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|Research center of Embrapa/Collection:||Embrapa Meio Ambiente - Artigo em periódico indexado (ALICE)|
|Type of Material:||Artigo em periódico indexado (ALICE)|
|Authors:||ROCHA, H. R. da|
FREITAS, H. C.
JUÁREZ, R. I. N.
TANNUS, R. N.
LIGO, M. A. V.
CABRAL, O. M. R.
DIAS, M. A. F. S.
|Additional Information:||MARIA A. F. SILVA DIAS, Departamento de Ciências Atmosféricas, IAG/Universidade de São Paulo.|
OSVALDO MACHADO RODRIGUES CABRAL, CNPMA
MARCOS ANTONIO VIEIRA LIGO, CNPMA
RAFAEL N. TANNUS, Departamento de Ciências Atmosféricas, IAG/Universidade de São Paulo
Robinson I.N. Juárez ROBINSON I. N. JUÁREZ, Departamento de Ciências Atmosféricas, IAG/Universidade de São Paulo
RAFAEL ROSOLEM, Departamento de Ciências Atmosféricas, IAG/Universidade de São Paulo
HELBER C. FREITAS, Departamento de Ciências Atmosféricas, IAG/Universidade de São Paulo
HUMBERTO R. da ROCHA, Departamento de Ciências Atmosféricas, IAG/Universidade de São Paulo
|Title:||Measurements of CO2 exchange over a woodland savanna (Cerrado Sensu stricto) in southeast Brasil.|
|Publisher:||Biota Neotropica, Campinas, v. 2, n. 1, p. 1-11, 2002.|
Sequestro de carbono.
|Description:||The technique of eddy correlation was used to measure the net ecosystem exchange over a woodland savanna (Cerrado Sensu stricto) site (Gleba Pé de Gigante) in southeast Brazil. The data set included measurements of climatological variables and soil respiration using static soil chambers. Data were collected during the period from 10 October 2000 to 30 March 2002. Measured soil respiration showed average values of 4.8 molCO m-2s-1 year round. Its 2 seasonal differences varied from 2 to 8 molCO m-2s-1 (Q = 4.9) during the dry (April to August) and wet season, respectively, and was concurrent with soil temperature and moisture variability. The net ecosystem CO2 flux (NEE) variability is controlled by solar radiation, temperature and air humidity on diel course. Seasonally, soil moisture plays a strong role by inducing litterfall, reducing canopy photosynthetic activity and soil respiration. The net sign of NEE is negative (sink) in the wet season and early dry season, with rates around -25 kgC ha-1day-1, and values as low as 40 kgC ha- 1day-1. NEE was positive (source) during most of the dry season, and changed into negative at the onset of rainy season. At critical times of soil moisture stress during the late dry season, the ecosystem experienced photosynthesis during daytime, although the net sign is positive (emission). Concurrent with dry season, the values appeared progressively positive from 5 to as much as 50 kgC ha-1day-1. The annual NEE sum appeared to be nearly in balance, or more exactly a small sink, equal to 0.1 0.3 tC ha-1yr-1, which we regard possibly as a realistic one, giving the constraining conditions imposed to the turbulent flux calculation, and favourable hypothesis of succession stages, climatic variability and CO2 fertilization.|
|Appears in Collections:||Artigo em periódico indexado (CNPMA)|