Unit 2 Flashcards
Types of Construction Aggregates
Soil Aggregates
Concrete Aggregates
Composite Aggregates
Almost all of natural aggregate materials originate from ______. There are three kinds of rocks namely igneous, sedimentary and metamorphic. These classifications are based on the mode of formation of rocks.
bed rocks
________ and_________ processes work together to create soil aggregates.
Cohesion, fragmentation
Generally ______ is an unconsolidated, or loose, combination of ____________________. The organic materials are composed of debris from plants & from the decomposition of many tiny life forms that inhabit or live in the soil, while the inorganic components of soil are: rocks & minerals, that have been gradually broken down by weather, chemical action and other natural processes.
soil, organic & inorganic materials
are considered a three-phase material composed of rocks or mineral particles, water and air. The voids of a soil, the spaces in between mineral particles, contain the water and air.
soil
Engineering properties of soil includes; shear strength, stiffness and permeability. These properties are being considered in order to determine and design the type of foundations, earthworks, and/or pavements subgrade required for the intended man-made structures to be built.
Fact
Foundations built for above-ground structures include shallow and deep foundation. Retaining structures include earth-filled dams and retaining walls. Earthworks include embankments, tunnels, dikes, reservoirs, and sanitary landfills.
Fact
Classification of Soil according to Size
Granular Soil
Fine Grained Soil
Organic Soil
particles passing 75 mm
and retained on (Sieve #10) 2.0 mm sieves, mostly found in rivers
Gravel
– passing 75 mm (3”) and retained on 0.075 mm (#200) sieves
Granular or coarse-grained
- passing 2.0 mm and retained on 0.075 mm sieves
~ Coarse sand – (+) 2.0 mm (-) 0.425 mm (#40)
~ Fine sand - (+) 0.425 mm (-) 0.075 mm(#200)
Sand
Good load bearing qualities.
Permeable, hence they drain easily.
Comparatively incompressible when subjected to static loads.
Not subject to changes in strength or volume due to variation in water content. However, loose granular materials will undergo considerable reduction in volume if subjected to vibratory loads.
Properties of granular soil
– passing 0.075 mm and larger than 0.002mm
(fine and barely visible grains)
Silt
– soil with particle size less than 0.002mm
(cohesive or plastic)
Clay
passing 0.001mm
(gray to black color)
Organic Soil
inferior than fine grained soils with respect to the properties. fibrous soil due to the presence of undecomposed plant matter. unhealthy sewage-sludge odor.
found as deposits in swamps and peat bogs.
Organic Soil
Presence of organic matter will adversely affect the engineering properties of either granular or fine-grained soil, if the amount is appreciable.
Fact
Soil containing quantities of organic material such as grass, roots and sewage.
Highly organic soil such as peat and muck.
Soil with liquid limit exceeding 80 and/or plasticity index exceeding 55. Soil with a natural water content exceeding 100 %.
Soil with very low natural density, 800 kg./m3 or lower.
Soil that can not be properly compacted as determined by the Engineer.
Unsuitable Soil Material
- determine the particle size distribution of soil and it is used to classify/identify the soil
Sieve/Grading test Hydrometer test
Or a combined analysis
(AASHTO T 88)
(ASTM D 422)
the lowest moisture content at which the soil will flow upon the application of a very small shearing force. It gives a certain measure of the shearing resistance of a soil when mixed with water.
Liquid limit
LIQUID LIMIT / PLASTIC LIMIT TESTS
(AASHTO T-89/T-90) (ASTM D 4318)
the minimum moisture content at which the soil can be readily molded without breaking or crumbling
Plastic Limit
LIQUID LIMIT / PLASTIC LIMIT TESTS
(AASHTO T-89/T-90) (ASTM D 4318)
MOISTURE DENSITY RELATION or COMPACTION TEST OF SOIL
(AASHTO T-99/T-180)
(ASTM D 698/D 1557)
- a process of increasing soil density and removing air, usually by mechanical means
Soil Compaction
By reducing the air voids, more soil can be added to the block.
T
When moisture is added to the block, water content is increasing
T
The soil particles will slip more on each other causing more reduction in the total volume, which will result in adding more soil and hence the dry density will increase, accordingly.
Spitting Fact
– involves the granular rearrangement of soil particles at a number of moisture contents ranging from slightly dry to very wet, by a specified amount of energy applied on a specified manner.
Compaction Test
Compaction Test
(Purpose) to determine:
Amount of mixing water(Optimum Moisture Content (OMC)
Maximum Dry Density (MDD)
jojowain
Moisture content of the soil is vital to proper compaction
TRUE
__________ acts as lubricant within soil, sliding the particles together.
Moisture
Too little moisture means inadequate compaction- the particles cannot move past each other to achieve density.
T
The highest density for most soils is at certain water content for a given compaction effort. The drier the soil, the more resistant it is to compaction.
T
In a water- saturated state the voids between particles are partially filled with water, creating an apparent cohesion that binds them together. This cohesion increases as the particle size decreases (as in clay type soils).
T
-is a method of evaluating the relative quality of subgrade, subbase, and base soil for pavements.
CALIFORNIA BEARING RATIO (CBR)
(AASHTO T-193)
CBR Requirements of Soil Aggregates:
Item- 201/202/300
80% minimum
Item 200
30% minimum
This test evaluates the structural strength of coarse aggregate. It gives an indication of quality as determined by resistance to impact and wear.
ABRASION TEST (AASHTO T-96) (ASTM C 131)
The abrasive charge- consist of cast-iron spheres or steel spheres approximately 46.8 mm in diameter & each weighing between 390-455 grams
T