4 aut
245	1	0	\|a Soil organic matter transformation influenced by silver birch (Betula pendula Roth) succession on abandoned from agricultural production sandy soil
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520			\|a Abstract A chronosequence approach was applied to evaluate the effects of silver birch succession on soil organic matter (SOM). The studies covered five plots (arable field [AF], fallow [FA] and three birch stands aged 8, 33 and 40 years), and all located in the same complex of Brunic Arenosols in central Poland. The O and A horizons of the soils were sampled and analysed using the standard procedures in soil science. It was found that the birch succession was accompanied by dynamic changes in the stock and quality of the SOM. The transition from AF to FA soils did not significantly change the content or pool of SOM in the A horizon; however, it did modify its fractional composition and internal structure. This was reflected by an increase in the humic acids content and a decrease in the fulvic acid, as well as in the values of the elemental and 13C-NMR analyses. Rapid losses in the SOM content and stock in the A horizon were recorded after entering the silver birch. The soils under the young birches were characterised by lower contents of low-molecular humus fractions, which are more susceptible to microbial degradation, than the FA soils. In addition, the birch succession contributed to a lower internal oxidation of the humic acids and an increase in the content of aliphatic structures in their molecules. The next stages of succession were characterised by gradually increasing SOM contents and stocks, accompanied by the increasing internal oxidation and maturity of the humic acids.
650		4	\|a Silver birch \|7 (dpeaa)DE-He213
650		4	\|a Soil organic matter \|7 (dpeaa)DE-He213
650		4	\|a Ecological succession \|7 (dpeaa)DE-He213
650		4	\|a Post-arable soils \|7 (dpeaa)DE-He213
650		4	\|a Soil quality \|7 (dpeaa)DE-He213
700	1		\|a Oktaba, Lidia \|0 (orcid)0000-0002-4937-9299 \|4 aut
700	1		\|a Pawłowicz, Edyta \|0 (orcid)0000-0003-4247-1479 \|4 aut
700	1		\|a Chojnacka, Aleksandra \|0 (orcid)0000-0001-7802-1678 \|4 aut
700	1		\|a Regulska, Edyta \|0 (orcid)0000-0003-0386-3306 \|4 aut
700	1		\|a Słowińska, Sandra \|0 (orcid)0000-0003-4233-7384 \|4 aut
700	1		\|a Olejniczak, Izabella \|0 (orcid)0000-0003-4746-7874 \|4 aut
700	1		\|a Oktaba, Jarosław \|0 (orcid)0000-0003-0934-0098 \|4 aut
700	1		\|a Kruczkowska, Bogusława \|0 (orcid)0000-0003-0764-9884 \|4 aut
700	1		\|a Kondras, Marek \|0 (orcid)0000-0002-1987-7983 \|4 aut
700	1		\|a Jankiewicz, Urszula \|0 (orcid)0000-0003-2240-6629 \|4 aut
700	1		\|a Wójcik-Gront, Elżbieta \|0 (orcid)0000-0002-7172-0529 \|4 aut
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912			\|a GBV_ILN_2015
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912			\|a GBV_ILN_2031
912			\|a GBV_ILN_2034
912			\|a GBV_ILN_2037
912			\|a GBV_ILN_2038
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912			\|a GBV_ILN_2044
912			\|a GBV_ILN_2048
912			\|a GBV_ILN_2049
912			\|a GBV_ILN_2050
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912			\|a GBV_ILN_2056
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952			\|d 142 \|j 2022 \|e 2 \|b 24 \|c 12 \|h 367-379

Indexfelder

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matchkey_str	article:16124677:2022----::olraimtetasomtoifunebslebrheuaedlrtscesooaadnd
hierarchy_sort_str	2022
publishDate	2022
allfields	10.1007/s10342-022-01527-8 doi (DE-627)SPR04999431X (SPR)s10342-022-01527-8-e DE-627 ger DE-627 rakwb eng Jonczak, Jerzy verfasserin (orcid)0000-0002-9577-5292 aut Soil organic matter transformation influenced by silver birch (Betula pendula Roth) succession on abandoned from agricultural production sandy soil 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2022 Abstract A chronosequence approach was applied to evaluate the effects of silver birch succession on soil organic matter (SOM). The studies covered five plots (arable field [AF], fallow [FA] and three birch stands aged 8, 33 and 40 years), and all located in the same complex of Brunic Arenosols in central Poland. The O and A horizons of the soils were sampled and analysed using the standard procedures in soil science. It was found that the birch succession was accompanied by dynamic changes in the stock and quality of the SOM. The transition from AF to FA soils did not significantly change the content or pool of SOM in the A horizon; however, it did modify its fractional composition and internal structure. This was reflected by an increase in the humic acids content and a decrease in the fulvic acid, as well as in the values of the elemental and 13C-NMR analyses. Rapid losses in the SOM content and stock in the A horizon were recorded after entering the silver birch. The soils under the young birches were characterised by lower contents of low-molecular humus fractions, which are more susceptible to microbial degradation, than the FA soils. In addition, the birch succession contributed to a lower internal oxidation of the humic acids and an increase in the content of aliphatic structures in their molecules. The next stages of succession were characterised by gradually increasing SOM contents and stocks, accompanied by the increasing internal oxidation and maturity of the humic acids. Silver birch (dpeaa)DE-He213 Soil organic matter (dpeaa)DE-He213 Ecological succession (dpeaa)DE-He213 Post-arable soils (dpeaa)DE-He213 Soil quality (dpeaa)DE-He213 Oktaba, Lidia (orcid)0000-0002-4937-9299 aut Pawłowicz, Edyta (orcid)0000-0003-4247-1479 aut Chojnacka, Aleksandra (orcid)0000-0001-7802-1678 aut Regulska, Edyta (orcid)0000-0003-0386-3306 aut Słowińska, Sandra (orcid)0000-0003-4233-7384 aut Olejniczak, Izabella (orcid)0000-0003-4746-7874 aut Oktaba, Jarosław (orcid)0000-0003-0934-0098 aut Kruczkowska, Bogusława (orcid)0000-0003-0764-9884 aut Kondras, Marek (orcid)0000-0002-1987-7983 aut Jankiewicz, Urszula (orcid)0000-0003-2240-6629 aut Wójcik-Gront, Elżbieta (orcid)0000-0002-7172-0529 aut Enthalten in European journal of forest research Berlin : Springer, 2004 142(2022), 2 vom: 24. Dez., Seite 367-379 (DE-627)378132512 (DE-600)2134019-5 1612-4677 nnns volume:142 year:2022 number:2 day:24 month:12 pages:367-379 https://dx.doi.org/10.1007/s10342-022-01527-8 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 142 2022 2 24 12 367-379
spelling	10.1007/s10342-022-01527-8 doi (DE-627)SPR04999431X (SPR)s10342-022-01527-8-e DE-627 ger DE-627 rakwb eng Jonczak, Jerzy verfasserin (orcid)0000-0002-9577-5292 aut Soil organic matter transformation influenced by silver birch (Betula pendula Roth) succession on abandoned from agricultural production sandy soil 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2022 Abstract A chronosequence approach was applied to evaluate the effects of silver birch succession on soil organic matter (SOM). The studies covered five plots (arable field [AF], fallow [FA] and three birch stands aged 8, 33 and 40 years), and all located in the same complex of Brunic Arenosols in central Poland. The O and A horizons of the soils were sampled and analysed using the standard procedures in soil science. It was found that the birch succession was accompanied by dynamic changes in the stock and quality of the SOM. The transition from AF to FA soils did not significantly change the content or pool of SOM in the A horizon; however, it did modify its fractional composition and internal structure. This was reflected by an increase in the humic acids content and a decrease in the fulvic acid, as well as in the values of the elemental and 13C-NMR analyses. Rapid losses in the SOM content and stock in the A horizon were recorded after entering the silver birch. The soils under the young birches were characterised by lower contents of low-molecular humus fractions, which are more susceptible to microbial degradation, than the FA soils. In addition, the birch succession contributed to a lower internal oxidation of the humic acids and an increase in the content of aliphatic structures in their molecules. The next stages of succession were characterised by gradually increasing SOM contents and stocks, accompanied by the increasing internal oxidation and maturity of the humic acids. Silver birch (dpeaa)DE-He213 Soil organic matter (dpeaa)DE-He213 Ecological succession (dpeaa)DE-He213 Post-arable soils (dpeaa)DE-He213 Soil quality (dpeaa)DE-He213 Oktaba, Lidia (orcid)0000-0002-4937-9299 aut Pawłowicz, Edyta (orcid)0000-0003-4247-1479 aut Chojnacka, Aleksandra (orcid)0000-0001-7802-1678 aut Regulska, Edyta (orcid)0000-0003-0386-3306 aut Słowińska, Sandra (orcid)0000-0003-4233-7384 aut Olejniczak, Izabella (orcid)0000-0003-4746-7874 aut Oktaba, Jarosław (orcid)0000-0003-0934-0098 aut Kruczkowska, Bogusława (orcid)0000-0003-0764-9884 aut Kondras, Marek (orcid)0000-0002-1987-7983 aut Jankiewicz, Urszula (orcid)0000-0003-2240-6629 aut Wójcik-Gront, Elżbieta (orcid)0000-0002-7172-0529 aut Enthalten in European journal of forest research Berlin : Springer, 2004 142(2022), 2 vom: 24. Dez., Seite 367-379 (DE-627)378132512 (DE-600)2134019-5 1612-4677 nnns volume:142 year:2022 number:2 day:24 month:12 pages:367-379 https://dx.doi.org/10.1007/s10342-022-01527-8 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 142 2022 2 24 12 367-379
allfields_unstemmed	10.1007/s10342-022-01527-8 doi (DE-627)SPR04999431X (SPR)s10342-022-01527-8-e DE-627 ger DE-627 rakwb eng Jonczak, Jerzy verfasserin (orcid)0000-0002-9577-5292 aut Soil organic matter transformation influenced by silver birch (Betula pendula Roth) succession on abandoned from agricultural production sandy soil 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2022 Abstract A chronosequence approach was applied to evaluate the effects of silver birch succession on soil organic matter (SOM). The studies covered five plots (arable field [AF], fallow [FA] and three birch stands aged 8, 33 and 40 years), and all located in the same complex of Brunic Arenosols in central Poland. The O and A horizons of the soils were sampled and analysed using the standard procedures in soil science. It was found that the birch succession was accompanied by dynamic changes in the stock and quality of the SOM. The transition from AF to FA soils did not significantly change the content or pool of SOM in the A horizon; however, it did modify its fractional composition and internal structure. This was reflected by an increase in the humic acids content and a decrease in the fulvic acid, as well as in the values of the elemental and 13C-NMR analyses. Rapid losses in the SOM content and stock in the A horizon were recorded after entering the silver birch. The soils under the young birches were characterised by lower contents of low-molecular humus fractions, which are more susceptible to microbial degradation, than the FA soils. In addition, the birch succession contributed to a lower internal oxidation of the humic acids and an increase in the content of aliphatic structures in their molecules. The next stages of succession were characterised by gradually increasing SOM contents and stocks, accompanied by the increasing internal oxidation and maturity of the humic acids. Silver birch (dpeaa)DE-He213 Soil organic matter (dpeaa)DE-He213 Ecological succession (dpeaa)DE-He213 Post-arable soils (dpeaa)DE-He213 Soil quality (dpeaa)DE-He213 Oktaba, Lidia (orcid)0000-0002-4937-9299 aut Pawłowicz, Edyta (orcid)0000-0003-4247-1479 aut Chojnacka, Aleksandra (orcid)0000-0001-7802-1678 aut Regulska, Edyta (orcid)0000-0003-0386-3306 aut Słowińska, Sandra (orcid)0000-0003-4233-7384 aut Olejniczak, Izabella (orcid)0000-0003-4746-7874 aut Oktaba, Jarosław (orcid)0000-0003-0934-0098 aut Kruczkowska, Bogusława (orcid)0000-0003-0764-9884 aut Kondras, Marek (orcid)0000-0002-1987-7983 aut Jankiewicz, Urszula (orcid)0000-0003-2240-6629 aut Wójcik-Gront, Elżbieta (orcid)0000-0002-7172-0529 aut Enthalten in European journal of forest research Berlin : Springer, 2004 142(2022), 2 vom: 24. Dez., Seite 367-379 (DE-627)378132512 (DE-600)2134019-5 1612-4677 nnns volume:142 year:2022 number:2 day:24 month:12 pages:367-379 https://dx.doi.org/10.1007/s10342-022-01527-8 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 142 2022 2 24 12 367-379
allfieldsGer	10.1007/s10342-022-01527-8 doi (DE-627)SPR04999431X (SPR)s10342-022-01527-8-e DE-627 ger DE-627 rakwb eng Jonczak, Jerzy verfasserin (orcid)0000-0002-9577-5292 aut Soil organic matter transformation influenced by silver birch (Betula pendula Roth) succession on abandoned from agricultural production sandy soil 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2022 Abstract A chronosequence approach was applied to evaluate the effects of silver birch succession on soil organic matter (SOM). The studies covered five plots (arable field [AF], fallow [FA] and three birch stands aged 8, 33 and 40 years), and all located in the same complex of Brunic Arenosols in central Poland. The O and A horizons of the soils were sampled and analysed using the standard procedures in soil science. It was found that the birch succession was accompanied by dynamic changes in the stock and quality of the SOM. The transition from AF to FA soils did not significantly change the content or pool of SOM in the A horizon; however, it did modify its fractional composition and internal structure. This was reflected by an increase in the humic acids content and a decrease in the fulvic acid, as well as in the values of the elemental and 13C-NMR analyses. Rapid losses in the SOM content and stock in the A horizon were recorded after entering the silver birch. The soils under the young birches were characterised by lower contents of low-molecular humus fractions, which are more susceptible to microbial degradation, than the FA soils. In addition, the birch succession contributed to a lower internal oxidation of the humic acids and an increase in the content of aliphatic structures in their molecules. The next stages of succession were characterised by gradually increasing SOM contents and stocks, accompanied by the increasing internal oxidation and maturity of the humic acids. Silver birch (dpeaa)DE-He213 Soil organic matter (dpeaa)DE-He213 Ecological succession (dpeaa)DE-He213 Post-arable soils (dpeaa)DE-He213 Soil quality (dpeaa)DE-He213 Oktaba, Lidia (orcid)0000-0002-4937-9299 aut Pawłowicz, Edyta (orcid)0000-0003-4247-1479 aut Chojnacka, Aleksandra (orcid)0000-0001-7802-1678 aut Regulska, Edyta (orcid)0000-0003-0386-3306 aut Słowińska, Sandra (orcid)0000-0003-4233-7384 aut Olejniczak, Izabella (orcid)0000-0003-4746-7874 aut Oktaba, Jarosław (orcid)0000-0003-0934-0098 aut Kruczkowska, Bogusława (orcid)0000-0003-0764-9884 aut Kondras, Marek (orcid)0000-0002-1987-7983 aut Jankiewicz, Urszula (orcid)0000-0003-2240-6629 aut Wójcik-Gront, Elżbieta (orcid)0000-0002-7172-0529 aut Enthalten in European journal of forest research Berlin : Springer, 2004 142(2022), 2 vom: 24. Dez., Seite 367-379 (DE-627)378132512 (DE-600)2134019-5 1612-4677 nnns volume:142 year:2022 number:2 day:24 month:12 pages:367-379 https://dx.doi.org/10.1007/s10342-022-01527-8 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 142 2022 2 24 12 367-379
allfieldsSound	10.1007/s10342-022-01527-8 doi (DE-627)SPR04999431X (SPR)s10342-022-01527-8-e DE-627 ger DE-627 rakwb eng Jonczak, Jerzy verfasserin (orcid)0000-0002-9577-5292 aut Soil organic matter transformation influenced by silver birch (Betula pendula Roth) succession on abandoned from agricultural production sandy soil 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2022 Abstract A chronosequence approach was applied to evaluate the effects of silver birch succession on soil organic matter (SOM). The studies covered five plots (arable field [AF], fallow [FA] and three birch stands aged 8, 33 and 40 years), and all located in the same complex of Brunic Arenosols in central Poland. The O and A horizons of the soils were sampled and analysed using the standard procedures in soil science. It was found that the birch succession was accompanied by dynamic changes in the stock and quality of the SOM. The transition from AF to FA soils did not significantly change the content or pool of SOM in the A horizon; however, it did modify its fractional composition and internal structure. This was reflected by an increase in the humic acids content and a decrease in the fulvic acid, as well as in the values of the elemental and 13C-NMR analyses. Rapid losses in the SOM content and stock in the A horizon were recorded after entering the silver birch. The soils under the young birches were characterised by lower contents of low-molecular humus fractions, which are more susceptible to microbial degradation, than the FA soils. In addition, the birch succession contributed to a lower internal oxidation of the humic acids and an increase in the content of aliphatic structures in their molecules. The next stages of succession were characterised by gradually increasing SOM contents and stocks, accompanied by the increasing internal oxidation and maturity of the humic acids. Silver birch (dpeaa)DE-He213 Soil organic matter (dpeaa)DE-He213 Ecological succession (dpeaa)DE-He213 Post-arable soils (dpeaa)DE-He213 Soil quality (dpeaa)DE-He213 Oktaba, Lidia (orcid)0000-0002-4937-9299 aut Pawłowicz, Edyta (orcid)0000-0003-4247-1479 aut Chojnacka, Aleksandra (orcid)0000-0001-7802-1678 aut Regulska, Edyta (orcid)0000-0003-0386-3306 aut Słowińska, Sandra (orcid)0000-0003-4233-7384 aut Olejniczak, Izabella (orcid)0000-0003-4746-7874 aut Oktaba, Jarosław (orcid)0000-0003-0934-0098 aut Kruczkowska, Bogusława (orcid)0000-0003-0764-9884 aut Kondras, Marek (orcid)0000-0002-1987-7983 aut Jankiewicz, Urszula (orcid)0000-0003-2240-6629 aut Wójcik-Gront, Elżbieta (orcid)0000-0002-7172-0529 aut Enthalten in European journal of forest research Berlin : Springer, 2004 142(2022), 2 vom: 24. Dez., Seite 367-379 (DE-627)378132512 (DE-600)2134019-5 1612-4677 nnns volume:142 year:2022 number:2 day:24 month:12 pages:367-379 https://dx.doi.org/10.1007/s10342-022-01527-8 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 142 2022 2 24 12 367-379
language	English
source	Enthalten in European journal of forest research 142(2022), 2 vom: 24. Dez., Seite 367-379 volume:142 year:2022 number:2 day:24 month:12 pages:367-379
sourceStr	Enthalten in European journal of forest research 142(2022), 2 vom: 24. Dez., Seite 367-379 volume:142 year:2022 number:2 day:24 month:12 pages:367-379
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Silver birch Soil organic matter Ecological succession Post-arable soils Soil quality
isfreeaccess_bool	true
container_title	European journal of forest research
authorswithroles_txt_mv	Jonczak, Jerzy @@aut@@ Oktaba, Lidia @@aut@@ Pawłowicz, Edyta @@aut@@ Chojnacka, Aleksandra @@aut@@ Regulska, Edyta @@aut@@ Słowińska, Sandra @@aut@@ Olejniczak, Izabella @@aut@@ Oktaba, Jarosław @@aut@@ Kruczkowska, Bogusława @@aut@@ Kondras, Marek @@aut@@ Jankiewicz, Urszula @@aut@@ Wójcik-Gront, Elżbieta @@aut@@
publishDateDaySort_date	2022-12-24T00:00:00Z
hierarchy_top_id	378132512
id	SPR04999431X
language_de	englisch
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The studies covered five plots (arable field [AF], fallow [FA] and three birch stands aged 8, 33 and 40 years), and all located in the same complex of Brunic Arenosols in central Poland. The O and A horizons of the soils were sampled and analysed using the standard procedures in soil science. It was found that the birch succession was accompanied by dynamic changes in the stock and quality of the SOM. The transition from AF to FA soils did not significantly change the content or pool of SOM in the A horizon; however, it did modify its fractional composition and internal structure. This was reflected by an increase in the humic acids content and a decrease in the fulvic acid, as well as in the values of the elemental and 13C-NMR analyses. Rapid losses in the SOM content and stock in the A horizon were recorded after entering the silver birch. The soils under the young birches were characterised by lower contents of low-molecular humus fractions, which are more susceptible to microbial degradation, than the FA soils. In addition, the birch succession contributed to a lower internal oxidation of the humic acids and an increase in the content of aliphatic structures in their molecules. 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author	Jonczak, Jerzy
spellingShingle	Jonczak, Jerzy misc Silver birch misc Soil organic matter misc Ecological succession misc Post-arable soils misc Soil quality Soil organic matter transformation influenced by silver birch (Betula pendula Roth) succession on abandoned from agricultural production sandy soil
authorStr	Jonczak, Jerzy
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topic_title	Soil organic matter transformation influenced by silver birch (Betula pendula Roth) succession on abandoned from agricultural production sandy soil Silver birch (dpeaa)DE-He213 Soil organic matter (dpeaa)DE-He213 Ecological succession (dpeaa)DE-He213 Post-arable soils (dpeaa)DE-He213 Soil quality (dpeaa)DE-He213
topic	misc Silver birch misc Soil organic matter misc Ecological succession misc Post-arable soils misc Soil quality
topic_unstemmed	misc Silver birch misc Soil organic matter misc Ecological succession misc Post-arable soils misc Soil quality
topic_browse	misc Silver birch misc Soil organic matter misc Ecological succession misc Post-arable soils misc Soil quality
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title	Soil organic matter transformation influenced by silver birch (Betula pendula Roth) succession on abandoned from agricultural production sandy soil
ctrlnum	(DE-627)SPR04999431X (SPR)s10342-022-01527-8-e
title_full	Soil organic matter transformation influenced by silver birch (Betula pendula Roth) succession on abandoned from agricultural production sandy soil
author_sort	Jonczak, Jerzy
journal	European journal of forest research
journalStr	European journal of forest research
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author_browse	Jonczak, Jerzy Oktaba, Lidia Pawłowicz, Edyta Chojnacka, Aleksandra Regulska, Edyta Słowińska, Sandra Olejniczak, Izabella Oktaba, Jarosław Kruczkowska, Bogusława Kondras, Marek Jankiewicz, Urszula Wójcik-Gront, Elżbieta
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author-letter	Jonczak, Jerzy
doi_str_mv	10.1007/s10342-022-01527-8
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title_sort	soil organic matter transformation influenced by silver birch (betula pendula roth) succession on abandoned from agricultural production sandy soil
title_auth	Soil organic matter transformation influenced by silver birch (Betula pendula Roth) succession on abandoned from agricultural production sandy soil
abstract	Abstract A chronosequence approach was applied to evaluate the effects of silver birch succession on soil organic matter (SOM). The studies covered five plots (arable field [AF], fallow [FA] and three birch stands aged 8, 33 and 40 years), and all located in the same complex of Brunic Arenosols in central Poland. The O and A horizons of the soils were sampled and analysed using the standard procedures in soil science. It was found that the birch succession was accompanied by dynamic changes in the stock and quality of the SOM. The transition from AF to FA soils did not significantly change the content or pool of SOM in the A horizon; however, it did modify its fractional composition and internal structure. This was reflected by an increase in the humic acids content and a decrease in the fulvic acid, as well as in the values of the elemental and 13C-NMR analyses. Rapid losses in the SOM content and stock in the A horizon were recorded after entering the silver birch. The soils under the young birches were characterised by lower contents of low-molecular humus fractions, which are more susceptible to microbial degradation, than the FA soils. In addition, the birch succession contributed to a lower internal oxidation of the humic acids and an increase in the content of aliphatic structures in their molecules. The next stages of succession were characterised by gradually increasing SOM contents and stocks, accompanied by the increasing internal oxidation and maturity of the humic acids. © The Author(s) 2022
abstractGer	Abstract A chronosequence approach was applied to evaluate the effects of silver birch succession on soil organic matter (SOM). The studies covered five plots (arable field [AF], fallow [FA] and three birch stands aged 8, 33 and 40 years), and all located in the same complex of Brunic Arenosols in central Poland. The O and A horizons of the soils were sampled and analysed using the standard procedures in soil science. It was found that the birch succession was accompanied by dynamic changes in the stock and quality of the SOM. The transition from AF to FA soils did not significantly change the content or pool of SOM in the A horizon; however, it did modify its fractional composition and internal structure. This was reflected by an increase in the humic acids content and a decrease in the fulvic acid, as well as in the values of the elemental and 13C-NMR analyses. Rapid losses in the SOM content and stock in the A horizon were recorded after entering the silver birch. The soils under the young birches were characterised by lower contents of low-molecular humus fractions, which are more susceptible to microbial degradation, than the FA soils. In addition, the birch succession contributed to a lower internal oxidation of the humic acids and an increase in the content of aliphatic structures in their molecules. The next stages of succession were characterised by gradually increasing SOM contents and stocks, accompanied by the increasing internal oxidation and maturity of the humic acids. © The Author(s) 2022
abstract_unstemmed	Abstract A chronosequence approach was applied to evaluate the effects of silver birch succession on soil organic matter (SOM). The studies covered five plots (arable field [AF], fallow [FA] and three birch stands aged 8, 33 and 40 years), and all located in the same complex of Brunic Arenosols in central Poland. The O and A horizons of the soils were sampled and analysed using the standard procedures in soil science. It was found that the birch succession was accompanied by dynamic changes in the stock and quality of the SOM. The transition from AF to FA soils did not significantly change the content or pool of SOM in the A horizon; however, it did modify its fractional composition and internal structure. This was reflected by an increase in the humic acids content and a decrease in the fulvic acid, as well as in the values of the elemental and 13C-NMR analyses. Rapid losses in the SOM content and stock in the A horizon were recorded after entering the silver birch. The soils under the young birches were characterised by lower contents of low-molecular humus fractions, which are more susceptible to microbial degradation, than the FA soils. In addition, the birch succession contributed to a lower internal oxidation of the humic acids and an increase in the content of aliphatic structures in their molecules. The next stages of succession were characterised by gradually increasing SOM contents and stocks, accompanied by the increasing internal oxidation and maturity of the humic acids. © The Author(s) 2022
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container_issue	2
title_short	Soil organic matter transformation influenced by silver birch (Betula pendula Roth) succession on abandoned from agricultural production sandy soil
url	https://dx.doi.org/10.1007/s10342-022-01527-8
remote_bool	true
author2	Oktaba, Lidia Pawłowicz, Edyta Chojnacka, Aleksandra Regulska, Edyta Słowińska, Sandra Olejniczak, Izabella Oktaba, Jarosław Kruczkowska, Bogusława Kondras, Marek Jankiewicz, Urszula Wójcik-Gront, Elżbieta
author2Str	Oktaba, Lidia Pawłowicz, Edyta Chojnacka, Aleksandra Regulska, Edyta Słowińska, Sandra Olejniczak, Izabella Oktaba, Jarosław Kruczkowska, Bogusława Kondras, Marek Jankiewicz, Urszula Wójcik-Gront, Elżbieta
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doi_str	10.1007/s10342-022-01527-8
up_date	2024-07-04T03:03:11.343Z
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Soil organic matter transformation influenced by silver birch (Betula pendula Roth) succession on abandoned from agricultural production sandy soil

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