LIZ DENMAN
Abstract
Stormwater management is shifting from systems that rapidly collect and discharge stormwater to nearby waterways towards more sustainable methods. These newer strategies aim to reduce contaminant load and the volume of runoff by incorporating stormwater treatment into the design of urban landscapes. The re-design of street tree rootzone environments is an option for incorporating stormwater treatment measures into streetscapes, where space is limited. This article details the performance of a pilot scale street tree bioretention system in reducing nitrogen loads in urban stormwater. Three tree species (L. confertus, E. polyanthemos and P. orientalis) and three soils of different hydraulic conductivity were tested in a randomised block design. Over the course of the experiment, all tree species displayed seasonal height growth patterns with maximum growth rates occurring in late Spring and Summer. Applications of stormwater increased height growth and root density compared with tapwater. Two species had significantly higher foliage nitrogen concentrations in trees receiving stormwater than those receiving tapwater. Tree growth was similar in the three soils studied. Leached nitrogen loads were significantly reduced in systems with a tree. Whilst there were some statistically significant differences in nitrogen removal between species, the output loads were all low compared to the unplanted systems. The difference between unplanted and planted profiles was consistent for the three forms of nitrogen measured: ammonium, oxidised nitrogen and organic nitrogen. Compared to the total nitrogen input (25.2 mg), the load leached in December 2004 from the L. confertus profiles following a 5 hour collection period was 95% less for the low SHC (1.4 mg), 85% for the medium SHC (4.1 mg) and 82% for the high SHC soils (4.6 mg). In the unplanted profiles the low SHC soil reduced nitrogen by 36% (16.2 mg), whereas the medium (25.2 mg, 0%) and high SHC soils (27.0 mg, -7%) did not remove nitrogen. Therefore, to achieve good nitrogen removal in these systems trees are required.
Keywords
Bioretention, Lophostemon confertus, Eucalyptus polyanthemos, Platanus orientalis, leachate, nitrate, ammonium, total nitrogen.
Introduction
Water Sensitive Urban Design (WSUD) aims to incorporate water cycle management initiatives into the design of urban landscapes. One goal of WSUD is reducing the negative impacts of stormwater discharge on aquatic environments, in terms of both runoff quality and quantity (Victorian Stormwater Committee 1999). Elevated nutrient levels contribute to eutrophication and in coastal ecosystems nitrogen is thought to be particularly important (Howarth & Marino 2005). Reducing the amount of nitrogen discharged from urban areas to the rivers and sea is therefore important.
The incorporation of stormwater management into urban landscapes is increasingly common. However, potential treatment measures are restricted in highly urbanised areas where space is limited. The re-design of street-tree rootzones is one option for incorporating stormwater treatment into such areas. This paper provides some detail from an experiment that was conducted to evaluate the potential for using street trees as elements of a bioretention system. In this paper, tree growth responses and nitrogen behaviour are reported.
Methods
The experimental method has been described previously (Breen et al. 2004). Briefly, trees were grown for 15 months in model soil profiles, which were built in above ground-containers. The species were Eucalyptus polyanthemos, Lophostemon confertus, Platanus orientalis and an unplanted control. Three soil treatments with different drainage rates (saturated hydraulic conductivities of 4, 95 and 170 mm/hr) were used and are referred to as, low, medium and high saturated hydraulic conductivity (SHC). Profiles were charged with tapwater (control) or a model stormwater solution weekly. The model stormwater solution, adapted from Davis et al. (2001), contained nitrate, organic nitrogen, phosphorus, copper and dissolved solids as sodium and magnesium chloride. No sediment was included. The total nitrogen load applied during each irrigation event was 25.2 mg, 8.4 mg N as nitrate and 16.8 mg N as glycine. In total the experiment contained 30 treatments with 8 replicates of each making a total of 240 experimental units.
Tree height was recorded monthly from September 2003 until January 2005. Relative height growth rate for each monthly interval (cm cm-1 week-1) is presented here. Foliage collected in January 2005 was oven dried (70°C), finely ground and then analysed for nitrogen content by the Dumas combustion method (Carlo Erbra, NA1500 Series II). For root analysis, a 400 mm long, 16 mm diameter, core sample was taken vertically from each profile in January 2005. The core samples were divided into four 100 mm long sections which were then halved lengthwise, to allow simultaneous analysis of both tree root growth and soil nutrient status. P. orientalis root length was measured with WinRHIZO (Regent Instrument Inc.) software using a flat bed scanner (Epson Expression 1680). Root lengths are reported as root length densities.
Leachate from the soil columns was collected for two hours after irrigation commencement. In December 2004 collection times were extended for another 3 hours from a sub sample of profiles to quantify the percent completeness of the standard collection. Leachate samples for nutrient analysis were stored at 4°C until analysed. Oxidised nitrogen (NOx) was analysed by an automated cadmium reduction method (Clesceri et al. 1998) with an Alpkem (Perstorp Analytical) segmented flow autoanalyser. Ammonium (NH3) was analysed with an automated phenate method (Clesceri et al. 1998) with a flow injection autoanalyser. Total nitrogen was determined as nitrate, following alkaline persulphate digestion (Clesceri et al. 1998). Organic nitrogen was calculated as the difference between total and mineral (NOx + NH3) nitrogen.
Results and Discussion
Tree growth parameters
Tree height
Figure 1 shows the relative height growth rate of E. polyanthemos, L. confertus and P. orientalis growing in the medium SHC soil from October 2003 to January 2005. The relative height growth rates were similar for all treatments. There appears to be a response to stormwater treatment during periods of accelerated growth. The species all exhibited seasonal changes in growth patterns with maximum growth rates occurring in late Spring and Summer. L. confertus also continued to grow through the Autumn months (Figure 1). Absolute height growth rates were significantly greater in the stormwater treatments compared with tapwater (Figure 2). In general there were no differences between height growth in the three soils used.


Foliage nitrogen
The significant interaction between species and water quality application for foliage nitrogen content is shown in Table 1. E. polyanthemos and P. orientalis receiving stormwater had significantly higher concentrations of foliage nitrogen than those receiving tapwater (Table 1). Stormwater application had no effect on foliage nitrogen concentration in L. confertus. There was no affect of soil on foliage nitrogen content.
Comparisons with published foliage data of the same or similar species suggests that the trees in this experiment were most likely nitrogen deficient (Table 1). Boardman et al. (1997) suggest 11–14 mg g-1 as an adequate concentration of foliage nitrogen for L. confertus. Dell (1996) reports Eucalyptus maculata foliage in the range of 10-12 mg g-1 nitrogen as deficient, while 17-26 mg g-1 indicates adequate nitrogen concentrations. Although not investigating critical levels for tree growth, Wood et al. (1977) reported foliage nitrogen concentrations of 17 mg g-1 in Platanus occidentalis trees growing on an unfertilised terrace site. Foliage nitrogen content was significantly higher in P. occidentalis following the addition of nitrogen fertiliser only (22.7 mg g-1) or nitrogen and phosphorus (21.8 mg g-1) fertiliser (Wood et al. 1977). Similarly, the nitrogen content of healthy looking Platanus x acerifolia ‘Bloodgood’ and Platanus occidentalis leaves were in the range of 16.2-27.3 mg g-1 (Mills & Jones Jr. 1996).
Table 1 Foliage nitrogen content (mg g-1) for the interaction between species and water quality
Species | Water quality yLSD = 0.9 | |
Tapwater | Stormwater | |
E. polyanthemos | 6.0 ab | 8.3 c |
L. confertus | 5.4 a | 6.3 ab |
P. orientalis | 9.9 d | 11.7 e |
y means followed by the same letter are not significantly (p<0.05) different

Root growth
Root length density of only P. orientalis is presented here. Root length measurements of E. polyanthemos and L. confertus, were not possible due to the presence of an apparent fungal association on the root samples (see Figure 3). The scanning equipment used to quantify root length was unable to distinguish between the roots and fungal mass. Dry weight will be used to estimate root growth for future reporting.
Analysis of P. orientalis root length density showed that the application of nutrients in the stormwater resulted in greater root growth. Interactions between depth/water quality and depth/soil were significant resulting in the pattern of root distribution down the profile varying between the water quality treatments. Root density peaked in the 100-200 mm zone for the control trees and then reduced significantly, to values similar to the surface, in the lower two zones (Table 2). In contrast, when stormwater was applied root density at the lowest two zones (200-300 and 300-400 mm) was similar to the 100-200 mm zone.
Table 2 P. orientalis root length density (cm cm-3): water quality and depth interaction
Water quality | Sample depth from surface (mm) yLSD=1.99 | |||
0-100 | 100-200 | 200-300 | 300-400 | |
Tapwater | 7.5 a | 10.5 c | 7.2 a | 8.2 ab |
Stormwater | 10.0 bc | 17.4 de | 15.9 d | 18.6 e |
y means followed by the same letter are not significantly (p<0.05) different
Table 3 P. orientalis root length density (cm cm-3): soil and depth interaction
Soil | Sample depth from surface (mm) yLSD=2.43 | |||
0-100 | 100-200 | 200-300 | 300-400 | |
Low SHC | 10.5 bcd | 15.2 g | 13.6 efg | 13.1 efg |
Medium SHC | 7.1 a | 13.7 fg | 11.3 cde | 14.6 fg |
High SHC | 8.6 ab | 12.9 efg | 9.7 bc | 12.5 def |
y means followed by the same letter are not significantly (p<0.05) different
In all three soils, root length density was lowest in the surface zone (0-100mm), significantly so except for one instance (High 200-300 mm). In the low SHC soil, root density was similar in the three lower zones (Table 3). The pattern differed in the medium and high SHC soils where root length density was significantly lower in the third zone, compared to the second and forth.
These tree height and root density results demonstrate that under the relatively high frequency of recharge events used in this experiment the trees were able to establish and grow successfully and there was an apparent response to the nutrients carried in the stormwater. P. orientalis, root growth was affected by the treatments in as much as roots were distributed through the profile in patterns that conform to expected behaviour. Especially encouraging was the uniform penetration of roots in the low SHC soil where it had been anticipated that low aeration would result in limited growth. Platanus has a reputation for tolerating poor soil aeration (Smith et al. 2001) and so this observation is perhaps not unexpected. The different distributions of roots in the medium and high SHC soils may be due to leaching of nutrients to lower parts of the profile in these more freely drained soils. Soil nutrient analysis will be used to validate this assumption. These data prove the concept in terms of plant success.
Nitrogen behaviour
NOx loads are presented for unplanted and planted (3 species averaged) for January, June and December 2004. Analysis of leachate volumes for these months is also provided to allow some assessment of the relationship between NOx load and concentration. Ammonium, NOx and Organic N loads leached from the planted profiles in December 2004 are also presented.
NOx Load: January, June and December 2004
The NOx leached from unplanted profiles was substantially greater than from planted systems in all three months (Figure 4). In the unplanted profiles all stormwater systems leached more NOx than tapwater systems. With the exception of the low SHC systems, this pattern was similar for the planted systems but much less pronounced. There was no difference between the loads leached from the low SHC for tapwater and stormwater. This suggests that low SHC can significantly influence nutrient retention. Some seasonal patterns seem evident, but are not considered to be significant in a practical sense.

Leachate volumes: January, June and December 2004.
In January, June and December 2004 leachate volumes from all systems were significantly affected by soil treatments (Table 4). In January and June the leachate volumes were statistically different with low SHC
Table 4 Leachate volumes (mL) in January, June and December 2004 in response to soil treatment
Soil | Month of leachate collection | ||
yJanuary 2004 (LSD = 137.6 ) | yJune 2004 (LSD = 172.8 ) | yDecember 2004 (LSD = 203.9 ) | |
Low SHC | 1367 a | 1950 a | 979 a |
Medium SHC | 1805 b | 2830 b | 1463 b |
High SHC | 1981 c | 3060 c | 1565 b |
y means followed by the same letter down the column are not significantly (p<0.05) different.
Table 5 Leachate volumes (mL) from all systems in January, June and December 2004: vegetation treatment and water quality interaction
Vegetation treatment | Water quality | Month of leachate collection | ||
yJanuary 2004 (LSD = 251.2) | June 2004 | yDecember 2004 (LSD = 263.2) | ||
E. polyanthemos | Tapwater | 1378 ab | 2559 | 1120 b |
Stormwater | 1291 ab | 2515 | 469 a | |
L. confertus | Tapwater | 1806 c | 2513 | 1714 c |
Stormwater | 1179 a | 2340 | 722 a | |
P. orientalis | Tapwater | 1478 b | 2897 | 991 b |
Stormwater | 1316 ab | 2758 | 516 a | |
Unplanted | Tapwater | 2675 d | 2586 | 2602 d |
Stormwater | 2795 d | 2711 | 2655 d |
y means followed by the same letter down the column are not significantly (p<0.05) different. Main effect (species) rather than interaction is significant in June.
In June 2004, the leachate volumes for the planted profiles were similar to the unplanted (Table 5). In this winter month, the leachate volumes were greatest from the P. orientalis profiles, and the difference between the P. orientalis profiles and the other two planted profiles was significant. In December 2004, the volume of leachate from the planted systems was significantly lower in stormwater treatments compared to tapwater. In contrast, the leachate volumes from the unplanted tapwater and stormwater treatments were similar. In January 2004, there was no difference between the water quality treatments for P. orientalis, E. polyanthemos and the unplanted, but as was the case for December the tapwater volumes were higher for L. confertus.
Leachate volumes were affected by the development of the trees (January > December 2004 and December tapwater > December stormwater), by season (June > December and January) and to some extent by species. In winter when P. orientalis had no leaves and therefore transpirational drying was reduced, the leachate volumes were significantly higher from this species.
Nitrogen in December 2004 leachate
Ammonium, NOx and Organic N loads were markedly lower in planted compared to unplanted systems. For both NOx and Organic N the loads from planted profiles receiving stormwater were not statistically greater than the unplanted tapwater controls when comparing the same soil treatment. As evidenced by increased tree height and root growth, the trees and potentially the soil microbes were clearly utilizing some of the nitrogen within the systems. The following sections detail the behaviour of NH3, NOx and Organic N in planted profiles only.
Ammonium
Analysis of the ammonium leachate load for L. confertus, E. polyanthemos and P. orientalis showed that the Species/Soil (Table 6) and Soil/Water Quality (Table 7) interactions were significant. In terms of species differences, in the low SHC soil significantly higher ammonium loads were leached from the L. confertus planted profiles as compared to the E. polyanthemos and P. orientalis. Although statistically significant, the differences are small in practical terms. In the medium and high SHC soils no statistically significant differences in ammonium leaching were found between the three species. The ammonium loads leached from the low, medium and high SHC soil profiles with tapwater were not statistically different. However, when stormwater charges were used the differences in ammonium leachate load between the three soils were significant with low < medium <high SHC (Table 7).
Table 6 Species and soil interaction for NH3-N load (mg) in December 2004 leachate, planted profiles
Species | ySoil | ||
Low SHCz | Medium SHC | High SHC | |
E. polyanthemos | 0.005 a | 0.036 bc | 0.065 bc |
L. confertus | 0.030 b | 0.045 bc | 0.054 bc |
P. orientalis | 0.006 a | 0.036 bc | 0.076 c |
y means followed by the same letter are not significantly (p<0.05) different. Means are log back transformed.
Zzero leachate volumes were measured for some of the E. polyanthemos and P. orientalis systems.
Table 7 Water quality and soil interaction for NH3-N load (mg) in December 2004 leachate, planted profiles
Water quality | ySoil | ||
Low SHC | Medium SHC | High SHC | |
Tapwater | 0.014 ab | 0.024 b | 0.019 b |
Stormwater | 0.007 a | 0.061 c | 0.216 d |
y means followed by the same letter are not significantly (p<0.05) different. Means are log back transformed.
Oxidised Nitrogen (NOx)
There was a significant species effect on NOx leaching (Table 8) and as with ammonium, the interaction between Soil and Water quality was also significant (Figure 5). In the medium and high SHC soils the NOx load from the stormwater treatments was significantly greater than from the tapwater (Figure 5). This was due to higher NOx concentrations in the stormwater charged leachate. In the low SHC soil, NOx load from the tapwater charged soil was higher than from stormwater, however the difference is not large in practical terms.

In terms of the species treatment effect, the NOx load leached from the L. confertus profiles was statistically greater than from the P. orientalis and E. polyanthemos profiles (Table 8). In comparison to the simulated stormwater input load (8.4 mg), these species differences in NOx load are small.
Table 8 NOx load (mg) leached from E. polyanthemos, L. confertus and P. orientalis systems in December 2004
Species | yNOx load (mg) |
E. polyanthemos | 0.27 a |
L. confertus | 0.42 b |
P. orientalis | 0.29 a |
y means followed by the same letter are not significantly (p<0.05) different. Means are log back transformed.
Organic Nitrogen
Organic nitrogen in leachate was determined by the calculation (TN – (NOx + NH3)). There was a significant species effect on organic N leaching load and the interaction between Soil and Water quality was also significant. As with NOx load, the Organic N load was higher in the L. confertus leachate than in the leachate from the P. orientalis and E. polyanthemos profiles (Table 9).
Table 9 Organic N load (mg) leached from planted systems in December 2004
Species | yOrganic Nitrogen load (mg) |
E. polyanthemos | 0.94 a |
L. confertus | 1.46 b |
P. orientalis | 1.03 a |
y means followed by the same letter are not significantly (p<0.05) different. Means are log back transformed.
There was a significant interaction between the Soil and Water quality treatments in terms of Organic N load (Figure 6). There was no difference between tapwater and stormwater treatments for the medium and high SHC soil. In the low SHC soil, the Organic N load leached from the stormwater treatments was significantly less than from the tapwater.

In the planted profiles, the two forms of mineral nitrogen measured in leachate tended to behave in a similar manner. Higher NH3 and NOx loads were lost from the stormwater medium and high SHC soils compared to the tapwater controls. In the low SHC soils loads were less in the stormwater than the tapwater treatments, significantly so in the case of NOx. Organic nitrogen behaved in a similar manner to NOx in the low SHC soil. In contrast to the inorganic nitrogen forms, the organic N leachate loads from tapwater and stormwater treatments in the medium and high SHC soils were similar. This indicates that the organic N applied in the stormwater was not being leached through the system. Mineralisation of the glycine added may be occurring between irrigation events, leading to higher discharges of ammonium in the stormwater treatments. The difference in ammonium leachate (low<medium<high SHC) presumably reflects less cation exchange (White 1997) or reduced reaction times in the sandier, faster draining soils.
Good reductions in nitrogen load were achieved in the planted profiles. Compared to the total nitrogen input (25.2 mg), the load leached after 5 hours from the L. confertus profiles was 95% less for the low SHC (1.4 mg), 85% for the medium SHC (4.1 mg) and 82% for the high SHC soils (4.6 mg). In the unplanted profiles the low SHC soil achieved a 36% (16.2 mg) reduction in the output load compared to the input. The unplanted medium (25.2 mg) and high SHC (27.0 mg) soils did not reduce nitrogen leaching. Trees are therefore a necessity in these proposed systems to reduce nitrogen loads, particularly if sandy, fast draining soils are used.
Conclusion
The trees were able to establish successfully and growth was enhanced by stormwater applications. Relative tree height growth rates were in practical terms similar for all treatments. Absolute height growth rates were greater for stormwater than tapwater treatments. P. orientalis and E. polyanthemos receiving stormwater had significantly greater nitrogen contents in their foliage than trees receiving tapwater. This water quality response was not seen in L. confertus. Foliage analysis suggests that nitrogen was limiting tree growth in the system. P. orientalis root length density was greater in response to stormwater and the differences were most pronounced in the lower half of the profiles. The leachate volumes in December 2004 were significantly less from trees receiving stormwater than tapwater, presumably due to these differences in tree growth. The presence of a tree resulted in significantly less nitrogen being leached from the systems. NOx and Organic N loads from the L. confertus systems were statistically higher than the other two species, although all these loads from planted systems were low compared to the nitrogen input. The species differences in loads were due to reduced leachate volumes in the Summer month rather than nitrogen concentrations and therefore suggest differences in transpiration rates rather than uptake efficiencies. The low SHC soil was more effective in reducing nitrogen losses, particularly the inorganic forms. However, the two faster draining soils would enable infiltration of larger volumes of stormwater in practice. Compared to the total nitrogen input (25.2 mg) the leachate loads in December 2004 following a 5 hour collection period were 82-95% reduced for the L. confertus profiles. However, the loads leached from the unplanted profiles ranged from a 36% reduction to a 7% increase in nitrogen output. The results suggest that street trees and their root zone soils can be successfully used as bioretention systems for nitrogen removal.
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