TY - JOUR
T1 - Greenhouse gas emissions from a chinampa soil or floating gardens in Mexico
AU - Ortiz-Cornejo, Nadia Livia
AU - Luna-Guido, Marco
AU - Rivera-Espinoza, Yadira
AU - Vásquez-Murrieta, María Soledad
AU - Ruíz-Valdiviezo, Víctor Manuel
AU - Dendooven, Luc
N1 - Publisher Copyright:
© 2015, Centro de Ciencias de la Atmosfera, UNAM. All rights reserved.
PY - 2015
Y1 - 2015
N2 - Agriculture in chinampas or ‘floating gardens’, is still found on the south of Mexico City, it is a high yield pre-Columbian cultivation system, which has soils enriched with organic matter. The objective of this research was to determine the greenhouse gas (GHG) emissions from a chinampa soil cultivated with amaranth (Amaranthus hypochondriacus L.), maize (Zea mays L.) or uncultivated. The soil was characterized and fluxes of GHG (CO2, N2O and CH4) were monitored for one year. The chinampa soil was alkaline saline with an organic C content that ranged from 21.7 t/ha in the 0-20 cm layer of the soil cultivated with amaranth to 28.4 t/ha in the 20-40 cm layer of the uncultivated soil. The cumulative GHG emissions (kg CO2-equivalents/ha/y) were 395, 376 and 258 for N2O, and 44, 30 and 26 for CH4in the uncultivated, amaranth cultivated and maize cultivated soil, respectively. No significant effect of cultivated crop or soil characteristics on GHG emissions over one year was found. In general, N2O contributed 91 % and CH4 9 % to the global warming potential of the GHG. The organic C was high and distributed equally over the soil profile, because it is an anthropic soil.
AB - Agriculture in chinampas or ‘floating gardens’, is still found on the south of Mexico City, it is a high yield pre-Columbian cultivation system, which has soils enriched with organic matter. The objective of this research was to determine the greenhouse gas (GHG) emissions from a chinampa soil cultivated with amaranth (Amaranthus hypochondriacus L.), maize (Zea mays L.) or uncultivated. The soil was characterized and fluxes of GHG (CO2, N2O and CH4) were monitored for one year. The chinampa soil was alkaline saline with an organic C content that ranged from 21.7 t/ha in the 0-20 cm layer of the soil cultivated with amaranth to 28.4 t/ha in the 20-40 cm layer of the uncultivated soil. The cumulative GHG emissions (kg CO2-equivalents/ha/y) were 395, 376 and 258 for N2O, and 44, 30 and 26 for CH4in the uncultivated, amaranth cultivated and maize cultivated soil, respectively. No significant effect of cultivated crop or soil characteristics on GHG emissions over one year was found. In general, N2O contributed 91 % and CH4 9 % to the global warming potential of the GHG. The organic C was high and distributed equally over the soil profile, because it is an anthropic soil.
KW - C sequestration
KW - Fluxes of carbon dioxide
KW - GHG
KW - Global warming potential
KW - Methane and nitrous oxide
UR - http://www.scopus.com/inward/record.url?scp=84963527874&partnerID=8YFLogxK
M3 - Artículo
SN - 0188-4999
VL - 31
SP - 343
EP - 350
JO - Revista Internacional de Contaminacion Ambiental
JF - Revista Internacional de Contaminacion Ambiental
IS - 4
ER -