Key-words:acid-mine drainage, stream acidification, watershed remediation, water quality, biological recovery Acid mine drainage (AMD) is a prominent threat to water quality in many of the world's mining districts as it can severely degrade both the biological community and physical habitat of receiving streams. There are relatively few long-term studies investigating the ability of stream ecosystems to recover from AMD. Here we assess watershed scale recovery of a coldwater stream from pollution by AMD using a 1967 survey of the biological and chemical properties of the stream as a pre-restoration benchmark. We sampled water chemistry, benthic macroinvertebrates, and fish throughout the watershed during the spring and summer of 2011. Water chemistry results indicated that pH and total alkalinity increased post-restoration, while acidity, sulfate, and iron concentrations decreased. Watershedlevel taxa richness, local taxa richness, biomass, diversity, and density of macroinvertebrates were significantly higher post-restoration; however, %EPT was not significantly different. Fish species richness, density, and brook trout density were all significantly higher post-restoration. These results provide clear evidence that both abiotic and biotic components of streams can recover from AMD pollution.
RĂSUMĂDrainage minier acide et restauration d'une riviĂšre : effets de la restauration sur la qualitĂ© de l'eau, des macroinvertĂ©brĂ©s et des poissons Le drainage minier acide (AMD) est une menace importante Ă la qualitĂ© de l'eau dans de nombreux districts miniers du monde, car il peut endommager gravement Ă la fois la communautĂ© biologique et l'habitat physique des cours d'eau rĂ©cep-teurs. Il y a relativement peu d'Ă©tudes Ă long terme sur la capacitĂ© des Ă©cosys-tĂšmes des cours d'eau Ă rĂ©cupĂ©rer de l'AMD. Ici, nous Ă©valuons la rĂ©cupĂ©ration Ă l'Ă©chelle d'un bassin versant d'un cours d'eau froid aprĂšs pollution par AMD en utilisant un suivi fait en 1967 des propriĂ©tĂ©s biologiques et chimiques de la riviĂšre comme rĂ©fĂ©rence prĂ©-restauration. Nous avons Ă©chantillonnĂ© la chimie de l'eau, les macroinvertĂ©brĂ©s benthiques, les poissons, dans tout le bassin au cours du printemps et de l'Ă©tĂ© 2011. Les rĂ©sultats de la chimie de l'eau ont rĂ©vĂ©lĂ© que le pH et l'alcalinitĂ© totale ont augmentĂ© post-restauration, alors que l'aciditĂ©, les concentrations en sulfate et en fer ont diminuĂ©. La richesse en taxons Ă l'Ă©chelle du bassin versant, la richesse locale en taxons, la biomasse, la diversitĂ© et la densitĂ© des macroinvertĂ©brĂ©s Ă©taient significativement plus Ă©levĂ©es aprĂšs restauration ;