Potential changes in Czech forest soil carbon stocks under different climate change scenarios

Detailed inventory data (n = 3,930; approximately one representative sampling point per 650 ha) on soil organic carbon (SOC) to a depth of 30 cm has been used to characterize carbon content in forest soils in the Czech Republic across all altitudinal vegetation zones and forest ecological series. Th...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	I. Marková [verfasserIn] D. Janouš [verfasserIn] M. Pavelka [verfasserIn] J. Macků [verfasserIn] K. Havránková [verfasserIn] K. Rejšek [verfasserIn] M.V. Marek [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2016

Schlagwörter:	oxidizable soil carbon content altitudinal vegetation zone ecological series

Übergeordnetes Werk:	In: Journal of Forest Science - Czech Academy of Agricultural Sciences, 2015, 62(2016), 12, Seite 537-544
Übergeordnetes Werk:	volume:62 ; year:2016 ; number:12 ; pages:537-544

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc Journal toc

DOI / URN:	10.17221/103/2015-JFS

Katalog-ID:	DOAJ082850143

Internformat


LEADER	01000naa a22002652 4500
001	DOAJ082850143
003	DE-627
005	20230311004704.0
007	cr uuu---uuuuu
008	230311s2016 xx \|\|\|\|\|o 00\| \|\|eng c
024	7		\|a 10.17221/103/2015-JFS \|2 doi
035			\|a (DE-627)DOAJ082850143
035			\|a (DE-599)DOAJeb94723c8bcc454aaf750bfa78208186
040			\|a DE-627 \|b ger \|c DE-627 \|e rakwb
041			\|a eng
050		0	\|a SD1-669.5
100	0		\|a I. Marková \|e verfasserin \|4 aut
245	1	0	\|a Potential changes in Czech forest soil carbon stocks under different climate change scenarios
264		1	\|c 2016
336			\|a Text \|b txt \|2 rdacontent
337			\|a Computermedien \|b c \|2 rdamedia
338			\|a Online-Ressource \|b cr \|2 rdacarrier
520			\|a Detailed inventory data (n = 3,930; approximately one representative sampling point per 650 ha) on soil organic carbon (SOC) to a depth of 30 cm has been used to characterize carbon content in forest soils in the Czech Republic across all altitudinal vegetation zones and forest ecological series. This data set was used to predict the most probable changes in soil carbon content in the altitudinal vegetation zones due to global warming. The mean value of the SOC content in forest soils of the Czech Republic was determined to be 62.6 ± 17.2 t.ha-1. Under different warming scenarios the major SOC loss was observed at an altitude of 700-900 m a.s.l. Using a pessimistic emission scenario in the climatic model (i.e. predicted temperature change by +4.24°C), losses of C from forest soils in the Czech Republic, or potentially in central Europe, could be as high as 13% of the current carbon stock in forest soils.
650		4	\|a oxidizable soil carbon content
650		4	\|a altitudinal vegetation zone
650		4	\|a ecological series
653		0	\|a Forestry
700	0		\|a D. Janouš \|e verfasserin \|4 aut
700	0		\|a M. Pavelka \|e verfasserin \|4 aut
700	0		\|a J. Macků \|e verfasserin \|4 aut
700	0		\|a K. Havránková \|e verfasserin \|4 aut
700	0		\|a K. Rejšek \|e verfasserin \|4 aut
700	0		\|a M.V. Marek \|e verfasserin \|4 aut
773	0	8	\|i In \|t Journal of Forest Science \|d Czech Academy of Agricultural Sciences, 2015 \|g 62(2016), 12, Seite 537-544 \|w (DE-627)387480773 \|w (DE-600)2145663-X \|x 1805935X \|7 nnns
773	1	8	\|g volume:62 \|g year:2016 \|g number:12 \|g pages:537-544
856	4	0	\|u https://doi.org/10.17221/103/2015-JFS \|z kostenfrei
856	4	0	\|u https://doaj.org/article/eb94723c8bcc454aaf750bfa78208186 \|z kostenfrei
856	4	0	\|u https://jfs.agriculturejournals.cz/artkey/jfs-201612-0002_potential-changes-in-czech-forest-soil-carbon-stocks-under-different-climate-change-scenarios.php \|z kostenfrei
856	4	2	\|u https://doaj.org/toc/1212-4834 \|y Journal toc \|z kostenfrei
856	4	2	\|u https://doaj.org/toc/1805-935X \|y Journal toc \|z kostenfrei
912			\|a GBV_USEFLAG_A
912			\|a SYSFLAG_A
912			\|a GBV_DOAJ
912			\|a GBV_ILN_20
912			\|a GBV_ILN_22
912			\|a GBV_ILN_24
912			\|a GBV_ILN_31
912			\|a GBV_ILN_39
912			\|a GBV_ILN_40
912			\|a GBV_ILN_60
912			\|a GBV_ILN_62
912			\|a GBV_ILN_63
912			\|a GBV_ILN_65
912			\|a GBV_ILN_69
912			\|a GBV_ILN_70
912			\|a GBV_ILN_73
912			\|a GBV_ILN_95
912			\|a GBV_ILN_105
912			\|a GBV_ILN_110
912			\|a GBV_ILN_151
912			\|a GBV_ILN_161
912			\|a GBV_ILN_213
912			\|a GBV_ILN_230
912			\|a GBV_ILN_285
912			\|a GBV_ILN_293
912			\|a GBV_ILN_602
912			\|a GBV_ILN_2014
912			\|a GBV_ILN_4012
912			\|a GBV_ILN_4037
912			\|a GBV_ILN_4112
912			\|a GBV_ILN_4125
912			\|a GBV_ILN_4126
912			\|a GBV_ILN_4249
912			\|a GBV_ILN_4305
912			\|a GBV_ILN_4306
912			\|a GBV_ILN_4307
912			\|a GBV_ILN_4313
912			\|a GBV_ILN_4322
912			\|a GBV_ILN_4323
912			\|a GBV_ILN_4324
912			\|a GBV_ILN_4325
912			\|a GBV_ILN_4367
912			\|a GBV_ILN_4700
951			\|a AR
952			\|d 62 \|j 2016 \|e 12 \|h 537-544

Indexfelder

author_variant	i m im d j dj m p mp j m jm k h kh k r kr m m mm
matchkey_str	article:1805935X:2016----::oetacagsnzcfrssicrosokudrifrnc
hierarchy_sort_str	2016
callnumber-subject-code	SD
publishDate	2016
allfields	10.17221/103/2015-JFS doi (DE-627)DOAJ082850143 (DE-599)DOAJeb94723c8bcc454aaf750bfa78208186 DE-627 ger DE-627 rakwb eng SD1-669.5 I. Marková verfasserin aut Potential changes in Czech forest soil carbon stocks under different climate change scenarios 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Detailed inventory data (n = 3,930; approximately one representative sampling point per 650 ha) on soil organic carbon (SOC) to a depth of 30 cm has been used to characterize carbon content in forest soils in the Czech Republic across all altitudinal vegetation zones and forest ecological series. This data set was used to predict the most probable changes in soil carbon content in the altitudinal vegetation zones due to global warming. The mean value of the SOC content in forest soils of the Czech Republic was determined to be 62.6 ± 17.2 t.ha-1. Under different warming scenarios the major SOC loss was observed at an altitude of 700-900 m a.s.l. Using a pessimistic emission scenario in the climatic model (i.e. predicted temperature change by +4.24°C), losses of C from forest soils in the Czech Republic, or potentially in central Europe, could be as high as 13% of the current carbon stock in forest soils. oxidizable soil carbon content altitudinal vegetation zone ecological series Forestry D. Janouš verfasserin aut M. Pavelka verfasserin aut J. Macků verfasserin aut K. Havránková verfasserin aut K. Rejšek verfasserin aut M.V. Marek verfasserin aut In Journal of Forest Science Czech Academy of Agricultural Sciences, 2015 62(2016), 12, Seite 537-544 (DE-627)387480773 (DE-600)2145663-X 1805935X nnns volume:62 year:2016 number:12 pages:537-544 https://doi.org/10.17221/103/2015-JFS kostenfrei https://doaj.org/article/eb94723c8bcc454aaf750bfa78208186 kostenfrei https://jfs.agriculturejournals.cz/artkey/jfs-201612-0002_potential-changes-in-czech-forest-soil-carbon-stocks-under-different-climate-change-scenarios.php kostenfrei https://doaj.org/toc/1212-4834 Journal toc kostenfrei https://doaj.org/toc/1805-935X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_20 GBV_ILN_22 GBV_ILN_24 GBV_ILN_31 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4367 GBV_ILN_4700 AR 62 2016 12 537-544
spelling	10.17221/103/2015-JFS doi (DE-627)DOAJ082850143 (DE-599)DOAJeb94723c8bcc454aaf750bfa78208186 DE-627 ger DE-627 rakwb eng SD1-669.5 I. Marková verfasserin aut Potential changes in Czech forest soil carbon stocks under different climate change scenarios 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Detailed inventory data (n = 3,930; approximately one representative sampling point per 650 ha) on soil organic carbon (SOC) to a depth of 30 cm has been used to characterize carbon content in forest soils in the Czech Republic across all altitudinal vegetation zones and forest ecological series. This data set was used to predict the most probable changes in soil carbon content in the altitudinal vegetation zones due to global warming. The mean value of the SOC content in forest soils of the Czech Republic was determined to be 62.6 ± 17.2 t.ha-1. Under different warming scenarios the major SOC loss was observed at an altitude of 700-900 m a.s.l. Using a pessimistic emission scenario in the climatic model (i.e. predicted temperature change by +4.24°C), losses of C from forest soils in the Czech Republic, or potentially in central Europe, could be as high as 13% of the current carbon stock in forest soils. oxidizable soil carbon content altitudinal vegetation zone ecological series Forestry D. Janouš verfasserin aut M. Pavelka verfasserin aut J. Macků verfasserin aut K. Havránková verfasserin aut K. Rejšek verfasserin aut M.V. Marek verfasserin aut In Journal of Forest Science Czech Academy of Agricultural Sciences, 2015 62(2016), 12, Seite 537-544 (DE-627)387480773 (DE-600)2145663-X 1805935X nnns volume:62 year:2016 number:12 pages:537-544 https://doi.org/10.17221/103/2015-JFS kostenfrei https://doaj.org/article/eb94723c8bcc454aaf750bfa78208186 kostenfrei https://jfs.agriculturejournals.cz/artkey/jfs-201612-0002_potential-changes-in-czech-forest-soil-carbon-stocks-under-different-climate-change-scenarios.php kostenfrei https://doaj.org/toc/1212-4834 Journal toc kostenfrei https://doaj.org/toc/1805-935X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_20 GBV_ILN_22 GBV_ILN_24 GBV_ILN_31 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4367 GBV_ILN_4700 AR 62 2016 12 537-544
allfields_unstemmed	10.17221/103/2015-JFS doi (DE-627)DOAJ082850143 (DE-599)DOAJeb94723c8bcc454aaf750bfa78208186 DE-627 ger DE-627 rakwb eng SD1-669.5 I. Marková verfasserin aut Potential changes in Czech forest soil carbon stocks under different climate change scenarios 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Detailed inventory data (n = 3,930; approximately one representative sampling point per 650 ha) on soil organic carbon (SOC) to a depth of 30 cm has been used to characterize carbon content in forest soils in the Czech Republic across all altitudinal vegetation zones and forest ecological series. This data set was used to predict the most probable changes in soil carbon content in the altitudinal vegetation zones due to global warming. The mean value of the SOC content in forest soils of the Czech Republic was determined to be 62.6 ± 17.2 t.ha-1. Under different warming scenarios the major SOC loss was observed at an altitude of 700-900 m a.s.l. Using a pessimistic emission scenario in the climatic model (i.e. predicted temperature change by +4.24°C), losses of C from forest soils in the Czech Republic, or potentially in central Europe, could be as high as 13% of the current carbon stock in forest soils. oxidizable soil carbon content altitudinal vegetation zone ecological series Forestry D. Janouš verfasserin aut M. Pavelka verfasserin aut J. Macků verfasserin aut K. Havránková verfasserin aut K. Rejšek verfasserin aut M.V. Marek verfasserin aut In Journal of Forest Science Czech Academy of Agricultural Sciences, 2015 62(2016), 12, Seite 537-544 (DE-627)387480773 (DE-600)2145663-X 1805935X nnns volume:62 year:2016 number:12 pages:537-544 https://doi.org/10.17221/103/2015-JFS kostenfrei https://doaj.org/article/eb94723c8bcc454aaf750bfa78208186 kostenfrei https://jfs.agriculturejournals.cz/artkey/jfs-201612-0002_potential-changes-in-czech-forest-soil-carbon-stocks-under-different-climate-change-scenarios.php kostenfrei https://doaj.org/toc/1212-4834 Journal toc kostenfrei https://doaj.org/toc/1805-935X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_20 GBV_ILN_22 GBV_ILN_24 GBV_ILN_31 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4367 GBV_ILN_4700 AR 62 2016 12 537-544
allfieldsGer	10.17221/103/2015-JFS doi (DE-627)DOAJ082850143 (DE-599)DOAJeb94723c8bcc454aaf750bfa78208186 DE-627 ger DE-627 rakwb eng SD1-669.5 I. Marková verfasserin aut Potential changes in Czech forest soil carbon stocks under different climate change scenarios 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Detailed inventory data (n = 3,930; approximately one representative sampling point per 650 ha) on soil organic carbon (SOC) to a depth of 30 cm has been used to characterize carbon content in forest soils in the Czech Republic across all altitudinal vegetation zones and forest ecological series. This data set was used to predict the most probable changes in soil carbon content in the altitudinal vegetation zones due to global warming. The mean value of the SOC content in forest soils of the Czech Republic was determined to be 62.6 ± 17.2 t.ha-1. Under different warming scenarios the major SOC loss was observed at an altitude of 700-900 m a.s.l. Using a pessimistic emission scenario in the climatic model (i.e. predicted temperature change by +4.24°C), losses of C from forest soils in the Czech Republic, or potentially in central Europe, could be as high as 13% of the current carbon stock in forest soils. oxidizable soil carbon content altitudinal vegetation zone ecological series Forestry D. Janouš verfasserin aut M. Pavelka verfasserin aut J. Macků verfasserin aut K. Havránková verfasserin aut K. Rejšek verfasserin aut M.V. Marek verfasserin aut In Journal of Forest Science Czech Academy of Agricultural Sciences, 2015 62(2016), 12, Seite 537-544 (DE-627)387480773 (DE-600)2145663-X 1805935X nnns volume:62 year:2016 number:12 pages:537-544 https://doi.org/10.17221/103/2015-JFS kostenfrei https://doaj.org/article/eb94723c8bcc454aaf750bfa78208186 kostenfrei https://jfs.agriculturejournals.cz/artkey/jfs-201612-0002_potential-changes-in-czech-forest-soil-carbon-stocks-under-different-climate-change-scenarios.php kostenfrei https://doaj.org/toc/1212-4834 Journal toc kostenfrei https://doaj.org/toc/1805-935X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_20 GBV_ILN_22 GBV_ILN_24 GBV_ILN_31 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4367 GBV_ILN_4700 AR 62 2016 12 537-544
allfieldsSound	10.17221/103/2015-JFS doi (DE-627)DOAJ082850143 (DE-599)DOAJeb94723c8bcc454aaf750bfa78208186 DE-627 ger DE-627 rakwb eng SD1-669.5 I. Marková verfasserin aut Potential changes in Czech forest soil carbon stocks under different climate change scenarios 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Detailed inventory data (n = 3,930; approximately one representative sampling point per 650 ha) on soil organic carbon (SOC) to a depth of 30 cm has been used to characterize carbon content in forest soils in the Czech Republic across all altitudinal vegetation zones and forest ecological series. This data set was used to predict the most probable changes in soil carbon content in the altitudinal vegetation zones due to global warming. The mean value of the SOC content in forest soils of the Czech Republic was determined to be 62.6 ± 17.2 t.ha-1. Under different warming scenarios the major SOC loss was observed at an altitude of 700-900 m a.s.l. Using a pessimistic emission scenario in the climatic model (i.e. predicted temperature change by +4.24°C), losses of C from forest soils in the Czech Republic, or potentially in central Europe, could be as high as 13% of the current carbon stock in forest soils. oxidizable soil carbon content altitudinal vegetation zone ecological series Forestry D. Janouš verfasserin aut M. Pavelka verfasserin aut J. Macků verfasserin aut K. Havránková verfasserin aut K. Rejšek verfasserin aut M.V. Marek verfasserin aut In Journal of Forest Science Czech Academy of Agricultural Sciences, 2015 62(2016), 12, Seite 537-544 (DE-627)387480773 (DE-600)2145663-X 1805935X nnns volume:62 year:2016 number:12 pages:537-544 https://doi.org/10.17221/103/2015-JFS kostenfrei https://doaj.org/article/eb94723c8bcc454aaf750bfa78208186 kostenfrei https://jfs.agriculturejournals.cz/artkey/jfs-201612-0002_potential-changes-in-czech-forest-soil-carbon-stocks-under-different-climate-change-scenarios.php kostenfrei https://doaj.org/toc/1212-4834 Journal toc kostenfrei https://doaj.org/toc/1805-935X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_20 GBV_ILN_22 GBV_ILN_24 GBV_ILN_31 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4367 GBV_ILN_4700 AR 62 2016 12 537-544
language	English
source	In Journal of Forest Science 62(2016), 12, Seite 537-544 volume:62 year:2016 number:12 pages:537-544
sourceStr	In Journal of Forest Science 62(2016), 12, Seite 537-544 volume:62 year:2016 number:12 pages:537-544
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	oxidizable soil carbon content altitudinal vegetation zone ecological series Forestry
isfreeaccess_bool	true
container_title	Journal of Forest Science
authorswithroles_txt_mv	I. Marková @@aut@@ D. Janouš @@aut@@ M. Pavelka @@aut@@ J. Macků @@aut@@ K. Havránková @@aut@@ K. Rejšek @@aut@@ M.V. Marek @@aut@@
publishDateDaySort_date	2016-01-01T00:00:00Z
hierarchy_top_id	387480773
id	DOAJ082850143
language_de	englisch
fullrecord	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000naa a22002652 4500</leader><controlfield tag="001">DOAJ082850143</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230311004704.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">230311s2016 xx \|\|\|\|\|o 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.17221/103/2015-JFS</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)DOAJ082850143</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)DOAJeb94723c8bcc454aaf750bfa78208186</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">SD1-669.5</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">I. Marková</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Potential changes in Czech forest soil carbon stocks under different climate change scenarios</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2016</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Detailed inventory data (n = 3,930; approximately one representative sampling point per 650 ha) on soil organic carbon (SOC) to a depth of 30 cm has been used to characterize carbon content in forest soils in the Czech Republic across all altitudinal vegetation zones and forest ecological series. This data set was used to predict the most probable changes in soil carbon content in the altitudinal vegetation zones due to global warming. The mean value of the SOC content in forest soils of the Czech Republic was determined to be 62.6 ± 17.2 t.ha-1. Under different warming scenarios the major SOC loss was observed at an altitude of 700-900 m a.s.l. Using a pessimistic emission scenario in the climatic model (i.e. predicted temperature change by +4.24°C), losses of C from forest soils in the Czech Republic, or potentially in central Europe, could be as high as 13% of the current carbon stock in forest soils.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">oxidizable soil carbon content</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">altitudinal vegetation zone</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">ecological series</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Forestry</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">D. Janouš</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">M. Pavelka</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">J. Macků</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">K. Havránková</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">K. Rejšek</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">M.V. Marek</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">Journal of Forest Science</subfield><subfield code="d">Czech Academy of Agricultural Sciences, 2015</subfield><subfield code="g">62(2016), 12, Seite 537-544</subfield><subfield code="w">(DE-627)387480773</subfield><subfield code="w">(DE-600)2145663-X</subfield><subfield code="x">1805935X</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:62</subfield><subfield code="g">year:2016</subfield><subfield code="g">number:12</subfield><subfield code="g">pages:537-544</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.17221/103/2015-JFS</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doaj.org/article/eb94723c8bcc454aaf750bfa78208186</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://jfs.agriculturejournals.cz/artkey/jfs-201612-0002_potential-changes-in-czech-forest-soil-carbon-stocks-under-different-climate-change-scenarios.php</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/1212-4834</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/1805-935X</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_DOAJ</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_24</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_31</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_39</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_69</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_73</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_95</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_151</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_161</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_213</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_230</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_285</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_293</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_602</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2014</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4125</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4126</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4249</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4306</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4307</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4322</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4323</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4324</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4325</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4367</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4700</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">62</subfield><subfield code="j">2016</subfield><subfield code="e">12</subfield><subfield code="h">537-544</subfield></datafield></record></collection>
callnumber-first	S - Agriculture
author	I. Marková
spellingShingle	I. Marková misc SD1-669.5 misc oxidizable soil carbon content misc altitudinal vegetation zone misc ecological series misc Forestry Potential changes in Czech forest soil carbon stocks under different climate change scenarios
authorStr	I. Marková
ppnlink_with_tag_str_mv	@@773@@(DE-627)387480773
format	electronic Article
delete_txt_mv	keep
author_role	aut aut aut aut aut aut aut
collection	DOAJ
remote_str	true
callnumber-label	SD1-669
illustrated	Not Illustrated
issn	1805935X
topic_title	SD1-669.5 Potential changes in Czech forest soil carbon stocks under different climate change scenarios oxidizable soil carbon content altitudinal vegetation zone ecological series
topic	misc SD1-669.5 misc oxidizable soil carbon content misc altitudinal vegetation zone misc ecological series misc Forestry
topic_unstemmed	misc SD1-669.5 misc oxidizable soil carbon content misc altitudinal vegetation zone misc ecological series misc Forestry
topic_browse	misc SD1-669.5 misc oxidizable soil carbon content misc altitudinal vegetation zone misc ecological series misc Forestry
format_facet	Elektronische Aufsätze Aufsätze Elektronische Ressource
format_main_str_mv	Text Zeitschrift/Artikel
carriertype_str_mv	cr
hierarchy_parent_title	Journal of Forest Science
hierarchy_parent_id	387480773
hierarchy_top_title	Journal of Forest Science
isfreeaccess_txt	true
familylinks_str_mv	(DE-627)387480773 (DE-600)2145663-X
title	Potential changes in Czech forest soil carbon stocks under different climate change scenarios
ctrlnum	(DE-627)DOAJ082850143 (DE-599)DOAJeb94723c8bcc454aaf750bfa78208186
title_full	Potential changes in Czech forest soil carbon stocks under different climate change scenarios
author_sort	I. Marková
journal	Journal of Forest Science
journalStr	Journal of Forest Science
callnumber-first-code	S
lang_code	eng
isOA_bool	true
recordtype	marc
publishDateSort	2016
contenttype_str_mv	txt
container_start_page	537
author_browse	I. Marková D. Janouš M. Pavelka J. Macků K. Havránková K. Rejšek M.V. Marek
container_volume	62
class	SD1-669.5
format_se	Elektronische Aufsätze
author-letter	I. Marková
doi_str_mv	10.17221/103/2015-JFS
author2-role	verfasserin
title_sort	potential changes in czech forest soil carbon stocks under different climate change scenarios
callnumber	SD1-669.5
title_auth	Potential changes in Czech forest soil carbon stocks under different climate change scenarios
abstract	Detailed inventory data (n = 3,930; approximately one representative sampling point per 650 ha) on soil organic carbon (SOC) to a depth of 30 cm has been used to characterize carbon content in forest soils in the Czech Republic across all altitudinal vegetation zones and forest ecological series. This data set was used to predict the most probable changes in soil carbon content in the altitudinal vegetation zones due to global warming. The mean value of the SOC content in forest soils of the Czech Republic was determined to be 62.6 ± 17.2 t.ha-1. Under different warming scenarios the major SOC loss was observed at an altitude of 700-900 m a.s.l. Using a pessimistic emission scenario in the climatic model (i.e. predicted temperature change by +4.24°C), losses of C from forest soils in the Czech Republic, or potentially in central Europe, could be as high as 13% of the current carbon stock in forest soils.
abstractGer	Detailed inventory data (n = 3,930; approximately one representative sampling point per 650 ha) on soil organic carbon (SOC) to a depth of 30 cm has been used to characterize carbon content in forest soils in the Czech Republic across all altitudinal vegetation zones and forest ecological series. This data set was used to predict the most probable changes in soil carbon content in the altitudinal vegetation zones due to global warming. The mean value of the SOC content in forest soils of the Czech Republic was determined to be 62.6 ± 17.2 t.ha-1. Under different warming scenarios the major SOC loss was observed at an altitude of 700-900 m a.s.l. Using a pessimistic emission scenario in the climatic model (i.e. predicted temperature change by +4.24°C), losses of C from forest soils in the Czech Republic, or potentially in central Europe, could be as high as 13% of the current carbon stock in forest soils.
abstract_unstemmed	Detailed inventory data (n = 3,930; approximately one representative sampling point per 650 ha) on soil organic carbon (SOC) to a depth of 30 cm has been used to characterize carbon content in forest soils in the Czech Republic across all altitudinal vegetation zones and forest ecological series. This data set was used to predict the most probable changes in soil carbon content in the altitudinal vegetation zones due to global warming. The mean value of the SOC content in forest soils of the Czech Republic was determined to be 62.6 ± 17.2 t.ha-1. Under different warming scenarios the major SOC loss was observed at an altitude of 700-900 m a.s.l. Using a pessimistic emission scenario in the climatic model (i.e. predicted temperature change by +4.24°C), losses of C from forest soils in the Czech Republic, or potentially in central Europe, could be as high as 13% of the current carbon stock in forest soils.
collection_details	GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_20 GBV_ILN_22 GBV_ILN_24 GBV_ILN_31 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4367 GBV_ILN_4700
container_issue	12
title_short	Potential changes in Czech forest soil carbon stocks under different climate change scenarios
url	https://doi.org/10.17221/103/2015-JFS https://doaj.org/article/eb94723c8bcc454aaf750bfa78208186 https://jfs.agriculturejournals.cz/artkey/jfs-201612-0002_potential-changes-in-czech-forest-soil-carbon-stocks-under-different-climate-change-scenarios.php https://doaj.org/toc/1212-4834 https://doaj.org/toc/1805-935X
remote_bool	true
author2	D. Janouš M. Pavelka J. Macků K. Havránková K. Rejšek M.V. Marek
author2Str	D. Janouš M. Pavelka J. Macků K. Havránková K. Rejšek M.V. Marek
ppnlink	387480773
callnumber-subject	SD - Forestry
mediatype_str_mv	c
isOA_txt	true
hochschulschrift_bool	false
doi_str	10.17221/103/2015-JFS
callnumber-a	SD1-669.5
up_date	2024-07-03T14:10:24.220Z
_version_	1803567312898359296
fullrecord_marcxml	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000naa a22002652 4500</leader><controlfield tag="001">DOAJ082850143</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230311004704.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">230311s2016 xx \|\|\|\|\|o 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.17221/103/2015-JFS</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)DOAJ082850143</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)DOAJeb94723c8bcc454aaf750bfa78208186</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">SD1-669.5</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">I. Marková</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Potential changes in Czech forest soil carbon stocks under different climate change scenarios</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2016</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Detailed inventory data (n = 3,930; approximately one representative sampling point per 650 ha) on soil organic carbon (SOC) to a depth of 30 cm has been used to characterize carbon content in forest soils in the Czech Republic across all altitudinal vegetation zones and forest ecological series. This data set was used to predict the most probable changes in soil carbon content in the altitudinal vegetation zones due to global warming. The mean value of the SOC content in forest soils of the Czech Republic was determined to be 62.6 ± 17.2 t.ha-1. Under different warming scenarios the major SOC loss was observed at an altitude of 700-900 m a.s.l. Using a pessimistic emission scenario in the climatic model (i.e. predicted temperature change by +4.24°C), losses of C from forest soils in the Czech Republic, or potentially in central Europe, could be as high as 13% of the current carbon stock in forest soils.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">oxidizable soil carbon content</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">altitudinal vegetation zone</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">ecological series</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Forestry</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">D. Janouš</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">M. Pavelka</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">J. Macků</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">K. Havránková</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">K. Rejšek</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">M.V. Marek</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">Journal of Forest Science</subfield><subfield code="d">Czech Academy of Agricultural Sciences, 2015</subfield><subfield code="g">62(2016), 12, Seite 537-544</subfield><subfield code="w">(DE-627)387480773</subfield><subfield code="w">(DE-600)2145663-X</subfield><subfield code="x">1805935X</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:62</subfield><subfield code="g">year:2016</subfield><subfield code="g">number:12</subfield><subfield code="g">pages:537-544</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.17221/103/2015-JFS</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doaj.org/article/eb94723c8bcc454aaf750bfa78208186</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://jfs.agriculturejournals.cz/artkey/jfs-201612-0002_potential-changes-in-czech-forest-soil-carbon-stocks-under-different-climate-change-scenarios.php</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/1212-4834</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/1805-935X</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_DOAJ</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_24</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_31</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_39</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_69</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_73</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_95</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_151</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_161</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_213</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_230</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_285</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_293</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_602</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2014</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4125</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4126</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4249</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4306</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4307</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4322</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4323</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4324</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4325</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4367</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4700</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">62</subfield><subfield code="j">2016</subfield><subfield code="e">12</subfield><subfield code="h">537-544</subfield></datafield></record></collection>
score	7.39818

Nicht das Richtige dabei?

Schreiben Sie uns!

Potential changes in Czech forest soil carbon stocks under different climate change scenarios

Nicht das Richtige dabei?

Zugang & Verfügbarkeit

Vorhandene Bände

Nicht das Richtige dabei?