rock weathering and soil mineralogy. physical weathering……

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Rock Weathering and Soil Mineralogy

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Page 1: Rock Weathering and Soil Mineralogy. Physical Weathering……

Rock Weathering and Soil Mineralogy

Page 2: Rock Weathering and Soil Mineralogy. Physical Weathering……

Physical Weathering……

Page 3: Rock Weathering and Soil Mineralogy. Physical Weathering……

I. WeatheringA . Chemical Weathering1. Water is critical (and heat serves as a

catalyst)2. Complex Process (involves several reactions)3. Biological Activity (helps accelerate

weathering processes)

Page 4: Rock Weathering and Soil Mineralogy. Physical Weathering……

1. Complex Process• Solution• Hydrolysis• Oxidation• Hydration• Chelation• Dialysis• Chemical Reconstitution

Page 5: Rock Weathering and Soil Mineralogy. Physical Weathering……

The negative log of hydrogen ion content

“The negative log of hydrogen in concentration”

Page 6: Rock Weathering and Soil Mineralogy. Physical Weathering……
Page 7: Rock Weathering and Soil Mineralogy. Physical Weathering……

6.02214129(27)×1023 atoms

Moles per liter

Page 8: Rock Weathering and Soil Mineralogy. Physical Weathering……

Concentration of H+ * Concentration of OH- = 10-14

[10-7 ][10-7 ] = 10-14 “Always a constant”

Page 9: Rock Weathering and Soil Mineralogy. Physical Weathering……

Concentration of H+ * Concentration of OH- = 10-14

[10-7 ][10-7 ] = 10-14“Always a constant”

pH of 0.1 M HCl = 10-1 M = log 10-1 = -1 = pH is 1

pH of 1 M HCl = 100 M = log 100 = 0 = pH is 0

pH: “The negative log of hydrogen in concentration”

Page 10: Rock Weathering and Soil Mineralogy. Physical Weathering……

“How much carbonic acid is there in rainwater?”

pH: “The negative log of hydrogen in concentration”

Page 11: Rock Weathering and Soil Mineralogy. Physical Weathering……

pH: “The negative log of hydrogen in concentration”

Page 12: Rock Weathering and Soil Mineralogy. Physical Weathering……

Why does it matter?

Page 13: Rock Weathering and Soil Mineralogy. Physical Weathering……

Why does it matter?

Ca2+ > Na+ > Mg2+ > K+ > Si4+ > Fe3+ > Al3+ MostMobile

LeastMobile

Page 14: Rock Weathering and Soil Mineralogy. Physical Weathering……

Molar BA Ratio

Page 16: Rock Weathering and Soil Mineralogy. Physical Weathering……

Molar BA Ratio

Moles of Na2O + K2O + CaO + MgO

Moles of Al2O3

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Page 30: Rock Weathering and Soil Mineralogy. Physical Weathering……

Cation Exchange Capacity (CEC):The amount of exchangeable cations that a given weight of soil is capable of holding

Page 31: Rock Weathering and Soil Mineralogy. Physical Weathering……
Page 32: Rock Weathering and Soil Mineralogy. Physical Weathering……

CEC is measured in units of Cmol/kg, which replaces milliequivilents (meq)/100 g.

Page 33: Rock Weathering and Soil Mineralogy. Physical Weathering……

CEC is measured in units of Cmol/kg, which replaces milliequivilents (meq)/100 g.

Wt. of 1 meq. = mole weight (g)charge of ion * 1000

Ex: the weight of 1 meq. of calcium is:

1 meq. Of Ca2+ = 40.08 g = 0.02 g (2) * 1000

Page 34: Rock Weathering and Soil Mineralogy. Physical Weathering……
Page 35: Rock Weathering and Soil Mineralogy. Physical Weathering……

Ex: the weight of 1 meq. of calcium is:

1 meq. Of Ca2+ = 40.08 g = 0.02 g (2) * 1000

So….the CEC of a soil containing 1.0316 g of exchangeable Ca2+ per 100 g of soil is:

1.0316 g (wt. of exchangeable Ca2+) 0.02 (wt. of 1 meq. of Ca2+)

Page 36: Rock Weathering and Soil Mineralogy. Physical Weathering……

Ex: the weight of 1 meq. of calcium is:

1 meq. Of Ca2+ = 40.08 g = 0.02 g (2) * 1000

So….the CEC of a soil containing 1.0316 g of exchangeable Ca2+ per 100 g of soil is:1.0316 g (wt. of exchangeable Ca2+) 0.02 (wt. of 1 meq. of Ca2+)

= 51.58 meq.=51.58 meq. Per 100 g, or 51.58 Cmol+/kg

Page 37: Rock Weathering and Soil Mineralogy. Physical Weathering……

C. CEC Capacities

Page 38: Rock Weathering and Soil Mineralogy. Physical Weathering……

Base Saturation

Page 39: Rock Weathering and Soil Mineralogy. Physical Weathering……

Base Saturation: the percentage of cation exchange capacity of a soil occupied by basic cations.

In general, the higher the base saturation, the higher the pH of the soil.

Why important?• Plant growth• Plant protection

Page 40: Rock Weathering and Soil Mineralogy. Physical Weathering……

Alfisols UltisolsMollisol

Page 41: Rock Weathering and Soil Mineralogy. Physical Weathering……

Alfisols UltisolsMollisol

base saturation between 35% - 50%

base saturation less than 35%

base saturation greater than 50%

Page 42: Rock Weathering and Soil Mineralogy. Physical Weathering……