soil properties Flashcards

1
Q

soil minerals?

A

ineral = sand, silt, and clay

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2
Q

soil texture?

A

Coarse= loose, more sand, less clay
Fine = heavy, more clay, less sand
Loamy= mixture

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3
Q

what acts as glue? pores?

A

rganic matter and clay act as glue to hold together aggregates
Pores are the spaces between aggregates that affect water and air movement

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4
Q

what odes porosity impact?

A

he porosity changes the rate of water and nutrients leaching through which changes the
concentration of them through the soil profile
Size of pores and total pore space in influenced by soil texture

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5
Q

describe coarse soil

A

Course soil: large pores but less total space affecting water infiltration, percolation, and
aeration

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6
Q

describe fine soil

A

Fine soil: small pores but more total space affecting water infiltration, percolation and
tends to waterlog

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7
Q

sandy loamy vs clay loamy?

A

Sandy loamy – fastest to percolate
Loamy
Clay loamy – slowest to percolate which can be beneficial to allocate water to top layer
where it may be limiting

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8
Q

permeability?

A

how fast air and water moves through soil (sand is more permeable than clay)

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9
Q

saturated soil?

A

pores are full of water, water drains b/c of gravity until field capacity (no more
free drainage)

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10
Q

unsaturated soil?

A

flow until wilting point (water held tightly by soil to be removed by plant)

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11
Q

what is field capacity? when is it low vs high

A

Field capacity – no more free draining
-Sand has lower field capacity because its drains better with gravity and had smaller total
space and has a lower wilting point because grains don’t hold water well
- Clay has enhanced field capacity and higher wilting point because although having
smaller pores, they have more percentage of pores thus can hold more water

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12
Q

5 organic content functions?

A
  1. Importance as nutrient
  2. Holds water (field capacity and wilting point)
  3. Cation exchange capacity: ability of soil to hold onto nutrients (cations) for plant use and
    prevent leaching beyond roots
  4. Decomposition
  5. Mycorrhizae – fungi symbioses with plants, increases plant water and nutrient absorption
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13
Q

what is soil solution?

A

the soup of dissolved chemicals available for plants and soils organism, containing
ions
-input from atmosphere and transformations and output through plant uptake,
transformations to solids

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14
Q

what is CEC

A

Cation Exchange Capacity
The ability of soil to hold onto nutrients (cations) for plant use and prevent leaching beyond roots
-Indicator of soil fertility, quality, and productivity
-Weaker cations are removed first

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15
Q

what is CEC influenced by?

A
  1. Soil texture (meq/100g) the number of ions that can be held:
    Sand (light) 3-5
    Sand (dark) 10-20
    Loam 10-25
    Clay 20-50
    Organic 50-100
  2. Strength of absorption (AL3+ strongest, Na+)
  3. Relative concentration of cations
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16
Q

AEC?

A

Anion Exchange Capacity
-Phosphate, Sulfate, Chloride, (Nitrate is weakly held to soil thus leaches)
-Most soils are negative

17
Q

when is AEC high

A

A low pH = high AEC (more positive charge)

18
Q

pH affects?

A

pH affects:
1. Nutrient availability
2. Organisms

19
Q

pH is affected by?

A
  1. acids from plants and soil microbes
  2. plant litter
  3. Parent materia