About 80% of communicable diseases around the world are waterborne (
1,
2). Access to improved drinking water is unavailable to an estimated 884 million people around the world, most of which live in rural, dispersed, and often remote communities in developing countries (
3).
There are many pollutants in water, such as pathogenic organisms, fecal matter, suspended solids, algae, organic matter, and harmful chemicals. Among the various adverse pollutants, coliform bacteria and arsenic are very important (
4,
5). Coliform bacteria are the indicator of water contaminated with human or animal wastes and if these exist in water, it is unsafe for drinking purposes. Generally, all bacteria are not harmful but other microbes could cause short-term health effects, such as diarrhea, cramps, nausea, headaches, or other symptoms (
5,
6).
Arsenic (As) contamination in groundwater, used for drinking purposes, has been envisaged as a problem of global concern (
7). Elevated arsenic concentration in drinking water sources is an issue of global concern and threatens over 200 million people worldwide, especially in Asia. Arsenic has been reported in groundwater of Bangladesh, Cambodia, China, Taiwan, Mongolia, India, Japan, Myanmar, Nepal, Pakistan, Thailand, Viet Nam, and Iran (
8-
10). In the rural areas of west and northwest Iran, Kurdistan and Azerbaijan provinces, arsenic contamination of groundwater was reported (
9). Arsenic exists in multiple oxidation states (+5, +3, 0 and -3); arsenate As (V) and arsenite As (III) are the most common inorganic forms of arsenic in aquatic environments. Arsenate species (AsO
43-, HAsO
42-, and H
2AsO
4-) are considered as soft acid and mostly stable in oxygen rich environments. However, arsenite species (AsO
33-, AsO
2OH
2-, As (OH)
4- and As(OH)
3) are stable in moderate reducing environments, such as underground water. Furthermore, As (III) has higher toxicity and greater mobility, which needs to be oxidized for better adsorbption of As (V) (
8,
11).
Arsenic in aqueous systems can originate from natural sources (e.g., geochemical reactions and volcanic emissions) as well as anthropogenic activities (such as metal mining, industrial waste discharge, and agricultural use of arsenical pesticides) (
12). These sources could pollute water systems, especially groundwater aquifers from different sources. Drinking of arsenic-contaminated water has become a serious threat to public health, and has affected millions of people across the world (Kong et al. 2014). Ingestion of inorganic arsenic could result in both cancer (skin, lung, and urinary bladder) and non-cancer effects (
13). Long-term exposure to high levels of arsenic may cause serious health problems, including skin, cardiovascular, neurological, renal, and respiratory diseases in humans (
8,
14). To reduce the incidence of waterborne diseases and make the water suitable for human consumption, the removal of water pollutants are absolutely necessary (
4,
15).
The world health organization (WHO) has set guidelines of 0.01 mg/L and 0 MPN/100 mL for arsenic and coliform bacteria in drinking water, respectively (
16).
Different treatment technologies to reduce concentrations of arsenic in drinking water are available or under investigation. Some of these include coagulation (
17,
18), sedimentation-filtration (
19,
20), nanofiltration (
21,
22), reverse osmosis (
21,
23), fluidized-bed sand reactor, and subsurface groundwater treatment (
24). Nevertheless, these technologies are inappropriate for application in rural communities (
25). Therefore, in these communities, simplistic design, and minimum maintenance and operating cost are some important factors that require consideration (
26). More than 50 household treatment technologies exist worldwide for water pollution removal (
24). Arsenic removal by low-cost adsorbents, such as filter based granulated adsorbents, has been the most promising technique, which meets all the mentioned criteria offering reliable and efficient performance for communities living in scattered settlements (
8,
25,
27). However, natural adsorbents are favorable for their low-cost and abundant sources, yet, some studies have shown that they had no sufficient capacity to remove total arsenic (As (III) + As (V)) from water resources (
28,
29). For example, natural adsorbents, such as limestone, and zeolites like clinoptilolite, chabazite, and sandy soils have been studied for arsenic removal in water (
30). The acceptable level of concentration of arsenic in drinking water is 0.01 mg/L (
31). Pravin et al. in 2009 used conventional and modified filters to remove coliform bacteria and arsenic. The study results showed that the efficiency of conventional and modified filters to remove coliform bacteria were 99.95% and 99.99%, and in the removal of arsenic were 14% and 75%, respectively (
6). The study results of Aviles et al. in 2013 showed that the efficiency of the domestic filter in arsenic removal was 95.4% (initial concentration of 0.11 mg/L) (
24). The considerable removal efficiencies of arsenic were also reported by several studies that used household filter, ceramic filter, and modified natural zeolite filter in Vietnam, Bangladesh, and Turkey (
13,
32,
33).
A study, done in 2011, showed that adsorbent characterization of natural zeolites could be affected by parameters, such as their surface morphologies, chemical composition, physical properties, and specific surface areas (
32). In another study in 2002, the researchers used granular slag columns for lead removal. It was concluded that the apparent mechanisms of lead removal by this column were sorption (ion exchange and adsorption) on the slag surface and precipitation (
34).