
This is how it works: in each teaspoon of soil are millions and millions of microscopic good-guy organisms: bacteria, fungi, algae, protozoa, nematodes (most of which are not disease-causing, but beneficial), and something called Actinomycetes, which are bacteria that have some fungal-like properties. Add it all up, and you can have more than 75 pounds of these critters in 1000 square feet of healthy soil, not counting the critters you can see, like earthworms and pillbugs and ground beetles. Every day, these invisible life forms are hard at work in your soil, doing important jobs like decomposing plant material, fighting disease-causing organisms, breaking down chemicals, and making nutrients available to plants. Soil microbes fix nitrogen, chelate minerals, and produce nitrogen waste, which plants can then take up through their roots.
So what makes soil microbes happy? Carbon-rich organic matter, particularly plant material, green or brown. For example, kitchen scraps. Or composted leaves. Or aged manure, which is what's left after an animal eats, ruminates and eliminates plant matter. Or cover crops, which are planted and turned into the soil before the next season's planting. Organic matter improves the structure of the soil, making soil more permeable to water and air, and improving its ability to maintain pH (a balance between acidity and alkalinity). This creates an environment where soil microbes can thrive and flourish.
Good soil teeming with microbes makes for happy plants. Some soil microbes have a symbiotic relationship with plant roots: the roots secrete stuff that the microbes like, and the microbes create a protective shield around the roots, or convert a particular nutrient to a form the plant can absorb and use. Other microbes break down stuff like leaves and manure and kitchen scraps and grass clippings and insect shells, releasing the nutrients into the soil. Some microbes eat other microbes, keeping checks and balances on the system.
As the foundation of a garden, nothing can replace or make up for lack of good soil. But creating good soil is a process and there are few short cuts. In forests, soil microbes turn layers of decomposing leaves into nutrient-rich humus; rain percolating through the leaf cover acts as a natural "compost tea." A natural, gradual sort of rototilling occurs as the roots of understory plants continually die and regenerate, releasing nutrients into the soil and creating small pockets for air and water to flow through. This process goes on for years, often decades. We can mimic this process by adding compost to our garden beds, mulching with leaves, planting cover crops, keeping tilling to a minimum, and wisely using water, fertilizers and pesticides. But even with good cultural practices, it can take 3 - 5 years to turn poor soil into good soil. So be patient and keep at it.
For more information on soil biology and soil organisms, visit the United States Department of Agriculture's Natural Resources Conservation Service's Soil Biology website.
(Today I Learned features a nugget of information I learned during training to become a Travis County Master Gardener.)
Words and photos © 2009-2011 Caroline Homer for "The Shovel-Ready Garden". Unauthorized reproduction is prohibited.










