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<br />fev,rer), the less likely that on-street parking \vill need to
<br />be provided as part of the road \vidth. The Bucks
<br />County (Pennsylvania) Planning Commission street
<br />\vidths for cluster subdivisions were set at 22 feet for
<br />streets with an average daily traffic volume of 2,000
<br />vehicles or less, and 24 feet for streets \vith traffic
<br />volumes greater than 2,000 vehicles per day. Both
<br />measurements include curbs. The issue of access by
<br />emergency vehicles is often raised \vhen a community
<br />seeks to reduce residential street \vidths in all or part of
<br />its jurisdiction.
<br />Clustering houses is an effective way of keeping
<br />floodplains largely free from development \vhile
<br />allmving the same level of density that vvould be
<br />permitted under normal conditions. The variable street
<br />configurations in such developments are beneficial
<br />because they tend to require less land area to be
<br />devoted to roads and impervious surfaces than in
<br />conventional subdivisions and they can be aligned in a
<br />manner that best accommodates natural drainage
<br />patterns. (The cluster development concept is described
<br />in detail in Chapter 3.)
<br />Detention and retelltio1t basins. In upland areas,
<br />detention basins of sufficient size and depth are used
<br />to hofd and gradually release runoff. [t is up to the
<br />regulating jurisdiction to dictate the size, location,
<br />storage capacity, and release rate of detention basins.
<br />A typical requirement is enough capacity to capture
<br />the two-year, 24-hour event and hold it for at least 24
<br />hours before it is released into a \vetland or other
<br />watercourse.
<br />Retention basins, sometimes called wet ponds, are
<br />subject to similar requirements although they are not
<br />usually designed to release storm water at a particular
<br />rate other than \vhat naturally occurs through
<br />evaporation and seepage. Retention basins can double
<br />as \vildlife habitat and as recreational facilities. The
<br />Urban Land Institute nm\' recommends the inclusion of
<br />retention basins in large developments for both their
<br />storm water management ability and their attractiveness
<br />to buyers and tenants (Urban Land 1992).
<br />Infiltration devices. Infiltration devices are designed
<br />to promote percolation of stormwater runoff from roofs,
<br />do\vnspouts, driveways, and large lawns into the
<br />ground before that runoff can reach a \\'ater body (e.g.,
<br />a stream). These devices can reduce the flow of \vater
<br />do\vnstream, help preserve natural vegetation, and
<br />potentially lower development costs by limiting the size
<br />of the se\'ver system needed.
<br />The most common infiltration devices arc trenches
<br />and basins. lnfiltration trenches are three. to eight-foot-
<br />deep gravel-filled trenches into which runoff is diverted
<br />from home sites. Runoff collected in the trench is then
<br />released into the subsoil. The trenches can be used in
<br />conjunction v....ith s\vales.
<br />Natural depressional areas. \Vatersheds naturally
<br />contain topographic depressions that collect storm1,.vater
<br />runoff and delay its release to stream and other outlets.
<br />These areas are ~also created by road\\'ay embankments.
<br />Some depressional storage areas release rainfall excess
<br />only via evaporation or by slow infiltration into
<br />groundwater, thus preventing runoff from
<br />contributing to the flood. Site grading often results in
<br />
<br />the loss of these depressional storage areas and can
<br />have serious effects on the rate and volume of site
<br />runoff. The initial site analysis and subsequent
<br />drainage plan should identify depressional storage
<br />areas so that they are not eradicated through grading
<br />and site preparation.
<br />Swales. A swale is a grass-lined natural depression or
<br />wide shallow ditch used to temporarily store, route, or
<br />filter runoff. (See Figure 4-2.) In low-density residential
<br />areas, swales are a very common alternative to curbs
<br />and gutters. "lan-made s\vales located along natural
<br />drainage path and on the lower portions and edges of a
<br />development site can collect or redirect flow from yards
<br />or streets. The sides of swales should be shallow to
<br />allow for the slmv, even flow of runoff, which enables
<br />the swale to also absorb \vater. Grasses should be
<br />planted in swales to help slov.' runoff, stabilize soil, and
<br />slow weed growth. The use of swale drainage is
<br />advocated as part of a total storm water management
<br />program in a number of states, including I\~ew Jersey,
<br />Maryfand, Ohio, and Florida.
<br />Riparian buffers. Buffers are forested or vegetated
<br />areas adjacent to \vater bodies designed to stabilize
<br />banks, limit erosion, reduce runoff volume, preserve
<br />wildlife habitats, and create open space and recreation
<br />areas. (A greem.vay, as described in Chapter 3, is a
<br />linear open space established along a natural corridor,
<br />such as a riverfront, stream valley, or ridgeline, or over
<br />land along a railroad right-of-way or canal route, which
<br />has been converted to recreational use. \Vithin a
<br />greenway, a riparian buffer \vmIld be the area
<br />immediately adjacent to the \vatercourse.) The
<br />appropriate \-vidth of a buffer depends on the site
<br />conditions (e.g., slope and vegetation), the nature of
<br />storm water flo\-v from adjacent properties (e.g., the
<br />quantity and velocity of \vater, and the existence of
<br />channels), and the cost and benefits of the buffer to
<br />the developer and the community. To assemble a
<br />riparian buffer, a local government may purchase the
<br />land or it may require a developer to set aside lands
<br />immediately adjacent to \-vaterfronts for buffers. Such
<br />requirements may be provided \-vithin a storm\-vater
<br />management ordinance or in a separate riparian
<br />buffer ordinance.
<br />Buildillg setbacks. A building setback line further
<br />protects the \vatenvay from erosion and water-quality
<br />degradation due to runoff caused by development. In
<br />many cases, a setback of IOO to 200 feet from the
<br />watC'rway will serve to channel the drainage in the
<br />opposite direction of the stream or river and thus
<br />reduce pollution.
<br />A number of states and communities have applied
<br />setback standards to designated streams, rivers, and
<br />lakes through their shoreland management programs.
<br />For example, the Michigan Department of Natural
<br />Resources plan for the Betsie River in Michigan
<br />establishes a 20D-foot setback, with a reduction of five
<br />feet for everyone foot of upward slope, with a
<br />minimum setback of 150 feet. NFIP standards for the
<br />tloodway can f1ct as a de facto setback in that they
<br />prOhibit-any buildings or other structures from J
<br />encroaching into the flood way if they result in any
<br />increase in flood levels during a IOO-year flood.
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