Definitions Flashcards

(39 cards)

1
Q

What is the definition of coarse-grained soil?

A

Coarse-grained soil consists of larger particles such as sand and gravel, with a size greater than 0.075m.

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2
Q

What is the permeability of coarse-grained soil?

A

Coarse-grained soil has high permeability, allowing water to drain easily.

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3
Q

What is sheer strength in soil mechanics?

A

Sheer strength depends on the friction between particles.

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4
Q

What is compressibility in soil mechanics?

A

Compressibility refers to how quickly soil settles under load.

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5
Q

What is the definition of fine-grained soil?

A

Fine-grained soil consists of smaller particles such as silt and clay, with a size less than 0.075m.

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6
Q

What is the permeability of fine-grained soil?

A

Fine-grained soil has low permeability, causing water to move slowly through the soil.

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7
Q

What does sheer strength depend on in fine-grained soil?

A

In fine-grained soil, sheer strength depends on cohesion and plasticity.

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8
Q

How does compressibility affect fine-grained soil?

A

Fine-grained soil compresses slowly over time.

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9
Q

Why are coarse-grained soils better for foundations?

A

Coarse-grained soils are better for foundations due to their strength and drainage properties.

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10
Q

What are the drawbacks of fine-grained soils?

A

Fine-grained soils are more cohesive but problematic in terms of drainage and settlement.

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11
Q
A
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12
Q

Gravel and sand

A

Visible and gritty

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13
Q

Silt

A

Smooth feeling. Non plastic

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14
Q

Clay

A

Sticky and plastic when moist due to extremely fine particles.

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15
Q

Soil strength

A

Proper moisture ensures good compaction and load bearing capacity; too much or too little weakens it

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16
Q

Bearing capacity

A

Moisture impacts the solid ability to support loads

17
Q

Volume changes

A

Moisture fluctuations in clayey soils cause expansion or shrinkages affecting foundations

18
Q

Permeability

A

Moisture affects soil drainage and water management

19
Q

Material durability

A

Proper moisture is needed for concrete curing.

20
Q

Frost action

A

Freezing can cause frost heaving , damages structures

21
Q

Construction delays

A

Excess moisture can slow n down work and complicate soil handling

22
Q

Attenders limits of soil

A

Used to determine the consistency and behaviour of fine grained soils at different moisture levels.they include liquid limit which is the moisture content at which soil changes from a liquid to plastic state.

23
Q

Effective stress

A

Stress carried by soil particles calculated as total stress minus pore water pressure. It determines the soils strength, stability and settlement behaviour, making it essential in geotechnical engineering

24
Q

Physical weathering

A

Breakdown of rocks into smaller pieces without changing their chemical composition

25
Causes of physical weathering
1.Freeze thaw cycles- water enters cracks and freezes and expands and breaks the rock. 2.Thermal expansion- repeated healing and cooling causes rock to crack . 3. Abrasion- wind, water or ice carry particles that grind against rock surfaces
26
Chemical weathering
The decomposition or dissolution of rocks due to chemical reactions
27
Causes of chemical weathering
1. Acid rain- accelerates chemical breakdown. 2. Oxidation- reaction with oxygen, often affecting rocks with iron. 3. Carbonation - reaction with carbonic acid especially in limestone.
28
Biological weathering
Weathering caused by living organisms
29
Causes of biological weathering
1. Plants : roots grow into and expand cracks in rocks. 2. Animal: burrowing animals disturb and expose rock to other weathering agents
30
Igneous rocks
1.Granite 2.Basalt
31
Granite
- an intrusive igneous rock formed from the slow cooling of magma beneath the earths surface
32
Basalt
And extrusive igneous rock formed from from the rapid cooling of lava at the surface
33
Not igneous
Marble ( metamorphic) Gneiss (metamorphic) Quartzite (metamorphic) Shale ( sedimentary)
34
Igneous rocks
Formed by the cooling of molten magma or lava. Granite and basalt
35
Sedimentary rocks
Formed from the accumulation and compaction of sediments over time. Sandstone and shale
36
Metamorphic rocks
When existing rocks are subjected to heat and pressure, altering their structure and composition. Marble and gneiss
37
Mining + quarrying
these activities disturb the earths crust, accelerate erosion and disturb natural geological formations.
38
Deforestation
removing vegetation increases soil erosion and sediment transport altering the natural sedimentary cycle.
39
Burning fossil fuels
This replaces large amounts of co2 , which contributes to climate change and ocean acidification affecting weathering processes