Topic 6) Soil Acidity Flashcards

1
Q

Sources of Hydrogen Ions

A

Carbonic Acids.
Accumulation of Organic Matter.
Oxidation of Nitrogen (Nitrifaction).
Oxidation of Sulfur .
Acids in Precipitation.
Plant Uptake in soil

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1
Q

Carbonic Acids

A

Most Common contributor to soil acidity.
Weak acid.
CO2 formed from root respiration and soil microoganisms.

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2
Q

Accumulation of Organic Matter

A

Forms soluble complexes with Cation Ca2+ and Mg2+.

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3
Q

Oxidation of Nitrogen

A

Oxidations reactions produce H+ ions.
Reduction consumes H+ ions.

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4
Q

Acids in Precipitation

A

Rain, Snow, and fog can contain acids that can contribute H+ ins

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5
Q

Plant up take of Cations

A

Plant roots exude H+ ions to balance cation uptake

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6
Q

How do plants maintain pH

A

They realse bicarbonate to maintan charge balance.

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7
Q

Aluminum role in soil pH

A

H+ ions attack sturture of mineral releasing AL3+ ions.

Then these ions become adsorbed on the CEC sites wihc mines theres more H+ in the soil

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8
Q

Pools of Soil Aciditiy

A

Activie Acidity
Exchangeable Acidity
Resdual Acidity

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9
Q

Active Acidity

A

Defined by the H+ ions active in the soil solution.
very small compared to other pools

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10
Q

Exchangelable Acidity

A

Exchangeable hydrogen and aluminiun ions.
can be released into the soil solutition by cation exchange.

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11
Q

Residual acidity

A

nonexchangebale hydrogen adn aluminun ions.

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12
Q

Buffering in soils

A

The ability to resistence the change of the pH in the soil.

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13
Q

How do we measure pH

A

pH strips
pH selective meters

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14
Q

Nitrogen fertilization

A

When nitrogen is added to the soil oxidations occurs which results in strong organic acids. So excess fertizer is harmful.

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15
Q

Acid Precipiation Pathway

A

Strong acids mobilize aluminminun and this increase Al3+ and H+ ions in the soil solution.

16
Q

How can we treat soil pH

A

by liming the soil. The addition of alkaline materials that provide associated bases of weak acids. The higher the CEC of the soil the more lime is required