Soil horizon/profile Flashcards

1
Q

What is a Soil Horizon/ profile?

A

An area used to indicate the type of soil in an area

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2
Q

How do you obtain a soil horizon?

A

Dig a pit and measur the soil depths

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3
Q

Name the horizons typically found

A
O-Organic/leaf litter layer
A-Top Soil
B-Sub Soil
C-Parent Rock
Bed Rock
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4
Q

Describe the leaf litter layer

A

Has turf/weeds/plant material on it

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5
Q

Describe Top Soil

A

The part used for crops
A mix of organic matter, gravel, stones, animal and plant waste.
Dark in colour due to presence of humus

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6
Q

Describe Sub soil

A

Lighter in colour as less humus
Nutients from above layer leached down so more clay like structure
Less soil organism life and less plant roots

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7
Q

What is Humus?

A

The black jelly that coats soil particles.
Created by broken down organic matter created by soil organisms and bacteria in soil
Gives top soil it’s dark colour

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8
Q

What is weathering?

A

The break down of rocks by:

Physical-water, wind, heat, frost, glaciers

Chemical: rainfall (carbonic acid)

Biological: action of all organisms-humans and animals and lichens on rocks

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9
Q

How does water break down rocks?

A

Moving water can carry particles in it.
The faster it moves the more it can carry.
Rocks being carried, knock against each other and those on the river bed so are scoured down.

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10
Q

How does wind break down rocks?

A

Sand blasting.

Wind carries abrasive particles and they rub against each other.
typically in hot climates

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11
Q

How does frost weather rocks?

A

In temperate areas.
Water gets into cracks, expands as it freezes, and that pressure forces the rock to crack more
Common in porous rock like chalk and limestone

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12
Q

Glaciers weather rocks how?

A

Ice sticks to adjacent rocks, the debris in the glacier scours against other material as it moves downhill like a scrubbing brush

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13
Q

What is biological weathering?

A

The action of plants and animals including humans on rock.

Eg: patches of lichens on rock
Humans mining

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14
Q

List three symptoms that indicate plants are lacking in nutrients

A

Chlorosis- yellowing of foliage
Stunted growth
Reduced yield/fruiting
Bitter pit in apples that are calcium deficient
Leaves can go purple in tomatoes that lack phosphorus

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15
Q

How can the growth of plants be increased without using fertiliser?

A

Use of organic mulch-reduces water loss and suppresses weeds

Remove weeds-reduces competition for nutrients, light and water

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16
Q

How can the growth of plants be increased without the use of fertilisers?

A

Use of mulch-suppresses weeds and retains moisture

Remove weeds-reduces competition for water, light and nutrients

Adequate water supply

Avoid overcrowding

Suitable temperature to induce growth of plant

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17
Q

Name a distinct horticultural situation for the use of the following fertiliser:

Top dressing
Base dressing
Liquid feed
Foliar feed

A

Top dressing: lawn
Base dressing- tree planting
Liquid feed-tomato’s
Foliar feed- camellias and roses (to overcome lime induced chlorosis)

18
Q

State two effects of pH on soil structure

A

Soil organisms cannot decompose OM as efficiently so less nutrients put into soil

Also less soil organisms in general

Flocclation necessary so soil more workable

19
Q

Describe the use of one named material to raise pH

A

Lime lowers acidity.

After digging apply 500g per sq metre

Lime isn’t effective on dry soil so must be watered in

Must be incorporated into soil

Use a lime spreader or spread by hand

Must be crushed or in powder form as not very soluble

Carry out liming prior to a crop being sown/planted

20
Q

What is a benefit of using sulphur?

A
Easy to apply
Measured accurately 
Fast acting
No impact on soil structure
Can be slow to act depending on particle size and requires re-application
21
Q

What is advantage of adding organic matter

A
Improves soil structure
Adds micro-organisms to soil
Natural
Sustainable
The ability of om to lower pH of soil is variable and requires re-application
22
Q

Describe how the formation of a soil cap can form in the surface of soil

A

Falling rain or over watering/cultivation caused soil structure to break down.

Lack of Organic matter contributes

More common in fine soil as particles bond together and form a crust when they dry out

As there is nothing to hold the particles together, they fall into the gaps in the soil surface causing them to block so surface water runs off.

23
Q

List three ways of minimising a soil cap

A

Water using a rose on watering can -or upturn it.

Avoid working on soil if too dry or rain imminent

Use a layer of Organic matter or mulch to protect surface
Hoe regularly between rows and seedlings

24
Q

State two effects a soil cap can have on plant growth

A

Seedlings cant penetrate cap

Water runs off surface , roots cant access water so wilting and poor growth occurs

roots unable to access oxygen as pore spaces in soil are filled

25
Q

What is meant by a pore space?

A

Pores are the spaces between the solid matter of soil

Macropores
mesopores
Micropores

26
Q

What is Available Water Content?

A

Water available for a plant to uptake and is held on the mesopores

Available water decreases as the volume of air in the soil increases

27
Q

Saturation Point

A

This is reached when all the pore spaces in the soil are filled with water

28
Q

Permanent Wilting Point

A

No more water available in soil for plant

macropores and mesopores are filled with air

No water available to plant in root zone

29
Q

Soil moisture deficit

A

the amount of water required to bring the soil back to field capacity

30
Q

What is parent material?

A

The base level of a soil horizon

Has been weathered over vast periods of time

All the smaller, broken down pieces are mixed throughout the top and subsoil

31
Q

What are the main soil types?

A

Loam
Sand
Silt
Clay

These are called soil separates

32
Q

Describe loam

A

A mixture of sand, silt and clay
Ideal for most crops
Well drained
Aerated with a balance of pore spaces

33
Q

Describe a sandy soil

A

particles are 0.05-2.0mm in size

85% or more of sand

No more than 10% clay

Heats up quickly

Short of nutrients-needs watering and feeding often “hungry”

Easily worked-dries quickly/good drainage

Large pores

Feels gritty when wet

Adding OM helps to bind particles together

34
Q

Describe a clay soil

A
40% or more clay
particles less than 0.002mm in size
Holds a lot of water and nutrients
poorly drained
slow to warm up in spring
prone to compaction especiallty when wet
Heavy soil, cloddy lumps
Feels slippy when wet
35
Q

How can a clay soil structure be improved?

A

frost helps break down the large lumps-frost crumb

weathering helps improve structure

Adding bulky OM opens air spaces and improves drainage

Adding Lime helps decrease acidity and encourages it to form crumbs

36
Q

Describe a silt soil

A

Micro-sand particles 0.002-0.05mm

Pores are smaller than sand pores

Feels silky/soapy when wet

Reasonable drainage

Holds more moisture than sand-sufficient for plants

Hard to manage as unstable characteristics

37
Q

What is average composition of soil

A

water: 20%-30%

Air (pore spaces) 20%-30%

Organic matter: 1%-5%

Mineral matter (From parent rock) 40%-60%

38
Q

Define a Macropore

A

Large pore that holds air

39
Q

Define a mesopore

A

Medium pore thats holds available water

40
Q

Define a micropore

A

Small pore, holds unavailable water (Hygroscopic)