Enzymatic Activity of Soybean Lipoxygenase-1 on Linoleoyl-Derivatized Agarose

Soybean lipoxygenase-1 (SBLO-1) catalyzes the oxygenation of linoleic acid to form 13(S) and 9(R) hydroperoxides. The manner in which substrates bind to the lipoxygenase family of enzymes is not known. It is believed fatty acid substrates may bind either with the aliphatic end first or with the carboxylate group facing the interior of the protein. This thesis tested a potential methyl-end first substrate binding mechanism by studying the activity of SBLO-1 to oxygenate immobilized linoleoyl residues attached to an insoluble polymer. Linoleic acid was attached to aminohexyl agarose in the presence of N-(3- dimethylaminopropyl)-N’-ethylcarbodiimide hydrochloride (EDC) and Nhydroxysuccinimide (NHS). The concentration of the covalently attached residues was facilitated by enriching linoleic acid with a small amount of the radioactive 14C-isotope. Functionalization yields of 3% available primary amines on the resin were obtained. Enzymatic oxygenation of the linoleoyl-residues was verified using the ferrous oxidation in xylenol orange (FOX) assay. Approximately 30% of the attached linoleoyl moieties were converted to hydroperoxides in the presence of SBLO-1. A disulfide-containing cleavable linker, cystamine, was used as part of an improved method to isolate the product in a facile manner. Cystamine was attached to NHS-activated agarose with approximately 5% overall functionalization yield of available functional groups. 14C-linoleic acid was successfully covalently linked to the cystamine moieties in the presence of EDC and NHS. The FOX assay verified the enzymatic oxygenation of the linoleoyl residues attached to cystamine-derivatized agarose. The isolation of the peroxide product was attempted in a series of extractions in organic solvents. The product was analyzed using GC/MS which did not show a new peak indicative of product. Further work is needed to successfully analyze the stereoand regiochemistry of the oxygenated product. The presence of the peroxides in this study indicated the linoleoyl residues behave as substrates of SBLO-1. It is unknown how bulky substrates bind to the active site; however, it is difficult to rationalize a carboxylate group-first binding mode. Discovery of the 13(S)-hydroperoxide product on the linoleoyl-agarose would support the claim of a potential methyl-end first binding mechanism.

Geochemical Modeling and Analysis of the Frac Water Used in the Hydraulic Fracturing of the Marcellus Formation, Pennsylvania

The hydraulic fracturing of the Marcellus Formation creates a byproduct known as frac water. Five frac water samples were collected in Bradford County, PA. Inorganic chemical analysis, field parameters analysis, alkalinity titrations, total dissolved solids(TDS), total suspended solids (TSS), biological oxygen demand (BOD), and chemical oxygen demand (COD) were conducted on each sample to characterize frac water. A database of frac water chemistry results from across the state of Pennsylvania from multiple sources was compiled in order to provide the public and research communitywith an accurate characterization of frac water. Four geochemical models were created to model the reactions between frac water and the Marcellus Formation, Purcell Limestone, and the oil field brines presumed present in the formations. The average concentrations of chloride and TDS in the five frac water samples were 1.1 �± 0.5 x 105 mg/L (5.5X average seawater) and 140,000 mg/L (4X average seawater). BOD values for frac water immediately upon flow back were over 10X greater than the BOD of typical wastewater, but decreased into the range of typical wastewater after a short period of time. The COD of frac water decreases dramatically with an increase in elapsed time from flow back, but remain considerably higher than typicalwastewater. Different alkalinity calculation methods produced a range of alkalinity values for frac water: this result is most likely due to high concentrations of aliphatic acid anions present in the samples. Laboratory analyses indicate that the frac watercomposition is quite variable depending on the companies from which the water was collected, the geology of the local area, and number of fracturing jobs in which the frac water was used, but will require more treatment than typical wastewater regardless of theprecise composition of each sample. The geochemical models created suggest that the presence of organic complexes in an oil field brine and Marcellus Formation aid in the dissolution of ions such as bariumand strontium into the solution. Although equilibration reactions between the Marcellus Formation and the slickwater account for some of the final frac water composition, the predominant control of frac water composition appears to be the ratio of the mixture between the oil field brine and slickwater. The high concentration of barium in the frac water is likely due to the abundance of barite nodules in the Purcell Limestone, and the lack of sulfate in the frac water samples is due to the reducing, anoxic conditions in the earth's subsurface that allow for the degassing of H2S(g).