Ongoing increases in dissolved organic carbon are sustained by decreases in ionic strength rather than decreased acidity in waters recovering from acidic deposition.

MLA

Lawrence, Gregory B., and Karen M. Roy. “Ongoing Increases in Dissolved Organic Carbon Are Sustained by Decreases in Ionic Strength Rather than Decreased Acidity in Waters Recovering from Acidic Deposition.” Science of the Total Environment, vol. 766, Apr. 2021, p. N.PAG. EBSCOhost, https://doi.org/10.1016/j.scitotenv.2020.142529.

APA

Lawrence, G. B., & Roy, K. M. (2021). Ongoing increases in dissolved organic carbon are sustained by decreases in ionic strength rather than decreased acidity in waters recovering from acidic deposition. Science of the Total Environment, 766, N.PAG. https://doi.org/10.1016/j.scitotenv.2020.142529

Chicago

Lawrence, Gregory B., and Karen M. Roy. 2021. “Ongoing Increases in Dissolved Organic Carbon Are Sustained by Decreases in Ionic Strength Rather than Decreased Acidity in Waters Recovering from Acidic Deposition.” Science of the Total Environment 766 (April): N.PAG. doi:10.1016/j.scitotenv.2020.142529.