Uranium, which is a toxic radionuclide and can generally be found in the environment as a hexavalent ion, is considered one of the important energy sources as nuclear fuel. Uranium, which can originate from various processes related to mining, enrichment and nuclear power plants, nuclear weapons production and electron microscopy, has a high potential to reach aqueous environments. [
1,
2,
3]. Uranium found in wastewater and air can cause acute toxic effects and harmful diseases such as lung, pancreas and liver cancer in humans. The formation and migration of wastes, which generally contain high levels of dissolved uranium, lead to contamination of soils and aquifers, but it is possible to protect groundwater for long periods of time with multiple barrier systems such as compressed bentonite fill [
4]. Multiple barrier systems, as geotechnical and geological barriers, are used to minimize or even prevent access to water and the potential for the release of radionuclides from reservoirs near the site. Clay minerals are considered suitable materials for geotechnical and geological barriers due to their high adsorption ability and capacity, swelling properties and low water permeability [
5]. Illite , montmorillonite and illite/montmorillonite mixtures are the main components of claystone rocks [
6,
7]. The recovery of uranium from natural seawater, river water, stagnant water and industrial wastewater is also a priority research topic [
8].The main strategy of nuclear waste management discussed worldwide is their disposal in deep geological formations, where salt dome, crystalline rocks and clay rocks are considered potential areas for nuclear waste storage [
9].On the other hand, it is known that in a nuclear waste repository hosted by clay rock, radioactive decay of actinides and their fission products can cause high temperature increases of up to 100
o C near waste containers [
10,
11].Determining the transport regime and amount of radioactive contaminants within aquifers, soils, or rock formations requires detailed knowledge of the geochemistry of the system and radionuclide retention mechanisms such as adsorption, association, and precipitation. The World Health Organization (WHO) and the United States Environmental Protection Agency (USEPA) recommend limit values of 0.015 and 0.030 mg/L, respectively, for the maximum uranium concentration in drinking water [
12]. The retention potential of radio pollutants largely depends on their adsorption/desorption behavior [
13]. Controlling the mobility of uranium in temporary storage, waste processing and contaminated land is important for the safe disposal of uranium and supporting the management of operations at nuclear facilities. Due to their high thermal and radiation resistance, carbon-based materials are used for the removal and recovery of uranium from aqueous solutions using solid phase extraction techniques [
14]. Additionally, organic exchange resins and various inorganic sorbents are other commonly used materials. Carbon fiber with high specific surface area and adsorption capacity, uniform pore size and mechanical strength, graphene with high electronic and thermal conductivity, excellent mechanical strength as well as ultra-light weight and large specific surface area, and graphene oxide, which has basal plane modified with carbonyl, carboxyl, epoxide and hydroxyl groups, can be listed as adsorbents of great interest in this field [
15,
16]. One of the most promising separation technologies for the removal and recovery of uranium from radioactive waste is solid phase extraction (SPE) due to its properties such as flexibility and emulsion-freeness. Among various solid phase extractants, carbon nanotubes (CNTs) have also attracted intense attention for their advantages such as higher thermal and radiation resistance, high acid-base stability, and large specific surface area [
17,
18,
19,
20]. However, the fact that CNT particles, which are highly hydrophobic, easily aggregate in aqueous solution may prevent effective adsorption behavior and cause a decrease in adsorption capacity [
9,
10]. Therefore, by adding various hydrophilic functional groups to CNTs, their dispersibility and adsorption performance can be increased [
9,
10,
21]. There are many studies examining the behavior of uranium in aqueous systems containing amberlite resin and its adsorption to the solid phase. The main processes affecting the retention of radionuclides are absorption and precipitation at the solid/water interface, which need to be studied in detail from quantitative, kinetic and thermodynamic perspectives. [
22,
23,
24,
25]. Various processes such as chemical precipitation, liquid-liquid extraction, nano-ultra filtration, membrane separation, ion exchange, electrodeposition, solid phase extraction, electro dialysis, photo catalysis and adsorption are widely used to remove radioactive ions from wastewater [
26,
27,
28,
29,
30,
31,
32,
33]. Adsorption is one of the most popular methods and the easiest way to remove radioactive ions from aqueous solutions and is therefore widely applied in the removal of uranium from industrial wastes [
34,
35,
36,
37,
38,
39,
40].Uranium adsorption on various natural adsorbents and ion exchange resins with various properties such as porosity and selective affinity is important for the purification, economic, environmental and disposal of radioactive waste [
39,
41,
42].Anion exchange resins have also been used successfully in the mining industry, particularly in the recovery of uranium from leaching fluid [
43,
44,
45,
46,
47,
48]. In addition, activated carbon and zeolites, immobilized siloxane polymers, natural and modified clay, and synthetic anion exchangers are also widely used [
49,
50,
51,
52].Clay minerals, and especially bentonite, are a particularly preferred material for filling and capping high-level radioactive waste repositories.2:1 type clay minerals such as illite and montmorillonite, which are layered alumino-silicates in which TOT (tetrahedron-octahedron-tetrahedron) layers are repeated and have a permanent negative charge with isomorphic displacements within the lattice, are popular for such uses with their large surface areas and strong adsorption capacities. [
5,
6,
53]. Montmorillonite is characterized by permanently negatively charged basal planes and amphoteric hydroxyl groups on the edge planes. It is a very suitable adsorbent for lanthanide/actinide cations due to its ability to bind to basal planes predominantly in the outer sphere mode through cation exchange at low pH and inner sphere complexation to occur at the edges at high pH [
54,
55,
56]. A model frequently applied to describe the interactions of various radionuclides with clay minerals was developed by Bradbury and Baeyens. This semi mechanical two-domain model of protolysis, non-electrostatic surface complexation, and cation exchange was used to successfully describe sorption isotherm data over a wide pH range [
6]. Under oxidative conditions, uranium exists in the hexavalent oxidation state as the uranyl ion UO2+2 and can form highly soluble aqueous complexes with many ligands found in groundwater. Dissolved carbonate is ubiquitous, especially in surface and deep groundwater, and can form strong aqueous complexes with U(VI) [
58]. The formation of such complexes could potentially lead to a decrease in adsorption and thus an increase in the migration rates of U(VI). A detailed understanding of sorption processes under a wide range of conditions is extremely important in the development of sorption models. Various surface complexation models based on macroscopic sorption experiments have been developed to explain the adsorption behavior of uranyl, especially on montmorillonite [
59,
60,
61,
62,
63]. It has been suggested that at low ionic strengths, uranyl will adsorb primarily to cation exchange sites in the interlayer below pH 5 and to edge sites (silanol and/or luminol) above this pH. It has been predicted that at high ionic strengths, cation exchange will decrease strongly and sorption will occur mainly in the edge regions of montmorillonite from pH 5 onwards [
61,
64].In the presence of carbonate, the adsorption of U(VI) on montmorillonite and bentonite was investigated, and the sharp decrease in absorption observed at pHs greater than 6.5 was explained by the formation of negatively charged uranyl-carbonate complexes [
65,
66,
67,
68]. Depending on pH and U(VI) charge, outer sphere complexation, that is, cation exchange, occurring in the edge regions of clay minerals can be distinguished from inner sphere complexation [
13]. Natural polymers such as polysaccharides have shown excellent potential, especially in the removal of heavy metals from waters, and are advantageous due to their low cost, availability and the presence of hydroxyl, amino and other compounds [
69].In addition to the existing traditional methods in wastewater treatment, the adsorption process using polymer-grafted biomaterials such as cellulose, chitosan, chitin, starch and some synthetic polymers is gaining increasing importance [
70,
71,
72].
In this study, melamine formaldehyde organo clay nanocomposite (MFCNC) was prepared as a novel low-cost and promising solid adsorbent to remove U(VI), and its uranium (VI) adsorption performance from aqueous solution was examined. Additionally, variables such as adsorption time, initial pH, adsorbent dosage and temperature were selected as experimental parameters.