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Description
Quercetin 2,3-dioxygenase from Bacillus subtilis has been identified and characterized as the first known prokaryotic quercetinase. This enzyme catalyzes the cleavage of the O-heteroaromatic ring of the flavonol quercetin to the corresponding depside and carbon monoxide. The first quercetinase was characterized from a species of Aspergillus genus, and was found

Quercetin 2,3-dioxygenase from Bacillus subtilis has been identified and characterized as the first known prokaryotic quercetinase. This enzyme catalyzes the cleavage of the O-heteroaromatic ring of the flavonol quercetin to the corresponding depside and carbon monoxide. The first quercetinase was characterized from a species of Aspergillus genus, and was found to contain one Cu2+ per subunit. For many years, it was thought that the B. subtilis quercetinase contained two Fe2+ ions per subunit; however, it has since been discovered that Mn2+ is a much more likely cofactor. Studies of overexpressed bacterial enzyme in E. coli indicated that this enzyme may be active with other metal ions (e.g. Co2+); however, the production of enzyme with full metal incorporation has only been possible with Mn2+. This study explores the notion that metal manipulation after translation, by partially unfolding the enzyme, chelating the metal ions, and then refolding the protein in the presence of an excess of divalent metal ions, could generate enzyme with full metal occupancy. The protocols presented here included testing for activity after incubating purified quercetinase with EDTA, DDTC, imidazole and GndHCl. It was found that the metal chelators had little to no effect on quercetinase activity. Imidazole did appear to inhibit the enzyme at concentrations in the millimolar range. In addition, the quercetinase was denatured in GndHCl at concentrations above 1 M. Recovering an active enzyme after partial or complete unfolding proved difficult, if not impossible.
ContributorsKrojanker, Elan Daniel (Author) / Francisco, Wilson (Thesis director) / Allen, James P. (Committee member) / Barrett, The Honors College (Contributor) / Department of Chemistry and Biochemistry (Contributor)
Created2014-05
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Description
In enzyme induced carbonate precipitation (EICP), calcium carbonate (CaCO3) precipitation is catalyzed by plant-derived urease enzyme. In EICP, urea hydrolyzes into ammonia and inorganic carbon, altering geochemical conditions in a manner that promotes carbonate mineral precipitation. The calcium source in this process comes from calcium chloride (CaCl2) in

In enzyme induced carbonate precipitation (EICP), calcium carbonate (CaCO3) precipitation is catalyzed by plant-derived urease enzyme. In EICP, urea hydrolyzes into ammonia and inorganic carbon, altering geochemical conditions in a manner that promotes carbonate mineral precipitation. The calcium source in this process comes from calcium chloride (CaCl2) in aqueous solution. Research work conducted for this dissertation has demonstrated that EICP can be employed for a variety of geotechnical purposes, including mass soil stabilization, columnar soil stabilization, and stabilization of erodible surficial soils. The research presented herein also shows that the optimal ratio of urea to CaCl2 at ionic strengths of less than 1 molar is approximately 1.75:1. EICP solutions of very high initial ionic strength (i.e. 6 M) as well as high urea concentrations (> 2 M) resulted in enzyme precipitation (salting-out) which hindered carbonate precipitation. In addition, the production of NH4+ may also result in enzyme precipitation. However, enzyme precipitation appeared to be reversible to some extent. Mass soil stabilization was demonstrated via percolation and mix-and-compact methods using coarse silica sand (Ottawa 20-30) and medium-fine silica sand (F-60) to produce cemented soil specimens whose strength improvement correlated with CaCO3 content, independent of the method employed to prepare the specimen. Columnar stabilization, i.e. creating columns of soil cemented by carbonate precipitation, using Ottawa 20-30, F-60, and native AZ soil was demonstrated at several scales beginning with small columns (102-mm diameter) and culminating in a 1-m3 soil-filled box. Wind tunnel tests demonstrated that surficial soil stabilization equivalent to that provided by thoroughly wetting the soil can be achieved through a topically-applied solution of CaCl2, urea, and the urease enzyme. The topically applied solution was shown to form an erosion-resistant CaCO3 crust on fine sand and silty soils. Cementation of erodible surficial soils was also achieved via EICP by including a biodegradable hydrogel in the stabilization solution. A dilute hydrogel solution extended the time frame over which the precipitation reaction could occur and provided improved spatial control of the EICP solution.
ContributorsHamdan, Nasser M (Author) / Kavazanjian Jr., Edward (Thesis advisor) / Rittmann, Bruce (Thesis advisor) / Shock, Everett (Committee member) / Arizona State University (Publisher)
Created2015