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Watershed Protection Plan - Lower Rio Grande Valley Development ...

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POLLUTION IN THE ARROYO COLORADO<br />

Storm Drain<br />

loads high in the Arroyo Colorado, and high suspended<br />

sediment prevents the Arroyo Colorado from<br />

assimilating nutrients along its course. Under normal<br />

conditions, ammonia and nitrates are removed by<br />

algae, which use these nutrients to grow. However,<br />

algal growth is suppressed when sediment loads are<br />

high because light penetration limits photosynthesis.<br />

Also, suspended<br />

sediments help to<br />

transport phosphate,<br />

another important<br />

nutrient, by adhering<br />

to it and releasing it<br />

downstream.<br />

The lack of an<br />

adequate riparian<br />

habitat can also<br />

help keep dissolved<br />

oxygen levels<br />

lower in a stream<br />

by keeping surface<br />

water temperatures<br />

higher. Oxygen<br />

gas stays dissolved<br />

in water better at<br />

cooler temperatures.<br />

The canopy offered<br />

by trees and other<br />

riparian vegetation<br />

shade the banks Llano <strong>Grande</strong> Lake<br />

of natural streams, helping to keep surface water<br />

temperatures lower, and thereby increasing the<br />

solubility of oxygen.<br />

Dredging in the tidal portion of the Arroyo Colorado<br />

also contributes signifi cantly to the stream’s inability<br />

to meet the State’s Water Quality Standards for a high<br />

aquatic life use. The removal of bottom sediments<br />

from the bed of the Arroyo Colorado results in the deep<br />

intrusion of hypersaline (very salty) water from the<br />

Laguna Madre to the Port of Harlingen. The intrusion<br />

of salt water this far inland causes the upper and lower<br />

portions of the water column of the Arroyo Colorado<br />

to segregate into distinct density layers that do not mix<br />

well vertically; this phenomenon is known as density<br />

stratifi cation. During periods of low fresh water fl ow<br />

and warm temperatures, the bottom depths (~3m) of<br />

the water column in much of the tidal segment of the<br />

Arroyo Colorado become almost completely depleted of<br />

oxygen (0-1.5 mg/l), leaving a surface layer of less than<br />

one meter with adequate conditions for aquatic life (DO<br />

between 4-6 mg/l).<br />

Natural aeration (i.e., oxygenation) in coastal<br />

streams is largely dependent on wind action. Oxygen<br />

is introduced into the surface layers of coastal water<br />

bodies through mechanical agitation caused by wind<br />

movement. Wind aeration can be inhibited in stream<br />

January 2007 61 Arroyo Colorado <strong>Watershed</strong> <strong>Protection</strong> <strong>Plan</strong>

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