7. Soil Compaction (Das, chapter 6)

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Presentation transcript:

7. Soil Compaction (Das, chapter 6) Sections: All except 6.5, 6.6, 6.10, 6.11

What is Compaction? Compaction- Densification of soil by reducing air voids by application of mechanical energy. Compaction is used in construction of highway embankments, earth dams and many other engineering structures, loose soils must be compacted to improve their strength by increasing their unit weight The degree of compaction is measured in terms of its dry unit weight. Air Air Compaction Most soil classifications employ very simple index-type tests to obtain the characteristics of the soil needed to place it in a given group. Clearly a soil classification loses its value if the index tests become more complicated than the test to measure directly the fundamental property needed. The most commonly used characteristics are particle size and plasticity. Empirical correlations between index properties and fundamental soil behavior have many large deviations. The particle size distribution and the Atterberg limits are useful index tests inherently involves disturbance of the soil, they may not give a good indication of the behavior of the in situ, undisturbed soil. Water Water Solid Solid

Purpose of Compaction Increases shear strength of soils Increases the bearing capacity of foundations Decreases the undesirable settlement of structures Reduction in hydraulic conductivity Increasing the stability of slopes on embankments.

Role of Water in Compaction Water is added to the soil during compaction which acts as a lubricating agent on the soil particles. The soil particles slip over each other and move into a densely packed position. In soils, compaction is a function of water content Consider 0% moisture -Only compact so much Add a little water - compacts better A little more water -a little better compaction Even more water – ???

Role of Water in Compaction For a given soil, the dry unit weight increases as water is added to the soil. This continues up to certain moisture content. Beyond this moisture content, more water added will fill the void space with water so further compaction is not possible. The moisture content at which the maximum dry unit weight is attained is generally referred to as the optimum moisture content.

Another Definition of Compaction Compaction is the densification of soil that is realized by re-arrangement of soil particles with outflow of air only. It is realized by application of mechanic energy. It does not involve fluid flow, but moisture content change.

Laboratory Compaction tests Purpose: Find the maximum dry unit weight and corresponding optimum moisture content. The standard was originally developed to simulate field compaction in the laboratory There are two types of standard tests (ASTM – 698) : 1. Standard Proctor test 2. Modified Proctor test

Standard Proctor Test Layer 3 Layer 2 Layer 1 No. of blows = 25

Modified Proctor Test No. of blows = 25 Layer 5 Layer 4 Layer 3 Drop = 457.2 mm (18 in) Layer 1 Drop = 304.8 mm (12 in) No. of blows = 25 hammer = 2.5 kg (5.5 lb) hammer = 4.9 kg (10 lb)

Summary of Laboratory Compaction Tests Hammer weight Height of drop #Blows per layer # Layers Volume of Mold Standard proctor Test 2.5 kg (5.5 lb) 304.8 mm (12 in) 25 3 944 cm3 (1/30 ft3) Modified Proctor test 4.9 kg (10 lb) 457.2 mm (18 in) 5 Standard test compaction effort = 600 kN-m/m3 (12,400 lb-ft/ft3) Modified test compaction effort = 2700 kN-m/m3 (56,000 lb-ft/ft3)

Compaction Test- Procedure W1 Oven drying @ 105oC Get water content (w %) W2

Presentation of Results For each test, the moist unit weight of compacted soil is Then the dry unit weight is calculated as Repeat the previous procedure for several water content and calculate corresponding gd.

Presentation of Results Dry of optimum wet of optimum

Presentation of Results To better understand and check the compaction curve, it is helpful to plot the zero air void curve. The zero air void curve is a plot of the dry unit weight against water content at 100% degree of saturation. This variation of gdry as function of water content and degree of saturation can be calculated using: Form definition of zero air voids, S =1

Presentation of Results To plot the zero air void curves, assume values for w ( say 5%, 10%. 15%, etc) and calculate gd zav Impossible zone The actual compaction curve will be always below the zero air void curve.

Factors Effecting Compaction Compaction effort Compaction effort is the energy per unit volume As the compaction effort increases: The maximum dry unit weight of compaction increase. The optimum moisture content decreases.

Factors Effecting Compaction Compaction Effort Compaction effort is the energy per unit volume As the compaction effort increases: The maximum dry unit weight of compaction increase. The optimum moisture content decreases.

Factors Effecting Compaction Soil Type Grain-size distribution, shape of the soil grains, specific gravity of soil solids, and amount and type of clay minerals present Fine grain soil needs more water to reach optimum; while coarse grain soil needs less water to reach optimum.

Factors Effecting Compaction Soil Type Grain-size distribution, shape of the soil grains, specific gravity of soil solids, and amount and type of clay minerals present Fine grain soil needs more water to reach optimum; while coarse grain soil needs less water to reach optimum.

Factors Effecting Compaction Soil Plasticity

Factors Effecting Compaction Soil Plasticity

Example Example 6.1  Das, Chapter 6.

Field Compaction Equipment 1. Smooth wheel rollers 2. Pneumatic rubber-tired rollers Suitable for proof rolling subgrades and for finishing operation of fills with sandy and clayey soils. They are not suitable for producing high unit weights of compaction when used on thicker layers. Better than the smooth-wheel rollers. can be used for sandy and clayey soil compaction. Compaction is achieved by a combination of pressure and kneading action.

Field Compaction Equipment 3. Sheepsfoot roller most effective in compacting clayey soils. 6. Vibratory rollers

Factors affecting Field Compaction Effect of No. of roller Passes Thickness of lift

Specification of Field Compaction During construction of soil structures (dams, roads), there is usually a requirement to achieve a specified dry unit weight. In most specifications, it is required to achieve a dry density of 90 to 98% of maximum dry density obtained from standard or modified Proctor tests. This is expressed as relative compaction as follows: gd field = dry unit weight in the field gd max-lab = max. dry unit weight from laboratory test

Specification of Field Compaction gd max - lab Target area Accept 95% gd max - lab Reject w1 w2

Example 1 Find (a) the maximum dry unit weight of crushed limestone fill to be used as road base material, (b) its OMC, and (c) the moisture range for 95% of Standard Proctor.

Example 2 Find (a) The dry unit weight and water content at 95%Std. Proctor; (b) The degree of saturation at maximum dry density, and (c) plot the zero air voids line.

Example 3

Compaction Field Control Calculate Relative compaction, R If R> specification  ok If R< specification remove lift and recompact gd field

Compaction Field Control The standard procedures for determining the field unit weight of compaction include: 1. Sand cone method 2. Rubber balloon method 3. Nuclear method

Determination of Field unit weight Sand Cone Test Procedure W1 =Wt. sand cone before test 1 2 3 4

Determination of Field unit weight Sand Cone Test Procedure 5 6 7 Oven dry @ 105oC  w% W2=moist wt. of soil from hole W4 =Wt. sand cone after test Weight of sand to fill the cone and hole, W5 = W1-W4 Now you can calculate: Wc = weight of sand to fill the cone gdsand = unit weight of sand Both obtained from laboratory calibration of sand cone

Example Example 6.3  Das, Chapter 6.