1
AGB dry of the tree community on the plane* afforestations measured 80.08±15.0 Mgha -1 , whereas the afforested tree community on the slope** measured less then half of this (37.23±12.6 Mgha -1 ). Combining soil sampling results for soil organic carbon and carbon contents of above- and below ground biomass, the total carbon pool for plane and sloped areas shows almost the same pattern (Tab.1). A CCA ordination of plot AGB dry shows a significant influence of soil and relief explaining the variation of the afforestations biomass and carbon accumulation (Fig.2). Condit, R. (1998): Tropical forest census plots: methods and results from barro colorade islands, panama and a comparison with other plots. Springer, Berlin Heidelberg New York, 212pp Magnussen, S. & Reed, D. (2004). Modeling for Estimation and Monitoring. FAO, Rome Tiepolo, G., Calmon, M., & Feretti, R. andre. (2002). Measuring and Monitoring Carbon Stocks at the Guaraqueçaba Climate Action Project , Paraná , Brazil. International Symposium on Forest Carbon Sequestration and Monitoring, Vol. 153 References Background Methods Sattler, D. 1 , Murray, L.T. 2 , Kirchner, A 1 . & Lindner, A 2 . 1 University of Leipzig, Institute of Geography, Department of Physical Geography and Geo-Ecology, Johannisallee 19, 04103 Leipzig, Germany, [email protected] 2 Technische Universität Dresden, Institute of International Forestry and Forest Products , Pienner Strasse 7, 01735 Tharandt, Germany, [email protected] The impact of Soil and Relief on the performance of afforested pastures in South East Brazil Results Tab. 1. Carbon pool estimates for afforestation plots in plane and slope position <0,001 62.64 ± 12.2 92.99 ± 10.5 Total n.s. 40.94 ± 2.6 46.32 ± 9.1 Soil (Organic Carbon, 30cm) <0,001 21.70 ± 7.3 46.67 ± 8.7 Biomass <0,001 4.2 ± 1.4 9.03 ± 1.7 Root <0,001 17.50 ± 5.9 37.64 ± 7.1 AGB dry P Slope (MgC ha -1 ) Plane (MgC ha -1 ) Carbon pool Projects involving the reforestation or afforestation of abandoned or degraded land are a practical biological approach to restore regional ecological functions and to sequester atmospheric carbon to help mitigate the global imbalance of atmospheric carbon associated with climate change. Large gaps remain, however, in understanding the dynamics of afforested tree communities. In this non-experimental, small-scale study, the effect topographical relief has on the growth performance of planted trees has been assessed. Above ground dry biomass accumulation was estimated to evaluate afforested tree communities performance, established on abandoned pasture at the Reserva Ecológica de Guapiaçu (REGUA), in the Serra dos Órgãos region of Rio de Janeiro, Brazil (Fig.1). Fig. 1. Study site at REGUA with afforested hill slope (S) in the background and plane area (P), both previously used as pasture. S P Eighteen 10x10m plots were established 2012 in afforested areas planted during the rainy season of 2007-2008. All trees with DBH≥1cm were tagged and censused following the guidelines for studying tropical forest census plots suggested by Condit (1998). To estimate AGB dry , the allometric model for young secondary forests developed by Tiepolo et al. (2002) was used. Root biomass has been estimated applying a root-to-shoot ratio of 0.24 of above ground biomass. To convert biomass to carbon, AGB dry was multiplied by 0.47 as suggested by the FAO-IUFRO (Magnussen & Reed 2004). Disturbed soil samples were taken 0 to 30cm below surface and analyzed for a basic set of chemical (C org , C/N, P, CEC, pH) and physical (grain size distribution, bulk density) soil properties. Soil analysis was performed by EMBRAPA Solos according to Brazilian standard procedures. The study revealed large discrepancies in AGB and respective organic carbon accumulation depending on topography and related soil conditions. Hence, these differences in tree growth performance should be considered to prevent misleading carbon sink estimates when developing regional REDD+ strategies promoted by afforestations. Fig. 2. Results of a CCA of plot AGB dry based on species composition. Factors that significantly reduced variation between sites are plotted with vectors. Dot diameters represent relative plot AGB dry . Hollow dots = plane plots, filled dots = slope plots * 151 individuals of 31 species (e.g.Trema micrantha, Piptadenia paniculata, Piptadenia gonoacantha, Nectandra membranacea, Vernonia polyanthes, Inga edulis, Schizolobium parahyba) ** 157 individuals of 23 species (e.g. Gochnatia polymorpha, Trema micrantha, Inga edulis, Guarea guidonia, Cecropia glaziovii, Piptadenia paniculata, Schizolobium parahyba)

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Page 1: The impact of Soil and Relief on the performance of ......Guarea guidonia, Cecropia glaziovii, Piptadenia paniculata, Schizolobium parahyba) Title: Folie 1 Author: PC Created Date:

AGBdry of the tree community on the plane* afforestations measured

80.08±15.0 Mgha-1, whereas the afforested tree community on the slope**

measured less then half of this (37.23±12.6 Mgha-1). Combining soil

sampling results for soil organic carbon and carbon contents of above- and

below ground biomass, the total carbon pool for plane and sloped areas

shows almost the same pattern (Tab.1).

A CCA ordination of plot AGBdry shows a significant influence of soil and

relief explaining the variation of the afforestations biomass and carbon

accumulation (Fig.2).

• Condit, R. (1998): Tropical forest census plots: methods and results from barro colorade islands, panama and a comparison with other plots. Springer, Berlin Heidelberg New York, 212pp

• Magnussen, S. & Reed, D. (2004). Modeling for Estimation and Monitoring. FAO, Rome

• Tiepolo, G., Calmon, M., & Feretti, R. andre. (2002). Measuring and Monitoring Carbon Stocks at the Guaraqueçaba Climate Action Project , Paraná , Brazil. International Symposium on Forest Carbon Sequestration and Monitoring, Vol. 153

References

Background

Methods

Sattler, D.1, Murray, L.T.2, Kirchner, A1. & Lindner, A2.1 University of Leipzig, Institute of Geography, Department of Physical Geography and Geo-Ecology, Johannisallee 19, 04103 Leipzig, Germany, [email protected]

2 Technische Universität Dresden, Institute of International Forestry and Forest Products , Pienner Strasse 7, 01735 Tharandt, Germany, [email protected]

The impact of Soil and Relief on the performance of afforested pastures in South East Brazil

Results

Tab. 1. Carbon pool estimates for afforestation plots in plane and slope position

<0,00162.64 ± 12.292.99 ± 10.5Total

n.s.40.94 ± 2.646.32 ± 9.1Soil (Organic Carbon, 30cm)

<0,00121.70 ± 7.346.67 ± 8.7 Biomass

<0,0014.2 ± 1.49.03 ± 1.7 Root

<0,00117.50 ± 5.937.64 ± 7.1 AGBdry

PSlope (MgC ha-1)Plane (MgC ha-1)Carbon pool

Projects involving the reforestation or afforestation of

abandoned or degraded land are a practical biological approach

to restore regional ecological functions and to sequester

atmospheric carbon to help mitigate the global imbalance of

atmospheric carbon associated with climate change. Large gaps

remain, however, in understanding the dynamics of afforested

tree communities. In this non-experimental, small-scale study,

the effect topographical relief has on the growth performance of

planted trees has been assessed. Above ground dry biomass

accumulation was estimated to evaluate afforested tree

communities performance, established on abandoned pasture

at the Reserva Ecológica de Guapiaçu (REGUA), in the Serra dos

Órgãos region of Rio de Janeiro, Brazil (Fig.1).Fig. 1. Study site at REGUA with afforested hill slope (S) in the background and plane area (P),both previously used as pasture.

S

P

Eighteen 10x10m plots were established 2012 in afforested areas planted during the rainy season of 2007-2008. All trees with DBH≥1cm were tagged

and censused following the guidelines for studying tropical forest census plots suggested by Condit (1998). To estimate AGBdry, the allometric model

for young secondary forests developed by Tiepolo et al. (2002) was used. Root biomass has been estimated applying a root-to-shoot ratio of 0.24 of

above ground biomass. To convert biomass to carbon, AGBdry was multiplied by 0.47 as suggested by the FAO-IUFRO (Magnussen & Reed 2004).

Disturbed soil samples were taken 0 to 30cm below surface and analyzed for a basic set of chemical (Corg, C/N, P, CEC, pH) and physical (grain size

distribution, bulk density) soil properties. Soil analysis was performed by EMBRAPA Solos according to Brazilian standard procedures.

The study revealed large discrepancies in AGB and respective organic

carbon accumulation depending on topography and related soil

conditions. Hence, these differences in tree growth performance

should be considered to prevent misleading carbon sink estimates

when developing regional REDD+ strategies promoted by

afforestations.

Fig. 2. Results of a CCA of plot AGBdry based on species composition. Factors thatsignificantly reduced variation between sites are plotted with vectors. Dot diametersrepresent relative plot AGBdry. Hollow dots = plane plots, filled dots = slope plots

* 151 individuals of 31 species (e.g.Trema micrantha, Piptadenia paniculata, Piptadenia gonoacantha,

Nectandra membranacea, Vernonia polyanthes, Inga edulis, Schizolobium parahyba)

** 157 individuals of 23 species (e.g. Gochnatia polymorpha, Trema micrantha, Inga edulis, Guarea guidonia, Cecropia glaziovii, Piptadenia paniculata, Schizolobium parahyba)