Soil microbiological attributes indicate recovery of an iron mining area and of the biological quality of adjacent phytophysiognomies

dc.creatorSilva, Aline Oliveira
dc.creatorCosta, Amanda Monique da
dc.creatorTeixeira, Anita Fernanda dos Santos
dc.creatorGuimarães, Amanda Azarias
dc.creatorSantos, Jessé Valentim dos
dc.creatorMoreira, Fatima Maria de Souza
dc.date.accessioned2019-04-01T16:44:13Z
dc.date.available2019-04-01T16:44:13Z
dc.date.issued2018-10
dc.description.abstractMining activities modify the landscape and may have severe environmental impacts. The degree of recovery or disturbance of these environments must be determined, and microbiological indicators are most sensitive for this evaluation. The aim of this study was to evaluate the soil microbiological attributes of an area rehabilitated after iron mining activities and evaluate the adjacent phytophysiognomies. Soil samples were collected in a rehabilitated area revegetated with grass (RA) and in the phytophysiognomies of ironstone outcrops (IO), of neotropical savanna (NS), and of Atlantic Forest (AF) in two climate seasons (dry and rainy). Microbial biomass carbon, soil respiration, and enzyme activities (β-glucosidase, acid and alkaline phosphatase, arylsulfatase, urease, fluorescein diacetate hydrolysis) were determined, and the metabolic quotient (qCO2), the microbial quotient (qMic), and specific enzyme activities were calculated. Analyses of variance, means testing, and principal component analysis between the soil microbiological and physicochemical attributes were carried out. The microbiological indicators differed according to the type of phytophysiognomy and the season. Enzyme activities, microbial biomass, qCO2, soil respiration, and qMic were sensitive in indicating differences among the phytophysiognomies, as well as organic carbon, total N, Fe, Cu, and Al3+ contents, pH, potential acidity, cation exchange capacity, and clay and sand contents. The IO and NS phytophysiognomies exhibited the highest organic carbon and total N contents, whereas AF, NS, and IO exhibited the highest values of microbial biomass carbon. In both climate seasons, the AF exhibited higher values of soil respiration and enzyme activities. The Ironstone Outcrops exhibited high microbial biomass that was active in the processes of nutrient cycling, shown by its enzyme activities, whereas lower values of microbial biomass carbon and enzymes and higher values of qCO2 were observed in RA. Nevertheless, RA exhibited higher specific enzyme activities and higher qMic, indicating that the process of revegetation with grass favors activity of the microbial community, and promotes recovery of this area.pt_BR
dc.identifier.citationSILVA, A. O. et al. Soil microbiological attributes indicate recovery of an iron mining area and of the biological quality of adjacent phytophysiognomies. Ecological Indicators, [S. l.], v. 93, p. 142-151, Oct. 2018.pt_BR
dc.identifier.urihttps://repositorio.ufla.br/handle/1/33421
dc.identifier.urihttps://www.sciencedirect.com/science/article/pii/S1470160X18303273#!pt_BR
dc.languageen_USpt_BR
dc.publisherElsevierpt_BR
dc.rightsrestrictAccesspt_BR
dc.sourceEcological Indicatorspt_BR
dc.subjectBioindicatorspt_BR
dc.subjectClimate seasonpt_BR
dc.subjectIronstone outcropspt_BR
dc.subjectRehabilitated areaspt_BR
dc.subjectNeotropical savannapt_BR
dc.subjectAtlantic forestpt_BR
dc.subjectBioindicadorespt_BR
dc.subjectTemporada climáticapt_BR
dc.subjectÁreas reabilitadaspt_BR
dc.subjectSavana neotropicalpt_BR
dc.subjectMata Atlânticapt_BR
dc.titleSoil microbiological attributes indicate recovery of an iron mining area and of the biological quality of adjacent phytophysiognomiespt_BR
dc.typeArtigopt_BR

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