The Long-Term Effects of Wildfire and Post-Fire Vegetation on Sierra Nevada Forest Soils

This paper compares carbon (C) and nutrient contents in soils (Alfisols derived from andesite), forest floor and vegetation in a former fire (1960) and an adjacent forest in the Sagehen Watershed in the Sierra Nevada Mountains of California. Soils from the former fire (now occupied predominantly by Ceanothus velutinus, a nitrogen-fixing shrub) had significantly lower contents of extractable SO42− and P (both Bray and bicarbonate) but significantly greater contents of exchangeable Ca2+ than the adjacent forested site (dominated by Pinus jeffreyii). 15N data suggested that N fixation had occurred in the former fire site, but N contents did not differ between the two sites. O horizon C and nutrient contents did not differ between the two sites, but vegetation C and nutrient contents were significantly greater in the forested than former fire site. These results contrast with those from a nearby, previous study at Little Valley Nevada, also dominated by P. jeffreyii growing on a different soil type (Entisols derived from granite). In the Little Valley study, soil C, N, Ca2+, Mg2+, and K+ contents within the former fire (1981, now also occupied predominantly by Ceanothus velutinus) were greater than in the adjacent forest (Pinus jeffreyii) but soil extractable P contents either did not differ or were greater in the former fire. We conclude that soil parent material is an indirect but strong mediator of the effects of post-fire vegetation on soils in this region, especially with respect to soil P changes, which vary substantially between andesite- and granite-derived soils. Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Watkins W. Miller [verfasserIn] Benjamin M. Rau [verfasserIn] Michelle McNulty [verfasserIn] Roger F. Walker [verfasserIn] Dale W. Johnson [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2012

Schlagwörter:	carbon long-term N-fixation nutrients soils vegetation wildfire

Übergeordnetes Werk:	In: Forests - MDPI AG, 2010, 3(2012), 2, Seite 398-416
Übergeordnetes Werk:	volume:3 ; year:2012 ; number:2 ; pages:398-416

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.3390/f3020398

Katalog-ID:	DOAJ022226788

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allfields	10.3390/f3020398 doi (DE-627)DOAJ022226788 (DE-599)DOAJ911868f8e5e84a3193e468065a92280a DE-627 ger DE-627 rakwb eng QK900-989 Watkins W. Miller verfasserin aut The Long-Term Effects of Wildfire and Post-Fire Vegetation on Sierra Nevada Forest Soils 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier This paper compares carbon (C) and nutrient contents in soils (Alfisols derived from andesite), forest floor and vegetation in a former fire (1960) and an adjacent forest in the Sagehen Watershed in the Sierra Nevada Mountains of California. Soils from the former fire (now occupied predominantly by <em>Ceanothus velutinus</em>, a nitrogen-fixing shrub) had significantly lower contents of extractable SO<sub>4</sub><sup>2</sup><sup>−</sup> and P (both Bray and bicarbonate) but significantly greater contents of exchangeable Ca<sup>2</sup><sup>+</sup> than the adjacent forested site (dominated by <em>Pinus jeffreyii</em>). <sup>15</sup>N data suggested that N fixation had occurred in the former fire site, but N contents did not differ between the two sites. O horizon C and nutrient contents did not differ between the two sites, but vegetation C and nutrient contents were significantly greater in the forested than former fire site. These results contrast with those from a nearby, previous study at Little Valley Nevada, also dominated by <em>P. jeffreyii</em> growing on a different soil type (Entisols derived from granite). In the Little Valley study, soil C, N, Ca<sup>2</sup><sup>+</sup>, Mg<sup>2</sup><sup>+</sup>, and K<sup>+</sup> contents within the former fire (1981, now also occupied predominantly by <em>Ceanothus velutinus</em>) were greater than in the adjacent forest (<em>Pinus jeffreyii</em>) but soil extractable P contents either did not differ or were greater in the former fire. We conclude that soil parent material is an indirect but strong mediator of the effects of post-fire vegetation on soils in this region, especially with respect to soil P changes, which vary substantially between andesite- and granite-derived soils. carbon long-term N-fixation nutrients soils vegetation wildfire Plant ecology Benjamin M. Rau verfasserin aut Michelle McNulty verfasserin aut Roger F. Walker verfasserin aut Dale W. Johnson verfasserin aut In Forests MDPI AG, 2010 3(2012), 2, Seite 398-416 (DE-627)614095689 (DE-600)2527081-3 19994907 nnns volume:3 year:2012 number:2 pages:398-416 https://doi.org/10.3390/f3020398 kostenfrei https://doaj.org/article/911868f8e5e84a3193e468065a92280a kostenfrei http://www.mdpi.com/1999-4907/3/2/398 kostenfrei https://doaj.org/toc/1999-4907 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 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_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 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 3 2012 2 398-416
spelling	10.3390/f3020398 doi (DE-627)DOAJ022226788 (DE-599)DOAJ911868f8e5e84a3193e468065a92280a DE-627 ger DE-627 rakwb eng QK900-989 Watkins W. Miller verfasserin aut The Long-Term Effects of Wildfire and Post-Fire Vegetation on Sierra Nevada Forest Soils 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier This paper compares carbon (C) and nutrient contents in soils (Alfisols derived from andesite), forest floor and vegetation in a former fire (1960) and an adjacent forest in the Sagehen Watershed in the Sierra Nevada Mountains of California. Soils from the former fire (now occupied predominantly by <em>Ceanothus velutinus</em>, a nitrogen-fixing shrub) had significantly lower contents of extractable SO<sub>4</sub><sup>2</sup><sup>−</sup> and P (both Bray and bicarbonate) but significantly greater contents of exchangeable Ca<sup>2</sup><sup>+</sup> than the adjacent forested site (dominated by <em>Pinus jeffreyii</em>). <sup>15</sup>N data suggested that N fixation had occurred in the former fire site, but N contents did not differ between the two sites. O horizon C and nutrient contents did not differ between the two sites, but vegetation C and nutrient contents were significantly greater in the forested than former fire site. These results contrast with those from a nearby, previous study at Little Valley Nevada, also dominated by <em>P. jeffreyii</em> growing on a different soil type (Entisols derived from granite). In the Little Valley study, soil C, N, Ca<sup>2</sup><sup>+</sup>, Mg<sup>2</sup><sup>+</sup>, and K<sup>+</sup> contents within the former fire (1981, now also occupied predominantly by <em>Ceanothus velutinus</em>) were greater than in the adjacent forest (<em>Pinus jeffreyii</em>) but soil extractable P contents either did not differ or were greater in the former fire. We conclude that soil parent material is an indirect but strong mediator of the effects of post-fire vegetation on soils in this region, especially with respect to soil P changes, which vary substantially between andesite- and granite-derived soils. carbon long-term N-fixation nutrients soils vegetation wildfire Plant ecology Benjamin M. Rau verfasserin aut Michelle McNulty verfasserin aut Roger F. Walker verfasserin aut Dale W. Johnson verfasserin aut In Forests MDPI AG, 2010 3(2012), 2, Seite 398-416 (DE-627)614095689 (DE-600)2527081-3 19994907 nnns volume:3 year:2012 number:2 pages:398-416 https://doi.org/10.3390/f3020398 kostenfrei https://doaj.org/article/911868f8e5e84a3193e468065a92280a kostenfrei http://www.mdpi.com/1999-4907/3/2/398 kostenfrei https://doaj.org/toc/1999-4907 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 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_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 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 3 2012 2 398-416
allfields_unstemmed	10.3390/f3020398 doi (DE-627)DOAJ022226788 (DE-599)DOAJ911868f8e5e84a3193e468065a92280a DE-627 ger DE-627 rakwb eng QK900-989 Watkins W. Miller verfasserin aut The Long-Term Effects of Wildfire and Post-Fire Vegetation on Sierra Nevada Forest Soils 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier This paper compares carbon (C) and nutrient contents in soils (Alfisols derived from andesite), forest floor and vegetation in a former fire (1960) and an adjacent forest in the Sagehen Watershed in the Sierra Nevada Mountains of California. Soils from the former fire (now occupied predominantly by <em>Ceanothus velutinus</em>, a nitrogen-fixing shrub) had significantly lower contents of extractable SO<sub>4</sub><sup>2</sup><sup>−</sup> and P (both Bray and bicarbonate) but significantly greater contents of exchangeable Ca<sup>2</sup><sup>+</sup> than the adjacent forested site (dominated by <em>Pinus jeffreyii</em>). <sup>15</sup>N data suggested that N fixation had occurred in the former fire site, but N contents did not differ between the two sites. O horizon C and nutrient contents did not differ between the two sites, but vegetation C and nutrient contents were significantly greater in the forested than former fire site. These results contrast with those from a nearby, previous study at Little Valley Nevada, also dominated by <em>P. jeffreyii</em> growing on a different soil type (Entisols derived from granite). In the Little Valley study, soil C, N, Ca<sup>2</sup><sup>+</sup>, Mg<sup>2</sup><sup>+</sup>, and K<sup>+</sup> contents within the former fire (1981, now also occupied predominantly by <em>Ceanothus velutinus</em>) were greater than in the adjacent forest (<em>Pinus jeffreyii</em>) but soil extractable P contents either did not differ or were greater in the former fire. We conclude that soil parent material is an indirect but strong mediator of the effects of post-fire vegetation on soils in this region, especially with respect to soil P changes, which vary substantially between andesite- and granite-derived soils. carbon long-term N-fixation nutrients soils vegetation wildfire Plant ecology Benjamin M. Rau verfasserin aut Michelle McNulty verfasserin aut Roger F. Walker verfasserin aut Dale W. Johnson verfasserin aut In Forests MDPI AG, 2010 3(2012), 2, Seite 398-416 (DE-627)614095689 (DE-600)2527081-3 19994907 nnns volume:3 year:2012 number:2 pages:398-416 https://doi.org/10.3390/f3020398 kostenfrei https://doaj.org/article/911868f8e5e84a3193e468065a92280a kostenfrei http://www.mdpi.com/1999-4907/3/2/398 kostenfrei https://doaj.org/toc/1999-4907 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 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_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 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 3 2012 2 398-416
allfieldsGer	10.3390/f3020398 doi (DE-627)DOAJ022226788 (DE-599)DOAJ911868f8e5e84a3193e468065a92280a DE-627 ger DE-627 rakwb eng QK900-989 Watkins W. Miller verfasserin aut The Long-Term Effects of Wildfire and Post-Fire Vegetation on Sierra Nevada Forest Soils 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier This paper compares carbon (C) and nutrient contents in soils (Alfisols derived from andesite), forest floor and vegetation in a former fire (1960) and an adjacent forest in the Sagehen Watershed in the Sierra Nevada Mountains of California. Soils from the former fire (now occupied predominantly by <em>Ceanothus velutinus</em>, a nitrogen-fixing shrub) had significantly lower contents of extractable SO<sub>4</sub><sup>2</sup><sup>−</sup> and P (both Bray and bicarbonate) but significantly greater contents of exchangeable Ca<sup>2</sup><sup>+</sup> than the adjacent forested site (dominated by <em>Pinus jeffreyii</em>). <sup>15</sup>N data suggested that N fixation had occurred in the former fire site, but N contents did not differ between the two sites. O horizon C and nutrient contents did not differ between the two sites, but vegetation C and nutrient contents were significantly greater in the forested than former fire site. These results contrast with those from a nearby, previous study at Little Valley Nevada, also dominated by <em>P. jeffreyii</em> growing on a different soil type (Entisols derived from granite). In the Little Valley study, soil C, N, Ca<sup>2</sup><sup>+</sup>, Mg<sup>2</sup><sup>+</sup>, and K<sup>+</sup> contents within the former fire (1981, now also occupied predominantly by <em>Ceanothus velutinus</em>) were greater than in the adjacent forest (<em>Pinus jeffreyii</em>) but soil extractable P contents either did not differ or were greater in the former fire. We conclude that soil parent material is an indirect but strong mediator of the effects of post-fire vegetation on soils in this region, especially with respect to soil P changes, which vary substantially between andesite- and granite-derived soils. carbon long-term N-fixation nutrients soils vegetation wildfire Plant ecology Benjamin M. Rau verfasserin aut Michelle McNulty verfasserin aut Roger F. Walker verfasserin aut Dale W. Johnson verfasserin aut In Forests MDPI AG, 2010 3(2012), 2, Seite 398-416 (DE-627)614095689 (DE-600)2527081-3 19994907 nnns volume:3 year:2012 number:2 pages:398-416 https://doi.org/10.3390/f3020398 kostenfrei https://doaj.org/article/911868f8e5e84a3193e468065a92280a kostenfrei http://www.mdpi.com/1999-4907/3/2/398 kostenfrei https://doaj.org/toc/1999-4907 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 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_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 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 3 2012 2 398-416
allfieldsSound	10.3390/f3020398 doi (DE-627)DOAJ022226788 (DE-599)DOAJ911868f8e5e84a3193e468065a92280a DE-627 ger DE-627 rakwb eng QK900-989 Watkins W. Miller verfasserin aut The Long-Term Effects of Wildfire and Post-Fire Vegetation on Sierra Nevada Forest Soils 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier This paper compares carbon (C) and nutrient contents in soils (Alfisols derived from andesite), forest floor and vegetation in a former fire (1960) and an adjacent forest in the Sagehen Watershed in the Sierra Nevada Mountains of California. Soils from the former fire (now occupied predominantly by <em>Ceanothus velutinus</em>, a nitrogen-fixing shrub) had significantly lower contents of extractable SO<sub>4</sub><sup>2</sup><sup>−</sup> and P (both Bray and bicarbonate) but significantly greater contents of exchangeable Ca<sup>2</sup><sup>+</sup> than the adjacent forested site (dominated by <em>Pinus jeffreyii</em>). <sup>15</sup>N data suggested that N fixation had occurred in the former fire site, but N contents did not differ between the two sites. O horizon C and nutrient contents did not differ between the two sites, but vegetation C and nutrient contents were significantly greater in the forested than former fire site. These results contrast with those from a nearby, previous study at Little Valley Nevada, also dominated by <em>P. jeffreyii</em> growing on a different soil type (Entisols derived from granite). In the Little Valley study, soil C, N, Ca<sup>2</sup><sup>+</sup>, Mg<sup>2</sup><sup>+</sup>, and K<sup>+</sup> contents within the former fire (1981, now also occupied predominantly by <em>Ceanothus velutinus</em>) were greater than in the adjacent forest (<em>Pinus jeffreyii</em>) but soil extractable P contents either did not differ or were greater in the former fire. We conclude that soil parent material is an indirect but strong mediator of the effects of post-fire vegetation on soils in this region, especially with respect to soil P changes, which vary substantially between andesite- and granite-derived soils. carbon long-term N-fixation nutrients soils vegetation wildfire Plant ecology Benjamin M. Rau verfasserin aut Michelle McNulty verfasserin aut Roger F. Walker verfasserin aut Dale W. Johnson verfasserin aut In Forests MDPI AG, 2010 3(2012), 2, Seite 398-416 (DE-627)614095689 (DE-600)2527081-3 19994907 nnns volume:3 year:2012 number:2 pages:398-416 https://doi.org/10.3390/f3020398 kostenfrei https://doaj.org/article/911868f8e5e84a3193e468065a92280a kostenfrei http://www.mdpi.com/1999-4907/3/2/398 kostenfrei https://doaj.org/toc/1999-4907 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 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_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 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 3 2012 2 398-416
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topic_title	QK900-989 The Long-Term Effects of Wildfire and Post-Fire Vegetation on Sierra Nevada Forest Soils carbon long-term N-fixation nutrients soils vegetation wildfire
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title	The Long-Term Effects of Wildfire and Post-Fire Vegetation on Sierra Nevada Forest Soils
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title_full	The Long-Term Effects of Wildfire and Post-Fire Vegetation on Sierra Nevada Forest Soils
author_sort	Watkins W. Miller
journal	Forests
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author_browse	Watkins W. Miller Benjamin M. Rau Michelle McNulty Roger F. Walker Dale W. Johnson
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title_sort	long-term effects of wildfire and post-fire vegetation on sierra nevada forest soils
callnumber	QK900-989
title_auth	The Long-Term Effects of Wildfire and Post-Fire Vegetation on Sierra Nevada Forest Soils
abstract	This paper compares carbon (C) and nutrient contents in soils (Alfisols derived from andesite), forest floor and vegetation in a former fire (1960) and an adjacent forest in the Sagehen Watershed in the Sierra Nevada Mountains of California. Soils from the former fire (now occupied predominantly by <em>Ceanothus velutinus</em>, a nitrogen-fixing shrub) had significantly lower contents of extractable SO<sub>4</sub><sup>2</sup><sup>−</sup> and P (both Bray and bicarbonate) but significantly greater contents of exchangeable Ca<sup>2</sup><sup>+</sup> than the adjacent forested site (dominated by <em>Pinus jeffreyii</em>). <sup>15</sup>N data suggested that N fixation had occurred in the former fire site, but N contents did not differ between the two sites. O horizon C and nutrient contents did not differ between the two sites, but vegetation C and nutrient contents were significantly greater in the forested than former fire site. These results contrast with those from a nearby, previous study at Little Valley Nevada, also dominated by <em>P. jeffreyii</em> growing on a different soil type (Entisols derived from granite). In the Little Valley study, soil C, N, Ca<sup>2</sup><sup>+</sup>, Mg<sup>2</sup><sup>+</sup>, and K<sup>+</sup> contents within the former fire (1981, now also occupied predominantly by <em>Ceanothus velutinus</em>) were greater than in the adjacent forest (<em>Pinus jeffreyii</em>) but soil extractable P contents either did not differ or were greater in the former fire. We conclude that soil parent material is an indirect but strong mediator of the effects of post-fire vegetation on soils in this region, especially with respect to soil P changes, which vary substantially between andesite- and granite-derived soils.
abstractGer	This paper compares carbon (C) and nutrient contents in soils (Alfisols derived from andesite), forest floor and vegetation in a former fire (1960) and an adjacent forest in the Sagehen Watershed in the Sierra Nevada Mountains of California. Soils from the former fire (now occupied predominantly by <em>Ceanothus velutinus</em>, a nitrogen-fixing shrub) had significantly lower contents of extractable SO<sub>4</sub><sup>2</sup><sup>−</sup> and P (both Bray and bicarbonate) but significantly greater contents of exchangeable Ca<sup>2</sup><sup>+</sup> than the adjacent forested site (dominated by <em>Pinus jeffreyii</em>). <sup>15</sup>N data suggested that N fixation had occurred in the former fire site, but N contents did not differ between the two sites. O horizon C and nutrient contents did not differ between the two sites, but vegetation C and nutrient contents were significantly greater in the forested than former fire site. These results contrast with those from a nearby, previous study at Little Valley Nevada, also dominated by <em>P. jeffreyii</em> growing on a different soil type (Entisols derived from granite). In the Little Valley study, soil C, N, Ca<sup>2</sup><sup>+</sup>, Mg<sup>2</sup><sup>+</sup>, and K<sup>+</sup> contents within the former fire (1981, now also occupied predominantly by <em>Ceanothus velutinus</em>) were greater than in the adjacent forest (<em>Pinus jeffreyii</em>) but soil extractable P contents either did not differ or were greater in the former fire. We conclude that soil parent material is an indirect but strong mediator of the effects of post-fire vegetation on soils in this region, especially with respect to soil P changes, which vary substantially between andesite- and granite-derived soils.
abstract_unstemmed	This paper compares carbon (C) and nutrient contents in soils (Alfisols derived from andesite), forest floor and vegetation in a former fire (1960) and an adjacent forest in the Sagehen Watershed in the Sierra Nevada Mountains of California. Soils from the former fire (now occupied predominantly by <em>Ceanothus velutinus</em>, a nitrogen-fixing shrub) had significantly lower contents of extractable SO<sub>4</sub><sup>2</sup><sup>−</sup> and P (both Bray and bicarbonate) but significantly greater contents of exchangeable Ca<sup>2</sup><sup>+</sup> than the adjacent forested site (dominated by <em>Pinus jeffreyii</em>). <sup>15</sup>N data suggested that N fixation had occurred in the former fire site, but N contents did not differ between the two sites. O horizon C and nutrient contents did not differ between the two sites, but vegetation C and nutrient contents were significantly greater in the forested than former fire site. These results contrast with those from a nearby, previous study at Little Valley Nevada, also dominated by <em>P. jeffreyii</em> growing on a different soil type (Entisols derived from granite). In the Little Valley study, soil C, N, Ca<sup>2</sup><sup>+</sup>, Mg<sup>2</sup><sup>+</sup>, and K<sup>+</sup> contents within the former fire (1981, now also occupied predominantly by <em>Ceanothus velutinus</em>) were greater than in the adjacent forest (<em>Pinus jeffreyii</em>) but soil extractable P contents either did not differ or were greater in the former fire. We conclude that soil parent material is an indirect but strong mediator of the effects of post-fire vegetation on soils in this region, especially with respect to soil P changes, which vary substantially between andesite- and granite-derived soils.
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title_short	The Long-Term Effects of Wildfire and Post-Fire Vegetation on Sierra Nevada Forest Soils
url	https://doi.org/10.3390/f3020398 https://doaj.org/article/911868f8e5e84a3193e468065a92280a http://www.mdpi.com/1999-4907/3/2/398 https://doaj.org/toc/1999-4907
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author2	Benjamin M. Rau Michelle McNulty Roger F. Walker Dale W. Johnson
author2Str	Benjamin M. Rau Michelle McNulty Roger F. Walker Dale W. Johnson
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