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Modeling the Effects of Low Impact Development on Runoff and Pollutant Loads from an Apartment Complex
  • 비영리 CC BY-NC
  • 비영리 CC BY-NC
ABSTRACT
Modeling the Effects of Low Impact Development on Runoff and Pollutant Loads from an Apartment Complex
KEYWORD
Low impact development , Site Evaluation Tool , Storm water management , Urban hydrology
  • 1. Introduction

    South Korea (hereafter, Korea) has experienced rapid urbanization in recent decades. Lee [1] reported that the rate of urbanization in Korea rose from 35.8% in the 1960s to 86.5% in 2005. Urban spaces in Korea have a very high percentage of impervious areas compared to similar spaces in other countries. Impervious surfaces are estimated to cover approximately 87% of residential, 92% of commercial, and 84% of industrial developments in Korea [2] Urbanization decreases infiltration and increases surface runoff, peak flow and the magnitude of flooding [3]. Reduced infiltration may decrease groundwater recharge and stream baseflow [4]; furthermore, hydrological alterations caused by urbanization contribute to stream channel degradation and increased non point sources of pollution.

    Recent research has demonstrated the successful use of low impact development (LID) strategies for managing the hydrology in urban areas. LID is a relatively recent stormwater management technique, which mimics the predevelopment site hydrology using integrated management practices (IMPs), such as bioretention, dry wells, filter strips, grass swales, infiltration trenches, permeable pavement, rain barrels, soil amendments, tree box filters, vegetated buffers and green roofs [5]. Schneider and McCuen [6] reported that the use of rain barrels can effectively reduce peak discharge during small storms. Meanwhile, Brander et al. [7] concluded that infiltration techniques were very effective for reducing runoff in a development area. Passeport et al. [8], Li et al. [9] and Hunt et al. [10] evaluated the effects of bioretention on the hydrology and pollutant removal. Moran[11] reported that a green roof retained approximately 60% of the total recorded rainfall and 85% of the average peak flow during a nine-month observation period, but the nutrient concentrations in the runoff from a greenroof were higher than those in the control roof, which was the result of leaching from the soil media. Hood et al. [12] experimented with LID techniques and illustrated their effective reduction of runoff and peak discharge, as well as runoff lag times and thresholds compared with traditional stormwater management practices. A number of researchers have developed models for LID design and evaluation.Prince George’s County [5] reported on a hydrological analysis of LID, and Jeon et al. [13] developed LIDMOD for LID modeling based on the method proposed by Prince George’s County. The Site Evaluation Tool (SET), developed by Tetra Tech, Inc., was designed to aid in assessing development plans and LID techniques, and to determine best management practices (BMPs) for the reduction of the impact of urban stormwater.

    In this study, the SET was used to model the effects of porous pavements and green roofs on the urban hydrology and pollutant loads from an apartment complex, with the applicability of these LID techniques evaluated for apartment complex developments.

    2. Materials and Methods

    2.1. Site Evaluation Tool

    The SET is a Microsoft Excel spreadsheet-based tool designed to aid in the assessment of LID methods and available IMPs [14], which was developed by Upper Neuse River Basin Association and Tetra Tech, with funding from the NC Division of Water Quality, USA, and is obtainable on the SET website [15]. The SET can be used as a screening tool to evaluate various site designs to help achieve the water quality goal of a site in a cost-effective manner [16]. The SET consists of two main components: the hydrology/pollutant component and the cost component (Fig. 1). The hydrologic balance is given in the SET as follows:

    image

    where P is the annual precipitation, R the runoff, E the annual evaporation and transpiration, ISW the annual groundwater recharge of storm water and IBMP the groundwater recharge via BMPs. The runoff is calculated using the “simple method” based on the fraction of the impervious to the total area:

    image

    where Aimp is the impervious area and Atot the total site area. The runoff is estimated in the SET using the Soil Conservation Service curve number (SCS-CN) method, based on the average antecedent moisture condition (AMC II):

    image

    where Q is the runoff, P the storm event precipitation and S the storage. The peak flow is calculated using the “rational method” and SCS-CN method, with pre- and post-development hydrographs estimated using the SCS-CN method. Pollutant loads are calculated as follows:

    image

    where L is the total load, LR the load from the runoff and LBMP the IMP load reduction. Loading from the runoff is calculated based on the event mean concentration (EMC):

    image

    where CR is the EMC and A the land area. Further details can be found in the SET documentation provided by Tetra Tech., Inc. [14, 16].

       2.2. Study Area and Data

    The study area was the Olympic Village Apartment Complex(41.4 ha), located at Sonpa-gu, Seoul, Korea (Fig. 2). Table 1 lists

    the land cover in the study area, obtained from 2009 Daum-Map data [17]. The study area was highly impervious (approximately 72%), with about half of the impervious area being parking lots. Hydrologic soil group data, in GIS shape-file format,were obtained from the National Institute of Agricultural Science and Technology. Soils in the study area generally drained well, with 19.5% for hydrologic soil group A, 53.7% for hydrologic soil group B and 26.8% for hydrologic soil group C (Table 2).

    The annual average precipitation from 1971-2000, as reported by the Korea Meteorological Administration [18], was approximately 1,429.6 mm, with considerable seasonal variation caused by the Asian monsoon. The annual average temperature, relatively humidity and wind speed were 12.2℃, 66.9% and 2.4 m/sec, respectively. Table 3 gives the probable amounts of precipitation at the Andong rain gauge station, which was used to estimate the peak flow and runoff volume during storms using the LID techniques.

       2.3. Parameter Updates

    The runoff volume and peak flow in the SET simulation were estimated using the SCS-CN method. Although the CN values were obtained from long-term experimental data, they sometimes required calibration, as they greatly depend on the field conditions, even for the same land use and soil type [19].

    To obtain more accurate simulation results, regionalized CN values for Korea, which were globally optimized for 10 watersheds during a 20-year period, were used in the SET, which are listed in Table 4.

    [Table 1.] Land cover in the study area

    label

    Land cover in the study area

    [Table 2.] Hydrologic soil groups in the study area (m2)

    label

    Hydrologic soil groups in the study area (m2)

    [Table 3.] Probable amounts of precipitation at Andong rain gauge station (mm) [1]

    label

    Probable amounts of precipitation at Andong rain gauge station (mm) [1]

    3. Results and Discussion

       3.1. LID Design

    This study evaluated two LID measures: green roofs and porous pavements. Green roofs covered with vegetation may retain stormwater and buffer nose [21]. Porous pavements may reduce the peak flow and runoff volume by enhancing water storage and infiltration into the soil; this system is best applied to areas where vehicular traffic is minimal, such as parking lots and sidewalks [21].

    In this study, the effects of replacing all the apartment rooftops with green roofs and all the sidewalks, parking lots and driveways within the apartment complex with porous pavements were simulated. Table 5 lists the current land uses and those under the LID design.

       3.2. Hydrologic Simulation

    Table. 6 and 7 provide summaries of the annual hydrology and the rates of reduction or increase in the hydrological components,respectively. The simulation indicated that the LID measures could reduce surface runoff and increase evapotranspiration and infiltration. The green roofs were found to reduce surface runoff and increased evapotranspiration, while the porous pavements were more effective than green roofs at increasing infiltration into the soil. The current surface runoff and current infiltration could be reduced by approximately 18% and increased by about 28%, respectively, using the combination of the two LID techniques.

    [Table 4.] CN values used in the SET [20]

    label

    CN values used in the SET [20]

    The simulated runoff and storage volumes for 2-year 24-hour storm events under the LID measures are summarized in Table 8. The simulated storage volumes for green roofs, porous pave

    [Table 5.] Current and LID land uses

    label

    Current and LID land uses

    [Table 6.] Summary of the annual hydrology (mm/yr)

    label

    Summary of the annual hydrology (mm/yr)

    [Table 7.] Reduction/increase of the hydrologic components due to the LID measures (mm/ha/yr)

    label

    Reduction/increase of the hydrologic components due to the LID measures (mm/ha/yr)

    [Table 8.] Summary of the runoff volumes for 2-year 24-hour storm events (m3)

    label

    Summary of the runoff volumes for 2-year 24-hour storm events (m3)

    [Table 9.] Peak flow during simulated storm events (m3/s)

    label

    Peak flow during simulated storm events (m3/s)

    ments and the combination of both LID measures were 825,983 and 1,808 m3, respectively

    Table 9 lists the peak storm flows under the LID measures, and Fig. 3 presents hydrographs for the current land use and the LID system of green roofs and porous pavements. The peak flows for the current land use for 2-year and 10-year 24-hour storms were estimated to be 7.58 and 10.88 m3/s, respectively. In the SET simulation, the peak flow was reduced by approximately 8% by the green roofs, 19% by the porous pavements and 27% by the combination of green roofs and porous pavements.

       3.3. Pollutant Load Simulation

    Modeled annual pollutant loads from various land covers are given in Table 10 and Fig. 4. Porous pavements and green roofs reduced the pollutant load by decreasing the surface runoff volume. Pollutant loads from the current land use were 9,323 kg/yr for biochemical oxygen demand (BOD), 1,565 kg/yr for total nitrogen (TN) and 232 kg/yr for total phosphorus (TP). These loads were reduced by 11% with green roofs, 7% with porous pavements and 18% with the combination of both LID systems.

    [Table 10.] Annual pollutant loads under the current and LID land uses

    label

    Annual pollutant loads under the current and LID land uses

    Considering the area of each LID measure, as given in Table 5, green roofs could more effectively reduce pollutant loads from the study area than porous pavements.

    4. Conclusions

    The SET has been designed to evaluate LID techniques. This study used the SET to evaluate the effects of green roofs and porous pavements on the surface runoff and pollutant loads for an apartment complex in Seoul, Korea. The results of the simulation indicated that the LID measures reduced the surface runoff and peak flow, but increased infiltration and evaporation. The increased soil infiltration could contribute to groundwater recharge and raise the level of the water table; thus, help to maintain base flow and supporting stream ecology. Per unit area, the green roofs out performed porous pavements at reducing the surface runoff and pollutant loads. However, porous pavements were better than green roofs at increasing infiltration into the soil and groundwater recharge. The results indicated that LID techniques can be used to help prevent urban flooding and erosion, as well as help maintain the ecological integrity of streams by controlling peak flow. Overall, the SET was useful for evaluating the effects of LID measures on the hydrology and pollutant loads. The application of LID measures is recommended for the management of water quality and preserving aquatic living resources and ecosystems in areas undergoing development.

참고문헌
  • 1. Lee WS 2006 The trend and characteristics of urbanization of Korea by analysis of population census. [KRIHS Policy Brief] Vol.106 P.1-4 google
  • 2. Oh KD, Jeon BH, Yang KK, An WS, Jho YH 2005 Curve number for urbanized areas. [J. Korean Soc. Water Qual.] Vol.38 P.1009-1020 google
  • 3. White MD, Greer KA 2006 The effects of watershed urbanization on the stream hydrology and riparian vegetation of Los Penasquitos Creek California. [Landscape Urban Plann.] Vol.74 P.125-138 google cross ref
  • 4. Paul MJ, Meyer JL 2001 Streams in the urban landscape. [Annu. Rev. Ecol. Syst.] Vol.32 P.333-365 google cross ref
  • 5. 1999 Programs and Planning Division. Low-impact development hydrologic analysis. google
  • 6. Schneider LE, McCuen RH 2006 Assessing the hydrologic performance of best management practices. [J. Hydrolog. Eng.] Vol.11 P.278-281 google cross ref
  • 7. Brander KE, Owen KE, Potter KW 2004 Modeled impacts of development type on runoff volume and infiltration performance. [J. Am. Water Resour. Assoc.] Vol.40 P.961-969 google cross ref
  • 8. Passeport E, Hunt WF, Line DE, Smith RA, Brown RA 2009 Field study of the ability of two grassed bioretention cells to reduce storm-water runoff pollution. [J. Irrigat. Drain. Eng.] Vol.135 P.505-510 google cross ref
  • 9. Li H, Sharkey LJ, Hunt WF, Davis AP 2009 Mitigation of impervious surface hydrology using bioretention in North Carolina and Maryland. [J. Hydrolog. Eng.] Vol.14 P.407-415 google cross ref
  • 10. Hunt WF, Jarrett AR, Smith JT, Sharkey LJ 2006 Evaluating bioretention hydrology and nutrient removal at three field sites in North Carolina. [J. Irrigat. Drain. Eng.] Vol.132 P.600-608 google cross ref
  • 11. Moran A 2004 A North Carolina field study to evaluate greenroof runoff quality runoff quality and plant growth [master thesis]. google
  • 12. Hood MJ, Clausen JC, Warner GS 2007 Comparison of stormwater lag times for low impact and traditional residential development. [J. Am. Water Resour. Assoc.] Vol.43 P.1036-1046 google cross ref
  • 13. Jeon JH, Choi D, Kim TD 2009 LIDMOD development for evaluating low impact development and its applicability to total maximum daily loads. [J. Korean Soc. Water Qual.] Vol.25 P.58-68 google
  • 14. 2005 Upper Neuse Site Evaluation Tool: model documentation. google
  • 15. c2009 Upper Neuse Site Evaluation Tool (SET) [Internet] google
  • 16. 2005 Upper Neuse Site Evaluation Tool: user’s manual and guidance. google
  • 17. c2009 Daum map [Internet] google
  • 18. c2009 Observed weather data [Internet] google
  • 19. Mohammed H, Yohannes F, Zeleke G 2004 Validation of agricultural non-point source (AGNPS) pollution model in Kori watershed South Wollo Ethiopia. [Int. J. Appl. Earth Observ.Geoinf.] Vol.6 P.97-109 google cross ref
  • 20. Jeon JH, Choi D, Kim JJ, Kim TD 2009 Regionalization of CN parameters for Nakdong Basin using SEC-UA algorithm. [J. Korean Soc. Water Qual.] Vol.25 P.245-255 google
  • 21. Montalto F, Behr C, Alfredo K, Wolf M, Arye M, Walsh M 2007 Rapid assessment of the cost-effectiveness of low impact development for CSO control. [Landscape Urban Plann] Vol.82 P.117-131 google cross ref
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  • [ Fig. 1. ]  The two main components and required spreadsheets of the Site Evaluation Tool [16]. BMP: best management practice.
    The two main components and required spreadsheets of the Site Evaluation Tool [16]. BMP: best management practice.
  • [ Fig. 2. ]  Study area.
    Study area.
  • [ Table 1. ]  Land cover in the study area
    Land cover in the study area
  • [ Table 2. ]  Hydrologic soil groups in the study area (m2)
    Hydrologic soil groups in the study area (m2)
  • [ Table 3. ]  Probable amounts of precipitation at Andong rain gauge station (mm) [1]
    Probable amounts of precipitation at Andong rain gauge station (mm) [1]
  • [ Table 4. ]  CN values used in the SET [20]
    CN values used in the SET [20]
  • [ Table 5. ]  Current and LID land uses
    Current and LID land uses
  • [ Table 6. ]  Summary of the annual hydrology (mm/yr)
    Summary of the annual hydrology (mm/yr)
  • [ Table 7. ]  Reduction/increase of the hydrologic components due to the LID measures (mm/ha/yr)
    Reduction/increase of the hydrologic components due to the LID measures (mm/ha/yr)
  • [ Table 8. ]  Summary of the runoff volumes for 2-year 24-hour storm events (m3)
    Summary of the runoff volumes for 2-year 24-hour storm events (m3)
  • [ Table 9. ]  Peak flow during simulated storm events (m3/s)
    Peak flow during simulated storm events (m3/s)
  • [ Fig. 3. ]  Hydrographs for 2-year and 10-year 24-hour storm events for the current and LID system land uses.
    Hydrographs for 2-year and 10-year 24-hour storm events for the current and LID system land uses.
  • [ Fig. 4. ]  Annual pollutant loads under current land use and the combination of green roofs and porous pavements (low impact development system). BMP: best management practice BOD: biochemical oxygen demand.
    Annual pollutant loads under current land use and the combination of green roofs and porous pavements (low impact development system). BMP: best management practice BOD: biochemical oxygen demand.
  • [ Table 10. ]  Annual pollutant loads under the current and LID land uses
    Annual pollutant loads under the current and LID land uses
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