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The rate of Urucurituba Channel width increase has been ≈ 5 m/month since 2011, increasing drainage capacity of the channel.
(1) Reducing the build-up of pore water pressure during and after earthquake by increasing drainage of the soil surrounding the columns.
Increasing drainage and cultivation of hot springs catchment and related wetlands when the water level recedes after the rains, has greatly affected the wetland ecosystem.
The values of stream frequency indicate that all the sub-watershed show positive correlation with increasing stream segments with respect to increasing drainage density.
The values of stream frequency indicate that all the sub-basins show +ve correlation with increasing stream population with respect to increasing drainage density.
The values of stream frequency indicate that the basin shows +ve correlation with increasing stream population with respect to increasing drainage density.
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Fig. 2 Increased drainage density causes faster hillslope response and higher peak flows.
With respect to water balance, the greatest sensitivity to parameter uncertainty was observed in the drained marsh area, where some scenarios showed increased flow of sea water into the interior and increased drainage.
Tiling and channelization have increased drainage efficiency and probably have contributed in part to the occurrence of large floods on the Mississippi River, but the magnitudes of their effects are unknown at present.
These patterns are consistent with a proposed conceptual model in which increased drainage density results in (1) greater transport of soil water to streams and (2) a delayed rise in the water table.
However, it was found that a sea-level rise of up to 1.2 m by 2010 would result in increased drainage times and higher volumes of over-topping when flooding occurs.
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