Publicación:
Bioadsorption of silver ions by calcareous chitin, chitin and chitosan; Bioadsorción de iones de plata por quitina calcárea, quitina y quitosano

dc.contributor.authorJáuregui-Nongrados, John
dc.contributor.authorAlvarado, Angel T.
dc.contributor.authorMucha, Miguel
dc.contributor.authorMuñoz-Jauregui, Ana María
dc.contributor.authorChávez-Orellana, Haydee
dc.contributor.authorMolina-Cabrera, Aura
dc.contributor.authorCuba-García, Pompeyo Arquimedes
dc.contributor.authorMelgar-Merino, Elizabeth Julia
dc.contributor.authorBolarte-Arteaga, Mario Antonio
dc.contributor.authorMori-Castro, Jaime A.
dc.date.accessioned2025-09-05T16:35:14Z
dc.description.abstractContext: Calcareous chitin, chitin, chitosan, and their modifications are used as bioadsorbents of metals and dyes that cause environmental pollution, endocrine disruption, and human diseases. Aims: To evaluate the selective bioadsorption of silver ions (Ag+) by calcareous chitin, chitin, and chitosan. Methods: Experimental and prospective study. The presence of functional groups of the bioadsorbents was identified by Fourier-transformed infrared spectroscopy (FT-IR), 1H-NMR spectroscopy and scanning electron microscopy (SEM). The Langmuir, Freundlich, and Elovich models were applied to describe the adsorption capacity of bioadsorbents according to granule size (20-40, 40-60, 60-80 meshes) and temperature (10, 20, and 30°C). Results: The FT-IR spectrum of calcareous chitin indicates the presence of carbonate (CO3= 1420 cm-1), amide III (1313 cm-1), –OH groups (3441.90 cm-1), and pyranose structure (952.83 cm-1); chitin has –OH groups (3441.90 cm-1), NH (3268 cm-1), amide I (1654 cm-1) and II (1559 cm-1); chitosan has –OH groups (3419.90 cm-1), –NH (3200 cm-1), amide I (1712.18 cm-1), –NH2 (1654.46 cm-1), amide III (1317.11 cm-1) and pyranose structure (1070.12 cm-1 and 1031 cm-1). The Langmuir model indicates greater bioadsorption of Ag+ ions at smaller particle sizes (60-80 = 0.25-0.18 mm) and at a temperature of 20-30°C. Conclusions: The bioadsorption of silver ions (Ag+) by chitosan is greater with respect to calcareous chitin and chitin; the Langmuir model fits for the Ag+ isotherm and suggests that the process is controlled by physisorption. © 2023 Elsevier B.V., All rights reserved.
dc.identifier.doi10.56499/jppres22.1529_11.1.101
dc.identifier.scopus2-s2.0-85149908689
dc.identifier.urihttps://cris.uwiener.edu.pe/handle/001/586
dc.identifier.uuid9fc6c61a-45a0-4aef-9590-6044f9a28a33
dc.language.isoen
dc.publisherAcademic Association of Pharmaceutical Sciences from Antofagasta (ASOCIFA)
dc.relation.citationissue1
dc.relation.citationvolume11
dc.relation.ispartofseriesJournal of Pharmacy and Pharmacognosy Research
dc.relation.issn7194250
dc.rightshttp://purl.org/coar/access_right/c_abf2
dc.titleBioadsorption of silver ions by calcareous chitin, chitin and chitosan; Bioadsorción de iones de plata por quitina calcárea, quitina y quitosano
dc.typehttp://purl.org/coar/resource_type/c_2df8fbb1
dspace.entity.typePublication
oaire.citation.endPage109
oaire.citation.startPage101

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