Lession A - Introduction Flashcards

1
Q

What is soil mechanics?

A

is the study of the response of soils to loads. These loads comes from
human-made structures and nature (earth pressures, earthquakes, environmental conditions
and so on).

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2
Q

Minerals

A

are chemical elements that constitute rocks.

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3
Q

Rocks

A

are the aggregation of minerals into a hard mass.

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4
Q

Soils

A

are materials that are derived from the weathering of rocks.

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5
Q

What 3 groups are rocks classified under?

A
  1. Igneous rocks
  2. Sedimentary rocks
  3. Metamorphic rock
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6
Q

Igneous rocks

A
  • magma (molten rock materials) emitted from

volcanoes that have cooled and solidified (e.g. granite)

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7
Q

Sedimentary rocks

A

sediments, animals and plant materials
that have been deposited in water or on land on the earth’s
surface and then subjected to pressures (e.g. shale)

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8
Q

Metamorphic rocks

A

are formed deep within the earth’s crust
from the transformation of igneous, sedimentary, and even
existing metamorphic rocks into denser rocks (e.g. phyllite)

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9
Q

How are soils formed?

A

Physical and chemical weathering of rocks (eg. rain and snow, tectonic, volcano)

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10
Q

Alluvial soils

A
s are fine sediments
that have been eroded from
rock, transported by water, and
have settled on river and stream
beds.
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11
Q

Collovial soils (Collovium)

A
are
soils found at the base of
mountains that have been eroded
by the combination of water and
gravity.
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12
Q

Expansive soils

A

are clays that
undergo large volume changes
from cycles of wetting and
drying.

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13
Q

Glacial soils

A

are mixed soils
consisting of rock debris, sand,
silt, clays, and boulders.

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14
Q

Glacial clays

A
are soils that were
deposited in ancient lakes and
subsequently frozen.The thawing
of these lakes revealed soil
profiles of neatly stratified silt
and clay, sometimes called
varved clay.
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15
Q

Rock

A

Natural aggergate of minerals connected by strong and somewhat perminent cohesive bonds.

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16
Q

Aggergate

A

Granular mineral particles of soil used for road, sub base, backfil and concrete (eg engineerd fill)

17
Q

Agriculture soils

A

Capable of supporting life, top 30 cm to 2 m of native soils

18
Q

Engineering Soils

A

Mineral soils with more narrow + predictable soil properties

19
Q

Residual or sedentary

A

developed in place (in situ) from the underlying rock. Typically it experienced long and intense weathering. Residual parent materials can be found overlying any rock type – provided that the landscape has been stable for a sufficient period of time for weathering to occur. This situation and type of parent material are uncommon in Canada.