Soil Flashcards

1
Q

an essential component on Earth that enabled life to exist on the planet and continues to support.

A

Soil

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2
Q

The term pedosphere is derived from the Greek words “” which means soil and “”which means sphere

A

Pedon and sfaira

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3
Q

Soil is composed of

A

Soil is generally composed of 45% mineral ( gravel, sand. silt and clay), 25% air, 25% water and 5% organic matter ( humus, roots, dead and decaying organisms). These components reflect the processes hat formed the so

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4
Q

Is a loose mixture of rock fragments, organic matter, water, and air – that portion of the regolith ( rhegos=blanket, lithos = stone) that support the growth of vegetation

A

Soil

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5
Q

First step of soil formation

A

Weathering of parent rock into smaller pieces

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6
Q

What causes soil to form?

A
  • Rock is broken down by weathering and plant root growth to form sediment
  • Some microorganisms, such as bacteria and fungi, decompose the remains of plants and animals
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7
Q

What factors determine how long it takes for soils to form?

A

These factors include parent material, time, climate, plants and animals, and topography

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8
Q

The source of the weathered mineral matter from which soil develops. The rate of weathering depends on the structure of the rock and minerals that make up the rock. When the parent material is bedrock, the soils are termed residual so

A

Parent material

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9
Q

By contrast, those developed on unconsolidated sediment are called

A

transported soil

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10
Q

an important component of every geological processes and soil is no exception. The longer a soil has been forming, the thicker it becomes and the less it resembles the parent materia

A

Time

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11
Q

Soil usually develops more quickly in warm, wet areas than in cold, dry areas. The most influential factor in soil formation. Variations in temperature and precipitation determine whether mechanical or chemical weathering prevails

A

Climate

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12
Q

The biosphere plays a vital role in soil formation. The types and abundance of organisms present have a strong influence on the physical and chemical properties of soil. Without a lot of_, soil tends to develop slowly

A

plants and animals

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13
Q

The lay of the land can vary greatly over short distances. Such variations can lead to the development of a variety of localized soil types.

A

Topography

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14
Q

Defined as the relative proportion of the particle sizes in the soil – sand, silt and clay.
- Clay ( <0.002 mm) – smallest particle
- Silt ( 0.002 – 0.005 mm)
- Sand – ( 0.005 – 2.00 mm

A

Soil Texture

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15
Q

Particles larger than coarse grained sand are called_ if they are > 75.00mm

A

gravel and rock

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16
Q

ideal soil for agriculture use since it provides good aeration and drainage properties of large particles with nutrient nutrition and water holding abilities of clay particle

A

Loam

17
Q

is the superficial or topmost layer of the soil that is primarily composed of decaying organic matter, living organism, and fresh soil. The color of the topmost layer is normally either brown or black due to its organic composition. It is the layer that hosts most of the roots of small vegetation cover like grass and contains about 20% of organic matter

A

O-Horizon

18
Q

is the second layer of the soil. It is referred to as the top-soil. It is composed of highly decaying organic matter and minerals, and its color ranges from gray to brown. It is the layer that hosts many plants and supports many agricultural and grassland areas. Thus, seed germination and the growth of plant roots take place in this soil layer. It is distinguishable by the different soil types including loam, clay, sand, and silt. It is also the soil layer that is most vulnerable to water and wind erosion

A

A-horizon

19
Q

This is the third and the thinnest soil layer, and it is lighter in color compared to the A-Horizon. It is termed as the eluviation layer due to the leaching of minerals. As a result, this layer is depleted of aluminum, clay, organic compounds, and other soluble elements. It is mainly made up of silt and sand after losing most of its minerals as they drip down through the soil

A

E-horizon

20
Q

is the fourth layer and is also referred to as the sub-soil. It is mainly made up of large rocks, clay, and bedrock. The color of the sub-soil is lighter than the layers above it and ranges from rust to tan. It is also composed of minerals and little organic matter. The sub-soil accumulates a lot of clay, aluminum, iron, and organic compounds from the layers above it from the dripping down of mineralized water through a process known as illuviation. Hence, it is sometimes called the illuviation zone. It is the layer where the roots of big trees en

A

B-horizon

21
Q

This is the fifth layer of the soil and it also known as the regolith. Plant roots do not go through this layer and it has very little organic matter. The color of the_ is gray and is made up of fragmented pieces of bedrock. Also, it has compacted sediment and cemented geological material. Very little activity is present in this layer but there may be instance of additions or losses of minerals and other soluble compounds.

A

C-Horizon

22
Q

The_ is the sixth and final layer of the soil. It is also known as the bedrock. The materials here are mainly solid un weathered rock that are cemented and compacted by the weight of the overlying layers. The color of this layer is gray with several hard rocks. This layer is beyond 50 meters from the top-soil. Some of the rocks found here include granite, limestone, and basalt

A

R-Horizon

23
Q

describes the relative amounts of differently sized soil particles

A

Soil texture

24
Q

Soil properties are used to classify different soil

A

These properties include soil texture, color, chemistry, pore space, and fertility

25
Q

Soil particles are classified as

A

sand (largest particles), silt, or clay (smallest particles

26
Q

Soil color depends on the _matter that make up the soil

A

minerals and organic

27
Q

is a measure of how acidic or basic the soil i

A

Soil pH

28
Q

describes the spaces between soil particles

A

Pore space

29
Q

describes how well a soil can support plant growth

A

Soil fertility

30
Q

are light, warm, dry and tend to be acidic and low in nutrients. Sandy soils are often known as light soils due to their high proportion of sand and little clay (clay weighs more than sand). These soils have quick water drainage and are easy to work with. They are quicker to warm up in spring than clay soils but tend to dry out in summer and suffer from low nutrients that are washed away by rain. The addition of organic matter can help give plants an additional boost of nutrients by improving the nutrient and water holding capacity of the soil

A

Sandy soil

31
Q

are heavy soils that benefit from high nutrients. Clay soils remain wet and cold in winter and dry out in summer. These soils are made of over 25 percent clay, and because of the spaces found between clay particles, clay soils hold a high amount of water. Because these soils drain slowly and take longer to warm up in summer, combined with drying out and cracking in summer, they can often test gardeners

A

Clay soils

32
Q

are light and moisture retentive soils with a high fertility rating. As silt soils compromise of medium sized particles they are well drained and hold moisture well. As the particles are fine, they can be easily compacted and are prone to washing away with rain. By adding organic matter, the silt particles can be bound into more stable clumps.

A

Silt soil

33
Q

are high in organic matter and retain a large amount of moisture. This type of soil is very rarely found in a garden and often imported into a garden to provide an optimum soil base for planting

A

Peat soil

34
Q

can be either light or heavy but always highly alkaline due to the calcium carbonate or lime within its structure. As these soils are alkaline they will not support the growth of ericaceous plants that require acidic soils to grow. If a chalky soil shows signs of visible white lumps then they can’t be acidified and gardeners should be resigned to only choose plants that prefer an alkaline soil

A

Chalk soil

35
Q

are a mixture of sand, silt and clay that are combined to avoid the negative effects of each type. These soils are fertile, easy to work with and provide good drainage. Depending on their predominant composition they can be either sandy or clay loam. As the soils are a perfect balance of soil particles, they are considered to be a gardeners best friend, but still benefit from topping up with additional organic matter

A

Loam soil