Geotechnical Engineering Quiz

Geotechnical Engineering Quiz

University

26 Qs

quiz-placeholder

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Geotechnical Engineering Quiz

Geotechnical Engineering Quiz

Assessment

Quiz

Engineering

University

Easy

Created by

Lesyeux .

Used 2+ times

FREE Resource

26 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

According to the Unified Soil Classification System, silt and clay are categorized as:

Particles smaller than 0.002 mm

Particles smaller than 0.075 mm

Particles smaller than 2 mm

Particles smaller than 4.75 mm

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Who developed the first ultimate bearing-capacity theory for shallow foundations?

Karl Terzaghi

Jean Victor Poncelet

William Rankine

Wolmar Fellenius

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

The conference that marked the formal establishment of soil mechanics as a field was held at:

Harvard University in 1936

Zurich University in 1953

Paris in 1961

Stockholm in 1981

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

In a three-phase soil system, which of the following is not a valid assumption?

The weight of air is negligible

The total weight is the sum of solid and water weights

The total volume is always equal to the sum of the solid, water, and air volumes

The volume of solids is always greater than the volume of voids

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which soil classification system is almost universally accepted today?

Massachusetts Institute of Technology

United States Department of Agriculture

Unified Soil Classification System

Rankine soil grading system

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

According to the Unified Soil Classification System, silt and clay are categorized as:

Particles smaller than 0.002 mm

Particles smaller than 0.075 mm

Particles smaller than 2 mm

Particles smaller than 4.75 mm

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

The primary characteristic that distinguishes residual soil from transported soil is:

The presence of organic matter

Its formation is at the same location as the parent rock

The lack of mineralogical composition changes

Its high-water retention capacity

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