Changes in ecosystem carbon stocks in a grassland ash (Fraxinus excelsior) afforestation chronosequence in Ireland

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TY  - JOUR
  - Wellock, ML,Rafique, R,LaPerle, CM,Peichl, M,Kiely, G
  - 2014
  - October
  - Journal Of Plant Ecology
  - Changes in ecosystem carbon stocks in a grassland ash (Fraxinus excelsior) afforestation chronosequence in Ireland
  - Validated
  - WOS: 10 ()
  - ash (Fraxinus excelsior L.) chronosequence soil biomass carbon ecosystem SOIL ORGANIC-CARBON SPRUCE PICEA-SITCHENSIS REPUBLIC-OF-IRELAND LAND-USE CHANGE AGRICULTURAL SOILS FOREST MANAGEMENT EASTERN PREALPS META ANALYSIS NEW-ZEALAND PEATY GLEY
  - 7
  - 429
  - 438
  - AimsGovernment policy in Ireland is to increase the national forest cover from the current 10% to 18% of the total land area by 2020. This represents a major land use change that is expected to impact on the national carbon (C) stocks. While the C stocks of ecosystem biomass and soils of Irish grasslands and coniferous forests have been quantified, little work has been done to assess the impact of broadleaf afforestation on C stocks.MethodsIn this study, we sampled a chronosequence of ash (Fraxinus excelsior) forests aged 12, 20, 27, 40 and 47 years on brown earth soils. A grassland site, representative of the pre-afforestation land use, was sampled as a control.Important FindingsOur results show that there was a significant decline (P < 0.05) in the carbon density of the soil (0-30 cm) following afforestation from the grassland (90.2 Mg C ha(-1)) to the 27-year-old forest (66.7 Mg C ha(-1)). Subsequently, the forest soils switched from being a C source to a C sink and began to sequester C to 71.3 Mg C ha(-1) at the 47-year-old forest. We found the amount of C stored in the above- and belowground biomass increased with age of the forest stands and offset the amount of C lost from the soil. The amount of C stored in the above-and belowground biomass increased on average by 1.83 Mg C ha(-1) year(-1). The increased storage of C in the biomass led to an increase in the total ecosystem C, from 90.2 Mg C ha(-1) at the grassland site to 162.6 Mg C ha(-1) at the 47-year-old forest. On a national scale, projected rates of ash afforestation to the year 2020 may cause a loss of 290 752 Mg C from the soil compared to 2 525 936 Mg C sequestered into the tree biomass. The effects of harvesting and reforestation may further modify the development of ecosystem C stocks over an entire ash rotation.
  - 10.1093/jpe/rtt060
DA  - 2014/10
ER  - 
@article{V279269066,
   = {Wellock,  ML and Rafique,  R and LaPerle,  CM and Peichl,  M and Kiely,  G },
   = {2014},
   = {October},
   = {Journal Of Plant Ecology},
   = {Changes in ecosystem carbon stocks in a grassland ash (Fraxinus excelsior) afforestation chronosequence in Ireland},
   = {Validated},
   = {WOS: 10 ()},
   = {ash (Fraxinus excelsior L.) chronosequence soil biomass carbon ecosystem SOIL ORGANIC-CARBON SPRUCE PICEA-SITCHENSIS REPUBLIC-OF-IRELAND LAND-USE CHANGE AGRICULTURAL SOILS FOREST MANAGEMENT EASTERN PREALPS META ANALYSIS NEW-ZEALAND PEATY GLEY},
   = {7},
  pages = {429--438},
   = {{AimsGovernment policy in Ireland is to increase the national forest cover from the current 10% to 18% of the total land area by 2020. This represents a major land use change that is expected to impact on the national carbon (C) stocks. While the C stocks of ecosystem biomass and soils of Irish grasslands and coniferous forests have been quantified, little work has been done to assess the impact of broadleaf afforestation on C stocks.MethodsIn this study, we sampled a chronosequence of ash (Fraxinus excelsior) forests aged 12, 20, 27, 40 and 47 years on brown earth soils. A grassland site, representative of the pre-afforestation land use, was sampled as a control.Important FindingsOur results show that there was a significant decline (P < 0.05) in the carbon density of the soil (0-30 cm) following afforestation from the grassland (90.2 Mg C ha(-1)) to the 27-year-old forest (66.7 Mg C ha(-1)). Subsequently, the forest soils switched from being a C source to a C sink and began to sequester C to 71.3 Mg C ha(-1) at the 47-year-old forest. We found the amount of C stored in the above- and belowground biomass increased with age of the forest stands and offset the amount of C lost from the soil. The amount of C stored in the above-and belowground biomass increased on average by 1.83 Mg C ha(-1) year(-1). The increased storage of C in the biomass led to an increase in the total ecosystem C, from 90.2 Mg C ha(-1) at the grassland site to 162.6 Mg C ha(-1) at the 47-year-old forest. On a national scale, projected rates of ash afforestation to the year 2020 may cause a loss of 290 752 Mg C from the soil compared to 2 525 936 Mg C sequestered into the tree biomass. The effects of harvesting and reforestation may further modify the development of ecosystem C stocks over an entire ash rotation.}},
   = {10.1093/jpe/rtt060},
  source = {IRIS}
}
AUTHORSWellock, ML,Rafique, R,LaPerle, CM,Peichl, M,Kiely, G
YEAR2014
MONTHOctober
JOURNAL_CODEJournal Of Plant Ecology
TITLEChanges in ecosystem carbon stocks in a grassland ash (Fraxinus excelsior) afforestation chronosequence in Ireland
STATUSValidated
TIMES_CITEDWOS: 10 ()
SEARCH_KEYWORDash (Fraxinus excelsior L.) chronosequence soil biomass carbon ecosystem SOIL ORGANIC-CARBON SPRUCE PICEA-SITCHENSIS REPUBLIC-OF-IRELAND LAND-USE CHANGE AGRICULTURAL SOILS FOREST MANAGEMENT EASTERN PREALPS META ANALYSIS NEW-ZEALAND PEATY GLEY
VOLUME7
ISSUE
START_PAGE429
END_PAGE438
ABSTRACTAimsGovernment policy in Ireland is to increase the national forest cover from the current 10% to 18% of the total land area by 2020. This represents a major land use change that is expected to impact on the national carbon (C) stocks. While the C stocks of ecosystem biomass and soils of Irish grasslands and coniferous forests have been quantified, little work has been done to assess the impact of broadleaf afforestation on C stocks.MethodsIn this study, we sampled a chronosequence of ash (Fraxinus excelsior) forests aged 12, 20, 27, 40 and 47 years on brown earth soils. A grassland site, representative of the pre-afforestation land use, was sampled as a control.Important FindingsOur results show that there was a significant decline (P < 0.05) in the carbon density of the soil (0-30 cm) following afforestation from the grassland (90.2 Mg C ha(-1)) to the 27-year-old forest (66.7 Mg C ha(-1)). Subsequently, the forest soils switched from being a C source to a C sink and began to sequester C to 71.3 Mg C ha(-1) at the 47-year-old forest. We found the amount of C stored in the above- and belowground biomass increased with age of the forest stands and offset the amount of C lost from the soil. The amount of C stored in the above-and belowground biomass increased on average by 1.83 Mg C ha(-1) year(-1). The increased storage of C in the biomass led to an increase in the total ecosystem C, from 90.2 Mg C ha(-1) at the grassland site to 162.6 Mg C ha(-1) at the 47-year-old forest. On a national scale, projected rates of ash afforestation to the year 2020 may cause a loss of 290 752 Mg C from the soil compared to 2 525 936 Mg C sequestered into the tree biomass. The effects of harvesting and reforestation may further modify the development of ecosystem C stocks over an entire ash rotation.
PUBLISHER_LOCATION
ISBN_ISSN
EDITION
URL
DOI_LINK10.1093/jpe/rtt060
FUNDING_BODY
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