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Master Gardeners’ Advanced Training Master Gardeners’ Advanced Training

Master Gardeners’ Advanced Training - PowerPoint Presentation

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Master Gardeners’ Advanced Training - PPT Presentation

June 2015 Q amp A Soils and Soil Fertility Trish Steinhilber psteinhiumdedu soil solution soil air primary minerals secondary minerals residues and byproducts humus biomass ID: 631355

organic soil high nutrient soil organic nutrient high medium texture plants water growth waste year capacity pores nutrients needed mineralization loams type

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Slide1

Master Gardeners’ Advanced TrainingJune 2015

Q & A – Soils and Soil

Fertility

Trish Steinhilber

psteinhi@umd.eduSlide2

soil solution

soil air

primary

minerals

secondary

minerals

residues

and by-products

humus

biomass

inorganic solids

organic solids

pore spaceSlide3

Organic Matter

75%

10%

15%

Department of Environmental Science and TechnologySlide4

Growth Factors:

What do plants need to grow?

1. water

2. oxygen

3. heat4. carbon dioxide

5. mechanical support6. nutrientsSlide5

Soil Aeration - The exchange of O

2

and CO

2 between the soil pores and the ambient atmosphere

HillelSlide6
Slide7

Compaction

bulk density high enough or pore space low enough to negatively impact plant growth

bulk density >1.6 grams per cubic centimeter or pore space <40% will restrict root growth

information on either is difficult to obtainSlide8

Balance Between Water and Air

macropores (large pores)

drain quickly after rain or irrigation

allow rapid infiltration of rainfall and replenishment of oxygen in the root

zone

mesopores (medium-sized pores)“storage pores”hold water in form most plants can usemicropores (very small pores)

water is held too tightly to be used by most plantsrefuge of soil organisms when soils dry outSlide9
Slide10
Slide11

fine texture

medium texture

coarse texture

available water capacity

medium

high

low

nutrient holding capacity (CEC)

high

medium

low

infiltration & percolation

slow

medium

fast

crusting

high

medium

low

compaction

high

medium

lowSlide12

Soil Texture and Cation Exchange Capacity

Soil Texture

Cation Exchange Capacity

cmol

c

/kg

sands

fine sandy loams

loams and silt loams

clay loams

clays

1-5

5-10

5-15

15-30

>30 Slide13

What is a fertile soil?

one that provides an adequate supply of all nutrients throughout the entire growing

season

test soil

Is soil too acidic for plants being grown?

Are major nutrients present in adequate supply? Lime first, then

add other nutrients if needed.Slide14

soil acidity

:

the

adverse condition in the soil solution in humid regionsSlide15
Slide16

Too much or too little ….Is too much of any nutrient bad for plants?

Is too much phosphorus bad for plants?

Is too little of a nutrient bad? Slide17
Slide18

Soil Tests and Their Interpretation

Soil Test Category

Interpretation

very low, low

nutrient will, in all likelihood, limit plant growth

medium

nutrient may not be limiting; addition of nutrient advisable

sufficient, optimum or high

nutrient supply is OK; no more is needed

high, very high or excessive

nutrient supply is more than adequate; no more is neededSlide19

Lowering Phosphorus Soil Test Levels

possible

not needed

not ethical (personal opinion) Slide20

What Nutrient Source Should Be Used?

most organic sources are mixtures of N, P and K

appreciate single source fertilizers

ammonium sulfate, ureatriple superphosphate

muriate of potashSlide21

Composting Organic Materials

thermophilic

, aerobic process which changes

readily-decomposable compounds to more stable compounds

humus-like end productrequires the correct mixture of starting materialsbrown (high C/N) and green (low C/N)requires aerationSlide22

How Does Composting Alter an Organic Material?

ammonium and nitrate virtually

disappear

virtually all of the nitrogen is organic nitrogen

- N is released more slowly in composts than in feedstock materialslow in pathogens; friable and crumbly; pleasant, earthy odorSlide23

Poultry Litter from Delmarva(Preusch)

Type

Soil Texture

Mineralization Rate

fresh

sandy loam

.42

composted

sandy loam

.085

fresh

clay

.35

composted

clay

-.055Slide24

Mineralization Rates of Meat & Fish Processing Residuals (f-min)

Material

Type

Year of application

blood meal

0.65 - 0.70

feather meal

hydrolyzed

fresh

0.60 - 0.65

0.10

pelletized fish by-product

0.93

* fraction of original organic NSlide25

Mineralization Rates of Yard Waste and Composts (f-min)

Material Type

Year of application

Huck’s

Hen Blend

(VA)

(8 parts yard waste - 1 part hen manure, C/N = 29)

0.002

Panorama

Pay Dirt

(VA)

(1 part yard waste - 2 parts poultry litter, C/N = 18)

0.05

grass clippings (NJ)

0.25 (scl)-0.40 (sl)

* fraction of original organic NSlide26

Mineralization Rate Composts (f-min)

Material Type

Year of application

Bovung

1

-0.02

Fertilife

1

-0.02

Erth-rite-C

1

0.05

on-farm sheep manure & house-hold vegetable waste compost

-0.05

* fraction of original organic N,

1

Douglas and MagdoffSlide27

Gutser et al., 2005, J. Plant Nutrition and Soil ScienceSlide28

Protect the Soil Surface (esp. in fall)

minimizes erosion

protects soil aggregates

conserves moisture

moderates soil temperatureSlide29

Protect the Soil Surface –How?

protect soil from direct impact of rainfall

encourage a complete crop

canopy

mulchplant a cool season cover crop

minimize bare soil all seasons of the year!Slide30

Soil Tilth

a soil property that assesses the suitability of soil to support plant growth

a physical condition of a soil that relates to its ease of tillage, the impedance of seedling emergence and root penetrationSlide31

Tips for Maintaining Good Tilth

add organic matter

food for most soil creatures (heterotrophs)

amendments

cover crops**

warm and cool season choicesuse mulchmoderates temperature and moisture content

protects soil from crusting and erosionminimize extreme tillagerototillingSlide32

Questions? www.extension.umd.edu

/anmp

“Workshop Tools” tab

Soils (Basic) cell