Abstract
Even a superficial attempt to record the earlier studies on the Firth of Forth brings out the importance of the Royal Society of Edinburgh in supporting research on the underlying principles of estuarine water conditions.My bibliography starts with the Transactions of that society for 1816, though it is not until 1884, with the studies of H. R. Mill, that we come to work which is really useful to our present purpose. Mill worked from a floating laboratory at Granton Sea Quarry. He carried out twice-daily observations at the Quarry, and systematic observations over a long period at 12 stations in mid-Firth, from Alloa to the Isle of May, and also at several points on the south coast. He reports on variations (largely seasonal) in temperature and on density as an index of salinity, and on the alkalinity of the water. These latter, of course, vary largely with the river inflow, which has a rather imprecise correlation with season.
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 callMore From: Proceedings of the Royal Society of Edinburgh. Section B. Biology
Disclaimer: 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.
