the living, the dead and the very deadfred magdoff 10/18/2017 2 • bacteria • fungi • protozoa...

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10/18/2017 1 THE LIVING, THE DEAD AND THE VERY DEAD The Role of Soil Organic Matter in the N Cycle SOIL FORMING PROCESSES LIVING ORGANISMS Soil differences related to difference in plant growth over time Macroscopic Microscopic Human BIOLOGICAL SOIL PROPERTIES “Soil Organic matter…. The living… The dead…. And the very dead”. Fred Magdoff

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Page 1: THE LIVING, THE DEAD AND THE VERY DEADFred Magdoff 10/18/2017 2 • Bacteria • Fungi • Protozoa • Nematodes • Arthropods • Algae • Plant roots • Earthworms, and other

10/18/2017

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THE LIVING, THE DEADAND

THE VERY DEAD

The Role of Soil Organic Matter in the N Cycle

SOIL FORMING PROCESSES LIVING ORGANISMS

• Soil differences related to difference in plant growth over time

• Macroscopic

• Microscopic

• Human

BIOLOGICAL SOIL PROPERTIES

“Soil Organic matter….

The living…The dead….

And the very dead”.

Fred Magdoff

Page 2: THE LIVING, THE DEAD AND THE VERY DEADFred Magdoff 10/18/2017 2 • Bacteria • Fungi • Protozoa • Nematodes • Arthropods • Algae • Plant roots • Earthworms, and other

10/18/2017

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• Bacteria

• Fungi

• Protozoa

• Nematodes

• Arthropods

• Algae

• Plant roots

• Earthworms, and other larger animals

O.M. represents about 15% of the total soil organic matter.

O.M. represents about 15% of the total soil organic matter.

SOIL ORGANIC MATTERTHE LIVING

SOIL ORGANIC MATTERTHE DEAD

• Crop residue

• Green manure

• Livestock manure

• Sewage sludge

Source of carbon and nutrition for soil microbes.Source of carbon and nutrition for soil microbes.

SOIL ORGANIC MATTERTHE VERY DEAD

Humus

• A product of plant and animal remains.

• More complex than organic matter

• More difficult for other organisms to breakdown.

• Humus can last for many years in the soil.

The “Good Stuff” that makes-up our fertile soils.

Page 3: THE LIVING, THE DEAD AND THE VERY DEADFred Magdoff 10/18/2017 2 • Bacteria • Fungi • Protozoa • Nematodes • Arthropods • Algae • Plant roots • Earthworms, and other

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TEMPORARY N LOSSImmobilization-Mineralization

Time

Plant-available

“+” Change

Activity of microorganisms

Add sawdust C:N = 500:1

NITRATES

MICROBES

Sawdust totally degraded

C:N ratio and direction of reaction

• C:N ratios of 20:1 or less (Mineralization)

• C:N ratios of 30:1 or more (Immobilization)

• C:N ratios of 20:1 to 30:1 (No net change)

SOIL ORGANIC MATTERCARBON-to-NITROGEN RATIO (C:N)

OUR C:N Ratio 18/3 = 6:1

SOIL ORGANIC MATTERHUMUS

Stable Organic MatterC:N Ratio = 10:1

Page 4: THE LIVING, THE DEAD AND THE VERY DEADFred Magdoff 10/18/2017 2 • Bacteria • Fungi • Protozoa • Nematodes • Arthropods • Algae • Plant roots • Earthworms, and other

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COMMON C:N RATIOS

GREEN MATERIAL C:N Ratio BROWN MATERIAL C:N RatioAged Chicken Manure 7:1 Leaves 70:1Food Scraps 17:1 Straw/Hay 90:1Coffee grounds 25:1 Wood chips 700:1Grass clippings (fresh) 25:1 Shredded newspaper 175:1Fresh weeds 20:1 Nut Shells 35:1Fruit waste 30:1 Pine Needles 80:1Rotted manure 20:1 Corn Stalks 60:1Seaweed 19:1 Wheat Straw 60:1General garden waste 30:1

Maintaining Soil O.M.

100%

50%

Begin permanent sod

25 years after tillage began

Tillage begins

Time

SOIL ORGANIC MATTERMINIMIZING LOSS

• Minimize tillage

• Add residues/green manure

• Maintain environment for good microbes

• Control soil erosion

Page 5: THE LIVING, THE DEAD AND THE VERY DEADFred Magdoff 10/18/2017 2 • Bacteria • Fungi • Protozoa • Nematodes • Arthropods • Algae • Plant roots • Earthworms, and other

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7.MINERALIZATION

6.4.

NITRIFICATION5.

1.

FIXATION

Plant Uptake

DENITRIFICATION

VOLATILIZATION

LEACHING

IMMOBILIZATION

7.MINERALIZATION

6.4.

NITRIFICATION5.

1.

FIXATION

DENITRIFICATIONIMMOBILIZATION

LECTURE 4 ASSIGNMENT

• Watch this short Youtube video and offer a comment about what you see.

https://www.youtube.com/watch?v=Mxp1nnrUG0Q

Bioturbation: The reworking of soils and sediments by animals or plants.

Soil Fauna: the organisms of the soil considered as a whole.

Page 6: THE LIVING, THE DEAD AND THE VERY DEADFred Magdoff 10/18/2017 2 • Bacteria • Fungi • Protozoa • Nematodes • Arthropods • Algae • Plant roots • Earthworms, and other

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ADDITONAL READING

• Building Soils for Better Crops is a one-of-a-kind, practical guide to ecological soil management, now expanded and in full color. It provides step-by-step information on soil-improving practices as well as in-depth background—from what soil is to the importance of organic matter. A must-read for farmers, educators and students alike.

http://www.sare.org/Learning-Center/Books/Building-Soils-for-Better-Crops-3rd-Edition