20150911
Author : Zhou, Z. Y. Xu, M. L. Kang, F. F. Sun, O. J.
Journal : Scientific Reports
Comment : Annual soil respiration varied from 409 g C m−2 in coniferous forest to 570 g C m−2 in mixed forest and to 692 g C m−2 in broad leaved forest, and was markedly explained by mean soil temperatures of the warmest day, July and summer, separately.
These three soil temperatures reflected the maximum values on diurnal, monthly and annual scales. In accordance with their higher temperatures, summer soil respiration accounted for 51% of annual soil respiration across forest types, and broad leaved forest also had higher soil organic carbon content (SOC) and soil microbial biomass carbon content (SMBC), but a lower contribution of SMBC to SOC.
Year : 2015
Title : Maximum temperature accounts for annual soil CO2 efflux in temperate forests of Northern ChinaJournal : Scientific Reports
Comment : Annual soil respiration varied from 409 g C m−2 in coniferous forest to 570 g C m−2 in mixed forest and to 692 g C m−2 in broad leaved forest, and was markedly explained by mean soil temperatures of the warmest day, July and summer, separately.
These three soil temperatures reflected the maximum values on diurnal, monthly and annual scales. In accordance with their higher temperatures, summer soil respiration accounted for 51% of annual soil respiration across forest types, and broad leaved forest also had higher soil organic carbon content (SOC) and soil microbial biomass carbon content (SMBC), but a lower contribution of SMBC to SOC.
댓글
댓글 쓰기