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<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>Ling Du</dc:contributor>
  <dc:contributor>Isis P Scott</dc:contributor>
  <dc:contributor>W. Dean Hively</dc:contributor>
  <dc:contributor>Zachary P. Simpson</dc:contributor>
  <dc:contributor>Zacharias J. Smith</dc:contributor>
  <dc:contributor>Cathleen J. Hapeman</dc:contributor>
  <dc:contributor>Martin C. Rabenhorst</dc:contributor>
  <dc:contributor>Raymond R. Weil</dc:contributor>
  <dc:contributor>Greg W. McCarty</dc:contributor>
  <dc:creator>Maryam Foroughi</dc:creator>
  <dc:date>2026</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Phosphorus (P) management remains a challenge in agricultural watersheds. The Choptank River Conservation Effects Assessment Project watershed, located in Maryland and Delaware and draining to the Chesapeake Bay, contains legacy soil P from historical dairy and poultry manure applications. These practices elevated soil P beyond crop needs, contributing to persistent P export to aquatic ecosystems. We assessed spatial P distribution and analyzed GIS (Geographic Information Systems)-derived landscape features driving legacy P movement on a farm (47&amp;nbsp;ha). We hypothesized that P accumulates in drained lowlands and depressional areas due to gravity-driven processes that accelerate P-enriched water to receiving waters via overland flow. In collaboration with the US Department of Agriculture Legacy P project, we collected 105 soil samples (0- to 5-cm and 5- to 15-cm depths) and 14 ditch sediment samples across five topographic openness classes from a farm with&amp;nbsp;&amp;gt;100 years of dairy manure application. Average Mehlich-III P concentrations were 218 and 179&amp;nbsp;mg kg&lt;/span&gt;&lt;sup&gt;−1&lt;/sup&gt;&lt;span&gt;&amp;nbsp;at 0- to 5-cm and 5- to 15-cm depths, respectively, with legacy areas defined by P content&amp;nbsp;&amp;gt;&amp;nbsp;100&amp;nbsp;mg kg&lt;/span&gt;&lt;sup&gt;−1&lt;/sup&gt;&lt;span&gt;. Soil P and clay particle size were positively correlated (&lt;/span&gt;&lt;i&gt;r&lt;/i&gt;&lt;span&gt;&amp;nbsp;=&amp;nbsp;0.42,&amp;nbsp;&lt;/span&gt;&lt;i&gt;p&lt;/i&gt;&lt;span&gt;&amp;nbsp;&amp;lt;&amp;nbsp;0.05), increased as landscape openness decreased, and were negatively correlated with topographic openness (ranging from −0.2 to −0.4,&amp;nbsp;&lt;/span&gt;&lt;i&gt;p&lt;/i&gt;&lt;span&gt;&amp;nbsp;&amp;lt;&amp;nbsp;0.05), indicating accumulation of P and clay in low-lying areas. These patterns suggest that historical field-level managements have primarily shaped P distribution, while hydrologic and landscape properties further influence its redistribution via transport pathways and drainage. These findings support the development of landscape models to map critical source areas in low-relief watersheds and guide targeted mitigation in high-risk P export zones.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1002/jeq2.70101</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America</dc:publisher>
  <dc:title>Assessing the topographic distribution of legacy soil phosphorus in agricultural fields of the Delmarva Peninsula, Mid-Atlantic Coastal Plain, USA</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>