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Forms and causes of soil erosion and prevention
Forms and causes of soil erosion and prevention
Soil erosion
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Compaction is a densification of the soil which reduces its biological activity, permeability, porosity, and water holding capacity, while at the same time increasing the risk of erosion due to accelerated run-off (13). While some soils are naturally compacted, mechanical pressure (i.e. heavy machinery) can compact soil (13). Erosion is a natural process which is actually essential in the soil formation process, but human activities have accelerated it (7). During erosion soil particles of the fertile topsoil are removed either by wind or water (i.e. runoff), this process is irreversible and can lead to the reduction of soil productivity (7).
Salinization refers to the problem where water-soluble salts containing sodium, potassium, magnesium,
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The whole world, not just Europe is heading to this point, it is estimated that 24 billion tons of fertile soil are lost annually; they are non-renewable (4). Local legislations exist in Europe to address some threats to soil, but there is nothing comprehensive for the EU. A proposal for a Soil Framework Directive was introduced in 2007, but the Commission decided in May 2014 to withdraw it (3).
This directive addressed the major threats to soil, such as the preservation of soil functions, the prevention of soil degradation (loss of biodiversity and organic matter), limit the concentration of dangerous substances that could harm humans and the environment (contamination), reducing erosion, and remediating contaminated and degraded sites (9, 15). Regarding soil organic matter content for example, carbon is lost when grasslands or forests are converted into croplands and vice versa, proper management and constraints have to be put into place in order to mitigate the losses (17). Another major issue is the interrelationship between the soil and climate change; with improper land use too much carbon dioxide is released into the atmosphere, this speeds up climate change, which in turn will increase carbon dioxide discharge, creating a viscous
Louisiana contains approximately 40% of the coastal wetlands of the lower forty-eight states. Louisiana has lost up to forty square miles of marsh per year for several decades (accounting for 80% of the nation’s annual coastal wetland loss) (lacoast.gov). From a hydrologic standpoint, the wetlands replenish aquifers, hold excess floodwaters from intense rainfalls, and provide storm surge protection.
Costal erosion, especially on barrier islands, is a major concern throughout the world. The issue represents a serious concern for many vulnerable coastlines throughout the coastal regions of the world. This issue must be studied for root causes so it can, if at all possible, be brought under some semblance of control before it is too late. The cost of ignoring this issue would be catastrophic to both communities on the beach and the marine life that depend on the coastal areas for their very survival.
Soil liquefaction describes a phenomenon whereby a saturated or partially saturated soil substantially loses strength and stiffness in response to an applied stress, usually earthquake shaking or other sudden change in stress condition, causing it to behave like a liquid. The phenomenon is most often observed in saturated, loose (low density), sandy soils. This is because the loose sand has a tendency to compress when a load is applied; dense sands by contrast tend to expand in volume. If the soil is saturated by water, then water fills the gaps between soil grains. In response to the soil compressing, this water increases in pressure and attempts to flow out from the soil to zones of low pressure (usually upward towards the ground surface). However, if the loading is rapidly applied and large enough, or is repeated many times (e.g. earthquake shaking, storm wave loading) such that it does not flow out in time before the next cycle of load is applied, the water pressures may build to an extent where they exceed the contact stresses between the grains of soil that keep them in contact with each other. These contacts between grains are the means by which the weight from buildings and overlying soil layers are transferred from the ground surface to layers of soil or rock at greater depths. This loss of soil structure causes it to lose all of its strength. According to the
Traditional agriculture requires massive forest and grassland removal to obtain land necessary to farm on. Deforestation and overgrazing has caused erosion flooding, and enabled the expansion of deserts. But with drainage systems, leveling, and irrigation provided by the Green Rev, all this terra deforming will unlikely happen again. We can retain clean air and lessen the global warming effect caused by deforestation.Many people argue that a revamp in agriculture will be way too expensive and unrealistic especially for those poor farmers in third world countries. However many times, they exaggerate the price.
The Grand Canyon in northern Arizona is considered the world’s best example of exposed geologic layering, and contains fossils ranging from Precambrian stromatolites to Ice Age. There is also a potentially active volcano on the western end of the Grand Canyon. Erosion has uncovered 1.7 billion years of geologic history.
It’s funny how things that you used to do as a kid can change the course of people’s lives. Myself, when my parents told me and my brothers and sisters that we were going to the cabin meant a week of solid fun. My family has a cabin up on Camano Island, which is about 20 minutes north of Everett, right off of the I-5 interstate. My family would go up there during the summer with my cousins and grandma, and go swimming when the tide was in, build sandcastles when the tide was out, only to have them washed away when the tide came back in, build forts with the new driftwood that came in each year, explore the wrecked ship down the beach in one direction from our cabin, and scour the dunes that were north of our cabin. The dunes were the best part going to the cabin. We would always try to get there by walking along the wood that had been washed up and once we got there, we would race up the hills and jump down into the sand pits below. Another things that we all used to love doing, were to see who had carved messages into the sides of the dunes. There were all sorts of messages, love message from husband to wife, boyfriend to girlfriend. ‘I was here’ messages, and then there were simply names. That is what we always used to do. Every year, my two cousins, dad, three siblings and I would climb up into the dunes and carve our names into the wall using sticks. This was done over and over again for about 8-10 years. Over the last couple of years we did this we noticed that we could see a house at the top of the dunes. This was something that we never noticed before and when we asked my dad, he said that he never noticed it either. We thought nothing about it at the time, carved our names in the wall and went back to the cabin. Later on we heard from other people who lived up there that there was a big concern by the people who live in that house that all of the messages that people had carved along with the natural erosion of the hills has caused the hill side to be dangerously close to being pushed back far enough to where the house might fall down.
NATURAL DUNE SYSTEM: Commonly, the dune at the back of a natural beach is called the fore-dune, a ridge of sand forming with its axis, or crest, parallel to the shoreline. Such a dune or sand ridge in association with a beach also is called a beach ridge. The vegetation serves as an anchor for wind-blown sediment and generates continuous dune growth. When the grass is removed by storms, fire, trampling, overgrazing, or simply too much sand coming ashore across the beach, the dunes are destabilized and may begin to migrate landward. The size of a dune is mainly a function of sand supply: the larger the supply from the beach, the higher the dunes. Prevailing wind directions, beach width and time available to build a dune are part of the sand
Contaminated land is characteristically remediated to address environmental risks, risks to users of the sites, as well as financial and legal liabilities. In addition, with more and more pressure being put on our countryside for the development of new industries, business and also housing, there is an increasing tendency to build on existing sites to preserve Greenfield sites for future generations. Some of these existing sites may contaminate. The government has set targets for housing that 60% of all new housing should be built on existing "Brownfield" sites to preserve our countryside.
How do people have an effect on erosion? mad isA According to the cites that I placed onto my “work cited” page, people have an affect on erosion in many different ways. From building things on top of where water runs, to digging ponds and making the wind blow differently. Precipitation is the most forceful factor when it comes to causing erosion.
Agriculture also leads to soil erosion, both through rainfall and wind. This soil can damage the aquatic ecosystems it ends up in, an...
Soil is the most important non-renewable resource on any farm. Healthy soil is key to a good
A study done by Johnson and Lewis (2007) imparts that trees are of importance to the environment since they help anchor the soil; for this reason deforestation remains a burden to the natural environment. Due to deforestation there is likely to be habitat destruction; with the change in land use species tend to lose their habitats. Before constructing filling stations there is removal of the topsoil, this results in soil erosion at the construction
As a result of this process, the mine sites "do not develop normal soil structure or support the establishment of a plant cover". Many mine sites have...
There is powerful evidence showing that clearing tress not only spews carbon into the atmosphere, it also leads to major shifts such as increased temperatures and rainfall worldwide
One of the reasons for loss in biodiversity is alteration of habitats. A habitat is the natural environment in which a species of living organism lives. If the habitat of a species is changed, it will cause the species to die or migrate to other places where it can find its natural habitat. There are many ways in which the habitat of plants and animals can be altered. One of them is land use changes. Since the beginning of human life, human beings have been changing land use for farming. Large areas of forests have been cleared by humans to increase the area of farming to satisfy their growing needs. Many biodiversity-rich landscape characteristics have been lost due to intensive farming (Young, Richards, Fischer, Halada, Kull, Kuzniar, Tartes, Uzunov & Watt, 2007). For example, traditional farming was replaced by private farms in Europe after the First World War causing an immense change in land use patterns. Another major proble...