BF 104 Soil Health & Management - University of …...Advancing the Business of Farming in...
Transcript of BF 104 Soil Health & Management - University of …...Advancing the Business of Farming in...
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
BF 104 Soil Health & Management Kip Kolesinskas, Conservation Scientist
Listo Para Iniciar Farming Program, Stamford, CT October 2016
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
INTRODUCTIONS
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
Advancing the Business of Farming in Connecticut in Partnership with Agricultural Learning Centers
Advancing the Business of Farming in Connecticut Project provides new farmers with core training and assistance to develop their farm plan, explore production options, and grow their farming enterprise. Visit
www.newfarms.extension.uconn.edu for resources and events. • Common Ground, New Haven
• Community Farm of Simsbury, Simsbury
• Green Village Initiative, Bridgeport
• Killingly Agricultural Education Center, Killingly
• Knox- Urban Farming Incubator Program, Hartford
• Grow Windham, Willimantic, Windham
• Listo Para Iniciar Program, Bethel, Stamford, New Milford
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
Advancing the Business of Farming in Connecticut in Partnership with Agricultural
Learning Centers – Core Trainings
• BF 101 New Farmer Business Planning
• BF 102 Setting Up Financial Records for Farm Business
• BF 103 Finding, Evaluating Farm Sites, Leasing Farmland
• BF 104 Soil Health & Management
• BF 105 Fruit Production for Small Scale Farming
• BF 106 Vegetable Production for Small Scale Farming
• BF 110 Unheated hoop houses- installation, production systems
• BF 120 Irrigation & Water Management Systems
• BF 130 Hydroponics/Aeroponics/Aquaponic Systems
• BF 140 Post –Harvest Handling
• BF 150 How to Enter the Market, State regulations and support for CT Grown, EBT sales
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
Core Trainings continued….
• BF 201 Quickbooks for Farm operations
• BF 202 Record Keeping for Organic Certification
• BF 203 Balancing Farmland Capacity with Conservation & Financial Goals
• BF 210 Design Fundamentals for Greenhouses & Tunnels
• BF 220 Safety & Maintenance for Small Engines & Power Tools
• BF 221 Tractor Safety & Maintenance
• BF 230 Safe & Effective Use of Pesticides- For organic/non-organic producers
• BF 240 Climate change and Adaptation Strategies
• BF 250 Marketing for Success- developing relationships, branding
• BF 261 Selling to Institutional Buyers-schools, hospitals, colleges
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Take an
apple
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Have it
represent
the Earth
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Cut out and
save …
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¼ of the
apple
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This much
represents
land area.
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Now cut that
slice in half,
and keep
one piece.
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This much
represents
where
people live.
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Cut that piece in
quarters and
keep one ¼. This
represents the
amount of soil
where food can
be grown.
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This is 3%
(1/32) of
the Earth’s
surface.
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It’s
All
About
the
Soil!!
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We Study Soil Because It’s A(n)
Great integrator
Producer and absorber of gases
Medium for plant growth
Medium of crop production
Home to organisms (plants, animals and others)
Waste decomposer
Snapshot of geologic, climatic, biological, and human history
Source material for construction, medicine, art, etc.
Filter of water and wastes Essential natural resource
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Five Soil Forming Factors
Parent Material
Topography
(The first four factors over) Time
Climate
Biota
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Hydrologic Cycle Water enters the soil, interacts with soil particles and leaves the soil (through evaporation, transpiration or leaching).
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Hydrologic Cycle and the Soil
Color
Structure
Bulk Density
Texture
pH
Temperature
Moisture
Horizon
Depths
Soil Properties that are part of the hydrologic cycle.
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A Soil Profile
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Soil Color Munsell Notation
Hue Value Chroma
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Soil Structure - With Structure Granular
Platy
Blocky
(Angular)(Subangular)
Wedge
ColumnarPrismatic
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Soil Structure – Without Structure
Single Grain Massive
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USDA Textural Triangle
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Sand + Silt + Clay = 100%
Texture =
CLAY LOAM
34 % Sand
33 % Silt
33 % Clay
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General Influence of Soil Separates on Properties and Behaviors of Soils
Property/Behavior Sand Silt Clay
Water holding Low Med-high high
Aeration Good Med Poor
OM decomposition Fast Med Slow
Water erosion pot. Low High Low
Compact-ability Low Med High
Sealing (ponds) Poor Poor Good
Nutrient supplying Poor Med-high High
Pollutant leaching High Med Low
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Soil Organic Matter
Decomposing organic matter (active fraction) 33% - 50%
Stabilized organic matter
(humus) 33% - 50%
Fresh residue <10%
Living organisms
<5%
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Landscape Factors
• Depth to bedrock
• Depth to water table
• Flooding vs. ponding vs. high water table
• Erosion & water quality concerns
• Human influence
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summit
shoulder
backslope
footslope
toeslope
drainageway
or
depression
Relative Landscape Position
Reading the Landscape: How Understanding Soil Resources Can Help Community Farms
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Slide 31
Summit
Lower Sideslope
Footslope
Toeslope
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Dinosaur Era
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Today
350 years ago
4,000 years ago
6,000 years ago
8,000 years ago
10,000 years ago
13,000 years ago
17,000 years ago
Adapted from the Mashantucket Pequot Museum
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Soil Parent Material
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Physiographic Regions of Connecticut
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Glacial Till Parent Material
Sutton Series
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Manchester Series
Glaciofluvial Parent Material
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Alluvium Parent Material
Hadley Series
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Scitico Series
Glaciolacustrine Parent Material
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Natchaug Series
Organic Parent Material
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Disturbed Parent Material
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Soil Classification
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Technical Soil Classification
Drainage
Class
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Criteria Used in Soil Taxonomy
• Chemical, physical, and biological
properties (such as moisture,
temperature, texture, structure, pH, soil
depth)
• Presence or absence of certain diagnostic
horizons (surface and subsurface
horizons)
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• Entisol
• Inceptisol
• Andisols
• Spodosols
• Mollisols
• Alfisols
• Ultisols
• Oxisols
• Aridisols
• Vertisols
• Histosols
• Gelisols
12 Soil Orders http://soils.usda.gov/technical/classification/orders/
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A polypedon or
soil individual
A pedon
Landscape
Solum
Soil Profile
{ Ap
Bw
BC
C
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Soil Mapping
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Click on the green “start” button
http://websoilsurvey.nrcs.usda.gov
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View the Soil Map
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Click on map unit name for description
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Example Soil Interpretation Land Capability Classification Rating
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
Networking Break & Soil Texture DEMO
Get to know other participants! 35 min
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Texture by Feel
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
SOIL QUALITY/HEALTH: The continued capacity of the soil to function as a vital living system that sustains plant, animal, and human health.
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
Properties of Soil Heath: Inherent Properties:
–Physical properties that usually cannot be changed without much difficulty
•Soil texture •Type of clay •Depth to bedrock •Drainage class
Dynamic Properties:
• Management dependant properties that we do have the ability to change relatively easily
•Organic matter content
•Biological activity
•Aggregate stability
•Infiltration
•Soil fertility
•Soil reaction (pH)
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
Benefits of Managing for Soil Health
•Improved Nutrient Cycling •Maximizes fertilizer availability •Fungi increase P and water supply to plants •Improved soil aggregation •Increased water movement and storage •Better root growth into more soil •Better habitat for the Soil Food Web •Fewer weeds and diseases •A balanced Food Web helps suppress pests •Less soil disturbance plants fewer weed seeds
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
Indicators of Soil Health:
Physical indicators commonly used to assess agronomic soil quality include: Indicators of Soil Health:
•Aggregate stability • Available water holding capacity • Bulk density • Infiltration • Root distribution • Soil crusts
• Soil structure and macropores • Visible soil fauna
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
Soil is a Living Factory
•Macroscopic and microscopic organisms–Food –Water –Shelter –Habitat –Powered by sunlight
Management activities improve or degrade soil health–Tillage –Fertilizer –Pesticides –Grazing –Plant Diversity
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
What the Soil Food web Does: Plant nutrient immobilization / mineralization
Creates stable soil aggregates Water infiltration / retention Habitat for soil food web Root movement Nematode, microarthropod movement Air movement
What is the most limiting element in the soil for agricultural production? Where does the Carbon contained in the soil come from?
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
Create Quality Microbial Habitat , Every Farmer has Livestock
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
Rhizosphere…where roots meet soil
Zone of concentrated biological activity adjacent to the root… Bacteria Fungi Protozoa Nematodes Microarthropods Earthworms
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
Principles of Managing for Soil Health
•Minimize Disturbance of the soil
•Maximize Diversity of plants in rotation
•Keep Living Roots in the soil as much as possible
•Keep the soil covered with plants and plant residues
•Create the most favorable habitat possible for the soil food
web
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
Soil Health Toolbox •(No) or reduced Tillage •Crop Rotation Diversity •Cover Crops •Degree of Fertilizer use •Degree of Pesticide use •Livestock Which of these tools could positively affect soil health on your farm or garden?
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
Reduce/Eliminate Tillage of the Soil •Tillage is physical soil disturbance •Destroys aggregates •Exposes organic matter to decomposition •Facilitates compaction •Damages soil fungi •Reduces habitat for all members of SFW •Disrupts soil pore continuity •Promotes salinity at the soil surface
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
CO2
CO2
Organic Matter
Organic Matter
Organic Matter
Organic Matter
Organic Matter
CO2
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Agroecology & Rural Livelihoods Group (ARLG)
Reduced Tillage and Infiltration
No-, zone-, strip-, ridge-till, etc.
Less macro-fauna disturbance (i.e., earthworms)
(Source: Herbek, AGR-101; www2.ca.uky.edu) (Dan Brainard, msue.anr.msu.edu)
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Compaction Pores spaces are where plant roots get air, water, and nutrients.
Soil compaction decreases valuable pore space between soil particles.
Uncompacted soil Compacted
soil
pore
space
soil
particles
Adapted from Sulzman and Frey, 2003
Decrease in pore spaces are where
plants get air, water, and nutrients.
Adapted from Sulzman and Frey, 2003
Field Assessment
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Try this at
home!
Test your
compaction!
Use what you
have:
• Fingers
• Shovel
• Pin flag
• Rod
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
Plant Diversity through crop rotation / cover crops: •Crop diversity = Soil Food Web (SFW) diversity •Diversity Balanced/Diverse diet to Soil Food Web •Help Reduce pest pressure •Help Increase soil nutrient cycling •Reduces risk •Increased influence of living roots Feeds Soil Food Web •Increase soil aggregation and porosity to increase available water holding capacity , infiltration and percolation •Increase OM holds more available water for plants •Stimulate SFW into increased activity •Integrate grazing •Nitrogen fixation/recovery
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Agroecology & Rural Livelihoods Group (ARLG)
(Dabney, 1998)
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Agroecology & Rural Livelihoods Group (ARLG)
Organic Matter and Infiltration
(Colla et al., 2000) Minutes
Cu
m.
Infi
ltra
tion
(m
3/m
2)
agnr.umd.edu/extension
Low O.M.
High O.M.
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
Soil Organic Matter Fun Facts •Soil organic matter (SOM) is <6% of soil by weight but controls >90% of the function •Density of SOM: .6 g/cm3 Density of Soil: 1.45 g/cm3 •SOM has less density than soil so it has more space for air and water storage. •SOM is negatively charged, but binds both cations and anions •As soil organic matter increases from 1% to 3%, the available water holding capacity of the soil doubles (Hudson, 1994). •Soils stockpile 1500 gigatons of carbon in SOM, more than Earth's atmosphere and all the plants combined (Dance, 2008). •The majority of the SOM is present in the top 10 cm of soil
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
Soil Organic Matter Nutrient Bank Account. •1.0% OM = 20,000 #10,000 # Carbon (5 ton)@ $4/ton = $20 •1,000 # Nitrogen@ $.50/# = $500 •100 # Phosphorous@ $.70/# = $70 •100# Potassium@ $.40/# -=$40 •100 lbs of Sulfur@ $.50/# = $ 50 •Total$680
Mineralization Rate = 2-3% from Organic N to Inorganic N. Resulting in 20 to 30 lbs of useable N per acre.
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Agroecology & Rural Livelihoods Group (ARLG)
Drought Resilience
Crops can’t use water that doesn’t infiltrate
Organic matter
For every 1% increase in OM, another inch of water available (Emerson, 1995)
Avoiding compaction
Deep moisture
Increased storage
Increased conductivity
Role for moisture sensors
Drought and compaction prevention
(Courtesy USDA-NRCS)
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
Chemical Soil Disturbance from Fertilizer •Excessive nitrogen or phosphorus fertilizer… Short- circuits the rhizosphere •Depresses activity of natural N fixers •Stimulates bacterial decomposition of Soil OM •N at risk for leaching or denitrification •Synthetic fertilizers are salts (salinity) and can lower pH
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
Chemical Soil Disturbance from Pesticide use: •Impact of pesticides on non-target organisms not well understood. •Pesticides simplify, not diversify SFW“cides” •Produces Crop rotation restrictions •Produces Cover crop diversity restrictions
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Keep soil covered as much as possible
• Control Erosion
• Protect Soil Aggregates
• Suppresses Weeds
• Conserves Moisture
• Cools the Soil
• Provides Habitat for Soil Organisms
David Lamm, “Soil Health Farming in the 21st Century: a practical approach to improve Soil Health Planning Principles”
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
When soil temperature reaches….. 140 F Soil bacteria die
130 F 100% moisture is lost through evaporation and transpiration
113 F Some bacteria species start dying
100 F 15% moisture is used for growth
95 F 85% moisture lost through evaporation and transpiration
70 F 100% moisture is used for growth J.J. McEntire, WUC, USDA SCS, Kernville TX, 3-58 4-R-12198. 1956
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
Livestock as a practice for soil health •Add and distribute biology to soil •Cycle residues, reduce C:N ratios •Puts plant residues in contact with soil •Can help control weeds and disease •Opportunity for increased income •Increase intensity & reduce duration to improve soil health on pastures
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
How do we know if soil health is improving? •Soil aggregate stability increases •Water infiltration increases •Organic matter increases •Crop response •Plants use less water, nutrients •Less crusting, ponding, erosion •Reduced input costs •Soil Food Web analysis
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
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MATTER CYCLING IN ECOSYSTEMS • Nutrient Cycles: Global Recycling
– Global Cycles recycle nutrients through the earth’s air, land, water, and living organisms.
– Nutrients are the elements and compounds that organisms need to live, grow, and reproduce.
– Biogeochemical cycles move these substances through air, water, soil, rock and living organisms.
To know if nutrients are available in the soil for plants, TEST the Soil!
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Nutrients in Soil
• Nutrients are chemical elements and compounds found in the environment that plants and animals need to grow and survive.
– Nitrate (NO3-),
– nitrite (NO2-),
– ammonia (NH3),
– organic nitrogen (in the form of plant material or other organic compounds), and
– phosphates (PO43-)(orthophosphate and
others)
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The Big 13
• The 13 mineral nutrients, which come from the soil, are dissolved in water and absorbed through a plant's roots. There are not always enough of these nutrients in the soil for a plant to grow healthy. This is why many farmers and gardeners use fertilizers to add the nutrients to the soil.
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Macronutrients: Primary Nutrients
• Macronutrients are those elements and compounds needed in large quantities for a plant to grow.
• The primary nutrients are nitrogen (N), phosphorus (P), and potassium (K).
• These major nutrients usually are lacking from the soil first because plants use large amounts for their growth and survival.
• A fertilizer of 5-10-10 contains 5% N, 10% P, 10% K
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Macronutrients: Secondary Nutrients
• The secondary nutrients are calcium (Ca), magnesium (Mg), and sulfur (S). There are usually enough of these nutrients in the soil so fertilization is not always needed. – Large amounts of Ca and Mg are added
when lime is applied to soils.
– Sulfur is usually found in sufficient amounts from the decomposition of soil organic matter.
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Micronutrients • Micronutrients are those elements
essential for plant growth which are needed in only very small (micro) quantities and are sometimes called minor elements or trace elements.
• Micronutrients include boron (B), copper (Cu), iron (Fe), chloride (Cl), manganese (Mn), molybdenum (Mo) and zinc (Zn).
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Soil pH is a major factor
• Soil pH (a measure of the acidity or alkalinity of the soil)
• Soil pH is one of the most important soil properties that affects the availability of nutrients. – Macronutrients tend to be less available in soils
with low pH.
– Micronutrients tend to be less available in soils with high pH.
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http://www.traylorchemical.com/images/faqs/phchart.jpg
Most nutrients are highest and most toxins are lower at pH 5.5-7
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The pH can be changed
• Lime can be added to the soil to make it less acidic and also supplies calcium and magnesium for plants to use.
– Lime also raises the pH to the desired range of 6.0 to 7.0. In this pH range, nutrients are more readily available to plants, and microbial populations in the soil increase.
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Nitrogen • Nitrogen is a part of all living cells and
is a necessary part of all proteins, enzymes and metabolic processes involved in the synthesis and transfer of energy.
• Nitrogen is a part of chlorophyll, the green pigment of the plant that is responsible for photosynthesis.
• Nitrogen is usable in the forms of NO3
-, NO2-, and NH3
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Where does N come from? • Helps plants with rapid growth, increasing seed and
fruit production and improving the quality of leaf and forage crops.
• Nitrogen often comes from fertilizer application whether it is industrial fertilizer or animal waste.
• Bacteria can fix Nitrogen from the atmosphere (N2) into a more usable form.
• Decomposition of organic matter puts nitrogen back into the soil.
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Phosphorus • Like nitrogen, phosphorus (P) is an essential part of
the process of photosynthesis.
• Involved in the formation of all oils, sugars, starches, etc.
• Helps with the transformation of solar energy into chemical energy; proper plant maturation; effects rapid growth; and, encourages blooming and root growth.
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Sources of Phosphorus
• Phosphorus often comes from fertilizer, bone meal, and from rock.
• Phosphorus is found in rock and is therefore a function of the rock cycle.
– P is in limited supply and is often a limiting factor because the rock cycle is so slow!
• Phosphorus also comes from bird guano.
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Potassium
• Potassium is absorbed by plants in larger amounts than any other mineral element except nitrogen and, in some cases, calcium.
• Helps in the building of protein, photosynthesis, fruit quality and reduction of diseases.
• Potassium is supplied to plants by soil minerals, organic materials, and fertilizer.
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Calcium
• Calcium, an essential part of plant cell wall structure, provides for normal transport and retention of other elements as well as strength in the plant. It is also thought to counteract the effect of alkali salts and organic acids within a plant.
• Sources of calcium are dolomitic lime and gypsum
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Magnesium
• Magnesium is part of the chlorophyll in all green plants and essential for photosynthesis. It also helps activate many plant enzymes needed for growth.
• Soil minerals, organic material, fertilizers, and dolomitic limestone are sources of magnesium for plants.
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Sulfur • Sulfur is essential plant food for production of protein. It promotes
activity and development of enzymes and vitamins; helps in chlorophyll formation; improves root growth and seed production; helps with vigorous plant growth and resistance to cold.
• Sulfur may be supplied to the soil from rainwater. It is also added in some fertilizers as an impurity, especially the lower grade fertilizers. The use of gypsum also increases soil sulfur levels.
• The decomposition of organisms can add sulfur to the soil. • Sulfur is used by plants in the form of sulfates (SO4
2-) and sulfites (SO3
2-)
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Micronutrients
Boron (B) • Helps in the use of nutrients and regulates other nutrients. • Aids production of sugar and carbohydrates. • Essential for seed and fruit development. • Sources of boron are organic matter and borax
Copper (Cu) • Important for reproductive growth.
Aids in root metabolism and helps in the utilization of proteins. Chloride (Cl)
• Aids plant metabolism. • Chloride is found in the soil.
Iron (Fe) • Essential for formation of chlorophyll. • Sources of iron are the soil, iron sulfate, iron chelate.
Manganese (Mn) • Functions with enzyme systems involved in breakdown of
carbohydrates, and nitrogen metabolism. • Soil is a source of manganese.
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Sampling instructions for a Soil Test
1. Follow the instructions from the testing lab, there are variations 2. Fill out the form, include crop information 3. If manure or compost applied, estimate amount 4. Sampling in Fall is best, other times ok too 5. Areas of different soils, crops, or management should be tested/sampled
separately 6. Avoid non typical areas for sampling 7. Take 6-20 (depends on size area) thin slices/cores of soil to depth of 4-8
inches, mix in clean container 8. No sample should be for an area larger than 10-15acres 9. Pull out one cup of soil mix, this = 1 soil sample 10. Label samples, keep track of location and sample # on a map/sketch
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Other Tests
• Percolation (permeability), infiltration
• Bulk density
• Organic matter
• Salinity
• Ion Exchange
• Heavy and Trace Metals
• Biological activity
• Aggregate stability
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
Soil pH Test Kit DEMO- 15min
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• Water Quality
• Water Quantity
• Soil Quality
• Air Quality
Conservation practices and systems address:
Best Management Practices for Agriculture
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• Energy Conservation
• Animal Health and Welfare
• Plant Health
• Fish and Wildlife Habitat
Conservation practices and systems address:
Best Management Practices for Agriculture
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Well managed agriculture systems provide:
Best Management Practices for Agriculture
• Food, Fiber, and Wood Products
• Clean and Abundant Water
• Clean Air
• Fish and Wildlife Habitat
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• Scenic Vistas
Well managed agriculture systems provide:
Best Management Practices for Agriculture
•Open Space
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• Cultural Heritage
• Support to Local Economies
Well managed agriculture systems provide:
Best Management Practices for Agriculture
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• Enhanced Quality of Life
Social Awareness
Well managed agriculture systems provide:
Best Management Practices for Agriculture
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Best management practices,
also called conservation
practices, are implemented
based on a conservation plan.
Best Management Practices for Agriculture
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• Taking an inventory of resource conditions
Conservation planning steps include:
Best Management Practices for Agriculture
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• Identifying issues and opportunities with
the farmer
Conservation planning steps include:
Best Management Practices for Agriculture
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• Developing choices and
solutions
• Scheduling
implementation of
practices
• Evaluating effectiveness
of the plan
Conservation planning steps include:
Best Management Practices for Agriculture
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• Cross slope tillage
• Contour strip cropping
Cropping Systems
Best Management Practices for Agriculture
•Residue management
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• Cover crops / green
manure
Cropping Systems
Best Management Practices for Agriculture
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• Crop rotation
• Grassed waterways
Cropping Systems
Best Management Practices for Agriculture
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• Nutrient management
• Pest Management
Cropping Systems
Best Management Practices for Agriculture
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• Irrigation water management
• Buffers and field borders
Cropping Systems
Best Management Practices for Agriculture
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• Rotational grazing
• Fencing systems
Grazing Systems
Best Management Practices for Agriculture
•Animal trails and walkways
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• Water systems
• Nutrient management
• Pathogen control
Grazing Systems
Best Management Practices for Agriculture
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• Waste storage structures
Manure / Waste Management
Best Management Practices for Agriculture
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• Heavy use/sacrifice areas
• Composting systems
Manure / Waste Management
Best Management Practices for Agriculture
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• Transfer and application
• Nutrient management
Manure / Waste Management
Best Management Practices for Agriculture
•Septic systems
•Silage leachate collection
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• Gutter systems
• Storm drains / subsurface drains
• Sediment basins
Farmstead Management
Best Management Practices for Agriculture
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• Diversions / waterways
• Wellhead protection
• Covered heavy use areas
Farmstead Management
Best Management Practices for Agriculture
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• Riparian buffers
• Streambank protection
• Food plots
• Pollinator plantings
Habitat Management
Best Management Practices for Agriculture
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• Woodland management
• Delayed mowing
• Wetland restoration
• Invasives control
Habitat Management
Best Management Practices for Agriculture
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Best Management Practices for Agriculture
Natural Resources Conservation Service
Helping People Help the Land Through …
• Conservation Planning and Technical
Consultation
• Conservation Implementation
• Technical Standards and References
• Financial Assistance Programs
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Best Management Practices for Agriculture
Natural Resources Conservation Service
•Technical Standards and References
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Best Management Practices for Agriculture
Conservation Partners
•Natural Resources Conservation Service
•UConn Cooperative Extension
•CT Agriculture Experiment Station
•CT Department of Agriculture
•CT Department of Energy & Environmental Protection
•USDA Farm Services Agency
•USDA Rural Development
•Conservation Districts
•CT NOFA
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Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers
Questions?
Charlotte Ross, Project Coordinator, 860-875-3331, [email protected]
Kip Kolesinskas, Conservation Scientist, 860-
878-0393, [email protected]
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Advancing the Business of Farming in Connecticut Project provides new farmers
with core training and assistance to develop their farm plan, explore production options,
and grow their farming enterprise. Visit www.newfarms.extension.uconn.edu
for resources and events.
Advancing the Business of Farming in Connecticut in Partnership with Agriculture Learning Centers