A Clean Look at Soil Mechanics
Soils are basically unconsolidated layers that cover the earth’s surface. Soils consist of particles of varying shapes and sizes formed after parent rock are subjected to and broken down by forces of climate, organisms and chemicals over time.
Soils mechanics refers to the art of applying the mechanics of solids to the soil to predict its deformation behavior and strength. Understanding soil mechanics enables engineers and other professionals to create structures with soil and appreciate its interaction with other structures built on it.
Soil formation
Soil is formed through the weathering of rocks. There are three main types of rocks from which soil forms; igneous, sedimentary and metamorphic. Igneous rocks form when hot magma that is in liquid form cools and solidifies forming crystalline rocks. Sedimentary
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Factors such as temperature also contribute to the chemical weathering process and may aid in accelerating or hindering the reactions.
SOIL TYPES
There are several major types of soil. Each type of soil has various characteristics that make it distinctive
• Sand soil. Rock particles that will pass a 4.75 mm sieve and be retained on a 75-μm sieve is considered to be sand. Depending on the particle sizes sand is usually classified as coarse, medium or fine.
• Clay soil/silt. Clay is usually fine grained and depending on the amount of water content, can exhibit plasticity. Soil that passes a number 200 sieve (US Standard) is considered to be clay.
• Gravel-This are rock particles that will pass a 75mm sieve but not a 4.75mm sieve. Gravel can either be coarse or fine depending on the particle size.
• Peat-This is mainly composed of decomposing organic matter and as a result it usually produces
As pH increases or decreases to get closer to the optimal pH --in this case it is 7 for this particular enzyme-- the rate of reaction peaks and is highest at that point, which is described by the molecular shape and structure of the enzyme at its optimal pH. When turnip peroxidase is at pH 7, the active site is able to fit perfectly with the substrate, therefore explaining why the reaction rate is fastest at this point. Accordingly, if the active site is disrupted, the substrate cannot fit perfectly causing the reaction rate to slow down. This can be supported by the data because the reaction rate gradually increased from pH 3 to pH 7 and reached its maximum at pH 7. Once it did reach the optimal pH, the reaction rate continuously decreased
This is because minerals are easy to fracture. They also poses a crystalline structure. Rocks are a mixture of minerals, whereas minerals are their own purest form.
According to Harrison Eutrophication is the excessive production of algae and higher plants through the enrichment of waters by nitrogen and phosphorus. Phosphorus in the form of phosphate is the limiting nutrient as the amount of biologically available phosphorus is small in relation to the amount needed for algal growth. Harrison states that sources of nutrients can be discrete, (sewage), or diffuse, (farmland fertilizers).
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 bedrock that Michigan sits on includes sandstones. As the glaciers eroded the landscape of Michigan, sand became much more abundant, giving us our sandy beaches, sand dunes and wetlands. When the sand blocks the ability for the water to drain from the land into the lakes, it traps the water and creates what we know today as wetlands. The sand eroded by the glaciers has also shaped Michigan’s shorelines today. Michigan obtains mostly western winds, causing the Lake Michigan coastline to have substantial dunes not only along the shoreline, but also further inland than the typical dunes.
Title: Enzymes Abstract: Enzymes can catalyze chemical reactions by speeding up the chemicals activation energy. Temperature and pH are just two of the factors that affects enzymes and their involvement with chemicals and the way they function. Throughout this experiment, we conducted a study on peroxidase, which is an enzyme. The following information consist of the recordings of when it was exposed to four different pH levels to come up with an optimum pH and IRV at the end. Introduction: Enzymes are proteins that are used in reactions in living organisms.
Its composition consists of Half Dome Granodiorite, which consists of quartz, feldspar, hornblende, and
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.
Another type of layer is called the Terrestrial Fossils. In this layer there are several rock layers and fossils that form this whole layer. Some layers are called the Hermit Shale, Supai Group, Coconino Sandstone, and Surprise Canyon Formation. There are many types of fossils called leaves, Tracks, and Dragonflies.
Phosphate and nitrates are examples of polyatomic ions. Polyatomic ions, also known as molecular ions, are charged chemical species composed of two or more atoms covalently bonded or of a metal complex that can be considered to be acting to a single unit. Phosphates and nitrates are found in fertilizers and some detergents. When rain dissolves these materials make their way into the creeks and rivers. When the surface waters are rich with these materials, they can cause algae to grow, which completes with other organisms for light and other nutrients.
For this program at the University of Arizona a large emphasis is placed in the role soils play in the environut. It is therefore important to learn how soils work under different conditions and how to classify them. In my major I am doing an emphasis in Physics and Chemistry. In order to understand and do well in higher level classes it is important to have a good understanding of the basic chemical and mathematical concepts used in this field. This is a subject that builds upon itself and a strong foundations will facilitate the understanding of more advanced concepts.
There are various options for paving the patio or driveway. If you are looking for the most economical option, than asphalt paving is the solution. However, you will lose on aesthetic appeal. The other two options that remain for paving is pavers and concrete material. Before you choose any one of them, know the different between them.
The hollow earth theory or ‘hohlwelttheorie’ as it is called in German, is the idea that the Earth is not a solid mass but rather an entirely hollow sphere that within contains a substantial interior space. The idea goes back to ancient mythology, folklore, and legends of a subterranean land inside the Earth, from which places of origin and afterlife were thought to be located, such as the Christian hell described by Dante, the Greek underworld, the Hindu ‘Patala’, the Celtic ‘Cruachan’ just to name few, which in its majority were caves or holes that connected the outside Earth with its interior, from which strange creatures would emerge and be seen in the surface. However, the idea didn’t have any scientific credibility until 1962 when English
Chorley said “Whenever anyone mentions theory to a geomorphologist, he instinctively reaches for his soil auger” (R.J Chorley 1978). Physical geographers are viewed as always being out in the field doing their own research and not sitting
An introduction to highway building: Although there are many methods to constructing a road, all are based on the principle that geographical objects are removed and replaced with harder and more wear-resistant materials. The pre-existing rock and earth is removed by digging or explosions. Tunnels, embankments and bridge are then added when necessary. The material that the road is being constructed from is then laid by various pieces of equipment, which will be looked at in greater detail in this assignment. The construction management of roads has become increasingly more difficult as larger structures are constantly being required in increasingly short amounts of time.