Beyond Green LID Zero Runoff Strategies for Our Cities. Barrett L. Kays 1

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Beyond Green LID Zero Runoff Strategies for Our Cities Barrett L. Kays 1 1 Dr. Barrett L. Kays, Landis, PLLC, 3908 Bentley Brook Drive, Raleigh, NC 27612-8076, 919-696-6930, e-mail: barrettkays@gmail.com Abstract The technology of green stormwater strategies has advanced rapidly in the last twenty years so that we can now design or retrofit cities to achieve zero runoff for large storm events. A detailed examination of projects that have achieved zero runoff, full groundwater recharge, or advanced treatment prior to attenuated discharge to surface waters, provides insight into the LID options for our cities. Beyond green critical thinking, true multi-disciplinary problem solving, and rethinking regulations has led to these new concepts. Yes stormwater systems can be beautiful, function to a high degree, achieve beyond green results, and help create dynamic green livable cities. Introduction The earliest large stormwater infiltration systems were deep unsightly infiltration basins that hold water for extended periods of time (Ferguson, 1994). This paper focuses on a new type of large infiltration systems that began in the early 1990 s (Kays, 2000), are designed to be both function and beautiful and are used in urban parks, major league baseball, football, and soccer sports fields, as well as, special use venues. Most of these new systems have been very successful, but some have not due to the fact that the critical design factors are not well understood (Kays, 2006). Seven projects were examined to better understand the factors that are important in the design of large infiltration and filtration systems. The projects were evaluated to study the system size, soil depth, drained porosity, sand gradation, organic matter, hydraulic conductivity, volume of soil storage, rainstorm capacity, and rainstorm frequency. One of the systems had failed, later was rebuilt, and offers insight into the critical factors affecting success. Three small systems projects that have recirculating filtration prior to discharge were also studied. Review of Large Bioretention Projects Studied High rate infiltration bioretention systems typically use a uniformly graded sand based structural soil for the proper functioning of both the landscape plantings and the stormwater system. Seven large bioretention zero runoff projects were reviewed and they are as follows: 1. The Great Lawn in Central Park, New York, NY a 0.762-meter deep uniformly graded sand based structural soil was installed in the Great Lawn (Figure 1) to capture rainfall events over a 9.72-hectare site, as well as, providing a compaction resistant surface for sports, concerts and other special venue events. The 1

project was completed by the Central Park Conservancy, Inc. Rainfall events are both detained and filtered through the sand, silt, and organic media before draining into the storm sewer system and treatment at the East River WWTP. The project design started in 1992 and construction was completed in 1997. In 1998 the conservancy was awarded a Design Honor Award by American Society of Landscape Architects and the Best Site Design of 1998 by New York Construction News. The project has functioned in an excellent manner and does not appear to have lost any hydraulic capacity over the last 17 years. Irrigation is provided and is especially needed in the summer months. Figure 1 Great Lawn in Central Park, New York, NY 2. Nelson Rockefeller Hudson River Park I, New York, NY a 1.067-meter deep well graded sandy loam soil was installed on 0.972-hectare meadow lawns along the Hudson River Promenade by the Battery Park City Authority (Figure 2). The soil materials did not meet the design specifications, had insufficient sand, was not uniformly graded sand, became highly compacted, and would only conduct water extremely slowly. After the opening of the park, rainfall events caused water to pond on the surface of the meadows and remained ponded for prolonged periods of time. This is the largest know failure of sand based structural soil and the meadows had to be excavated and rebuilt. 3. Nelson Rockefeller Hudson River Park II, New York, NY a new 1.067- meter uniformly graded deep sand based structural soil was installed on 0.972-hectare meadow lawns along the Hudson River Promenade by the Battery Park City Authority. The soil material meets the design specifications, had sufficient s uniformly graded sand, and properly conduct water when compacted. The soil has now been in place for over 12 years and has function to adequately drain and treated all of the stormwater for the park. 4. Longwood Gardens Main Fountain Garden, Kennett Square, PA a 1.067- meter deep uniformly graded sand based structural soil 0.972-hectare in size will be 2

installed in 2015 on the 3.645-hectare Main Fountain Garden at Longwood Gardens, as part of its modernization of the famous fountain garden. Thousands of people attend the daily light and fountain shows at this venue. Therefore, it was critical for the lawns to rapidly drain immediately after a rainfall so that the events would not need to be cancelled. The sand based structural soil for the lawn, shrubs and trees provides a bioretention system for stormwater. Figure 2 Nelson Rockefeller Hudson River Park left of the Solaire Building, Lower Manhattan, New York, NY 5. National Capital Mall, Washington, DC a 0.381-meter deep well graded sand based structural soil was installed in 2012 on a 2.633-hectare portion of the National Capital Mall by the National Park Service. This is the first section of the mall to be rebuilt. The soil s primary function is to be a structural system that is resistant to compaction of pedestrians. In addition, the soil serves to minimize runoff from rainwater falling onto the lawn. This approach will be utilized as other sections of the National Capital Mall are subsequently rebuilt. 6. Dwight D. Eisenhower Memorial, Washington, DC a 1.372-meter deep uniformly graded sand based structural soil is proposed on the 1.215-hectare Dwight D. Eisenhower Memorial for the Eisenhower Memorial Commission, along a section of Maryland and Independence Avenues. The soil is unusually deep to accommodate the large trees that will be planted. The soil serves as structural soil that is resistant to compaction and as a stormwater treatment system for the new park. 7. Northern Guilford Middle & High School Campus, Greensboro, NC a 1.829-meter deep loamy sand structural soil was installed in 2007 in three sports fields on the campus by the Guilford County School System (Figure 3). One of the fields is dripped irrigated with treated wastewater effluent from the two schools. The other two fields provide sports fields and stormwater retention. All three of the fields are built to provide a structural soil that is resistant to compaction and playing surfaces that can be used immediately after a large rainstorm event. The clayey 3

subsoils on the fields were excavated down to friable saprolite that contains less than 10% clay. The excavations extended down to as much as 3-meters but average 1.829-meters and was filled with friable saprolite that was mined elsewhere on the site. Thus the loamy sand saprolite extends from the surface down to the water table which is more than 12-meters below the ground. A 0.23-meter coarse sand cap was installed for rapid surface detention in the soil. In 2008 the project received the Beyond Green Award from the Sustainable Building Industry Council as the best school project in the US. Figure 3 Sports field at Northern Guilford Middle & High School Campus, Greensboro, NC Review of Stormwater Biofiltration Projects Recirculating Biofiltration is a method that uses a uniformly graded sand/organic media or sand media to effectively treatment the stormwater prior to discharge into storm sewers or streams. The stormwater is recirculated using solar pumps to pass the stormwater through the filter multiple times to enhance treatment and denitrification. Below are three projects that illustrate this LID application (Table 2): 8. Creative Arts Building Campus, Haywood Community College, Clyde, NC a 0.61-meter deep uniformly graded sandy media recirculating biofiltration system with 25% organic matter was installed in 2011 to treat the stormwater prior to stream discharge. Stormwater first flows through a single pass biofilter and cascades down four waterfalls before flowing into the stormwater pond. Next the water flows from the stormwater pond into the top of a 0.002-hectare biofilter and then flows into a storage tank. A solar pumping system is used for recirculation of the water back to the top of the waterfalls and subsequently into the biofilter for additional treatment. Once the tank becomes full it begins to discharge to the stream. 9. Isaac Dickson Elementary School, Asheville, NC a 0.91-meter deep uniformly graded sandy media recirculating sand filtration system with 25% organic matter in the 0.016-hectare biofilter will be installed in 2015 to treat the stormwater prior to stream discharge. Stormwater will flow first into the biofilter, then into a storage tank, then it will be pumped to a shallow stormwater wetland pond, and the 4

outflow of the pond will flow back into the biofilter. Once the tank becomes full it will discharge to stream. 10. Turman Hall, Emory University, Atlanta, GA a 0.61-meter deep uniformly graded sandy media recirculating biofiltration system with 4 percent organic matter was installed in 2010 to apply the roof rainwater harvesting and condensate water by irrigation of the sandy media. The sandy soil was installed on top of a parking deck and serves as an outdoor student plaza and garden for Turman Hall residents. The biofilter covers 0.061-hectare area on the parking deck. The excess water drain into a storage tank which is used to spray irrigated and filters the storm-water again. Once the tank becomes full it begins to discharge into the storm sewer. Figure 4 Turman Hall sand media filter system plaza over a parking garage at Emory University, Atlanta, GA Discussion of Design Factors Many of the basic design factors dealing with soils, porosity, pore size distribution; compaction, water movement, and layering of soils are explained in a recent publication (Kays, 2013). These systems are described as bioretention, but they are different from bioretention systems included in best management practice stormwater manuals. Design standards for small bioretention system cannot simply be scaled up to large systems. Bioretention Systems with Under Drainage - The hydraulic conductivity of the five bioretention systems with under drainage ranged from 9.515 to 14.480 cm/hr (Table 1), had a mean conductivity of 12.07 cm/hr, mean percent sand of 86.2, mean percent of coarse + medium sand of 71.0, mean percent of organic matter of 7.8, mean soil depth of 0.93 meters, and mean size of 3.64-hectare. 5

Co+M Sand Organic Soil Sat. Hydraulic System No. Project Type of System Sand Sand Diameter Matter Depth Conductivity, K Size % wt. % wt. mm % Vol. m cm/hour ha 1 Central Park Bioret./Under Drainage 92.0 82.0 0.25 to 1.00 10 0.762 14.480 9.720 2 Hudson River Park 1 Bioret./GW Recharge 60.0 18.1 0.50 to 1.00 5 1.067 0.025 0.972 3 Hudson River Park 2 Bioret./Under Drainage 90.0 76.5 0.25 to 1.00 10 1.067 12.700 0.972 4 Longwood Gardens Bioret./Under Drainage 86.9 73.6 0.25 to 1.00 4 1.067 12.700 3.645 5 National Capital Mall Bioretention 79.1 49.2 0.005 to 2.00 5 0.381 10.920 2.633 6 Eisenhower Memorial Bioret./Under Drainage 83.0 73.6 0.25 to 1.00 10 1.372 9.525 1.215 7 Northern Guilford Schools Bioret./GW Recharge 72.3 36.0 0.05 to 2.00 0 1.829 2.515 2.475 Mean 86.2 71.0 7.8 0.930 12.065 3.64 Table 1 Comparison of Sand Based Structural Soil Infiltration Projects Co+M Sand Organic Soil Sat. Hydraulic System No. Project Type of System Sand Sand Diameter Matter Depth Conductivity, K Size % wt. % wt. mm % Vol. m cm/hour ha 8 Haywood Community Coll. Recirculating Biofilter 90.0 85.4 0.25 to 1.00 25 0.61 12.700 0.002 9 Isaac Dickson Elem. Sch. Recirculating Biofilter 90.0 86.7 0.25 to 1.00 25 0.91 12.700 0.016 10 Turman Hall, Emory Univ. Recirculating Biofilter 90.6 84.0 0.25 to 1.00 4 0.61 12.700 0.061 Mean 90.2 85.4 18.0 0.711 12.70 0.026 Table 2 Comparison of Sand Organic Media Biofiltration Projects 6

Sat. Hydraulic Conductivity, cm/hour Bioretention Systems with Groundwater Recharge Two of the projects were designed for groundwater recharge (Table 1). Project #2 hydrologically failed to function and was rebuilt. Project #7 was the only successful groundwater recharge system and it was constructed in saprolite that existed on the site. The hydraulic conductivity was 2.515 cm hr -1, percent sand was 72.3, percent coarse + medium sand was 36.0, percent organic matter was 0.0, soil depth was 1.820 meters, and its size was 2.475-hectares. The hydraulic conductivity of the seven systems is proportional to the percent sand in the bioretention soil (Figure 5). The lowest data point on the graph represents the failed system #2. The second lowest data point on the graph represents the loamy sand textured saprolite. 16 14 12 10 8 6 4 2 0 y = 0.4711x - 28.93 R² = 0.9158 0 10 20 30 40 50 60 70 80 90 100 Percent Total Sand Figure 5 Effect of Percent Sand on the Conductivity of Bioretention Systems The hydraulic conductivity is also proportional to the percent of coarse + medium sand (Figure 6). The systems clustered in the top right corner of the graph all consist of uniformly graded sands, while the three lowest percentages are systems using well graded sands. After the total percent of sand, the second most important factor is the percent of uniformly graded coarse and medium sand. Recirculating Biofiltration Systems The three systems had hydraulic conductivities of 12.70 cm hr -1 (Table 2), mean percent sand of 90.2, mean percent of coarse + medium sand of 85.4, mean percent of organic matter of 18.0, mean soil depth of 0.71 meters, and mean size of 0.026-hectares. The detention storage capacity of bioretention systems was calculated for the systems based upon the estimated drained porosity at 0.1 bars of soil moisture tension, depth of soil, and size of the system (Table 3). The rainfall capacity for 24-hour rainstorms ranged from 2.134 to 45.720 cm, and the frequency of the rainfalls ranged from 0.25 7

Rainfall Capacity, cm Figure 6 Effect of Percent Coarse + Medium Sand on the Conductivity to 1000 year events. It is interesting that the rainfall capacity of the bioretention system is so proportional to the rainstorm frequency over a rather large geographic area (Figure 7). 50 40 30 20 10 0 y = 4.3733x 0.3117 R² = 0.9637 0 500 1000 1500 2000 Rainfall Return Frequency, years Figure 7 Rainfall Capacity of Bioretention System are Proportional to Rainstorm Frequency over a Large Geographic Area of New England, Mid- Atlantic, and Southeast Regions of United States The maximum rainfall events for recirculating filtration systems was calculated based upon the hydraulic conductivity and system size (Table 4). Projects #8 and #9 are typical filtration systems that are sized to handle numerous small storm events ranging from 1.306 to 1.582 cm rainfalls. Project #10 has a maximum rainfall capacity of 32.657 cm, although it typically operates only when the landscape needs to be irrigated. 8

24-Hr Rainfall Capacity Drained Soil System Soil in Soil Detention Storage No. Project Type of System Ksat 1 Porosity 2 Depth 3 Size Storage Rainfall Frequency cm/hour % m ha m 3 cm years 1 Central Park Bioret./Under Drainage 14.480 25% 0.762 9.720 18,516.60 19.050 100 2 Hudson River Park 1 Bioret./GW Recharge 0.025 2.0% 1.067 0.972 207.39 2.134 0.25 3 Hudson River Park 2 Bioret./Under Drainage 12.700 25% 1.067 0.972 2,592.32 26.670 200 4 Longwood Gardens Bioret./Under Drainage 12.700 25% 1.067 3.645 9,721.22 26.670 500 5 National Capital Mall Bioretention 10.920 20% 0.381 2.633 2,005.97 7.620 2 6 Eisenhower Memorial Bioret./Under Drainage 9.525 25% 1.372 1.215 4,166.24 34.290 1000 7 Northern Guilford Schools Bioret./GW Recharge 2.515 25% 1.829 2.475 11,313.87 45.720 2000 Mean 8.981 0.210 1.078 3.090 6931.942 23.165 543 Footnotes: 1-Saturated hydraulic conductivity, 2-Difference in soil moisture between saturation and 100 cm pressure, 3-Soil depth includes depth of planting soil and chocker layer Table 3 Comparison of Hydraulic Capacity of Sand Based Infiltration Projects Table 4 Comparison of Hydraulic Capacity of Sand Organic Media Biofiltration Projects System Max. Rate Storage Drainage 24-Hr Rainfall Capacity No. Project Type of System Ksat 1 Size Filtration Tank Area Rainfall Frequency m/day m 2 m 3 /day m 3 m 2 cm years 8 Haywood Community Coll. Recirculating Biofilter 3.048 24.300 74.066 30.267 5,670.00 1.306 0.1 9 Isaac Dickson Elem. Sch. Recirculating Biofilter 3.048 166.050 506.120 56.751 31,995.00 1.582 0.25 10 Turman Hall, Emory Univ. Recirculating Biofilter 3.048 303.750 925.830 37.834 2,835.00 32.657 1000 Mean 3.048 164.700 502.006 41.617 13500.000 11.848 333.450 Footnotes: 1-Saturated hydraulic conductivity 9

Summary The sand based bioretention systems provide an excellent LID stormwater system for highly density urban sites. However, it is essential that the system are constructed with 80 or more percent sand, and that at least 70 percent or more of the sand be uniformly graded medium to coarse sand. Large bioretention systems have been used for parks, sports fields, and other urban special use venues that need a compaction resistant surface for large numbers of pedestrians. All of the bioretention systems reviewed do not look like stormwater systems, because they are designed to blend into the landscape and also serve other purposes in our cities. When there is not sufficient space for a large landscape bioretention stormwater system, recirculation biofiltration provides an excellent treatment system. Literature Cited Ferguson, Bruce K. 1994. Chapter 7, Infiltration Cases and Experiences, in Stormwater Infiltration. Lewis Publishers, New York, NY. Kays, Barrett L. 2015. Beyond Green LID Zero Runoff Strategies for Our Cities, Paper to International Low Impact Design Conference, American Society of Civil Engineers, Houston, TX. Kays, Barrett L. 2015. Amending Soils for Enhanced Infiltration of Stormwater, Paper to International Low Impact Design Conference, American Society of Civil Engineers, Houston, TX. Kays, Barrett L. 2015. Designing Beyond Green Urban Stormwater Systems for Zero Runoff from Large Storm Events, Workshop Presentation to International Low Impact Design Conference, American Society of Civil Engineers, Houston, TX. Kays, Barrett L. 2013. Planting Soils for Landscape Architectural Projects. LATIS Series Publication, American Society of Landscape Architects, Washington, DC. Kays, Barrett L. 2006. Problem Solving in Stormwater Bioretention Systems: Pitfalls in Bioretention Systems and How to Avoid Them, Landscape Architecture Magazine, June 2006, pp. 94 105. Kays, Barrett L. 2000. Environmental Site Assessments: Site Characterization Methodologies, Chapter 3, in Brown, Randall, et al, (ed.) Managing Soils in an Urban Environment, American Society of Agronomy, Inc., Crop Sciences Society of America, Inc., and Soil Science Society of America, Inc., Monograph Series, Madison, WI. Kays, Barrett L. 1980. "Relationship of Forest Destruction and Soil Disturbance to Increased Flooding in the Suburban North Carolina Piedmont," Paper to Meetings, Metropolitan Tree Improvement Alliance, New Brunswick, NJ.

Kays, Barrett L. 1979. Relationship of Soil Morphology, Soil Disturbance and Infiltration to Stormwater Runoff in the Suburban North Carolina Piedmont, Dissertation, Soil Science, North Carolina State University, Raleigh, NC, 348p. Kays, Barrett L. 1978. "Relationship of Soil Morphology and Infiltration to Runoff and Flooding of a Suburban Southeastern Piedmont Watershed," Paper to 70th Annual Meeting, Soil Science Society of America, Chicago, IL. 11