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    Introduction 1.1 Problem Statement Fractures are prevalent in natural and synthetic structural media‚ even in the best engineered materials. We find fractures in bedrock‚ in sandstone aquifers and oil reservoirs‚ in clay layers and even in unconsolidated materials (Figures 1.1 to 1.4). Fractures are also common in concrete‚ used either as a structural material or as a liner for storage tanks (Figure 1.5). Clay liners used in landfills‚ sludge and brine disposal pits or for underground storage

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    Define the key term sinkhole‚ explain how a sinkhole forms‚ and give an example you researched. The text book defines sinkholes as “a depression produced in a region where soluble rock has been removed by groundwater.” According to the Florida Department of Environmental Protection‚ sinkholes form in karst terrain mostly due to the collapse and erosion of surface sediments into underground cavities in the limestone bedrock. Karst is commonly used term referring to the characteristic terrain produced

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    Valley”‚ it explained some problems with property rights‚ the cost‚ and workers with the regulation of how the water should be in the agriculture with government. It first stated‚ “As farmers ramp up drilling and install larger‚ more powerful pumps‚ aquifers that had quietly flourished beneath the soil for thousands of years are dropping at dangerous rates” (Sabalow‚ Kasler‚ Reese‚ 2). The cost of pumping is low and there will is no loss of evaporation but the supply form groundwater is pollutants have

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    Working Paper Corporate Social Responsibility Does Not Avert the Tragedy of the Commons -Case Study: Coca-Cola India Aneel Karnani Stephen M. Ross School of Business The University of Michigan E-mail: akarnani@umich.edu Ross School of Business Working Paper Series February 2014 This paper will be published in Economics‚ Management‚ and Financial Markets‚ forthcoming. Keywords: corporate social responsibility; tragedy of the commons; common-pool resource; environmental sustainability. I would like

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    In terms of landscape characteristics‚ the town has a rugged topography. It is encircled by the mountains of Gabriel (north) and Korie (south). The town runs along the corridors of these mountains. In other words‚ it is a mountainous town with an elevation ranging from 1840 meter to 2170meter a.s.l.topographically; the built-areas of the town are located around the part of the mountain which slopes down. The slopping down continues along the west and south-west directions‚ making these directions

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    hydro geological conditionswhich leads to different aquifers. The upper zone is predominantly volcanic with relativelygood water yielding aquifers. The middle zone has localized aquifers in the fractured andweathered zones of the Basement system‚ with alluvial aquifers being locally important.Chyulu Hills host the aquifer that supplies the Mzima Springs‚ as well as the spring units thatflow from the eastern side of the range. Volcanic aquifers on the northern flank of Kilimanjaroare sources of a

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    the definition has changed as economics‚ protection of ground water‚ and environmental affects have been considered in this concept as well. So‚ safe yield is now defined as the amount of naturally occurring ground water that can be taken from an aquifer on a regular basis‚ economically and legally‚ without affecting the native ground water quality or forming an unwanted effect such as environmental damage. When pumping water from a ground water supply‚ there are many possible adverse environmental

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    Physical Characteristics The site is located in an industrial and residential area in northeast Oklahoma City‚ Oklahoma (Section 31‚ Township 12 North‚ Range 2 West). The site is located on the south side of Tenth Street between Bryant Avenue and the North Canadian River and covers approximately 3.5 acres. One residence is located adjacent to the west side of the site. Residential subdivisions are located approximately one block to the north and approximately one block to the west of the site

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    long term average groundwater contours (for pre-monsoon) in msl are shown in figure 3b. The tendency of contours towards the rivers/streams indicated that continuous and greater interaction between river and groundwater aquifer. The groundwater velocity vectors indicated that aquifers feedthe rivers in non-monsoon season (Figure 4b). 4.2 Regression analysis The multi linear regression model was used for post-monsoon recharge‚ topographic elevations and pre-monsoon water level. The regresson model

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    Ground water! What is it? Well it’s basically self-explanatory and is any water that is held under ground. That is only a very simple definition of it though and well in fact ground water is very critical to every ones life locally and worldwide. Most of the water that you drink comes from ground water and not from lakes and rivers even though those are considered as a part of ground water components. Ground water has many components that it can be divided into and this paper will explain what

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