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Land cover changes and greenhouse gas emissions in two different soil covers in the Brazilian Caatinga.

Authors :
Ribeiro, Kelly
Sousa-Neto, Eráclito Rodrigues de
JuniorCarvalho, João Andrade de
Sousa Lima, José Romualdo de
Menezes, Rômulo Simões Cezar
Duarte-Neto, Paulo José
da Silva Guerra, Glauce
Ometto, Jean Pierre Henry Baulbaud
Source :
Science of the Total Environment. Nov2016, Vol. 571, p1048-1057. 10p.
Publication Year :
2016

Abstract

The Caatinga biome covers an area of 844,453 km 2 and has enormous endemic biodiversity, with unique characteristics that make it an exclusive Brazilian biome. It falls within the earth's tropical zone and is one of the several important ecoregions of Brazil. This biome undergoes natural lengthy periods of drought that cause losses in crop and livestock productivity, having a severe impact on the population. Due to the vulnerability of this ecosystem to climate change, livestock has emerged as the main livelihood of the rural population, being the precursor of the replacement of native vegetation by grazing areas. This study aimed to measure GHG emissions from two different soil covers: native forest (Caatinga) and pasture in the municipality of São João, Pernambuco State, in the years 2013 and 2014. GHG measurements were taken by using static chamber techniques in both soil covers. According to a previous search, so far, this is the first study measuring GHG emissions using the static chamber in the Caatinga biome. N 2 O emissions ranged from − 1.0 to 4.2 mg m − 2 d − 1 and − 1.22 to 3.4 mg m − 2 d − 1 in the pasture and Caatinga, respectively, and they did not significantly differ from each other. Emissions were significantly higher during dry seasons. Carbon dioxide ranged from − 1.1 to 14.1 and 1.2 to 15.8 g m − 2 d − 1 in the pasture and Caatinga, respectively. CO 2 emissions were higher in the Caatinga in 2013, and they were significantly influenced by soil temperature, showing an inverse relation. Methane emission ranged from 6.6 to 6.8 and − 6.0 to 4.8 mg m − 2 d − 1 in the pasture and Caatinga, respectively, and was significantly higher only in the Caatinga in the rainy season of 2014. Soil gas fluxes seemed to be influenced by climatic and edaphic conditions as well as by soil cover in the Caatinga biome. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
00489697
Volume :
571
Database :
Academic Search Index
Journal :
Science of the Total Environment
Publication Type :
Academic Journal
Accession number :
117914539
Full Text :
https://doi.org/10.1016/j.scitotenv.2016.07.095