Data Collection Essay Example for Free

Data Collection Essay * The Rough was excluded during the calculation of the mean as the rough was a trial to indicate the general whereabouts of the end point, which is inaccurate of the exact end point. Table 2. Observations collected during the experiment. Table contains observations which were recorded during each trial of the experiment. Trials Observations Before trials * When water was added to the crystals of oxalic acid, it dissolved almost instantly with a light stirring of the beaker. Rough * When two drops phenolphthalein was added to the solution of sodium hydroxide, the solution turned pink. * After adding about 20.8dm3 of oxalic acid into the sodium hydroxide solution, while swirling the conical flask, the solution turned completely clear the oxalic acid was filled up to 21dm3 to have a rounded rough end point to work with. 1 * When two drops of phenolphthalein was added to the sodium hydroxide solution, the solution turned pink. * After adding about 20dm3 of oxalic acid solution, while swirling the conical flask gently, each drop of oxalic acid solution began to turn the pink solution slightly clear. * After about 20.6dm3 oxalic acid solution was added, the pink solution turned completely clear. 2 * Two drops of phenolphthalein was added to sodium hydroxide solution, producing a pink coloured solution. * After about 20dm3 of oxalic acid solution was added, each drop began turning the pink solution slightly clear. * After adding around 20.4dm3 of oxalic acid solution, the pink solution turned completely clear. 3 * Two drops of phenolphthalein was added to the sodium hydroxide solution, turning the solution in the conical flask pink. * After adding about 20dm3 of oxalic acid solution, each drop began turning the pink solution slightly clear. * When about 20.3dm3 of the acid was added, the pink solution turned completely clear. Data Processing 1. Write an equation for the reaction. (COOH)2 + 2NaOH 2NaCO3 + 2H2O 2. What amount (in moles) of NaOH is present in 20.0 cm3 of 0.097 mol dm-3 sodium hydroxide solution? c = n/v c = 0.097mol dm-3 à ¯Ã‚ ¿Ã‚ ½0.001 = 0.097mols à ¯Ã‚ ¿Ã‚ ½ (0.001/0.097 x 100%) = 0.097mols dm-3 à ¯Ã‚ ¿Ã‚ ½1.03% v = 20.0cm3 à ¯Ã‚ ¿Ã‚ ½0.04 = (20.0/1000) à ¯Ã‚ ¿Ã‚ ½ (0.04/20.0 x 100%) = 0.020dm3 à ¯Ã‚ ¿Ã‚ ½0.2% n = ? n = c x v n = 0.097 à ¯Ã‚ ¿Ã‚ ½1.03% x 0.020 à ¯Ã‚ ¿Ã‚ ½0.2% n = 0.00194 à ¯Ã‚ ¿Ã‚ ½ (1.03 + 0.2)% ? n = 0.00194 mols à ¯Ã‚ ¿Ã‚ ½1.23% 3. What amount of oxalic acid was present in the average volume required to react exactly with the sodium hydroxide solution? Using the molar ratio of 1:2 for acid : base respectively: 0.00194 à ¯Ã‚ ¿Ã‚ ½1.23% / 2 = 0.00097 mols ? amount of oxalic acid present = 0.00097 mols à ¯Ã‚ ¿Ã‚ ½1.23% 4. What amount of oxalic acid was present in your 250 cm3 volumetric flask? Concentration of acid in 250mL is the same as the concentration of acid in 1L. Therefore the concentration of acid in 1 dm-3 of acid solution is the same as concentration of acid in 250mL: c = n/v c = 0.0119à ¯Ã‚ ¿Ã‚ ½2.03% / 0.25 à ¯Ã‚ ¿Ã‚ ½(0.15/250 x 100%) c = 0.0476 à ¯Ã‚ ¿Ã‚ ½ (2.03+0.06)% ? c = 0.05 mols dm-3 à ¯Ã‚ ¿Ã‚ ½2.09% (concentration of acid) c = n/v 0.05à ¯Ã‚ ¿Ã‚ ½2.09% = n / 0.25 à ¯Ã‚ ¿Ã‚ ½0.06% 0.05à ¯Ã‚ ¿Ã‚ ½2.09% x 0.25à ¯Ã‚ ¿Ã‚ ½0.06% = n ? n = 0.0125 à ¯Ã‚ ¿Ã‚ ½ (2.09 + 0.06)% ? moles of oxalic acid in 250mL solution = 0.0125 mols à ¯Ã‚ ¿Ã‚ ½2.15% 5. What is the mass of one mole of oxalic acid? n = m/MM MM = m/n MM = 1.5g à ¯Ã‚ ¿Ã‚ ½0.02 / 0.0125mols à ¯Ã‚ ¿Ã‚ ½2.15% MM = 1.5 à ¯Ã‚ ¿Ã‚ ½(0.02/1.5 x100%) / 0.0125à ¯Ã‚ ¿Ã‚ ½2.15% MM = 120 à ¯Ã‚ ¿Ã‚ ½(1.33+2.15)% MM = 120 à ¯Ã‚ ¿Ã‚ ½3.48% m = n x MM m = 1 x 120à ¯Ã‚ ¿Ã‚ ½3.48% ? mass of one mole of oxalic acid = 120g à ¯Ã‚ ¿Ã‚ ½3.48% 6. How many molecules of water of crystallisation are present in one mole? MM of (COOH)2 = 2(12.01 + 32 + 1) = 90.04 MM of H2O = (2.02 + 16) = 18.02 (COOH)2.xH2O = 120g à ¯Ã‚ ¿Ã‚ ½3.48% ? 90.04 + 18.02x = 120g à ¯Ã‚ ¿Ã‚ ½3.48% ? 18.02x = 120g à ¯Ã‚ ¿Ã‚ ½3.48% 90.04 ? 18.02x = 29.96à ¯Ã‚ ¿Ã‚ ½3.48% (/18.02) ? x = 1.6626à ¯Ã‚ ¿Ã‚ ½3.48% ? Molecules of water of crystallisation = 1.66à ¯Ã‚ ¿Ã‚ ½0.06 Conclusion and Evaluation Discussion 1. Estimate the degree of uncertainty in your readings using the balance, the volumetric flask, the pipette and the burette. How accurately can you quote your answer? Balance = à ¯Ã‚ ¿Ã‚ ½0.02g Volumetric flask = à ¯Ã‚ ¿Ã‚ ½0.15mL Pipette = à ¯Ã‚ ¿Ã‚ ½0.04cm3 Burette = à ¯Ã‚ ¿Ã‚ ½0.15cm3 The equipments used were relatively accurate as the uncertainties compared to the collected values are small. 2. Compare your answer with the correct answer and work out the percentage error. Percentage error = [(experimental value actual value) / actual value] x 100% = [(1.6626 à ¯Ã‚ ¿Ã‚ ½3.48% 2) / 2] x 100% = 16.87% à ¯Ã‚ ¿Ã‚ ½1.74% 3. Suggest any other reasons for possible error. Other reasons for possible error include the uncertainty of equipments, human errors and mistakes, possibility of contaminated solutions, air bubbles and transference of solution between equipments. This experiment was conducted to find the ratio of water in hydrate oxalic acid crystals. This included calculations of the theoretical and experimental values for the ratio of water in the hydrate oxalic acid crystals and the percentage errors of values compared. The equation for the reaction between the sodium hydroxide solution (NaOH) and the oxalic acid solution ((COOH)2) was worked out, with the product being a salt (NaCO3) and water (H2O). As the oxalic acid solution is a dibasic acid solution, the reaction ratio with sodium hydroxide is 1:2. The amount of NaOH, in moles, was also calculated by multiplying the concentration of the sodium hydroxide solution and the volume of sodium hydroxide solution used. The equation c = n/v was used to calculate this. The result was 0.00194 moles of NaOH in the sodium hydroxide solution with an uncertainty of à ¯Ã‚ ¿Ã‚ ½1.23%. The amount of oxalic acid presented in the average volume required to react exactly with the sodium hydroxide solution was also calculated; by dividing the moles of NaOH (0.00194à ¯Ã‚ ¿Ã‚ ½1.23%) by 2, based on the 1:2 reaction ratio stated before. The result was 0.00097 moles with an uncertainty of à ¯Ã‚ ¿Ã‚ ½1.23%. The amount of oxalic acid present in 250cm3 was also calculated. The concentration of acid in 250mL is the same as the concentration of acid in 1L, therefore, the concentration of acid in 1dm-3 of the oxalic acid solution is the same concentration as the acid in 250mL. With this understood, the equation c = n/v was used once again. The concentration was first calculated by dividing the moles of NaOH by 0.25dm3. The result (0.05mols dm-3 à ¯Ã‚ ¿Ã‚ ½2.09), was used in further calculations to determine the moles of oxalic acid by multiplying the previous calculated concentration (0.05mols dm-3 à ¯Ã‚ ¿Ã‚ ½2.09) with 0.25dm3, resulting in the moles of oxalic acid in the 250mL solution as 0.0125mols à ¯Ã‚ ¿Ã‚ ½2.15%. This value was used in the calculation of the mass of one mole of oxalic acid. The equation n = m/MM was used in this calculation. The MM (molar mass) was first calculated, dividing the mass of oxalic acid crystals by the moles of oxalic acid (1.5 / 0.0125). The mass (m = n x MM) was calculated with the result of this (1 x 120à ¯Ã‚ ¿Ã‚ ½3.48%), resulting in the mass of one mole of oxalic acid being 120à ¯Ã‚ ¿Ã‚ ½3.48%. Finally, the molecules of water of crystallisation presented in one mole were calculated. This was done by using the mass of one mole of oxalic acid (120à ¯Ã‚ ¿Ã‚ ½3.48%), subtracting the MM of (COOH)2 (90.04) from it and dividing the result by MM of H2O (18.02). The final result of the number of molecules of water in crystallisation equalled 1.66 with an uncertainty of à ¯Ã‚ ¿Ã‚ ½3.48% or 0.06. With this final result, the percentage error was calculated, being 16.87%à ¯Ã‚ ¿Ã‚ ½1.74%. All the uncertainties within the values used were calculated into percentage through dividing the uncertainty by the value and multiplying it by 100%. The uncertainties were converted into percentages before doing calculations were done. There were several limitations found during this experiment which would have been the cause of an inaccurate final result the variation between the theoretical value of 2 and the experimental value of 1.66à ¯Ã‚ ¿Ã‚ ½0.06. These limitations include the uncertainties of the equipment, human errors and mistakes, possibility of contaminated solutions, air bubbles found in solutions and the transference of solution between equipments. The significance of these errors and the improvements are listed in the table below. Limitations Significance Improvements Uncertainty of equipments Uncertainties were obtained during the experiment through the use of equipments. The inaccurate recording of data would have affected the results in the end. Eg. The readings on the electronic scale werent fully stable and consistent at one value, it varied increasing and decreasing slightly. In the case of the electronic scale, it was suggested that the variation in weight value was due to the air-conditioning blowing down on it. The air-conditioner could be turned off to reduce the uncertainties and variations. Students could also prevent themselves from breathing heavily down onto the scale while measuring, this could have contributed to the variation as well. Human errors and mistakes Mistakes could affect the outcome and accuracy of results. Eg. While adding water into the volumetric flask to dissolve the oxalic acid crystals, a student accidentally added a little too much, over the 250cm3 that was intended. This would have over diluted the oxalic acid. This could have been avoided through patience while adding the water into the volumetric flask. This could also have been done slowly and carefully, probably using a pipette towards the end at the 250cm3 mark. Reading the measurement of the pipette, burette and volumetric flask could have been inaccurate, causing results to be inaccurate and in turn affecting the calculations. Inaccuracy could have been due to improper way of reading the measurement. Students should have bent down slightly with the measurement at eye level. Student`s heads should not be tilted but level with the equipment as well. The measurement should also be read at the parallax, not above or below it. Possibility of contaminated solutions The experiment was conducted with the use of several different solutions. These solutions could have accidentally been mixed in with each other, causing the solution to be contaminated. The results obtained due to this could have been inaccurate, affecting the final results. Being careful with the solutions used would help avoid this. Using clean equipments for each different solution, making sure the solutions that are not meant to be placed together do not get mixed with each other. After the use of some of the equipments, they were to be washed and reused for another solution. The equipments were not dried before being used again; this could have diluted the solution and contaminated it. Drying the equipment each time after it is washed/cleaned would prevent access water and dilution of solutions. Air bubbles When transferring the dissolved oxalic acid into the burette, there were some tiny air bubbles. This would have because the measurement to be inaccurate as the air bubbles would have caused the reading of the solution to be greater than it actually is. Over time when the bubbles removed itself from the solution which would have caused a decrease in solution. The inaccurate measurement reading would have affected the final results of the experiment. The burette could have been left alone for awhile to allow the bubbles to float to the top. Whatever the amount the bubbles made up for, fill the burette up again with the use of a pipette. Transference of solution between equipments When transferring solutions between two or more differing equipments would have caused an increase of decrease in measurement. An inaccurate amount of solution would have affected the results or recorded data. When using a funnel during the transference of solution into the burette, it caused some increase in the desired amount. This is due to the tip of the funnel having some drops of solution left in it and when the funnel was removed, the movement could have caused those drops to drop into the burette, causing an increase in amount of solution. This could be prevented by either slowly removing the funnel or using the funnel up to a certain mark, remove it and fill up to the desired amount with the use of a small pipette drop by drop. When using the 20mL pipette to transfer the sodium hydroxide into the conical flask, the tip of the nozzle had a drop that was tempted to drop out of the pipette. Avoid touching the sides and move the pipette over the flask slowly would reduce the chances of it dripping out and altering the volume of solution. A small amount of the solution was also stuck at the tip of the nozzle after being emptied. By touching the tip to the side of the flask would help that tiny bit of solution flow out. If possible have the nozzle flat on the side of the flask, this would allow it to flow out smoothly. To avoid or reduce these significant errors, these solutions and improvements should be taken into consideration during future repetition of this experiment. The experiment overall was invalid. Though the values in data collection may have been to a 0.10cm3 difference, the final calculation of the percentage error, 16.87%à ¯Ã‚ ¿Ã‚ ½1.74%, was much greater than the desired 1% causing the experiment to be invalid.

Do Endogenic Processes Influence Global Climate Systems Environmental Sciences Essay

Do Endogenic Processes Influence Global Climate Systems Environmental Sciences Essay All processes that take place inside  Earth  (and other  planets) are considered endogenous. They make the  continents  migrate, push the  mountains  up, and trigger  earthquakes  and  volcanism. Endogenous processes are driven by the warmth that is produced in the core of Earth by  radioactivity  and  gravity. The geography and movement of tectonic plates is a key influence on global climate as it determines the form of the ocean basins, Patterns of heat ransfer in the oceans, large scale atmospheric circulation and the geometry of mountain chains. The movement and geometry of the lithospheric plates is a key long term influence on global climate and hea transfer and plae movements can be both vertical e.g the formation of the Himalayas and the Tibetan plateau or horizontal e.g sea floor spreading or the closing of the panama seaway and the development of the north atlantic gulf stream. Internal energy drives endogenic processes such as plate tectonics, volcanic activity, seismicity. The geography of the tectonic plates is a key influence on a global climate, this influences: the form and size of the ocean basins and land masses, patterns of heat transfer in the oceans thermohaline circulation, large scale atmospheric circulation and vertical heat exchange, the location and elevation of mountain chains and plateaus, the amount of elevated crust. The formation of the Himalayas and the Tibetan plateau that began 52 to 44ma key events that led to a step change in the climate system and long term global cooling. Horizontal crustal movement the closing of the panama seaway around 4 ma and the development of the north atlantic gulf stream taking warm water to higher latitudes a key factor in the formation of ice sheets in the northern hemisphere. The closing of the panama seaway around 4ma and the development of the north atlantic gulf stream taking warm water to higher latitudes. The movement and geometry of the lithospheric plates is a key longterm influence on global climate and heat transfer, vertical crustal movements are most rapid at plate boundaries and we will be exploring their potential impact on weathering rates and carbon cycle. Location and elevation of mountain chains and high plateau landscapes across the earths surface is a key influence on climate over a range of timescales. The essay is about the last 65 million years, so the Big Bang theory is not really relevant. You need a nice range of examples to show how endogenic processes can influence global climate (long and short term). We covered some in the lectures (i.e. vertical and horizonatal crustal movements). We did not really look at volcanic processes, but you need to mention them too (short and longterm impacts) we mentioned other controls too (not related to endogenic processes) so you can mention them briefly to round things off. When Mount Pinatubo erupted in the Philippines June 15, 1991, an estimated 20 million tons of sulfur dioxide and ash particles blasted more than 12 miles (20 km) high into the atmosphere. The eruption caused widespread destruction and loss of human life. Gases and solids injected into the stratosphere circled the globe for three weeks. Volcanic eruptions of this magnitude can impact global climate, reducing the amount of solar radiation reaching the Earths surface, lowering temperatures in the troposphere, and changing atmospheric circulation patterns. The extent to which this occurs is an ongoing debate.  Large-scale volcanic activity may last only a few days, but the massive outpouring of gases and ash can influence climate patterns for years. Sulfuric gases convert to sulfate aerosols, sub-micron droplets containing about 75 percent sulfuric acid. Following eruptions, these aerosol particles can linger as long as three to four years in the stratosphere. Major eruptions alter the Earths radiative balance because volcanic aerosol clouds absorb terrestrial radiation, and scatter a significant amount of the incoming solar radiation, an effect known as radiative forcing that can last from two to three years following a volcanic eruption. Volcanic eruptions cause short-term climate changes and contribute to natural climate variability, says Georgiy Stenchikov, a research professor with the Department of Environmental Sciences at Rutgers University. Exploring effects of volcanic eruption allows us to better understand important physical mechanisms in the climate system that are initiated by volcanic forcing. Stenchikov and Professor Alan Robock of Rutgers University with Hans Graf and Ingo Kirchner of the Max Planck Institute for Meteorology performed a series of climate simulations that combined volcanic aerosol observations from the Stratospheric Aerosol and Gas Experiment II (SAGE II) available from the Langley DAAC, with Upper Atmosphere Research Satellite (UARS) data from the Goddard Space Flight Center DAAC. The research team ran a general circulation model developed at the Max Planck Institute with and without Pinatubo aerosols for the two years following the Pinatubo eruption. To study the sensitivity of climate response to sea surface temperature, using data from the NASA Jet Propulsion Laboratory DAAC, they conducted calculations with climatologically mean sea surface temperature, as well as with those observed during particular El Nià ±o and La Nià ±a periods. By comparing the climate simulations from the Pinatubo eruption, with and without aerosols, the researchers found that the climate model calculated a general cooling of the global troposphere, but yielded a clear winter warming pattern of surface air temperature over Northern Hemisphere continents. The temperature of the tropical lower stratosphere increased by 4 Kelvin (4 °C) because of aerosol absorption of terrestrial longwave and solar near-infrared radiation. The model demonstrated that the direct radiative effect of volcanic aerosols causes general stratospheric heating and tropospheric cooling, with a tropospheric warming pattern in the winter. The modeled temperature change is consistent with the temperature anomalies observed after the eruption, Stenchikov says. The pattern of winter warming following the volcanic eruption is practically identical to a pattern of winter surface temperature change caused by global warming. It shows that volcanic aerosols force fundamental climate mechanisms that play an important role in the global change process. This temperature pattern is consistent with the existence of a strong phase of the Arctic Oscillation, a natural pattern of circulation in which atmospheric pressure at polar and middle latitudes fluctuates, bringing higher-than-normal pressure over the polar region and lower-than-normal pressure at about 45 degrees north latitude. It is forced by the aerosol radiative effect, and circulation in winter is stronger than the aerosol radiative cooling that dominates in summer. Man-made, or anthropogenic emissions can make the consequences of volcanic eruptions on the global climate system more severe, Stenchikov says. For instance, chlorofluorocarbons (CFCs) in the atmosphere start a chain of chemical reactions on aerosol surfaces that destroy ozone molecules in the mid-latitude stratosphere, intensifying observed stratospheric ozone depletion. While we have no observations, the 1963 Agung eruption on the island of Bali probably did not deplete ozone as there was little atmospheric chlorine in the stratosphere. In 1991 after the Pinatubo eruption, when the amount of CFCs in the stratosphere increased, the ozone content in the mid-latitudes decreased by 5 percent to 8 percent, affecting highly populated regions, says Stenchikov. NASA and the National Science Foundation have funded Robock and Stenchikov to study the Pinatubo eruption in more detail, and to conduct another model comparison with the volcanic aerosol data set. They plan to combine SAGE II data with available lidar and satellite data from various DAACs to improve their existing data set. By understanding the impact of large volcanic eruptions on Earths climate system in more detail, perhaps scientists will be in a better position to suggest measures to lessen their effects on people and natural resources. Both technological change and economic growth are seen as major determinants of future global energy demand levels, the associated carbon dioxide (CO2) emissions, and global climate impacts Until recently, however, the modelling of energy-economy-climate interactions has largely regarded technological progress as an exogenous process, rather than as endogenous technological change. Energy Economics Volume 24, Issue 1, January 2002, Pages 1-19 a momentary glance at a map of the world today to realise that the disposition of the continents has a marked effect on both local and global climate. Not the least of these effects results from the difference in the thermal properties of land versus ocean a continental region will be colder in winter and warmer in summer than an oceanic region at any given latitude. Moreover mountain belts formed as a consequence of plate tectonic activity dramatically modify rainfall through the effects of  orography   the development of a rain shadow on the leeward side of mountain belts. Global climate is also strongly controlled by ocean currents. For example, northwestern Europe is significantly warmer than other regions at similar latitudes because of the warming effects of the Gulf Stream and North Atlantic Drift. The reversal of oceanic currents in the equatorial Pacific a phenomenon known as El Nià ±o has a far-reaching effect on climate around the Pacific. Ocean currents depend on the geometry of the oceans and this is controlled by plate tectonics. Hence, over geological timescales the movement of plates and continents has a profound effect on the distribution of land masses, mountain ranges and the connectivity of the oceans. As a consequence, plate tectonics has a very direct and fundamental influence on global climate. http://openlearn.open.ac.uk/mod/resource/view.php?id=172207 The climate of modern Antarctica is extreme. Located over the South Pole and in total darkness for six months of the year, the continent is covered by glacial ice to depths in excess of 3 km in places. Yet this has not always been the case. 50 Ma ago, even though Antarctica was in more or less the same position over the pole, the climate was much more temperate there were no glaciers and the continent was covered with lush vegetation and forests. So how did this extreme change come about? The modern climate of Antarctica depends upon its complete isolation from the rest of the planet as a consequence of the Antarctic Circumpolar Current that completely encircles Antarctica and gives rise to the stormy region of the Southern Ocean known as the roaring forties. The onset of this current is related to the opening of seaways between obstructing continents. Antarctica and South America were once joined together as part of Gondwana and were the last parts of this original supercontinent to separate. By reconstructing continental positions from magnetic and other features of the sea floor in this region, geologists have shown that the Drake Passage opened in three phases between 50 Ma and 20 Ma, as illustrated in Figure 32. At 50 Ma there was possibly a shallow seaway between Antarctica and South America, but both continents were moving together. At 34 Ma the seaway was still narrow, but differential movement between the Antarctic and South American Plates created a deeper c hannel between the two continents that began to allow deep ocean water to circulate around the continent. Finally, at 20 Ma there was a major shift in local plate boundaries that allowed the rapid development of a deep-water channel between the two continental masses. The coincidence of the change in motion of the Pacific Plate with changes in plate motions between S. America and Antarctica shows how the motions of all the plates are interconnected a change in the true motion of one plate leads to changes in the true motions of many others. While these plate motions were taking place the effect on Antarctica was profound. By 34 Ma the climate cooled from the temperate conditions that previously existed. This was sufficient for glaciers to begin their advance, and was followed by a period of continued cooling until at about 20 Ma, glaciation was complete. Even though the Drake Passage first opened at 50 Ma it was not until it opened to deep water at 34 Ma that glaciation really took hold Today, the Antarctic Circumpolar Current is the strongest deep ocean current and its strength is responsible for the icehouse climate that grips the planet. The opening of the Drake Passage had both a local and a global effect, initially cooling the climate of Antarctica from temperate to cold and ultimately playing an important role in the change from global greenhouse conditions 50 Ma ago to the global icehouse of today. This example shows how plate tectonics, continental drift and the opening and closing of seaways can have a profound influence on both local and global climate. Throughout the Phanerozoic there were long periods when the Earth was much warmer than today often called a greenhouse climate and other times when it was cold called an icehouse climate. These cycles, like the Wilson cycle, occur over periods of 100 Ma, reflecting the timescale of plate movements and the growth and destruction of oceans. Given the clear link between ocean circulation and climate, and the similar timescales of global climate change and plate motions, it is inescapable that one of the chief controls on long-term changes in the global climate must be plate tectonics. Every two to seven years a climatic disturbance brings floods to California, droughts to Australia, and famine to Africa . Known as El Nino, it is essentially a warming of surface waters in the eastern Pacific near the equator. Although scientists understand the mechanics of El Nino, its origins have yet to be determined. Most believe that the interaction between the atmosphere and the sea somehow generates this climatic disturbance that wreaks havoc upon those regions of the world that lie in its path. But now a new theory on the origins of El Nino has been proposed and, surprisingly, it has very little to do with the atmosphere or the sea. The new theory suggests that the primary mover behind El Nino is hot magma welling up between tectonic plates on the Pacific sea-floor. The upwelling magma heats the overlying waters enough to affect the ocean surface, initiating the cascade of events that brings on the wrath of El Nino. Volcanic Ash Eruptions, like that pictured above, throw tons of ash into the atmosphere, and have short term affects of the climate. If the eruption is potent enough, the ash will stop some of the shortwave radiation coming in from the Sun. This, in turn, will lead to a decrease in the global temperature. The reason for this is that the shortwave radiation that comes in from the Sun and reaches the Earths surface, gets absorbed in the the Earth. About 4 to 6 hours later, the Earth reradiates that energy in the form of longwave radiation. This is where the temperature comes from. So if some of the sunlight is shut off, then this will lead to a decrease the global temperature. With the eruption of Mount Pinatubo in June 1991 (image above), about 22 million tons of ash was thrown into the atmosphere. This was enough to block a fraction of the sunlight from reaching the Earths surface, which cooled the global temperature on Earth by as much as 0.5 degrees C. The most powerful eruption in recorded his tory, the eruption of the Tambora Volcano in Indonesia in April of 1815, threw up so much ash that the global temperature on Earth fell by as much as 3 degrees C. Europe and North America know this time as the year without a summer. The volcanic ash does not keep the temperatures down for a very long period of time geologically speaking, so its impacts are on a short term basis. Rain-Shadow Effect The long term impacts of volcanoes come from a look at simple geography. Volcanoes are gigantic mountains, so their affect on climate is the same as a normal mountain. This leads to the rain-shadow effect (explained in the  Continental Movement  section), which comes into play with volcanoes just as it does with mountain building. Until that volcano can be eroded away, it will continue to have some sort of impact on climate. This can last for thousands of years. Volcanoes have quite a bit of affect on climate. And this affect can be rather short term (volcanic ash) or long term (rain-shadow effect) in nature. Again biology can be affected by this too. For example, a desert area may quickly develop on the leeward side of a new volcano. If life is not able to adjust, extinction will become a significant threat. http://www.djburnette.com/projects/volcanoes.html

Comparing Half Caste and Search for my Tongue Essay examples -- John A

Comparing Half Caste and Search for my Tongue Culture. It’s a very complicated term, with many different interpretations, but what does it actually mean? In this essay I will compare two poems from completely different cultures to see if we get any comparisons, the poems I have chosen to write about are Half-Caste by John Agard and Search for my Tongue by Sujata Bhatt, I have chosen these because I feel they raise some very significant points. But back to the question mentioned earlier, what is culture? Everyone has a different view on culture, but to me it is a huge influence on our everyday lives, many different issues contribute to the term ‘Culture’ from the way we dress, to our beliefs, attributes, how we live, and even what we eat. It affects us all differently depending on how we understand it, for example, if we were to believe that culture was just a religious matter we would only be affected by what that religion tells us, whereas if we were to believe that culture was a whole way of life we would be affected in a completely different way. Culture is important to us all, regardless of how we feel about it, it gives us a guide to our lives and shows us some boundaries; it can also give us advice and help us to be a better person. The word ‘different’ can be used in two contexts; we can say it both complimentarily and offensively, my understanding of this is that some people are afraid of what’s different and therefore have to make comments to feel safe. But when we say ‘different’ cultures we are referring to the way other people live, and if we are afraid of this we must all seriously reconsider ourselves. As I have already mentioned one of the poems I will be studying is Half-Caste by John ... ... the end of the poem though she seems to have won the fight. In conclusion, everyone looks upon culture differently; there are those who take it seriously and those that don’t. But whether or not we like it we are all part of a culture and should therefore respect other’s. Of course culture can be seen as something to fight with, there are so many people in the world with different views it would be surprising if it wasn’t! In my opinion both authors use language as something to fight with and against in their own unique ways. Both of these poems use some sort of violence to get a message across, this to me is a type of fighting, so the answer to my question is ‘YES’ we could see culture as something to fight with or against because of the language both poems use, for instance the taunting that John Agard uses and the metaphors that Sujata Bhatt uses.

Hermann Hesse: A Classic Take on the Modern Age Essay -- Biography Bio

Hermann Hesse: A Classic Take on the Modern Age Hermann Hesse, writing in the twentieth century, extolled many of the virtues of the past. His unique style, dependent upon German Romanticism, adapted the issues of the modern age. Using subject matter from various sources, Hesse built fictional worlds that mirrored reality. In the novel Siddhartha, Hesse deals specifically with the spiritual quest. Although writing about the spiritual landscape of India, this work addresses the desire for meaning that the entire world felt after the events of World War I. Born in Germany in 1877, Hesse would live through the complete change in existence that occurred in the twentieth century. Coming from a family of devout Protestants, Hesse had been exposed to the traditional Christian existence. He began to write while still in his teens. A lifelong pacifist, Hesse would continue to fight against the violence of his age. The works of Hesse were always tinged with the notion of the outsider (The Steppenwolf) or the search for meaning (Siddhartha). Utilizing a higher artistic style than many of his colleagues, Hesse acknowledged Romanticism in his work. His subject matter could be highly simple in the case of Gertrude or extremely complex like Magister Ludi:The Glass Bead Game, for which he would win the Noble Prize in the year 1946. Until his death in 1962, Hesse would struggle to find meaning in the horrible events in his lifetime. Although Hesse concerns himself with the same issues of isolation and meaninglessness that Franz Kafka addresses, he utilizes a poetic writing style to bring out the beauty of his subject. The lofty style helps "with the construction of an ideal as an escape from his emotional crisis of the war years" (Ziolk... ...ction of the previous paths. Humanity could no longer be content with religion or with consumer needs. A spiritual truth had to be found, but it would require a long journey and many failures along the way. Mankind could learn as much about the beliefs of the past in order to discover "the condition of the present world and a revelation of the relationship of all things to one another" (Ziolkowski 154), the lesson that all things are interconnected. All of the past, present and future are inextricably linked as part of a continuous flow. Works Cited Freedman, Ralph. Hermann Hesse: Pilgrim of Crisis. New York: Pantheon Books, 1978. Hesse, Hermann. Siddhartha. New York: New Directions Publishing Corporation And Bantam Books, 1951. Ziolkowski, Theodore. The Novels of Hermann Hesse: A Study in Theme and Structure. Princeton: Princeton University Press, 1965.

Deontology: Ethics and Kant Essay

In our world today it is often hard to genuinely decide what in fact is right or wrong. The reason that it is so tough to determine is because of our human nature given everyone has their own opinion. We do not all think the same or think the same actions and consequences have the same effect. It is this reason we analyze situations with ethical theories, such as that of Kant’s deontology. Kant’s theory in its own right has a strong moral foundation in which it seems understandable to decide what is right or wrong. However it has its weakness as well. To me however, I believe Kant’s theory on deontology offers a sound premise for which to determine what is morally right or wrong. Kant’s theory on deontology is a way of assessing one’s actions. One’s actions are either right or wrong in themselves. To determine if actions are right or wrong we do not look at the outcome in deontology. Instead Kant wants us to look at the way one thinks when they are making choices. Kant believes that we have certain moral duties in regards to one’s actions. It is our moral duty that motivates ones to act. Theses actions are driven either by reason or the desire for happiness. Since happiness is differs from person to person, it is conditional. Reason on the other hand is universal and can be applied to all making it unconditional. In Kant’s theory on deontology, actions are either intrinsically right or wrong, which is based largely on reason. Kant says that it is in virtue of being a rational being that we as humans have the capacity to be moral beings. Also that moral law amounts to one’s duty. Kant says duty is grounded in a supreme rational principle, thus it has the form of an imperative. To determine what actions one should take Kant utilized imperatives. Imperatives are a form of instructions that will guide an individual on what one should do. Kant had two classifications between imperatives, hypothetical and categorical. Hypothetical imperatives can apply to one who aspires for a desired outcome. These imperatives allow one to take an action for the method of obtaining a certain outcome, meaning if one has a desired outcome, then they ought to act. Kant has divided hypothetical imperatives into two subcategories, the imperatives of skill and imperatives of prudence. The imperatives of skill are imperatives that lead to an action in which the end result desired would be anything other than happiness. The imperatives of prudence are imperatives that lead one to actions, where the desired outcome is happiness. Kant believes that morality however is not like this. Morality does not tell one how to act in order to achieve a goal. Instead morality is made up of categorical imperatives. Kant taught that morality is universal, meaning it could be applied to all and moral law must be obeyed. He believed that when we act we are using moral law and act on the maxims, or the universal rules, of our actions. Kant’s categorical imperative states one can â€Å"act only on that maxim through which you can at the same time will that it should become universal law. † Kant’s uses categorical imperative commands one to take an action. Before one can act they must analyze the principle on which they are acting. Once they have determined why they are acting, it may no longer be ideal, then it is wrong for one to use that maxim as a basis for taking that action. Kant’s principle of morality is the categorical imperative. This means that as an imperative it is a command and being categorical the command has its whole worth with in itself. The categorical imperative doesn’t have some proposed end as in a hypothetical situation, it has its own rational necessity in its justification. Kant’s principle of morality is essential to â€Å"good will. † This is a will that acts for the sake of duty. It is the only thing that is good without qualification. Thus a good will cannot be made better or worse by the result it produces. Good will is also the basis for a major part of Kant’s theory and that is the Universal Law Formula, which is the basis in which Kant uses to determine whether or not things are morally right or wrong. This formula states that one should act in such a way that your maxim could become a universal law of nature. That is if you took your belief or ideal and applied it to the entire world would it hold true and not contradict itself. Kant’s categorical imperative has two formulations included within it, one being the Formula of Universal Law and the other being the Formula of Humanity. The second formulation, The Formula of Humanity, is a principle under the Formula of Universal Law. Kant’s defines the Formula of Humanity as â€Å"Act in such a way that you always treat humanity, whether in your own person or in the person of any other, never simply as a means, but always at the same time as an end. † This formulation states that one’s actions are immoral if it is using a person as a means to an end. It also has to be understood that Kant’s ideals greatly fall on a matter of agency, whether or not you are in fact the one willing an action that causes a negative outcome even if you did so now the result of that action would do more good. Because you took action you are the agent that caused a negative outcome. The proposed â€Å"better† outcome has no value towards the morality of your action. Kant’s strengths in his theory are that they can be applied to nature as a whole, thus the universal law formula. His theory doesn’t depend on an individual’s virtues or character. His weakness is that his morality is based on one’s personal action and doesn’t take in to account the outlying consequences that could ultimately benefit from that action. With Kant’s theory I believe we can make a more sound argument as an approach to ethics. With Kant we have to take situations and become very specific with them. We focus on what the action is and universalize it. That way no matter where in the world it can apply to everyone and won’t contradict itself. Then and only then we decided if it is morally right. Also Kant’s theory is good because it leave no grey area with its matter of agency. It doesn’t let possibilities of better or worse consequences affect the morality of the action in question. Thus I believe in all Kant has a more promising approach for ethics.

Mexico: the Yucatan Peninsula

Mexico: The Yucatan Peninsula The Yucatan Peninsula is located in southeastern Mexico, which separates the Caribbean Sea from the Gulf of Mexico, on the northern coastline on the Yucatan Channel. The Yucatan Peninsula lies east of the Isthmus of Tehuantepec, a northwestern geographic divider separating the region of Central America from the rest of North America. The Yucatan Peninsula comprises of the Mexican states of Yucatan, Campeche, and Quintana Roo; the northern part Belize; and Guatemala's northern subdivision of El Peten. Geology The peninsula is the exposed part of the large Yucatan Platform. The Yucatan Peninsula is an unconfined flat lying erosion landscape. Sinkholes, locally called cenotes are widespread in the northern lowlands. According to the Alvarez hypothesis, the mass extinction of the dinosaurs at the transition from the Cretaceous (K) to the Tertiary (T) Periods (the K-T Boundary) 65 million years ago was caused by an asteroid impact somewhere in the Caribbean Basin. The deeply buried Chicxulub Crater is centered off the north coast of the peninsula near the town of Chicxulub. The now-famous â€Å"Ring of Cenotes† outlines one of the shock-waves from this impact event in the rock of ~65 millions years of age, The presence of the crater has been determined first on the surface from the Ring of Cenotes, but also by geophysical methods, and direct drilling with recovery of the drill cores. Water resources Due to the extreme erosion nature of the whole peninsula, the northern half barely consists of any rivers. Where lakes and swamps are present, the water is marshy and is not suitable for drinking water. The thousands of sinkholes, locally called Cenotes throughout the region provide access to the groundwater system, and the cenotes have long been relied on by ancient and contemporary Mayan people. Vegetation The short and tall tropical jungles are the predominant natural vegetation types of the Yucatan Peninsula. The boundaries between northern Guatemala (El Peten), Mexico (Campeche and Quintana Roo), and western Belize are still occupied by the largest continuous tracts of tropical rainforest in Central America. However, these forests are suffering extensive deforestation. Etymology There is a popular myth that the name Yucatan comes from the Yucatec Maya phrase for â€Å"listen how they speak,† or â€Å"I don't understand your words† — supposedly said by contact period Maya, when the first Spanish explorers asked, what the area was called. The proper derivation of the word Yucatan is widely debated. However, it is also claimed that the actual source of the name â€Å"Yucatan† is the Nahuatl (Aztec) word Yokatlan, â€Å"place of richness. † People The Yucatan Peninsula comprises a significant proportion of the ancient Maya Lowlands. There are many Mayan archaeological sites throughout the peninsula; some of the better-known sites are in Chichen Itza, Tulum and Uxmal. Indigenous Mayans and Mestizos of partial Mayan descent still make up a sizable portion of the region's population, and Mayan languages are still widely spoken there. Economy In the late historic and early modern eras, the Yucatan Peninsula was largely a cattle ranching, logging, chicle and henequen production area. Since the 1970’s, the Yucatan Peninsula has fixed its economy towards tourism, especially in the Mexican state of Quintana Roo. Once a small fishing village, Cancun in the northeast of the peninsula has grown into a thriving city. The Riviera Maya, which stretches along the east coast of the peninsula between Cancun and Tulum, houses over 50,000 beds and is visited by millions of tourists every year. The best-known locations are the former fishing town of Playa del Carmen, the ecological parks Xcaret and Xel-Ha and the Mayan ruins of Tulum and Coba. Climate Like much of the Caribbean, the Yucatan Peninsula lies within the Atlantic Hurricane Belt, and with its almost uniformly flat terrain, it is vulnerable to these large storms coming from the east. The 2005 Atlantic Hurricane Season was a particularly bad season for Mexico's tourism industry, with two forceful category 5 storms hitting, Hurricane Emily and Hurricane Wilma. The 2006 Atlantic Hurricane Season was a typical year which left the Yucatan untouched, but in the 2007 Atlantic Hurricane Season Yucatan was hit by the Hurricane Dean (which is also a category 5 storm); nevertheless Hurricane Dean left little damage on the peninsula despite heavy localized flooding. Strong storms called nortes can quickly descend on the Yucatan Peninsula any time of year. Although these storms pummel the area with heavy rains and high winds, they tend to be short-lived, clearing after about an hour. The average percentage of days with rain per month ranges from a monthly low of 7% in April to a high of 25% in October. Breezes can have a cooling effect; humidity is generally high, particularly in the remaining rainforest areas. Bibliography â€Å"Beautiful Underground Lakes & Rivers. † Wonderfulinfo. com. 5 January 2010. http://www. wonderfulinfo. com/photos/underground/ â€Å"Climate and Weather of Mexico. † yahoo. answers. com. 26 Sept 2009. http://answers. yahoo. com/question/index? qid=20090419162859AAZ2D7m&. crumb=eYF8u9vJN5s â€Å"Mapas de Mexico. † Mexicoadventourist. com. 5 January 2010. http://www. mexicoadventourist. com/Mapas/YucatanMap. jpg â€Å"Mexico’s Government. † Viva Mexico. 2 October 2009. http://staff. esuhsd. org/balochie/studentprojects/mexico/MexGovernment. html Parfit, Michael, â€Å"Yucatan Peninsula,† National Geographic. Aug 1996. 108-113. â€Å"Sunset over the Yucatan. † flickr. com/photos/afagen/. 5 January 2010. http://www. flickr. com/photos/afagen/2262221520/ The World And Its People. â€Å"Mexico – The Land Yucatan†. New York. Greystone Press. 1964. 34-35. â€Å"The World Factbook – Mexico. † CIA the World Factbook, 10 Sept 2009. ttp://www. cia. gov/library/publications/the-world-factbook/geos/countrytemplate_mx. html â€Å"Yucatani iguanaleso naplo. † atjeffs. blog. hu/2008. 5 January 2010. http://m. blog. hu/at/atjeffs/image/Yucatan_peninsula_250m. jpg â€Å"Yucatan Sunset. † flickr. com/photos/bjkresearch/. 5 January 2010. http://www. flickr. com/photos/bjkresearch/183792616/ â€Å"Yucatan Peninsula Sunset. † flickr. com/photos/kevmac66/. 5 January 2010. http://www. flickr. com/photos/kevmac66/3495944443/ â€Å"Yucatan Peninsula Resort. † Alwaysonvacation. com. 5 January 2010. http://www. a lwaysonvacation. com/LSS/images/29225/YucatanPeninsula3BedroomsSle

The Importance Of Effective Induction Is Explained Business Essay - Free Essay Example

Sample details Pages: 7 Words: 1976 Downloads: 9 Date added: 2017/06/26 Category Business Essay Type Research paper Did you like this example? UBA is a large financial service provider in Nigeria with subsidiaries in 20 sub-Sahara countries including Nigeria plus new York, with it offers services to over 7 million customers across 750 branches and today UBA is the third in the fifth largest bank in Nigeria an average breach has not less than 30 employee. My job role as an assistant human resource manager trainee is to assist the head the head human resource manager in recruiting, assessment of staff, carry out induction of new staff, as a pay roll manager, manage employment relationships and with approval from the head manager apply disciplinary actions. Description of the Problem The problem I am meant to solve here involves recruitment, selection and induction of new employee. The organizational policies serves as a guides for the first line manager in recruitment and selection of new employees and the type of induction to be carried out for the new employee and to show how important the induction process is for the new employee and it benefits to the organization as a whole and also the problem of collecting feedback as to be considered in this essay Don’t waste time! Our writers will create an original "The Importance Of Effective Induction Is Explained Business Essay" essay for you Create order Analysis of the Problem The issue of the best methods of recruitment ,selection and induction cannot be over emphasized as different organizations are constantly looking for different method that best solve this problem and this is done in order make the new employee comfortable and have a sense of belonging in the organization and therefore lead growth of the organization. Taking a special brand of UBA called the UBA prestige (where I work) as a case study being a growing arm of UBA which is meant for the elites, therefore charged with bulk cash transactions. A typical case reaches the manager that there has been much pressure on the front desk cashiers because of the large sums of deposit and withdrawal and at the same time carrying out other foreign/ local fund transaction and therefore it takes longer time in attending to the long cue of customers, this means that the standard turnaround time of 5 minute per customer cannot be met and therefore putting much pressure on the employees and making them demotivated the result of this is dissatisfied staff and customers. This is a serious problem considering the reputation of the organization and considering the competition out there should in case the customer decides to go to other banks and also the welfare of staff has to be taken into consideration. Resolutions of the Problem After considering the problem as the assistant human resource manager trainee my surjection will be to create another position and recruit staff called BULK CASHIER/TELLERS to carry out this duties and in order to do this I have to consider some topic/heading that will show how this proses will be carried out. The organisations policies and procedures that could guide the first line manager in recruitment, selection and induction are identified The organizational policies that can guide in the recruitment, selection, induction process can either be the formal or informal methods depending on the size of your business For a small sized company one can carry out these procedures by referrers while in the large organizations like United Bank of Africa the INFORMAL process is used and this processes are Identifying that there are vacancies to be filled Agreeing that the vacancies need to be filled Analyse the job, Prepare job description, Prepare person specification. Get authorization from the superior officer/personnel Attract applicant by averting on the media e.g. Newspaper, website, TV, radio. After collecting application ,going through them, then you SHORTLIST candidates Prepare and carry out interviews With the interviewees performance make the final selections. Prepare and carry out INDUCTION for the new employee A job analysis is conducted and a job description and person specification for a post within own area of responsibility In order to answer this question I will use the Banking system and the cash department as an example, United Bank of Africa is a very big organization with huge numbers of customers, having just four cashier that attend to thousands of customer daily for cash ,cheque, and other fund transfer transactions and are expected to meet up to the maximal five minute turnaround time (TAT) per customer, it has been noticed that the work load is too much for just four cashiers, so we need to recrui t and some steps must be followed. JOB ANALYSIS Does a vacancy really exist YES What is the nature of job Bulk cash collection and posting What is the purpose of the post to make job easier in order to increase customer satisfaction. What are the performance satisfaction we are looking for the person must have the basic arithmetics and computer knowledge, must be fast in typing, should be able to work under pressure. What is the contribution of the post to the organization employee wellness and motivation increase, better customer satisfaction, more business for the organization, What happens when the post is not created = depreciation in employees wellness and efficiency, loss of businesses. Will the post continue to exist yes JOB DESCRIPTION JOB TITLE -Bulk cashier REPORTING TO -Cash officer/ head cashier FUNTION -Attending to every bulk cash transactions DUTIES -Operate and set the counting machine, collection and posting of bulk cash, issue out deposit slips to customers, movement of cash into the vault. WORK CONDITION -Constantly unconducive with a temperature below recommended work environments. PERSONNEL SPECIFICATION STANDARD OF EDUCATION Must have at list an OND or NCE in any social science course or any relevant courses ABILITY TO COMMUNICATE -Should have good command of English, Spoken Written. APPEARANCE The person should look good and smart all the time. SOCIAL SKILL The person should be appreciably computer literate. The way that you would prepare for selection interviews to ensure impartiality and optimum decision making in selecting the most suitable applicant is explained This can be done by Preparing questions that will be use during the interview and applying same to all candidate Setting up a venue and making sure its conducive Selecting or shortlisting the successful candidate by application or cv Having a list of what to access By not using clauses that is illegal or discriminatory in the job advert Stating clearly the qualification, experience and qualities the candidate should possess A recognised selection technique that could be used during interviews is explained Introduction and opening remark Asking direct questions to confirm facts stated in the application Asking the interviewee an open ended question in order to know more about the interviewee and to give him/her an opportunity to express themselves Testing candidates on the skill specified o the job Administering personality test on the candidates to see which candidate possesses the right attribute for the job Rounding of the interview by summarizing the position and stating what the next step is. Verifying the candidates resume by calling the referees The induction process On taking up a new appointment, irrespective of whether an employee has previous service within the same organization, the new employee should be advised of the full requirements of his or her post and given any other relevant information which will enable him or her to settle in quickly and become effective. Appropriate induction should be provided for each new employee, and the progress of a probationary employee should normally be reviewed no later than halfway through the probationary period. Overall responsibility for planning an individuals induction should lie with one person, and this will usually be their line manager, although induction of new staff members will normally include contributions from a range of people like older employees and the induction can also be done by having a general seminal and also by printing out hand books to assist the new employee. The importance of effective induction is explained An induction is important in the sense that in the process the employee gets to know the organizations aims objectives. During the induction process the employees job function is described to the employee and this will make the employee more effective and not confuse This will put the employee at ease, by familiarizing them with the other employees and their next line manager, so there is no confusion as to who they are answerable to During the induction process the employee is also introduced to the work area and other departments. A properly done induction can also reduce the need for supervision since all employees knows what their jobs are. A proper induction gives the new employee a sense of belonging It makes the new employee aware of the company rules and norms It makes the job easier for the new employee and gives proper familiarization with the job and therefore not confused. It keeps the new employee away from breaking the company rules unknowingly . The phases of induction in the organisation are described Induction is done by giving out GENERAL INFORMATION this is relating to the organization, including values and philosophy as well as structure and history, services, trade union. INFORMATION ABOUT THE JOB this is relating to the roles that the new employee will be performing e.g. work schedules, time sheet, payment, job description, use of office equipments etc. HEALTH SAFETY INFORMATION- This is related to health and safety and other essentials e.g. emergency procedures, location of first aid and how to use them and if the job requires special clothing and accessories like overall safety hard hats and boots etc. INFORMATION ABOUT RULES this relates to the rules if the organization, all terms and condition of the employment and also information concerning payment and salaries etc. The legal and practical aspects of health and safety that should be included in the organisations induction process is are described This is describe as those health and safety rules that should be made known to the new employee to safe guide the employees health and keep the organization from liabilities and some of this rules are Emergency procedures Making the hazard areas known to the employee What medical facilities is available in case health issues and where to find them Making known the actions that will be taken to discipline an employee that breaks the safety rules. Benefit that will be given to those that has been exposed to health hazards. One method that could be used to record an individuals progress during induction is explained One method that could be used to record an individual progress during induction is by evaluation. This is the process where we try to score an induction procedure; the aim of this procedure is to see how much the new employee understood the message that has been passed across, it is also used to check the effectiveness of the induction process. How an induction process could be evaluated is explained The induction process could be evaluated by collection of feedback from the person being inducted When it is one person or a few people being inducted we can evaluate the process by asking questions of their understanding of the induction but in the case of many people questionnaires are given to them to fill. They can also be allowed to speak about their experience. IMPLEMENTATION THE MANAGER SAW THAT THE POSTION WAS IMPORTANT due to my analysis and I was given the task to implement and after this implementation my branch had more staff this time staff that are dedicated to receiving bulk cash which has cause a major setback for the branch and the recruitment of the new staffs has taken the pressure off the other operation staffs and therefore leading to increase in the motivation of staff and the customer are moving from satisfied customers to loyal customer which is the ultimate goal of any organization. Word count 1970

The Teachings Of The Buddhist Religion - 962 Words

October 19 (attended): Began discussion on the Buddhist Religion. Introduced to the history of the religion, talking about the the historical beginning, and Siddhartha Gautama’s journey and struggles. We also discussed the religion itself, but on a visceral level, concerning ourselves with the fact that there was no god and no alternate reality. Class closed on the differences that exist between all the other religions that developed in the subcontinent of India. October 22 (attended): Discussion was centered around Buddhism, exploring aspects of the two main schools of thought, Theravada and Mahayana. Going over the pillars of Theravada Buddhism we learned how the religion is structured in such a manner that people do not have to practice in a specific location or to a specific deity, but that the school is very introspective and is isolated path to enlightenment. Also discussing the difference between being in an elevated state of bliss and actual enlightenment. Theravada is structured in such a way that it does not follow the current template of devotion, care and practice that religion has set throughout time rather it focuses on following the tenets that the left behind, and allowing each individual to tread their own path. October 26 (attended): We continued our discussion on Theravada Buddhism, analyzing the aspects what tenets devotees need to adhere to, such as the four noble truths and the eight-fold path. We then dove deeper into the significance of the what theShow MoreRelatedSiddhartha Gautama and His Religious Development Essay example1267 Words   |  6 PagesSiddhartha Gautama and His Religious Development Siddhartha Gautama, who became the Buddha or the enlightened one was born about 560 BC and died at the age of eighty. He was the founder of the Buddhist religion. 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