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Nature and properties of soils
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The term expansive soil indicates to soils, which ahs the tendency to swell when their moisture content is allowed to increase. The moisture may come from rain, flooding, leaking water or sewer lines, or from a reduction in surface evapotranspiration when an area is covered by a building or pavement. The term cracking soils is also used for these soils as they have the tendency to shrink and crack when the moisture is allowed to decrease. Soils containing the clay mineral montmorillonite generally show these properties (Komine and Ogata, 1996; Rao and Triphaty, 2003; Sivapullaiah et al. 1996; Wayne et al. 1984).
There are many correlations that are useful in identifying potentially expansive soils. It may also be possible to identify them visually. Visual indications include (Wayne et al. 1984):
1) Wide and deep shrinkage cracks occurring during dry periods
2) Soil is rock-hard when dry, but very sticky and soft when wet
3) Damages on the surrounding structures due to expansion of soil
Expansive soils are mostly found in arid and semi-arid regions of the world. The presence of montmorillonite clay in these soils imparts them swell-shrink potentials (Chen, 1988).
Expansive soils cover nearly 20% of the landmass in India and include almost the entire Decan plateau, Western Madhya Pradesh, parts of Gujurat, Andhra Pradesh, Uttar Pradesh, Karnataka, and Maharastra (Gopal Ranjan and Rao, 1991).
Expansive soils are a worldwide issue that poses many challenges for civil engineers. These are considered a potential natural hazard, which can cause extensive damage to structures if not properly treated. Such soils swell when given an access to water and shrink after they dry out (Al-Rawas et al. 2002).
In general, expansive soils hav...
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...ssification tests
Atterberg limits are usually used for identifying swelling soil. The increase in plasticity index is considered as an indicator of increased swelling potential. Chen (1988) presented a classification of swelling soil based on the plasticity index of the soil as shown in Table 2.1.
Table 2.1 Expansive soil classification based on the plasticity index
PI (%) Swelling potential
0 - 15 Low
10 - 35 Medium
35 - 55 High
55 and above Very High
Classification based on shrinkage index is found to be undependable to predict swelling potential of soil. However, the shrinkage index may be used with plasticity index for identification as shown on Table 2.2..
Table 2.1 Expansive soil classification based on the plasticity index and shrinkage index
PI (%) SI (%) Degree of expansion
< 12 < 15 Low
12 - 23 15 - 30 Medium
23 - 32 30 - 40 High
> 32 > 40 Very High
Mississippi has a variety of different soils .The three general soils are 1) the river flood plain, known as the Delta, 2) a loess region, or bands of soils formed in windblown material that adjoins the Delta, and 3) Coastal Plain. The Mississippi Delta is better for growing row crop, while the loess and Coastal Plain region are better for animal production and forestry. The loess and Coastal Plain regions are divided based on similar soils, geology, climate, water resources, and land use called Major Land Resource Areas. The Mississippi Delta’s soil comes from sediments left by flooding various rivers in the region, rather than being a typical Delta formed by the mouth of a river. In the Delta most of the land is farmed, with three-fourths of the cropland to the north. Controlling surface water and drainage are major soil management issues. In the Delta soils are naturally diverse because of their alluvial origin. Particle sizes within the sediment decrease as distance from the originating stream increase. Another factor in Delta soil formation us surface water movement over time, because soils that formed under standing water have different properties than soils formed under moving water. Soils with large amounts of clay particles have unique features. When the soil is dry, small round aggregates form at the surface that look like shotgun buckshot, which is where the popular name for Delta clay soils “buckshot” came from. Soils with large clay content have very slow water filtration rates; this has led to significant aquaculture and rice production in the region. When floodwaters receded in the Delta, strong winds blew some of the dry sediment left by flooded river to the adjacent uplands to form the loess areas. Because of eas...
Desert pavements are common landforms in arid regions. They consist of flat or sloping surfaces where stones are closely packed angular or rounded, and generally exhibit low relief (Mabbutt, 1977). Pavements tend to form on both alluvial fan toposequences and on weathering volcanic flow fields in arid regions. Soils are often found under desert pavements and they play an important role in the evolution of pavements (McFadden et. al., 1987). In the past there have been several theories as to the formation pavements and soil development beneath them. Deflation, or the erosion of finer grained particles from a surface, stone concentration by wash erosion and upward displacement of stone due to shrink and swell clay characteristics were at one time believed to be the main factors in the formation of desert pavements (Mabbutt, 1977). However, more recent research has shown that desert pavements are born and maintained at the surface, and that the soil below them is mainly eolian in origin. Slow accretion of eolian dust below the pavement is a process that eventually develops cumulate horizons. Eolian dust in environments where pavements often develop is rich in carbonate salts and clays due to the fact it often originates from nearby playa lake evaporate basins (McFadden et. al., 1987). Soils that form below the pavements over time develop calcic horizons and clay rich structure due to the influx of these eolian fines through the pavement surface. In turn the development of mature or plugged calcic horizons effects the form of the pavement surface because it alters the water drainage infiltration rate and causes pavements to decline.
The rich dark soil of Texas, Oklahoma, New Mexico, Kansas, and Colorado—an area also known as the Great Plains—formed from thousands of years of soil forming factors in action (Surviving the Dust Bowl). From the beginning of human populations living in the area, the soils, for the most part, remained untouched and unscathed by the plow. Thick prairie grasses covered the area and held the soils in the ground even during the periodic times of drought. This area of land was suitable for grazing practices and it was in this area that the large cattle ranches flourished. Little did the newly arrived farmers realize that this seemingly plentiful land followed a pattern of several years of rain followed by several years of drought and high winds.
Singer, M.J., and Munns, D.N., 1996, Soils: An Introduction: Upper Saddle River, New Jersey, Prentice-Hall, Inc., 480p.
This soil is geographically associated with Atsion, Berryland, and Downer soils that were discussed above. Galloway series soils have a taxonomy class of mesic which is the lower level of soil taxonomy temperature scale. The distribution of the soil is through New Jersey, Maryland, and Delaware, Maryland, and Delaware. The vegetation developed with the galloway soils are wooded areas that are heavily dominated by mixed oaks, sweetgum, red maple, pond pine, and loblolly pine. Major uses of the Galloway soils are cultivated crops that consist of corn, soybeans, hay, and truck crops. Loamy soil loses the quality of nutrients when it is strictly compacted because it depletes the organic matter, dispersing clay throughout the now compacted soil. Usually loamy soil can be found useful in farms and is used for its crumbly and soft conditions. Another way loamy soil can be used is for the construction of building homes. The development using this soil would be post and beam construction layering the soil within the walls to control humidity and air
To ensure validity, measure abiotic factors including soil temperature, light intensity, soil texture, and soil pH
In April 2013, a special memorial playground opened in Sea Bright, NJ. The project, The Sandy Ground Project: Where Angels Play, was organized by New Jersey’s Firefighter’s Mutual Benevolent Association. The playground was one of twenty-six playgrounds being installed in New Jersey, New York, and Connecticut towns honoring the children and teachers killed in the massacre at Sandy Hook Elementary School. Each town that received a playground was a town directly impacted by Superstorm Sandy. This particular playground is dedicated to Anne Marie Murphy, a special education teacher, wife, mother, and hero who passed away during the horrific shooting and is located on Sea Bright Beach which was brutally devastated by Superstorm Sandy.
Proper design of foundation required a strong basis on mechanics, but should also be enhanced by the satisfactory performance of the foundation. Soil types can affect structures in different ways, such as strength and stiffness, which will may cause stable foundation or lead to collapse. In fact, history cases helps to avoid such failure may occur in future design of foundations.
(I): Rock masses yielding low water (WPT) and cement takes (CT) are practically tight and need no treatment:
• Identifying the different aspects of soil such as colour, compaction, moisture, soil structure and soil texture will help in determining whether the soil can act as a breeding ground for pathogenic diseases. • Soil temperature plays a major role in determining the rate of plant growth. Certain temperatures are optimum for the growth of bacteria and fungi which could be hazardous as it may be disease
While it is possible for the actual sediment concentration (C) in the flow to equal Cmax, it is usually lower than Cmax by an amount depending on the strength of the soil matrix (β). The erodibility parameter (β) can be defined from the relationship,
... although we may never be able to understand exactly what soil failures can occur when a natural disasters take place, as time goes on and testing instruments and materials advance we will hopefully have a better understanding of what we can do to avoid soil failures and come up with a better and more sufficient method of improving the soils structure and strength permanently. While researching the information for this report I feel I have a much better understanding for construction geo-technics and foundations especially regarding the deformation, liquefaction and pile information related to this specific event. I hope to carry the information I have learned from this event into the construction field and apply them towards an authentic project that’s taking place and know that the information, regarding soils, I have given input on will be precise and accurate.
Soil is the most important non-renewable resource on any farm. Healthy soil is key to a good
Agriculture increase and misuse is one of the central causes of desertification. Agricultural practices require the use and often the drying up of rivers. While water overuse is fundamental to the creation of drought conditions, the deforestation and soil erosion could be considered far more detrimental. To create agricultural surfaces, land must be cleared of existing vegetation. As roots bond soils and create micro bacterial gums, their loss has significant consequences for the soil strength (1).W...
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