北太平洋垃圾带的形成与变化Formation and Variation of the Great Pacific Garbage Patch8页word文档.doc
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1、如有侵权,请联系网站删除,仅供学习与交流北太平洋垃圾带的形成与变化Formation and Variation of the Great Pacific Garbage Patch【精品文档】第 8 页Formation and Variation of the Great Pacific Garbage PatchXiaoben Liu, Liuwu Shi, Yue ZhaoAbstract We build four models to do a deep analysis on the formation, variation and distribution of the Grea
2、t Pacific Garbage Patch. The first two models are created to research the mechanism of how the garbage island comes into existence from a microscopic scale. The velocity of trash alleviates as time goes on. Trash does its motion in two probable ways, one is due to resistances given by sea water, ano
3、ther is due to damp vibration. Using classic physical theories, we capture main motives propelling trash into the North Pacific Gyre. The third model is a compartment model aiming to find the possible increasing amount of trash in the garbage patch. A function of total garbage amount is extrapolated
4、 from the model. We use this model to predict that the number of plastic debris will be more than three times larger in the next 10 years successfully. In our fourth model, we work out a density function. Using the function, we depict the temporal and spatial distribution of garbage in the ocean. We
5、 also make a simulation reflecting its distributing rules more obviously. At last, we release some suggestions to prohibit deterioration in the Great Pacific Garbage Patch.Introduction Where is the largest landfill in the world? Its in the Pacific Ocean, about one thousand kilometers near the shore
6、of America, called the Great Pacific Garbage Patch. Its a specific area between California State and Hawaii, but until now theres no accurate estimation about its coverage. The Great Pacific Garbage Patch is notorious for its high concentration of littered trash, plastic debris. According to a recen
7、t investigation, 80 percent of the trash is from main continents, 10 percent consists of used nets or other fishing tools and the other 10 percent of trash is from passing-by ships. Most of the garbage islands are in oceanic gyres.Undoubtedly the accumulation of garbage has already made huge negativ
8、e influence on the environment. Large amount of oceanic animals die of eating up plastic trash by mistake. Its a critical moment to release some feasible and practical methods to prevent deterioration. Proper methods involve comprehensive information about the object. We verify many basic parameters
9、 characterizing the formation process of the huge landfill. The effect of ocean current is considered as the top factor in transferring garbage to America seashore.We build several models to solve three problems separately: the accumulation and motion of trash on the Pacific Ocean; the increasing ra
10、tio of the garbage amount in Great Pacific Garbage Patch; the distribution of the garbage density in Great Pacific Garbage Patch.The first question The first section mainly discusses the possible motion track and the way how trash pile in the Pacific Ocean. There are two mechanisms of how trash thro
11、wn into the oceanic gyre.Lets start from the Great Pacific Garbage Patch. In our analysis, main mechanism for formation of this garbage area is due to force reactions on trash. As trash is floating in the current, it has a velocity similar to that of the current. When trash moves out the current, it
12、 enters a district where no wind exists. Forced by water resistances, the initial velocity decreases with a certain acceleration. Finally trash stays static in some area in the oceanic gyre. As time goes on, more trash accumulates in the district, forming a garbage patch. Assumptions Velocity of tra
13、sh is low enough to calculate resistance given by water using the formula: .All the debris has discrete motion without conglomeration.Oceanic surface out of the currents is considered to be static.Ignore the differences generated by various figures.Glutinosity of sea water is neglected.Our first mod
14、elAccording to our discovery, the North Pacific Current doesnt keep its motion direction as a uniform straight line. As we can see from Figure 1, the North Pacific Current branches near the pacific garbage patch. Consequently trash is conveyed inside the oceanic gyre. Figure 1 Current flow in the No
15、rth Pacific Gyre.When trash is in the current, its motion is regarded as a static condition relative to the oceanic surface with a communal velocity , as shown in Figure 2.Figure 2 Trash moving in the current.After moving for a distance, at the crossing where current branches, trash enters the area
16、where no winds blow. As the direction of velocity alters, trash makes a turn and rotates for a certain angel. In this condition, forces imposed on it are completely different. The oceanic surface is static, but trash is floating with a velocity , so trash will be oppressed by resistances, as shown i
17、n Figure 3. Figure 3 Trash moving in the no-wind area.Trash is influenced by three forces: Coriolis Force, and two resistances given by sea water. In our model, we just analyze forces on the direction of . Obviously the velocity is on a decline. Computations for acceleration:-constant of resistanceS
18、o we can extrapolate the equation of velocity:-constant of resistance-the initial velocityThe distance that trash could float before it stops can be computed like below:Weve tested many values for , but keeps its value between 600km and 800km. The result is illustrated by simulation in Figure 4.Figu
19、re 4 Distance that trash can float with different values of .So we reach to the conclusion that, if trash moves with branch currents, entering the no-wind area, the distance that it can float is between 600km and 800km. And there will be a large garbage island about 600km to 800km distant from the N
20、orth Pacific Current.Out second modelThis model is built to solve problems why there are so much trash accumulating near Japan coastline.In this model, we mainly concentrate on the dissipation effect along the current. It makes the water flow move in a radiating way, though the radiating flow is muc
21、h thinner comparing with the main stream. As a result, some trash is pulled into the gyre by the radiating stream. We use damp vibration model to explore how the velocity varies in this condition. The basic equation is:1We make computations to verify how far trash could float in the ocean.Figure 5 D
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