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The adsorption\/desorption properties of arsenic (\n                    <jats:styled-content style=\"fixed-case\">\n                      As\n                      <jats:sup>V<\/jats:sup>\n                    <\/jats:styled-content>\n                    )\/antimony (\n                    <jats:styled-content style=\"fixed-case\">\n                      Sb\n                      <jats:sup>V<\/jats:sup>\n                    <\/jats:styled-content>\n                    ) oxyanions were tested with two types of soil with a variable content of natural organic matter (\n                    <jats:styled-content style=\"fixed-case\">NOM<\/jats:styled-content>\n                    ). Sample\n                    <jats:styled-content style=\"fixed-case\">JEZ<\/jats:styled-content>\n                    (I) represented a locality near a brown\u2010coal power plant, and therefore formerly exposed to large amounts of atmospheric pollution, while sample\n                    <jats:styled-content style=\"fixed-case\">LIZ<\/jats:styled-content>\n                    (\n                    <jats:styled-content style=\"fixed-case\">II<\/jats:styled-content>\n                    ) originated in an uncontaminated region without anthropogenic impact. Soil samples were investigated from the organic O and mineral B horizons. Different\n                    <jats:styled-content style=\"fixed-case\">As<\/jats:styled-content>\n                    \/\n                    <jats:styled-content style=\"fixed-case\">Sb<\/jats:styled-content>\n                    fixations were indicated by their different adsorption affinity to O and B horizons. Arsenic as\n                    <jats:styled-content style=\"fixed-case\">\n                      As\n                      <jats:sup>V<\/jats:sup>\n                    <\/jats:styled-content>\n                    was strongly adsorbed in B horizons, while antimony as\n                    <jats:styled-content style=\"fixed-case\">\n                      Sb\n                      <jats:sup>V<\/jats:sup>\n                    <\/jats:styled-content>\n                    was predominantly bound in O horizons. The sorption followed the Langmuir model with maximum adsorption capacities of 1.4 \u00d7 10\n                    <jats:sup>\u22122<\/jats:sup>\n                    mmol g\n                    <jats:sup>\u22121<\/jats:sup>\n                    for\n                    <jats:styled-content style=\"fixed-case\">As<\/jats:styled-content>\n                    and 1.0 \u00d7 10\n                    <jats:sup>\u22122<\/jats:sup>\n                    mmol g\n                    <jats:sup>\u22121<\/jats:sup>\n                    for\n                    <jats:styled-content style=\"fixed-case\">Sb<\/jats:styled-content>\n                    adsorptions. The release of\n                    <jats:styled-content style=\"fixed-case\">As<\/jats:styled-content>\n                    and\n                    <jats:styled-content style=\"fixed-case\">Sb<\/jats:styled-content>\n                    to distilled water and 0.1\n                    <jats:sc>m<\/jats:sc>\n                    <jats:styled-content style=\"fixed-case\">KCl<\/jats:styled-content>\n                    illustrated the significantly larger stability of\n                    <jats:styled-content style=\"fixed-case\">As<\/jats:styled-content>\n                    and\n                    <jats:styled-content style=\"fixed-case\">Sb<\/jats:styled-content>\n                    oxyanions in ionic solutions, where available ions prevented the aggregation of organic matter, thus maintaining the balanced distribution of surface charge. Distilled water with a\n                    <jats:styled-content style=\"fixed-case\">pH<\/jats:styled-content>\n                    of about 6 supported a negative surface charge density and enhanced the release of\n                    <jats:styled-content style=\"fixed-case\">As<\/jats:styled-content>\n                    \/\n                    <jats:styled-content style=\"fixed-case\">Sb<\/jats:styled-content>\n                    oxyanions.\n                  <\/jats:p>","DOI":"10.1111\/ejss.12206","type":"journal-article","created":{"date-parts":[[2014,12,23]],"date-time":"2014-12-23T06:21:22Z","timestamp":1419315682000},"page":"74-82","update-policy":"https:\/\/doi.org\/10.1002\/crossmark_policy","source":"Crossref","is-referenced-by-count":63,"title":["Effect of organic matter on arsenic(V) and antimony(V) adsorption in soils"],"prefix":"10.1111","volume":"66","author":[{"given":"B.","family":"Dousova","sequence":"first","affiliation":[{"name":"Institute of Chemical Technology Prague  Technicka 5 166 28 Prague 6 Czech Republic"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"F.","family":"Buzek","sequence":"additional","affiliation":[{"name":"Czech Geological Survey  Geologicka 6 152 00 Prague 5 Czech Republic"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"L.","family":"Herzogova","sequence":"additional","affiliation":[{"name":"Institute of Chemical Technology Prague  Technicka 5 166 28 Prague 6 Czech Republic"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"V.","family":"Machovic","sequence":"additional","affiliation":[{"name":"Institute of Chemical Technology Prague  Technicka 5 166 28 Prague 6 Czech Republic"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"M.","family":"Lhotka","sequence":"additional","affiliation":[{"name":"Institute of Chemical Technology Prague  Technicka 5 166 28 Prague 6 Czech Republic"}],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"311","published-online":{"date-parts":[[2014,12,23]]},"reference":[{"key":"e_1_2_6_2_1","doi-asserted-by":"publisher","DOI":"10.1021\/ja01145a126"},{"key":"e_1_2_6_3_1","volume-title":"Methods of Soil Analysis. 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