permeability test

Civil Engineering - Texas Tech University

CE 3121: Geotechnical Engineering Laboratory

Class 5

Permeability Test

Sources:

Soil Mechanics – Laboratory Manual,B.M. DAS (Chapters 10, 11)

Soil Properties, Testing, Measurement, and Evaluation, C. Liu, J. Evett


Permeability in Soils Hydraulic Conductivity Darcy’s Law Permeability Tests

Constant-Head Test Falling-Head Test

Class Outlines


Soil Permeability

Physical(Soil Characteristics)

Mechanical

Moisture ContentUnit Weight

CompressibilityPermeabilitySpecificGravity

GradationAtterberg

LimitsStrength(Shear)

Soil Properties

Compaction

1 – Constant-Head Test

2 – Falling-Head Test


Permeability in Soils

Permeability is the measure of the soil’s ability to permit water to flow through its pores or voids

It is one of the most important soil properties of interest to geotechnical engineers


Importance of permeability

The following applications illustrate the importance of permeability in geotechnical design: Permeability influences the rate of settlement of a

saturated soil under load. The design of earth dams is very much based upon the

permeability of the soils used. The stability of slopes and retaining structures can be

greatly affected by the permeability of the soils involved.

Filters made of soils are designed based upon their permeability.


Use of Permeability

Knowledge of the permeability properties of soil is necessary to: Estimating the quantity of underground

seepage Solving problems involving pumping seepage

water from construction excavation Stability analyses of earth structures and earth

retaining walls subjected to seepage forces


Hydraulic Conductivity

Hydraulic Conductivity, k, is a measure of soil permeability

k is determined in the lab using two methods: Constant-Head Test Falling-Head Test

K is usually expressed in cm/sec Hydraulic conductivity is also known as the

coefficient or permeability


Hydraulic Conductivity (Cont.)

Hydraulic conductivity of soils depends on several factors: Fluid viscosity Pore size distribution Grain size distribution Void ratio Degree of soil saturation


Darcy’s Law

The hydraulic conductivity, k, is a product of Darcy’s Law.

In 1856, Darcy established an empirical relationship for the flow of water through porous media known as Darcy’s Law, which states: q = kiA

q = flow rate (cm3/s)

k = coefficient of permeability (cm/s)

A = cross-sectional Area (cm2)

i = hydraulic gradient

where;L

hi


Constant Head Test

The constant head test is used primarily for coarse-grained soils

This test is based on the assumption of laminar flow where k is independent of i (low values of i)

ASTM D 2434 This test applies a constant head of water to

each end of a soil in a “permeameter”


Permeameter


Procedure (Constant head)

1. Setup screens on the permeameter 2. Measurements for permeameter, (D), (L), H1 3. Take 1000 g passing No.4 soil (M1)4. Take a sample for M.C.5. Assemble the permeameter – make sure seals are air-tight6. Fill the mold in several layers and compact it as prescribed.7. Put top porous stone and measure H28. Weigh remainder of soil (M2)9. Complete assembling the permeameter. (keep outlet valve closed)10. Connect Manometer tubes, but keep the valves closed.11. Apply vacuum to remove air for 15 minutes (through inlet tube at top)12. Run the Test (follow instructions in the lab manual) …..13. Take readings

Manometer heads h1 & h2 Collect water at the outlet, Q ml at time t 60 sec.


Calculation (Constant head)

Determine the unit weight Calculate the void ratio of the compacted specimen

Calculate k as

Calculate

Aht

QLk

C

CT

CTkk

C020

0

0020


Falling Head Test

The falling head test is used both for coarse-grained soils as well as fine-grained soils

Same procedure in constant head test except: Record initial head difference, h1 at t = 0 Allow water to flow through the soil specimen Record the final head difference, h2 at time

t = t2

Collect water at the outlet, Q ml at time t 60 sec


Calculation (Falling head)

Calculate k as

Where;a = inside cross sectional area of the water tank

h1 = distance to bottom of the beaker before the test

h2 = distance to bottom of the beaker after the test

Calculate

2

1lnh

h

At

aLk

C

CT

CTkk

C020

0

0020


Typical Values of k

permeability test

Documents

measure of soil permeability

constant head of water

permeability testsources

saturated soil

soil m1take

important soil properties

flow of water

cmsechydraulic conductivity