Abstract
A one-year study was made of the salt concentrations of rainfall and the static water table across the lower Rio Grande Valley of Texas. A linear decrease in salt concentration was observed with logarithmic distance inland. The concentrations of individual ions determined, except calcium, follow the logarithmic relationship. The salt content of the shallow saline groundwater also decreases with distance inland. The decline in groundwater salt concentration with distance inland was more rapid than the decline in annual salt deposition by rainfall. /Author/
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.
