The Yellow Wallpaper and the Tell Tale Heart Analysis

Hawkins 1 Deidre Professor Connors English 102-15 March 12, 2011 Narrative Unreliability and Symbolisms in â€Å"The Tell -Tale Heart† and â€Å"The Yellow Wallpaper† â€Å"The Tell -Tale Heart† by Edgar Allan Poe, was released in 1843. It is one of Poe’s shortest stories and provides a look into paranoia and mental deterioration. â€Å"The Yellow Wallpaper† by Charlotte Perkins Gilman, was released in 1899. This story also provides a look into mental deterioration and had been misinterpreted when it was first published. The Poe and Gilman stories discussed in this essay will help readers comprehend the credibility of the narrators and the different symbolisms used to create informative yet suspenseful content. In â€Å"The Tell -Tale Heart,† Poe†¦show more content†¦He laughs at me so about this wallpaper!† (Gilman, p327) The credibility of the narrators in both stories is very unreliable. In â€Å"The Tell Tale Heart†, the narrator is giving demonstrations of what he believes to be reasonable. â€Å"Now this is the point. You fancy me mad. Madmen know nothing. But you should have seen me.† (Poe, p37) It makes the reader wonder if the character of the narrator is beliveable because he is able to recall the events, or is he truly mad. The narrator is telling his story as if it were a one on one session, which can make it believable and then we begin to separate the madness from the â€Å"actual† events that occurred. While Gilman has written her story as the form of journal entries, this also alters the credibility of the Hawkins 3 narrator because we only know what she wants us to know, resulting in leaving out important facts. â€Å"I did write for a while in spite of them; but is does exhaust me a good deal---having to be so sly abut it, or else meet with heavy opposition.† (Gilman, p326) She is not honest about writing with her husband, and this proves that she is more than willing to tell her story her way. The symbolisms greatly have an impact on the suspense in each story. 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Failure of the Belmont Report - 847 Words

One. The Belmont Report has failed to distinguish different sources including the kinds of vulnerability or to map particular protections to particular vulnerabilities (Rogers Lange, 2013). This can be a problem because different kinds of vulnerability justify different responses. Nickel (2006) claims that there are two overlapping senses of vulnerability at work with the Belmont Report and in following human research ethics guidelines (p.2141). The first relates to the capacity to give informed consent, which the Belmont Report connects to the principle of respect for autonomy (Nickel, 2006). The second is the sense of vulnerability, as explained by Nickel, which relates to the Belmont Reports principles of justice meaning fairness (Nickel, 2006). The concern here is that vulnerable groups may be overrepresented in research for example, when the group lacks understanding or power to refuse participation (Rogers Lange, 2013). This is explicit in the Belmont Report. 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Incremental and Radical Innovation Free Essays

In recent years, the importance of innovation in business cannot be emphasized too much. Along with rapid economic development, the cooperation having innovative ability enables them to own a place in this competitive society. In order to achieve the goal of survival, the firms need to understand the different types of innovation from incremental innovation and radical innovation for those firms who guarantee with the product quality, the lower cost and increasing profits. We will write a custom essay sample on Incremental and Radical Innovation or any similar topic only for you Order Now Following this essay, the difference between incremental and radical innovation are the distinctness of change level of technology and the difference of effectiveness. Following this essay, the effectiveness of two different types of innovation and an example of each types would be explanatory. Innovation can be used in invention or improvement of products, production process, organization and staff creativity. According to the change level of technology , there are different types of innovation, one is incremental innovation and the other is radical innovation. Utilizing which types of innovation depends on what kind of conditions does a cooperation faces. Different consequence would be reached while adopting these two types on innovative system. To begin with, the definition of incremental innovation is ‘doing what we do but better’ (Tidd, Bessant, 2009, p. 27). It usually bases on improvement or boost the existing technology, products or process for maintaining the competitiveness of specific market. Adopting incremental innovation could results in enormous cost saving through upgrading or improving old products or service. Stamm,2003,p260) . In terms of reduction of inefficiencies and waste, which could benefit company from saving money, resources or time. Also this effectiveness from incremental innovation could benefit not only cooperation, but also customers. For example, a famous US airplane company – American Airlines Incorporated (AA). In 1986, when AA had faced a downturn trend with profits, they cut a signific ant cost on their on board meal. (Maynard 2005). Their crew found out that 72% of passengers do not use olive in their salad catering from airplane. The price of salad was included five items, if they change their ingredients of food without olive, it can save $500,000 cost annual year. Since this incremental innovation had reduced the operating cost significantly, increasingly amenities had been cut for less spending such as playing cards, postcards and some toys for children. Although this type of innovation cannot bring new income directly, it does not mean it cannot save a enormous money. Compared with incremental innovation which means doing what we do better, the radical innovation refers to do something different. (Tidd, Bessant, 2009, p. 7) Radical innovation is the revolutionary change in technology or market. To make a breakthrough on the limitation of current technology and production capability , which could strengthen and sustain a firm’s leadership in the market. Moreover, a radical innovation could change current competitive condition, creating a new market and making more opportunities for much benefits and profitability . For example a light emitting diode-LED which is a major device in current life. (It would be finished next time) These two different types of innovation are used in different conditions. Incremental innovation is generally a short-term innovation. On the other hand, radical innovation would continue more longer, usually over 10 years, referring to an high risk investment. Furthermore, radical innovation requires ability of high level of technology innovation, which means it need a relative large expense of investment rather than that of incremental innovation. (Ten3 Business e-Coach 2004) To sum up, in this changing commercial environment, each company should keep learning and carrying out knowledge of innovation to achieve their commitments with profits growth. How to cite Incremental and Radical Innovation, Papers

Cfcs Cause Deterioration Of The Ozone Layer Essay Example For Students

Cfcs Cause Deterioration Of The Ozone Layer Essay Cfcs Cause Deterioration of the Ozone LayerThe deterioration of the ozone layer , caused by Cfcs, endangers thelives of humans. Cfcs have a diminishing effect on the ozone layer. Furthermore, the deterioration of the ozone cause an increase of Ultraviolet(UV) radiation which can have a negative effect on human skin and eyes. As awriter for newsweek, I have investigated the scenario and found the followinginformation. The earths atmosphere is a blanket of air that surrounds the planet. This atmospheric air is made up of many different gases, 78% nitrogen, 21%oxygen, and 1% of a dozen or more other gases like carbon dioxide, helium, andozone. This atmosphere extends many miles out from the earths surface. However, this layer is not a uniform layer, from top to bottom. As one movesout from the planets surface the atmosphere becomes progressively dense. Thisatmosphere can be divide into four major regions. The first region is the troposphere which extends about 6.5 miles abovethe planets surface. The troposphere contains the oxygen that we breath and iswhere a majority of our weather takes place. Beyond the troposphere is the second region of the atmosphere, thestratosphere. The stratosphere extends from roughly 6.5-30 miles from theearths surface. The air on this region is much less dense than in thetroposphere, and its a lot drier. The stratosphere is the area that containsthe majority of the ozone layer. Past the stratosphere is the mesosphere which extends to 50 miles abovethe planet. The last region is the thermosphere. The thermospheres outermostedge is roughly 600 miles above the surface of the earth. Beyond it, theairless vacuum of space begins. Oxygen is made up of two oxygen atoms that are bonded together. In theperiodic table it is represented by O2. Like oxygen, ozone is a gas that is made up of oxygen atoms. However,a molecule of ozone is made up of three atoms of oxygen bonded together,therefore, O3, represents ozone. The ozone makes up only .01% of the atmosphere. Furthermore, 90% of the ozone is found in the stratosphere. It is concentratedin a layer between 7 and 22 miles above the earths surface. The massive depth of the ozone in the stratosphere would lead you tobelieve that it is very thick, it is not. If it were condensed, the ozonelayer would only be a few millimeters thick (Rowland and Molina 1994. p.23). The ozone is made in the stratosphere. It is continuously being formed,broken down, and reformed, over and over again. Furthermore, the three keyelements of the cycle are: oxygen, ozone, and the energy from the sun. The ultimate source of energy for our planet is the sun. This energytravels through space in the form of Electromagnetic Radiation. Furthermore,this electromagnetic radiation is often referred to as waves and their length,therefore, wavelengths. The sun has a wide range of wavelengths. This range isknown as the Electromagnetic Spectrum. In this spectrum there is Gamma,Ultraviolet, Visible, Infrared, and Radio waves. It is the ultraviolet (UV) radiation coming from the sun that drives theozone cycle in the stratosphere. When a oxygen molecule is hit by a high-energyUV ray, the O2 molecule absorbs the rays energy. As a result, the bond holdingthe oxygen molecule together breaks. This break separates the molecule, O2=O+O. These separate molecules quickly join with nearby oxygen molecules to form aozone molecule, O3=O2+O. Simultaneously, ozone molecules are being hit, theyabsorb the rays energy and break apart, leaving behind an oxygen molecule and asingle oxygen molecule, O3O2-O. At this time, the entire process repeatsitself making new molecules that are separated which combine to make newmolecules, over and again (Rowland and Molin 1991 p. 42). As a result of this cycle, about the same amount of ozone is produced asis broken down in the stratosphere. Therefore, the amount of ozone stays thesame under normal circumstances (Rowland and Molina 1991 p.43). A constant and stable ozone layer are important for life on earthbecause the high-energy UV rays that are absorbed in the ozone layer areextremely dangerous. These rays can kill some things while seriously damagingothers. For example, some bacteria exposed to UV rays will die. Plants, onland and in oceans, can be seriously damaged or even destroyed by UV rays. Whenhumans are exposed to the powerful rays, their skin can burn, damage to the eyes, and permanent changes in cells that can lead to cancer and other problems canoccur. By absorbing the UV rays, the ozone molecules in the ozone layer form ashield that protects life on earth from the dangerous and even deadly UV rays. Gaining the Respect of Others EssayIn the US there were 500,000 cases of the first, 100,.000 cases of the second,and 27,000 of the third type, in 1990(Wayne p. 47). Furthermore, cases ofmelanoma have been estimated to be increasing at an average of 10% from 1979 to1993 and even larger increases are believed to be occurring in the southernhemisphere. Also, studies suggest that a 1% decrease in stratospheric ozonewill result in a 2% increase of skin cancers (Wayne p.49). Moreover, some ofthese skin cancers can result in death. Malignant melanoma is much moredangerous, however, they are the least common. Malignant melanoma effects thepigment cell in the skin which can spread rapidly to the blood and lymphaticsystem. Furthermore, Wayne says, these have become increasingly frequentthroughout the world, especially in areas of higher latitudes. Moreover, thereis a correlation between melanomas and exposure to UV. Melanoma incidence iscorrelated with latitude, with twice as many deaths (re lative to statepopulation) in Florida or Texas as in Wisconsin or Montana(Wayne p.50). Furthermore, melanomas can take up too 20 years to develop, therefore, time willgive us a better example of the effects of increased UV rays have on the skin. The eyes are also affected by UV rays. An increase in UV rays results in an increase of UV absorption by theeye. Chronic UV exposure has been shown to be a factor in eye disease, saysRoach. Moreover, blindness from cataracts is the number one preventable causeof cataracts (Roach p.119). The latest findings indicate that for every 1%decrease in ozone levels results in a .6-.8% increase in eye cataracts, orannually approximately 100,000 to 150,000 additional cases of cataract-inducedblindness worldwide (Roach p.122-3). Moreover, UV rays cause other eye injures including photokeratitis, alsoknown as sun blindness or snow blindness, damage to the retina, and intraocularmelanoma tumors. Roachs predictions suggest a substantial future increase ineye cancer rates. However, some, object to the effects Cfcs have on the ozoneand on humans. Two of the more common objections are: Cfcs are two heavy to reach thestratosphere and we should not be concerned about Cfcs because the majority ofchlorine in the atmosphere is created by the acidification if salt spray. However, for the first objection, atmospheric gases do not segregate byweight in the troposphere and the stratosphere. This is because verticaltransport in the troposphere takes place by convection and turbulent mixing,says Wayne. Furthermore Wayne says, in the stratosphere and in the mesosphere,it takes place by eddy diffusion, the gradual mechanical mixing of gas bymotions on smaller scales, these mechanisms due not distinguish molecularmasses (Wayne Ch. 4). As for the second objection, it is an assumption that is not correct atall. Eighty percent of the chlorine found is from Cfcs and other man madeorganic chlorine compounds (Rowland 1989 p.77). In conclusion, despite the increasing list of negative affects of UVradiation, we continue to release ozone depleting chemicals into the atmosphere. Despite the availability of safer alternatives, we continue to promotetechnologies that are only slightly safer than the ones they replaced. Despiteall of the current information on the destructive affects of Cfcs, we stillcontinue to use them on a mass scale. Scientific research has only began to discover the impacts of UVradiation, however, what we do know should be enough for action. We cannotafford to sit around and wait for the damage to reach a point that makes usreact, by then it will be too late. The time to act is now because even with an immediate and complete endto production and release of ozone-depleting substances to the environment, weare still left with many decades of decreasing ozone and increased UV exposure. We must think long term and act now. Works CitedFarman, J.C., B.G. Gardiner, and J.D. Shankin. Large losses of total ozone inAntarticareveal seasonal CIOx/NOx interaction. Nature v.230 (Aug.4,1985): p.205-215. Roach, M. Sun Track. Health v.201 (May/June 1992): p.119-125. Rowland, F.S. Chloroflourocarbons and the depletion of stratospheric ozone.American Scientist v.128 (Nov. 4,1989): p. 70-78. Rowland, F.S. and M.J. Molina. Ozone depletion: 20 years after the alarm.ChemicalEngineering News v.20 (Jan.11,1994): p. 20-34. Rowland, F.S. and M.J. Molina. Chloroflourocarbons in the environment.Rev.Geophys. and Space Phys. v.7 (Mar.1975): p. 13-73Wayne, R.P. Chemistry of Atmosphere. New York: Oxford Univ.,1991.