Introduction

Urban brownfields are abandoned industrial sites close to inhabited areas. These brownfields may contain pollutants, thus significantly restricting land-use planning (O’Connor et al. 2019). However, they also offer strategic opportunities for the sustainable transition of metropolitan territories (Rey et al. 2022) as their remediation is essential to create new green zones. Reclamation of brownfield sites eliminates environmental risks and helps to reduce greenhouse gas emissions (Hou et al. 2018). In this context, phytoremediation has proved to be a cost-effective and environmentally friendly alternative to conventional soil remediation methods and it is included in the new trend of nature-based solutions (NBS) for environmental remediation (Guidi Nissim and Labrecque 2021). The use of phytoremediation for brownfield remediation enhances soil health helps to regulate urban temperature, improves urban hydrology, supports greater biodiversity, and attenuates air and noise pollution (Guidi Nissim and Labrecque 2021). The two most common phytoremediation options are phytostabilization and phytoremediation.

Plant species vary in their capacities to accumulate or tolerate metal(loid)s in aerial structures and roots, and this capacity is determined by the concentration of metal(loid)s present in the soil, by the physiological features of the species and by their selectivity for specific metal(loid)s (Massenet et al. 2021; Pilon-Smits 2005). Phytostabilization is a type of phytoremediation aimed at immobilizing pollutants in a contaminated substrate, by establishing vegetation on top of the polluted material (Forján et al. 2018). On the other hand, phytoextraction is a phenomenon in which hyperaccumulator plants absorb metals from the soil through the root system and translocate them to the harvestable shoot, making it possible to recover metals from the harvestable parts of plants (Forján et al 2017; Rodríguez-Vila et al. 2016).

A key aspect when implementing phytoremediation is the selection of the appropriate species. A common strategy is to use a plant that grows spontaneously and abundantly in the contaminated soil (Ali et al. 2013). Authors such as Mukhopadhyay et al. (2017) and Midhat et al. (2016) have shown that species that grow spontaneously in contaminated soils exhibited good phytoremediation behavior. Subsequently, the phytoremediation capacity, i.e., phytoextraction or phytostabilization properties of the potential candidates, should be evaluated (Forján et al. 2018). Indeed, several studies have shown that species and ecotypes present in metal(loid)-polluted sites tolerate high concentrations of soil pollutants and often show tolerance mechanisms that allow them to grow under these stress conditions (Schat et al. 2020).

Langreo (Spain) is an example of an area severely affected by heavy industry and mining activities. One of the most important activities of this area for decades was the production of fertilizers, which lead to the development of a 20 ha urban brownfield site named Nitrastur (Gallego et al. 2016; Gil-Díaz et al. 2016). Previous studies on this site revealed the presence of native herbaceous plants useful for phytostabilization purposes (Matanzas et al. 2021), whereas Mesa et al. (2017) focused on a specific study of enhanced phytoextraction via bioaugmentation; however, in those works, the main criteria that could be followed to design a real-scale phytoremediation were not addressed.

Following the previous considerations, the aim of this work was the study of the phytoremediation capacities and strategies followed by Buddleja davidii Franch (B. davidii), Betula celtiberica Rothm. & Vasc (B. celtiberica), and Acer pseudoplatanus L (A. pseudoplatanus), all of them growing abundantly in the study site and in the neighboring area. Of note, we addressed the different behaviors of these plants at different levels of soil pollution (very high inside the polluted site and much lower in the surroundings). Results will be helpful in the species selection for real-scale treatments, depending on the degree of soil pollution and the phytoremediation strategy to be followed (phytoextraction or phytostabilization).

Material and methods

Study area

The study area includes the urban brownfield of Nitrastur (20 ha)—which is colonized by a range of pollution-tolerant plants—and its surroundings, where some of the same species are also abundant (Fig. 1). Nitrastur was one of the main fertilizer plants in Spain; it is located in Langreo (Asturias) that has been an important industrial area since the nineteenth century, hosting activities such as coal mining and a coal-fired power plant, steel, and chemical industries. Most of these industrial and mining activities were abandoned in the last three decades leaving behind large amounts of waste that were disposed of in natural soil (see Gallego et al. 2016 and references therein).

Fig. 1
figure 1

Study sites and sampling areas

Nitrastur is currently one of the largest brownfields in Spain and was included in the national inventory of polluted areas in 2001 and recently again in 2018. A detailed study (Gallego et al. 2016) revealed pyrite ashes, resulting from the roasting of pyrites for sulfuric acid production, as the main source of pollution whereas an assessment of site-specific human health risks (Wcislo et al. 2016) demonstrated the need for remediation, and thus, several attempts have been made (Baragaño et al. 2021). Within the brownfield, the values of pseudototal concentrations of As, Cu, Zn, and other elements usually exceed the limits established by the Spanish regulation in force (BOPA 2014), peaking up nowadays to thousands of mg·kg−1 in some areas.

Soil and plant sampling design

Three of the predominant species were Acer pseudoplatanus L (A. pseudoplatanus), Betula celtiberica Rothm. & Vasc (B. celtiberica), and Buddleja davidii Franch (B. davidii). Clusters of these plants were found in surrounding areas of the brownfield. The sampling was based on the simultaneous sampling of vegetation and soil (Fig. 1). The sampling stations were selected in locations in which several individuals of one of the target plants were found within a few square meters. The sampling locations were labelled M1, M2, and M3 (inside Nitrastur), and M4, M5, and M6 (outside). To build a composite sample for vegetation, six samples were taken from the aerial part and roots of individual plants belonging to the same species. For soil sampling, each sample consisted of four increments (1 kg) of the first 20 cm of soil, which was collected using a Dutch Edelman probe at each sampling point. This soil corresponded to the rhizosphere of the sampled vegetation. Soil samples were preserved in sterilized plastic bags and stored at 4 °C until preparation and analysis.

Soil analysis

Soil pH was determined using a Mettler Toledo SevenCompact multimeter (1:2.5 water/soil). The organic matter content (OM) was determined by ignition (24 h–540 °C). Pseudototal metal(loid) concentrations were extracted with aqua regia (HCl + HNO3) in an Anton Paar 3000 microwave and measured by ICP-MS (Inductive Coupled Plasma Mass Spectrometer; ICP-MS 7700, Agilent Technologies). Phytoavailable concentrations of metal(loids)s were extracted by two methods to obtain more reliable data (Asensio et al. 2018; Lebourg et al. 2010; Menzies et al. 2007). In this regard, we performed one extraction with 0.01 M CaCl2 (Houba et al. 2008) and another with 0.1 M (NH4)2SO4 (Fresno et al. 2016). Metal(loid) concentrations were determined using the same ICP-MS device described above, and Standard Reference Material 1515 Apple leaves from NIST (National Institute of Standards and Technology) were used.

Plant analysis and accumulation of metal(loid)s in plant tissues

Biomass was washed with deionized water, and fresh biomass was weighed. Dry biomass was assessed after oven-drying for 48 h at 80 °C and cooling at room temperature. Metal(loid) concentrations were quantified by Inductively ICP-MS (7700; Agilent Technologies, USA) after acid digestion (H2O2 and HNO3 (1:2 v/v)) in a microwave oven (Milestone ETHOS 1, Italy). The behavior of the metal(loid)s in the soil/plant system was addressed by examining the following parameters (Table 1):

  • The translocation factor (TF), where a high value indicates a relatively high shoot metal concentration compared to its root concentration (Forján et al. 2018).

  • The transfer coefficient (TC) in the studied plants measured their efficiency to take up metals from the soil (Rodríguez-Vila et al. 2014).

  • The bioconcentration factor (BF) describes the ratio of available metal(loid) concentration that is taken up into shoots or roots. High BF values indicate a high concentration of elements in shoots or roots compared to the available concentration of the metal(loid)s (Rodríguez-Vila et al. 2015).

Table 1 Relation of soil/vegetation factors calculated

A high TF value indicates a relatively high shoot metal(loid) concentration compared to its root concentration; i.e., a plant species moves metal(loid)s effectively from the roots to shoots when the TF > 1. In contrast, TF values below 1 may indicate that the plant accumulates the contaminants in the root and thus acts as a phytostabilizer (Forján et al. 2018). In this regard, the ideal plant species for phytostabilization purposes are the “metal excluders,” which show a very low root-to-shoot TC (Kidd et al. 2009). This coefficient indicates efficiency to take up metals from the soil, and a plant is considered to be an accumulator biosystem whenever TC is higher than 1 (Busuioc et al. 2011). Finally, as regards BF, this parameter relates the extractable metal(loid) concentration in the soil to the concentrations in the aerial and root parts of the plant; BF is highly dependent on the method used to measure the extractable metal(loid) concentration (Karami et al. 2011), and thus, we have applied two different extractants ((NH4)2SO4 and CaCl2) to obtain the extractable metal(loid) concentration.

Statistical analysis

The analytical determinations were performed in triplicate. Analysis of variance (ANOVA) and test of homogeneity of variance were carried out. In the case of homogeneity, a post hoc least significant difference (LSD) test was performed. If there was no homogeneity, Dunnett’s T3 test was performed. The Student’s t-test was used to compare the results of two samples at a time. A correlated bivariate analysis was also carried out using Pearson’s correlation. All data were processed with the statistical program SPSS (V.19).

Results and discussion

General characteristics of soils

The difference in pH between the samples taken inside and outside the urban brownfield was not relevant (Table 2). The soil with the lowest pH was M1, (pH 6.08), followed by M2. In this context, acidic pH values inside Nitrastur may have been caused by the presence of pyrite ash residues mixed with soil (Gallego et al. 2016). The rest of the pH values coincided with previous reports of slightly alkaline values (Baragaño et al. 2021). Regarding vegetation, the lowest pH values were observed in the soils hosting B. davidii, followed by B. celtiberica and A. pseudoplatanus (Table 2). As regards organic content, the soils inside the urban brownfield (M1, M2, M3) had a similar OM content, which was generally lower than that recorded outside the site. The soils M4 and M6 had the highest OM content, possibly because they had well-defined O and A horizons. In turn, these points were associated with B. davidii and B. celtiberica (Table 2).

Table 2 General soil characteristics: inside and outside the urban brownfield

As expected, soils M1, M2, and M3 showed significantly higher pseudo-total concentrations of Cu, Zn, and As than M4, M5, and M6 (Fig. 2, Table 3). These higher concentrations are attributed to the disposal, erosion, and blend of different types of waste, such as slag, coal waste, and pyrite ash, found throughout the brownfield with natural soil aggregates (Baragaño et al. 2020; Gallego et al. 2016).

Fig. 2
figure 2

Graphical representation of pseudo-total concentrations of Cu, Zn, and As

Table 3 Pseudo-total concentrations of Cu, Zn, and As (mg.kg−1) in soils inside and outside the urban brownfield

Inside the brownfield, the highest concentrations of Cu and Zn were detected in soils encompassing the B. celtiberica sampling area, whereas As concentrations were the highest in the soils in which B. davidii was growing (Fig. 2). B. celtiberica can grow in soils with high concentrations of Cu and Zn (Fernández-Fuego et al. 2017a, 2017b). Other authors (Chaoyang et al. 2011) have also described B. davidii growth in soils with high concentrations of As, and, in general terms, it can grow in soils with considerable metal(loid) concentrations (Ge & Zhang 2014; Zhu et al. 2018). Coherently, outside the urban brownfield, the soils with the highest pseudototal concentrations of Cu, Zn, and As coincided with those in which B. davidii was growing (Fig. 2).

Phytoavailable concentrations of Cu, Zn, and As

Phytoavailable concentrations of Cu, Zn, and As were higher inside the brownfield (M1, M2, M3 samples) irrespective of the extractants used (Figs. 3, 4). These high concentrations may be explained by the different types of residues, mainly pyrite ash, that were accumulated over time at this site (Gallego et al. 2016). In addition, the lower OM content and pH values within the brownfield soil (Table 2) may cause reduced sorption capacity compared to the natural soils outside the brownfield (Forján et al. 2016).

Fig. 3
figure 3

Graphical representation of phytoavailable concentrations of Cu, Zn, and As ((NH4)2SO4 extracted) in soil

Fig. 4
figure 4

Graphical representation of the phytoavailable concentrations of Cu, Zn, and As (CaCl2 extracted) in soil

Regarding the proportions of extractable contaminants (Table 4), in general terms, the values were higher for Cu and Zn inside the brownfield, as was the case for As, although the latter showed very low values. The same, but to a greater extent, was observed for Pb. In this regard, notable pseudo-total Pb concentrations were previously reported (Gallego et al. 2016), but in the present study, we found that phytoavailable Pb was below the detection limit in all the samples examined, and thus, Pb data were not considered in this study. For more information, consult Table S1 (Supplementary material).

Table 4 Phytoavailable concentrations of Cu, Zn, and As (mg.kg−1) and their percentage vs pseudo-total concentrations in soils, inside and outside the urban brownfield

Phytoavailable concentrations of metal(loid)s inside the brownfield could be attributed to the presence of soils mixed with the residues mentioned above, specifically pyrite ash, which is largely composed of oxides, hydroxides, and also sulfides of iron and other metal(loid)s, which were produced as by-products of the sulfide ore roasting process (Gallego et al. 2016; Mesa et al. 2017). As an exception, Zn in sample M6 (outside) showed a higher phytoavailable percentage, both with (NH4)2SO4 (7.93%) (Fig. 3) and CaCl2 extractants (5.15%) (Fig. 4), than that of any other sample inside the brownfield (< 2.10% for both extractants, Table 4). There could be various explanations for this observation, including the location of the different industries that have been operating in Langreo for more than a century and that left a heavy pollution footprint in the environmental compartments (Boente et al. 2022).

Specifically for the sampling stations of plants clusters, Zn presented the highest phytoavailable concentrations, both inside (0.11% with (NH4)2SO4 and 0.04% with CaCl2) and outside (7.93% with (NH4)2SO4 and 5.15% with CaCl2) the brownfield, coinciding with soils where B. celtiberica grew (Fig. 4, Table 4). Therefore, in the outside station, the percentage of extractable concentration versus pseudototal concentration was higher than inside the brownfield (Table 4) irrespective of the higher pseudototal concentration observed inside. This suggests that the mobility of Zn inside the brownfield is very low due to the pollution source (pyrite ash) as previously observed by Baragaño et al. (2020). A similar pattern was observed for phytoavailable concentrations of Cu inside the brownfield in the case of B. davidii with (NH4)2SO4 extraction (Fig. 3, Table 4). In contrast, the soils outside where B. davidii grew presented the highest concentrations of Cu, whereas phytoavailable As exceeded the detection limit values only in the inside area in which B. davidii grew (Fig. 4, Table 4).

Metal(loid) concentrations in plants and plant/soil system

In general, all the plant species presented higher concentrations of the metal(loids)s inside the brownfield than outside, both in the root and aerial part, with As presenting the lowest values and Zn the highest in all species (Fig. 5, Table S2 (Supplementary material)).

Fig. 5
figure 5

Metal(loid) concentrations in plants and plant/soil system. A. B. davidii, B B. celtiberica, and C A. pseudoplatanus. Locations inside the urban brownfield are indicated in orange and those outside in blue

B. davidii sampled inside the urban brownfield had higher concentrations of Cu, Zn, and As (in roots and aerial part) compared to B. davidii sampled outside the urban brownfield (Fig. 5, Table S2). The area where B. davidii was collected revealed phytoavailable concentrations of Cu, Zn, and As that were significantly positively correlated (p < 0.01) with the contents of Cu, Zn, and As in the root and leaves of B. davidii.

Inside the urban brownfield, B. celtiberica presented higher contents of Cu, Zn, and As in both the root and aerial part than B. celtiberica outside the brownfield, except for As in the aerial part, although no significant differences were found (Fig. 5, Table S2). Phytoavailable Zn concentrations were significantly positively correlated with Zn contents in the root and aerial part of B. celtiberica. However, in the case of Cu, significant positive correlations were found only between phytoavailable Cu concentrations and root Cu content.

A. pseudoplatanus followed the same pattern as B. davidii and B. celtiberica. Inside the brownfield, A. pseudoplatanus had the highest concentrations of Cu, Zn, and As, both in the root and aerial part (Fig. 5, Table S2). These results are in concordance with those reported by authors such as Mleczek et al. (2017). Phytoavailable Zn concentrations were significantly positively correlated with Zn contents in the root and aerial part, and also with the BF values.

Soil/vegetation indexes

The species studied inside the urban brownfield can be classified as accumulators or hyperaccumulators of metal(loid)s, presenting, in general, TC > 1 or proximal values according to Busuioc et al. (2011) (Table 5). In contrast, following the study by Baker and Brooks (1989), the species outside the brownfield present a high degree of meta(loid) translocation between soil and vegetation (Table 5).

Table 5 Cu, Zn, and As soil/vegetation factors (TF, TC, BFroot, BFaerial) in areas inside and outside the urban brownfield

B. davidii outside the urban brownfield had a TF > 1 for Cu and Zn (Table 5). In addition, the BF-aerial value for Cu and Zn was higher than the BFroot value, and the opposite was true inside the brownfield (Table 5). These values indicate that the behavior of B. davidii is distinct when inside and outside the urban brownfield. Outside the area, B. davidii has a high capacity to accumulate Cu and Zn in the aerial part, whereas inside the site, it accumulates these elements in the root, thereby suggesting phytostabilization capacity (Baker and Brooks 1989; Karami et al. 2011). The behavior of B. davidii that we observed in the soils with high concentrations of Cu and Zn is consistent with data reported by Zhu et al. (2018).

B. celtiberica inside the urban brownfield did not show TF or TC > 1 for any of the metal(oid)s analyzed. However, outside the area, it showed TF and TC > 1 for Cu and TF values higher than 1 for Zn. As in the case of B. davidii, the TF and TC values indicate two very different phytoremediation behaviors of B. celtiberica. Inside the brownfield, where phytoavailable concentrations are higher, B. celtiberica behaves as a phytostabilizing species, but outside, where concentrations are lower, it is a phytoextractive species. In fact, B. celtiberica is a fast-growing, deciduous, and pseudometallophilic tree. It has a high biomass and a well-developed root system. Although it has colonized the study area, it is usually found in restricted areas of the Iberian Peninsula (Shaw et al. 2014). Thus, the autoecology of this species suggests that it might be a suitable candidate to phytoremediate contaminated soils in Asturias (Mesa et al. 2017), like the urban brownfield examined herein. Authors such as Kříbek et al. (2020) concluded that B. celtiberica can grow on substrates with extremely high concentrations of trace elements and can therefore be used for phytoremediation purposes, especially on Zn-contaminated sites. In this regard, it should be noted that, in the urban brownfield studied here, Zn was the element with the highest pseudo-total and phytoavailable concentrations. Consequently, Zn was the metal that B. celtiberica accumulated the most (Table 5).

The TF and TC values exceeded 1 only in A. pseudoplatanus outside the brownfield, although it should be noted that these values did not exceed 1 for Cu in this species either inside or outside the brownfield (Table 5). For Zn, the BF values inside the site and the TF and TC values outside indicate the high capacity of A. pseudoplatanus to phytoremediate Zn-contaminated soils. In addition, A. pseudoplatanus can enhance the reduction of metal(loid) concentrations in the soil as it has good litter quality, which promotes rapid decomposition, lower production of acids, and the formation of stable humus (Reich et al. 2005). Another positive feature of A. pseudoplatanus is that lower amounts of Zn are found in the litter it produces compared to other phytoremediation species (Mertens et al. 2007).

Conclusions

Spontaneously growing species showed a high capacity for adaptation to the environmental conditions. The phytoavailable concentrations of metal(loid)s showed that concentrations were higher inside the brownfield than outside. However, the TF and TC indicated that the species studied outside the brownfield, on average, had phytoextractive capacity and that those inside the brownfield had phytostabilization capacity. Thus, on the basis of the results obtained from the indexes related to phytoremediation, A. pseudoplatanus, B. celtiberica, and B. davidii follow different phytoremediation strategies depending on the degree of contamination of the soil. Therefore, for real-scale treatments, the three species studied herein emerge as candidates for phytostabilization actions in areas with high levels of contaminants, whereas their phytoextraction capacity is suitable only for soils with low levels of pollution.