Soil Properties determination

Slides:



Advertisements
Similar presentations
In Place Soil Density Test Methods
Advertisements

Soil Mechanics - II Practical Portion.
Sedimentation Methods for Determining Particle Sizes
Soil Compaction.
 Soil compaction :  Compaction is the reduction in voids content due to air being forced out of the soil or dissolved in the soil water by mechanical.
ENGINEERING MATERIAL PROPERTIES (CE1303)
Contain have END SHOW. Soil is Important! Soil is the link between the rocky crust of the Earth and all life on the Earth’s surface. It is a subsystem.
Aggregate Properties HMA
CSUS Department of Chemistry
Matt Galloway. 2 Volumetric water content sensors measure volumetric water content, right?
Review of Relative Density Principles v Relative Density principles apply to compaction of relatively clean, coarse- grained soils. v Relatively clean.
SOIL MECHANICS & TESTING
SPECIFIC GRAVITY & ABSORPTION CAPACITY OF AGGREGATES
Dr. Sophia Hassiotis.  Laboratory set up  Personal Protective equipment  Directions for mixing  Slump test  Cylinder casting  Cleaning up your station.
Specific Gravity of Soils
Consolidation Theory Examples.
ENCI 5791 Compaction In-situ soils used as: –Bases for the construction of highway pavements –embankments or leveling material for construction projects.
Experiment (2) Specific gravity determination
Soil Water ContentSoil Moisture Content Water that may be evaporated from soil by heating at C to a constant weight Gravimetric moisture content.
Field Density (Sand Cone Method) ASTM D 1556/02
The steps how to calculate mass, volume, and density
COMPACTION Topic COMPACTION Presented to Dr. Ayub Elahi Presented by Group leader. M.Zeeshan haider yousaf Zia. # 14 Haider ayub # 13 Bilal ansari #35.
7. Soil Compaction (Das, chapter 6)
Water in Soil. The basis of irrigation Soil Plant Evapotranspiration Plant requirements.
CHAPTER TWO SOIL COMPRESSION.
Density A physical property of matter I can apply an equation to determine the density of a substance based on its mass and volume Apply the relationship.
Scientific Measurements: The Metric System Credit to A. Rubel.
4. Phase Relations (Das, Chapter 3) Sections: All except 3.6
Lecture 7 b Soil Water – Part 2
Prepared by: Marcia C. Belcher Construction Engineering Technology.
1 Specific Gravity. 2 Specific Gravity Gs 3 Phase Material.
AGGREGATES.
UNIT: CONCRETE/MASONARY
Sedimentation & filtration
On page 10 of your notebook, predict how the layers will form. Which one will go at the bottom? Which one will go on top?
Properties of Matter Mass Volume Density.
GEO-MECHANICS (CE2204) Engineering Properties of Soils
Chapter 1 – Section 2 p Measuring Matter. I. Weight – a measure of the force of gravity A. Changes if you go to the moon or another planet since.
Examination Procedures Goods Sold by Volume
Soil Structure, Density, and Porosity
Asphalt Concrete Mix Design
Density A booklet to learn from.
Civil Engineering Department College of Engineering Course: Soil and Rock Mechanics (CE 260) Lecturer: Dr. Frederick Owusu-Nimo.
METRIC SYSTEM. What is the metric system? What is the metric system? A system used to measure length, mass volume and temperature all over the world.
Free Powerpoint TemplatesPage 1Powerpoint Templates Page 1 Powerpoint Templates Page 1 INDEX PROPERTIES, RELATIONSHIPS AND TEST.
Civil Engineering Department College of Engineering Course: Soil and Rock Mechanics (CE 260) Lecturer: Dr. Frederick Owusu-Nimo.
Copyright February 22, Index Properties of Soils Prof. Basuony El-Garhy Geotechnical Engineering and Foundations Civil Engineering Department Faculty.
Aggregate Properties HMA
2016/6/181 ISO 6540 ISO 6540 (first edition 1980) International Standard Maize – Determination of moisture content (on milled grains and on whole grains.
Lecture 7 b Soil Water – Part 2 Source: Dept of Agriculture Bulletin 462, 1960.
UNIT: CONCRETE/MASONARY Concrete Proportions Modified by Georgia Agricultural Education Curriculum Office July, 2002.
GROUND IMPROVEMENT PRINCIPLES OF COMPACTION. A good foundation has a safe and economic design with the following properties: 1.Have adequate shearing.
DETERMINATION OF FIELD DENSITY BY CORE CUTTER METHOD
INDEX PROPERTIES, RELATIONSHIPS AND TEST
SOIL COMPACTION GEOLOGY AND APPLIDE GEOLOGY -:Prepared By:- GEC,GODHRA
SARDAR VALLABHBHAI PATEL INSTITUTE OF TECHNOLOGY
Water content DEFINITION:
GOVERNMENT ENGINEERING COLLEGE
INDEX PROPERTIES, RELATIONSHIPS AND TEST
Compaction According ASTM D 1557/02
FIELD COMPACTION CONTROL
SEM 3 CIVIL.
California Bearing Ratio Test
Laboratory glassware Dr. Ebtihaj Jambi.
Geotechnics 1 (BFC 21702) SOIL COMPACTION.
Permeability By Falling Head Method
Team Croatia Reporter: Luka Mikšić
WORKABILITY OF CONCRETE
Maximum Size of Aggregate
Light Compaction Equipment
Presentation transcript:

Soil Properties determination Prepared by : Akshay Kacha-130040106024

7.6 Water Content Oven-drying method IT = 7.6 Water Content Oven-drying method Usual standard laboratory method in which the soil is dried in an oven at 105ºC to 110ºC. Most accurate method. The temperature range of 105 to 110ºC Drying up to 24 hours or more depending upon the amount and type of soil. The water content is always reported on the basis of the dry weight of the soil sample.

7.6 Water Content b) Sand Bath method IT = 7.6 Water Content b) Sand Bath method Field method requiring only about one hour’s drying period. A sand bath (a basin containing about 50mm thick sand layer) is heated over a gas burner or stove. Wet soil sample kept in a container, is placed on the sand bath and heated until dry. The sand is stirred with a palette knife (or a rod) during heating to assist drying.

7.6 Water Content c) Other methods IT = 7.6 Water Content c) Other methods Infrared lamp and torsion balance method, calcium carbide method and nuclear method can be used for rapid determination of water content.

7.6 Water Content c) Other methods IT = 7.6 Water Content c) Other methods Infrared lamp and torsion balance method, calcium carbide method and nuclear method can be used for rapid determination of water content.

IT = 7.7 Specific Gravity Knowledge of the specific gravity of soils is required for the determination of voids ratio, degree of saturation, and in the sedimentation and consolidation tests. The individual mineral particles constituting a soil have different specific gravities. The specific gravity can be determined either by the use of a 50 - 100ml density bottle, a 500ml flask or a pycnometer. Density bottle method is the usual laboratory method.

7.7 Specific Gravity – cont’d Phase diagram for determination of Specific Gravity

7.7 Specific Gravity – cont’d Mass of soil solids = M2 – M1 Mass of water in (iii) = M3 – M2 Mass of water in (iv) = M4 – M1

7.7 Specific Gravity – cont’d  Hence mass of water equivalent in volume of that of soil solids = Mass of water in (iv) minus Mass of water in (iii) = (M4 – M1) – (M3 – M2)

7.7 Specific Gravity – cont’d

7.7 Determination of Field Density Core Cutter method A core cutter is a steel cylinder open at both ends with one end sharpened to form the cutting edge. The usual dimensions are 10cm internal diameter and height about 12 to 15 cm.

7.7 Determination of Field Density Core Cutter method The internal diameter, height and mass of core-cutter are noted. The place where the field density is to be determined is cleared of shrubs, if any, levelled and the core-cutter is placed vertically on the ground surface.

7.7 Determination of Field Density Core Cutter method A steel ring about 2.5cm height (Steel Dolly) is placed on top of the core cutter and is gently driven into the ground by blows of a rammer, until the top of the steel ring is nearly flush with the ground surface. Sufficient soil is excavated from around the core-cutter to enable a person to put his hands and lift the core-cutter with soil inside off the ground.

7.7 Determination of Field Density Core Cutter method The core cutter with soil inside is brought to the laboratory, the ends are trimmed, levelled and weighed. The soil is removed from the core-cutter and the samples are taken from top, middle and bottom positions for water content determination. The average of the three determinations gives the in-situ water content.

7.7 Determination of Field Density b) Sand replacement method Small pouring cylinder: suitable for fine and medium grained soils. Metal tray to excavate the hole with suitable shape and size. Calibration container of the small pouring cylinder (size 100 x 150mm). Large pouring cylinder: suitable for fine, medium and coarse grained soils. Calibration container

7.7 Determination of Field Density b) Sand replacement method Medium pouring cylinder: suitable for medium and coarse grained soils. Tools for levelling and excavating. Containers. Sand. Balance

7.7 Determination of Field Density b) Sand replacement method

7.7 Determination of Field Density b) Sand replacement method The unit’s base plate is laid on the compacted surface and material is excavated through the hole in the plate to a depth of about 150 mm. This wet material is weighed, dried in an oven and weighed again to determine the moisture content.

7.7 Determination of Field Density b) Sand replacement method The volume of the hole is measured by filling it with dry, free-flowing sand from a special sand-cone cylinder. Since the density of the sand is known, the volume of the hole is calculated. The density (wet unit weight) of the compacted sample is found by dividing the weight of the material by the volume of the hole.

7.7 Determination of Field Density b) Sand replacement method Dry unit weight is found by using the formulae;

7.7 Determination of Field Density b) Sand replacement method