CO2 emission from soils under different uses and flooding conditions |
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| Authors: | ME Guntiñas MC Leirós |
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| Institution: | a Departamento de Edafología y Química Agrícola, Facultad de Farmacia, Universidad de Santiago de Compostela, E-15782 Santiago de Compostela, Spain
b Departamento de Bioquímica del Suelo, Instituto de Investigaciones Agrobiológicas de Galicia, CSIC, Apartado 122, E-15780 Santiago de Compostela, Spain |
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| Abstract: | The emission of CO2 from Galician (NW Spain) forest, grassland and cropped soils was studied in a laboratory experiment, at different temperatures (10-35 °C) and at moisture contents of 100% and 160% of the field capacity (FC) of each soil (the latter value corresponds to saturated conditions, and represents between 120% and 140% of the water holding capacity, depending on the soil). In the forest soil, respiration in the flooded samples at all temperatures was lower than that at 100% field capacity. In the agricultural (grassland and cropped) soils the emission was higher (particularly at the highest incubation temperatures) in the soils wetted to 160% of the field capacity than in those wetted to 100% of the field capacity. In all cases the emission followed first order kinetics and the mineralization constants increased exponentially with temperature. In the forest soil, the Q10 values were almost the same in the soils incubated at the two moisture contents. The grassland and cropped soils displayed different responses, as the Q10 values were higher in the soils at 160% than in those at 100% of field capacity. In addition, and particularly at the highest temperatures, the rate of respiration increased sharply 9 and 17 days after the start of the incubation in the grassland and in the cropped soil, respectively. The above-mentioned anomalous response of the grassland and cropped soils under flooding conditions may be related to the agricultural use of the soils and possibly to the intense use of organic fertilizers in these soils (more than 150 kg N ha−1 year−1 added as cattle slurry or manure, respectively, in the grassland and cropped soils). The observed increase in respiration may either be related to the development of thermophilic facultative anaerobic microbes or to the formation during the incubation period of a readily metabolizable substrate, possibly originating from the remains of organic fertilizers, made accessible by physicochemical processes that occurred during incubation under conditions of high moisture. |
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| Keywords: | Soil respiration Soil emission Flooding conditions Climatic change Soil use |
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