geotech Flashcards

(48 cards)

1
Q

It is an in-depth study of soil
and rock properties and behavior to ensure the
safety and stability of structures.

A

Geotechnical engineering

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2
Q

the
publication of key theories on soil mechanics and
the movement of water through soil by scientists
such as

A

Coulumb, Darcy and Atterberg

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3
Q

The publication of “Theoretical Soil
Mechanics” by the prominent civil engineer

A

Karl Anton von Terzaghi 1925

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4
Q

during 1773 was credited as the first
person to use mechanics to solve soil problems

A

Coulumb

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5
Q

was recognized as
the undisputed father of soil mechanics

A

Karl Anton von Terzaghi

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6
Q

Leaning Tower of Pisa or

A

Torre Pendenti di
Pisa

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7
Q

It is located at Pisa, Italy and designed by

A

Architect Bonanno Pisano last 1173 and
completed 1372

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8
Q

The height of the tower is
meters from the ground on the low side

A

55.86

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9
Q

meters on the high side.

A

56.67

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10
Q

By 1990 the tilt reached

A

5.5
degrees

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11
Q

the structure was stabilized by
remedial work between 1993 and 2001 which
reduced the tilt to

A

3.97 degrees.

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12
Q

Two Towers or

A

Le due Torri

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13
Q

The two towers are the most prominent
Towers of

A

Bologna

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14
Q

The smaller one is called the

A

Garisenda Tower

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15
Q

while the taller one is called

A

Asinelli Tower.

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16
Q

The names of the towers were
derived from the families which are traditionally
credited and constructed the towers between

A

1109
and 1119

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17
Q

is the study of the response of
soils to loads and these loads may come from
human-made structures (buildings), gravity
(earthpressures) and natural phenomena
(earthquake).

A

Soil mechanics

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18
Q

s defined an uncemented aggregate of
mineral grains and decayed organic matter (solid
particles) with liquid and gas in the empty spaces
between the solid particles, and it supports
structural foundations.

A

Soil

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19
Q

is the branch of science that deals
with the study of the physical properties of soil
and the behavior of soil masses subjected to
various types of forces.

A

Soil Mechanics

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20
Q

is the application of the
principles of soil mechanics to practical
problems.

A

Soils Engineering

21
Q

is defined as sub
discipline of civil engineering that involves
natural materials found close to the surface of the
earth. It includes the application of the principles
of soil mechanics and rock mechanics to the
design of foundations, retaining structures and
earth structures.

A

Geotechnical Engineering

22
Q

s the branch of
engineering which deals with design,
construction and maintenance of shallow footings
and deep foundations and other structural
members which comprise foundation of buildings
and other engineering structures. It also includes
investigation of sites for foundation purpose

A

Foundation Engineering

23
Q

is known as the “Father
of Soil Mechanics.”

A

Karl Anton von Terzaghi

24
Q

s defined as a natural aggregate of mineral
grains, loose or moderately cohesive, inorganic in
nature, that have the capacity of being separated
by means of simple mechanical process, e.g. by
agitation in water.

25
is defined as hard and compact natural aggregates of mineral grains cemented by strong and more or less permanent bonds.
Rock
26
involves reduction of size without any change in the original composition of the parent rock. The main agents responsible for this process are exfoliation, unloading, erosion, freezing, and thawing.
Physical weathering
27
causes both reduction in size and chemical alteration of the original parent rock. The main agents responsible for chemical weathering are hydration, carbonation, and oxidation.
Chemical weathering
28
The sands
coarse particles
29
silts and clays
fine particles
30
disintegration of rock may stay at the place of their formation.
residual soils.
31
If these soils are carried away by forces of gravity, water, wind and ice deposited at another location, they are known as
transported soils.
32
are formed by solidification of molten magma ejected from deep within the earth’s mantle.
Igneous rocks
33
are deposits of gravel, sand, silt and clay formed by weathering may become compacted by overburden pressure and cemented by agents like iron oxide, calcite, dolomite and quartz.
Sedimentary rocks
34
are either igneous or sedimentary rocks that have undergone considerable in their constitution, in their shape, structure and sometimes even in their mineral composition.
Metamorphic rocks
35
is the process of breaking down rocks by mechanical and chemical processes into smaller pieces.
Weathering
36
may be caused by the expansion and contraction of rocks from the continuous gain and loss of heat, which results in ultimate disintegration.
Mechanical weathering
37
the original rock minerals are transformed into new minerals by chemical reaction.
Chemical weathering
38
formed by transportation and deposition of glaciers.
Glacial soils
39
transported by running water and deposited along streams.
Alluvial soils or Fluvial soils
40
formed by deposition in quiet lakes.
Lacustrine soils
41
formed by deposition in the seas.
Marine soils
42
transported and deposited by wind.
Aeolian soils
43
formed by movement of soil from its original place by gravity, such as during landslides.
Colluvial soils
44
is the process of changing the composition and texture of rocks, without melting by heat and pressure; and chemical fluids.
Metamorphism
45
if its individual particle is visible to unaided eyes.
coarse grained
46
if its individual particle is not visible to unaided eyes.
fine grained
47
are those which contain an amount of decayed animals and/or plant matter.
Organic soils
48