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HCS412 Forage Crops
Soil fertility and fertilizer- Chapter 12 (pg 263-293)

Introduction

Essential nutrients and micro-nutrients

Cation exchange capacity

Potassium

Sodium, magnesium, calcium

 

 

 

 

 

 

 

Introduction to soil fertility

Fertility is the capacity of the soil to provide the nutrients needed for plant growth
No quantitative definition or measurement
Includes chemical composition (CEC), parent material (basic igneous rocks), physical structure (porous, high water holding capacity, aerated), soil biological activity (soil organic matter)
Fertility is the basis of plant production
Soil fertility determines the performance and quality of desirable forage species
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Macro- & micro-nutrients, essential & non-essential

macro-nutrients are those essential minerals that exceed 0.1% of plant dry weight
C, H, O, N, P, K, S, Ca, Mg

micro-nutrients (or trace elements) are those essential minerals that are typically <0.05% of dry weight (500 ppm)

include silicon (Si), boron (B), iron (Fe), manganese (Mn), copper (Cu), zinc (Zn), chlorine (Cl), molybdenum (Mo) and nickel (Ni) (in order of decreasing abundance)

non-essential nutrients are those nutrients present in plants but are not essential for plant function. Typically many of these are required for animal function

include silicon (Si), chlorine (Cl), sodium (Na), iodine (I), chromium (Cr), cobalt (Co), and selenium (Se)

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Cation exchange capacity

CEC is the weak electrostatic charge on soil particles, resulting from
loss of H+ ions, which attracts soil cations
holding them in a plant-available form

Depends on

- soil micro-structure
- proportion of clay (SA:volume ratio)
- mineralogy of parent material
- pH
- low <12 meq/100 g soil, high >12 meq/100 g soil


Diagram of CEC
click to enlarge (44kb)


Effect of liming on CEC
click to enlarge (65kb)

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Potassium (potash) (pg 281-283)

Historically was applied to soil in the ash from blast furnaces
Released into the soil by the mineral apatite
or applied as fertilizer
essential in plants, promotes nodulation in legumes, important in osmotic adjustment (drought tolerance and freezing resistance), metabolic processes
in fertilizer is measured as K2O
Molecular Weight
K 39.098 78.2 83%
O 15.9994 16.0
94.2

in soil -
is measured as kgK/ha (lb/acre) or ppm (g/1000 kg)

It takes 4 lbs/acre of K2O to increase soil test by 1 lb/acre
It takes 8 lbs/acre of K2O to increase soil test by 1 ppm
Soil K should be at least 300 kg/ha (270 lb/ac), depending on CEC, and soil K supplying power

in forage is measured as ppm (g/1000 kg) or % (g/100g)

desirable levels in forage are at least 2.5%

high losses when forage is removed as hay/silage that must be replaced by fertilizer (see pg 277)

 

 

Sodium, calcium, magnesium

Na

- not required by plants, and in excess can displace K+
- when present in plants it does help regulate osmotic balance
- it is required by animals, hence is required in forage

Mg

- required by plants for enzymatic function (chlorophyll)
- typical levels are 0.25-0.30%
- it is required by animals, deficiency results in hypomagnesemia of lactating cows
- can be applied as dolomite (Ca CO3/MgCO3)
- can be suppressed by Ca (in lime) or high rates of K

Ca

- minor role in plants, contributes to good soil structure
- typical levels are 1-2%
- it is required by animals for bone growth
- can be applied as lime (Ca CO3) or dolomite (Ca CO3/MgCO3)
- increases soil pH

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