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Stream ordering of the watershed suggests that Makhawan watershed is a fifth-order basin.
This would possibly explain why EcO157 was only found once in 178 samples from Farm A. Frequent isolation from the Gabilan watershed suggests there may be a higher concentration of EcO157 in this region compared to other sites.
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The stream ordering of the watershed suggested that the Makhawan watershed is of fifth order.
Differences between DOM released from the ALD vs. the undisturbed watershed suggest that these shallow detachment slides have significantly impacted the quality of Arctic DOM.
Still, measurable Ra activity was measured downgradient of even the constructed wetlands in the Kankakee watershed, suggesting that the attenuation of Ra was low.
Recharge temperatures calculated at pressures corresponding to well head elevations are similar to mean annual air temperatures at lower elevations of the watershed, suggesting that most recharge is occurring at these elevations, after equilibrating in the vadose zone.
Stream frequency values indicate positive correlation with the drainage density of all the sub-watersheds suggesting increase in stream population with respect to increase in drainage density.
While the difference in species composition between pasture and developing sites may have multiple, species-specific explanations, the dramatic differences between amphibian and reptile species richness in urban watersheds suggest broad trends that may be important to conservation planning.
Furthermore, the low F f, R e, and R c values of these sub-watersheds suggested a lower chance of occurrence of heavy rainfall covering the entire area, and hence lesser vulnerability to flash floods and as a result easier flood management than those of the circular basins (Pandey et al. 2004).
Modelling the C exported from the terrestrial to the inland aquatic system on a watershed scale suggests allochthonous C storage in lake sediment may be a significant C sink.
Multiple regression identified slope, runoff and agriculture as primary predictors of nitrate and phosphorus across the watershed, which suggests that both natural and anthropogenic landscape characteristics have a strong influence on nutrient levels in the Guare catchment.
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