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EMPIRICAL STUDY ON EFFICIENCY AND SUSTAINABILITY OF SOIL PURIFICATION FACILITY FORDISCHARGED POLLUTANTS FROMROAD SURFACE

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Tiêu đề Empirical study on efficiency and sustainability of soil purification facility for discharged pollutants from road surface
Tác giả K. Yamada, T. Shiota, Y. Nagaoka, M. Shiono, K. Nishikawa
Trường học Ritsumeikan University
Chuyên ngành Environmental Systems Engineering
Thể loại Bài báo
Năm xuất bản 2005
Thành phố Kusatsu
Định dạng
Số trang 8
Dung lượng 445,33 KB

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Abstract Penetration experiments were carried out for a period of over two years at an experimental field located in Kusatsu City. The field was divided into two tanks and each tank filled with different types of soil. Polluted water discharged from the road surface was supplied to the field during storm events. The effluent from the field was composed of Surface and Infiltrated flow. The flow was gauged at three points and water sampled for quality analysis. In order to analyze measures against clogging, soil in one tank was replaced to investigate the recovery of soil contents, penetration efficiency, and purification efficiency. The other tank was researched continuously for 26 months to analyze the change of purification efficiency with precipitation characteristics and the continuous use the facility. Sustainability was analyzed by modeling long-term mass balance in the facilities using water quality data (COD, N, P and SS) and comparing the results with actual measured data of the change of pollutants in the soil. The facility achieved high pollutant removal efficiencies of between 50% - 90% during the survey. Simulation results using water quality data compared well with actual measured data of change of pollutants in soil

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EMPIRICAL STUDY ON EFFICIENCY AND SUSTAINABILITY OF SOIL PURIFICATION FACILITY FOR DISCHARGED POLLUTANTS FROM ROAD SURFACE

K Yamada1, T Shiota1, Y Nagaoka1, M Shiono2 and K Nishikawa3

1 Department of Environmental Systems Engineering, Ritsumeikan University, 1-1-1 Nojihigashi, Kusatsu, Shiga, 525-8577, Japan (E-mail: yamada-k@se.ritsumei.ac.jp)

2 Agrex Co Ltd., STS Bldg., 5-12-8, Nishinakajima, Yodogawa-ku, Osaka-shi, Osaka 532-0011, Japan (E-mail: masayuki_shiono@agrex.co.jp)

3 NJS Consultants Co Ltd., 9 -15 Kaigan 1 –Chome, Minato-ku, Tokyo 105-0022, Japan (E-mail: kouichi_nishikawa@njs.co.jp)

Abstract

Penetration experiments were carried out for a period of over two years at an experimental field located in Kusatsu City The field was divided into two tanks and each tank filled with different types of soil Polluted water discharged from the road surface was supplied to the field during storm events The effluent from the field was composed of Surface and Infiltrated flow The flow was gauged at three points and water sampled for quality analysis In order to analyze measures against clogging, soil

in one tank was replaced to investigate the recovery of soil contents, penetration efficiency, and purification efficiency The other tank was researched continuously for 26 months to analyze the change of purification efficiency with precipitation characteristics and the continuous use the facility Sustainability was analyzed by modeling long-term mass balance in the facilities using water quality data (COD, N, P and SS) and comparing the results with actual measured data of the change of pollutants in the soil The facility achieved high pollutant removal efficiencies of between 50% - 90% during the survey Simulation results using water quality data compared well with actual measured data of change of pollutants in soil.

Keywords

Road surface runoff, soil purification facility, model

INTRODUCTION

Lake Biwa is the largest lake in Japan, and it covers 1/6 of land area of Shiga Prefecture The water quality of the lake has been leveling off since 1980, and does not meet environmental standards (Figure 1) Thus, despite various measures undertaken to control pollution such as setting of environmental and effluent standards and construction of wastewater treatment plants, the water quality has not improved This is attributed to diffuse sources of pollution which are a significant source of pollution to the lake (Figure 2) Among diffuse sources of pollution, those from urban areas have increased due to increase in number of impermeable residential areas and surfaces Road surface runoff contributes a high proportion

of this pollutant load and therefore requires appropriate measures Soil penetration is considered as one of the measures

Figure 1 Trend of water quality of Lake Biwa, Shiga Prefectural Government (2004)

0 0.01 0.02 0.03

Environmental Standard

T-P

0

1

2

3

4

5

Environmental Standard

COD

0 0.1 0.2 0.3 0.4 0.5

Environmental Standard

T-N

00 0 1

1 9 9 5

T-South Lake North Lake

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Figure 3 Experimental facilities

In this study, purification of storm water runoff from road surface using a soil penetration demonstration experiment facility was investigated The decrease of penetration capacity and purification efficiency during continuous use of the facility was investigated The facility consisted of two tanks In one of the tanks, continuous use of the facility and change in purification efficiency depending on precipitation characteristics were analyzed with the results of experiments carried out over a period of 26 months starting in 2001 The soil in the other tank was replaced to consider measures against clogging by analyzing the recovery of soil contents, penetration efficiency and purification efficiency Sustainability was analyzed by modeling long-term mass balance in the facilities using water quality data (COD, N, P and SS) The calculated results were then compared with actual

measured data of the change of pollutants in the soil This study

was a continuation of earlier studies whose results are reported

elsewhere (Sugihara et al., 2000; Nishikawa et al., 2001;

Nishikawa et al., 2002)

Figure 2 Pollutant load going into Lake Biwa (Shiga Prefectural Government, 2004)

OUTLINE OF SURVEY

Experimental field and soil penetration facility

The outline of the soil penetration facility is shown

in Figure 3 and Table 1 The facility consisted of two

parallel soil tanks; Tank A and Tank B (Figure 3)

each with soil of 45 cm depth Tank A consisted of

two types of soil, 5 cm deep Akadama soil in the top

layer and 40 cm deep pit sand in the bottom layer

Tank B consisted of only pit sand Soil replacement

was carried out in Tank B in 2003 Runoff water

from 750 m2 of road surface area flows into the soil

penetration facility Inflow water leaves the facility

as Overflow or Infiltrated water The bottom of the

facility is covered with a water proof sheet to

comprehend the water balance Water that penetrates

through the soil is gathered at the bottom of the

facility and drained by a drainage pipe provided at

the bottom This water is referred to here as

Infiltrated water As Inflow water increases,

surface flow goes over the weir and is drained

This is called Overflow

Outline of measurement

The amount of Inflow water, Infiltrated

Industrial Agricultual

Land

Total amount

of Loads (t/day)

Water flow

Akadama soil

Pit sand

Points of Soil sampling

Points of Flow measurement and Water sampling

Soil

Inflow water

Infiltrated water

Overflow water

Weir

Weir

Overflow water

Infiltrated water

7m Inflow

Tank A

Tank B

Soil penetration facility 24.5m 2 ×2

Road Surface 750m 2

T-P T-N

13%

10%

28%

20%

29%

56.1

(t/day)

'95

15%

21%

34%

14%

16%

44.7 (t/day)

'05(Forecast)

16%

6%

26%

16%

36% 21.6 (t/day)

'95

27%

11%

8%

39%

15%

20.1 (t/day)

'05(Forecast)

16%

5%

39%

27%

13%

1.35 (t/day)

'95

36%

8%

19%

22% 15%

1.08 (t/day)

'05(Forecast) COD

Table 1 Outline of experimental facility

Lower layer Soil type

Pit sand (45)

Surface area Depth

Height

of weir Upper layer

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water and Overflow water were measured by a flow meter In addition, water quality analysis, soil content measurement and water permeability tests were carried out There were 219 rainfall events over the duration of the experiment Flow measurements for Inflow water, Infiltrated water and Overflow water were undertaken for all the rainfall events using an automatic flow meter installed on site Sampling for water quality analysis was done for 14 of the rainfall events (Table 2) SS, T-COD, T-N, T-P, D-COD, D-N and D-P were targeted in water quality analysis Soil was sampled from both the surface and at a depth of 5cm for soil content analysis In Tank A, which consisted of two types of soil, only Akadama soil was sampled Sampling was done at three sites at the upstream, mid-stream and downstream as shown in Figure 3 Soil sampling was done 22 times Carbon, nitrogen, phosphorus and particle size were targeted

in soil content measurement Sediments were collected from the road surface and analyzed for nitrogen, phosphorus and carbon content Permeability tests were done at three locations near the points used for soil sampling To measure permeability, the amount of water that flowed through a pipe installed in the soil over a fixed period of time was determined Permeability tests were undertaken 25 times (Table 2)

Table 2 Characteristics of selected storm events

-Water quality survey ID

Ave

rainfall intensity (mm/hr)

Antecedent days (day) Date

Precipi tation (mm)

Duration (hr)

Soil content survey ID

Water permeability survey ID

Max

rainfall intensity for 10 min (mm/hr)

Antecedent days (day) Date

Water

quality

survey

ID

Soil

content

survey

ID

Water permeability survey ID

Precipi tation (mm)

Duration (hr)

Ave

rainfall intensity (mm/hr)

Max

rainfall intensity for 10 min (mm/hr)

RESULTS AND DISCUSSION

Survey results

T-N content ratio Figure 4 shows the results of nitrogen content in the soil For Tank A the data

correspond to the content in the top layer Akadama soil only while for Tank B the data correspond to content in pit sand The initial nitrogen content of Akadama sand in Tank A was higher than that of pit sand of Tank B The nitrogen content in both Tanks increased with time In both Tank A and B, the content of nitrogen in the surface soil leveled off to a value comparable to that of sediment collected from the road surface (3.4 mg/g) The nitrogen content of soil at 5 cm depth remained constant from the start of the survey but begun to rise at a relatively slow rate at about the same time that the nitrogen content in the top soil begun level off In Tank B, after the soil was replaced (at 645 days) the nitrogen content recovered to almost the same level as that at the initial state The results of the subsequent measurements

showed an increasing tendency in nitrogen content similar to the situation before soil replacement

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The above results show that the nitrogen content in the soil at 5 cm did not rise significantly above the initial content at the start of the survey In other words, the results of the soil content survey showed that most of the nitrogen was stored in the upper 5 cm depth of the soil during 26 months (804 days)

Figure 4 T-N content in soil

Removal efficiency For the purpose of evaluating pollutant removal efficiency, Gross Removal Efficiency

(GRE) and Net Removal Efficiency (NRE) were defined as follows:

GRE = (Pollutant load held in soil)/( Pollutant load of Inflow) (1) NRE = (Pollutant load held in soil)/( Pollutant load of Inflow – Pollutant load of Overflow) (2) GRE and NRE are shown in Figure 6 GRE ranged between 60 – 95% and 20 – 95% for Tank A and Tank

B, respectively Except for the first three initial surveys, the average GRE in Tank A were about 75% for T-COD and T-P, 65% for T-N and 90% for SS In tank B, though the Overflow ratio (surface Overflow water / Inflow water) was comparatively high, the corresponding GRE values were about 60% for T-COD, 60% for T-P, 50% for T-N and 85% for SS before soil replacement The GRE values after soil replacement showed almost similar values as those before soil replacement, contrary to the expectation that the removal efficiency would improve with soil replacement In particular, for SS the average removal efficiency after soil replacement decreased to nearly 60%

On the other hand, NRE was higher than GRE by about 10% in Tank A, 20% in tank B before soil replacement and 5-20% in Tank B after soil replacement The relatively higher NRE for Tank B compared

to Tank A is due to the fact that the Overflow ratio was relatively higher in Tank B As with GRE, the NRE in Tank B after soil replacement was lower than that before soil replacement This could be attributed to the fact that the soil was unstable after replacement and therefore some of the soil may have flowed out together with infiltrated water However, the removal efficiencies after soil replacement show

an increasing tendency with time In particular, the removal efficiencies for the last two surveys after soil replacement (survey No wps13 and wps14) show a relatively high increase, indicating that the soil may have stabilized There is need to further study the recovery of purification capacity

0

1

2

3

4

5

Days

Days

0 1 2 3 4 5

Days

Surface Surface (after soil replacement) 5cm Depth 5cm Depth (after soil replacement)

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Figure 6 Pollutant removal efficiency in Tank A (upper graphs) and Tank B (lower graphs)

Simulation of long-term mass balance

Flow A conceptual diagram of mass balance in the soil treatment facility is shown in Figure 7

Simulation of long-term mass balance is considered for Tank A only where continuous survey was undertaken The effect of rainfall characteristics on the mass balance was investigated by classifying the rainfall events into 7 types according to the average rainfall intensity and the precipitation (Table 3)

Figure 7 Conceptual diagram of mass balance

Road surface runoff (Ro) was calculated as follows:

Ro = rr×(R - Iw) (3)

Table 3 Classification of rainfall

Net removal efficiency in soil Gross removal efficiency

0 20 40 60 80 100

Analysis No.

0 20 40 60 80 100

Analysis No.

0 20 40 60 80 100

0 20 40 60 80 100

0

20

40

60

80

100

0

20

40

60

80

100

Analysis No.

R

O LO

Ro

LRo

I

LI

(Rainfall)

(Road surface runoff)

(Pollutant load of road surface runoff)

(Inflow water)

(Pollutant load of inflow)

(Overflow water) (Pollutant load of Overflow)

D LD

S

LS

F

LF

(Infiltrated flow)

(Pollutant load of infiltrated flow)

(Water held in soil)

(Pollutant load of water held in soil)

Infiltrated water Pollutant load of infiltrated water

Road Surface

Soil Field

F=I-O LF=LI-LO S=F-D LS=LF-LD

Rainfall type

Precipitation

R (mm)

Ave rainfall intensity

I (mm/hr)

B C D

3.0≦R <20.0

I <1.0

1.0≦I <4.0 4.0≦I

E F G

20.0≦R

I <1.0

1.0≦I <4.0 4.0≦I

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In Equation (3) rr is Road surface runoff ratio, R is precipitation (L) and Iw is Initial lost water (L) Initial

lost water was calculated by the amount of initial rainfall and the measured value of Road surface runoff According to Equation (1), rr was calculated as the slope of the regression equation of measured Road surface runoff and the difference between precipitation and Initial lost water Typical calculation results for rr for rainfall of type A are shown in Figure 8 The calculated values of runoff ratios are given in Table

4 The relationship between values of Ro estimated by Equation (3) and measured values is shown in

Figure 9

The gross quantity of Flow into soil (F) and Water held in soil (S) for one rainfall event were calculated from measured values of gross Inflow water (I), Overflow water (O) and Infiltrated water (D), as follows

(all units in liters):

F = I – O = I×(1 – ro) (4)

S = F – D (5)

In Equation (5), ro is Overflow runoff ratio of flow The Overflow runoff ration of flow is related to

Inflow water, cumulative rainfall, antecedent days of no rain and average of rainfall intensity Multiple

linear regression analysis with these four factors set as explanatory variables was used to calculate ro as

follows (Figures 10 and 11):

4

3 3

2 2

5 1

10

2

1 × − x + × − x + × − x + − × − x + − × − (6)

In Equation (6), x1 is Inflow water (L), x2 is cumulative rainfall (mm), x3 is the number of antecedent days

of no rain (days), and x4 is average of rainfall intensity (mm/hr)

R2 = 0.16

R2 = 0.42

R2 = 0.32

0.0 0.2 0.4 0.6 0.8 1.0

Ave rainfall intensity(mm/hr)

0 5000 10000 15000

Actual measurement(L)

Figure 9 Estimated and measured Road surface runoff

Figure 8 Road surface runoff and

precipitation (rainfall type A)

Table 4 Road surface

R2 = 0.8183

0 500 1000 1500

Precipitation reduced initial lost(L)

Precipitation reduced by initial lost water (L)

R2 = 0.04

R2 = 0.05

R2 = 0.06

0.0

0.2

0.4

0.6

0.8

1.0

Antecedent days (day)

2000mm~

△ 1000mm~2000mm

Figure 10 Overflow runoff ratio

and antecedent days of no rain

Figure 11 Overflow runoff ratio and rainfall intensity

Rainfall

type

Runoff ratio,

rr

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Figure 15 Overflow runoff ratio of load and flow

Figure 16 Estimated and measured values of pollution load (T-N)

The relationship between gross Flow into Soil (F) and gross Infiltrated water (D) is shown in Figure 12,

and the regression equation is given in below:

The relationship between values estimated by the model and values measured by water quality survey and flow rate survey is shown in Figure 13

Figure 12 Infiltrated water and Flow into soil

Mass balance of pollution load Pollution load was calculated by the relationship between Road surface

runoff (Ro) and Pollutant load from road surface runoff (LRo) As an example, the following relationship

was established for T-N (Figure 14):

LRo=0.5833×Ro0 3785 (8)

The amount of pollutant load in overflow was calculated by the regression analysis of Overflow runoff

ratio of flow (ro) and Overflow runoff ratio of load (Lro) The following relationship was established for

T-N (Figure 15):

Lro=0.6059×ro (9)

T-N

R2 = 0.5291 0

10

20

30

40

50

Surface runoff, Ro (L)

0 5000 10000 15000 20000

measured value(L)

R2 = 0.9451

0

5000

10000

15000

volume of Flow into soil:F(L)

Figure 14 Pollutant load

and Road surface runoff

Figure 13 Estimated and measured values of flow

Overflow runoff ratio (flow), ro (%)

R2 = 0.966

R2 = 0.939

R2 = 0.8874

R2 = 0.9284

0 10 20 30 40 50

0 5 10 15 20

measured load(g)

Measured load (g)

Measured value (L)

Flow into soil, F (L)

△ Pollutant load held in soil Pollutant load in overflow Pollutant load into soil

Trang 8

Measured values of Pollutant load into soil (LS) and Pollutant load infiltrated (LD) were calculated from

water quality analysis data The relationship between the measured values and values estimated by the

model equations above is shown in Figure 16

Comparison between simulation results based on water quality data and actual measurement data of

pollutant load in soil Gross water flow and gross pollutant load of road surface runoff, overflow water,

flow into soil, infiltrated water and water held in soil were calculated for all the precipitation data (total

precipitation 3,300 mm) from September 2001 to November 2003 The simulation results of gross water

balance and gross pollutant load balance are shown in Tables 5 and 6, respectively From the results of

soil content survey before and after the simulation term, the contents of pollutants at 5 cm-depth and

surface soil were calculated, assuming the following values: specific gravity as 2.65, void ratio as 50%

and proportion of particles under 75 µm as about 35% Comparisons of increase in soil pollutant content

amounts are shown in Table 6 Simulation results of (LS) compared well with measured data

Table 5 Simulation results of gross water balance (mm)

I O F D S

Table 6 Simulation results of gross pollutant load balance and increased soil contents (g)

Pollutant load of inflow water (LI) 1699.5 511.9 179.8 123.1

Pollutant load of overflow water (LO) 228.4 69.1 21.4 11.8 Model simulation Pollutant load of flow into soil (LF) 1471.1 442.8 158.3 111.3

Pollutant load of infiltrated water (LD) 423.6 57.0 20.6 9.2

Pollutant load of water held in soil (LS) 1047.9 385.8 137.8 102.2 Actual measurement Increase in pollutant amount in soil 1006.4 145.8

CONCLUSIONS

Sustainability of a soil penetration facility for storm water runoff was analyzed by carrying out a mass

balance analysis using data measured from surveys of permeability, flow rate and water quality The

simulation results were compared with actual measured data of pollutant content in soil The following

results were obtained:

1 Nitrogen accumulated in the upper 5 cm layer of soil in of the soil purification facility

2 Average pollutant removal efficiencies of 50% - 90% were obtained for COD, N, P and SS An

obvious decline in pollutant removal efficiency was not seen in the facility over the two years the

survey was carried out However, further studies are needed to investigate recovery of the pollutant

removal efficiency after soil replacement

3 Mass balances of flow and pollutant load in the penetration facility were carried out Regression

equations relating flow and pollutant load to rainfall characteristics were established

REFERENCES

Sugihara, M., Yamada, K., and Terada, A (2000) Study on soil filtration treatment for pollutants from

road surface during storm events Proceedings, 3rd Annual Symposium, JSWE, 95-96

Nishikawa, K., Sugihara, M and Yamada, K (2001) Study on soil penetration facility for pollutants

discharged from road surface Proceedings, 56th Annual Meeting, JSCE, 488-489

Nishikawa, K., Sugihara, M., and Yamada, K (2002) Study on removal by soil of pollutants discharged

from road surface during storm events Proceedings, 6th International Conference on Diffuse Pollution,

IWA, 616-621

Shiga Prefectural Government (2004) http://www.pref.shiga.jp/index.html

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