Environmental Pollution 133 (2005) 265–274 www.elsevier.com/locate/envpol Influence of temperature and salinity on heavy metal uptake by submersed plants Å. Fritioff*, L. Kautsky, M. Greger Department of Botany, Stockholm University, S-106 91 Stockholm, Sweden Received 21 November 2003; accepted 31 May 2004 Metal concentrations increase with increasing temperature and decreasing salinity in two aquatic plants. Abstract Submersed plants can be useful in reducing heavy metal concentrations in stormwater, since they can accumulate large amounts of heavy metals in their shoots. To investigate the effects of water temperature and salinity on the metal uptake of two submersed plant species, Elodea canadensis (Michx.) and Potamogeton natans (L.), these plants were grown in the presence of Cu, Zn, Cd, and Pb at 5, 11, and 20 C in combination with salinities of 0, 0.5, and 5&. The metal concentrations in the plant tissue increased with increasing temperature in both species; the exception was the concentration of Pb in Elodea, which increased with decreasing salinity. Metal concentrations at high temperature or low salinity were up to twice those found at low temperature or high salinity. Plant biomass affected the metal uptake, with low biomass plants having higher metal concentrations than did high biomass plants. Ó 2004 Elsevier Ltd. All rights reserved. Keywords: Elodea canadensis; Potamogeton natans; Phytoremediation; Stormwater; Cd; Cu; Zn; Pb 1. Introduction Submersed plants may be useful in reducing heavy metal concentrations in stormwater, since they have the ability to take up heavy metals directly from water and accumulate them in their shoots (St-Cyr et al., 1994; Coquery and Welbourn, 1995; Greger et al., 1995; Rai et al., 1995; Jackson, 1998). Stormwater comprises rainwater and meltwater draining from hard surfaces, such as roads and roofs in urban areas, and often contains heavy metals, in particular Cu, Zn, Cd, and Pb (Morrison, 1989; Sansalone et al., 1996; Boller, 1997; Pettersson et al., 1999). The metal uptake of submersed plants may be influenced by several factors, including * Corresponding author. Tel.: C46 8 161348; fax: C46 8 165525. E-mail address: fritioff@botan.su.se (Å. Fritioff). 0269-7491/$ - see front matter Ó 2004 Elsevier Ltd. All rights reserved. doi:10.1016/j.envpol.2004.05.036 pH, redox potential, and surrounding metal concentrations as well as the temperature and salinity of the surrounding stormwater. The chemistry of stormwater is highly variable depending on its origin, on rain intensity, and on the season; its pH, however, is often around 7 (Pettersson, 1999). In a temperate climate, like that of Sweden, the temperature and salinity of stormwater vary with the season: the water temperature may exceed 20 C in the summer and can decrease to below 0 C in the winter. Salinity is very low most of the year, but salinities up to 5& have been measured (Wittman, 1979; Sandersson, 1997; Christer Lännergren, pers. comm.) during winter when NaCl is used for deicing roads. During summer, slightly elevated salinities up to 0.5& can be measured (Wittman, 1979; Sandersson, 1997; Christer Lännergren, pers. comm.), probably due to the resuspension of sediment (Odum, 2000). 266 Å. Fritioff et al. / Environmental Pollution 133 (2005) 265–274 Water temperature may influence water chemistry, metal solubility, metal uptake by plants, and plant growth. According to Zumdahl (1992), seasonal variation in water temperature has no direct effect on the solubility of metal in water. However, cool water contains more dissolved oxygen than does warm water. Thus, metal concentration in the interstitial water of the sediment may decrease with decreasing temperature, as more metals are bound to sediment colloids at high rather than low redox potentials (Förstner, 1979). In addition, temperature has a profound effect on plant growth rates and higher temperatures will thus result in greater biomass production and distribution of submersed macrophyte communities (Marschner, 1995; Rooney and Kalff, 2000). A plant of relatively high biomass may have a greater metal uptake capacity; this results from lower metal concentration in its tissue because of a growth rate that exceeds its uptake rate (Ekvall and Greger, 2003). Changes in temperature further change the composition of the plasma membrane lipids (Lynch and Steponkus, 1987). This alters the plant membrane fluidity, resulting in lower membrane permeability at low temperatures and lower metal uptake (Marschner, 1995). In the aquatic environment, the Cu adsorption to the alga Dunaliella tertilecta increases with increasing temperature (Gonzalez-Davila et al., 1995). Further, in the lichen Peltigera horizontalis (Huds.) (Beckett and Brown, 1984) and the liverwort Dumortiera hirsuta (Sw.) (Mautsoe and Beckett, 1996), both intracellular and extracellular uptake of Cd was stimulated by an increase in temperature. Similarly, several studies of terrestrial plants grown at high root temperatures found higher uptakes of Zn, Pb, Ag, Cr, Sb, and Cd than was the case with plants grown at low root temperatures (Hooda and Alloway, 1993; Macek et al., 1994; Baghour et al., 2001; Albrecht et al., 2002). Therefore, a general increase of metal uptake with increasing temperature seems likely. The salinity of stormwater may affect the plant growth rate and plant metal uptake through the toxic effects of both the NaC and Clÿ ions. NaC ions may release Cd from the sediment to the water, thereby increasing the Cd concentration in the water (Greger et al., 1995). In seawater, chloride commonly forms complexes with Zn, Cd, and, to a lesser extent, Cu, but not with Pb, and thus the free ion concentration of the former metals will be reduced (Förstner, 1979; Williams et al., 1994). Fewer free Cd ions in water of higher salinity correlates with a lower uptake of Cd by Potamogeton pectinatus (L.) growing in higher salinity water (Greger et al., 1995). At a higher salinity, the increased NaC concentration reduced both intracellular and extracellular uptake of Cd in the free-floating plant, Lemna polyrhiza (L.) (Noraho and Gaur, 1995). Not only in submersed (Greger et al., 1995) and free-floating (Noraho and Gaur, 1995) plants, but also in macro- algae, such as the seaweed Fucus vesiculosus (L.), did the uptake of metal (Zn) decrease with increasing salinity (Munda and Hudnik, 1988). Thus, a general decrease in metal uptake with increasing salinity could be expected. Variations in the temperature and salinity of stormwater result in different combinations of these two factors over the course of a year (Wittman, 1979; Sandersson, 1997). In winter/early spring, low temperature is combined with low to high (5&) salinity, while in summer, high or medium temperatures are combined with low to medium (0.5&) salinity. Furthermore, in late autumn/early winter both temperature and salinity may be low. To the best of our knowledge, no investigation has as yet determined the effects of temperature in combination with salinity on the heavy metal uptake of submersed plants. This study evaluates the combined effects of temperature and salinity on the uptake of a set of heavy metalsdCu, Zn, Cd, and Pbd in two morphologically different submersed aquatic plant species, Elodea canadensis and Potamogeton natans. In a previous study (Fritioff and Greger, 2003), these two species were shown to accumulate higher concentrations of heavy metals when grown in stormwater ponds than were emergent species sampled. Although these are known as freshwater species, they also grow in somewhat brackish water (Luther, 1951). Furthermore, both species grow in ponds and wetlands until an ice layer covers the water surface. Our hypotheses were that metal concentrations and accumulations in submersed plant species would: (1) independent of salinity, increase with increasing water temperature and (2) independent of temperature, decrease with increasing salinity. 2. Materials and methods 2.1. Plant material The two studied species commonly grow in stormwater treatment ponds and wetlands. Although both are submersed, E. canadensis (L.) and P. natans (Michx.) have quite different morphologies. Elodea has very thin submersed leaves, almost lacking a cuticle, arranged around the stem, giving a high surface-to-volume ratio. In contrast, Potamogeton has long petioles and leaves that are several cell layers thick floating on the water surface. These leaves are covered with a comparatively thick cuticle, resulting in a much lower surface-tovolume ratio. Both studied species grow and remain green until an ice layer covers the wetland (during cold winters), causing a die back. Below the ice, Potamogeton over-winters by means of its hardy rootstocks, while Elodea over-winters by means of short vegetative shoots. Whole plants of Potamogeton were collected in August 2001 from an unpolluted pond called Å. Fritioff et al. / Environmental Pollution 133 (2005) 265–274 Skåbydammen, located south of Stockholm, Sweden. Plants were gently cleaned with tap water to remove the sediment, planted in a greenhouse pond containing tap water and minimally contaminated sediment, and left growing for 4 weeks until the start of the experiment. For Elodea, 10-cm-long vegetative shoots were collected from a greenhouse pond. The shoots were planted in a new pond containing the same types of sediment and water as did the pond containing the Potamogeton plants, and grown for about 5 weeks until new vegetative shoots had developed. 2.2. Growth conditions The two species were grown in a greenhouse equipped with supplementary lamps. During the pre-experimental phase, Osram daylight lamps (HQI-BT 400W) were used for a light period of 12 h. Temperature in the pond water was 18 G 1 C. The acclimatization and experimental phases were carried out in a climate-controlled chamber with an air temperature of 10 G 1 C. Halogen lamps (Osram Poverstar HQI-E) were used to create light intensity of 50 G 5 mmol photons mÿ2 sÿ1 for a light period of 18 h. 2.3. Experiment To study the effects of salinity and water temperature on the heavy metal uptake of Potamogeton and Elodea, a two-factorial design, 32 (Sokal and Rohlf, 1995), was set up with temperature and salinity as the two factors. Each Potamogeton plant (with 1–5 leaves) was thoroughly cleaned under running tap water to remove sediment and other particles and then rinsed in redistilled water before being put in a container containing 2 L of 2% Hoagland medium (Eliasson, 1978) with a pH of 5.0 G 0.2; the medium was not aerated. In the experiment with Elodea, four vegetative shoots (one each of 10, 15, 20, and 25 cm in length) were cut and placed together in each container, a single container comprising one replicate. Seven replicates were used for each treatment and each species. Containers with plants were randomly placed in large, waterfilled tubs. Water in one-third of the tubs was chilled to 5 C using a compressor (TECO RA 680, Italy), thermostats (Jäger, Type LZRH, Wüstenrot) to keep it at 20 C, heated the water of another third of the tubs and the water of the remaining third of the tubs was kept at 11 C. To reduce evaporation, all containers were covered with transparent plastic film. After 10 days of acclimatization, the fresh weights (FW) of the individuals of both species were measured after first gently shaking the plants for 10 s to remove water. Additionally, the lengths of the Elodea plants were measured. Plants were then again set in containers of fresh medium kept at the same temperatures as before. 267 After another day of acclimatization, plants from three containers at each temperature were used to determine the baseline heavy metal content in the plants. Thereafter, heavy metals and NaCl were added to all containers. To simulate a storm event, when a flush of highly polluted water originating from rainfall enters the pond, the plants were treated for 48 h with metal levels of 1.5, 20, 1, and 4 mM (equal to 95, 1307, 112, and 836 mg Lÿ1) of Cu, Zn, Cd, and Pb, respectively (Morrison, 1989; Sansalone et al., 1996; Boller, 1997; Pettersson et al., 1999). Then, NaCl was added, which resulted in final salinity levels of 0, 0.5, and 5&. After 48 h, the experiment was ended and the fresh weights of plants were measured as well as the length of the Elodea plants. The pH remained at 5.0 G 0.1 for the duration of the experiment. All plants of both species were rinsed twice in redistilled water, once in 20 mM EDTA, and twice in redistilled water, for half a minute each time. They were dried at 105 C for 24 h and then weighed to determine the plant dry weights (DW). All plant materials from each container was wet digested in concentrated HNO3:HClO4 (7:3, v:v). Metal concentration was measured using a flame atomic absorption spectrophotometer (SpectrAA-100, Varian, Springvalve, Australia). Standards were added to the samples to eliminate the interaction of the sample matrix. Lagharosiphon major was used as a reference material (BCR No 60 N 675, Commission of the European communities). 2.4. Calculations and statistics Dry weight-to-fresh weight ratios (DW/FW) were calculated for both species. To determine the growth rate, the increase in fresh weight of Potamogeton and the increase in length of Elodea during the 48-h experimental period were calculated as g FW (24 h)ÿ1 and cm (24 h)ÿ1, respectively. Metal accumulations during the experiment were calculated by subtracting control concentrations from the concentrations found in the treated plants. The effects of the fixed factors, temperature and salinity, on Zn, Cu, Cd, and Pb concentrations in Potamogeton and Elodea were analyzed in a general linear model which used biomass ( g DW Lÿ1) as a covariable, in order to sort out the effects of the various factors on the metal concentrations in the two plant species. Insignificant interactions with the continuous covariable were dropped from the model using a backward elimination procedure. Analysis of the metal accumulations was preformed in the same way. Tukey’s honest significant difference was used as a post hoc test (Statistica software, StatSoft Inc., ’99 edition, kernel release 5.5 A). 268 Å. Fritioff et al. / Environmental Pollution 133 (2005) 265–274 3. Results Growth rate, measured as increase in length (cm ! 24 hÿ1), increased significantly with increasing temperature for Elodea (Table 1). Furthermore, Elodea plants grew significantly longer (cm) in containers kept at 20 C than in containers kept at colder temperatures. The DW/FW ratio (%) was significantly higher in Elodea subject to colder rather than warmer treatments. The dry and fresh weights of Elodea per liter did not differ significantly among treatments. For Potamogeton, no significant differences in dry or fresh weights, DW/ FW ratios, or growth rates ( g FW ! 24 hÿ1) were found among treatments. The plant fresh weights were slightly higher for Potamogeton than for Elodea, while the plant dry weights and DW/FW ratios were more than twice as high for Potamogeton as for Elodea. Because of the higher biomass (DW lÿ1) of Potamogeton than of Elodea (Table 1), total metal accumulations (mg containerÿ1) in the plant material of Potamogeton in some cases exceeded those of Elodea (Fig. 1). Thus, compared with Elodea, Potamogeton removed more of the added Zn from the medium in all treatments and more Cu and Cd from the medium in the 5 C treatment. However, the metals added to the nutrient solution were never depleted in any of the treatments. The metal concentrations in the plants at the end of the experiment are shown in Table 2. Elodea had, with a few exceptions in the case of Zn, higher concentrations of heavy metals than did Potamogeton in both treated and control plants. Except for Cu in Elodea at 5 C and 5& salinity, controls had lower metal concentrations than did the treated plants. Concentrations of each metal in the control plants did not differ significantly among temperature treatments. The metal concentrations in plants increased with increasing temperature in most cases (Fig. 2, Tables 3 and 4). This was found to be significant in Elodea for Cu, Zn, and Cd and in Potamogeton for Cu, Cd, and Pb, and a tendency was found in Potamogeton for Zn. Furthermore, the concentrations of Cu, Zn, and Cd increased with decreasing salinity: this was significant in both species for Zn and Cd and in Elodea for Cu, and a tendency was found in Potamogeton for Cu. Lead concentration, however, was unaffected by salinity. Analysis of metal accumulations (not shown) revealed the same patterns as were found for metal concentrations. Biomass affected the metal uptake in plants, smaller plants having higher metal concentrations and accumulations than larger plants, significantly so for Cu and Zn in Elodea and for all the metals measured in Potamogeton (Fig. 3, Tables 3 and 4). Several interactions were seen. Temperature and salinity interacted both with each other and with the biomass. Between temperature and salinity, two interactions were found (Fig. 4, Tables 3 and 4). First, Potamogeton plants growing in medium salinity water (0.5&) accumulated more Zn than did plants growing in high salinity water (5&) at 5 and 20 C but not at 11 C. Second, the temperature effect on Pb concentration in Potamogeton was significant only when plants were growing in medium salinity water (0.5&). The different temperatures had stronger effects on the metal concentrations and accumulations in plants with lower biomass rather than in plants with higher biomass, Table 1 Treatment averages of dry and fresh weights, DW/FW ratio (dry weight/fresh weight ratio), length, and growth rate for Elodea and Potamogeton treated for 48 h with metal levels of 1.5 mM Cu, 20 mM Zn, 1 mM Cd, and 4 mM Pb, temperatures of 5, 11, or 20 C, and salinities of 0, 0.5, or 5& Species Treatment Elodea Potamogeton Dry weight ( g DW Lÿ1) Fresh weight ( g FW Lÿ1) DW/FW ratio (%) Total length (cm) Growth rate (cm (24 h)ÿ1) Growth rate ( g FW (24 h)ÿ1) Temperature ( C) 5 11 20 0.43 G 0.01 a 0.43 G 0.00 a 0.44 G 0.01 a 8.1 G 0.08 a 8.7 G 0.06 a 9.0 G 0.08 a 5.2 G 0.03 a 5.0 G 0.02 b 4.8 G 0.02 b 76.76 G 0.106 b 75.10 G 0.059 b 83.67 G 0.251 a 0.23 G 0.01 b 0.32 G 0.01 ab 0.43 G 0.01 a n.d. n.d. n.d. Salinity (&) 0 0.5 5 0.45 G 0.01 a 0.44 G 0.01 a 0.41 G 0.00 a 8.7 G 0.08 a 8.7 G 0.08 a 8.3 G 0.06 a 5.1 G 0.03 a 5.0 G 0.02 a 4.9 G 0.02 a 78.50 G 0.26 a 78.82 G 0.286 a 78.21 G 0.16 a 0.31 G 0.01 a 0.32 G 0.01 a 0.35 G 0.01 a n.d. n.d. n.d. Temperature ( C) 5 11 20 1.32 G 0.03 a 1.49 G 0.04 a 1.11 G 0.03 a 11.1 G 0.23 a 12.4 G 0.26 a 10.3 G 0.27 a 11.8 G 0.1 a 11.8 G 0.1 a 10.5 G 0.1 a n.d. n.d. n.d. n.d. n.d. n.d. 0.00 G 0.01 a 0.12 G 0.02 a 0.02 G 0.01 a Salinity (&) 0 0.5 5 1.35 G 0.04 a 1.39 G 0.03 a 1.19 G 0.03 a 11.7 G 0.28 a 11.7 G 0.24 a 10.3 G 0.25 a 11.2 G 0.1 a 11.7 G 0.1 a 11.2 G 0.1 a n.d. n.d. n.d. n.d. n.d. n.d. 0.03 G 0.02 a 0.00 G 0.00 a 0.06 G 0.01 a Different letters indicate significant differences within each metal and treatment (n = 21) GSE. n.d. = no data. 269 Å. Fritioff et al. / Environmental Pollution 133 (2005) 265–274 µg Cd accumulated 100 50 0 0 0.5 5 Salinity (‰) Temperature (°C) 5 µg Zn accumulated 150 Cu 0 0.5 5 0 0.5 5 11 20 1200 800 400 0 0 0.5 5 Salinity (‰) Temperature (°C) 5 100 50 0 0.5 5 5 Zn 1600 Cd 0 µg Pb accumulated µg Cu accumulated 150 0 0.5 5 0 0.5 5 11 20 0 0.5 5 11 0 0.5 5 20 Pb 1000 800 600 400 200 0 0 0.5 5 5 0 0.5 5 11 0 0.5 5 20 Fig. 1. Total accumulation of Cu, Zn, Cd, and Pb in mg containerÿ1 in Elodea (black bar) and Potamogeton (white bar), treated for 48 h with metal levels of 1.5 mM Cu, 20 mM Zn, 1 mM Cd, and 4 mM Pb, temperatures of 5, 11, or 20 C, and salinity of 0, 0.5, or 5&. Each container contained 2 L of medium and on average 0.43 and 1.31 g of Elodea and Potamogeton, respectively (n = 7). this being the case for Cu in both plant species and for Cd and Pb in Potamogeton (Tables 3 and 4). Biomass also interacted with salinity, and the concentration and accumulation of Cu in Elodea and Zn in Potamogeton were more affected by differences in salinity at lower rather than higher biomasses. Furthermore, the Cd concentration and accumulation in Elodea increased with increasing biomass when grown at 11 C, while at the other temperatures Cd concentrations decreased with increasing biomass (Table 3). Table 2 Concentrations of Cu, Zn, Cd, and Pb in Elodea and Potamogeton both before (Controls) and after treatment for 48 h with 1.5 mM Cu, 20 mM Zn, 1 mM Cd, and 4 mM Pb, temperatures of 5, 11, or 20 C, and salinities of 0, 0.5, or 5& (n = 7, for controls n = 2–3, GSE) Metal accumulation (mg( g DW)ÿ1) Species Temperature ( C) Salinity (&) Cu Zn Cd Pb Elodea 5 0 0.5 5 Control 340 G 15 311 G 24 246 G 7 271 G 81 1165 G 41 1137 G 114 548 G 37 387 G 91 145 G 11 117 G 9 38 G 4 3G2 1732 G 289 1838 G 336 1495 G 184 145 G 55 11 0 0.5 5 Control 345 G 10 354 G 15 302 G 15 116 G 12 1168 G 65 1128 G 50 626 G 62 208 G 62 259 G 43 181 G 27 85 G 19 3G1 1447 G 208 1528 G 300 2037 G 225 16 G 7 20 0 0.5 5 Control 444 G 15 406 G 30 348 G 25 154 G 19 2193 G 118 1919 G 138 1354 G 276 178 G 21 269 G 16 244 G 24 212 G 23 1G1 1771 G 152 1694 G 134 2190 G 168 53 G 33 5 0 0.5 5 Control 145 G 22 118 G 13 137 G 25 23 G 0 1381 G 122 1258 G 264 560 G 64 48 G 6 94 G 12 70 G 8 32 G 4 5G1 127 G 40 74 G 19 110 G 20 5G5 11 0 0.5 5 Control 133 G 19 111 G 22 70 G 10 17 G 3 1297 G 132 873 G 139 672 G 74 69 G 9 108 G 12 74 G 13 32 G 3 3G2 88 G 17 75 G 9 113 G 39 7G3 20 0 0.5 5 Control 193 G 60 160 G 40 142 G 26 21 G 5 1679 G 255 1311 G 194 693 G 84 61 G 6 151 G 33 100 G 18 63 G 27 2G1 151 G 40 227 G 68 162 G 42 7G0 Potamogeton 270 Å. Fritioff et al. / Environmental Pollution 133 (2005) 265–274 µg Me / g DW Cd Cu 400 Cu Cd 300 200 Table 3 Analysis of variance of heavy metal concentrations in Elodea exposed to Cu, Zn, Cd, and Pb, three different salinities, and three different water temperatures Response variable Source of variation df MS F p Cu Temperature Salinity Biomass Temperature ! Salinity Temperature ! Biomass Salinity ! Biomass Error 2 2 1 4 17784 9548 54589 1034 15.7 8.4 48.1 0.9 !0.001*** !0.001*** !0.001*** 0.4655 2 6564 5.8 0.0056** 2 4143 3.6 0.0334* 49 1136 Temperature Salinity Biomass Temperature ! Salinity Error 2 2 1 4 5282023 2357154 462852 40936 53.4 23.8 4.7 0.4 !0.001*** !0.001*** 0.0351* 0.7981 53 98979 Temperature Salinity Biomass Temperature ! Salinity Temperature ! Biomass Error 2 2 1 4 33081 57252 1139 6665 11.7 20.2 0.4 2.4 !0.001*** !0.001*** 0.5288 0.0663 2 22256 7.9 0.0011** 51 2833 Temperature Salinity Biomass Temperature ! Salinity Error 2 2 1 4 343788 584252 1355437 314637 1.0 1.6 3.8 0.9 0.3889 0.2049 0.0569 0.4823 53 357601 100 0 5 11 20 5 11 20 0 0.5 5 0 0.5 5 2500 Pb Zn Pb Zn Zn µg Me / g DW 2000 1500 1000 Cd 500 0 5 11 20 5 11 Temperature (°C) 20 0 0.5 5 0 0.5 5 Salinity (‰) Fig. 2. Treatment averages of Cu, Zn, Cd, and Pb concentrations in Elodea (black bar) and Potamogeton (white bar) treated for 48 h with metal levels of 1.5 mM Cu, 20 mM Zn, 1 mM Cd, and 4 mM Pb, temperatures of 5, 11, or 20 C, and salinities of 0, 0.5, or 5& (n = 21) GSE. 4. Discussion This research found that metal concentration and accumulation in the two studied submersed macrophyte species generally increased with increasing temperature but decreased with increasing salinity (Fig. 2, Tables 3 and 4). The influences of temperature and salinity were not always independent of each other (Fig. 4, Tables 3 and 4). Furthermore, metal concentrations and accumulations increased with decreasing biomass in most cases (Fig. 3, Tables 3 and 4). Interactions between temperature and biomass or salinity and biomass were sometimes found as well (Tables 3 and 4). Because of the higher biomass (DW lÿ1) of Potamogeton than of Elodea (Table 1), total metal accumulations (mg containerÿ1) in Potamogeton plant material in some cases exceeded those of Elodea (Fig. 1). Thus, compared with Elodea, Potamogeton removed more added Zn from the medium in all treatments and more Cu and Cd from the medium in the 5 C treatment. In line with the first hypothesis, metal concentrations and accumulations increased with increasing water temperature for Cu, Zn, and Cd in Elodea (Fig. 2, Table 3) and for Cu, Zn, Cd, and Pb in Potamogeton (Fig. 2, Table 4), independent of salinity. Furthermore, total Pb Plants were allowed to acclimatize to the temperatures for 10 days before exposure to salinity treatments and heavy metals. Only single factors (temperature and salinity), the covariable (biomass, as dry weight), interactions between main factors (temperature and salinity), and significant interactions are shown. Error, within group variance; df, degrees of freedom; MS, between group variance; F, ratio between MS and Error. *p ! 0.05, **p ! 0.01, ***p ! 0.001. metal accumulations (mg containerÿ1) increased with increasing temperature (Fig. 1). One likely explanation for this is that increased temperature will increase the biomass and thus the absorption area of the plant; this, in turn, will increase the metal uptake. This was found to be the case for Cd uptake by Pinus silvestris (L.) (Ekvall and Greger, 2003). In the present study, Elodea length increased significantly more in containers at 20 C than in those subject to colder treatments (Table 1). However, biomass did not differ between treatments; thus the effect of temperature on metal uptake was direct, and an explanation other than growth rate must be found. Earlier investigations suggested that the extracellular concentration increases with increasing temperature because there is a change in the equilibrium between the cell wall exchange sites and the metal in solution Å. Fritioff et al. / Environmental Pollution 133 (2005) 265–274 Table 4 Analysis of variance of heavy metal concentrations in Potamogeton exposed to Cu, Zn, Cd, and Pb, three different salinities, and three different water temperatures Response variable Source of variation df MS F p Cu Temperature Salinity Biomass Temperature ! Salinity Temperature ! Biomass Error 2 2 1 4 16893 6306 182345 1894 6.7 2.5 72.1 0.7 0.0026** 0.0926 !0.001*** 0.5632 2 13555 5.4 0.0077** 51 2528 Temperature Salinity Biomass Temperature ! Salinity Salinity ! Biomass Error 2 2 1 4 204246 1888943 4417721 216076 2.6 23.6 55.3 2.7 0.0876 !0.001*** !0.001*** 0.0406* 2 510731 6.4 0.0033** 51 79944 Temperature Salinity Biomass Temperature ! Salinity Temperature ! Biomass Error 2 2 1 4 11998 25012 42135 1033 11.3 23.6 39.7 1.0 !0.001*** !0.001*** !0.001*** 0.4305 2 7696 7.2 0.0017** 51 1062 Temperature Salinity Biomass Temperature ! Salinity Temperature ! Biomass Error 2 2 1 4 36547 1807 191946 16666 6.8 0.3 35.8 3.1 0.0024** 0.7152 !0.001*** 0.0229* 2 19125 3.6 0.0354* 51 5355 Zn Cd Pb Plants were allowed to acclimatize to the temperatures for 10 days before exposure to salinity treatments and heavy metals. Only single factors (temperature and salinity), the covariable (biomass, as dry weight), interactions between main factors (temperature and salinity), and significant interactions are shown. Error, within group variance; df, degrees of freedom; MS, between group variance; F, ratio between MS and Error. *p ! 0.05, **p ! 0.01, ***p ! 0.001. (Gonzalez-Davila et al., 1995; Mautsoe and Beckett, 1996). However, if this was the only factor, temperature should affect Pb accumulation in Elodea in the same way it affects accumulation of the other three metals, which was not the case (Fig. 2, Table 3). Instead, it is suggested that the absence of a temperature effect on Pb accumulation is due to a high proportion of extracellular binding sites for Pb in Elodea. This was earlier shown by Vásquez et al. (1999) to be the case in two aquatic bryophyte species, Fontinalis antipyretica Hedw. and Scapania undulata (L. Dum.). Extracellular binding of metal is less temperature dependent than is intracellular uptake, according to Beckett and Brown (1984), Marschner (1995), and Mautsoe and Beckett (1996). The intracel- 271 lular uptake of Cu, Cd, and Zn might also be the fractions most affected by temperature in the present study. Slightly increased extracellular uptake could facilitate intracellular uptake by concentrating metals close to the membrane. Furthermore, a higher temperature changes the lipid composition of the plasma membrane (Lynch and Steponkus, 1987) and thereby its fluidity, which may facilitate both passive and active metal flux through the membrane. In addition, increased temperature increases both metabolism (Marschner, 1995; Nilsen and Orcutt, 1996) and protein synthesis (Nilsen and Orcutt, 1996), and this may result in higher metal uptake at additional uptake sites on membranes or an increased release of molecules facilitating metal uptake. The second hypothesis, that metal concentration and accumulation decrease with increasing salinity, was supported by the results for Cu, Zn, and Cd in both species (Fig. 2, Tables 3 and 4), independent of temperature. E. canadensis and P. natans are freshwater species and have been found growing in the field in salinities up to 3& and 2&, respectively (Luther, 1951). Even at the highest salinity used in this study, 5&, no toxic effect was observed in these species (not shown). The likely reason for the decreased accumulation with increasing salinity is the decreased availability of the metals in the growth medium because of the complexes formed between chloride and metals (Förstner, 1979). This has, for example, been shown to depress Cd uptake in P. pectinatus (Greger et al., 1995). In addition, increased competition with sodium ions at uptake sites, both on the plasma membrane and in apparent free space in the cell walls, may account for the decreased metal accumulation at higher salinities (Noraho and Gaur, 1995). That salinity has no influence on Pb accumulation (Fig. 2, Tables 3 and 4) may be because Pb does not form a complex with chloride (Förstner, 1979), is retained briefly in water, and has a high affinity to bind to organic matter (Förstner, 1979) such as plant surfaces (Vásquez et al., 1999). Therefore, despite different salinities, the same amount of Pb will bind to and be taken up by plants. Biomass did not differ among treatments, but rather varied within each treatment (Table 1), and plants with lower biomasses had higher metal accumulations and concentrations than did plants with higher biomasses (Fig. 3, Tables 3 and 4). This may be because a proportionally larger absorption area in relation to the external metal concentration may result in a dilution effect and thus a low internal metal concentration. Ekvall and Greger (2003) showed that this was the case for Cd in Pinus sylvestris. Besides different amounts of biomass, different metal accumulations may also be due to different proportions of stems to leaves. Preliminary results for P. natans indicate that the uptake by its leaves is almost 10 times higher than the uptake by its stems (Fritioff and Greger, unpublished). 272 A 2000 1000 0 0.5 0.75 Elodea biomass (g DW) 0 2 1 3 Biomass (g DW) 200 0 0.25 1000 400 Biomass (g DW) 200 2000 0 0.25 0.5 0.75 (µg Me / g DW) (µg Me / g DW) B 0 0 400 0 (µg Me / g DW) (µg Me / g DW) Å. Fritioff et al. / Environmental Pollution 133 (2005) 265–274 0 1 2 3 Potamogeton biomass (g DW) Fig. 3. The effect of biomass on Cu, Zn, Cd, and Pb concentrations in Elodea (A) and Potamogeton (B) treated for 48 h with metal levels of 1.5 mM Cu, 20 mM Zn, 1 mM Cd, and 4 mM Pb, temperatures of 5, 11, or 20 C, and salinities of 0, 0.5, or 5&. Only trend lines are shown; the line pattern indicates which metal is represented: Cu (d – d – d –), Zn (––– ––– ––– –––), Cd (– – – – – –), Pb (ddd). n = 21. The concentrations of the various metals tested were, in almost all cases, higher in Elodea than in Potamogeton (Fig. 2). The Zn concentration was about the same in the two species, while Cu and Cd concentrations were about twice as high in Elodea than in Potamogeton and the Pb concentration was over 10 times higher in Elodea. This is 5 ºC 11 ºC 20 ºC A µg Pb / g DW 300 250 200 150 100 50 0 0 0.5 5 Salinity (‰) B 0‰ 0.5 ‰ 5‰ µg Zn / g DW 2000 1500 1000 500 0 5 11 20 Temperature (°C ) Fig. 4. Concentrations (mg ! g ÿ1 ! DWÿ1) of Pb and Zn in Potamogeton (A and B, respectively), showing interactions between temperature and salinity after treatment for 48 h with 1.5 mM Cu, 20 mM Zn, 1 mM Cd, and 4 mM Pb, temperatures of 5, 11, or 20 C, and salinity of 0, 0.5, or 5& (n = 7) GSE. in accordance with other studies done both in laboratory-scale wetlands (Nyquist and Greger, 2003) and in the field (Yurukova and Kochev, 1994). First, Potamogeton plants had higher biomasses than did the Elodea plants (Table 1); as previously discussed, within a species, plants with higher biomass will have lower metal concentrations when exposed to the same metal concentration in the medium. Second, Elodea had a higher water content than did Potamogeton, as shown by low DW:FW ratio (Table 1). This may facilitate metal uptake, by presenting larger vacuoles for storage and because a higher water content in the cell wall facilitates diffusion into the apparent free space by dilution. Other reasons for the higher metal accumulation in Elodea than in Potamogeton (Fig. 2) may be species differences in uptake capacities and differences in the proportion of stems to leaves. Sculthorpe (1967) described how Elodea had a higher leaf uptake of solutes than did Potamogeton, because of their differences in morphology. Elodea’s high surface-to-volume ratio as well as its high proportion of leaves relative to total plant biomass may facilitate metal uptake by diffusion, while the thick waxy cuticle of Potamogeton may obstruct metal uptake. Submersed plants often display high metal accumulations in the field (Galiulin et al., 2001). In the present laboratory experiment, Elodea had in most cases higher metal concentrations than did Potamogeton. In some cases, however, Potamogeton removed more of the added metals in total from the containers than did Elodea. Depending on the treatment, Elodea removed at most 70, 30, 51, and 56% and at least 13, 5, 8, and 40% of the added Cu, Zn, Cd, and Pb, respectively, during the 48-h treatment with elevated levels of metals. Å. Fritioff et al. / Environmental Pollution 133 (2005) 265–274 Potamogeton removed at most 75, 64, 50, and 11% and at least 50, 22, 14, and 5% of the added Cu, Zn, Cd, and Pb, respectively, during the same 48-h treatment. The average weight of plant material in each container was 0.43 g DW for Elodea and 1.3 g DW for Potamogeton (Table 1). Thus, the high removal might depend on a high plant biomass per volume of solution. Both metal concentration in plant material and total uptake were highly dependent on plant biomass; therefore, biomass in combination with metal load was important for overall metal removal during the experiment. In fact, Potamogeton removed at least twice as much Zn as did Elodea in this experiment. However, Nyquist and Greger (2003) found the opposite in a laboratory-scale wetland experiment. They reported that Elodea removed 64% of the total amount of added Zn, while Potamogeton removed just 23%. The present study found that Elodea and Potamogeton did accumulate heavy metals, although the quantity depended on the biomass, indicating that Elodea and Potamogeton can both remove metals from stormwater during storm events. 5. Conclusions Although Elodea and Potamogeton are most effective at accumulating heavy metals discharged in stormwater at high temperatures, they have still good heavy metal accumulation capacity down to at least 5 C. They may therefore be useful in treating stormwater in temperate climates. Since plant biomass is low in early spring, metal accumulation per unit of biomass can be expected to be comparatively high, because of generally higher metal accumulation when a small, compared to a large, biomass is exposed to a given amount of metal in the water. Increased salinity resulting from road deicing will reduce metal accumulation in both Elodea and Potamogeton more than temperature will. Low salinity levels in the summer lower Cu, Zn, and Cd accumulation by plants, while salinity peaks in the winter may reduce the accumulations by plants by over 50%. Unlike the other metals, Pb accumulation is generally unaffected or very little affected by temperature and/or salinity, and will thus remain relatively stable throughout all seasons and possible salinity levels. Although during the experiment Potamogeton accumulated more Zn and sometimes more Cu and Cd from the medium than did Elodea, Potamogeton more often had a lower metal concentration than did Elodea; this is possibly because Potamogeton had a higher biomass per liter than did Elodea. 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