<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>D.J. Pinckney</dc:contributor>
  <dc:creator>R.L. Wershaw</dc:creator>
  <dc:date>1973</dc:date>
  <dc:description>&lt;p&gt;Humic acids, the most abundant organic components of&amp;nbsp;natural water systems, are complex mixtures of molecular aggregates of&amp;nbsp;different chemical and physical properties. The first step in the study of&amp;nbsp;such a mixture is the fractionation of the mixture. The most common&amp;nbsp;approach with humic acids is to attempt to obtain a molecular weight&amp;nbsp;fractionation by gel-permeation chromatography. However, since the&amp;nbsp;preponderance of evidence indicates that the components of humic acid&amp;nbsp;do not fulfill the basic criteria of uniform shape and chemical structure&amp;nbsp;necessary for obtaining a molecular fractionation on gel-permeation&amp;nbsp;media, molecular weight distributions in humic acids cannot be&lt;br /&gt;evaluated by this method. A fractionation dependent upon chemical&amp;nbsp;structure can be obtained by the manipulation of elution conditions on&lt;br /&gt;a gel-permeation column. This procedure provides a beginning in the&amp;nbsp;isolation and identification of discrete components of humic acids.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>The fractionation of humic acids from natural water systems</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>