<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Autry, A. R.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Sulfur fractions and retention mechanisms in forest soils.</style></title><secondary-title><style face="normal" font="default" size="100%">Canadian Journal of Forest Research 20: 337-342</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">CWT</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">1990</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://cwt33.ecology.uga.edu/publications/1196.pdf</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Organic S was found to constitute over 78% of total S in the uppermost mineral(0-20 cm; A,E) horizons.  Several forests of varying elevation, vegetation, location, and soil type were considered. Organic S exceeded 65% of total S inall but one site for both intermediate (20-40 cm; primarily A/B) and deeper (40+cm; B,C) horizons.  In almost all cases, the adsorbed sulfate anion constituted substantially less of the total S than did organic S. Carbon-bonded S was themost prevalent form of organic S for most sites at all depths.  Adsorbed estersulfate, recovered by extraction with basic phosphate, generally constituted a substantial portion of the adsorbed S pool for both O1 and O2 components of the forest floor and for the uppermost mineral horizon of most sites.  This trend did not hold true with increasing depth. Because organic S was the dominant form of S, irrespective of horizon, the data suggest that organosulfur formation, not sulfate adsorption, may represent the primary mechanism for S retention in forest soil.</style></abstract><accession-num><style face="normal" font="default" size="100%">LTER.1990-80847</style></accession-num></record></records></xml>