| Natural zeolites |
200 μg L−1 of water treated with HCl |
— |
— |
75% |
133
|
| Chabazite-phillipsite, clinoptilolite, and volcanic glass |
Deionized water was used to prepare the solution spiked with 100 μg L−1
|
— |
— |
40–78% |
134
|
| Clinoptilolite |
Zeolites were washed with 2 M HCl and the pH was adjusted at 5, water solution contained 500 μg per L As |
98% |
98% |
— |
135
|
| Cancrinite |
Loading cancrinite alumina to water at pH range of 4.9–7.0 |
— |
— |
34.5 mg g−1
|
136
|
| Natural zeolite |
Aqueous solution contained 5 mM As, zeolite loaded with lanthanum at pH range 2–8 |
— |
95% |
— |
130
|
| Zeolite P |
Exchange of zeolite sodium with cerium(iii) at pH 3–10 |
|
23.42 mg g−1
|
|
137
|
| Raw zeolite |
Iron-coated zeolite at a pH range of 3.0–10.0 |
|
0.68 mg g−1
|
|
138
|
| Zeolite |
Coating zeolite with magnetic nanoparticle (γ-Fe2O3) at a pH value of 2.5 |
|
44 mg g−1
|
|
139
|
| Clinoptilolite-Ca |
Modification of clinoptilolite-Ca zeolite with MnO2
|
|
2.5 μg g−1
|
|
131
|
| Zeolite |
Groundwater spiked with 2000 μg L−1, magnetic nanoscale Fe–Mn binary oxides loaded zeolite at pH 7 |
|
99% |
|
140
|
| Clinoptilolite |
Zeolite (clinoptilolite) supported mono- (Fe or Al) and bi-metallic (Fesingle bondAl) oxides at pH 5 |
|
3.86 mg g−1
|
|
141
|