{"id":{"repo_id":"central-wash","oai_identifier":"oai:digitalcommons.cwu.edu:etd-2287"},"canonical_url":"https://search.dev.ndltd.org/etd/central-wash/oai:digitalcommons.cwu.edu:etd-2287","repository":{"repo_id":"central-wash","name":"Central Washington University","base_url":"https://digitalcommons.cwu.edu/do/oai/"},"display":{"title":"Seasonal soil carbon fluxes in transitioning agricultural soils in Central Washington State: Relations to land-use, environmental factors and soil carbon-nitrogen characteristics","abstract":"Changing agricultural land-use practices to increase soil carbon sequestration contributes to climate change mitigation and improved food security by moving CO<sub>2</sub> from the atmosphere into soil as soil organic carbon (SOC). In 2016, a farm in Thorp, Washington, Spoon Full Farm, began converting land historically farmed using conventional methods of tillage and synthetic fertilizers to conservation farming methods with direct seeding and organic soil amendments with a goal of sequestering carbon in the soil. This project evaluates relationships of soil CO<sub>2</sub> respiration and net ecological exchange (NEE) with land-use types, seasonal environmental factors (air temperature, relative humidity, soil temperature and soil moisture) and soil carbon and nitrogen properties (SOC, SON, δ<sup>13</sup>C, and δ<sup>15</sup>N) on that farm in order to inform land management decisions affecting soil carbon sequestration. Three farm land-use areas studied were: 1) no-till vegetable garden with regular organic matter amendments; 2) no-till hay fields; and 3) historically unfarmed areas. Soil CO<sub>2</sub> fluxes were measured on these three land-use areas in spring after snowmelt; summer, when garden and hay fields are irrigated and unfarmed areas are dry; and fall when soil and air temperatures are lower and moisture has returned to soils. Continuous soil CO<sub>2</sub> flux measurements of garden soils indicate primary environmental factors influencing soil CO<sub>2</sub> flux during summer are air and soil temperature, and during fall are soil temperature and moisture. Garden beds have positive NEE during summer and spring days indicating net CO<sub>2</sub> losses from soil. Garden bed respiration is likely dominated by microbial decomposition of compost. Summer period soil CO<sub>2 </sub>flux correlates with SOC for all land-use types individually, while vegetable garden SOC and SON correlate with CO<sub>2</sub> flux annually. This suggests SOC influences summer soil CO<sub>2</sub> flux regardless of land-use type, while annual CO<sub>2</sub> flux from composted garden soil depends on overall organic content from compost inputs. Hay field CO<sub>2</sub> flux during summer shows strong correlation with elevated surface SOC within the crop root zone. <strong></strong>","abstract_html":"Changing agricultural land-use practices to increase soil carbon sequestration contributes to climate change mitigation and improved food security by moving CO&lt;sub&gt;2&lt;/sub&gt; from the atmosphere into soil as soil organic carbon (SOC). In 2016, a farm in Thorp, Washington, Spoon Full Farm, began converting land historically farmed using conventional methods of tillage and synthetic fertilizers to conservation farming methods with direct seeding and organic soil amendments with a goal of sequestering carbon in the soil. This project evaluates relationships of soil CO&lt;sub&gt;2&lt;/sub&gt; respiration and net ecological exchange (NEE) with land-use types, seasonal environmental factors (air temperature, relative humidity, soil temperature and soil moisture) and soil carbon and nitrogen properties (SOC, SON, δ&lt;sup&gt;13&lt;/sup&gt;C, and δ&lt;sup&gt;15&lt;/sup&gt;N) on that farm in order to inform land management decisions affecting soil carbon sequestration. Three farm land-use areas studied were: 1) no-till vegetable garden with regular organic matter amendments; 2) no-till hay fields; and 3) historically unfarmed areas. Soil CO&lt;sub&gt;2&lt;/sub&gt; fluxes were measured on these three land-use areas in spring after snowmelt; summer, when garden and hay fields are irrigated and unfarmed areas are dry; and fall when soil and air temperatures are lower and moisture has returned to soils. Continuous soil CO&lt;sub&gt;2&lt;/sub&gt; flux measurements of garden soils indicate primary environmental factors influencing soil CO&lt;sub&gt;2&lt;/sub&gt; flux during summer are air and soil temperature, and during fall are soil temperature and moisture. Garden beds have positive NEE during summer and spring days indicating net CO&lt;sub&gt;2&lt;/sub&gt; losses from soil. Garden bed respiration is likely dominated by microbial decomposition of compost. Summer period soil CO&lt;sub&gt;2 &lt;/sub&gt;flux correlates with SOC for all land-use types individually, while vegetable garden SOC and SON correlate with CO&lt;sub&gt;2&lt;/sub&gt; flux annually. This suggests SOC influences summer soil CO&lt;sub&gt;2&lt;/sub&gt; flux regardless of land-use type, while annual CO&lt;sub&gt;2&lt;/sub&gt; flux from composted garden soil depends on overall organic content from compost inputs. Hay field CO&lt;sub&gt;2&lt;/sub&gt; flux during summer shows strong correlation with elevated surface SOC within the crop root zone. &lt;strong&gt;&lt;/strong&gt;","abstract_has_math":false,"creators":["Kautzman, Brandon"],"institution":null,"degree_name":"Master of Science (MS)","degree_level":null,"degree_discipline":"Geological Sciences","degree_department":null,"school":null,"contributors":["Carey Gazis","Susan Kaspari","Karl D. Lillquist"],"advisors":[],"committee_chairs":[],"committee_members":[],"year":2019,"date_issued":"2019-01-01T08:00:00Z","date_published":"2019-01-01T08:00:00Z","updated_at":"2026-07-24T01:37:42Z","subjects":["Acadmemic Theses","Conservation","agriculture","soil","carbon","cycling","Biogeochemistry","Environmental Chemistry","Geochemistry","Natural Resources and Conservation","Soil Science","Sustainability"],"languages":["English"],"rights":[],"rights_urls":[],"identifier_entries":[]},"links":{"outbound_url":"https://digitalcommons.cwu.edu/etd/1266","outbound_label":"Repository record","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:contributor","label":"Contributor","values":["Carey Gazis","Susan Kaspari","Karl D. Lillquist"]},{"key":"dc:creator","label":"Author","values":["Kautzman, Brandon"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date.available","label":"Dc Date Available","values":["2019-08-19T07:00:00Z"]},{"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":["Acadmemic Theses","Conservation","agriculture","soil","carbon","cycling","Biogeochemistry","Environmental Chemistry","Geochemistry","Natural Resources and Conservation","Soil Science","Sustainability"]}]},{"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/1266"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description.abstract","label":"Abstract","values":["Changing agricultural land-use practices to increase soil carbon sequestration contributes to climate change mitigation and improved food security by moving CO<sub>2</sub> from the atmosphere into soil as soil organic carbon (SOC). In 2016, a farm in Thorp, Washington, Spoon Full Farm, began converting land historically farmed using conventional methods of tillage and synthetic fertilizers to conservation farming methods with direct seeding and organic soil amendments with a goal of sequestering carbon in the soil. This project evaluates relationships of soil CO<sub>2</sub> respiration and net ecological exchange (NEE) with land-use types, seasonal environmental factors (air temperature, relative humidity, soil temperature and soil moisture) and soil carbon and nitrogen properties (SOC, SON, δ<sup>13</sup>C, and δ<sup>15</sup>N) on that farm in order to inform land management decisions affecting soil carbon sequestration. Three farm land-use areas studied were: 1) no-till vegetable garden with regular organic matter amendments; 2) no-till hay fields; and 3) historically unfarmed areas. Soil CO<sub>2</sub> fluxes were measured on these three land-use areas in spring after snowmelt; summer, when garden and hay fields are irrigated and unfarmed areas are dry; and fall when soil and air temperatures are lower and moisture has returned to soils. Continuous soil CO<sub>2</sub> flux measurements of garden soils indicate primary environmental factors influencing soil CO<sub>2</sub> flux during summer are air and soil temperature, and during fall are soil temperature and moisture. Garden beds have positive NEE during summer and spring days indicating net CO<sub>2</sub> losses from soil. Garden bed respiration is likely dominated by microbial decomposition of compost. Summer period soil CO<sub>2 </sub>flux correlates with SOC for all land-use types individually, while vegetable garden SOC and SON correlate with CO<sub>2</sub> flux annually. This suggests SOC influences summer soil CO<sub>2</sub> flux regardless of land-use type, while annual CO<sub>2</sub> flux from composted garden soil depends on overall organic content from compost inputs. Hay field CO<sub>2</sub> flux during summer shows strong correlation with elevated surface SOC within the crop root zone. <strong></strong>"]},{"key":"dc:title","label":"Title","values":["Seasonal soil carbon fluxes in transitioning agricultural soils in Central Washington State: Relations to land-use, environmental factors and soil carbon-nitrogen characteristics"]}]}],"canonical_facts":{"dc:contributor":["Carey Gazis","Susan Kaspari","Karl D. Lillquist"],"dc:creator":["Kautzman, Brandon"],"dc:date.available":["2019-08-19T07:00:00Z"],"dc:description.abstract":["Changing agricultural land-use practices to increase soil carbon sequestration contributes to climate change mitigation and improved food security by moving CO<sub>2</sub> from the atmosphere into soil as soil organic carbon (SOC). In 2016, a farm in Thorp, Washington, Spoon Full Farm, began converting land historically farmed using conventional methods of tillage and synthetic fertilizers to conservation farming methods with direct seeding and organic soil amendments with a goal of sequestering carbon in the soil. This project evaluates relationships of soil CO<sub>2</sub> respiration and net ecological exchange (NEE) with land-use types, seasonal environmental factors (air temperature, relative humidity, soil temperature and soil moisture) and soil carbon and nitrogen properties (SOC, SON, δ<sup>13</sup>C, and δ<sup>15</sup>N) on that farm in order to inform land management decisions affecting soil carbon sequestration. Three farm land-use areas studied were: 1) no-till vegetable garden with regular organic matter amendments; 2) no-till hay fields; and 3) historically unfarmed areas. Soil CO<sub>2</sub> fluxes were measured on these three land-use areas in spring after snowmelt; summer, when garden and hay fields are irrigated and unfarmed areas are dry; and fall when soil and air temperatures are lower and moisture has returned to soils. Continuous soil CO<sub>2</sub> flux measurements of garden soils indicate primary environmental factors influencing soil CO<sub>2</sub> flux during summer are air and soil temperature, and during fall are soil temperature and moisture. Garden beds have positive NEE during summer and spring days indicating net CO<sub>2</sub> losses from soil. Garden bed respiration is likely dominated by microbial decomposition of compost. Summer period soil CO<sub>2 </sub>flux correlates with SOC for all land-use types individually, while vegetable garden SOC and SON correlate with CO<sub>2</sub> flux annually. This suggests SOC influences summer soil CO<sub>2</sub> flux regardless of land-use type, while annual CO<sub>2</sub> flux from composted garden soil depends on overall organic content from compost inputs. Hay field CO<sub>2</sub> flux during summer shows strong correlation with elevated surface SOC within the crop root zone. <strong></strong>"],"dc:identifier":["https://digitalcommons.cwu.edu/etd/1266"],"dc:language":["English"],"dc:subject":["Acadmemic Theses","Conservation","agriculture","soil","carbon","cycling","Biogeochemistry","Environmental Chemistry","Geochemistry","Natural Resources and Conservation","Soil Science","Sustainability"],"dc:title":["Seasonal soil carbon fluxes in transitioning agricultural soils in Central Washington State: Relations to land-use, environmental factors and soil carbon-nitrogen characteristics"],"dc:type":["Text"],"thesis:degree_discipline":["Geological Sciences"],"thesis:degree_name":["Master of Science (MS)"]},"updated_at":"2026-07-24T01:37:42Z"}