Presentation is loading. Please wait.

Presentation is loading. Please wait.

Experiment No.5: Soil Consistency (Atterberg limits)

Similar presentations


Presentation on theme: "Experiment No.5: Soil Consistency (Atterberg limits)"— Presentation transcript:

1 Experiment No.5: Soil Consistency (Atterberg limits)

2 In the early 1900s, a Swedish scientist named Atterberg developed a method to describe the consistency of fine-grained soils with varying moisture contents. At a very low moisture content, soil behaves more like a solid. When the moisture content is very high, the soil and water may flow like a liquid. Hence, on an arbitrary basis, depending on the moisture content, the behavior of soil can be divided into four basic states— solid, semisolid, plastic, and liquid. The moisture content, in percent, at which the transition from solid to semisolid state takes place is defined as the shrinkage limit. The moisture content at the point of transition from semisolid to plastic state is the plastic limit, and from plastic to liquid state is the liquid limit. These parameters are also known as Atterberg limits.

3

4 Liquid limit (LL) ASTM (Casagrande)
Liquid limit (LL) Theoretical: The moisture content in percent at the point of transition from plastic state to liquid state.

5 Tools Liquid limit test device and grooving tools

6 Procedures: To perform the liquid limit test, one must place a soil paste in the cup. A groove is then cut at the center of the soil pat with the standard grooving tool . By the use of the crank-operated cam, the cup is lifted and dropped from a height of 10 mm (0.394 in.). The moisture content, in percent, required to close a distance of 12.7 mm (0.5 in.) along the bottom of the groove after 25 blows is defined as the liquid limit. 25 blows is defined as the liquid limit. It is difficult to adjust the moisture content in the soil to meet the required 12.7 mm (0.5 in.) closure of the groove in the soil pat at 25 blows. Hence, at least three tests for the same soil are conducted at varying moisture contents, with the number of blows, N, required to achieve closure varying between 15 and 35.

7 Photographs showing the soil pat in the liquid
limit device: (a) before test; (b) after tes

8 Flow curve for liquid limit determination of
a clayey silt

9 fall cone method (British Standard—BS1377).
In this test the liquid limit is defined as the moisture content at which a standard cone of apex angle 30 and weight of 0.78 N (80 gf) will penetrate a distance d = 20 mm in 5 seconds when allowed to drop from a position of point contact with the soil surface. Due to the difficulty in achieving the liquid limit from a single test, four or more tests can be conducted at various moisture contents to determine the fall cone penetration, d. A semilogarithmic graph can then be plotted with moisture content (w) versus cone penetration d. The plot results in a straight line.

10 tools 1- Penetrometer device: cone with angle 30o and mass of 80grams. 2- Metal cup 55mm width and 40mm depth 3- Water content apparatus (Oven dry – Cans – Balance).

11

12

13 Plastic Limit Test Plastic limit is defined as the moisture content, in percent, at which a cohesive soil will change from a plastic state to a semisolid state. In the laboratory, the plastic limit is defined as the moisture content (%) at which a thread of soil will just crumble when rolled to a diameter of 1/8in. (3.18 mm).

14 tools 1- Glass plate. 2- Water content apparatus.

15 Procedures


Download ppt "Experiment No.5: Soil Consistency (Atterberg limits)"

Similar presentations


Ads by Google