Chapter8_KEY
Types of Lakes
Ice block lakes: Formed by buried ice blocks melting after glacial retreat, creating kettle lakes.
Oxbow lakes: Created through differential erosion and sedimentation that leads to meandering rivers forming U-shaped lakes cut off from the river during flooding.
Dams of glacial lakes: Occur when natural drainage ways are blocked, forming a lake.
Lakes at confluence of two rivers: Formed by blockages in channels resulting in water buildup (e.g., Lake Pepin).
Lake Distribution in Minnesota
Very few lakes: Southern region (prairie).
Few lakes: Driftless region (southeast MN) not covered by recent glaciers.
Most lakes: Northern region.
Very shallow lakes: Prairie region.
Narrow lakes with steep rocky shorelines: Northeastern and BWCAW region.
Physical and Chemical Characteristics
Water chemistry influenced by:
Drainage basin (parent rock).
Runoff and groundwater.
Chemistry modified by:
Depth and size of the lake.
Soil, land use, pollution.
Nutrient Influence on Algae Growth
Phosphorus and nitrogen function as limiting resources for algae and aquatic plant growth.
Increased phosphorus leads to greater productivity in lakes.
Factors Affecting Light and Transparency
Reduced light in winter due to:
Snow cover.
Ice.
Reduced transparency caused by:
Water color (e.g., tea-like coloration from leaves).
Suspended material (sediment and algae).
Measurement of water clarity: Secchi disk method.
Oxygen Dynamics in Lakes
Oxygen sources/removers:
Summer: Photosynthetic organisms add oxygen; animals and heterotrophs remove it.
Winter: No addition; consumption by organisms occurs at all levels.
Temperature Profiles in Lakes
Summer Stratification:
Epilimnion: Warmed by the sun, mixed by wind.
Thermocline: Sharp temperature decline.
Hypolimnion: Cold, stable layer below.
Fall and Spring Turnover Events: Mixes temperature layers, especially as temperatures reach 39°F, where water is densest.
Winter behavior: Ice seals lakes, keeping sunlight and wind out.
Lake Zones and Ecosystem Roles
Labeling Zones:
Benthic, profundal, pelagic, and littoral zones.
Littoral Zone Benefits:
Provides habitat and infuses water with oxygen.
Consumers: Invertebrates (caddisfly larvae, scuds), small fish, snails, muskrats.
Ecological Role of Zooplankton
Example: Water fleas (Cladocera) feed on phytoplankton, increasing water clarity when abundant.
Filter feeders: Organisms collecting food while allowing water to pass through.
Examples: Copepods and rotifers.
Hypolimnion Environment
Conditions: Cold, dark (aphotic), lacking photosynthetic organisms.
Organisms: Fish preying on invertebrates, detritivores (e.g., protozoa, bacteria).
Lake Productivity and Aging
Types of lakes:
Oligotrophic: Deep, cold, high DO, low nutrients, high clarity, low productivity.
Eutrophic: Shallow, high nutrient levels, high productivity, lower clarity.
Aging process: Succession from oligotrophic to eutrophic, with sedimentation leading to increased nutrient levels.
Cultural Eutrophication and Restoration
Reducing eutrophication: Slowing nutrient input, restoring banks and wetlands.
Case Study: Lake Superior
Characteristics:
1,333 feet deep; 21,280 sq. miles; largest freshwater lake in N. America.
Cold, well oxygenated, oligotrophic, low productivity.
Lake Contamination
Sources of contamination: Sediment, surface runoff, sewage, industrial wastes, atmospheric deposition, nitrogen, phosphorus from farmlands, invasive species.
Progress in pollutant reduction: Notable progress for point sources; nonpoint pollutants remain challenging.
Contaminants of Emerging Concern
Examples: Pharmaceuticals, personal care products (e.g., DEET, cotinine).
Lake Restoration Success - Chain of Lakes, Minneapolis
Restoration efforts: Clean Water Partnership focused on reducing sediment and nutrient pollution and increasing public awareness, leading to improved water quality in three of four lakes.