Maple Tree Density

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The null hypothesis being tested states that there is no difference in maple tree density in rural versus urban habitats. The experiment conducted observed maple tree density in both rural and urban habitats. The observed mean number of maple trees per quadrant in an urban habitat (Jackson Park) was 2 trees. The observed mean number of maple trees per quadrant in a rural habitat (Ojibway) was 6.25 trees. A student’s t-test was performed to test the null hypothesis. The tree density was measured in 16 quadrants in a total from the two habitats, thus the degrees of freedom of the experiment was 14. The critical t-value was 2.14 and the observed t-value was 3.12. Since the observed t-value is greater than the critical t-value, the results are …show more content…

The difference in means highlights the anthropogenic effects on maple tree density. According to Bubank (2014), maple trees are declining due to air pollution from sulfuric acid rain and climate change. A lower tree density at Jackson Park can be explained by these factors as it is found in an urban setting where more pollution is likely to occur and this adversely affects maple tree growth. Moreover, the urbanization of natural and agricultural land acts as an environmental stressor which adversely affects plant growth (Kolbe et al, 2016). Ojibway, on the other hand, is a conservation park where efforts are made to reduce anthropogenic stressors on plant development so that there are less chances of pollution occurring and this explains the higher maple tree density there. This experiment reflects the positive effect that conservation has on plant ecosystems and more conservation efforts should be done in the future to tackle climate change and preserve wildlife. Another factor that affects tree density, is nutrient richness in the soil. Natural soil develops as a result of aggregation of salt, clay and other substances which forms a soil structure that enables nutrient availability, which is vital to plant development. Urban soils lack this natural process of structure formation, compacting the soil since it is disturbed often by anthropogenic factors (Craule,

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