PMID-sentid	Pub_year	Sent_text		comp_official_name	comp_offsetprotein_name	organism	prot_offset
33774247-6	2021	The arsenic and trace metals released via oxidation of the sulfide phases (particularly Fe sulfides) were almost entirely sequestered by the Fe(III) (oxyhydr)oxides, but acidification during the oxidation stage of the incubation resulted in the pH-dependent release of the As and trace metals (Co, Cu, Ni) (especially in the Fe-rich/organic-low soil).	Arsenic	4-11	general transcription factor IIE subunit 1	Homo sapiens	141-148	
35217035-5	2022	It was concluded that two selected Pseudomonas strains have NAFO functionality by addition of iron as iron reduction-oxidation pair in the arid soil, further potentially fixing NH4+ while As(III) can be effectively remediated through the FeOB participation in forms of adsorption and co-precipitation of Fe(OH)3 through an oxidation of Fe(II) process.	Arsenic	188-190	general transcription factor IIE subunit 1	Homo sapiens	304-311	
34388870-7	2022	This review collates knowledge regarding the fate of As in multicomponent As-DOM-Fe systems, including ternary complexes involving both Fe and DOM.	Arsenic	53-55	general transcription factor IIE subunit 1	Homo sapiens	81-83	
34388870-7	2022	This review collates knowledge regarding the fate of As in multicomponent As-DOM-Fe systems, including ternary complexes involving both Fe and DOM.	Arsenic	53-55	general transcription factor IIE subunit 1	Homo sapiens	136-138	
34388870-8	2022	Additionally, the release mechanisms of As from sediments into groundwater in the presence of both Fe and DOM have been discussed.	Arsenic	40-42	general transcription factor IIE subunit 1	Homo sapiens	99-101	
34271453-4	2021	Although the oxidation of Fe2+ and As(III) during oxic storage was considerably faster, the As/Fe removal ratio was higher during anoxic storage (61-80+-5 microgAs/mgFe) compared to the oxic storage (45+-5 microgAs/mgFe).	Arsenic	92-94	general transcription factor IIE subunit 1	Homo sapiens	95-97	
33034807-1	2021	Biochar derived from food waste was modified with Fe to enhance its adsorption capacity for As(III), which is the most toxic form of As.	Arsenic	92-94	general transcription factor IIE subunit 1	Homo sapiens	50-52	
33071297-12	2020	Arsenic release during arsenopyrite oxidation resulted in both downward translocation and As(V) attenuation by stable Fe(III)(oxyhydr)oxide and Fe(III) (hydroxy)sulfate minerals over time, highlighting the need for sampling at multiple depths and time points for accurate interpretation of arsenic speciation, lability, and translocation in weathering profiles.	Arsenic	0-7	general transcription factor IIE subunit 1	Homo sapiens	118-125	
33071297-12	2020	Arsenic release during arsenopyrite oxidation resulted in both downward translocation and As(V) attenuation by stable Fe(III)(oxyhydr)oxide and Fe(III) (hydroxy)sulfate minerals over time, highlighting the need for sampling at multiple depths and time points for accurate interpretation of arsenic speciation, lability, and translocation in weathering profiles.	Arsenic	0-7	general transcription factor IIE subunit 1	Homo sapiens	144-151	
33044731-7	2021	Arsenic (As) is probably derived from the dissolution of Fe oxide and hydroxide (i.e., Fe(OH)3, goethite, maghemite, and magnetite).	Arsenic	0-7	general transcription factor IIE subunit 1	Homo sapiens	87-94	
33044731-7	2021	Arsenic (As) is probably derived from the dissolution of Fe oxide and hydroxide (i.e., Fe(OH)3, goethite, maghemite, and magnetite).	Arsenic	9-11	general transcription factor IIE subunit 1	Homo sapiens	87-94