Influences of hexafluoropropylene oxide (HFPO) homologues on soil microbial communities
Introduction
With the phase-out of legacy perfluoroalkyl substances (PFASs), PFASs with shorter carbon chain length and containing ethers have found increasing applications, and have therefore been released into the environment (Wang et al., 2013, 2015, 2017, 2019). Hexafluoropropylene oxide (HFPO) homologues belong to the perfluoro-ether carboxylic acids and have replaced perfluorooctanoic acid (PFOA) as processing aids (Heydebreck et al., 2015; Pan et al., 2017; Song et al., 2018). They play a critical role as additives in the manufacture of fluorine polymers (Song et al., 2018), so fluorine factories are major sources of HFPO homologues pollution (Brandsma et al., 2019). HFPO homologues include dimer, trimer and tetramer acids of HFPO (HFPO-DA, HFPO-TA, and HFPO-TeA) (Song et al., 2018). HFPO homologues are attracting mounting attention because of their ubiquitous detection in multimedia environmental samples (Brandsma et al., 2019; Cui et al., 2018; Pan et al., 2017, 2018), and their similarity to legacy PFASs in terms of persistence and toxicity (Bao et al., 2018a; Brandsma et al., 2019; Cui et al., 2018; Li et al., 2019). The reported highest concentration of HFPO-DA in surface water near fluorine factories is 631 ng/L in the USA, 108 ng/L in Germany, 812 ng/L in The Netherlands, and 3830 ng/L in China (Gebbink et al., 2017; Heydebreck et al., 2015; Sun et al., 2016a). In China, HFPO-TA has been reported to have reached 68 500 ng/L (maximum) in a river downstream of a fluorine plant, 1510 ng/L (median) in wild common carp, and 2.93 ng/L (median) in the sera of residents (Pan et al., 2017). HFPO-TeA ranged from <LOQ (limit of quantification) to 42.6 ng/g in 2014 and <LOQ to 363 ng/g in 2016 in sediment (Song et al., 2018). HFPO homologues have even exhibited greater risks than their predecessor PFOA, owing to their stronger disruptive effects on adipogenic activity related with hepatoxicity and estrogenic effects in vitro and vivo experiments (Li et al., 2019; Song et al., 2018; Xin et al., 2019).
Since HFPO homologues are frequently detected in surface water near fluorine plants, it is reasonable to speculate that HFPO homologues can also exist in soil via air transportation, water penetration and surface runoff (Brandsma et al., 2019; Cai et al., 2019). Therefore, soil could be an important sink for HFPO homologues. Soil microbial density and community structure are sensitive to the pressure of legacy PFASs (Bao et al., 2018b; Li et al., 2017; Qiao et al., 2018). In addition, PFASs greatly altered sediment microbial community (Zhang et al., 2017). PFOA could induce a long-term change of microbial community in activated sludge (Yu et al., 2018). Nonetheless, it is still unknown whether HFPO homologues can alter microbial community in natural or man-made environment. In addition, microorganisms are a crucial participator in nitrogen transformation (Ju et al., 2017). Ammonia oxidation is the first and rate-determining step in nitrification and it is important in soil nitrogen transformation (Wan et al., 2014). Both ammonia-oxidizing bacteria (AOB) and archaea (AOA) assign the role of ammonia oxidization. These two ammonia-oxidizing microorganisms (AOMs) harbor the ammonia monooxygenase (amoA) gene catalyzing ammonia conversion. AOA usually play a dominant role in salty, acid and nitrogen deficient environments (Nicol et al., 2008; Sterngren et al., 2015). Ammonia oxidation is sensitive to many pollutants such as heavy metal, antibiotics, pesticides and poly brominated diphenyl ethers (Du et al., 2018; Xia et al., 2019; Wang et al., 2018a), yet the effect of HFPO homologues on soil nitrification remains unclear.
Previous studies have indicated that emerging HFPO homologues influenced eukaryotic cells (e.g., zebrafish, mice and human cells) and caused estrogen disruption and hepatotoxicity (Li et al., 2019; Xin et al., 2019). HFPO homologues with longer carbon chains exhibit a strong binding affinity with estrogen receptors and peroxisome proliferator-activated receptors (Li et al., 2019; Xin et al., 2019). In addition, legacy PFASs of various chain lengths could have different consequences for bacteria in terms of membrane damage, oxidative stress, cell lesion and DNA damage (Nobels et al., 2010). Quorum sensing in bacteria was found to increase when exposed to PFASs with longer carbon chains due to the increase in cell membrane permeability (Fitzgerald et al., 2018; Mulkiewicz et al., 2007). Therefore, we hypothesized that HFPO homologues of different carbon chain lengths might cause different disturbances to soil communities. In this context, the objective of the current work was to explore the effects of different HFPO homologues on the microbial community and ammonia oxidation in soil.
Section snippets
Chemicals and materials
HFPO-DA (97% purity), HFPO-TA (98% purity) and HFPO-TeA (97% purity) were purchased from J&K Chemical Company (Beijing). At Peking University (Beijing, China, 39°59′33″ N, 116°18′6″ E), grassland soil (0–5 cm) without previous exposure to PFASs was selected to set up the microcosms. The collected soil was air-dried and stones and plant roots were removed. Soil was homogenized using 0.9-mm screen and then stored at 4 °C for subsequent experiments. The soil contained NH4+-N (5.53 mg/kg), NO2−-N
Microbial abundance
Archaeal and bacterial 16S rRNA gene densities were 1.48107−3.31108 and 1.56108−4.91108 copies/g of dry soil, respectively (Fig. 1a). The 16S rRNA gene density of bacteria outnumbered that of archaea on average (4.62 folds). At days 7 and 21, the archaeal gene density was decreased by the addition of HFPO-DA but it recovered in the later period. For example, the inhibition rate of high-dosage HFPO-DA on archaea was 73.9% at day 7 but the activation rate finally turned to 34.4% (
Effect of HFPO homologues on microbial abundance
In the present study, archaeal and bacterial abundance were lowered by all HFPO homologues at two dosages (0.1 and 10 mg/kg) in the earlier period, but recovered and even increased in the later period. Microorganisms can potentially be inactivated by PFASs via DNA damage, oxidative stress and membrane damage (Fitzgerald et al., 2018; Liu et al., 2016b; Yang et al., 2017). After the exposure to HFPO homologues, some sensitive microbial species might be phased out, which might account for the
Conclusions
Soil microbial communities showed different responses to the addition of HFPO homologues. Archaeal, bacterial and AOA abundance could be promoted by HFPO homologues after long-term incubation. AOB were sensitive to HFPO homologues. Ammonia oxidation could be impacted by HFPO homologues because of the changes in AOM communities and PNR. In addition, the type of HFPO homologues could also impact the soil microbial community and ammonia oxidation.
Author agreement
This manuscript is submitted for consideration of publication in journal Chemosphere. This paper has not been published before and all authors approve of its submittal. This work has no actual or potential conflict of interest including any financial, personal or other relationships with other people or organizations.
Declaration of competing interest
The authors declare that they have no competing interests.
Acknowledgments
This work was financially supported by the National Key Research and Development Program of China (2018YFC1803100), and the Special Fund of State Key Joint Laboratory of Environment Simulation and Pollution Control (19Y01ESPCP).
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These authors contributed equally to this study.