Growing vegetables is much more demanding than growing most perennial ornamentals or lawns.  Excuse me, flower gardeners, but I’ve observed that even most flowers will thrive if only slight improvements are made in their soil.  The same is true for most herbs.  Difficulties with ornamentals or herbs are usually caused by attempting to grow a species that is not particularly well-adapted to the site or climate.  Fertilized with sacked steer manure or mulched with average-to-poor compost, most ornamentals will grow adequately.

But vegetables are delicate, pampered critters that must grow as rapidly as they can grow if they are to be succulent, tasty, and yield heavily.  Most of them demand very high levels of available nutrients as well as soft, friable soil containing reasonable levels of organic matter.  So it is extremely important that a vegetable gardener understand the inevitable disruption occurring when organic matter that has a C/N is much above 12:1 is tilled into soil.

Organic matter that has been in soil for a while has been altered into a much studied substance, humus.  We know for example that humus always has a carbon to nitrogen ratio of from 10:1 to about 12:1, just like compost from Garden “B.”  Garden writers call great compost like this, “stable humus,” because it is slow to decompose.  Its presence in soil steadily feeds a healthy ecology of microorganisms important to plant health, and whose activity accelerates release of plant nutrients from undecomposed rock particles.  Humus is also fertilizer because its gradual decomposition provides mineral nutrients that make plants grow.  The most important of these nutrients is nitrate nitrogen, thus soil scientists may call humus decomposition “nitrification.”

When organic material with a C/N below 12:1 is mixed into soil its breakdown is very rapid.  Because it contains more nitrogen than stable humus does, nitrogen is rapidly released to feed the plants and soil life.  Along with nitrogen comes other plant nutrients.  This accelerated nitrification continues until the remaining nitrogen balances with the remaining carbon at a ratio of about 12:1.  Then the soil returns to equilibrium.  The lower the C/N the more rapid the release, and the more violent the reaction in the soil.  Most low C/N organic materials, like seed meal or chicken manure, rapidly release nutrients for a month or two before stabilizing.  What has been described here is fertilizer.

When organic material with a C/N higher than 12:1 is tilled into soil, soil animals and microorganisms find themselves with an unsurpassed carbohydrate banquet.  Just as in a compost heap, within days bacteria and fungi can multiply to match any food supply.  But to construct their bodies these microorganisms need the same nutrients that plants need to grow—­nitrogen, potassium, phosphorus, calcium, magnesium, etc.  There are never enough of these nutrients in high C/N organic matter to match the needs of soil bacteria, especially never enough nitrogen, so soil microorganisms uptake these nutrients from the soil’s reserves while they “bloom” and rapidly consume all the new carbon presented to them.