Limnology 3 - Lake Nutrients PDF

Summary

These lecture notes cover limnology, specifically focusing on lake nutrients and the chemistry of lakes. They discuss various aspects, including zones, stratification, chemical variations, cultural eutrophication, and nutrient cycles. The notes also include case studies of specific lakes.

Full Transcript

School of Environment and Geomatics ENVR 150 Review Dimictic Lakes  Zones  Midsummer Stratification  Photic  Epilimnion  Aphotic  Metalimnion (thermocline)  Littoral  Hypolimnion  Pelagic  Fall overturn ...

School of Environment and Geomatics ENVR 150 Review Dimictic Lakes  Zones  Midsummer Stratification  Photic  Epilimnion  Aphotic  Metalimnion (thermocline)  Littoral  Hypolimnion  Pelagic  Fall overturn  Temp  Isothermal  4◦c  Winter Stratification  Fetch  4◦c at bottom 0◦c at top  Early Spring  Isothermal  Early Summer Lake Chemistry  Chemistry impacted by  Size of watershed  Climate  Geology (karst) Lake Karachay, Russia Dumping spot for nuclear waste Chemistry  Concerns  pH (too acidic or too basic)  Sulfates and Nitrates (SO4-2 & NO3)  Acid Rain (Sulfur dioxide)  Heavy metals eg. Mercury (Hg) Powdered lime  Bioaccumulation in aquatic webs  Oil spills  Salt (NaCl) concentrations  Nutrients(N & P)  Pollutants  Point Source  Non-Point Source  Cumulative Lan County, Sweden Dead Lake from Acid Rain Fundamentals of Environmental Measurements http://www.fondriest.com/environmental-measurements/parameters/water-quality/ph/ Chemical Zonation  Horizontal variations  Concentrations close to shorelines  Algal blooms, plant and animal concentrations  Wave action mixes sediments and erodes shoreline  Overland flow and ground water bring nutrients from  weathering, landslides,fires  fertilizers, land clearing, urbanization  Vertical Variations  Chemocline - A rapid vertical change in water chemistry  Salts – Summit Lake, Kitlope Lake  Annoxic conditions - Sannich Inlet (225 m deep)  Purple sulfur bacteria – need both sunlight and H2S produced by anaerobic bacteria, Mahoney Lake Stratification can cause pH levels within a body of water to differ above and below the cline. Kitlope Lake Green color / salt on the bottom and freshwater layers Laguna Verde and Licancabur Volcano, Bolivia, sediments, containing copper minerals Laguna Colorada Bolivia Shallow salt lake – red sediments and red algae, contrasted with white islands Exploding lakes  Lake Nyos, Cameroon August 21, 1986 belched carbon dioxide and killed between 1,700 people and 3,500 livestock Surface Area 1.58 km2 Depth 208 m Active Volcanic Crater 500 yrs old Lake Kivu, Cameroon Methane + CO2 (500 million tons of Carbon in the lake ) 2% of humans annual emissions 2 million people living in basin Nutrient supply  “Nutrients” N (nitrogen) P (phosphorous)  A low level of nutrients means that N or P is absent  Limiting factors for growth and production of  Algae  Phytoplankton  Zooplankton  Fish  Nutrient Retention Time  How long a particular nutrient is held in a lake  Often reflects HRT  But nutrients can also be consumed by or changed in form by organisms The Phosphorus Cycle Nitrogen Cycle Oligo-Eutro classification scheme  Succession of Lakes  oligotrophic > mesotrophic > eutrophic > marsh > land  Oligotrophic Lakes  Poorly supplied with nutrients  Support little plant growth  Biological productivity is low  Waters are clear, blue-green  Secchi disk depth of 15 m<  Large, deep, cold, steep  Lots of DO at deepest layers throughout the year Oligo-Eutro classification scheme  Mesotrophic Lakes  Moderately well supplied with plant nutrients  Support moderate plant growth  Secchi disk depth of 7.5 - 15 m Eutrophic Lakes Richly supplied with nutrients Abundant plant growth Biological productivity high (plankton, algae, macrophytes) Waters are turbid green/yellow Secchi disk depth is < 7. 5 m Small, shallow, warm lakes Reduced DO during stratification Eutrophication  Natural eutrophication  slow and gradual process  occurring over many centuries  production and consumption out of balance  lake slowly becomes over fertilized  Cultural eutrophication  green algae and other microorganisms  human-generated fertilization of water bodies  nitrates and phosphates  treated sewage  runoff from farms and urban areas  eventually lake dies How would you classify Kootenay Lake?

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