905R90117
United States            Watershed Management Unit
Environmental Protection     Water Division, Region V
Agency                Chicago, IL
                                                           December 1990
xvEPA
Impacts of Changes in
Hydrology  Due to
Urbanization
The  Problem
          hen agricultural or natural areas
          become urbanized, bare soil or
          vegetation such as grasses,
          sedges, shrubs, and trees are
          replaced by impervious surfaces
          such as asphalt, concrete, and roof
          tops. Urbanization results in
                      increased flooding of local streams and channels,
                      washoff and transport of pollutants to the stream,
                      scour of the stream bottom, and streambank
                      caving or sloughing (Figure 1). Urbanization can
                      change watershed hydrology and subsequently
                      stream water quality and aquatic life.
              Paving & Buildings
                 Cause
              Increased  Runoff,
                Sediment, fc
              Chemical Transport
                                 Higher
                              Water Elevations,
                               Faster Flow
                                           Sediment
                                         Vegetation Scour
   Figure 1.—Effects of urbanization on streams.

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The  Cause
            s an area becomes urbanized, more
            roads are built and paved, houses,
            buildings, parking lots, and storm
            sewers are constructed, and areas
            become impervious to rainfall.
            Urbanization can result in two
            important changes in watershed
            hydrology:

   1.  The amount of runoff is increased because
      rainfall no longer percolates into the soil or
      is stored in small depressions in the soil, and
   2.  Runoff reaches the stream much faster and
      peak flows are higher because the
      resistance encountered as it flows overland
      is reduced.
   In general, the higher the peak rate of runoff,
the faster the flow velocity and the higher the
water levels in the stream. A stream that floods
only once a year with natural conditions is more
likely to have larger floods or flood more frequently
with urbanized surroundings. The energy
associated with the increased runoff is also likely
to be greater.
   The increased energy can cause sediment,
fertilizers, pesticides, metals, and oil and grease to
be transported into and down the stream. With the
increased energy of the flow in the channel,
sediments and vegetation can be scoured from the
bottom. The increased frequency of flooding, the
deepening of the channel and loss of rooted
vegetation can cause decreased bank stability and
eventually bank erosion.
   Storm sewers can aggravate the problem since
they collect stormwater from a large area and
deliver it to a single discharge point, often at a rate
faster than that of a natural stream.
 Impacts
             ncreased flow and pollutant loadings
             into and down the stream can have
             an adverse effect on aquatic life in
             the stream. Flow itself can flush
             established aquatic life downstream,
             especially if vegetation that provides
             shelter from the current is uprooted.
 Pollutants such as oil and grease can be washed
 off the surface of parking lots and roads and can
 smother many aquatic organisms. Surface oil also
 inhibits oxygen transfer between the air and the
 water. In addition, some of the degradation
 products of oil and grease  are toxic to aquatic
 organisms. Nitrates from fertilizers are easily
 leached from the soil by runoff and can promote
 aquatic plant growth; if the growth is sufficient,
 oxygen depletion by plant respiration at night can
 kill aquatic organisms unable to move out of the
 affected reach.
    Sediment erosion and deposition can have
 several impacts on aquatic life. The sediment that
 is eroded will eventually deposit in an area of
 slower flow and can smother bottom-dwelling
 organisms and fish eggs. Deposition can also
 cover critical aquatic habitats.
    If trees along the banks are lost due to bank
 erosion (or clearing during urbanization), shading
 is lost and stream temperatures rise. Stream
 temperatures can get too warm for some stream
 organisms. In addition, water holds less oxygen as
 it gets warmer so  decreased dissolved oxygen
 also may make the stream uninhabitable for
 stream organisms.
    Sediment may also carry adsorbed phosphorus
 from fertilizers and/or pesticides from residential
 areas. Phosphorus can promote algae and aquatic
 plant growth just as nitrate does and can have a
 similar impact. Both phosphorous and nitrate
 create problems in lakes because of nutrient
 enrichment  (i.e., eutrophication). Pesticides are
 toxic to some organisms and also can
 bioaccumulate  in  them.

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Stabilization  and  Remediation
           ften bank and channel erosion are
           dealt with by using stream
           stabilization measures that further
           change the ecology of the stream.
           Dredging to remove sediment
           accumulation physically removes
           bottom dwellers and can resuspend
           fine soils that eventually settle again
and smother downstream organisms. Associated
with the resuspended material may be
contaminants that were previously not impacting
aquatic life. Resuspension could release these
contaminants to the environment. Replacing a
natural earthen section with a wide concrete lined
channel eliminates the natural habitat and makes it
difficult for re-establishment of organisms. A better
approach is to use rip rap (i.e., rocks) which not
only stabilize the channel but also provides
physical habitat for aquatic organisms. Holes also
can be dredged to create endearing or permanent
pools in the stream to act as a refuge for aquatic
organisms during dry periods.
   The installation of sedimentation, retention, or
detention basins in the channel can disrupt
resident aquatic life and replace desirable
organisms with nuisance organisms. However, the
basins can be designed to continuously contain
water and once established, become a natural
resource such as a lake or pool.
Example Case Study
            he Northeastern Illinois Planning
            Commission studied the
            effectiveness of existing and
            alternative detention practices in
            limiting downstream peak flood
            events and in controlling minor flood
            events which cause channel erosion.
They found that runoff volumes increased by
25 percent and that peak flows more than doubled
after urbanization for the 2 year frequency flow.
They also found that properly designed detention
facilities reduced peak flow rates to
predevelopment levels and prevented downstream
scour and bank destabilization.

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                           TERRENE
                               INSTITUTE
This project was funded by the U.S. Environmental Protection Agency Office of Water Enforcement
and Permits-Water Permits Division and managed by Region V Watershed Management Unit-
Water Division. Prepared by Dynamac Corporation, FTN Associates, and JT&A, Inc. For copies of
this publication,  contact  The  Terrene Institute,  1000  Connecticut Avenue,  NW,  Suite  300,
Washington, DC 20036, (202) 833-3380.
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