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Frontiers of Environmental Science & Engineering

ISSN 2095-2201

ISSN 2095-221X(Online)

CN 10-1013/X

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2018 Impact Factor: 3.883

Front. Environ. Sci. Eng.    2023, Vol. 17 Issue (12) : 145    https://doi.org/10.1007/s11783-023-1745-6
RESEARCH ARTICLE
Elevated methylmercury production in mercury-contaminated soil and its bioaccumulation in rice: key roles of algal decomposition
Di Liu1,2,3, Yan Wang1,2,3, Tianrong He1, Deliang Yin1(), Shouyang He1, Xian Zhou1,2,3, Yiyuan Xu2, Enxin Liu1,2,3
1. Key Laboratory of Karst Georesources and Environment (Ministry of Education), Guizhou University, Guiyang 550025, China
2. College of Resources and Environmental Engineering, Guizhou University, Guiyang 550025, China
3. Guizhou Karst Environmental Ecosystems Observation and Research Station, Ministry of Education, Guiyang 550025, China
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Abstract

● AOM input elevates water-soluble cysteine and labile DOM fractions in soil.

● AOM input fuels potential Hg methylators and non-Hg methylators in soil.

● Decayed algal aggregate is Hg methylating “hotspot” and MeHg source in soil.

● AOM-driven SDOM variations elevate soil MeHg production and bioaccumulation in rice.

Algal-derived organic matter (AOM) regulates methylmercury (MeHg) fate in aquatic ecosystems, whereas its role in MeHg production and bioaccumulation in Hg-contaminated paddies is unclear. Pot and microcosm experiments were thus performed to understand the response characteristics of MeHg concentrations in soil and rice in different rice-growing periods to algal decomposition. Compared to the control, algal decomposition significantly increased soil water-soluble cysteine concentrations during the rice-tillering and grain-filling periods (P < 0.05). It also significantly lowered the molecular weight of soil-dissolved organic matter (SDOM) during the rice-tillering period (P < 0.05) and SDOM humification/aromaticity during the grain-filling period. Compared to the control, AOM input increased the abundance of potential Hg and non-Hg methylators in soil. Furthermore, it also greatly increased soil MeHg concentrations by 25.6%–80.2% and 12.6%–66.1% during the rice-tillering and grain-filling periods, with an average of 42.25% and 38.42%, respectively, which were significantly related to the elevated cysteine in soil and the decrease in SDOM molecular weight (P < 0.01). In the early stage (within 10 days of microcosm experiments), the MeHg concentrations in decayed algal particles showed a great decrease (P < 0.01), suggesting a potential MeHg source in soil. Ultimately, algal decomposition greatly increased the MeHg concentrations and bioaccumulation factors in rice grains, by 72.30% and 16.77%, respectively. Overall, algal decomposition in Hg-contaminated paddies is a non-negligible factor promoting MeHg accumulation in soil-rice systems.

Keywords Mercury      Methylmercury      Algae      Organic matter      Rice (Oryza sativa L.)     
Corresponding Author(s): Deliang Yin   
Issue Date: 12 July 2023
 Cite this article:   
Di Liu,Yan Wang,Tianrong He, et al. Elevated methylmercury production in mercury-contaminated soil and its bioaccumulation in rice: key roles of algal decomposition[J]. Front. Environ. Sci. Eng., 2023, 17(12): 145.
 URL:  
https://academic.hep.com.cn/fese/EN/10.1007/s11783-023-1745-6
https://academic.hep.com.cn/fese/EN/Y2023/V17/I12/145
Fig.1  DOC (a) and water-soluble cysteine (b) concentrations in Hg-contaminated soils regulated by algal decomposition. Data are represented by average ± standard deviation (AVE ± SD). Different lowercase letters indicate significant differences between different rice growing periods at the same treatment at 0.05 level. “**” and “*” represent the significant differences between algal treatments and the control at 0.01 and 0.05 levels at the same rice growing period, respectively. (A3.5, A7, and A15 = algal treatments with 3.5, 7, and 15 g biomass, respectively).
Fig.2  Optical properties of soil DOM including a(355) (a), SR (b), SUVA254 (c) and HIX (d) regulated by algal decomposition. Data are represented by AVE ± SD. Different lowercase letters indicate significant differences between different rice growing periods at the same treatment at 0.05 level. “*” represents the significant differences between algal treatments and the control at 0.05 level at the same rice growing period. (A3.5, A7, and A15 = algal treatments with 3.5, 7, and 15 g biomass, respectively).
Fig.3  Fluorescent components in soil DOM regulated by algal decomposition (a–b), and their 3D-EEMs (c). C1, C2 and C3 represent humic-like components, and C4 represents protein-like components. Data are represented by AVE ± SD. Different lowercase letters indicate significant differences between different rice growing periods in the control or algal treatment at 0.05 level, and “*” represents the significant differences between algal treatments at 0.05 level. (A3.5, A7, and A15 = algal treatments with 3.5, 7, and 15 g biomass, respectively).
Fig.4  Abundance of potential MeHg regulators including Hg methylators and non-Hg methylators regulated by algal decomposition at Phylum (a) and Genus (b) levels. (A15 = algal treatments with 15 g biomass).
Fig.5  Absolute THg and MeHg contents in the decayed algal particles in the pot experiment (a). Decomposition percentage and residual mass of algal powders in the microcosm experiment (b). Absolute THg (c) and MeHg contents (d) in the algal particles in the microcosm experiment. Data are represented by AVE ± SD in the graphs a, c and d. Different lowercase letters indicate significant differences between different incubation time at 0.05 level. (“AW” = “algae + water”; “AWS” = “algae + water + soil”; A3.5, A7, and A15 = algal treatments with 3.5, 7, and 15 g biomass, respectively).
Fig.6  MeHg concentrations in soil (a), THg concentrations in husks and grains (b), MeHg concentrations in husks and grains (c) and bioaccumulation factor (BAF) of MeHg in grains (d) regulated by algal decomposition. Data are represented by AVE ± SD. Different lowercase letters indicate significant differences between different algal treatments and the control at 0.05 level. (A3.5, A7, and A15 = algal treatments with 3.5, 7, and 15 g biomass, respectively).
Fig.7  Pearson’s correlation matrix of soil MeHg concentration with soil DOM properties (DOC concentration, HIX, a(355), SUVA254, SR, C1, C2, C3 and C4) and soil cysteine concentrations (a); Linear fitting between soil MeHg concentration and inorganic Hg (IHg = THg minus MeHg), or MeHg concentration in rice tissues (b).
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