Journal
SCIENCE OF THE TOTAL ENVIRONMENT
Volume 613, Issue -, Pages 1196-1206Publisher
ELSEVIER
DOI: 10.1016/j.scitotenv.2017.09.170
Keywords
Carbon sequestration; Surface mining; Reclaimed mine soils
Categories
Funding
- Foundation for Public Welfare of the Ministry of Land and Resources of the People's Republic of China [201411017]
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The reclamation of discarded spoils has the potential to stimulate carbon (C) sequestration in reclaimedmine soils (RMSs). Nevertheless, to date the temporal dynamics of labile organic C fractions have not been sufficiently elucidated in RMSs. In this study, soil organic carbon (SOC) and labile organic C fractions, including microbial biomass organic C (MBC), easily oxidizable organic C (EOC) and dissolved organic C (DOC), were determined in Robinia pseudoacacia monoculture forests (reclamation periods of 0, 8, 10, 13, 15, 18 and 30 years), Pinus tabuliformis forests (reclamation periods of 0, 10, 19, 23 and 25 years) and Ulmus pumila forests (reclamation periods of 0, 18, 20 and 22 years) situated on RMSs in the Pingshuo opencast coal mine, China. Changes in labile organic C fractions within the soil profiles (0-100 cm) were also identified at the 18-or 19-year plots under the three monoculture forests. Our results showed that, SOC and labile organic C fractions, together with soil microbial quotient (SMQ) and C management index (CMI), increased with time since reclamation, indicating that the quality of RMSs improved over time after initial reclamation under the three forest types. R. pseudoacacia significantly increased the accretion of SOC and EOC in the early stage of reclamation while P. tabuliformis accelerated the accumulation of the MBC fraction. Results for U. pumila indicated that this species had a better ability to store C in RMSs 10 years or more after reclamation. SOC and labile organic C fractions both had S-shaped distributions within the soil profiles (0-100 cm), with the 0-20 cm layer recording the highest values (P < 0.05). Labile organic C fractions were closely associated and correlated with soil physicochemical properties; our results also showed that nitrogen played an important role in the development of labile organic C fractions. Overall, reclamation accelerated the accretion of both SOC and labile organic C fractions, results of which varied among the reclaimed forests. (C) 2017 Elsevier B.V. All rights reserved.
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