Influence of swell on shear strength of expansive soils

Download
2016
Deliktaş, Ceren
Behavior of swelling soils is thoroughly investigated since they cause significant hazard to structures all around the world, especially in the regions with climate of arid or semi-arid. These types of soils expand upon wetting and shrink when water is removed. Existence of water significantly alters the shear strength of swelling soils. Therefore, the objective of this study is to examine the influence of swell on the shear strength of expansive soils. For the first series of tests, an artificial expansive soil was prepared in the laboratory by mixing 15% bentonite and 85% kaolinite. Grain size distribution, specific gravity, Atterberg limits and dry density versus moisture content curve were determined. Then, to obtain swell percent and rate of swell, swell tests were conducted in special molds and unconfined compression tests were made. For the first series of tests, soil samples were sheared without allowing expansion to take place. This test was considered as the reference test. Then, specimens were sheared after they were allowed to swell in specially designed molds until vertical swell stopped, which were referred to 100% swell. In the mid-steps, shear strength was obtained when soil sample reached to 10%, 15%, 20%, 25%, 50% and 75% of ultimate vertical swell. These eight swell and shear tests were repeated for three expansive Ankara clays having different swelling potentials since natural soil samples could be found just in Ankara. As the result of shearing tests, it was seen that when the specimen reached to ultimate swell, shear strength was reduced to approximately 90% of its initial value. Free swell index test and methylene blue test were performed to estimate the swelling potential. Besides, tests showed that a frictional stress equal to about 17-25% of swell pressure developed between the mold and specimen.

Suggestions

Effect of cyclic swell – shrink on swell percentage of an expansive clay stabilized by class c fly ash
As, Mehmet; Çokça, Erdal; Department of Civil Engineering (2012)
Expansive soils are a worldwide problem especially in the regions where climate is arid or semi arid. These soils swell when they are exposed to water and shrink when they dry. Cyclic swelling and shrinkage of clays and associated movements of foundations may result in cracking of structures. Several methods are used to decrease or prevent the swelling potential of such soils like prewetting, surcharge loading, chemical stabilization etc. Among these, one of the most widely used method is using chemical adm...
Influence of swell on undrained shear strength of expansive Ankara clay
Deliktas, Ceren; Çokça, Erdal (Springer Science and Business Media LLC, 2020-09-01)
Expansive clays cause problems throughout the earth, in particular for the locations in arid or semi-arid climate. Ankara (Turkey) is in semi-arid climate and change in moisture content of the reddish-brown expansive Ankara clay causes swell-shrink related movements and damages on lightweight structures. Over-estimation of undrained shear strength of an expansive clay without considering swell amount can lead to failures (i.e., bearing capacity, slope stability, and pile capacity). Since the existence of wa...
Stabilization of expansive soils by using red mud
Çağlar, Cemre; Çokça, Erdal; Department of Civil Engineering (2019)
Expansive soils are generally existing in semi-arid and arid regions of the world. This type of soils expands when they absorb water and shrink when they dry out. Expansive soils are causing problems to the lightweight structures. The purpose of the study is to suggest a cost-effective alternative method for coping with these problems. The widely used traditional method is the stabilization of the soil with the chemical admixtures. In this study; waste red mud and waste fly ash were used as stabilizers. The...
Effects of drying on Atterberg limits of pyroclastic soils of Northern Turkey
Huvaj Sarıhan, Nejan (2018-09-15)
In this study, the effects of drying on Atterberg limits is investigated using 30 soil samples taken from 0.2 m to 4 m depths, from nine different landslide sites in pyroclastic deposits in Northern Turkey. Samples for Atterberg limits are prepared by (i) starting from in-situ moisture content without any drying, (ii) drying at 60 degrees C and (iii) drying at 110 degrees C. The range of liquid limit values is 35%-103% and plasticity index is 0%-37% when samples are prepared from their in-situ moisture cont...
Lateral versus vertical swell pressures in expansive soils
Sapaz, Burak; Erol, Orhan; Department of Civil Engineering (2004)
Expansive or swelling soils, exist in many part of the world, show excessive volume changes with increasing water content. As a result of this volume increase, expansive soils apply vertical and lateral pressures to the structures located or buried in these regions. Many researchs have been carried out on vertical swelling pressures helping to the engineers to design structures withstanding on these stresses. However, lateral swell behaviour of swelling soils have not been fully understood yet. Structures s...
Citation Formats
C. Deliktaş, “Influence of swell on shear strength of expansive soils,” M.S. - Master of Science, Middle East Technical University, 2016.