abe 482 lecture 5
TRANSCRIPT
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ABE 482Environmental
Engineering in Biosystems
September 15, 2008Lecture 5
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Today
Composting
Definition, types of composting,pros/cons
Required conditions
C/N, oxygen, moisture, temperature, pH
Physical properties
Particle size distn, density, porosity andairspace, moisture content
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Definition
Composting: A controlled process in which
aerobic, thermophilic microorganismsconvert organic material into a hygienic,biostable, humus-like product.
Organic Matter Compost
Microbes Water Oxygen
Heat Water CO2
What is organic matter made up of??
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Types of Composting
Natural
Leaves, grass, twigs on forest floor
Planned
Static piles/windrows Aerated piles
Channels
In-vessel or bin
What is the difference between decomposing and composting?
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Natural composting
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Static piles/windrows
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Aerated static pile/windrow
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Channel composting
In-vessel or bincomposting
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Pros/Cons of Composting
Pros
Mass/volume reduction (approx 50%)
Pathogen and weed seed reduction (ifthermophilic for >4 days)
Useful/marketable product with fertilizervalue, good water holdling capacity,reduced bulk density and erosion control
value Stabilize putrescible material by reducing
BOD, smell, pollutants
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Pros/Cons of Composting
Cons
Requires time, money and space
Lack of site availability
Lack of suitable materials
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Conditions Required for Composting
C:N ratio for microorganism activityand growth
Oxygen levels that support aerobic
organisms Moisture to permit biological activity
without hindering aeration
Temperature for vigorous microbialactivity from thermophilic organisms
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Carbon and Nitrogen
Carbon
Needs to be available to microbes
1/3:1/3:1/3 organisms, metabolism, heat
brown, dry ingredients
Nitrogen Major nutrient needed by microbes for
assimilating carbon (protein and reproductivity)
Takes 25-30 units of C for every unit of N
green, wet ingredients
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C:N Ratio
Optimum C:N = 25-30
If C:N too low, not all N is utilized ammonia given off smelly
If C:N too high, process is slowed left with undecomposed substrate
Organic carbon and nitrogen contents
of ingredients can be analyzed in lab
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Oxygen
Required for aerobic microbes to live
Require approximately 5-20% oxygencontent to sustain aerobic microbes
Can be measured using oxygen probeor calculate from airspace content
What percentage of air is made of up oxygen?
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Moisture (cont)
If pile too wet, can turn anaerobic
Pore spaces fill with water instead of air Structure degrades, leads to excessive compaction Excessive moisture leachate nitrate and
pollutant runoff
If pile becomes too dry, cannot support microbial
populations, activity stops TMECC (Test Methods for the Examination of
Compost and Composting) suggests drying samples(approx 500 g) in oven at 705C for 24 hours todetermine gravimetric moisture content
ASTM specifies 105C for 16 hours
What are some other ways to measure moisture content?
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pH
Want preferred range of 6.5-8.0
Tends to fall at start due to organic acid production If pH too high, tends to encourage ammonia
volatilization (loss of N and smelly)
Let pile go anaerobic for awhile (really??)
If pH too low, pile becomes acidic and microbe activityis slowed
Add lime
Measure pH by making a slurry and use pH meter(use 2 slurry dilutions and extrapolate to zerodilution)
What does the pH versus time relationship look like?
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Temperature
Best indicator of activity
Prefer pile to be active (>40C) forabout a week
Compost temperatures can reachthermophilic range even in -30Cweather
20C-40C Mesophilic range
40C-60C Thermophilic range
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20C
40C
60C
Temp
Time2-3 days 1 week
Thermophilic
Mesophilic
Mesophiles die off
High rate composting
Active Curing
Compost Temperature Evolution with Time
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Physical Properties of Compost
Properties: particle size, density,porosity, etc.
Proper management will ensure
Microbes can access sufficient substratesto satisfy metabolism and multiply
A suitable environment exists (enoughO
2
)
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Next Day
Physical properties of compost
Density
Porosity and airspace
Composting material andamendments
Calculation examples
Compost maturity