Organic Matter The key to healthy soils Fred Magdoff Dept. of Plant & Soil Science University of Vermont.

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Presentation transcript:

Organic Matter The key to healthy soils Fred Magdoff Dept. of Plant & Soil Science University of Vermont

Are these problems or symptoms? erosion and runoff low nutrient levels compact soil many pest problems droughty

erosion and runoff low nutrient levels compact soil many pest problems droughty ProblemSymptoms Degraded and unhealthy soil

Why are soils which in our father’s hands were productive now relatively impoverished?

The depletion of the soil humus supply is apt to be a fundamental cause of lowered crop yields. —J.H. Hills, C.H. Jones, and C. Cutler, 1908

Soil organic matter and its management are at the heart of soil health

Characteristics of Healthy Soils  Sufficient (but not excess) nutrients  Good tilth  Sufficient depth  Good water storage and drainage  Free of chemicals that might harm plants

Characteristics of Healthy Soils  Low populations of plant disease and parasitic organisms  High populations of organisms that help plant growth  Low weed pressure  Resistance to being degraded  Resilience

There are three general “types” of organic matter in soils Living Dead Very Dead

—Living — nematodes fungi bacteria mites earthworms springtails moles plant roots

Moisture conservation Residue cover Soil ecology in balance Tighter system More fluid / greater biological diversity Changing ecology of system Imbalance in species Some groups increasing in number; some groups eliminated MANAGEMENT PRACTICES INFLUENCE ECOLOGY High disturbance Tillage Burning Steam sterilization Monoculture Overgrazing Fumigants Herbicides Fungicides Insecticides Low disturbance Direct seeding Permanent planting Cover cropping Infiltration Drainage Irrigation management Crop rotation Build organic matter Soil fertility / slow nutrient release Manure / biosolids Neutral pH

—Dead — Recently dead soil organisms and crop residues provide the food (energy and nutrients) for soil organisms to live and function. Also called “active” or “particulate” organic matter.

Karen Hills, 2007

—Very Dead — Well decomposed organic materials, also called humus. Humus contains very high amounts of negative charge.

All three “types” of soil organic matter play important roles in helping produce high yields of healthy crops.

Soil organic matter Organic matter is 1-6% of total soil mass living 10-20% active (dead) 10-20% humus (very dead) 60-80%

Organic Matter Influences a Vast Number of Important Soil Properties Nutrient availability Aggregation (and infiltration and drainage) Water storage Diversity and activity of soil organisms Soil color Presence of growth stimulating compounds Important global cycles — carbon, nitrogen, and water — are strongly influenced by soil organic matter For Example:

Nutrient Availability

As organic matter is decomposed nutrients are transformed into forms that are available to plants.

From 50% to close to 100% of the CEC is due to soil organic matter

Cation Exchange Capacity and chelation

Corn grown in nutrient solution with (right) and without (left) humic acids. Photo by R. Bartlett.

Soil Tilth

a) aggregated soilb) soil crusts after aggregates break down runoff infiltration

Root heavily infected with mycorrhizal fungi (note round spores at the end of some hyphae). Photo by Sara Wright.

Sticky substance, glomalin, surrounding root heavily infected with mycorrhizal fungi. Photo by Sara Wright.

Sticky substance, glomalin, surrounding soil aggregates. Photo by Sara Wright.

carbon dioxide (CO 2 ) (0.04% in the atmosphere) root respiration and soil organic matter decomposition crop and animal residues photosynthesis respiration in stems and leaves crop harvest The role of soil organic matter in the carbon cycle. Losses of carbon from the field are indicated by yellow color around the words describing the process. erosion carbon in soil organic matter

Karen Hills, 2007

Add organic matter Increased biological activity (& diversity) Decomposition Nutrients released Aggregation increased Pore structure improved Humus and other growth promoting substances Reduced soil-borne diseases, parasitic nematodes Improved tilth and water storage HEALTHY PLANTS Harmful substances detoxified

Two conditions are necessary to maintain an adequate amount of organic matter in the soil. These are, first, an adequate supply, and second, avoidance of a too-rapid loss... – Lyon and Fippin The Principles of Soil Management