Anthropogenic pollution of Arsenic can be traced back to mining and other industrial activities, as well as pesticide and herbicide use in agricultural soils (Kahakachchi et al., 2004). Besides anthropogenic pollution, Arsenic can also be found naturally, e.g., in many subsurface drinking water aquifers (Oremland & Stolz, 2003). Arsenic, similar to Lead, Copper, Zinc, and Cadmium, is a potentially toxic metal, because even trace amounts of Arsenic can have a carcinogenic effect on humans (Mondal et al., 2006). The mode of toxicity varies depending on the chemical form of Arsenic. Arsenic exists in four oxidation states: Arsenate [As (V)], the predominant form of inorganic arsenic in aerobic aqueous environments; and trivalent arsenite [As (III)] in anoxic environments (Bilici Baskan & Pala, 2011; Kahakachchi et al., 2004; Oremland & Stolz, 2003; Yuan & Chiang, 2008). As(III) is 10 to 60 times more toxic than As(V) (Mukhopadhyay et al., 2018; Oremland & Stolz, 2003). Arsenate impedes the oxidative phosphorylation, whereas Arsenite impairs the function of many proteins by binding to sulfhydryl groups.
Arsenic is present in the soil as Arsenate and Arsenite (the inorganic forms), whereas monomethyl arsenic (MMA) and dimethyl arsenic (DMA) can be traced at lower amounts (Chowdhury, 2015). The presence of Arsenic in natural waters and soils can be attributed to the presence of iron (hydr)oxides because Fe-oxides strongly sorb Arsenate and Arsenite onto their surfaces, forming inner-sphere complexes (Suzuki et al., 2015; Violante et al., 2010). Arsenic can occur naturally in the soil in the range of 1–40 mg/kg (U.S. EPA, 2011; WHO, 1996). Regardless of the form of Arsenic, its concentration in soils needs to be controlled due to its potential toxicity. Canada has set a limit of 12 mg/kg for Arsenic in agricultural soils, whereas Australia, Czech Republic, Denmark, Poland, and the UK have a cap of 20 mg/kg (Chen et al., 2018; Liu et al., 2018). Environmental Protection Agency of the USA has limited the Arsenic concentration to 5.0 mg/L or 100 mg/kg for hazardous wastes. In South Korea, for an industrial land use area, Arsenic concentrations in the soils should be less than 50 mg/kg. Although the regulations are established, the arsenic contamination around the abandoned mines in South Korea (Ko et al., 2012) is still an issue that needs immediate response.
Although the remediation of Arsenic-contaminated soil and Arsenic-contaminated water is extensively studied, solidification and stabilization technique (Hunce et al., 2012; Kargar et al., 2015; Xia et al., 2019) has captured the attention of researchers due to the benefits associated with the technology. Different stabilizer compounds, such as limestone, steel mill slag, and granular ferric hydroxide (Ko et al., 2012), have been investigated. Among them, Zeolite (Babel & Kurniawan, 2003; Bilici Baskan & Pala, 2011; Pan et al., 2022) and Oyster shell (OS) powder (Moon et al., 2013; Ok et al., 2010; Torres-Quiroz et al., 2021) were effective in stabilizing potentially toxic metals, such as Pb, Cu, Cd, and Zn. However, OS powder was not effective in stabilizing Arsenic-contaminated soils (Lim et al., 2009). Many researchers have been investigating different chemical agents that can improve the performance of binding agents by adding oxidizing chemicals. Mondal et al. (2006) investigated the performance of Zeolite with chlorine and potassium permanganate (Mondal et al., 2006), and others (Bilici Baskan & Pala, 2011) observed that NaCl and FeCl3 solutions improved the performance of Zeolite (Clinoptilolite). Moreover, some researchers Smedley and Kinniburgh (2002) demonstrated that Ca increased the As (V) adsorption at high pH, and others Jang et al. (2016) showed that phosphate (PO4-3) improved Arsenic adsorption. Fe (III) has a high affinity for inorganic Arsenic. Thus, its use in the stabilization of Arsenic-contaminated soils has attracted the attention of scientific communities. Hydrous ferric oxide was the most effective compound for removing Arsenic (III) and Arsenic (V) from aqueous solutions because of the high specific area and iso-electric point (Huo et al., 2017). However, the removal of Arsenic was affected by the pH, in fact in soils, it was found that Arsenic sorption was less in Alkaline soils (pH range > 11). Most oxyanions including Arsenate become less sorbed when the pH increases (Cui et al., 2010; Dzombak & Morel, 1990), as a result it increases the arsenic mobility in alkaline soils. Therefore, the binders seek to reduce the mobility of Arsenic.
A large amount of oyster shells is being discarded as waste from various industries, and it is well known that the decomposition of OS emits toxic gases(Bonnard et al., 2020; Lim et al., 2009; Lu et al., 2018; Ramakrishna et al., 2018; Silva et al., 2019; Xu et al., 2019). The calcination properties of OS provides good characteristics for its use as a good alternative and a low-cost binder. However, calcium carbonate tends to increase the pH and has not shown good performance in controlling arsenic contamination. Considering these factors, this study aimed to enhance the performance of the OS powder by adding low doses of Fe (2) to converted it into a new value-added product.