The Latest Dirt: Research-Based Innovation in Soil Healthccag-eh.ucanr.edu/files/255515.pdf · The...
Transcript of The Latest Dirt: Research-Based Innovation in Soil Healthccag-eh.ucanr.edu/files/255515.pdf · The...
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The Latest Dirt: Research-Based Innovation in Soil Health
CLCA Landscape Industry ShowFeb. 1, 2017
Chuck Ingels
Farm & Horticulture Advisor
http://ccag-eh.ucanr.edu
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Topics to be Covered• Physical Characteristics of Soil
Soil texture and its effects water & nutrient retention
Soil organic matter and soil aggregation
• Plant Roots and the Rhizosphere
Root structure and Rhizosphere
Mycorrhizae
Soil Structure
Effects of tilling & compaction
Dealing with compaction
Mulches
Cover Cropping
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Topics to be Covered• Physical Characteristics of Soil
Soil texture and its effects water & nutrient retention
Soil organic matter and soil aggregation
• Plant Roots and the Rhizosphere
Root structure and Rhizosphere
Mycorrhizae
Soil Structure
Effects of tilling & compaction
Dealing with compaction
Mulches
Cover Cropping
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Typical Soil Profile
www.timberpress.com
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Makeup of Soils
Pore Space
Solid
Organic
Air
Water(sand, silt,
& clay)
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Physical Characteristics of Soil
Texture
Structure
Sandy loam Clay loam
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Soil Texture vs. Structure
Texture: Percent sand/silt/clay
• Examples: sandy loam, clay loam
Structure: Arrangement of particles into aggregates, clods, crusts, pans, etc.
• Affected by compaction
Impractical to change
Can be changed – for better or worse
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Soil Texture
The Soil Triangle
(Based on lab analysis)
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Soil Particle Sizes
Sand 2.00 to 0.05 mm
Silt 0.05 to 0.002 mm
Clay 0.002 to <0.0002 mm
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Soil Texture
Loamy sand LIGHTSandy loamLoamSilty loamClay loamClaySilty claySandy clay HEAVY
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Soil Texture Affects Soil Moisture
Water Holding Capacity
Permeability
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Water Infiltration through Soils
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Water Movementin Soil
Sand Loam Clay
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Wetted Pattern and Area½ GPH Emitter
Clay20-38 ft2
Loam7-20 ft2
Sand3-7 ft2
Source: Ewing Irrigation
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Soil Wetted AreaSoil Type
Emitter Flow Rate(gal/hr) Diameter (ft) Area (ft2)
Sand0.5
1.0
2.0
2 to 3
3 to 3.5
3.5 to 4
3 to 7
7 to 10
10 to 13
Sandy Loam0.5
1.0
2.0
3 to 4.5
4.5 to 5
5 to 5.5
7 to 16
16 to 20
20 to 24
Loam0.5
1.0
2.0
3 to 5
5 to 6
6 to 7
7 to 20
20 to 28
28 to 38
Clay Loam0.5
1.0
2.0
4 to 6
6 to 7
7 to 8
13 to 28
28 to 38
38 to 50
Clay0.5
1.0
2.0
5 to 7
7 to 8
8 to 9
20 to 38
38 to 50
50 to 64
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Capillary Water Movement inClay Loam Soil
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Topics to be Covered• Physical Characteristics of Soil
Soil texture and its effects water & nutrient retention
Soil organic matter and soil aggregation
• Plant Roots and the Rhizosphere
Root structure and Rhizosphere
Mycorrhizae
Soil Structure
Effects of tilling & compaction
Dealing with compaction
Mulches
Cover Cropping
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Soil Organic Matter• Serves as energy source
(food) for microbes, which promote aggregation
• Essential nutrients are obtained by plants as OM decomposes
• Enhanced by OM additions but destroyed by cultivation
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Soil Organic Matter LossRecent Research
Sources: Univ. of Minnesota,Ohio State Univ.
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Makeup of Soil Organic Matter
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HumusWhat We’ve Been Taught
• What’s left over after organic matter decomposes
• Cannot be seen by naked eye
• Very reactive (CEC)
• In equilibrium with organic matter additions
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A New Understanding of HumusBackground
• Many years ago soil scientists noticed that good agricultural soil was black
– Devised a method to extract it from the soil
– Treated soil with a strong alkaline solution (pH 13)
• Pulled the organic component out of soil for study
– Treatment with alkali produces humic acid and fulvic acid!
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A New Understanding of Humus“The Contentious Nature of Soil Organic Matter”http://www.nature.com/nature/journal/v528/n7580/abs/nature16069.html
• Nature journal, Dec. 2015
• Humus is created during the pH 13 extraction process – the strong alkali creates humus
– Molecules interact with soil - hiding from microbes
– Microbes build large molecules making the process start all over again
• Humus does not exist! (This is largely academic)
Source: http://www.gardenmyths.com/humus-does-not-exist-says-new-study/
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Humus, OM, plant & microbial exudates, and earthworm castings act as “binding” agents
Soil Aggregate Formation
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• Bacteria, polysaccharides, etc. –micro-aggregate formation
• Fungal hyphae – enmeshing micro-aggregates into macro-aggregates
Soil Aggregation
© 2012 Nature Education
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Fungi
• Fungi grow as long strands (hyphae) several thousandths of an inch in diameter
• They push their way between soil particles, roots, and rocks
• A single hyphae can span in length from a few cells to many yards.
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Netlike fungal mycelia can stabilizemicro-aggregates
http://www.microped.uni-bremen.de/SEM_index.htm
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http://www.microped.uni-bremen.de/SEM_index.htm
Stabilization of Soil Structure by Actinomycete Filaments
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What Do Earthworms Do?
• Stimulate microbial activity
• Mix and aggregate soil
• Increase infiltration (burrows)
• Improve water-holding capacity by increasing aggregation and soil porosity
• Provide channels for root growth
• Bury and shred plant residue
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Topics to be Covered• Physical Characteristics of Soil
Soil texture and its effects water & nutrient retention
Soil organic matter and soil aggregation
• Plant Roots and the Rhizosphere
Root structure and Rhizosphere
Mycorrhizae
Soil Structure
Effects of tilling & compaction
Dealing with compaction
Mulches
Cover Cropping
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Anatomy ofYoung Roots
Emerging
lateral
root
Root
hairs
Root
cap
Root
hairs
Cell
elongation
Cell
division
Root cap
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Root Hairs
• Cells, not roots!
• Greatly increase root surface area
• Very short livedNucleus
Root hair
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Root Cap
• Covers apical meristem
• Produces slimy “mucigel”
Sugars, enzymes, amino acids
Protects & lubricates root tip
Improves soil aggregate
formation
Source: Laprotox (UFRGS)
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Plant Roots Feed the Microbes!• Use 25-40% of carbohydrate supplies to feed microbes
• Use hormones to attract and “farm” bacteria, fungi, and other organisms to help recycle soil nutrients & water
Sources:1. J. Hoorman, Ohio State Univ.2. www.nature.com
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The Rhizosphere
• Thin region of soil that is directly influenced by root secretions (exudates) and soil microbes
• Roots release organic substances into the rhizosphere
• There are over 1000 times more microbes associated with a live root than in the bulk soil
Source: J. Hoorman, Ohio State Univ.
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Topics to be Covered• Physical Characteristics of Soil
Soil texture and its effects water & nutrient retention
Soil organic matter and soil aggregation
• Plant Roots and the Rhizosphere
Root structure and Rhizosphere
Mycorrhizae
Soil Structure
Effects of tilling & compaction
Dealing with compaction
Mulches
Cover Cropping
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Mycorrhizae(“Fungus-Roots”)
• Fungal infection of roots – symbiotic relationship
• Fungi – receive sugars; Plants – phosphorus & water
• Help roots explore up to 20x the volume of soil
Increases plant resistance to drought
• Lacking only in sedges & brassicas (cabbage fam.)
• Poor growth without myc. where nutrients limited
• Soil inoculation helpful only in poor/disturbed soils
• Two main types: Ecto- and endo-mycorrhizae
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Mycorrhizal Fungus
Sources: Bonfante & Genre 2010,Astrid Volder, UCD
Ecto Endo
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Mycorrhizal FungiEcto-Mycorrhizae
• Grow on trees in pine, oak, beech, birch, and willow families
• Grow outside and between cells of young roots
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• Most important is vesicular-
arbuscular myc. (AMF or VAM)
Vesicle = bladder-like structure
Arbuscule = branched structure
• 80% of plant species
• Most crops (monocots & dicots),
hardwoods, non-pine conifers
Mycorrhizal FungiEndo-Mycorrhizae
Infection directly into root cells
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Mycorrhizae
Poor growth of
forest trees without
mycorrhizae –
where nutrients are
limited
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Add Mycorrhizal Inoculants?
• Plants often choose fungi selectively
• Research shows that the wrong fungi, or wrong combination, can impair plant growth
• Adding purchased AMF not wise:
– Often dead in the bag
– May not be the correct species
– Adding fungi has unknown effects on the growth of that plant, the soil organisms in your area, etc.
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Research on Adding MycorrhizaeSalyards et al., 2003
Sandy loam soil sterilized, then treated with a mycorrhizal inoculum (Glomus intraradices), forest duff, organic matter, or nothing. “Inoculation with AMF is unnecessary except in sites where early colonization is essential.”
Salyards, J.E. Richard, and A. Berry. 2003. Mycorrhizal development and plant growth in inoculated and non-inoculated plots of California native grasses and shrubs. Native Plants. Fall issue pp. 143-149.
Source: Richard Evans
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At 68 weeks: No effects on percentage of grass roots infected with mycorrhizae
Salyards et al. 2003
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After 95 weeks there were no significant effects on biomass of the grasses
Salyards et al. 2003
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Topics to be Covered• Physical Characteristics of Soil
Soil texture and its effects water & nutrient retention
Soil organic matter and soil aggregation
• Plant Roots and the Rhizosphere
Root structure and Rhizosphere
Mycorrhizae
Soil Structure
Effects of tilling & compaction
Dealing with compaction
Mulches
Cover Cropping
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Tillage vs. No-TillEffects on Soil Aggregation
No-till Tilled
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Soil Structure
Structure - the arrangement of soil particles into aggregates
Good structure: holds water (micropore space) and has air space (macropore space)
Poor structure: lacks adequate macropore space
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A Key Goal = Good Soil Tilth
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Soil Stratification
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Soil Structure May Vary Greatly
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Soil structure & texture can be highly variable across small areas
Photos: Larry Costello
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Cemented Hardpan
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Cemented hardpan
Compacted soil
Cemented hardpan
Compacted soil
Hardpan vs. Compaction
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Good vs. Poor Soil Structure
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Effects of Compaction on Soil
• Soil structure is destroyed – pore space is severely reduced
• Soil drains slowly and is prone to being anaerobic
• Compacted soil physically impedes root growth
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Water Movement in Soils
Poorly Structured/Compacted Soil
WellStructured Soil
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Results ofCompacted Soils,
Poor Drainage
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Topics to be Covered• Physical Characteristics of Soil
Soil texture and its effects water & nutrient retention
Soil organic matter and soil aggregation
• Plant Roots and the Rhizosphere
Root structure and Rhizosphere
Mycorrhizae
Soil Structure
Effects of tilling & compaction
Dealing with compaction
Mulches
Cover Cropping
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Some Soil Layers Restrict Air, Water,and Root Penetration
• Hardpan – cemented (by silica, iron, carbonates)
• Traffic or compaction pan – caused by vehicles, tillage implements, feet, hooves
• Crust – brittle, compact/hard when dry
• Claypan – higher clay than overlying layer
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Tire CompactionAvoid Traffic on Wet Soil
No compaction,good aggregation
Compaction,no aggregates
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Plow Pan
Ripping to break up plow pan
Plow Pan Disked Soil (18 mo. Ago)
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Crust Forms on Unprotected SoilRainfall or Sprinklers
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Cemented Hardpan
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Protect SoilsAvoid Compaction During Construction
– Create Temporary Walkways
Photo:Marcia Braga
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– Remove and store topsoil
Protect SoilsAvoid Compaction During Construction
Photos: Marcia Braga
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Protect SoilsPrevent Erosion
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Protect & Nurture SoilsAerate Compacted Soils
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De-Compacting Soils
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Dealing with Compaction and Hardpan
Rip / Drill
Backhoe
Trencher
Jackhammer / clay spade / pick ax
Dynamite
Break it up – down to good soil
Use raised planters
With walls or barriers
Without walls (raised mounds)
Provide drainage
Will gypsum or compost break it up? NO
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Drainage systems need to be carefullydesigned and installed
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Subsurface drainage can be improved with drain lines, but…
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…maximize soil drainage to minimize runoff
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Ripper
(maybe a little too big
for landscapes)
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Drill or Trench Soil
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Backhoe or Excavate
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Jackhammer, clay spade attachment
Or Break it Up Manually
Pick axe
Traditional approach
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Use Raised Beds…
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…Or Raised Planters
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Evaluate Soils and Soil Moisture
Soil
sampling
tube
Soil probe Soil auger
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Organic Amendments
• Composts
• Manures
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“Finished” Compost
• Thermophilic heating process with turning
• Temperature low, no ammonia smell
• Contains diverse microbial populations
• Contains most nutrients required by plants
• Should not contain weeds & plant pathogens
• N content usually 1-1.5%, very slow release
• Usually considered a soil amendment to add organic matter, not fertilizer
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Earthworm Castings Better than Compost?
• Both add slow-release nutrients, improve soil structure, increase water & nutrient retention
• Earthworm castings may be better for:
– Promoting beneficial microbial activity
– Adding more humic acid to stimulate plant growth
– Improving soil aggregation
• Using compost and some EW castings ideal
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Topics to be Covered• Physical Characteristics of Soil
Soil texture and its effects water & nutrient retention
Soil organic matter and soil aggregation
• Plant Roots and the Rhizosphere
Root structure and Rhizosphere
Mycorrhizae
Soil Structure
Effects of tilling & compaction
Dealing with compaction
Mulches
Cover Cropping
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Mulching with Wood Chips
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Potential Benefits of Mulch
• Reduces weeds & erosion
• Reduces impact of raindrops
• Insulates roots from temp. extremes
• Conserves soil moisture ↑ root growth
• Increases microbial activity
• Increases water penetration
• Improves plant establishment
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Potential Problems with Mulch
• May prolong saturation in heavy soils
Favors root and crown rot
• May host plant diseases, insects, and nuisance fungi
• Some wood chips poor quality
• Can’t see soil moisture
• Time consuming to spread
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Mulch Basics (Wood Chips)(LGtoM, CIWMB, 2002)
• Remove weeds, water before applying
• Replace grass with mulch under trees
• Keep 6-12 in. away from the base of trees & shrubs
• Application rate: Generally 2-4 in. deep
– Fine = <2 in. Coarse = 4-6 in.
• Keep mulch on top of soil to prevent N tie-up
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More Mulch Basics
• Durability of wood chips increases with underlying fabric or plastic
– But no contact of soil with organic matter
• Mulch has little or no effect on termites
• Softwood mulches (conifers) last longest
– Less microbial feeding
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Wood ChipsWeight and Coverage
• Weight per yard is highly variable
• Average (depends on moisture):
– 500 to 700 lbs. per yard
– 3 to 4 yards per ton
• 4 inch application:
– 1 cubic yard covers 81 square feet
– 538 cubic yards covers 1 acre
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Do Wood Chips Affect Soil Nutrients?
• Tie-up of N?
N immobilization from high C:N mulch
Generally N tie-up at interface only
Avoid mulch in planting holes
• Soil pH (pine needles acidic) – little effect unless incorporated
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Mulching and Weed Control
• Thickness to mulch depends on mulch type
• Various studies:
– 3-in. layer: 85% weed control over 3-yrs.
– 4-in. mulch gave better control than 3-in.
– Phenols & tannins in coniferous bark improved weed control
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Can Mulches Spread Diseases?Some Potential Problems
• Pine pitch canker
• Sudden oak death
• Dutch elm disease
• Don’t transport these wood chips
• Keep mulch 6 in. away from trunks
Oak root fungus?
Verticillium wilt?
Fire blight?
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Dog Vomit Fungus(Slime Mold)
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Dyemaker's puffball
Stinkhorn
Other Mulch Fungi
Bird’s nest fungus
Mushrooms
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Synthetic MulchesPolypropylene and Polyester
• Better weed control than chips alone
• Slower breakdown of wood chips
• Allow water & air movement
• Do not improve soil quality
• Most are effective 3-5 yrs. (under chips)
• Most are not recyclable (landfill!)
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Plastic or Fabric Underneath?
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Needs to be Held in Place on Slopes
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Synthetic mulches will usually become exposed and shred, especially on
slopes
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Weed Control After 4 Years (UCD)
1 pre-emerg.
applic.
1 wood chip
applic.
Wood chips
+ woven
polyprop.
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Problems with Quality of Mulch from Tree Service
Companies
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Mower
blight
Avoid
weedeating
by trunk
Avoid turf or
weeds by trunk
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Mulch alone won’t keep soil in place on steep slopes
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Conclusions - Mulches• Avoid mulch in planting holes
• Control perennial weeds first
• Caution on clay soils; away from trunks
• Little or no N tie-up; add N or compost
• Little or no disease transmission
• Root growth improved
• Benefits outweigh disadvantages
• Fabric reduces weeds but it shreds
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Topics to be Covered• Physical Characteristics of Soil
Soil texture and its effects water & nutrient retention
Soil organic matter and soil aggregation
• Plant Roots and the Rhizosphere
Root structure and Rhizosphere
Mycorrhizae
Soil Structure
Effects of tilling & compaction
Dealing with compaction
Mulches
Cover Cropping
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Cover Crop Before Establishing Fair Oaks Horticulture Center
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Cover CropsDefinitions
Cover crop
• A non-harvested crop planted to provide any of a number of benefits, such as improving soil quality, reducing erosion, adding N, and/or attracting beneficial insects
Green manure cover crop
• A crop grown & plowed under for its beneficial effects to the soil and subsequent crops
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• Lowest fertilizer energy use: On-site production of N
May still need additional N
• Add organic matter
• Improve soil tilth and water penetration
Cover CropsBenefits
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Cover Crop RootsGrass roots more
beneficial to soil structure
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• Competition with trees for water & nutrients
• Insect and vertebrate pests
• Increased costs and management
• Additional equipment required
• Requires chopping/disking in spring
Cover CropsPotential Problems
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• Atmosphere = 78% N; only legumes can use
• Rhizobium bacteria in roots use N in soil air
Symbiotic relationship
Store N in nodules on roots
Nodules resemble root-knot nematodes
• Most N translocated to foliage
Cover CropsNitrogen Fixation of Legumes
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Nodules Created by Rhizobium Bacteria
Berseemclover
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• Low ratios (legumes) – rapid decomposition, net release of N
• High ratios (cereals/grasses) – slow decomposition, & net tie-up of N
Cover CropsC/N Ratio
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Example of C/N Ratios
Oat straw 70:1
Wood chips 60:1
Corn stubble 57:1
Rye (mature) 37:1
Rye (vegetative) 26:1
Mature alfalfa hay 25:1
Source: J. Hoorman, Ohio State Univ.
Ideal microbial diet 24:1
Rotten manure 20:1
Legume 17:1
Young alfalfa hay 13:1
Hairy vetch 11:1
Soil microbes (avg.) 8:1
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Cover CropsGeneral C/N Ratios
RESIDUE C/N RATIO
Legume 15:1 to 20:1
Brassica 20:1 to 30:1
Grass 40:1 to 80:1
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Mineralization and Immobilization
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C:N Ratio of Organic Matter
• As a rule of thumb:
• At C:N >20:1, NH4+ is immobilized (tied up)
• At C:N < 20:1, NH4+ is mineralized (released)
N in organic matter and microbes
NH4+
(ammonium)
C:N < 20:1
C:N > 20:1
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• Standard winter green manure legume mix:
High N mix: Bell beans, vetch, and field peas
Add for soil tilth (or use alone): Oats or barley
• Annual reseeding mix (orchards & vineyards):
Crimson, rose, subclover + bur medic
• Summer:
Cowpeas, buckwheat
Cover CropsSpecies
Vetch/Pea/Oat Mix
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Annual Clovers
Subclover
Crimson Rose
● Self reseeding● Mainly for orchards
and vineyards
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• Good seedbed preparation; inoculate seed
• Scatter seed and rake in (or drill)
• Rototill 3-4 weeks before planting spring crop
Reduced soil-borne diseases
Reduced tie-up of soil N
Cover CropsPlanting and Incorporation
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Inoculating Legume Seeds
Background
• Specialized bacteria (Rhizobium sp.)
Not to be confused with Mycorrhizae
Creates nodules on roots
Captures N in plant, most moves into foliage
• Insures that N fixation will occur
• Not essential to inoculate for same soil in year 2
• Good to inoculate garden peas & beans too
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• Use at least 1 oz./10 lbs. of seed
• To help inoculant adhere to the seed:
Mix 9:1 hot water (non-chlor.) + corn syrup
Let cool, add a small amount to seeds
Rate effect (up to a point) – Use plenty!
• Pouring dry into hopper may work but would not provide uniform application
Inoculating Legume Seeds
Methods
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• Grass alone may require N
• Avoid N fertilizers on legumes
High soil N legumes fix little N
• Max. N contribution is at early flowering (incorporate in March)
• >80% of N is in above-ground parts; <20% in roots
Cover CropsNutrition
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Cover Crop, Tomatoes
FOHC