Promoting sustainable land-use management: water, carbon and nutrient turnover Dirk Hölscher & Pak Soekisman.

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Presentation transcript:

Promoting sustainable land-use management: water, carbon and nutrient turnover Dirk Hölscher & Pak Soekisman

Objectives Present key results Draw conclusions for agricultural and forest management

Land use types & land use gradients

Aboveground biomass, premontane natural forests Hertel et al. 2009

Steffan-Dewenter et al., 2007 Tree cover (%) Steffan-Dewenter et al., 2007

Meteorological flux tower in a montane rainforest, Bariri

Measured net ecosystem exchange flux Fc, extrapolated respiration flux RE, and the sum of both fluxes Pg (gross photosynthesis) Ibrom et al., 2007

CO2 fluxes between the atmosphere: forest vs. cacao Ibrom et al., 2007

Land use types and net ecosystem productivities: scenarios Olchev et al., 2008

Land use types and net ecosystem productivities: model results Olchev et al., 2008

Fluxes of sensible (H) and latent (E) energy: forest vs. cacao Ibrom et al., 2007

Sap flux of cacao and shade trees Köhler et al. 2009

Cacao tree water use vs. canopy gap fraction Shade trees enhanced water use by cacao trees (R2adj = 0.39, p = 0.043, n = 9) Köhler et al. 2009

Gumbasa river watershed Catchment size: 1275 km² River discharge R2 = 0.86 R²=0.83 automatic stage recorder stage recorder – Forestry climate station climate station STORMA main irrigation chanel Lore Lindu National Park Palu river watershed Gerold & Leemhuis 2008 Gauging stations

Modeling discharge of the river discharge, Gumbasa watershed: effects of land cover change Discharge (2003): status quo 2003: 590 mm land use scenario A1: 838 mm + 42%  1200m annual crops Land use scenario A2: 724 mm + 23%  1200m change into cacao Gerold & Leemhuis 2008

Modeled run off components 1 2 3 4 5 6 7 8 Discharge (mm d -1 ) Direct flow Interflow Base flow Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec 2003 Kleinhans et al. 2004

Nutrient balance of maize and agroforest Dechert et al., 2004

Summary land use types & land use gradients High carbon storage in forests of Sulwesi High carbon uptake by forest Shade trees enhance transpiration from agrofrests River discharge change with land cover change suggested Agroforestry strongly benefits from nitrogen input by N fixing shade trees

Implications Very important to conserve remaining forests Shade trees positively influence cacao cultivation

Drought experiments Premontane rainforest Cacao/Gliricidia agroforest

Cacao-Gliricidia agroforest

n=3 roof (treatment) plots, n=3 control plots 80% of plot area was covered by plastic panels (March 07- mid April 08); n=3 roof (treatment) plots, n=3 control plots M. Köhler G Moser

Tree sap flux Soil water content Cacao bean yield Litterfall

Moser et al. under review Cacao yield Roof closure -55%, p<0.05 -10%, p>0.05 Moser et al. under review

Soil water storage (mm) Roof to control ratio Soil water storage and cacao water use Sap flux cacao -11%, p>0.05 Roof closure Soil water storage (mm) Roof to control ratio Mean±SD, n=3 - 40%, p < 0.05)

Complementary use of soil water deuterium signal δ Cacao Gliricidia Schwendenmann et al. 2009

Water uptake depth cacao and Glricidia Schwendenmann, unpublished

Root water potential Cacao Gliricidia Osmotic adjustment in cacao Control Roof Osmotic adjustment in cacao Moser et al. under review

Van Straaten, unpublished CO2 soil efflux Period of roof closure CO2 efflux (Mg C m-1 h-1) Experiment period If you are interested I can also give you an interpretation of what we believe took place in time…. i.e during and after the natural drought in Jan/Feb 2008 CO2 efflux remained consistently lower than control plot given drought stress in trees Van Straaten, unpublished

CO2 efflux response to soil moisture Volumetric water content (m3 m-3) CO2 efflux (Mg C m-1 h-1) Dirk: I can also give you a similar graph but instead with pF instead of VWC… But I guess for a general meeting it is easier to understand VWC. (Adj R2 = 0.338, n = 94) Van Straaten, unpublished

Summary cacao drought experiment Cacao yield was little influenced for several months; a strong (~50%) reduction was observed at the end of the experiment Little response of tree water use to drought Cacao and Glriricidia trees use soil water resources complementary Small effects of drought on soil CO2 efflux

Implications Cacao is a suitable crop even where short dry spells occur Shade trees: no negative effect on cacao tree performance

Forest

Soil moisture Köhler, unpublished 10 cm 40 cm 150 cm Roof closure 06/2007 06/2008 6/2009

Sap flux: all trees Schuldt, unpublished

Stem wood production (2nd year) Moser, unpublished

Van Straaten, unpublished CO2 soil efflux CO2 efflux (Mg C m-1 h-1) Experiment period Period of roof closure If you are interested I can also give you an interpretation of what we believe took place in time…. i.e during and after the natural drought in Jan/Feb 2008 CO2 efflux remained consistently lower than control plot given drought stress in trees Van Straaten, unpublished

CO2 soil efflux vs. soil moisture CO2 efflux (Mg C m-1 h-1) (Adj R2 = 0.79, n = 93) Van Straaten, unpublished

Summary forest drought experiment Little response in tree sap flux to drought Tree diameter growth was significantly reduced Strong effect of drought on soil CO2 efflux

Overall summary Old-growth forest is to be conserved Agroforestry is a promissing option in post-forest landscapes Shade trees play a central role in cacao cultivation

Thank you for attention!