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<br /> <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. <br /> <br />31 <br />