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The most common factor, Cooper says, is changing groundwater levels, or a sudden increase in surface water.
While, the increase, in surface water and groundwater salinity, ranges from 3 to 30% with 3% increment between groups.
Climate change and increasing urbanization are projected to result in an increase in surface water flooding and consequential damages in the future.
There has been an approximate threefold increase in surface water nitrate concentrations since the early 1960s to a current value of ∼35 mg l−1 (8 mg l−1 NO3–N).
In this context, perceived water quality of the improved sources was also important, with a 17% increase in surface water access in towns with one reported water quality problem as compared to towns with no problems.
Since the lakes were otherwise similar, we hypothesized that a DOC-mediated increase in surface water temperature would translate directly to higher rates of evaporation thereby informing climate response models.
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Decreases in acid deposition could also drive decreases in fish Hg due to increases in surface water pH.
Over the past decades, concentrations of dissolved organic carbon (DOC) have increased in surface waters.
In the urea treatments N runoff losses were significantly (P < 0.001) positively correlated (r = 0.851) with applied N. N concentration in surface water increased rapidly to maximum two days after urea application and then decreased quickly.
With higher N inputs from livestock manure, increased nitrate, ammonium, or total N concentrations in surface water or groundwater could lead to increased δ15N of food sources, and fish tissue would have higher δ15N in the food web (Anderson and Cabana 2006).
BAP concentration in groundwater significantly fluctuated with the seasons, and the ratio of total BAP in groundwater to that in surface water gradually increased during the rainy season.
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