A Look at Amazon Basin Seasonal Dynamics with the Biophysical ...
A Look at Amazon Basin Seasonal Dynamics with the Biophysical ... A Look at Amazon Basin Seasonal Dynamics with the Biophysical ...
COMPARISION THE SOIL RESPIRATION IN FOREST, PASTURE ANDAGROSILVIPASTORAL SYSTEM IN THE SOUTH AMAZONPaulo César Nunes 1 (Av. 04 de Julho n. 53, Centro – 78340-000 Juruena MT- Brazil;prnatura@terra.com.br)José Holanda Campelo Jr. 2 , Nicolau Priante Filho 2 ,Linda Akiko Yamamura 1 , Elke Leite Bezerra 31 . Instituto Pro Natura –IPN 2 Universidade Federal de Mato Grosso-UFMT3 Universidade de Varzea Grande -UNIVAGThe aim of this work was to compare the soil respiration of an area of primaryforest cover, with an extensive pasture system and an agrosilvopastoral system, inthe plane dystrophic dark Argissolo Red soil. We used an infrared gas analyzer(the Environment Gas Monitor, EGM-1/WMA-2: GAS ANALYSERS), attachedto a container able to retain 1170 cm 3 CO 2 . The experimental area is located in theExperimental Center of Agroforestry of the Instituto Pró Natura, in themunicipality of Juruena, Northwest Mato Grosso - Brazil. The treatmentsconsisted of three areas under different uses: an area of primary forest, a sevenyears old agrosilvipastoral system and a five years old extensive pasture system.The plots have 10m x 10 m, with 1 m measurement network executed betweenJanuary 2001 and February 2002. The results showed that in wet season during inthe morning, the soil respiration and soil temperature, measured at 1 cm depth,was significant different in three areas, with means 7.9 µmol CO 2 m -2 s -1 at 27.2ºCto pasture, 5.4 µmol CO 2 m -2 s -1 at 26.3 ºC to agrosilvipastoral system and 4.4µmol CO 2 m -2 s -1 at 24.8 ºC to jungle. In wet season in the afternoon the soiltemperature was significant different for the three places, but the soil respirationshowed significant differences only between forest with pasture and forest withagrosilvipastoral. The average during wet season in the afternoon ranged by 5.8µmol CO 2 m -2 s -1 at 30.8 ºC to the pasture, 5.38 µmol CO 2 m -2 s -1 at 28.5 ºC to theagrosilvipastoral system and 4,13 µmol CO 2 m -2 s -1 at 25.84 ºC to the forest.
- Page 168: Carbon Release from Stems and Branc
- Page 172: Estimation of Amazon night-time CO
- Page 176: using block kriging. Data were over
- Page 180: FOREST CANOPY-TROPOSPHERE CO 2 AND
- Page 184: Calibrating the carbon and energy-w
- Page 188: Comparison of the fast response ins
- Page 194: Soil-Atmosphere Flux of Carbon Diox
- Page 198: Comparison of an Open-Path Mk3 Hydr
- Page 202: A MULTI-LAYER BIOPHYSICAL MODEL CAL
- Page 208: Dynamics of dissolved organic matte
- Page 212: INFLUENCE OF SEASONALITY AND LAND U
- Page 216: Using Eddy Covariance and Bowen Rat
- Page 222: THE USE OF A FOOTPRINT MODEL TO ANA
- Page 226: MODELLING FLUXES FROM AMAZONIAN RAI
- Page 230: Submitted to: IISCLBA - 2 ND SCIENT
- Page 234: ASSESSING THE CHANGE FROM PASTURE T
- Page 238: Toward Mapping Spatial Distribution
- Page 242: Carbon balance and seasonal pattern
- Page 246: Climatic and edaphic control of reg
- Page 250: Study of the mean wind speed profil
- Page 254: An analytical approach for estimati
- Page 258: Leland PierceLiane GuildLívia Vasc
- Page 262: Respiration from a Tropical Forest
- Page 266: The Net Carbon Flux Due to Deforest
COMPARISION THE SOIL RESPIRATION IN FOREST, PASTURE ANDAGROSILVIPASTORAL SYSTEM IN THE SOUTH AMAZONPaulo César Nunes 1 (Av. 04 de Julho n. 53, Centro – 78340-000 Juruena MT- Brazil;prn<strong>at</strong>ura@terra.com.br)José Holanda Campelo Jr. 2 , Nicolau Priante Filho 2 ,Linda Akiko Yamamura 1 , Elke Leite Bezerra 31 . Instituto Pro N<strong>at</strong>ura –IPN 2 Universidade Federal de M<strong>at</strong>o Grosso-UFMT3 Universidade de Varzea Grande -UNIVAGThe aim of this work was to compare <strong>the</strong> soil respir<strong>at</strong>ion of an area of primaryforest cover, <strong>with</strong> an extensive pasture system and an agrosilvopastoral system, in<strong>the</strong> plane dystrophic dark Argissolo Red soil. We used an infrared gas analyzer(<strong>the</strong> Environment Gas Monitor, EGM-1/WMA-2: GAS ANALYSERS), <strong>at</strong>tachedto a container able to retain 1170 cm 3 CO 2 . The experimental area is loc<strong>at</strong>ed in <strong>the</strong>Experimental Center of Agroforestry of <strong>the</strong> Instituto Pró N<strong>at</strong>ura, in <strong>the</strong>municipality of Juruena, Northwest M<strong>at</strong>o Grosso - Brazil. The tre<strong>at</strong>mentsconsisted of three areas under different uses: an area of primary forest, a sevenyears old agrosilvipastoral system and a five years old extensive pasture system.The plots have 10m x 10 m, <strong>with</strong> 1 m measurement network executed betweenJanuary 2001 and February 2002. The results showed th<strong>at</strong> in wet season during in<strong>the</strong> morning, <strong>the</strong> soil respir<strong>at</strong>ion and soil temper<strong>at</strong>ure, measured <strong>at</strong> 1 cm depth,was significant different in three areas, <strong>with</strong> means 7.9 µmol CO 2 m -2 s -1 <strong>at</strong> 27.2ºCto pasture, 5.4 µmol CO 2 m -2 s -1 <strong>at</strong> 26.3 ºC to agrosilvipastoral system and 4.4µmol CO 2 m -2 s -1 <strong>at</strong> 24.8 ºC to jungle. In wet season in <strong>the</strong> afternoon <strong>the</strong> soiltemper<strong>at</strong>ure was significant different for <strong>the</strong> three places, but <strong>the</strong> soil respir<strong>at</strong>ionshowed significant differences only between forest <strong>with</strong> pasture and forest <strong>with</strong>agrosilvipastoral. The average during wet season in <strong>the</strong> afternoon ranged by 5.8µmol CO 2 m -2 s -1 <strong>at</strong> 30.8 ºC to <strong>the</strong> pasture, 5.38 µmol CO 2 m -2 s -1 <strong>at</strong> 28.5 ºC to <strong>the</strong>agrosilvipastoral system and 4,13 µmol CO 2 m -2 s -1 <strong>at</strong> 25.84 ºC to <strong>the</strong> forest.