Selecting Sand-Dominated Rootzones for Sports Fields

Transcription

Selecting Sand-Dominated Rootzones for Sports Fields
Selecting Sand-Dominated
Rootzones for Sports Fields
Tom Serensits
Penn State University
Why Sand ?
Why Sand?
• Many Disadvantages
– Does not much hold
water for plant use
– Must water more often
Why Sand?
• Low nutrient retention
(Cation Exchange Capacity)
• Must fertilize more often
• Must fight against organic matter accumulation
• Must aerify and topdress with sand often
• No soil structure
• Expensive
Why Sand ?
Porosity
Porosity
• Clay
– 75% pores, 25% solid
– 65% micropores
– 10% macropores
• Silt
– 50% pores, 50% solid
• Sand
– 35% pores, 65% solid
– 10% micropores
– 25% macropores
Ideal Soil
Pores
Solid
Organic Matter (1-5%)
Why Sand ?
Even after maximum compaction, sand still retains “ideal” pore distribution
and therefore continues to drain and retain airspace
Soil Structure
Arrangement of soil particles into groups
Bulk Density
• Under normal
conditions, sand has a
higher bulk density
than clay
• Clay = many pores
• Bulk density affected
by compaction
Frequent Question: How many
events can a native soil field
withstand vs. a sand rootzone?
Answer is 1 game if soil is saturated
And the field is destroyed...
Followed Golf’s Lead
Perched Water Table
Sand – No Structure
Good Balance of Air and Water
Amending a soil
• When amending a high
clay soil
– Need a lot of sand
(> 60%)
• When amending a high
sand soil
– Need only a little clay
Will turf growing on sand wear better
than turf growing on soil?
• Components of wear
– Compaction
– Abrasion
– Divoting
Why Sand?
Sand Cap Method
Michigan State Sand Cap Publication
Beaver Stadium
• Built like a road
– 22 inches of compacted
silt loam soil over gravel
On-Site Mixing
Need to Use a Quality Sand
Characteristics of a Quality Sand
• Particle Shape
– Angular or Round?
Sand Shape
How important is shape?
Sand Sizes
USGA: 35-55%
USGA: 15-30%
You want a good balance between
air-filled and capillary porosity
USGA: 15-25%
USGA: min. 6 in/hr
Total Porosity – Sand Effects
• Average sand size increases = T.P. decreases
• Uniformity of sand increases = T.P. increases
• Sand get rounder = T.P. decreases
• **total porosity only tells part of the story
“Holes” in the USGA Specs
Doesn’t regulate too uniform
Calcareous Sands
• Quartz (Silica) sand is best – hard and durable
• Calcareous Sand (calcium carbonates)
–
–
–
–
Physically breaks down
High pH
High particle density
Calcium Carbonate Equivalent
• < 3% - OK
• 3 - 9% - High
• > 9% - Problem
– Color?
Sand and Gravel Matching
Gravel
Rootzone
Bridging
Permeability
Uniformity
Sand and Gravel Matching
• Bridging: Will sand migrate into gravel?
– Will you need an intermediate layer?
– Largest 15% of rootzone
– Smallest 15% of gravel
• Use wet sand as first layers on top of gravel
Sand and Gravel Matching
• Permeability: Will there be clogging at the
interface?
– Smallest 15% of rootzone
– Smallest 15% of gravel
D15 (gravel) ≥ 5 x D15 (rootzone)
Sand and Gravel Matching
• Gravel Uniformity: Is the gravel uniform
enough?
– Largest 10% of gravel
– Smallest 15% of gravel
The Quality Control Program
• Make sure you get what you are paying for
• Work with a soil testing lab experienced with
sand-based athletic fields
• Small jobs – the soil test lab may be able to
supply the soil specifications
• Large jobs - architect
The Quality Control Program
• Get soil suppliers to submit either blends of
individual components
• Lab will test blends to see if they meet spec or
will construct blends in lab to determine
appropriate ratio
• Once approved by the lab, the soil supplier
will be allowed to bid the job
The Quality Control Program
• One of the bidders is awarded the job
• Company makes small batches to be tested.
These are called calibration runs
• After the lab has the blenders “dialed in” , a
benchmark mix is established
The Quality Control Program
• Confidence intervals
are established
• All soil testing up to
this point is borne by
the soil supplier
The Quality Control Program
• Now begins the quality control phase
• QC tests done every 500 tons mixed at the
blending site
– Dig into pile with shovel
– use 4 ft long, 2 inch PVC pipe, cap one end, drive
into pile
– Put in bucket and repeat 6 times
– Put on tarp and “quarter” until fill gallon ziplock
The Quality Control Program
• Send someone to check a few piles
• Explain you will be spot checking when the
mix arrives as well
• Pay someone to take a small sample of every
truck load that arrives. Label it and save it if
questions arise later
Components in Rootzone Blends
• Sand
• Organic Matter
• Soil?
Heinz Field
• 85-5-10 Mix
• Percolation rate: 3.5 in/hr
• Aeration porosity: 15%
What does 80-20 mix mean?
• 80% sand, 20% organic
matter
• By volume
• 80-20 mix is usually
about 0.7% OM by
weight
Organic Matter
• Increased moisture
retention
• Reduce bulk density
• Buffer capacity
• Increase cation exchange
capacity
• Microbial activity
Peat
Reed Sedge
Sphagnum
Peat
• Reed Sedge
– North Dakota /
Minnesota
– Age: Old
– Stable
– Fine texture
• Sphagnum
–
–
–
–
–
–
Canada
Age: Young
Fibrous
High OM content
High water holding
Lower pH
Organic Matter
• OM should only ever
be added at
construction
• K. bluegrass deposits
5,000 lbs. of oven dry
OM per acre per year
Organic Matter
Topsoil
• “Friend”
Sand Rootzone
• “Enemy” (over time)
• > 3% OM = adequate
• > 3% (by wt.) = concerned
• > 4% OM = Good
• > 4% (by wt.) = may see
problems (poor drainage,
shallow rooting, divoting)
• > 5% OM = Superior
• > 5% (by wt.) = problems
typically evident
Too much organic matter...
Too much organic matter...
Reducing Organic Matter
Dilution
Removal
Cores must be removed
What to look for in a soil test report
• Soil Texture
–
–
–
–
% Gravel
% Sand
% Silt
% Clay
What to look for in a soil test report
• Sieve Analysis
– Breakdown of sand sizes
– Does it meet spec?
– Anything that jumps out?
What to look for in a soil test report
• Acid Reaction
– Is it calcareous?
• Shape
– Angularity and sphericity
• D15 and D85
– Used for bridging with gravel
What to look for in a soil test report
• Bulk density
– Indicator of compaction and hardness
– Used to calculate porosities
• Total porosity
– USGA: 35 – 55%
What to look for in a soil test report
• Air-filled porosity (Macroporosity)
– What % of the pores are airfilled?
– USGA: 15 – 30%
• Capillary porosity (Microporosity)
– What % of the pores are filled with water?
– USGA: 15 – 25%
What to look for in a soil test report
• Hydraulic conductivity (percolation rate)
– USGA: minimum 6 in/hr
• Particle Density
– Density of the solid portion of the soil
– Around 2.65 – higher if calcareous, lower if a lot of OM
– Needed for porosity calculations
• Organic Matter
What to look for in a soil test report
• Quality Control Testing
– Particle size analysis with silt and clay combined
– Organic Matter
– Quick turnaround
Other Things to Consider
• What is the soil
makeup of the sod?
• Thick cut or thin cut?
• Aerify and topdress
with sand similar to
rootzone
Reasons for Sand Field Failure
• Pre-installation
– Poor design / sand
selection
• Too coarse – will be
droughty
• Too fine – slow drainage,
compaction
• Wrong particle size
distribution
Reasons for Sand Field Failure
• Pre-installation
– Calcareous sands
– Too much / too little
organic matter
– Poor design
• Irrigation systems
• Drainage system
Reasons for Sand Field Failure
• During Installation
– On-site mixing
– No Quality Control
testing
– Sod soil with high
amounts of fines
Reasons for Sand Field Failure
• After installation
– Allow buildup of organic
matter
• Shallow rooting
• Reduced drainage
• Divoting
Reasons for Sand Field Failure
• Improper maintenance
– Fertilizer program
– Irrigation scheduling
– Not removing cores
– Not topdressing enough
Reasons for Sand Field Failure
• Topdressing with the
wrong material
• Match topdressing
sand with rootzone
– If not, layers can
develop
(perched water table)
• No fines or gravel
Reasons for Sand Field Failure
• Loss of turf cover
– No cohesion between
particles
– Rely on rhizomes and
roots
Plant Growth
Regulator Study
Research Trial
• Kentucky bluegrass
• 2 Rootzones
– USGA Sand
– Silt loam soil
• Evaluated divot
resistance, tiller density,
and root mass
Plant Growth Regulator Study
• Plant growth regulator
- Reduce vertical shoot
growth by altering
hormone levels
• Trinexapac-ethyl (TE) Inhibits gibberellic acid
– Side effects – increased
tiller density and
rooting
www.turffiles.ncsu.edu
Trinexapac-ethyl Applications
• Rate 0.5 oz/ 1000 ft2
• 28-day intervals
• 2 application regimes
– May – July (3 applications)
– May – Oct (6 applications)
Simulated Football Season
Simulated Football Season
No Wear
Medium Wear
High Wear
Results
• TE applied from May – July reduced divot size
most
– Sand: 10-20% reduction
– Soil: 10% reduction
• TE applied from May – Oct was not better or
worse than untreated plots
Results
• Tiller Density
– TE treatments increased
tiller density up to 15%
– Root Mass
• TE applied from May –
July increased root mass
by 10%
Turfgrids (3, 5 g kg-1)
Fiber Reinforced Sand Systems
Nike Reuse-A-Shoe
Netlon
Turfgrids
DuPont Shredded Carpet
Fiber Reinforced Sand Systems
• Increases surface
stability
• Popular on European
Soccer fields
• Synthetic fibers sewn
into existing turf
– Every ¾”
– 7 inches deep
Fiber Reinforced Sand Systems
• 22 million fibers
• 25,000 miles of fibers
on a single field
• 3% of field
• NFL fields
Sewing Needles
Fibers
Fiber Reinforced Sand Systems
• Advantages
• Disadvantages
– Increase stability
– Cannot core aerify
– Less Divoting
– Cannot re-sod
– As field get worn, plays
better
– Fibers tend to lay over
– Roots intertwine with
fibers?
– Topdressing buries
fibers
Final Thoughts
• Sand maintains good air and water balance
even under compaction
• Sand-based fields prevent the disaster rain
game
• Sand mix must be carefully selected to realize
benefits
Final Thoughts
• Maintenance practices must be adjusted and
intensified
– Manage organic matter
– More frequent irrigation
– More frequent fertilization
– Topdressing with proper sand
– Maintain turf coverage
– More expensive to build and maintain
Penn State’s Center for Sports Surface Research
Website: http://ssrc.psu.edu
“Like” Penn State’s Center for
Sports Surface Research
@ PSUsportsturf