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Relationship between Hardness Levels in Eslava Creek and ...

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Methods<strong>Hardness</strong> levels <strong>in</strong> <strong>Eslava</strong> <strong>Creek</strong> from January 1999 to August 2007 were obta<strong>in</strong>ed fromthe Alabama Water Watch organization website. The hardness levels were compared to theaverage monthly ra<strong>in</strong>fall for the city of Mobile, obta<strong>in</strong>ed from the National Weather Service, tosee if an <strong>in</strong>direct relationship could be found <strong>between</strong> the two variables. Bar graphs, scatterplots, <strong>and</strong> l<strong>in</strong>e graphs were used to show the <strong>in</strong>direct relationships. Other studies were also usedto better underst<strong>and</strong> the reasons for the outcome of the research.ResultsIncreased Ra<strong>in</strong>fall = Decreased <strong>Hardness</strong>The hardness levels <strong>in</strong> <strong>Eslava</strong> <strong>Creek</strong> were found to be lower dur<strong>in</strong>g prolonged periods of higherthan normal ra<strong>in</strong>fall amounts. Figure 2 shows that from January 2003 to August 2005, ra<strong>in</strong>fallamounts are above average while, hardness levels <strong>in</strong> <strong>Eslava</strong> <strong>Creek</strong> are below average. For themost part of 2003, ra<strong>in</strong>fall amounts trended towards above normal, while hardness levels trendedtowards below average levels. The same occurred for a brief time from April to August 2004.While the ra<strong>in</strong>fall amounts were above normal <strong>in</strong> Mobile, Alabama, the flow of <strong>Eslava</strong> <strong>Creek</strong>would have been faster than normal due to the additional water <strong>in</strong> the stream. In a related studyby the United States Environmental Protection Agency, hardness levels <strong>in</strong> a creek near SanDiego were lower, while stream flow <strong>in</strong>creased (USEPA 2000). Another study by scientists fromthe Philadelphia Water Department found that “river flow was the major determ<strong>in</strong>ant of dailyvariability <strong>in</strong> alkal<strong>in</strong>ity, conductivity, hardness, <strong>and</strong> calcium levels (Interl<strong>and</strong>i <strong>and</strong> Crockett2002).” I also produced a scatter plot to show the <strong>in</strong>direct relationship <strong>between</strong> the ra<strong>in</strong>fall

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