Abstract
Grassland abandonment followed by progressive forest expansion is the dominant land-use change in the European Alps. Contrasting trends in soil organic carbon (SOC) stocks have been reported for mountainous regions following forest expansion on grasslands. Moreover, its effects on SOC properties involved into long-term stability are largely unknown. The aim of this PhD thesis was to explore changes in: (i) SOC stocks; (ii) physical SOC fractions; and (iii) labile soil carbon components following forest expansion on mountain grasslands.
A land-use gradient located in the Southern Alps (Italy) was examined, comprising managed grassland, two transitional phases in which grassland abandonment led to colonization by Picea abies (L.) Karst., and old forest dominated by Fagus sylvatica L. and P. abies. Mineral soil samples were physically separated through aggregate size and size-density fractionation. Changes in labile soil C were assessed by carbohydrate and thermal analyses of soil samples and fractions.
Forest expansion on mountain grasslands caused a decrease in SOC stocks within the mineral soil. The SOC accumulation within the organic layers following forest establishment could not fully compensate the mineral SOC stock difference between forest and grassland successional stages. Within the mineral soil, forest expansion caused an increase in the dimension of aggregates, while the physical SOC protection within stable aggregates decreased. Ratios of microbially to plant-derived carbohydrates and thermally labile to resistant components decreased from grassland to forest successional stages, and corresponded to decreased SOC protection within stable aggregates.
This PhD thesis showed that mineral SOC stocks and physically protected SOC fractions decreased following forest expansion on mountain grasslands, which can be explained by lower accumulation of binding agents of microbial origin. This can have implications for the accumulation of atmospheric CO2 in soil and for the susceptibility of SOC to external disturbances such as management and environmental changes.
A land-use gradient located in the Southern Alps (Italy) was examined, comprising managed grassland, two transitional phases in which grassland abandonment led to colonization by Picea abies (L.) Karst., and old forest dominated by Fagus sylvatica L. and P. abies. Mineral soil samples were physically separated through aggregate size and size-density fractionation. Changes in labile soil C were assessed by carbohydrate and thermal analyses of soil samples and fractions.
Forest expansion on mountain grasslands caused a decrease in SOC stocks within the mineral soil. The SOC accumulation within the organic layers following forest establishment could not fully compensate the mineral SOC stock difference between forest and grassland successional stages. Within the mineral soil, forest expansion caused an increase in the dimension of aggregates, while the physical SOC protection within stable aggregates decreased. Ratios of microbially to plant-derived carbohydrates and thermally labile to resistant components decreased from grassland to forest successional stages, and corresponded to decreased SOC protection within stable aggregates.
This PhD thesis showed that mineral SOC stocks and physically protected SOC fractions decreased following forest expansion on mountain grasslands, which can be explained by lower accumulation of binding agents of microbial origin. This can have implications for the accumulation of atmospheric CO2 in soil and for the susceptibility of SOC to external disturbances such as management and environmental changes.
| Originalsprog | Engelsk |
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| Forlag | Department of Geosciences and Natural Resource Management, Faculty of Science, University of Copenhagen |
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| Antal sider | 155 |
| Status | Udgivet - 2014 |