Abstract
The ratio of the spatial and temporal distribution of dissolved organic carbon to acid neutralizing capacity in the surface waters of the Lake Baikal Basin was studied. This ratio reflects the geological and geographical conditions of the watershed. In the warm season, the ratio depends on the watershed's size and relief; in the cold season, it depends on the watershed's chemistry. The ratio was used to estimate the contributions of dissolved matter sources, such as subsoil, topsoil, and the atmosphere, to the surface water. A correlation analysis was performed to establish relationships between the sources and solutes. The processes with the greatest effect on water chemistry were determined by analyzing these relationships.
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.
