{"id":{"repo_id":"central-wash","oai_identifier":"oai:digitalcommons.cwu.edu:etd-2014"},"canonical_url":"https://search.dev.ndltd.org/etd/central-wash/oai:digitalcommons.cwu.edu:etd-2014","repository":{"repo_id":"central-wash","name":"Central Washington University","base_url":"https://digitalcommons.cwu.edu/do/oai/"},"display":{"title":"Stream water and soil water chemistry after the Table Mountain wildfire, Washington, USA","abstract":"Analyses of major and trace elements, major ions, and nutrient concentrations were made to investigate how stream water and soil water chemistry changed over 16 months following the Table Mountain wildfire. Sites with different burn severity were also compared. The fire occurred in 2012 in Kittitas County, north of Ellensburg, Washington. Samples were collected at severely burned, moderately burned, and unburned field sites from within and adjacent to the wildfire perimeter. Total nitrogen concentrations increased in the second year after the fire in both the severely and moderately burned sites. In contrast, total phosphorus was variable at all three sites and did not increase significantly after the fire. Major elements, trace elements, and major ion groups do not show a gradation from severely burned to moderately burned to unburned sites. However, both burned sites had soil waters with lower Ca/Mg ratios in the first year after the fire.","abstract_html":"Analyses of major and trace elements, major ions, and nutrient concentrations were made to investigate how stream water and soil water chemistry changed over 16 months following the Table Mountain wildfire. Sites with different burn severity were also compared. The fire occurred in 2012 in Kittitas County, north of Ellensburg, Washington. Samples were collected at severely burned, moderately burned, and unburned field sites from within and adjacent to the wildfire perimeter. Total nitrogen concentrations increased in the second year after the fire in both the severely and moderately burned sites. In contrast, total phosphorus was variable at all three sites and did not increase significantly after the fire. Major elements, trace elements, and major ion groups do not show a gradation from severely burned to moderately burned to unburned sites. However, both burned sites had soil waters with lower Ca/Mg ratios in the first year after the fire.","abstract_has_math":false,"creators":["Roccanova, Vincent J."],"institution":null,"degree_name":"Master of Science (MS)","degree_level":null,"degree_discipline":"Geological Sciences","degree_department":null,"school":null,"contributors":["Carey Gazis","Lisa Ely","Clay Arango"],"advisors":[],"committee_chairs":[],"committee_members":[],"year":2018,"date_issued":"2018-01-01T08:00:00Z","date_published":"2018-01-01T08:00:00Z","updated_at":"2026-07-24T01:37:23Z","subjects":["geochemistry","wildfire","nitrogen","phosphorus","anions","cations","Earth Sciences","Geology","Physical Sciences and Mathematics"],"languages":["English"],"rights":[],"rights_urls":[],"identifier_entries":[]},"links":{"outbound_url":"https://digitalcommons.cwu.edu/etd/1009","outbound_label":"Repository record","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:contributor","label":"Contributor","values":["Carey Gazis","Lisa Ely","Clay Arango"]},{"key":"dc:creator","label":"Author","values":["Roccanova, Vincent J."]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date.available","label":"Dc Date Available","values":["2018-09-10T07:00:00Z"]},{"key":"dc:type","label":"Dc Type","values":["Text"]},{"key":"thesis:degree_discipline","label":"Discipline","values":["Geological Sciences"]},{"key":"thesis:degree_name","label":"Degree Name","values":["Master of Science (MS)"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["geochemistry","wildfire","nitrogen","phosphorus","anions","cations","Earth Sciences","Geology","Physical Sciences and Mathematics"]}]},{"id":"language_rights","label":"Language and Rights","entries":[{"key":"dc:language","label":"Dc Language","values":["English"]}]},{"id":"identifiers","label":"Identifiers","entries":[{"key":"dc:identifier","label":"Identifier","values":["https://digitalcommons.cwu.edu/etd/1009"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description.abstract","label":"Abstract","values":["Analyses of major and trace elements, major ions, and nutrient concentrations were made to investigate how stream water and soil water chemistry changed over 16 months following the Table Mountain wildfire. Sites with different burn severity were also compared. The fire occurred in 2012 in Kittitas County, north of Ellensburg, Washington. Samples were collected at severely burned, moderately burned, and unburned field sites from within and adjacent to the wildfire perimeter. Total nitrogen concentrations increased in the second year after the fire in both the severely and moderately burned sites. In contrast, total phosphorus was variable at all three sites and did not increase significantly after the fire. Major elements, trace elements, and major ion groups do not show a gradation from severely burned to moderately burned to unburned sites. However, both burned sites had soil waters with lower Ca/Mg ratios in the first year after the fire."]},{"key":"dc:title","label":"Title","values":["Stream water and soil water chemistry after the Table Mountain wildfire, Washington, USA"]}]}],"canonical_facts":{"dc:contributor":["Carey Gazis","Lisa Ely","Clay Arango"],"dc:creator":["Roccanova, Vincent J."],"dc:date.available":["2018-09-10T07:00:00Z"],"dc:description.abstract":["Analyses of major and trace elements, major ions, and nutrient concentrations were made to investigate how stream water and soil water chemistry changed over 16 months following the Table Mountain wildfire. Sites with different burn severity were also compared. The fire occurred in 2012 in Kittitas County, north of Ellensburg, Washington. Samples were collected at severely burned, moderately burned, and unburned field sites from within and adjacent to the wildfire perimeter. Total nitrogen concentrations increased in the second year after the fire in both the severely and moderately burned sites. In contrast, total phosphorus was variable at all three sites and did not increase significantly after the fire. Major elements, trace elements, and major ion groups do not show a gradation from severely burned to moderately burned to unburned sites. However, both burned sites had soil waters with lower Ca/Mg ratios in the first year after the fire."],"dc:identifier":["https://digitalcommons.cwu.edu/etd/1009"],"dc:language":["English"],"dc:subject":["geochemistry","wildfire","nitrogen","phosphorus","anions","cations","Earth Sciences","Geology","Physical Sciences and Mathematics"],"dc:title":["Stream water and soil water chemistry after the Table Mountain wildfire, Washington, USA"],"dc:type":["Text"],"thesis:degree_discipline":["Geological Sciences"],"thesis:degree_name":["Master of Science (MS)"]},"updated_at":"2026-07-24T01:37:23Z"}