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LE 4

LE 4
60問 • 2年前
  • Mharvie Nagal
  • 通報

    問題一覧

  • 1

    are the primary source of information for various aspects of land-use planning, including the siting of buildings and transportation systems.

    Geologic Maps

  • 2

    represent the distribution of different types of rock and surficial deposits, as well as locations of geologic structures such as faults and folds.

    Geologic Maps

  • 3

    MAJOR TYPES OF GEOLOGICAL MAPS

    Topographical, Cross Sectional, Structural

  • 4

    map where locations of equal elevation are connected by lines called contour lines. It represents the three-dimensional lay of the terrain, but on a two-dimensional surface.

    Topographical Map

  • 5

    a map that shows the cross-section from the side.

    Cross Sectional Map

  • 6

    a map that shows the geologic features of an area, including features such as the type of rocks and geologic structures which includes folds, faults and joints.

    Structural Map

  • 7

    is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements.

    Fault

  • 8

    Types of Fault

    Reverse, Normal, Strike-Slip

  • 9

    stack of originally planar surfaces, such as sedimentary strata, that are bent or curved during permanent deformation.

    Folds

  • 10

    Types of Folds

    Anticlines, Synclines, Monoclines

  • 11

    a break of natural origin in a layer or body of rock that lacks visible or measurable movement parallel to the surface of the fracture. It can occur singly; they most frequently appear as joint sets and systems.

    Joints

  • 12

    Types of joints

    Nonsystematic, Systematic, Columnar

  • 13

    is an aggregate of mineral properties. To determine the rock’s performance under specific conditions, geologists must look and test its:

    Rock Materials

  • 14

    2 properties of rock Material

    Physical, Mechanical

  • 15

    MAY BE KNOWN AS INDEX PROPERTIES, WHICH DESCRIBE THE ROCK MATERIAL AND HELPS IN CLASSIFYING THEM.

    Physical Properties

  • 16

    THIS IS THE INTRINSIC PROPERTY CONTROLLING THE STRENGTH OF THE ROCK. ALTHOUGH THERE EXIST MORE THAN 2000 KINDS OF KNOWN MINERALS, ONLY ABOUT NINE OF THEM PARTAKE DECISIVELY IN FORMING THE COMPOSITION OF ROCKS. THESE INCLUDES (1) QUARTZ, (2) FELDSPAR, (3) MICA, (4) AMPHIBOLE, (5) PYROXENE,(6) OLIVINE, (7) CALCITE, (8) KAOLIN AND, (9) DOLOMITE

    Mineralogic Composition, Structure, And Texture

  • 17

    RATIO OF THE DENSITY OF SOLIDS TO THE DENSITY OF WATER. BASED ON ITS VALUE, THE OBJECT COULD EITHER FLOAT OR SINK IN THE REFERENCE SUBSTANCE

    Specific Gravity

  • 18

    DESCRIBES AND RELATES SIZE (VOLUME), AMOUNT (MASS), CONCENTRATION (DENSITY), AND FORCE (WEIGHT), AS WELL AS SPECIFIC GRAVITY

    Unit Weight

  • 19

    The __________ of an object in a given volume is a measure of how compact or heavy it is.

    Density

  • 20

    are open spaces in the ground that are commonly encountered as unforeseen ground conditions in engineering geology.

    Voids

  • 21

    is the ratio of the volume of voids to the volume of solids, and is closely related with porosity.

    Void Ratio

  • 22

    The _________ of a material tells how densely it is packed. It is the proportion of non-solid material volume to total material volume. It decreases with increasing age of the rock nad the depth of the rock.

    Porosity

  • 23

    it simply how much water is in a product

    Moisture Content

  • 24

    it influences the physical properties of a substance including weight, density, viscosity, conductivity and others.

    Moisture Content

  • 25

    the weight of water in the void divided by the weight of dry solids in the rock sample.

    Ratio Of Moisture Content

  • 26

    denotes the actual relationship between the weight of moisture existing in a space and the weight that would exist if the space were saturated

    Degree Of Saturation

  • 27

    it can be calculated by dividing the total volume of voids in the rock sample by the volume of water in the void .

    Degree Of Saturation

  • 28

    The rock mass having a higher porosity has...

    Higher Degree Of Saturation

  • 29

    this refers to a porous materials ability to let liquid pass through its pores.

    Permeability

  • 30

    all related properties of any rock or loose sediment , but related to the number, size, and connections of openings in the rock .

    Porosity And Permeability

  • 31

    the majority of rocks are dielectric , and measurements of dielectric constants are used to interpret data.

    Electrical Properties

  • 32

    the increase in temperature also makes rock weaker due to the formation of cracks in the rock mass

    Thermal Properties

  • 33

    the volume of mass increases as a result of water suction or prolonged contact with water.

    Swelling

  • 34

    is more common in weaker rocks.

    Swelling

  • 35

    due to the sequence of rock formation , the properties of the elements of the rock mass are not identical in all directions

    Anisotropy

  • 36

    has a weakness in one direction only.

    Anisotropic Material

  • 37

    is the resistance to destruction.

    Durability

  • 38

    if rock is more ________, it means it will last for a longer period when put into use.

    Durable

  • 39

    It depends upon the nature of environment against which the rock is going to be used.

    Durability

  • 40

    is used to describe nature of weathering.

    Swelling Index

  • 41

    methods in testing the rock strength

    Direct, Indirect

  • 42

    for calculating the above strength values in the lab.

    Direct Methods

  • 43

    For determining the above strength value approximately in the lab or at the field site.

    Indirect Methods

  • 44

    the test are carried out on intact rock specimens in the laboratory or on rock mass in the field to determine the strength values.

    Mechanical Properties

  • 45

    is an important parameter to describe the stress and strain relationship.

    Young Modulus

  • 46

    describes the capacity of rock deformation or stiffness of a rock.

    Young Modulus

  • 47

    For a high elastic modulus rock, it is...

    Less Deformable

  • 48

    For a low elastic modulus (soft) rock, it is...

    More Deformable

  • 49

    applying compressive load until failure occurs in the core by a fracture in the middle using high-capacity compressive testing machinery verifies the _______________ of rock and material and deformation behavior under loading.

    Uniaxial Compressive Strength

  • 50

    is the strength exhibited by a rock specimen when it is subjected to confining pressure in addition to vertical pressure.

    Triaxial Compressive Strength

  • 51

    can also be used to determine the shear strength parameters of rock materials using this test

    Mohr's Envelope

  • 52

    Example of direct methods

    Uniaxial Compression Test, Triaxial Compression Test

  • 53

    Example of indirect Methods

    Point Load Test, Rebound Hammer Test

  • 54

    is an index test that classifies rocks based on their weight.

    Point Load Test

  • 55

    it is commonly used to determine the hardness of a rock sample's surface because it is simple to use and handle.

    Rebound Hammer Test

  • 56

    is defined as the maximum _______ which a material is capable of developing.

    Tensile Strength

  • 57

    _____ are weak in tension.

    Rocks

  • 58

    the maximum resistance to deformation caused by a shear stress.

    Shear Strength

  • 59

    it primarily concerns the shear strength and shear behavior of the rock's shearing and weakness planes, which hold a rock specimen together.

    Shear Strength Test

  • 60

    Common modes of failure in rock sample under compression

    Simple Extension, Multiple Extension, Multiple Fracturing, Multiple Shear, Simple Shear

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    問題一覧

  • 1

    are the primary source of information for various aspects of land-use planning, including the siting of buildings and transportation systems.

    Geologic Maps

  • 2

    represent the distribution of different types of rock and surficial deposits, as well as locations of geologic structures such as faults and folds.

    Geologic Maps

  • 3

    MAJOR TYPES OF GEOLOGICAL MAPS

    Topographical, Cross Sectional, Structural

  • 4

    map where locations of equal elevation are connected by lines called contour lines. It represents the three-dimensional lay of the terrain, but on a two-dimensional surface.

    Topographical Map

  • 5

    a map that shows the cross-section from the side.

    Cross Sectional Map

  • 6

    a map that shows the geologic features of an area, including features such as the type of rocks and geologic structures which includes folds, faults and joints.

    Structural Map

  • 7

    is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements.

    Fault

  • 8

    Types of Fault

    Reverse, Normal, Strike-Slip

  • 9

    stack of originally planar surfaces, such as sedimentary strata, that are bent or curved during permanent deformation.

    Folds

  • 10

    Types of Folds

    Anticlines, Synclines, Monoclines

  • 11

    a break of natural origin in a layer or body of rock that lacks visible or measurable movement parallel to the surface of the fracture. It can occur singly; they most frequently appear as joint sets and systems.

    Joints

  • 12

    Types of joints

    Nonsystematic, Systematic, Columnar

  • 13

    is an aggregate of mineral properties. To determine the rock’s performance under specific conditions, geologists must look and test its:

    Rock Materials

  • 14

    2 properties of rock Material

    Physical, Mechanical

  • 15

    MAY BE KNOWN AS INDEX PROPERTIES, WHICH DESCRIBE THE ROCK MATERIAL AND HELPS IN CLASSIFYING THEM.

    Physical Properties

  • 16

    THIS IS THE INTRINSIC PROPERTY CONTROLLING THE STRENGTH OF THE ROCK. ALTHOUGH THERE EXIST MORE THAN 2000 KINDS OF KNOWN MINERALS, ONLY ABOUT NINE OF THEM PARTAKE DECISIVELY IN FORMING THE COMPOSITION OF ROCKS. THESE INCLUDES (1) QUARTZ, (2) FELDSPAR, (3) MICA, (4) AMPHIBOLE, (5) PYROXENE,(6) OLIVINE, (7) CALCITE, (8) KAOLIN AND, (9) DOLOMITE

    Mineralogic Composition, Structure, And Texture

  • 17

    RATIO OF THE DENSITY OF SOLIDS TO THE DENSITY OF WATER. BASED ON ITS VALUE, THE OBJECT COULD EITHER FLOAT OR SINK IN THE REFERENCE SUBSTANCE

    Specific Gravity

  • 18

    DESCRIBES AND RELATES SIZE (VOLUME), AMOUNT (MASS), CONCENTRATION (DENSITY), AND FORCE (WEIGHT), AS WELL AS SPECIFIC GRAVITY

    Unit Weight

  • 19

    The __________ of an object in a given volume is a measure of how compact or heavy it is.

    Density

  • 20

    are open spaces in the ground that are commonly encountered as unforeseen ground conditions in engineering geology.

    Voids

  • 21

    is the ratio of the volume of voids to the volume of solids, and is closely related with porosity.

    Void Ratio

  • 22

    The _________ of a material tells how densely it is packed. It is the proportion of non-solid material volume to total material volume. It decreases with increasing age of the rock nad the depth of the rock.

    Porosity

  • 23

    it simply how much water is in a product

    Moisture Content

  • 24

    it influences the physical properties of a substance including weight, density, viscosity, conductivity and others.

    Moisture Content

  • 25

    the weight of water in the void divided by the weight of dry solids in the rock sample.

    Ratio Of Moisture Content

  • 26

    denotes the actual relationship between the weight of moisture existing in a space and the weight that would exist if the space were saturated

    Degree Of Saturation

  • 27

    it can be calculated by dividing the total volume of voids in the rock sample by the volume of water in the void .

    Degree Of Saturation

  • 28

    The rock mass having a higher porosity has...

    Higher Degree Of Saturation

  • 29

    this refers to a porous materials ability to let liquid pass through its pores.

    Permeability

  • 30

    all related properties of any rock or loose sediment , but related to the number, size, and connections of openings in the rock .

    Porosity And Permeability

  • 31

    the majority of rocks are dielectric , and measurements of dielectric constants are used to interpret data.

    Electrical Properties

  • 32

    the increase in temperature also makes rock weaker due to the formation of cracks in the rock mass

    Thermal Properties

  • 33

    the volume of mass increases as a result of water suction or prolonged contact with water.

    Swelling

  • 34

    is more common in weaker rocks.

    Swelling

  • 35

    due to the sequence of rock formation , the properties of the elements of the rock mass are not identical in all directions

    Anisotropy

  • 36

    has a weakness in one direction only.

    Anisotropic Material

  • 37

    is the resistance to destruction.

    Durability

  • 38

    if rock is more ________, it means it will last for a longer period when put into use.

    Durable

  • 39

    It depends upon the nature of environment against which the rock is going to be used.

    Durability

  • 40

    is used to describe nature of weathering.

    Swelling Index

  • 41

    methods in testing the rock strength

    Direct, Indirect

  • 42

    for calculating the above strength values in the lab.

    Direct Methods

  • 43

    For determining the above strength value approximately in the lab or at the field site.

    Indirect Methods

  • 44

    the test are carried out on intact rock specimens in the laboratory or on rock mass in the field to determine the strength values.

    Mechanical Properties

  • 45

    is an important parameter to describe the stress and strain relationship.

    Young Modulus

  • 46

    describes the capacity of rock deformation or stiffness of a rock.

    Young Modulus

  • 47

    For a high elastic modulus rock, it is...

    Less Deformable

  • 48

    For a low elastic modulus (soft) rock, it is...

    More Deformable

  • 49

    applying compressive load until failure occurs in the core by a fracture in the middle using high-capacity compressive testing machinery verifies the _______________ of rock and material and deformation behavior under loading.

    Uniaxial Compressive Strength

  • 50

    is the strength exhibited by a rock specimen when it is subjected to confining pressure in addition to vertical pressure.

    Triaxial Compressive Strength

  • 51

    can also be used to determine the shear strength parameters of rock materials using this test

    Mohr's Envelope

  • 52

    Example of direct methods

    Uniaxial Compression Test, Triaxial Compression Test

  • 53

    Example of indirect Methods

    Point Load Test, Rebound Hammer Test

  • 54

    is an index test that classifies rocks based on their weight.

    Point Load Test

  • 55

    it is commonly used to determine the hardness of a rock sample's surface because it is simple to use and handle.

    Rebound Hammer Test

  • 56

    is defined as the maximum _______ which a material is capable of developing.

    Tensile Strength

  • 57

    _____ are weak in tension.

    Rocks

  • 58

    the maximum resistance to deformation caused by a shear stress.

    Shear Strength

  • 59

    it primarily concerns the shear strength and shear behavior of the rock's shearing and weakness planes, which hold a rock specimen together.

    Shear Strength Test

  • 60

    Common modes of failure in rock sample under compression

    Simple Extension, Multiple Extension, Multiple Fracturing, Multiple Shear, Simple Shear