cation exchange capacity

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CATION EXCHANGE CAPACITY and PLANT NUTRITION

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CATION EXCHANGE CAPACITY. and PLANT NUTRITION. Cation Exchange Capacity (CEC). Clay Particles and Humus affect chemical properties of soil complex structures with many negative charge sites negative charge sites attract positive ions called cations. CEC. - PowerPoint PPT Presentation

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Page 1: CATION EXCHANGE CAPACITY

CATION EXCHANGE CAPACITY

and

PLANT NUTRITION

Page 2: CATION EXCHANGE CAPACITY

Cation Exchange Capacity (CEC)

Clay Particles and Humus

- affect chemical properties of soil- complex structures with many negative

charge sites- negative charge sites attract positive ions

called cations

Page 3: CATION EXCHANGE CAPACITY

CECNegative charge sites are referred to as . . .

Cation exchange sites

+ attract cations from soil solution+

Page 4: CATION EXCHANGE CAPACITY

CEC

Force of attraction is called:

Adsorption

similar to force of a magnet holding iron filings

Page 5: CATION EXCHANGE CAPACITY

                          

   Figure 3.10 Unlike charges attract, like charges

repel.

Page 6: CATION EXCHANGE CAPACITY
Page 7: CATION EXCHANGE CAPACITY

CEC

Cations can move on and off particles . . .

when one leaves, another replaces it

This process is called cation exchange, and cations involved are said to be exchangeable

Page 8: CATION EXCHANGE CAPACITY
Page 9: CATION EXCHANGE CAPACITY

CEC

The number of sites that a colloid (small particle) of charged clay or humus (micelles) contains is measured by the:

Cation Exchange Capacity expressed in mEq/100g

Note: newer units expressed in cmolc/kg

Page 10: CATION EXCHANGE CAPACITY

CEC

may range from:

2.0 mEq/100g for sand

to

> 50 mEq/100g for some clays

humus 100-300 mEq/100g

Page 11: CATION EXCHANGE CAPACITY

CEC

How fertile can a soil be?

Does applying more fertilizer always provide more nutrients to plants?

How much of the CEC is actually filled with cations?

Page 12: CATION EXCHANGE CAPACITY

CEC

The proportion of the CEC occupied by basic (+) nutrients such as Ca, Mg, K, Na, is called:

Percent Base Saturation and is an indication of the potential CEC of a given soil

Page 13: CATION EXCHANGE CAPACITY

CEC

Estimations that > 99% of cations in soil solution are adsorbed . . .

does not mean that percent base saturation is 99%

Page 14: CATION EXCHANGE CAPACITY

CEC

Example:

A soil with CEC of 10 mEq/100g has 6 mEq/100g of bases (Ca, Mg, K, Na) occupying exchange sites

What is the percent base saturation of the soil?

Page 15: CATION EXCHANGE CAPACITY

CEC

6 mEq/100g bases

10 mEq/100g sites

= 60 % base saturation

Page 16: CATION EXCHANGE CAPACITY

CEC

Cation Exchange is determined by:

1) strength of adsorption

2) law of mass

Page 17: CATION EXCHANGE CAPACITY

CEC

Strength of adsorption is as follows:

H+ and Al3+ > Ca2+ > Mg2+ > K+ > NH4+ > Na+

Page 18: CATION EXCHANGE CAPACITY

CEC

Law of Mass

the more of one ion available,

the greater the chance of adsorption

Page 19: CATION EXCHANGE CAPACITY

NUTRITION

There are at least 17 elements recognized as essential nutrients for plants;

we will recognize 18 elements:

C, H, O, P, K, N, S, Ca, Fe, Mg,

Mn, Mo, Cl, Cu, Zn, B, Co, Ni

Page 20: CATION EXCHANGE CAPACITY

NUTRITIONNutrients grouped into 2 categories according to the

relative amount used by plants:

Macronutrients – major elements; large amounts

Micronutrients – minor elements; small amounts

Both are essential for optimal plant production

Page 21: CATION EXCHANGE CAPACITY

NUTRITION

Note:

C, H, O . . .

essential elements not considered innutritional studies;

Why?

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NUTRITION

> 95% of plant dry wt. from C, H, O;

(balance from macro, micro and other elements)

Page 23: CATION EXCHANGE CAPACITY

NUTRITION

Except for C, H, O . . .

- Nitrogen (N) is present in greatest concentrations;

- Plants respond readily to Nitrogen (N)