Groundwater is a one of the world’s drinking water primary sources. Iron and ammonia are present in groundwater in dissolvable reduced state due to both natural, chemical environment and human activities [
1,
2,
3]. Metal ions in water resources causes a variety of aesthetic and operational issues, including repulsive unpleasant taste, laundry stains, and network accumulation [
4,
5,
6,
7] are caused issues by ammonia in ground water. Chemical oxidizing of ammonia and iron is useful, but harmful byproducts and secondary pollutants limits their use [
8,
9,
10,
11]. Iron is the fourth most prevalent element, the second most abundant metal in Earth’s crust [
12], and a common part of groundwater. Two types of iron sources in groundwater: geogeic and anthropogenic. Geogeic source is where groundwater flows from the aquifer’s soils, sands, gravels, and rocks [
13]. Anthropogenic sources e.g. industrial effluents, landfill leakages, acid mine drainage, and others lead to high concentrations in groundwater [
14]. Water percolating through soil and rock dissolves iron-containing minerals and keeps them in solution [
15], which are widespread in groundwater and surface waters with significant groundwater input [
16]. Staining, disagreeable tastes and appearances come from them [
17]. higher Fe concentrations hampered Fe
+2 oxidation and caused undesired properties. In addition, Presence of iron bacteria in water supply system alters the water smell and promotes the bacteria growth in pipes. Excessive iron content in groundwater creates technical challenges, failure of water supply systems, water quality degradation, and unwanted incrustations form in greater oxygen water, resulting in a reduction in pipe flow cross-section [
18,
19,
20,
21]. There are no health-related recommendations for the content of iron in drinking water. Based on taste and annoyance concerns, the World Health Organization recommends that the iron concentration in drinking water be less than 0.3 mg/L [
22]. Polluted water causes for 80% of diseases in affluent countries, with a death toll of 10 million every year [
23]. Elemental Fe is rarely found in nature because Fe
+2 and Fe
+3 interact with oxygen and sulphur-containing molecules creating oxides, hydroxides, carbonates, and sulphide. Oxides are the most common form in nature [
24]. Ammonia removal from water is accomplished using a variety of processes [
25,
26,
27,
28]. Many techniques are employed to recover Fe compounds from groundwater [
29]. Extracting iron compounds from groundwater for drinking purposes using aerobic oxidation wasn’t sufficient due to the full oxidation of Fe
+2 and the growth of iron bacteria on sand filters or valves, causing discoloration and turbidity. This study used a poly (acrylate/acrylamide) grafted with 3-chloroaniline to extract iron and ammonia through adsorption technique [
30,
31,
32,
33]. Synthesized grafted hydrogel grafted was studied using TEM, SEM, TGA, XRD, FTIR Computationally. Efficiency removal of iron and ammonia from groundwater was studied using contact time, adsorbent dosage, and temperature. The sorption data was evaluated by Langmuir, Frendlich, and Temkin’s models.