Lecture 11: Chapter 7- Soil Acidity, Alkalinity, Salinity, Sodicity Flashcards

1
Q

Where are alkaline soils found relative to climate?

A

Grasslands and dryer climates have higher soil pH (alkaline)

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2
Q

how to fix saline soils

A

-overirrigation so water can wash salt out of the rooting zone
-adding gypsum provides competition from calcium
-plant more salt tolerant plants
-plant deep rooted plants to add more air

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3
Q

Explain how an alkaline soil pH affects the availability/toxicity of plant macro- and micronutrients

A

UNSTABLE SOIL STRUCTURE, FE AND P DEFICIENCY
-Alkaline soils have available plant nutrients
-Increased amounts of Ca, Mg, Mo
-Phosphorus, Iron, and Manganese precipitate

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4
Q

Explain how alkaline soils can be improved for agricultural use or managed to reduce to risk of erosion

A

-adding organic matter or compost

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5
Q

Discuss how soil pH affects the activity and composition of the soil microbial community and availability of plant nutrients

A

-Fungi easily available with wide range of pH
-Bacteria and plant nutrients less available at lower pH
-Phosphorus, Iron, and Manganese ten to precipitate at low and high pHs (not at neutral)
-Increase of Al, Fe, Mn, and Zn at lower pHs

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6
Q

Explain the term base saturation and why Al3+ is considered an acidic cation

A

base saturation:
Al3+ ions have a strong tendency to hydrolyze, splitting water molecules into H+ and OH- ions, and to form hydroxy Al ions.

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7
Q

active acidity

A

defined by the H+ ions activity on the soil solution. determines the solubility of many substances and provides the soil solution environment to which plant roots and microbes are exposed

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8
Q

List the 3 dominant soil pH buffering systems and their approximate pH range

A

Buffered by aluminum compounds: pH 3-4.5
Buffered by cation exchange and pH dependent charge sites: pH 4.5-7
Buffered by carbonates: pH 7-9

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9
Q

Describe where acid soils are found relative to climate, and how the typical range of soil pH associated with specific vegetation types/land use

A

Humid and Temperate climates that have a wet climate, like the east coast, have acidic soils

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10
Q

List processes that result in the acidification of soils and how they have been accelerated by humans

A

-ADDING ORGANIC MATTER
-OXIDATION OF N AND S FERTILIZERS
-ALUMINUM
-CATIONS LOSS VIA PLANT UPDATE OR LEACHING
-WET AND DRY ACID DEPOSITION FROM THE ATMOSPHERE
-ACID RAIN

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11
Q

Explain how soil acidity affects the availability/toxicity of plant macro- and micronutrients

A

LOSS OF MACRONUTRIENTS (Ca, Mg,K) Al TOXICITY, P DEFICIENCY

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12
Q

Explain how acid soils can be improved for agricultural use or managed to protect ground and surface waters

A

-raising soil pH by liming
-amelioration of Al toxicity= not changing pH by adding gypsum or organic matter to get rid of Al
-for agricultural use: ash creates a lot of Ca (calcium) so people have been adding ash to their soils to increase pH for farming

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13
Q

Acidifying process equation

A

CO2 + H2O -> H2CO3 <-> HCO3 - + H+ <-> CO3 2- + H+
(Carbon dioxide-> carbonic acid-> bicarbonate->carbonate)

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14
Q

How is carbon dioxide produced?

A

-[in atmosphere] respiration of plants and animals and combustion processes (~400ppm)
-[in soil] respiration

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15
Q

Acidification of soils: organic matter

A

-adding organic matter to soils acidifies them (like adding mulch, fertilizer, and sewage sludge)
-soil organic matter contains a lot of functional groups from which H+ ions can dissociate. they can form soluble complexes with non-acidic cations (Ca2+, Mg2+) and facilitate their leaching

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16
Q

Acidification of soils: aluminum

A

-weathering destroys minerals and releases Al which makes soils more acidic
-dissolved Al 3+ is highly toxic to most organisms and responsible for much of the deleterious impact of soil acidity on plants and aquatic organisms
-Al 3+ ions have a strong tendency to hydrolyze, splitting water molecules into H+ and OH- molecules and to form hydroxy Al ions

17
Q

Acidification of soils: cations loss via plant uptake or leaching

A

-plants add a lot of H+ ions to take nutrients so they also acidify soils

18
Q

Acidification of soils: wet and dry acid deposition from the atmosphere

A

-SO2 emissions from combustion of coal causes acid rain
-NOx comes from atmosphere and combustion of carbon because it gets so hot it splits NO2 from air to form NOx

19
Q

salt replaceable (exchangeable) acidity

A

involving the aluminum and hydrogen that are easily exchangeable by other cations in a simple unbuffered salt solution.

20
Q

residual acidity

A

accompanied by hydrogen and aluminum ions. residual acidity usually a lot larger than the active or salt replaceable acidity. can be neutralized by limestone or other alkaline materials

21
Q

total acidity

A

total acidity = active acidity + salt replaceable acidity + residual acidity