(Materials & methods
to ensure quality compost)
There
are some essential factors involved in determining what type of
pile to build and how to manage the feedstocks. Organisms cannot
decompose organic material as efficiently without certain requirements,
such as air, water and appropriate particle size. Following are the
most important considerations.
carbon-nitrogen
relationships
The
course of decomposition of organic matter is affected by the
presence of carbon and nitrogen. The C:N ratio represents the relative
proportion of the two elements. A material, for example, having 25
times as much carbon as nitrogen is said to have a C:N ratio of 25:1,
or more simple, a C:N ratio of 25. Actually, the ratio of available
carbon to available nitrogen is the important relationship because
there may be some carbon present so resistant to biological attack
that its presence is not significant.
Organisms that decompose organic matter use carbon as a source of
energy and nitrogen for building cell structure. They need more carbon
than nitrogen. If there is too much carbon, decomposition slows when
the nitrogen is used up and some organisms die. Other organisms form
new cell material using their stored nitrogen. In the process more
carbon is burned. Thus the amount of carbon is reduced while nitrogen
is recycled. Decomposition takes longer, however, when the initial
C:N ratio is much above 30.
 In the soil,
using organic matter with excess carbon can create problems. To
complete the nitrogen cycle and continue decomposition,
the microbial cells will draw any available soil nitrogen in the
proper proportion to make use of available carbon. This is known
as "robbing" the soil of nitrogen, and delays availability
of nitrogen as a fertilizer for growing plants until some later season
when it is no longer being used in the life-cycles of soil bacteria.
When
the energy source, carbon, is less than that required for converting
available nitrogen into protein, organisms make full use of the available
carbon and get rid of the excess nitrogen as ammonia. This release
of ammonia to the atmosphere produces a loss of nitrogen from
the compost pile and should be kept to a minimum.
A C:N ratio
of 20, where C and N are the available quantities, is the upper
limit at which there is no danger of robbing the soil of
nitrogen. If a considerable amount of carbon is in the form of lignin
or other resistant materials, the actual C:N ratio
could be larger than 20. The C:N ratio is a critical
factor in composting to prevent both nitrogen robbing from the soil
and conserving maximum
nitrogen in the compost..
Since organisms use about 30 parts carbon for each part of nitrogen,
an initial C:N (available quantity) ratio of 30 promotes rapid composting
and would provide some nitrogen in an immediately available form
in the finished compost. Researchers report optimum values from 20
to 31. A majority of investigators believe that for C:N ratios above
30 there will be little loss of nitrogen. University of California
studies on materials with a initial C:N ratio varying from 20 to
78 and nitrogen contents varying from 0.52% to 1.74% indicate that
initial C:N ratio of 30 to 35 was optimum. These reported optimum
C:N ratios may include some carbon which was not available. Composting
time increases with the C:N ratio above 30 to 40. If unavailable
carbon is small, the C:N ratio can be reduced by bacteria to as low
a value as 10. Fourteen to 20 are common values depending upon the
original material from which the humus was formed. These studies
showed that composting a material with a higher C:N ratio would not
be harmful to the soil, however, because the remaining carbon is
so slowly available that nitrogen robbery would not be significant.
CARBON NITROGEN (C:N) RATIOS IN FEEDSTOCKS
Plant residues are made up largely of the following: |
1. sugar, starch, simple proteins
|
(decompose
rapidly) |
2. crude protein
|
(decompose
slowly |
3. hemicellulose
|
(decompose
slowly |
4. cellulose
|
(decompose
slowly |
5. lignin, fat, wax, etc.
|
(decompose
slowly |
Rate
of decay and release of nutrients to the soil vary greatly. Likewise,
demands of living soil microorganisms
vary as they "break down" plant residue. Sawdust (made
primarily of lignin and cellulose) uses vast amounts of energy to
maintain the lives of microorganisms digesting it. A major product
of plant decay is nitrogen (N) while the undigested portion is primarily
carbon (C).
The optimum ratio in soil organic matter is about 10 carbons to
1 nitrogen, or a C:N ratio of 10:1.
Following are some sample C:N ratios of organic matter:
Sandy loam (fine) |
7:1 |
Humus |
10:1 |
Food scraps |
15:1 |
Alfalfa hay |
18:1 |
Grass clippings |
19:1 |
Rotted manure |
20:1 |
Sandy loam (coarse) |
25:1 |
Vegetable trimmings |
25:1 |
Oak leaves |
26:1 |
Leaves, varies from |
35:1
to 85:1 |
Peat moss |
58:1 |
Corn stalks |
60:1 |
Straw |
80:1 |
Pine needles |
60:1
to 110:1 |
Farm manure |
90:1 |
Alder sawdust |
134:1 |
Sawdust weathered 3 years |
142:1 |
Newspaper |
170:1 |
Douglas fir bark |
491:1 |
Sawdust weathered 2 months |
625:1 |
|