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- Genre: Masters Thesis
- Member of: ASU Electronic Theses and Dissertations
- Member of: Theses and Dissertations
Description
Dissolved organic matter (DOM) is an important part of aquatic foodwebs because it contains carbon, nitrogen, and other elements required by heterotrophic organisms. It has many sources that determine its molecular composition, nutrient content, and biological lability and in turn, influence whether it is retained and processed in the stream reach or exported downstream. I examined the composition of DOM from vascular wetland plants, filamentous algae, and riparian tree leaf litter in Sonoran Desert streams and its decomposition by stream microbes. I used a combination of field observations, in-situ experiments, and a manipulative laboratory incubation to test (1) how dominant primary producers influence DOM chemical composition and ecosystem metabolism at the reach scale and (2) how DOM composition and nitrogen (N) content control microbial decomposition and stream uptake of DOM. I found that differences in streamwater DOM composition between two distinct reaches of Sycamore Creek did not affect in-situ stream respiration and gross primary production rates. Stream sediment microbial respiration rates did not differ significantly when incubated in the laboratory with DOM from wetland plants, algae, and leaf litter, thus all sources were similarly labile. However, whole-stream uptake of DOM increased from leaf to algal to wetland plant leachate. Desert streams have the potential to process DOM from leaf, wetland, and algal sources, though algal and wetland DOM, due to their more labile composition, can be more readily retained and mineralized.
ContributorsKemmitt, Kathrine (Author) / Grimm, Nancy (Thesis advisor) / Hartnett, Hilairy (Committee member) / Throop, Heather (Committee member) / Arizona State University (Publisher)
Created2018
Description
Two challenges in the implementation of enzyme induced carbonate precipitation(EICP) are the cost of enzyme and the variability of the enzyme. Urease enzyme costs
can be lowered drastically with the use of crude extract from plant materials, but
experience has shown variability in the source of the crude urease enzyme, the crude
urease enzyme extraction methods, and the concentration of the EICP solution can cause
significant variability in the efficacy of the EICP solution.
This thesis examines the variability in the efficacy of crude enzyme derived from
jack beans (Canavalia ensiformis) and sword beans (Canavalia gladiata), two of the
most commonly used sources of urease enzyme for EICP. The sources of variability
investigated herein include the crude extraction method (including the effect of the bean
husks on extraction) and different chemical constituent concentrations. These effects
were assessed using enzyme activity measurements and precipitation efficiency tests. The
activity tests were performed via spectrophotometry using Nessler's reagent. The
precipitation tests looked at the influence of chemical constituent concentrations of 0.67
M calcium chloride and 1 M urea with non-fat dry milk in the EICP solutions and a
higher concentration solution with chemical constituent concentrations of 2 M for both
calcium chloride and urea with non-fat dry milk. The high concentration solution was
selected based on preliminary testing results to maximize carbonate precipitation in one
cycle of treatment. Significant sources of a decline in activity (and increase in variation)
of the crude urease enzyme were found in extraction from sword beans with husks, high
chemical constituent concentrations, and juicing instead of cheesecloth filtration.
This thesis also examines the accuracy of commonly used correlation factors for
converting electrical conductivity to urease enzyme activity. Crude jack bean and sword
bean urease enzyme activity measurement via electrical conductivity was found to have a
correlation coefficient that differed from the previously reported correlation when
compared to activity measured via the more accurate spectrophotometry using Nessler’s
reagent measurements.
ContributorsPearson, Rayanna (Author) / Kavazanjian, Edward (Thesis advisor) / Khodadadi Tirkolaei, Hamed (Committee member) / Salifu, Emmanuel (Committee member) / Arizona State University (Publisher)
Created2022
Description
Soil organic carbon (SOC) is a critical component of the global carbon (C) cycle, accounting for more C than the biotic and atmospheric pools combined. Microbes play an important role in soil C cycling, with abiotic conditions such as soil moisture and temperature governing microbial activity and subsequent soil C processes. Predictions for future climate include warmer temperatures and altered precipitation regimes, suggesting impacts on future soil C cycling. However, it is uncertain how soil microbial communities and subsequent soil organic carbon pools will respond to these changes, particularly in dryland ecosystems. A knowledge gap exists in soil microbial community responses to short- versus long-term precipitation alteration in dryland systems. Assessing soil C cycle processes and microbial community responses under current and altered precipitation patterns will aid in understanding how C pools and cycling might be altered by climate change. This study investigates how soil microbial communities are influenced by established climate regimes and extreme changes in short-term precipitation patterns across a 1000 m elevation gradient in northern Arizona, where precipitation increases with elevation. Precipitation was manipulated (50% addition and 50% exclusion of ambient rainfall) for two summer rainy seasons at five sites across the elevation gradient. In situ and ex situ soil CO2 flux, microbial biomass C, extracellular enzyme activity, and SOC were measured in precipitation treatments in all sites. Soil CO2 flux, microbial biomass C, extracellular enzyme activity, and SOC were highest at the three highest elevation sites compared to the two lowest elevation sites. Within sites, precipitation treatments did not change microbial biomass C, extracellular enzyme activity, and SOC. Soil CO2 flux was greater under precipitation addition treatments than exclusion treatments at both the highest elevation site and second lowest elevation site. Ex situ respiration differed among the precipitation treatments only at the lowest elevation site, where respiration was enhanced in the precipitation addition plots. These results suggest soil C cycling will respond to long-term changes in precipitation, but pools and fluxes of carbon will likely show site-specific sensitivities to short-term precipitation patterns that are also expected with climate change.
ContributorsMonus, Brittney (Author) / Throop, Heather L (Thesis advisor) / Ball, Becky A (Committee member) / Hultine, Kevin R (Committee member) / Munson, Seth M (Committee member) / Arizona State University (Publisher)
Created2019