الفهرس | Only 14 pages are availabe for public view |
Abstract The calcareous soil is extensively found near the coastal areas of Egypt, such as the northern coast on the Mediterranean Sea. Due to its structural weakness, its performance is usually connected with different interdependent problems, such as crushability, compressibility and chemical dissolving. Furthermore, the aforementioned problems affect development of projects; such as soil replacement, excavation works for water channels, roads and railways. In earth works applications, the calcareous soil is unable to respond effectively to the imposed stresses and has become a dominant factor responsible for structure damages. Therefore, calcareous soils with such conditions need stabilization to be suitable as a construction material. Therefore, the main goal of the present study is to explore the feasibility of applying a treatment approach in the improvement of calcareous soils toward mixing the calcareous soil with Kaolinite clay. Additionally, the effects of salinity on geotechnical properties of the carbonate soil were investigated through investigating the effect of different types of water (e.g. fresh and sea water) used in compacting the soil. An extensive experimental program was performed. Whereas, the laboratory tests included chemical analysis (to evaluate some predominant chemical characteristics, e.g. carbonate content and The lower the power of hydrogen “pH”); mechanical tests on compacted material (to reveal the geomechanical behavior, e.g. shear parameters by triaxial test) after different soaking periods in fresh water (0, 4 and 90 days), and compaction tests, in addition to the California Bearing Ratio-(CBR) and hence, some of geotechnical aspects (modulus of subgrade reaction “Ks” and modulus of elasticity “E”) estimated from California Bearing Ratio-(CBR) are investigated . Additionally, physical tests (to ascertain the soil physical properties, e.g. particles gradation). To explore the crushability analyses, sieve and hydrometer analyses were applied on three different states of loading and soaking in fresh water. Thus, the first state is “natural state whether without soaking in fresh water or without applying compaction test” (NS); the second state is “after applying compaction with fresh water test only” (CS); and the third state is “after applying both of soaking in fresh water for three months and compaction test” (SCS). These tests are complemented by permeability test to 161 investigate the effect of Kaolinite added on the coefficient of permeability. Whereas, it is important in evaluating the relative influences of the treated calcareous soil formations on the stability and serviceability of earth slopes of excavated water channels. The results of the experimental study have shown that a gradual increase in maximum dry density (ɤ dry max) of Kaolinite - carbonate sand mixtures was shown by increasing the Kaolinite content “from 3% to 9%”, which the increase ratio becomes more significant in the state of sea water. Accordingly, a gradual decrease in optimum moisture content (O.M.C) of Kaolinite - carbonate sand mixtures was shown due to the lubrication phenomena, wherein the planar-shaped clay minerals are helping the sand grains to slip against each other and also, Kaolinite exhibits low quantities required for both of absorption and adsorption properties, which are due to the low surface charge on the particle. Moreover, The CBR values of the all treated mixtures, whether in the unsoaked state or after soaking in fresh water whether for four days or three months, are higher than it in the pure carbonate sand. In short term of soaking in fresh water “after four days soaking”. Both of the modulus of subgrade reaction “Ks” and the modulus of elasticity “E” take the same trend of California Bearing Ratio-(CBR) because they proportional directly with it. Cohesion strength of Kaolinite - carbonate sand mixtures compacted with sea water is generally lower than it in the same mixtures but compacted with fresh water. Furthermore, friction angle of Kaolinite - carbonate sand mixtures compacted with sea water is generally higher than it in Kaolinite - carbonate sand mixtures compacted with fresh water. However, in long term of soaking in fresh water “after ninety days soaking”, cohesion strength of Kaolinite - carbonate sand mixtures compacted with sea water is generally higher than it in the same mixtures but compacted with fresh water. On the other hand, a gradual decrease in the permeability was shown by increasing the Kaolinite content “from 3% to 9%” which the decrease ratio became more significant when the Kaolinite content is equal to three percent. Particle breakage is reduced by increasing the Kaolinite content to the calcareous sand up to 9%. |