Trees and grass contribution to soil organic carbon in agroforestry systems.

Agroforestry systems have the potential to enhance carbon (C) sequestration in soil compared with treeless (agricultural) systems (Montagnini & Nair, 2004). When one type of vegetation is replaced with another, stable isotope contents (?13 C) values can be used to identify soil organic carbon (SOC) derived from residues in the native vegetation and the new vegetation based on discrimination between C3 and C4 plants. The present study aimed to assessing the impact of difference land-use systems on C3 and C4 contribution to SOC. The experimental area is located inside the Cerrado biome. Soil samples were taken from six different land-use sites: (i) native local forest; (ii) Eucalyptus forest (EF) established in 1985 (OEC); (iii) EF established in 2004 (NEC); (iv) pasture of B. decumbens; (v) Agroforestry System (AF) established on 1994 (OAF); and (vi) AF established on 2004 (NAF). The establishment on AF was placed first with the eucalyptus planted and rice (Oryza sativa), soybean (Glycine max) and braquiaria grass (B. Brizantha cv. Marandu) in between trees rows. Soil was collected from four depths (0-10; 10-20; 20-50 and 50-100 cm). For stable C isotope analysis, whole soil was analyzed mass spectrometer. The percentage of SOC derived from the Brachiaria ssp., a C4 plant, or from the eucalyptus or native forest, a C3 plant, was estimated based on the equations: % C4-derived SOC = (?- ?T)/(?G- ?T) x 100 (1); % C3-derived SOC = 100 - % C4-derived SOC (2) Based on the equations 1 and 2 were calculated the contributions of each C3 and C4 species in SOC C-derived, as follows: C3-devived SOC (Mg ha-1) = (% C3-derived SOC) x (SOC content, Mg ha-1) (3); C4-derived SOC (Mg ha-1) = (% C4-derived SOC) x (SOC content, Mg ha-1) (4). A complete randomized design was used with Tukey?s studentized. Statistical differences were considered significant at p <0.05.

Saved in:
Bibliographic Details
Main Authors: TONUCCI, R. G., GARCIA, R., NAIR, V.
Other Authors: RAFAEL GONCALVES TONUCCI, CNPC; Rasmo Garcia, Federal Univ. of Viçosa (UFV) - Viçosa, MG, Brazil; Vimala Nair, Soil and Water Science Dep. Univ. of Florida, Gainesville.
Format: Anais e Proceedings de eventos biblioteca
Language:English
eng
Published: 2015-09-04
Subjects:Sistema agroflorestal, Organic carbon, Brasil, Minas Gerais, Agroforestry systems., Solo, Carbono, Composto orgânico, Uso da terra, Cerrado, Soil, Organic compounds, Land use, Brazil.,
Online Access:http://www.alice.cnptia.embrapa.br/alice/handle/doc/1023312
Tags: Add Tag
No Tags, Be the first to tag this record!
id dig-alice-doc-1023312
record_format koha
spelling dig-alice-doc-10233122017-08-16T02:34:29Z Trees and grass contribution to soil organic carbon in agroforestry systems. TONUCCI, R. G. GARCIA, R. NAIR, V. RAFAEL GONCALVES TONUCCI, CNPC; Rasmo Garcia, Federal Univ. of Viçosa (UFV) - Viçosa, MG, Brazil; Vimala Nair, Soil and Water Science Dep. Univ. of Florida, Gainesville. Sistema agroflorestal Organic carbon Brasil Minas Gerais Agroforestry systems. Solo Carbono Composto orgânico Uso da terra Cerrado Soil Organic compounds Land use Brazil. Agroforestry systems have the potential to enhance carbon (C) sequestration in soil compared with treeless (agricultural) systems (Montagnini & Nair, 2004). When one type of vegetation is replaced with another, stable isotope contents (?13 C) values can be used to identify soil organic carbon (SOC) derived from residues in the native vegetation and the new vegetation based on discrimination between C3 and C4 plants. The present study aimed to assessing the impact of difference land-use systems on C3 and C4 contribution to SOC. The experimental area is located inside the Cerrado biome. Soil samples were taken from six different land-use sites: (i) native local forest; (ii) Eucalyptus forest (EF) established in 1985 (OEC); (iii) EF established in 2004 (NEC); (iv) pasture of B. decumbens; (v) Agroforestry System (AF) established on 1994 (OAF); and (vi) AF established on 2004 (NAF). The establishment on AF was placed first with the eucalyptus planted and rice (Oryza sativa), soybean (Glycine max) and braquiaria grass (B. Brizantha cv. Marandu) in between trees rows. Soil was collected from four depths (0-10; 10-20; 20-50 and 50-100 cm). For stable C isotope analysis, whole soil was analyzed mass spectrometer. The percentage of SOC derived from the Brachiaria ssp., a C4 plant, or from the eucalyptus or native forest, a C3 plant, was estimated based on the equations: % C4-derived SOC = (?- ?T)/(?G- ?T) x 100 (1); % C3-derived SOC = 100 - % C4-derived SOC (2) Based on the equations 1 and 2 were calculated the contributions of each C3 and C4 species in SOC C-derived, as follows: C3-devived SOC (Mg ha-1) = (% C3-derived SOC) x (SOC content, Mg ha-1) (3); C4-derived SOC (Mg ha-1) = (% C4-derived SOC) x (SOC content, Mg ha-1) (4). A complete randomized design was used with Tukey?s studentized. Statistical differences were considered significant at p <0.05. 2015-09-04T11:11:11Z 2015-09-04T11:11:11Z 2015-09-04 2015 2016-03-04T11:11:11Z Anais e Proceedings de eventos In: WORLD CONGRESS ON INTEGRATED CROP-LIVESTOCK-FOREST SYSTEMS; INTERNATIONAL SYMPOSIUM ON INTEGRATED CROP-LIVESTOCK SYSTEMS, 3., 2015, Brasília, DF. Towards sustainable intensification: proceedings. Brasília, DF: Embrapa, 2015. http://www.alice.cnptia.embrapa.br/alice/handle/doc/1023312 en eng openAccess
institution EMBRAPA
collection DSpace
country Brasil
countrycode BR
component Bibliográfico
access En linea
databasecode dig-alice
tag biblioteca
region America del Sur
libraryname Sistema de bibliotecas de EMBRAPA
language English
eng
topic Sistema agroflorestal
Organic carbon
Brasil
Minas Gerais
Agroforestry systems.
Solo
Carbono
Composto orgânico
Uso da terra
Cerrado
Soil
Organic compounds
Land use
Brazil.
Sistema agroflorestal
Organic carbon
Brasil
Minas Gerais
Agroforestry systems.
Solo
Carbono
Composto orgânico
Uso da terra
Cerrado
Soil
Organic compounds
Land use
Brazil.
spellingShingle Sistema agroflorestal
Organic carbon
Brasil
Minas Gerais
Agroforestry systems.
Solo
Carbono
Composto orgânico
Uso da terra
Cerrado
Soil
Organic compounds
Land use
Brazil.
Sistema agroflorestal
Organic carbon
Brasil
Minas Gerais
Agroforestry systems.
Solo
Carbono
Composto orgânico
Uso da terra
Cerrado
Soil
Organic compounds
Land use
Brazil.
TONUCCI, R. G.
GARCIA, R.
NAIR, V.
Trees and grass contribution to soil organic carbon in agroforestry systems.
description Agroforestry systems have the potential to enhance carbon (C) sequestration in soil compared with treeless (agricultural) systems (Montagnini & Nair, 2004). When one type of vegetation is replaced with another, stable isotope contents (?13 C) values can be used to identify soil organic carbon (SOC) derived from residues in the native vegetation and the new vegetation based on discrimination between C3 and C4 plants. The present study aimed to assessing the impact of difference land-use systems on C3 and C4 contribution to SOC. The experimental area is located inside the Cerrado biome. Soil samples were taken from six different land-use sites: (i) native local forest; (ii) Eucalyptus forest (EF) established in 1985 (OEC); (iii) EF established in 2004 (NEC); (iv) pasture of B. decumbens; (v) Agroforestry System (AF) established on 1994 (OAF); and (vi) AF established on 2004 (NAF). The establishment on AF was placed first with the eucalyptus planted and rice (Oryza sativa), soybean (Glycine max) and braquiaria grass (B. Brizantha cv. Marandu) in between trees rows. Soil was collected from four depths (0-10; 10-20; 20-50 and 50-100 cm). For stable C isotope analysis, whole soil was analyzed mass spectrometer. The percentage of SOC derived from the Brachiaria ssp., a C4 plant, or from the eucalyptus or native forest, a C3 plant, was estimated based on the equations: % C4-derived SOC = (?- ?T)/(?G- ?T) x 100 (1); % C3-derived SOC = 100 - % C4-derived SOC (2) Based on the equations 1 and 2 were calculated the contributions of each C3 and C4 species in SOC C-derived, as follows: C3-devived SOC (Mg ha-1) = (% C3-derived SOC) x (SOC content, Mg ha-1) (3); C4-derived SOC (Mg ha-1) = (% C4-derived SOC) x (SOC content, Mg ha-1) (4). A complete randomized design was used with Tukey?s studentized. Statistical differences were considered significant at p <0.05.
author2 RAFAEL GONCALVES TONUCCI, CNPC; Rasmo Garcia, Federal Univ. of Viçosa (UFV) - Viçosa, MG, Brazil; Vimala Nair, Soil and Water Science Dep. Univ. of Florida, Gainesville.
author_facet RAFAEL GONCALVES TONUCCI, CNPC; Rasmo Garcia, Federal Univ. of Viçosa (UFV) - Viçosa, MG, Brazil; Vimala Nair, Soil and Water Science Dep. Univ. of Florida, Gainesville.
TONUCCI, R. G.
GARCIA, R.
NAIR, V.
format Anais e Proceedings de eventos
topic_facet Sistema agroflorestal
Organic carbon
Brasil
Minas Gerais
Agroforestry systems.
Solo
Carbono
Composto orgânico
Uso da terra
Cerrado
Soil
Organic compounds
Land use
Brazil.
author TONUCCI, R. G.
GARCIA, R.
NAIR, V.
author_sort TONUCCI, R. G.
title Trees and grass contribution to soil organic carbon in agroforestry systems.
title_short Trees and grass contribution to soil organic carbon in agroforestry systems.
title_full Trees and grass contribution to soil organic carbon in agroforestry systems.
title_fullStr Trees and grass contribution to soil organic carbon in agroforestry systems.
title_full_unstemmed Trees and grass contribution to soil organic carbon in agroforestry systems.
title_sort trees and grass contribution to soil organic carbon in agroforestry systems.
publishDate 2015-09-04
url http://www.alice.cnptia.embrapa.br/alice/handle/doc/1023312
work_keys_str_mv AT tonuccirg treesandgrasscontributiontosoilorganiccarboninagroforestrysystems
AT garciar treesandgrasscontributiontosoilorganiccarboninagroforestrysystems
AT nairv treesandgrasscontributiontosoilorganiccarboninagroforestrysystems
_version_ 1756021335324098560