Soil respiration and plant growth across a chronosequence of tallgrass prairie reconstructions

dc.contributor.advisor Heidi Asbjornsen
dc.contributor.author Maher, Ryan
dc.contributor.department Natural Resource Ecology and Management
dc.date 2018-08-23T04:37:48.000
dc.date.accessioned 2020-06-30T07:41:26Z
dc.date.available 2020-06-30T07:41:26Z
dc.date.copyright Mon Jan 01 00:00:00 UTC 2007
dc.date.issued 2007-01-01
dc.description.abstract <p>An understanding of changes in soil respiration (Rs) and plant growth in tallgrass prairies planted into formerly cultivated land is critical if we are to predict the effects of grassland reconstructions on belowground carbon cycling. In addition, predicting changes in the ecosystem carbon balance in grassland reconstructions will require identifying the climatic and biological controls on Rs across a landscape of cultivated and reconstructed grassland ecosystems. This study used a 12 yr chronosequence of tallgrass prairie reconstructions in central Iowa, including a no-till soybean field (age 0), to quantify the relationship between tallgrass prairie age, R s, root biomass, root ingrowth, and aboveground production. We also assessed the strength and interaction of soil temperature and soil moisture in predictions of Rs across the chronosequence. Linear regressions showed a significant increase in standing root biomass carbon (R2 = 0.89) and growing season Rs (R2= 0.83) with prairie reconstruction age while changes in aboveground production and root ingrowth were less predictable. Growing season (gs) Rs represented the largest carbon flux among prairie ages, ranging from 624 g C m-2 gs -1 in the soybean cropping system to 939 g C m-2 gs -1 in the oldest reconstruction (age 12), and was positively correlated with changes in root biomass. Among all tallgrass prairie reconstructions there was a strong, positive relationship between soil temperature and R s (R2 = 0.80 to R2 = 0.91) while the effect of soil moisture was greatest for the youngest prairie (age 4). Soil temperature was less correlated with Rs in the no-till soybean field (R 2 = 0.40) and the inclusion of soil moisture added limited additional predictive power (R2 = 0.48). Our findings indicate that an increase in cumulative Rs with prairie reconstruction age was related to the interaction of soil temperature and the accumulation of root biomass with young grassland development.</p>
dc.format.mimetype application/pdf
dc.identifier archive/lib.dr.iastate.edu/rtd/15048/
dc.identifier.articleid 16047
dc.identifier.contextkey 7013806
dc.identifier.doi https://doi.org/10.31274/rtd-180813-7046
dc.identifier.s3bucket isulib-bepress-aws-west
dc.identifier.submissionpath rtd/15048
dc.identifier.uri https://dr.lib.iastate.edu/handle/20.500.12876/68640
dc.language.iso en
dc.source.bitstream archive/lib.dr.iastate.edu/rtd/15048/1446047.PDF|||Fri Jan 14 20:34:58 UTC 2022
dc.subject.disciplines Agriculture
dc.subject.disciplines Agronomy and Crop Sciences
dc.subject.disciplines Ecology and Evolutionary Biology
dc.subject.disciplines Natural Resources Management and Policy
dc.subject.disciplines Other Animal Sciences
dc.subject.disciplines Other Plant Sciences
dc.subject.disciplines Soil Science
dc.subject.disciplines Terrestrial and Aquatic Ecology
dc.subject.keywords Natural resource ecology and management;Sustainable agriculture
dc.title Soil respiration and plant growth across a chronosequence of tallgrass prairie reconstructions
dc.type article
dc.type.genre thesis
dspace.entity.type Publication
relation.isOrgUnitOfPublication e87b7b9d-30ea-4978-9fb9-def61b4010ae
thesis.degree.discipline Sustainable Agriculture
thesis.degree.level thesis
thesis.degree.name Master of Science
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