Block 7: Weathering, Soils, & Surface Waters Flashcards

(23 cards)

1
Q

What is chemical weathering?

A

The chemical alteration of rocks, e.g. dissolution & secondary mineral formation

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2
Q

What is physical weathering & how does it assist chemical weathering?

A

The mechanical breakdown of rocks into smaller pieces
This creates more points of access for chemical weathering agents

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3
Q

What are primary & secondary minerals?

A

Primary minerals are inherited from igneous, sedimentary, or metamorphic rocks (e.g. feldspars, micas, quartz, olivine, plagioclase, amphiboles)
Secondary minerals are formed by chemical weathering (e.g. clays, oxides, hydroxides, carbonates)

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4
Q

How do primary & secondary minerals trend along the soil profile?

A

Primary minerals dissolve up the soil profile, whereas secondary minerals form

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5
Q

What are congruent & incongruent weathering?

A

In congruent weathering, minerals completely dissolve into constituent ions (i.e. evaporites & carbonates)
In incongruent weathering, minerals only partially dissolve & leave behind residual soil weathering products (i.e. sulphides & silicates)

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6
Q

How does weathering affect evaporites, carbonates, sulphides, & silicates?

A

Evaporites are highly soluble & the most easily weathered in the presence of a polar solvent
Sulphides weather through oxidation as bonds are formed from reduced Fe & S
Carbonates are highly soluble in acidic solutions through acid hydrolysis
Silicates have mineral-dependent solubilities & weathering rates

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7
Q

What is soil & how is it produced?

A

Soil is a mixture of minerals & organic matter consisting of secondary minerals made during silicate weathering

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8
Q

What are the 4 main soil horizons?

A

O Horizon: above ground material
A Horizon: organic-rich surface soils
B Horizon: mineral-rich subsoil
C Horizon/Saprolite: transition to bedrock, including primary minerals

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9
Q

Which 2 methods are used for interpreting weathering in soil profiles?

A
  1. Normalisation of data to the parent material to yield concentration change
  2. Normalisation of mobile to immobile content, correcting for volumetric strain
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10
Q

What is volumetric strain?

A

The change in mineral volume during weathering as water leaches out original mineral mass, creating higher porosity & lower bulk density in soils than in the protolith

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11
Q

What is the ion exchange capacity?

A

The amount of electric charge on the surface of secondary phases, which allows soil to retain ions important for pH regulation

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12
Q

What is the Chemical Index of Alteration?

A

An index using mol/kg oxide concentrations to quantify degrees of (mainly thermal) weathering experienced in soils
* Higher CIA indicates more weathering

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13
Q

Which common elements are immobile in surface waters?

A

Be, Al, Ti, Fe(III), Ti, sometimes Si

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14
Q

How does conservative Cl trace rain inputs & evapotranspiration?

A

As Cl typically doesn’t react or degrade, surface/soil water concentration directly reflects rainfall quantity & source
Cl also concentrates in remnant water according to degree of evapotranspiration

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15
Q

How can [Cl] track silicate weathering, input to grass & input from silicates, & clay uptake?

A

Silicate weathering: relationship with [Na]
Grass & silicate uptake: relationship with [K]
Clays: negative values

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16
Q

What is the difference between hydrolysis & hydration?

A

Hydrolysis: H+ replaces a cation
Hydration: H2O is incorporated into the molecule

17
Q

Which silicates are the least & most susceptible to chemical weathering?
How does this relate to order of crystallisation from igneous melts?

A

Least to most: quartz, muscovite, biotite, amphibole, pyroxene, olivine
This is the inverse of Bowen’s reaction series

18
Q

What general trend occurs in heavy metal mobility with pH?

A

As pH decreases heavy metals become more mobile
This is the same for Al

19
Q

In what environments are soils generally acidic?

A

Environments in which high amounts of rain weathering of primary minerals & leaching of base cations, i.e. humid tropics or moist temperate forests

20
Q

How does the plot of Na/(Na+Ca) vs TDS change across streams in different climate zones?

A

Tropics: High Na & low TDS due to rainfall dilution
Temperate: High Ca & medium TDS due to limestone weathering
Arid: High Na & high TDS due to evaporation; Ca becomes supersaturated & precipitates out of waters

21
Q

How does hydrolysis affect acidity?

A

Solutions are buffered by consumption of H+ ions in hydrolysis, decreasing acidity

22
Q

Which metals are amphoteric?

A

Arsenic, cadmium, iron, lead, & zinc can act as an acid or base & can therefore have higher solubilities at acidic & basic pH than at neutral ph

23
Q

How does precipitation have the capacity to dissolve surface minerals?

A

Rainwater contains little TDS & CO2 incorporation creates carbonic acid