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Chapter 1: Introduction
Infiltration:
Water penetrates the porous ground surface
Contaminants & particulates removed by filtration through the soil
Dissolved constituents removed through adsorption
Decrease in rate when the area of impervious surface increase
Chapter 1: Introduction
Hydrologic cycle:
Exchange of water between the earth and the atmosphere
Produces rainwater to meet the demand
Chapter 1: Introduction
Unsaturated soils:
Contain air and fluid phases in pores
Volume & strength change behaviour upon wetting and drying (Expansive soils & collapsible soils)
Slope failure is closely related to heavy rainfall and infiltration
Chapter 1: Introduction
Water
Unsaturated soil
Infiltration
Increase in matric suction
Decrease in shear strength
Increase in soil moisture content
Chapter 1: Introduction
Problem statement:
1. Slope Stability and Slope Failure
Intense rainfall generates positive pore pressure. Shear strength of the soil decrease.
Increase of moisture content above the phreaticsurface, reduce the suction in slope.
As water infiltrates further, position of phreaticsurface will rise
Chapter 1: Introduction
Problem statement:
2. Pollution of Groundwater Sources
Recharged by the runoff infiltration
Urbanisation reduce permeable surface
Urbanisation pollutes water sources
Infiltration of chemicals into the soil
Chapter 1: Introduction
Objectives:
Provide experimental evidence for soil water infiltration.
Comparing the unsaturated soil properties before and after the rainfall infiltration.
Chapter 1: Introduction
Scope of study:
Emphasize on rainwater infiltration into unsaturated soil column.
Analysis of data to explain the behaviour of unsaturated soil.
Usage of apparatus and software to obtain data.
Chapter 2: Literature Review
Rainwater Infiltration
Larger pore size, greater infiltration rate.
Greater infiltration rate, better soil water adsorption capacity.
Percolation- Downward flow of water in the unsaturated zone of the soil.
Variation between permeability of finer and coarser soil >> Effect of rainfall condition to the infiltration
Chapter 2: Literature Review
Soil Column:
Used in the hydrogeological properties study.
Evaluate transport models.
Monitor the outcome and mobility of contaminant.
Evapotranspiration study.
Chapter 2: Literature Review
Soil Moisture:
Held in pores in liquid and vapour phase.
Important in agriculture:
Proper water resource management
Irrigation scheduling
Crop production
Chemical monitoring
Chapter 3: Methodology
2 sets of soil sample were tested.
i. Gravelly sand
ii. UKM’s forest soil sample
Parameters taken into consideration:
i. Soil moisture content
ii. Soil matric suction
iii. Soil water retention ability
iv. Soil porosity
Chapter 3: Methodology
Soil Column
Soil moisture content:
Measured by time-domain reflectometry (TDR) probe
Inserted at multiple points
Record the real time moisture content during infiltration
Chapter 3: Methodology
Soil Column
Soil matric suction:
Suction exerted that induces water flow in unsaturated soil
Measured by tensiometer probe
When soil is getting saturated, soil around probe’s tip wets.
Water get sucked into the tip and the vacuum in tube reduces.
Chapter 3: Methodology
Soil Column
Soil permeability:
Ability of the soil to let water flow through it.
Measured using raingauge
Monitors rainfall events and at the end of each minute, stores the minute rainfall to memory.
Software used: Rainlogger
To extract information from the rainlog
Chapter 3: Methodology
Soil Properties
Tests conducted to determine the soil properties of the soil sample
Tests conducted:
Moisture content
Bulk density
Soil water retention ability
Chapter 3: Methodology
Soil Properties
Tests conducted to determine the soil properties of the soil sample
Weight of soil sample (wet and dried) being measured.
Volume is fixed.
Chapter 3: Methodology
Soil Properties
Soil porosity – measure of void spaces between the particles of the soil
Chapter 3: Methodology
Soil Properties
Soil Water Retention Ability
Shown through SWCC (Soil Water Characteristic Curve)
Using SWCC pressure chamber (5 bars, 15 bars)
Chapter 4: Results & Discussions
Soil Column
3 datas logged:
i. Moisture content
ii. Matric suction
iii. Outflow of water
Chapter 4: Results & Discussions
Soil Column
Sample 1: Gravelly Sand (19-25 Apr 2011)
10-70 mins (1 hr rainfall)
1170-1350 mins (3 hr rainfall)
3940-4300 mins (6 hr rainfall)
Chapter 4: Results & Discussions
Soil Column
Sample 2: Forest Sample (28 Apr-6 May 2011)
10-70 mins (1 hr rainfall)
1300-1480 mins (3 hr rainfall)
7120-7450 mins (5 hr rainfall) – due to water ponding
Chapter 4: Results & Discussions
Soil property tests
Moisture content
Gravelly sand = 0.673%
Forest sample = 6.69%
Bulk density
Gravelly sand = 1.723 g/cm3
Forest sample = 1.217 g/cm3
Data from soil column (TDR):
Gravelly sand = 7.6%
Forest sample = 6.6%
Chapter 4: Results & Discussions
Soil property tests
Soil water retention ability
SWCC from pressure chamber test (gravelly sand)
Chapter 4: Results & Discussions
Soil property tests
Soil water retention ability
SWCC from pressure chamber test (forest sample)
Chapter 4: Results & Discussions
Soil property tests
Soil water retention ability
SWCC from soil column data (gravelly sand)
Chapter 4: Results & Discussions
Soil property tests
Soil water retention ability
SWCC from soil column data (forest sample)
Chapter 5: Conclusion &Recommendations
Soil water infiltration
Infiltration pattern & rate for both sample is different.
Moisture condition will affect the pore water pressure (matric suction).
Matric suction will affect the infiltration rate and water retention ability.
Chapter 5: Conclusion &Recommendations
Comparison
Water infiltration will alter the properties of the soil.
Alteration of soil properties will affect slope stability. (Eg., pore water pressure of forest sample during infiltration – negative pore pressure)
Chapter 5: Conclusion &Recommendations
Suggestions
Duration of the rain infiltration
Equipments
Soil column design
Study on the behaviour of soil