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reservior
defined location and/or form of an element
flux
mass movement in/out of reservior over time (at steady state if min=mout)
two common oxidized forms of carbon
CO2, CO
two reduced forms of carbon
CH4, C6H12O6
oxidizing C atoms releasing useable energy?
aerobic environment (burning methane)
reducing C atoms releasing useable energy?
anaerobic environments (landfills, intestines, wetlands)
reactive nitrogen (Nr)
not stable (NH3,NH4, NO3-, NO2-,N in biomolecules)
one common oxidized form of nitrogen
NO3-
one common reduced form of nitrogen
NH3
nitrogen fixation
N2 to N in biomolecules
nitrification
NH3/NH4 to NO3-
denitrification
NO3- to N2
anthropogenic sources of excess P in water
fertilizer, wastewater, and detergents
major problem by excess P
eutrophication
accumulation term, dm/dt
steady state=0
reaction term, mrxn
no chemical reactions=0
m
mass (kg or g)
m dot
mass flow rate (kg/s, g/min)
Q
volume flow rate (L/min, m³/s)
V
volume (L, m³)
C
concentration (mg/L=ppm, micro/L=ppb)
p
density (g/mL, kg/m³)
k
rate constant (first order) time^-1
advantage of CMFRs over PFR
handles spikes in toxicants well, distrubutes evenly
advantage of PFR over CMFR
more efficient, less materials
limitations of ideal reactor models vs real life
imperfect mixing, non-uniform conditions, non-ideal flow
5 major reserviors in carbon cycle
atmosphere, permafrost, fossil fuel reserves, CO2 gas, biomolecules
major fluxes in carbon cycle
burning fossil fuels +cement production, photosynthesis, respiration, ocean/atmosphere gas exchange
flux increased by fertilizer production
nitrogen fixation
nitrification is more dominant in aerobic environments
bacteria need oxygen to convert NH3 to NO3-
eutrophication
excess N and P are plant fertilizers which cause algae blooms, algae dies and sinks to botttom of lake becoming food for microrganisms, booming microbial population comsumes O2 causing lake to become anerobic, lake cant support animal life and produces smelly byproduct