Abstract
Contents of Corg, as well as humine (HA) and fulvic (FA) acids, have been investigated within soil, riverine and marine sediments along the profile, joining the Razdolnaya River and the Amur Bay. The elevated contents of the Corg. have been elucidated within soil deposits against to riverine and marine sediments, and it is associated with peatlands. There has been noted, that the increase of HA contents against FA ones has been taken place just within those sediments, that has been corresponded the initial period of the water mixing, and it has been connected with flocculation. There have been established the riverine sediments with extended contents of FA, Fe, Mn, and it has testified about the active processes of flocculation and Fe-Mn oxihydroxides forming. It has been noted, that the soil sediments have contained more humiphicated organic matter than marine ones. To a great extent, marine sediments have contained not biogeochemically processed organic matter.
Sign-in/Register to access full text options 
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.
