2017
DOI: 10.1007/978-3-319-43394-3_14
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Soil Organic Carbon Stocks and Soil Respiration in Tropical Secondary Forests in Southern Mexico

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Cited by 20 publications
(11 citation statements)
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“…The lower CO 2 fluxes at the abandoned pasture site were related to differences in soil and vegetation characteristics as indicated by lower soil C and N concentrations and by lower stem number and basal area (Table 1). Aryal et al (2017) also related higher soil respiration rates in Mexican mature forests and secondary forests (>35 yr) compared with younger secondary forests (<20 yr) to differences in substrate availability and microclimate conditions created by the vegetation. Root density and root biomass also vary over the course of forest succession, which contributes to differences in soil respiration rates between forest stages (e.g., Yan et al, 2006).…”
Section: Discussionmentioning
confidence: 98%
“…The lower CO 2 fluxes at the abandoned pasture site were related to differences in soil and vegetation characteristics as indicated by lower soil C and N concentrations and by lower stem number and basal area (Table 1). Aryal et al (2017) also related higher soil respiration rates in Mexican mature forests and secondary forests (>35 yr) compared with younger secondary forests (<20 yr) to differences in substrate availability and microclimate conditions created by the vegetation. Root density and root biomass also vary over the course of forest succession, which contributes to differences in soil respiration rates between forest stages (e.g., Yan et al, 2006).…”
Section: Discussionmentioning
confidence: 98%
“…Aryal et al . (2017) reported that the soil CO 2 fluxes were correlated with the carbonate content of the soil and not with soil organic matter, indicating that the abiotic carbon exchange could significantly influence soil CO 2 fluxes. However, we did not separate the abiotic fluxes in this study.…”
Section: Discussionmentioning
confidence: 99%
“…Recent estimates indicate a net release of C between 0.42 and 1.60 Pg/year in the tropics because of the deforestation, of which, 0.1–0.3 Pg is because of the loss of soil organic matter (Xu & Qi, 2001; Zimmermann et al ., 2009). Besides, the release of C occurs in a context of high spatial and temporal variability attributed to the structure and composition of species, age, management practices, climatic and edaphic conditions (Villanueva‐López et al ., 2016a, 2016b; Aryal et al ., 2017; Nocentini & Monti, 2019).…”
Section: Introductionmentioning
confidence: 99%
“…Lo anterior puede atribuirse a los siguientes factores: i) el carbono orgánico del suelo es un reservorio más estable y es afectado, lentamente, por el cambio de uso suelo, patrones que también se han observado en otros estudios realizados en el sur-sureste mexicano (Orihuela-Belmonte et al, 2013;Aryal et al, 2015, Villanueva-López et al, 2016Aryal et al, 2017).…”
Section: Abundancia De Los áRbolesunclassified