Md Rokonuzzaman, Li Wai Chin, Man Yu Bon, Tsang Yiu Fai, Ye Zhihong
Review
Arsenic Accumulation in Rice:Sources, Human Health Impact and Probable Mitigation Approaches
Md Rokonuzzaman1, Li Wai Chin1, Man Yu Bon1, Tsang Yiu Fai1, Ye Zhihong2
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The human body loading with arsenic (As) through rice consumption is a global health concern. There is a crucial need to limit As build-up in rice, either by remediating As accumulation in soils or reducing As levels in irrigation water. Several conventional approaches have been utilized to alleviate the As accumulation in rice. However, except for some irrigation practices, those approaches success and the adoption rate are not remarkable. This review presents human health risks posed due to consumption of As contaminated rice, evaluates different biomarkers for tracing As loading in the human body, and discusses the latest advancement in As reducing technologies emphasizing the application of seed priming, nanotechnology, and biochar application for limiting As loading in rice grains. We also evaluate different irrigation techniques to reduce As accumulation in rice. Altering water management regimes significantly reduces grain As accumulation. Bio- and nano-priming of rice seeds improve germination and minimize As translocation in rice tissues by protecting cell membrane, building pool around seed coat, methylation and volatilization, or quenching harmful effects of reactive oxygen species. Nanoparticle application in the form of nano-adsorbents or nano-fertilizers facilitates nano-remediation of As through the formation of Fe plaque or sorption or oxidation process. Incorporating biochar in the rice fields significantly reduces As through immobilization, physical adsorption, or surface complexation. In conclusion, As content in cooked rice depends on irrigation source and raw rice As level.
arsenic; rice; scalp hair; irrigation management; seed priming; nanotechnology; biochar; human health
Globally, 37% of terrestrial land is used for agriculture, and its major portion is used for rice production to feed more than half of the human population as a staple food (Smith et al, 2008; Islam et al, 2020a). Although more than a hundred countries currently produce rice worldwide, 14 Asian countries account for 90% of global rice production using groundwater as the significant irrigation source (Islam et al, 2016; Yu et al, 2020). Rice is a semiaquatic plant and requires a vast quantity of water starting from its establishment in the main fields (Mainuddin et al, 2020). Arsenic (As) is released into the groundwater both naturally and anthropogenically. The occurrence of As over its safe limit proposed by WHO (< 10 μg/L) and FAO (100 μg/L) for irrigation water is a significant concern worldwide (Chakraborti et al, 2018).
Of the total accumulated As in rice, inorganic As (iAs) accounts for up to 86%–99% (Rahman et al, 2014). Rice accumulates almost 10 times more As than other crops including barley, maize and wheat since reductive conditions prevail in rice fields (Williams et al, 2007), and naturally, this problem is even higher in Asian rice-producing countries such as Bangladesh, Indiaand China (Williams et al, 2005). Since approximately 54% of global rice production is used for local consumption and the rests are traded worldwide crossing the borders of the countries, which leads to place As enriched rice in the bowls of the daily meal of the people far from its country of origin (Meharg et al, 2009). Thus, rice consumption exemplifies a key route for As exposure in most nations, exclusively for populaces enjoying rice diets constituting up to 60% of their daily meal (Islam et al, 2016). Because of the daily consumption of rice, As accumulates and poses severe threats to the human body (Williams et al, 2005). Many researchers have revealed that chronic exposure to As may induce cancers and other diseases (Mazumder et al, 2000; Sobel et al, 2020).
To minimize the body loading of As through the consumption of contaminated rice, researchers suggested several mitigating strategies over the last few decades, focusing on their technical feasibility, practical applicability and efficiency (Kumarathilaka et al, 2020). Here,we evaluated human exposure with As through rice consumption and potential biomarkers used to trace the As, and also evaluated the impact of manipulating irrigation management, seed priming, some technical agronomic innovations such as nanotechnology and biochar application for limiting As loading in rice grains. Future research direction is also highlighted for producing safe rice.
Although there are both natural and anthropogenic sources of As exposure of humans, drinking of contaminated groundwater, and consumption of fish and rice cultivated with contaminated groundwater are the major natural sources. Since As toxicity is associated with its solubility, which is actually influenced by pH differences and redox variations(Upadhyay et al, 2019). For example, the bioavailability of As increases with an increase in soil pH (Yao B M et al, 2021), and the inorganic form of As such as As(III) is the stable form under reducing conditions, i.e., anaerobic soil, while arsenate As(V) is the dominant form under aerobic conditions (Meharg and Zhao, 2012; Upadhyay et al, 2019). Among the organic forms, in addition to some other methylated arsenicals, monomethylarsonous acid [CH3As(OH)2, MMA(III)], monomethylarsonic acid [CH3AsO–OOH, MMA(V)], dimethylarsinous acid [(CH3)2AsOH, DMA(III)], and dimethylarsinic acid [(CH3)2AsOO–, DMA(V)] are regarded as the critical metabolites of As metabolism, where several thiolated arsenicals are also considered potential As species available in soils and crops (Upadhyay et al, 2019). However, inorganic forms of As are known to be more toxic than organic forms due to their bioavailability and toxicological and physiological effects, and the toxicity of As species occurs in the following order: DMA(V) < MMA(V) < As(V) < As(III) (Baig et al, 2010; Upadhyay et al, 2019), while Luvonga et al (2020) claimed the following order of toxicity: DMA(V) = MMA(V) < As(V) < As(III). On the other hand, Nookabkaew et al (2013) found that the major As species in rice followed the order: MMA(V) < As(V) < DMA(V) < As(III).
When considering the species of As based on the spatial differences, various As species prevail in rice at different origins. According to Batista et al (2011), As(III) (39.7%) prevails in Brazilian rice, followed by DMA(V) (38.7%), As(V) (17.8%) and MMA(V) (3.7%). Torres-Escribano et al (2008) claimed that Spanish rice contains an average of 62% iAs. As(III) (60%–80%) prevails in Switzerland rice, followed by DMA(V) (20%), As(V) (15%) and MMA(V) (< 3%) (Guillod-Magnin et al, 2018). The market basket study of Sarwar et al (2021), collecting rice from 14 cities of Pakistan (= 438), suggested that Pakistani rice contains more As(III) than As(V). Indian and Bangladeshi rice contains almost 80% iAs (Williams et al, 2005), similar to Chinese rice (78% iAs) (Zhu et al, 2008), while the European Union (EU) and USA (46% iAs) rice contains a higher percentage of DMA(V) (Zavala et al, 2008; Zhao et al, 2013). According to Nookabkaew et al (2013), brown rice in Vietnam contains the highest amount of As(III) (190.50 ± 1.00) μg/kg compared to brown rice (110.45 ± 8.01) μg/kg and red rice (105.47 ± 7.13) μg/kg in Thailand.
As translocation from rice roots to grains involves several steps, which causes possible variations among genotypes, and higher accumulation in roots due to the transformation of As(V) to As(III) may minimize As translocation to aerial parts as well as grains (Islam et al, 2017; Suriyagoda et al, 2018). As accumulates in rice plants in the following manner: grain < husk < leaf < straw(stem) < root (Islam et al, 2016). However, Yao B M et al (2021) claimed that rice roots and leaves accumulate more As than stems and grains in the following order: grain < husk < stem < leaf < root. With rising soil As concentrations, plant As increases accordingly, and researchers have demonstrated overwhelming deviations in grain-As levels globally (Islam et al, 2016). Mukherjee et al (2017) reported that As in irrigation water is positively correlated with grain As. Soil-available As is also significantly correlated with As content in the roots (Bhattacharya et al, 2010a) and grains (Chohan et al, 2020), but no such relationship is observed between As in grain- and soil-total As (tAs) (Khan et al, 2010; Mukherjee et al, 2017), although soil-available As has a significant positive correlation with soil tAs (Kar et al, 2013). In contrast, Hossain et al (2008) explored a strong positive correlation between soil- and grain-tAs. According to Lu et al (2009), grain tAs levels usually increase with increasing soil tAs and reach a saturation plateau at > 10 mg/kg soil. However, Talukder et al (2012) claimed that straw As has a strong positive relationship with grain As for both boro (BRRI dhan29) and aman (BRRI dhan32) rice varieties. Similar findings were reported by Wu et al (2011).
Bogdan and Schenk (2009) revealed that soil tAs has a significant positive influence on the As content in rice straw and polished rice through linear multiple regression analysis. Considering grain As(V), DMA(V), As(III), arsenocholine (AsC) and MMA(V)as the dependent variables and soil tAs, root As species, straw As species and root tAs as the parameters for prediction, the stepwise multiple linear regression analysis of Ma et al (2017) showed that straw MMA(V) and straw As(V) explain 76% of the variance (2= 0.760) for grain As(III), where root arsenobetaine, straw MMA and straw As(III) explain 72% of the variance (2= 0.721) for grain As(V). The four predictors, root As(V), root tAs, straw MMA(V) and straw DMA(V) explain more than 85% of the variance (2= 0.854) for grain MMA(V); straw AsC, root As(III), straw DMA and soil tAs explain almost 90% of the variance (2= 0.907) for grain DMA, and 92% of grain AsC variance (2= 0.929) is explained by two predictors, root As(V) and straw AsC. According to Lin et al (2015), rice roots (2= 0.930) are a more significant determinant of grain As than rice straw (2= 0.560) and top soils (2= 0.000). However, Hossain et al (2008) and Lu et al (2009) in Bangladesh revealed a highly significant regression relationship between soil and shoot As, as well asbetween soil and grain As.
The status of various elements is critical to modulate the biogeochemical cycle of As, and many biological functions that can affect As accumulation in rice grains. As(III) and silicic (Si) acid use the same transport routes to reach the rice root cells, therefore, more Si input poses a significant antagonistic impact on As(III) and limits its uptake and aboveground transportation in rice (Ma et al, 2008). Similarly, higher phosphate content is vital in limiting As(V) absorption and accumulation in rice since both elements are chemical analogues and use the same transporter, OsPT8, to enter into the rice roots from the soil solution (Wang et al, 2016). Research revealed the linkage of nitrate (NO3–) to oxidize As(III) to As(V) in the presence of denitrifying bacteria (Oremland and Stolz, 2003). Chen et al (2008) showed that KNO3incorporation to rice soils decreases tAs level in shoots and roots by up to 40%. The environmental coexistence of As and sulfur (S) facilitates sharing identical chemical as well as biological redox transformations and interlinked biogeochemical cycles (Hollibaugh et al, 2005), where S is reported to facilitate the whole redox cycle (Hollibaugh et al, 2006). Williams et al (2009) revealed a significant decrease in grain As content with the increase in grain selenium (Se). Norton et al (2010) reported that higher As-containing varieties accumulate lower Se, Cu and Ni contents in rice grains.
Hydride generation-atomic absorption spectroscopy (HG- AAS), HG-atomic fluorescence spectroscopy (HG-AFS),inductively coupled plasma mass spectrometry (ICP-MS),ICP-optical emission spectroscopy (ICP-OES), high- performance liquid chromatography coupled to ICP- MS (HPLC-ICP-MS), electrothermal-atomization atomicabsorption spectrometry (ET-AAS),graphite furnace- AAS (GF-AAS), neutron activation analysis (NAA) and test kit method (low cost field based method) all can be used to detect As content in rice. Given the limit of detection constraints, only HG-AFS and ICP-MS are extensively used for determining As content in rice grains, while HG-AAS and ICP-OES are appropriate for higher As content in grains (Meharg and Zhao, 2012). Though ICP-OES is equipped for chromatographic eluent acceptance, it is still lack of the capability as a detector functioning to determine species of grain As (Tyson, 2013). The detection efficiency of ETAAS for As is two magnitude inferior than that of ICP-MS, however, it is possible to measure tAs by ETAAS adequate precision but not the iAs since it cannot work to detect capillary electrophoresis or chromatography (Tyson, 2013). HPLC-ICP-MS is preferred for measuring As species with the benefits of detecting low limit (Rasmussen et al, 2013). According to de la Calle et al (2011), with a view to mediating the issue whether the determination of iAs and tAs depends on their analytical method or not, a proficiency test was organized by the European Union Reference Laboratory for Heavy Metals in Feed and Food entitled ‘Report of the seventh inter-laboratory comparison organized by the European Union reference laboratory for heavy metals in feed and food IMEP-107: Total and inorganic As in rice’. The IMEP-107 (International Measurement Evaluation Programme-107) took the endeavor with 103 laboratories registered from 35 countries where results for tAs and iAs came from 98 and 32 laboratories, respectively, using different instrumental techniques (NAA, ICP-MS and HG-AAS). Results showed the grain iAs concentration measured does not rely on the analytical method used to determine, while all the instrumental methods are come across to be dependable to characterize grain As concentration. However, this conclusive remark cannot be justified independently due to lack of available raw database.
A significant variation in grain As content has been noticed with the variation in cultivation seasons, particularly, winter (boro) and monsoon (aman) seasons (Bhattacharya et al, 2010b). According to Imamul Huq et al (2011), the higher As loading in the rhizosphere and its rapid bioavailability during the winter season mainly due to the irrigation with As-contaminated groundwater in rice fields. Williams et al (2006) recorded the variability in rice growing seasons, boro and aman significantly determine the grain As content. Guo et al (2013) put forward an increased use of groundwater that might trigger dissociation of sediment-As into the groundwater facilitated by the iron oxyhydroxides dissolution or As(V)’s reductive desorption. In contrast, Chauhan et al (2009) argued no significant seasonal variance in groundwater As level in winter, monsoon and summer season. Cheng et al (2005) also claimed similar results. Roberts et al (2010) calculated a 13%–62% loss of soil As due to monsoon flooding accumulated during the winter crop cultivation. Such seasonal basis loss of soil As during rice cultivation has been reported in study of Lu et al (2009).
The quantity of daily As uptake via rice consumption is largely determined by the volume of rice in meals (Singh et al, 2015). According to the FAO (2004), the average consumption rate of rice for one person varies by up to 650 μg/din many Asian countries, where much lower consumption rates have been reported in some European and African nations. Out of the tAs content in rice, iAs accounts for approximately 96.8% (Roychowdhury, 2008), whereas rice from Asian countries contains up to 99% (Rahman et al, 2014). Exposure to iAs through rice consumption is responsible for internal and external cancers and many other diseases (Sobel et al, 2020). The daily intake of tAs through foods has been estimated in different countries. Mean daily tAs intake and its limit in rice and rice-based foods are presented in Table 1. The PTWI (Provisional Tolerable Weekly Intake) of As is 15 µg/kg body weight each week for everybody as established by FAO/WHO (Díaz et al, 2004). The NOAEL (No Adverse Effect Level) for chronic exposure through oral intake was established at 1µg/kg per day for everybody, where the LOAEL (Low Adverse Effect Level) for the same was established at 10–100 µg/kg body weight per day for everybody (Larsen, 1993;Díaz et al, 2004).
According to Mossop (1989), exposure to only 0.25 mg/kg iAs can generate poisoning symptoms in the human body. Just after ingestion, As is quickly metabolized and precipitously defecated in the urine, mostly following direct dietary exposure (Vahter, 2002). The rest of the As binds with the hemoglobin protein (Habib et al, 2002). Within 24 h, As present in the blood accumulates in various body organs, includingskin tissue, liver, spleen, bone, lung, kidney and muscle(Habib et al, 2002). Two to four weeks after absorption, the maximum As present in the body system is concentrated in the skin, nails and hairs, and gradually excreted (Habib et al, 2002).
Since As mobility in wetlands is controlled by the redox potential of soils, As mobility in rice fields and its uptake and transfer to rice grains can be minimized by altered water management (Zhao et al, 2010). Besides water management, seed priming (Moulick et al, 2016, 2017, 2018a, b), some technical agronomic interventions such as biochar (Wen et al, 2021) and application of nanotechnology (Maity et al, 2021) are some recently innovated techniques to limit As accumulation in rice.
Table 1. Mean daily total arsenic (As) intake and its limit in rice and rice-based foods.
WHO, World Health Organization; FAO, Food and Agriculture Organization of the United Nations; JFWCAC, Joint FAO-WHO Codex Alimentarius Commission; iAs, Inorganic As.
Very few field trials have been conducted with AWD as an As mitigation approach. A study by Das et al (2016) with three treatments, AWD, non-flooded (NF), and conventionally flooded (CF) practices, explored insignificant differences in soil As levels and found a decrease in grain As in the order of NF < AWD < CF, while yield contribution was reported in the increasing order of AWD > NF > CF. Compared with CF, AWD and NF treatments reduces tAs concentration in rice grain by 49.7% and 53.0%, respectively. Further, significant (< 0.05) decreases in As(V) and As(III) levels in husks and grains are reported in NF and AWD than in CF. The enhanced phytoavailability of As in CF might be due to the enhanced reductive mobilization of As in flooded conditions (Roberts et al, 2010). Chou et al (2016) and Acharjee et al (2021) support this finding concerning As reduction in AWD compared with CF. Acharjee et al (2021) revealed significant As reduction in rice under AWD compared with CF. Chou et al (2016) investigated the effect of CF, aerobic (AR) and AWD irrigation practices on As loading status of two rice varieties Tainan 11 and Tainong 84, each in one season. The result reported that As(III) (AWD < AR < CF) prevails in brown rice in the both rice season, followed by As(V) and DMA(V). Grain tAs content reduces significantly in AR and AWD compared with CF because of the changes in oxidation and reduction process due to irrigation management.
While practicing single soil drying with ‘safe AWD’, Carrijo et al (2018) observed that grain As content does not decrease at ~0 cm soil water potential at 0–15 cm below the soil surface, but soil drying to -71 kPa or -154 kPa, marked as medium severity and high severity, respectively, reduces 41%–61% of grain As. They suggested that since the grain As level reductionlargely depends on soils reaching the unsaturated state, safe AWD allows continuous saturation state and therefore cannot perform well. This finding is comparable with the results of Islam et al (2019) and Yang et al (2019). The field trials of Rahman et al (2015) and Shah et al (2016) revealed AWD practice contributes significant grain As reduction with higher grain yield compared to continuous flooding.
The two-year field trial of Linquist et al (2015) in the USA with several irrigation treatments revealed that AWD accounts for a yield decline (< 1% to 13%), but the As content in rice grains under AWD decreases remarkably compared to that under CF. In contrast, when practicing AWD with fertilizer management, Islam et al (2020b) observed that early AWD practices reduce grain As by 66% without sacrificing grain yield. This sustained yield with AWD management agrees well with the previous studies (Qin et al, 2010; Islam et al, 2017). AWD’s success largely depends on the rice variety selected (Norton et al, 2019). Grain As levels are increased with the increasing number of identifying quantitative trait loci (QTLs) in selected rice varieties (Norton et al, 2019; Fernández-Baca et al, 2021). For example, Norton et al (2019) conducted a 2-year study with AWD irrigation management and some rice varieties to determine genotype by the interaction of water management with QTL for As accumulation. They observed a 15.7% grain As reduction in the first year when the declining percentage is 15.1% in the next year, and concurrently, 27% less As accumulation is recorded compared to continuous flooding practice. They reported that six QTLs exhibit stability in water treatments across years out of a large number (74) identified individual QTLs for As. On the other hand, Fernández-Baca et al (2021) identified seven QTLs influencing grain iAs accumulation such as C4_2481896, C4_27292997, C5_19872059, C8_5186967, C9_18034390, C11_2659978 and C12_824609.
Xu et al (2008) evaluated As accumulation in a greenhouse experiment in rice grains and shoots under aerobic and flooded conditions. Under CF condition, the As level in the soil solution was 7–16- and 4–13-fold higher than that under NF conditions, i.e., without As and adding As (added 10 mg/kg as arsenite or arsenate), respectively.CF enhances the reductive dissolution of iron oxyhydroxides, which facilitates the dissociation of the adsorbed As to the solution. However, the result represents 10–15-fold grain As and 10–15-fold grain yield reduction compared to CF. They also claimed that with increasing tAs level in rice grains, the proportion of DMA(V) increases while iAs (predominant species) decreases. Arao et al (2009) reported tAs, iAs and DMA reduction in rice grains (tAs from 950 to 100 μg/g; iAs, As(III) + As(V), from 450 to 120 μg/g; DMA from 480 to 10 μg/g) of Koshihikar rice variety in aerobic rice cultivation than those for flooded cultivation. The greenhouse experiment of Li et al (2009) and the pot experiment of Talukder et al (2012) support this finding. As a semiaquatic plant, rice cultivation typically needs a flooding state to ensure maximum yields, therefore, substantial grain yield losses have been recorded under aerobic irrigation practices (Sarkar et al, 2012). In contrast, Duxbury and Panaullah (2007) found a positive impact on rice yield while practicing aerobic irrigation regimens.
In a field experiment, Somenahally et al (2011) found grain As reduction upto 50% for As(V) and 5%–30% for As(III) inaddition to tAs in intermittent flooding (IF) than CF plots. According to Shrivastava et al (2020), IF gradually reduces grain As by 40%–63% in the consecutive years of 2013 to 2016. The possible explanation behind such grain As reduction in IF is the lower irrigation requirement and subsequent lower As bioavailability. Xu et al (2008), Sarkar et al (2012) and Spanu et al (2012) support the above findings. While comparing intermittent ponding with aerobic ponding, Sarkar et al (2012) argued a decrease in As content in roots, leaves and grains in the order of intermittent ponding > aerobic regimes. The only exception is Duxbury and Panaullah (2007), who could not generate a conclusive argument for the effect of deficit irrigation practice on reduced grain As content. The selection of suitable rice variety determines IF practice’s performance. For example, Hua et al (2011) revealed statistically similar (< 0.98) As accumulation on Cocodrie and Rondo rice varieties, while another variety, Zhe 733, accumulates much less As (< 0.07 or 0.12) in similar water management and soil As content.
Duxbury and Panaullah (2007) conducted a field trial with a boro rice variety BR29 with two irrigation regimens, conventional flooding and raised bed practice. The results indicated a reduced straw and grain As accumulation in aerobic practice than in conventionally flooded plots. This reduction is possibly due to the less-reducing state in the soil during the rice growth stage (Somenahally et al, 2011). Talukder et al (2011) observed that raised bed cultivation requires 30% less water use than conventional practices and simultaneously reduces straw and grain As by 86% and 62%, respectively, with an increase of 13% in grain yield. The possible reason might be that there remains a higher redox potential (Eh) value in raised beds than the conventional rice fields and thus contains low As content. Similar to permanent raised beds, furrow- irrigated periodically raised beds significantly decreasebioaccumulation of As compared with the conventionally flooded practice (Talukder et al, 2011). Iron- oxyhydroxides are pretty stable in the furrow-irrigated fields because of a comparatively oxidized state there, which ultimately keeps the soil As unavailable to the rice plants (Aide et al, 2016).
Moreno-Jiménez et al (2014) compared flooded and sprinkler irrigation (SI) practices under the Mediterranean regime with rice variety Gladio. The results revealed that grain tAs decreases over seven years in successive SI to one-sixth (tAs decreases from 547 to 89 μg/g; iAs decreases from 138 to 25 μg/g) of it’s early concentration in the submerged system, while one-third (tAs decreases from 547 to 200 μg/g; iAs decreases from 138 to 70 μg/g) of grain As is reduced in only one cycle of SI, with no significant difference for yield between the two practices. On the contrary, iAs and DMA concentration in ricegrain are enhanced by two folds under CF compared with SI, which might be due to the methylation under CF condition. The field trial of Spanu et al (2012) with 37 genotypes revealed 50 times (tAs reduced from 95–235 μg/g to 1.3–5.1 μg/g) less grain As under SI than those under CF. However, for all genotypes, a total of 95.5% to 98.0% As is reduced. They added such extensive genotypic variability in As bioaccumulation suggests a ‘genetic variability effect’. Genetic effect on As bioaccumulationin rice is also evident (Norton et al, 2009; Ahmed et al, 2011). Since 9%–10% of the variability of grain As accumulation accounts for the genetic variation (Ahmed et al, 2011), the environment plays a crucial role by 69%–80% in the amount of As accumulation in rice grains (Norton et al, 2009).
There is a range of seed priming techniques, viz., osmopriming, hydropriming, nutripriming, hormonal priming, biopriming, nanopriming or some plant- based natural extracts (Farooq et al, 2019). Different parameters for seed priming with the consequesnes for rice are presented in Table 2.
Table 2. Effect of seed priming on arsenic (As) accumulation and toxicity in rice plant.
Mridha et al (2021b) suggested that the overall impact of potassium humate (K-humate) on As stress is the gibberellin and abscisic acid regulating capacity of both K and humic acid and the metal chelation characteristics of humate. Moulick et al (2016, 2017, 2018a, b, 2019) proposed that rice seed priming with selenium (Se) prior to sowing may stimulate seed germination, and increase seedling growth by quenching the harmful effects of reactive oxygen species, and reduce As induced toxicity by building Sepool around the seed coat and enhancing detoxification, and defend the damage of cell membrane by maintaining total phenolics and proline and decrease As uptake by As-induced redox imbalance modulation in both soil-less and soil-based environments.
Upadhyay et al (2021) reported a decline in As uptake by rice roots in Thiourea (TU) amendment might be attributed to the expression changes of As transporters such as(). Further, nodes and shoot tissues play a potential role in As sequestering to cell walls and vacuoles to limit its upward transportation. TU application works at the molecular level and controls redox which acts critically to maintain the reduced As(III) to facilitate its sequestration. Yadav and Srivastava (2021) also reported a similar finding. Verma et al (2019) suggested the seedling improvement and significant As reduction in rice plantsmight due to the methylation and volatilization process imparted by genetically engineered (GE) yeast. This finding is comparable with the result of Chen et al (2014) using GE microorganisms. Enhanced seed germination and improved seedling growth parameters reported by Sivakumar et al (2017) with phosphobacteria are due to its phosphorus solubilizing capacity. Apart from the above, Kumar et al (2022) foundleaf extract ameliorates As toxicity through limiting malondialdehyde level and electrolyte leakage.
The prime benefit of priming rice seeds in respect of impacting the agro-environmental factors is that this technology bypasses soil texture, presence or absence of cationic and anionic species, pH for irrigation water and soil, redox potential (Eh), varietal differences, agronomic practices and seasonal aspects that can influence As loading in the plant (Moulick et al, 2021). Nanomaterial utilization in seed priming supplements nutrients, and enhances nitrogen use efficiency and consequently reduces chemical fertilizer application and protects the agro-environmental (Upadhyaya et al, 2017; Priya et al, 2018). Despite substantial improvements in the utilization of seed priming nanotechnology in rice cultivation, of concern, there is still no general rule regarding the nanopriming of rice seeds and no distinct trend concerning the responses of priming based on the species taxonomy (Shelar et al, 2021). Such misdirections can facilitate bacterial and fungal contamination, significantly impacting the rice agro-environment and subsequently hindering seed germination (do Espirito Santo Pereira et al, 2021). Extensive research is still required in applying nanomaterials and nanoparticles used for priming rice seeds, particularly for shaping the comprehensive impact of those techniques on rice agro-environment and human health (Moulick et al, 2021; Shelar et al, 2021).
In recent years, the rapid advancement and utilization of nanotechnology hastens the invention of engineered nanoparticles and their practical applications in crop production (Wang et al, 2019). The modification of the synthesized nanomaterials into nano-adsorbents, nanofertilizers and nanopesticides makes it suitable for need-based nano-remediation of heavy metals (Khan et al, 2020; Ma et al, 2020; Maity et al, 2021). Different parameters and consequences of nanoparticlescurrently being used predominantly for As reduction in rice production are presented in Table 3.ZnO and zinc ion (Zn2+) significantly lowers the As load in rice tissues (Ma et al, 2020), suggesting thattransporter might have been affected by the Zn2+treatment. The significant decrease of As(V) in Zn2+amended roots may be because of enhanced reduction of As(V) into As(III) by As reductase within the root cells. Wu F et al (2020) and Yan et al (2021) suggested that the significant improvement in germination, promoted biomass, and reduced As accumulation in rice are due to the supplement of Zn nutrients upon ZnO application. On the other hand, Wang et al (2018) claimed a possible negative phyto-effect of co-occurring As(V) or As(III) and ZnO NPs (nanoparticles), leading to a significantly weak performance of As transporters for less As content in rice plants.
Wu et al (2021) demonstrated that nano-titanium oxide (TiO2) amendment notably alleviates oxidative stress resulting from As exposure and significantly reduces As bioaccumulation in rice seedlings. According to Li et al (2019), the addition of α-MnO2nanorods can effectively control the soil-to-solution partitioning of As under anaerobic conditions, which dramatically reduces the mobilization and transportation of As in soil-rice systems. Zhou et al (2015) reported a significant negative relation between As and Mn in rice, leading to less As loading in rice. Liu et al (2014) showed that reduction of As content in brown rice is possibly by As sequestration into shoot cell walls facilitated by nanoscale silica (Si) of rice shoot. Cui et al (2020) found that the minimized As uptake in rice is due to the loweredand2 gene expression.
Hu et al (2020) revealed iAs reduction in rice is due to Fe plaque formation upon zerovaleation (Fe0)application. On the other hand, Huang et al (2018) found nano-Fe3O4and nano-Fe0lower the effect of antioxidants to the aboveground portion of rice plants.
Table 3. Effect of nanotechnology on arsenic (As) accumulation and toxicity in rice plant.
Fe0, Fe plaque formation upon zerovaleation; DMA, Dimethylarsinic acid; MMA, Monomethylarsonic acid; iAs, Inorganic As; tAs, Total As.
Khan et al (2020) showed Fe3O4attracts negatively charges As on its surface and reduces As entry. Wang et al (2019) addressed CuO’s unique ‘nano-effect’ for impacting As loading in rice. Liu et al (2018a) reported that CuO decreases the As concentration below the ‘no observed adverse effect level’ (0.80 μg/kg per day) by reducing the life cycle of rice plants.
Biochar is prepared through the thermal decomposition of organic biomass under low levels of O2(pyrolysis) (Kumarathilaka et al, 2020). Different parameters of biochar including its preparation, using media and effect on rice are presented in Table 4. According to Khan et al (2014), sewage sludge- derived biochar increases the phosphate content which protects As to be transferred together with the same transporter. Seyfferth et al (2016) observed the formation of As-DOC (dissolved organic carbon) complexes speeds up As immobilization due to the application of rice husk-derived biochar (1%) enriched with Si. According to Wu et al (2017), rice straw biochar modified with the red mud develops special features by combining metal oxides of red mud with the large surface area and porous structure of biochar. Wu J Z et al (2020) revealed that calcium-based magnetic biochar (Ca-MBC) facilitates the adsorption of pore water As and limits rice As. Yu et al (2017) suggested that manganese oxide reduces As content because it can strongly adsorb As(V) and promote arsenite to arsenate oxidation.
As reduction in rice tissue uponiron-manganese oxide modified corn straw-based biochar (FMBC1) application reported by Lin et al (2017) is due to the oxidation of As(III) to As(V) which might be facilitated by Fe-Mn oxide and the formation of Mn and Fe plaque on the root surface. Qiao et al (2018, 2019) explored that the palm fiber and Fe0application might impose a synergistic effect and reduce As bioavailability by forming Fe plaque. Pan et al (2019) observed that the grain As reduction is facilitated by the increase in soil pH by single or combined application of biochar/FeSO4/silica sol. On the other hand, Leksungnoen et al (2019) and Linam et al (2021) suggested that Si facilitates the methylation of As and reduces As uptake by rice plant.
According to Rong et al (2020), biochar +Fe(II) facilitates Fe plaque formation and limits As content in rice tissues. The As immobilization for modified rice husk-based biochar application is facilitated by (i) oxidation of As(III) to As(V) bygene, (ii) lowering of microbe mediated As release from iron minerals, and (iii) adsorption on a Si-ferrihydrite complex(Herath et al, 2020). Liu et al (2020) postulated that carbide slag amendments change the forms of As to less-available and form Fe-Mn plaque to restrict As transfer in rice.
Islam et al (2021a) recorded substantial grain As reduction due to the formation of Fe-plaque in roots. Similarly, Yao Y et al (2021) revealed As reduction in rice since As gets bound with the crystalline hydrous oxide and Fe-plaque. According to Kumarathilaka et al (2021a), As reduction in RBC (rice biochar) is due to the introduction of Si and sulphate in rice water. Kumarathilaka et al (2021b) suggested that grain As reduction in birnessite-modified rice hull biochar (Mn-RBC)-intermittent water management facilitates through oxidation of As(III) by Mn. Wen et al (2021) revealed a significant grain As reduction might be due to the reduction of soil urease and catalase activities with Fe+ biochar application.
According to Lin et al (2021), the application of corn stem-based biochar amended with Fe-Mn-La can control As volatilization, and reduce methylation, crystallization and dissolution of As. Yang et al (2020) revealed that-gene carried byand-gene carried byandpotentially mediate As(V) decrement under straw and straw biochar amendments, respectively. On the contrary, Wang et al (2017) showed that the supplementation of biochar augments the richness ofandgenes, which is associated with the reduction of As(V) into As(III). Zhang et al (2020) showed that the corn stalks derived biochar amended with iron-manganese-cerium oxide decreases As bioavailability, and improves soil pH and potentially enhances soil redox capacity. With similar biochar and amending materials, Lian et al (2020) showed grain As reduction due to the formation of Fe-Mn plaques, which restricts the As uptake by the rice plants.
The prime causes for higher As content in cooked rice in As burdened regions are the As content in raw rice derived from soils and irrigating As contaminated groundwater and cooking with As-contaminated water (Mridha et al, 2021a). Again, since changes in As speciation are not evident due to cooking, the As species present in the cooked rice depends on its source orientation, which means cooking water or raw rice. Laparra et al (2005) revealed no significant modifications in iAs and tAs contents in cooked rice boiled with uncontaminated water while iAs concentrationis increased found after adding As(V) in the cooking water. O’Neill et al (2013) measured 24 times higher iAs ingestion through cooked rice whencooking water containing As above 50 μg/L. Similarincreasing trend is also evident from the studies of Roychowdhury (2008) and Mandal et al (2019). Sengupta et al (2006) revealed that the traditional method of cooking (at rice water ratio of 1:6) with less As-contaminated water and discarding gruel removes approximately 57% of As in the cooked rice while cooking rice with As contaminated water of 50 μg/L enhances up to 35%–40% of As in cooked rice. According to Mridha et al (2021a), cooking rice with As-safe water significantly releases As into the gruels. The result of Chowdhury et al (2020) supports this finding. Bae et al (2002) measured the retained As content in cooked rice as the impact of boiling and observed a higher As content in cooked rice than the raw rice, which might be due to the induced chelating effect. Laparra et al (2005) explored the iAs and tAs in cooked rice simulated gastrointestinal digestion.
Table 4. Biochar type to mitigate arsenic (As) accumulation and toxicity in rice.
Fe0, Fe plaque formation upon zerovaleation; Fe-BC, Iron-modified biochar; MMT, Montmorillonite; iAs, Inorganic As; tAs, Total As.
Gray et al (2016) demonstrated a decreasing trend of grain iAs accumulation while cooking As contaminated brown longgrain, white medium grain, and parboiled rice with deionized water at a ratio of 2:1, 6:1 and 10:1 (water:grain) with increasing the volume of water. Cooking with a low amount of water does not eliminate As content, however, increasing water volume reduces up to 45% of iAs. A similar trend has been reported with As water by Jitaru et al (2016). Liu K L et al (2018) and Liao et al (2019) revealed an insignificant change in As concentration in cooked rice cooking in pressure cooker and stainless steel pot with deionized water. Menon et al (2021) tested a revised absorption method combining some cooking techniques. They suggested that parboiled and absorbed treatmentsdecrease 73% and 54% of iAs in white and brown rice, respectively.
The future research should consider integrating water management with other As mitigating strategies such as the application of nanotechnology, biochar and/or seed priming to avail the dual effect for bioaccumulation of As in rice.
This study was supported by the Seed Funding Grant (Grant No. RG53/19-20R), General Research Fund Proposal (Grant No. RG21/2020-2021R), Dean’s Research Fund (Grant No. IRS-10-2020) and Department of Science and Environmental Studies Grant for Collaborative Research Project of the Education University of Hong Kong, China (Grant No. 04487).
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28 October 2021;
11 February 2022
Li Wai Chin (waichin@eduhk.hk)
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