IRIS publication 279269066
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 -
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@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} }
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AUTHORS | Wellock, ML,Rafique, R,LaPerle, CM,Peichl, M,Kiely, G | ||
YEAR | 2014 | ||
MONTH | October | ||
JOURNAL_CODE | Journal Of Plant Ecology | ||
TITLE | Changes in ecosystem carbon stocks in a grassland ash (Fraxinus excelsior) afforestation chronosequence in Ireland | ||
STATUS | Validated | ||
TIMES_CITED | WOS: 10 () | ||
SEARCH_KEYWORD | 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 | ||
VOLUME | 7 | ||
ISSUE | |||
START_PAGE | 429 | ||
END_PAGE | 438 | ||
ABSTRACT | 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. | ||
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DOI_LINK | 10.1093/jpe/rtt060 | ||
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