Lesson 1: Introduction to Soils Flashcards

1
Q

soil

A

“the unconsolidated mineral or organic material on the immediate surface of the earth that serves as a natural medium for the growth of land plants.”

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2
Q

unconsolidated materials

A

loose materials composed of multiple units (e.g., sand, gravel, etc.) unlike hard, massive materials like rock

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3
Q

soil composition (well-managed)

A

usually around 50% percent of the soil’s volume is composed of solid particles (i.e. decomposed rocks or sediments), with 1-5% being organic matter

the other 50% is empty space, i.e. “pores” (25% water, 25% air)

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4
Q

organic matter

A

the live organisms in the soil, and plant, animal, and microbial residues in various stages of decomposition

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5
Q

five soil-forming factors

A

factors that cause variation in soils in different locations

  1. Parent material (i.e. starting material for a soil)
  2. Climate (precipitation, temperature, wind)
  3. Topography
  4. Biological organisms
  5. Time
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6
Q

horizons

A

In naturally formed soils, distinct layers develop. They may blend together gradually or have abrupt borders between layers, and are identified by letter codes.

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7
Q

A horizon

A

“topsoil”

The A horizon is usually the surface horizon. This is an area of high biological activity with the greatest organic matter content. It is also a zone of leaching. Most plant roots are found in the A horizon.

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8
Q

B horizon

A

“subsoil”

This layer usually contains less organic matter than the surface layer but accumulates the dissolved materials leached from the A horizon (clays, iron oxides, aluminum, and dissolved organic compounds). For this reason, the B horizon typically contains more clay than the surface layer.

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9
Q

C horizon

A

The C horizon contains unconsolidated material that has been minimally affected by the soil forming factors, and may or may not be the same as the parent material from which the soil formed.

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10
Q

landscape soils

A

“urban” soils

soils that are found in a typical neighborhood community around homes, parks, schools, offices, parking lots, and buildings

In compacted landscape soils, the horizons are scrambled and not defined, organic content is low, and air and water movement is reduced.

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11
Q

texture

A

the size of the particles that make up the soil (e.g., sand, silt, clay)

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12
Q

sand

A

the largest particle size and feels gritty

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13
Q

silt

A

moderate in size with a smooth or floury texture

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14
Q

clay

A

the smallest sized particle and feels sticky

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15
Q

loam

A

a soil with a combination of sand, silt, and clay sized particles

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16
Q

soil structure

A

structure refers to how the various particles of sand, silt, and clay fit together, creating pore spaces of various sizes

17
Q

aggregates

A

chemical and biological processes that glue sand, silt, and clay particles together

soil microorganisms including mycorrhizae, earthworms, and plant roots help created aggregates

18
Q

granular structure

A

common in the upper layer of undisturbed native soils, rapid drainage

19
Q

block structure

A

common in the lower layers undisturbed native soils, rapid to moderate drainage

20
Q

platy structure

A

common in soils high in clay, slow to no drainage

21
Q

peds

A

describes the soil’s individual aggregates or clods

22
Q

pore space

A

controls soil drainage characteristics

23
Q

large pores

A

water moves rapidly down through the soil profile, common in sandy soils

pose environmental hazards due to rapid leaching

24
Q

small pores

A

water is slow to move or may not move at all, common in compacted soil and soils with greater than 20% clay content

easily waterlog

25
Q

soil pH

A

a measurement of the acidity or alkalinity of a soil

7.0 is neutral, below 7.0 is acidic, and above 7.0 is basic or alkaline. a pH range of 6.8 to 7.2 is near neutral

26
Q

soil amendment

A

any material mixed into a soil

27
Q

humus

A

the stable end products of decay, it can take decades to decompose and is very dark in color

humus improves soil suitability for beneficial organisms and plants

28
Q

improve water- and nutrient- holding capacity in sandy, gravelly, and decomposed granite soils

A

select well-decomposed materials like finished compost, aged manure, and peat

29
Q

improve aeration and infiltration (improve structure in clayey soils)

A

select fibrous materials like composted wood chips, peat, and straw

30
Q

mulch

A

any material placed on the soil surface

31
Q

plant nutrition

A

the need for basic chemical elements for plant growth (17 elements needed for normal growth)

32
Q

fertilization

A

the application of plant nutrients to supplement the nutrients naturally occurring in the soil

33
Q

primary nutrients derived from water and air

A

carbon, hydrogen, oxygen

34
Q

primary nutrients derived from soil

A

nitrogen, phosphorus, potassium