NR 504 Exam 2|85 Questions with Answers 2023,100% CORRECT

NR 504 Exam 2 Questions with Answers 2023 Water Quality – CORRECT ANSWER Specific characteristics of water defined within the context of its intended use Polluted Water – CORRECT ANSWER When impurities in water are sufficient to render the water as unacceptable for its intended use Compensation Point – CORRECT ANSWER Depth where photosynthesis equals respiration (below this depth photosynthetic organisms can’t survive) Limnology – CORRECT ANSWER Study of lakes Lake Formation Methods – CORRECT ANSWER 1) Tectonic Activity-Volcanoes, Depressions formed by movement of Earth’s crust 2) Rivers (oxbow lakes) 3) Glaciers- formed from gradual erosion and deposition to advancing/retreating glaciers***Great Lakes 2 Systems of Lake Ecological Zones – CORRECT ANSWER Light and Temperature Littoral Zone – CORRECT ANSWER Extends from shore until not enough light to support rooted plants (light) Limnetic Zone (pelagic) – CORRECT ANSWER area beyond influence of shore, photosynthesis occurs by floating microorganisms (light) Profundal Zone – CORRECT ANSWER area of lake where not enough light penetrates for photosynthesis (light) Lake Ecological Zone based on Temperature – CORRECT ANSWER Summer-Stratification (layers) due to temperature differences. Warm less dense water remains at surface–due to density, waters do not mix Fall-turnover of water occurs when density at surface increases, results in mixing of nutrients and dissolved oxygen Summer Stratification–Epilimnion – CORRECT ANSWER mixed layer top/surface water warm/less dense dissolved oxygen is high photosynthesis is dominant Summer Stratification–Metalimnion – CORRECT ANSWER Middle layer, steep thermal gradient (thermocline) Summer Stratification– Hypolimnion – CORRECT ANSWER Deeper water, cold/dense Decomposition dominates low dissolved oxygen Great Lakes – CORRECT ANSWER HOMES Largest system of fresh surface water on earth (~18%) Vulnerable to pollution Outflows less than 1% of volume Wetlands – CORRECT ANSWER Areas of land inundated by water enough to affect soils (hydric) and plants (hydrophytes) Transitional land between terrestrial and aquatic ecosystems Water table is near or at the ground surface or land is covered by water Hydroperiod – CORRECT ANSWER Seasonal pattern of water level in a wetland Importance of Wetlands – CORRECT ANSWER -cleanse polluted water Prevention of floods Protection of shorelines Recharge of aquifers Wildlife habitat Maintain plant and animal diversity Carbon Storage Central and South Florida (C&SF) Project of 1948 – CORRECT ANSWER 1947- 108 inches of water fell on South Florida and ****d everything up Created 720 miles of levees, 1000 miles of canals, 16 pumping stations, 200 water control structures Positive Impacts: Reduce flooding, increased water supply, sugar cane production, water management for SF Negative Impacts: reduced Everglades by 50% Surface flows reduced by 70% Water quality, quantity, and timing modified, loss of habitat, deleterious effects on estuaries and citrus crop Everglades Restoration Project – CORRECT ANSWER Capture most diverted water and deliver to areas where needed. Used mostly for environmental restoration and some for farmers and urban areas. Restore quantity, quality, and timing of water flows Importance of Soil Water Movement – CORRECT ANSWER Irrigation Recharge zones for groundwater Soil as a filter Storage of wastes Flood Predictions Soil – CORRECT ANSWER Porous medium Consists of: Solid (sand, silt, clay, OM) Liquid(water) Gas(air, water vapor, CO2) Porosity – CORRECT ANSWER Amount of void space in a soil Volume of pores / Volume of soil (solid +pores) Soil Moisture Zone – CORRECT ANSWER Region of soil water available to Plants Intermediate Zone – CORRECT ANSWER Transition Zone (water content begins to increase) Capillary Fringe – CORRECT ANSWER Pores are filled with water but water is held by capillary forces Saturated Zone(groundwater zone) – CORRECT ANSWER Pores are filled with water and water moves due to gravity Soil Moisture Properties – CORRECT ANSWER Saturated – all pores are filled with water Volumetric moisture content =porosity Unsaturated= pores contain air and water. Volumetric moisture content < porosity Volumetric Moisture Content – CORRECT ANSWER Volume of water / Volume of soil (cm3/cm3) Equal to porosity when soil is FULLY saturated Field Capacity – CORRECT ANSWER Amount of water held against gravity Water in soil after saturating then draining Permanent Wilting Point – CORRECT ANSWER Soil moisture content at which water is no longer available to plants Available Water (Soil) – CORRECT ANSWER Difference between field capacity and wiling point Forces driving Water movement through soil – CORRECT ANSWER Gravity (pulls water to center of Earth) Capillarity (Rise of water in small tubes against force of gravity) Osmotic Tensions (plant uptake of water) Infiltration – CORRECT ANSWER Movement of rain and melting snow into the soil Rate: Rate at which water enters the soil Capacity: Maximum infiltration rate Infiltration Capacity – CORRECT ANSWER Max. infiltration rate Initially very high in dry soils Decreases as soil gets more wet When reduced below rainfall rate water will accumulate on surface leading to runoff P-Rate > I-Rate Factors Affecting Infiltration Rates – CORRECT ANSWER -Physical Factors of soils (soil permeability, macropores) -Biological (organic content, presence of roots, vegetation presence/type, animal burrows) -Meteorological (storm intensity, antecedent moisture conditions, temperature-water viscosity increases as temp. falls) -Anthropogenic (urbanization, vegetation removal, agricultural methods) Infiltration in Forests – CORRECT ANSWER Very high due to organic matter Rarely does precipitation exceed infiltration Infiltration in Agriculture – CORRECT ANSWER Variable- depends on tilling practices, crop type, grazing Infiltration in Urban – CORRECT ANSWER Low due to impervious cover, promotes flash flooding Groundwater – CORRECT ANSWER Water below the water table Pores are saturated Water flows by gravity (capillary forces are not important) Depth of groundwater varies Aquifer – CORRECT ANSWER Water bearing layer of soil that contains and transmits significant amount of water unconsolidated- sand and gravel Consolidated-limestone, fractured bedrock Aquiclude (aquatard) – CORRECT ANSWER Contains significant water but does not transmit it Low permeability media, clays, shales Confining Unit Aquifuge – CORRECT ANSWER Does not contain or transmit significant quantities of water Confining unit Unconfined Aquifer – CORRECT ANSWER Water table is the upper boundary Water table – CORRECT ANSWER Where pores are filled with water and water pressure is atmospheric Confined Aquifer – CORRECT ANSWER Bounded on top by a confining layer Fluid is under pressure Artesian well-well in which water reaches surface without pumping Perched Aquifer – CORRECT ANSWER Localized zone of saturation associated with a confining layer How does groundwater move? – CORRECT ANSWER Rate at which water moves through aquifers is a function of: -Force doing the pushing (hydraulic head gradient) -The ease with which the soil will allow the water to move (hydraulic conductivity of permeability) q=K(h1-h2/L) Hydraulic Gradient – CORRECT ANSWER Gradient in water table (dh/dl) What can increase groundwater flow rates? – CORRECT ANSWER -increase force doing the pushing (gradient) -increase permeability (decrease resistance to flow) Why is calculating groundwater flow important? – CORRECT ANSWER Avoid over pumping (aquifer mining) Assess pollution sources ***Woburn, MA case study (A Civil Action) Flow direction and flow rate were crucial factors in the trial Calculating Groundwater Flow – CORRECT ANSWER Darcy’s Law Q=KA(h1-h2/L) where Q=discharge (L3/T) K = hydraulic conductivity(L/T) A= Area (L2) h/l= hydraulic gradient (L/L) Calculating Groundwater Velocity – CORRECT ANSWER v=q/n where v=velocity n=porosity q=groundwater movement How are aquifers recharged? – CORRECT ANSWER Recharge Areas- downward movement of water through soil zone to saturated zone unconfined (unsaturated zone above water table) Confined (distant uplands) Groundwater Recharge Types – CORRECT ANSWER Passive (rainfall) Induced (recharge from losing streams, lakes, or wetlands) Artificial (induced recharge by humans) Discharge Areas – CORRECT ANSWER Outward movement of water across water table point where water table intersects the ground surface ‘Gaining’ streams, lakes, wetlands, springs 2 Problems of