STABILIZATION OF CLAYEY SOIL USING CHEMICALS Bhawna Sahay1, Prof. V.K.Arora2
ABSTRACT: Soil stabilization is a technique of enhancing the geotechnical properties and strength of soil to modify the bearing capacity and durability of weak soil. There are numerous methods of stabilising the soil such as soil replacement , grouting ,reinforcing ,chemical, mechanical, electrical method, using additives such as fly ash, rice husk, gypsum and cement. Chemical stabilization with lime and sodium hydroxide is time saving method. All these chemicals are highly reactive in nature and react with clay particles during stabilization process which leads to improve the geotechnical properties of soil.
KEY WORDS: stabilization; optimum
…show more content…
EXPERIMENTAL WORK
1. LIQUID LIMIT
2. PLASTIC LIMIT
3. SPECIFIC GRAVITY
4. COMPACTION
5. UNCONFINED COMPRESSIVE STRENGTH
All these are laboratory test which conduct on soil sample individually or with combination of soil with chemicals, the percentage of used during testing is 3%, 7%, 10% of lime and 8%, 12% 16%, of sodium hydroxide. Chemical stabilizer is used for mixing of chemicals with soil in fine proportions so that during testing chemicals should be thoroughly mixed with soil as these chemicals are available in powder form or in chips form which are not easily mixed.
The table shows the value of clayey soil sample of the above test: Table 1: Details of soil sample PHYSICAL PROPERTIES VALUE GRAIN SIZE DISTRIBUTION GRAVEL SAND SILT +
Cadet Eric Wiggins Date: 18 September 2014 Course Name: Chem 100 Instructor: Captain Zuniga Section: M3A Identification of a Copper Mineral Intro Minerals are elements or compounds that are created in the Earth by geological processes. The method of isolating metals in a compound mineral is normally conducted through two processes.
In this lab we were trying to figure out if Salt Creek and Barker Lake had the correct chemical balances to sustain catfish for the years coming. In order to find this out, we tested the water using a Hach Water Testing Kit. Inside were dissolved oxygen reagent powder pillows 1, 2 and 3 which we added and mixed into our sample water to prepare it for testing. Then we added droplets of Sodium Thiosulphate Solution into the prepared water too see how much dissolved oxygen parts per million were in the water. Our independent variable in this experiment was the 5 different testing sites that we went to for water samples.
Characteristic Property- Test 2- Density Materials: Triple Beam balance, distilled water, graduated cylinder, unknown 6 Procedure: first we found the mass of the empty graduated cylinder and then its mass with the now distilled unknown. After subtracting the mass of the graduated cylinder, we were able to find the volume. For every 1mL=1cm³ so there we had the volume found with the graduated cylinder. We divided the mass by the volume in order to get the density Data: We found that the density of our unknown was 0.76 g/cm3.
Introduction For two days, on the 14th and 15th of April, a field excursion to Hastings Point, New South Wales was conducted. At Hastings Point, topography, abiotic factors and organism distribution were measured and recorded, with the aim of drawing links between the abiotic factors of two ecosystems (rocky shore and sand dunes), the organisms which live in them, and the adaptations they have developed to cope with these conditions. Within these two ecosystems, multiple zones were identified and recorded, and this report also aims to identify the factors and organisms associated with each zone. Lastly, using data and observations from the past, predictions for the future of the rock pool ecosystem were made.
The data observed and recorded in this lab shows that the concentration of miracle gro’ does affect the growth rate and germination speed of black eyed peas. The data is shown through two graphs and two data tables. The control group in this experiment is the seeds with a 0% concentration of miracle gro’, therefore the seeds with just water. The experimental groups are different concentrations of miracle gro’ including a 10%, 15%, 20%, 25%, and 30% concentration. The variable in this experiment is the amount/concentration of miracle gro’.
To find chemical equilibrium, the following chemical equation is used in the experiment: Fe3+(aq) + SCN-(aq) FeSCN2+(aq). When iron (III) and thiocyanate react, thiocyanoiron (III) is produced. When the concentration of all ions at equilibrium are known, the equilibrium constant can be calculated by dividing the equilibrium concentration of the reactant by the equilibrium concentration of the products. In this experiment, four equilibrium systems containing different concentrations of three different ion types (Fe(NO3)3, KSCN-, and distilled water) are made and used to determine equilibrium concentrations.
How the landscape and soil shape middle,new england and southern colonies New England ; the Soil in the New England region is quite rocky, hilly, and shallow. It made England hard to plant and export cash crops England was by the Atlantic ocean. The land in New England was shaped by glaciers. During the Ice Age, thick sheets of ice cut through the mountains. Glaciers pushed rocks and rich soil south.
In this lab, the water molecules stick strongly together and
In the next steps the density of water between 30-40 °C, 40-50 °C and 50-60 °C was measured. Then our results ρ vs T and also density vs temperature values given in the Steam Tables were plotted on the same graph in order to compare. In the second part the density of water was measured by density bottle. The densities obtained from the experiment are 995, 992.5, 991, 990 kg/m3 for the first part and
The loamy sand appeared in the A horizon which is considered to be the top soil region. Loamy sand is characterized by containing approximately 25% medium coarse sand particulates, 25% very coarse sand, and less than 50% fine sand and very fine sand (USDA, n.d). The larger the soil particles the less hydrophilic the soil is. Many horticulturalists find that loamy soils are very productive because of their ability to retain water while also draining well (Lerner). This can therefore explain the high levels of vegetative growth in the three locations the soil texture was present in.
Abstract: The purpose of this experiment was to determine whether the amount of topsoil would influence the growth of radish plants. It was hypothesized that if the amount of topsoil increased by 50% would increase because topsoil contains the essential nutrients which are required for proper plant growth. The principle findings indicated that a medium amount of topsoil is ideal for plant growth as the radish plant potted in 50 ml of topsoil experienced the most growth in comparison to the radish plants potted either in 25 ml or 200 ml of topsoil. Introduction: A healthy layer of topsoil comprises of a mixture of clay, sand, silt, and humus that supply the plants with vital nutrients, such as nitrogen, phosphorus, potassium and other necessary
Introduction In this lab, density was discussed and was the main topic of the lab. Density is how much of a substance is in a given volume. The purpose of this lab was to see how density changes in solutions at different temperatures, in this case, Oobleck, a non-newtonian fluid. Hypothesis
Acids are proton donors in chemical reactions which increase the number of hydrogen ions in a solution while bases are proton acceptors in reactions which reduce the number of hydrogen ions in a solution. Therefore, an acidic solution has more hydrogen ions than a basic solution; and basic solution has more hydroxide ions than an acidic solution. Acid substances taste sour. They have a pH lower than 7 and turns blue litmus paper into red. Meanwhile, bases are slippery and taste bitter.
TABLE OF VARIABLES Independent Variable Method of measurement Concentration of HCl
The thinner the container the slower the reaction as there are less particles which the substances can collide with. Use the same sized container for every experiment