The success of any geotechnical engineering design is heavily dependent on engineering properties of soils/rocks that involve with the project. Therefore, it is essential to measure engineering properties of soils/rocks accurately following the given standards and specifications.
Objectives
In this Lab practice, we are required to:
Practical
This test is carried out to determine the percentages present of various sizes (governed by sieves used) of particles in a soil (generally on soil particles coarser than 212 ).
Equipment:
Materials: Soil (sand)
Procedure:
Note: The water content of the sand was assumed to be zero since the sand was oven dried.
Col 1 |
Col 2 |
Col 3 |
Col 4 |
Col 5 |
Col 6 |
Col 7 |
Sieve Size (mm) |
Mass Of sieve (g) |
Mass Of sieve + retained Soil (g) |
Mass of Retained Soil(g) (Col3-C0l 2) |
Cumulative Retained Mass(g) |
Cumulative % retained (Col5/ms *100) |
% passing |
4.75 |
116.23 |
166.13 |
49.9 |
49.9 |
4.53 |
95.47 |
2.0 |
99.27 |
135.77 |
36.5 |
86.4 |
11.34 |
88.66 |
0.84 |
97.58 |
139.68 |
42.1 |
128.5 |
19.13 |
80.87 |
0.425 |
98.96 |
138.96 |
40 |
168.5 |
39.87 |
60.13 |
0.25 |
91.46 |
114.46 |
23 |
191.5 |
75.69 |
24.31 |
0.106 |
93.15 |
184.15 |
91 |
282.5 |
89.64 |
10.36 |
0.075 |
90.92 |
101.12 |
10.2 |
292.7 |
96.12 |
3.88 |
PAN |
70.19 |
301.19 |
231 |
523.7 |
100 |
0.00 |
D50 =0.37
D50 =0.16
k=0.01 x 0.16
k= 1.6 x 10-3m/sec
Cu= D60/D10
Cu= 0.43/0.16
Cu= 2.69
Coefficient of curvature (CZ)
CZ=D302/D10 x D60
CZ=0.282/0.16 x0.43
CZ=1.14
Sieve analysis is a technique used to assess the particle distribution of granular materials (soils) used in engineering practices. The size of the granular materials is of critical importance to the manner the material performs in use. Sieve analysis is used to deduce the appropriate materials to be used on construction activities such as backfilling, mortar preparation among other activities.
Flow measuring apparatus designed to accustom students to typical methods of measuring the discharge of an incompressible fluid assuming flow is under the steady-Energy flow condition (Bernoulli’s flow condition). Discharge is determined through a Venturi Meter, Orifice Plate Meter and a Rotameter.
Shows the flow measuring apparatus where water from the Hydraulic bench enters the equipment through a Perspex venture meter, which consists of a gradually converging section, followed by a throat, and a long gradually diverging section. After a change in cross-section through a rapidly diverging section, the flow continues along a plate with a hole of reduced diameter through which the fluid flows.
Following a further settling length and a right-angled bend, the flow enters the Rotometer. This consists of a transparent tube in which a float takes up an equilibrium position. The position of the float is a measure of the flow rate.
After the Rotometer water returns via a control valve to the Hydraulic Bench and the weigh tank. The equipment has nine pressure tappings as detailed in Fig 1, each of which is connected to its own manometer for immediate read out.
Theory:
ZA, ZB : Datum heads and section A and B
VA, VB : Velocity at section A and B
PA, PB : Pressure at section A and B
HA, HB : Pressure head at section A and B
AA, AB : Cross sectional area at section A and B
Applying Bernoulli’s Equation between section A and B:
Equation of continuity:
From Equation (1) and (2),
Compared to pressure head and velocity head, datum head is negligible;
Compared to theoretical flow rate actual flow rate is little short. Hence Actual flow rate is given by;
– Coefficient of discharge
By considering Log and rearranging above equation;
Can be found from the intercept (C) of the equation 3.
(ii) Orifice meter
Applying Bernoulli’s Equation between section E and F:
Here consists of two factors
: Ratio of actual velocity to ideal velocity at the orifice.
: Ratio of effective cross sectional area of flow at the contracted section to the actual cross sectional area of the orifice.
In orifice meter there is a slight increase of pressure head due to reflection of impact pressure from the orifice wall. Hence desired head difference across the Orifice meter is less than that of measured.
For comparison purposes we can define a dimensionless parameter as follows;
Apparatus:
Test |
Mass Kg |
Time (S) |
Flow rate m3/s x10-4 |
H1mm |
H2mm |
?H m |
H1mm |
H2mm |
?H m |
1 |
6 |
12.80 |
4.7 |
380 |
113 |
0.267 |
368 |
63 |
0.305 |
2 |
6 |
13.39 |
4.5 |
360 |
113 |
0.247 |
352 |
80 |
0.272 |
3 |
6 |
14.74 |
4.1 |
340 |
138 |
0.202 |
333 |
100 |
0.233 |
4 |
6 |
13.39 |
3.7 |
320 |
158 |
0.162 |
313 |
128 |
0.185 |
5 |
6 |
18.58 |
3.3 |
300 |
175 |
0.125 |
295 |
153 |
0.142 |
6 |
6 |
22.75 |
2.7 |
279 |
195 |
0.084 |
274 |
183 |
0.091 |
Discussion:
Variation in the height of the water column of the venture meter is less than the variation in the height of water column in the orifice plate this is for the reason that the difference in diameter of the areas of orifice is more than the venture meter. So we can say that the difference in height of water column is directly proportional to the difference in the diameter of the area.
Advantages of Venturimeter
Disadvantages of Venturimeter
Advantages of Orifice meter
Disadvantages of Orifice meter
Reference
Rajapakse, R. (2015). Geotechnical engineering calculations and rules of thumb. Available at: https://search.ebscohost.com/login.aspx?direct=true&scope=site&db=nlebk&db=nlabk&AN=1100417. [Accessed: 25 Jul. 2018].
Global Water Instrumentation. (2011). Rotameters. Available at:https://www.globalw.com/support/rotameter.html. (Accessed: 25 Jul 2018).
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