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Soil CO2 exchange in seven pristine Amazonian rain forest sites in relation to soil temperature

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Kesselmeier,  Jürgen
Biogeochemistry, Max Planck Institute for Chemistry, Max Planck Society;

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引用

Zanchi, F. B., Meesters, A. G. C. A., Waterloo, M. J., Kruijt, B., Kesselmeier, J., Luizão, F. J., & Dolman, A. J. (2014). Soil CO2 exchange in seven pristine Amazonian rain forest sites in relation to soil temperature. Agricultural and Forest Meteorology, 192, 96-107. doi:10.1016/j.agrformet.2014.03.009.


引用: http://hdl.handle.net/11858/00-001M-0000-0024-B505-9
要旨
We analysed soil respiration measurements made in seven distinctly different pristine rain forests in Central Amazon, ranging from stunted heath forest (Campina) to tall terra-firme rain forest. The differences in soil respiration fluxes between sites and their causes were investigated, as well as diurnal patterns and their dependency on temperature. Ensemble averages of hourly fluxes were calculated for both wet and dry seasons (as far as these were sampled). These values were processed using an analytical model estimating soil surface temperature from the temperature measured at two depths. The soil CO2 efflux can be viewed as a proxy for forest productivity. The low productive Campina stunted heath forest site (on leached sandy soils and covered by scleromorphic vegetation) has the lowest respiration (<1.5 mu mol CO2 m(-2) s(-1), dry period). Respiration increased in local patches of taller heath forest on finer textured soil to about 4 mu mol CO2 m(-2) s(-1). In the Cuieiras lowland rain forest respiration changed along a toposequence. The lowest value of 2.5 p,mol CO2 m(-2) s(-1) was observed on the plateau (terra-firme rain forest), whereas a maximum of 6.0 pawl CO2 m(-2) s(-1) was observed in the valley (Campinarana forest). Soil respiration decreased to about 4 mu mol CO2 m(-2) s(-1) close to the river (riparian forest) where soils remained close to saturation. To find the optimum correlation between soil temperature and respiration flux, relationships were derived between the amplitudes and phases of respiration and soil temperatures measured at different depths. Compared to the use of soil temperatures measured at 5 cm and 10cm depth, the use of (modelled) soil surface temperatures strongly reduced the hysteresis between respiration and temperature, and improved the coefficient of determination (R-2) for the Cuieiras forest sites, whereas the Campina sites still showed time lags of several hours between respiration and soil temperature diurnal patterns. With respect to the surface temperature, Q(10) ranged from 1.7 (bare soil, dry season) to 2.0-2.5 (Cuieiras slope and plateau sites, dry season) and 3.3-5.2 (ibidem, wet season) to 5.5-7.7 (Cuieiras Campinarana and valley forests, dry/wet season). (C) 2014 Elsevier B.V. All rights reserved.