Aquatics Flashcards
Water: def
medium of which all chemical processes occur; aquatic organisms depend heavily on water
Water: molecular composition
polar: good solvent
hydrogen bonds: surface tension
Water: specific heat
- water has high specific heat capacity
- strong hydrogen bonds are able to absorb lots of thermal energy before changing temperature
Water: density
- like all liquids, density increases as it cools
- max density: 3.98 degrees C
- however water becomes less dense when it freezes because of hydrogen bonds
Water: why is ice less dense than water?
- H bonds: molecules arrange into crystalline structure that increases spaces between individual molecules
- ice will float on top of liquid before extending down
- so in winter, ice will reach 2-5 meters max
Water: turbidity def
the greater amount of total suspended solids (TSS) in water, the murkier it appears and the higher the turbidity
Water: sources of turbidity
- sources of turbidity include phytoplankton, clays from erosion, etc.
- increased flow rates, floods, or too many bottom feeding fish may stir up bottom sediments
Water: impact of turbidity on aquatic organisms
- modify light penetration affecting photosynthesis = less oxygen in water & growth of macrophyth (food chain)
- organic materials collect at bottom, suffocating eggs
- may also damage gill structure, decrease organism’s resistance to disease, prevent proper egg development
Water: impact of turbidity on humans
- we don’t like the aesthetic
- costs $ to treatment of surface water for drinking (must get rid of heay metals)
Water: types of junk for turbidity
- Algae
- Detritus (dead organic material from dead algae, bacteria, plants, fungi)
- Silt (inorganic mineral, suspended sediment)
Water: nephelometric turbidity units (NTUs)
- how we measure turbidity (400+ is real turbid)
- nephelometric: turbidimeter estimates amount of TSS
Water: ways to measure turbidity
- Secchi disk
- circular plate divided into quarters painted black and white
- attached to rope and lowered into water until no longer visible
- higher secchi readings = clearer water
- in spring, lower secchi readings because algae flourish - Turbidity tube
- look through tube at black and white disk and record how much water is needed to make disk disappear
Water: stream flow def + factors + affects
- volume of water that passes through specific point in river/stream
- affects temp of water + concentration of various substances in water + oxygen levels (low flow = higher temperatures, higher temperatures = liquids cannot dissolve O2)
- factors include precipitation and vegetation (increases time for water to reach stream by infiltrating it)
Water: carbon dioxide
- sources: atmosphere, biological activity, breakdown of limestone
- carbon isn’t limited but may fluctuate as photosynthesis cycles come and go (high photosynthesis = lower C, high decomposition = higher C)
Water: buffering capacity (carbon dioxide from breakdown of limestone)
- CO2 is often from bicarbonates from limestone
- benefits by buffering water against shifts in pH
- eg. acid + water = hydrogen ions will combine to bicarbonate to prevent change in pH
Water: pH
- determines solubility and biological availability (nutrients that can be used that can be used by organisms)
- pollution + photosynthesis changes pH
Water: hardness
amount of dissolved solids (calcium, calcium carbonate, magnesium)
water is soft = less than 10 ppm
water is hard = more than 40 ppm (therefore more living matter)
Water: temperature
- aquatic organisms are poikilothermic (unable to regulate body temperature)
- higher temp = greater biological activity
- temperature influences what organisms will thrive and water chemistry (more chemical reactions when hotter)
- reasons for variation: seasonal temperature which causes thermal stratifcation
Water: thermal stratification
- surface water is warmed by sun but bottom of lake is cold
- epilimnion: top water layer
- hypolimnion: deep cool layer