Abstract
Relationships between within-year variations in Fe(II)/Fe(III) ratio in silt pore solution were obtained. The samples to be examined were taken from silts of the channel zone of the Krasnovidovo Pool, the Mozhaisk Reservoir. Specific features of the within-year redistribution of Fe forms in the pore solution of the sediment column were identified.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
