Notes for In Conclusion…<\/p>\n
1. Some background to my involvement. I was a faculty member of the Biology Department at Dalhousie University 1973-2008, with specialization in coastal marine biology, plant and microbial ecology; since retirement I have been active in several natural history and trail organizations (more details here<\/a>).\u00a0 In the late spring of 2017, I was asked by the Sandy Lake Conservation Association<\/a> if I would do a \u201cflora survey\u201d of Sandy Lake and Environs for along the lines I had conducted on the Williams Lake Backlands in 2013\/2014<\/a>. I agreed and conducted field trips on 22 days over the period June 14 to Nov 1, 2017; a few were mostly on water (paddling), most were on land. It was a volunteer activity, there was no payment and no contract. As a component of that study and because I was familiar with limnological techniques and out of curiosity, on Oct 3, 2017\u00a0 I conducted\u00a0 limnological observations at 3 points in Sandy Lake\u00a0 with the help of a local volunteer.\u00a0 The results\u00a0 raised some concerns. In the late fall of 2017, I realized that far more observations – and time – were needed to adequately describe “Sandy Lake & Environs” at large. So\u00a0 rather than submit a single final report, I would post observations and related info on a website –\u00a0Sandy Lake & Environs (Bedford, Nova Scotia)<\/a> – on an ongoing basis. The website was launched on Dec 20, 2017<\/a>. I posted a “A DRAFT Report On the\u00a0 State of Sandy Lake, the Historical Trends and its Future Trajectory” on Feb 23, 2021<\/a> which integrated all limnological observations to that point, but observations have been continuing and are reported in the section Surface Waters<\/a> and it subpages.<\/small><\/p>\n 2. Detales in other pages:<\/p>\n 2. The limnological profiles consist of measurements made with a Water Quality Multimeter of temperature, conductivity (a measure of salt content), oxygen and (sometimes) pH at 1 meter or shorter depth intervals. Beginning in August of 2022, we conducted our observations under the umbrella of the newly formed HRM LakeWatchers program<\/a>, which allowed us to make the observations within more consistent time intervals – prior to that, the equipment was borrowed from community equipment banks and we could not always get it at the desired sampling times. Sandy Lake is one of 72 Lakes that had been “assessed as either highly vulnerable or moderately vulnerable through a previous study<\/a>” and were selected initially to be included in the LakeWatchers Program. The Vulnerability Class for Sandy Lake was “Class A – High Vulnerability” and the Priority Concerns concerns were identified as “Eutrophication” and “Bacteria Contamination (Beaches)” – Table 9, p 53 in HRM Water Quality Monitoring Policy and Program Development (AECOM 2020) In addition to the Limnological profiles at the deepest spot in the lake, the observations include secchi disk (a measure of water transparency), top and near-bottom water samples analyzed for TP (Total Phosphorous, deep measurement in summer sampling only), chlorophyll-a (surface only) and chloride – 1 m off the bottom, summer sampling only; and Multimeter measurements of and a sample of surface water near the outlet. As Sandy lake is a “Class A \u2014 High Vulnerability Lake”.\u00a0 2 sampling events per year are prescribed (Table 12, p 66) 103. Casey Doucet; inlcude paper.<\/p>\n 104 (Numberg (2004).<\/a><\/p>\n in actuality, Sandy Lake is exhibiting features characteristic of lakes in an upper mesotrophic to eutrophic state [107]<\/p>\n 106 Access to AECOM, not on halifax.ca<\/p>\n 99.Further, the deep water total P value was\u00a0 highly elevated (40 ug\/L) indicating phosphorous mobilization at the sediment surface or occurrence “internal phosphorus loading”, also observed in 2021 and in some earlier years [99]<\/p>\n 100. Spring Total P values in Oligotrophic to low Mesotrophic range: View (i) values of Spring Total P for Sandy Lake 1980 to 2021 in\u00a0 Synoptic snapshots: monitoring lake water quality over 4 decades in an urbanizing region<\/strong>, Supplemental Material<\/a> by Doucet et al. 2023 in Lake and Reservoir Management; (ii) Values for Total P 1979-2014 in AECOM 2014, Fig 8, page 22 (spring values only) & Fig 9, page 24 (all values)\u00a0 (iii) Total P spring values, 2022 onward: Halifax LakeWatchers<\/a>, view link to Lab Results.<\/p>\n 110: See AECOM 2014, 9. Recommendations for Water Quality Monitoring, page 42<\/p>\n <\/p>\n [201] Anoxia begets anoxia: A positive feedback to the deoxygenation of temperate lakes<\/p>\n https:\/\/onlinelibrary.wiley.com\/doi\/10.1111\/gcb.17046<\/p>\n Lakeshore Capacity Assessment Handbook: Protecting Water Quality in Inland Lakes on Ontario\u2019s Precambrian Shield Appendix C : Dorset Environmental Science Centre Technical Bulletins<\/a> chart in Supplemental Materials in<\/p>\n ———-<\/p>\n Canadian Council of Ministers of the Environment. 2004. Canadian water quality guidelines for the protection of aquatic life:<\/a>
\n– once in spring during mixed-water column conditions\u00a0 [our samplings have been in April whihc is\u00a0 at or following spring turnover of the water column]
\n– once at the end of summer [our sampling have been in the latter part of August which is close to the time of peak summer stratification]
\nHalifax Regional Municipality Water Quality Monitoring Policy and Program Development<\/a>, Prepared by: AECOM Canada Ltd., September 2020, 99 pages + Appendices, 505 pages total. Also view Environment & Sustainability Standing Committee June 3, 2021<\/a> SUBJECT: Water Quality Monitoring Policy & Program Development (14 pages)<\/p>\n
\nIncludes: Hypolimnetic Oxygen: Data Collection Strategies For Use In Predictive Models<\/a><\/p>\n
\nPhosphorus: Canadian Guidance Framework for the Management of Freshwater Systems. In: Canadian environmental quality guidelines, 2004, Canadian Council of Ministers of the Environment, Winnipeg<\/p>\n