INTERACTIONS BETWEEN SUSPENDED SEDIMENTS, NUTRIENTS AND

dc.contributor.authorPaudel, Bhanu
dc.date.accessioned2014-11-10T21:23:16Z
dc.date.available2014-11-10T21:23:16Z
dc.date.issued11/10/2014
dc.descriptionSubmitted in Partial Fulfillment of the Requirements for the Degree of DOCTOR OF PHILOSOPHY in COASTAL MARINE SYSTEM SCIENCEen_US
dc.description.abstractThe objectives of the present study were to identify the effects of freshwater inflow (FWI) on sediment transport and nutrients supply to estuaries, and the effects of sediments on nutrient supply at sediment-water interface. The Nueces River and its estuary, the Guadalupe River and its estuary, and the Lavaca-Colorado Estuary were selected for field studies. Laboratory experiments were conducted to test the study hypotheses, and data was analyzed using multivariate modeling and statistical approaches. In the Guadalupe Estuary, variability of suspended solids and nutrients were correlated with FWI, whereas in the Nueces and Lavaca-Colorado Estuary they were related with seasonal differences. Suspended solids in the estuaries increased during frontal events and during windy days. In some of the field samplings, stations closer to the Gulf of Mexico had higher suspended sediments than the stations closer to the river. The increase in suspended sediments increased ammonia concentration in the Guadalupe Estuary, phosphorus and silicate concentrations in the Nueces Estuary, and silicate concentration in the Lavaca-Colorado Estuary. The presence of silicate minerals in the estuaries maintains silicate concentration as well. Organic matter and calcium carbonate shells in sediments of the estuaries can bind phosphate, thus, may have played role in decreasing phosphate concentration in the water. Guadalupe River sediments, when transported to the estuary, can release ammonia at higher concentrations the river water concentration. Salinity in the estuary, thus, has a significant role in controlling nutrient concentrations. The release of ammonia by organic matter decomposition was lower in the Guadalupe Estuary than in the Nueces Estuary. The high inflow volumes in the Guadalupe Estuary may have washed away organic matter from the sediments and may have disturbed bacterial community resulting in the lower release of ammonia from Guadalupe Estuary sediments. The research performed here demonstrates the importance of sediments, organic matter, and inflow in maintaining nutrient concentrations in estuaries. Fluctuation of these nutrients can affect water quality, and hence, may influence the ecology of the estuary.en_US
dc.description.collegeCollege of Science and Engineeringen_US
dc.description.departmentPhysical and Environmental Sciencesen_US
dc.identifier.urihttp://hdl.handle.net/1969.6/578
dc.language.isoen_USen_US
dc.rightsThis material is made available for use in research, teaching, and private study, pursuant to U.S. Copyright law. The user assumes full responsibility for any use of the materials, including but not limited to, infringement of copyright and publication rights of reproduced materials. Any materials used should be fully credited with its source. All rights are reserved and retained regardless of current or future development or laws that may apply to fair use standards. Permission for publication of this material, in part or in full, must be secured with the author and/or publisher.en_US
dc.subjectfreshwater inflowen_US
dc.subjectMineralen_US
dc.subjectMultivariate modelingen_US
dc.subjectnutrientsen_US
dc.subjectorganic matteren_US
dc.subjectsedimentsen_US
dc.titleINTERACTIONS BETWEEN SUSPENDED SEDIMENTS, NUTRIENTS ANDen_US
dc.typeTexten_US
dc.type.genreDissertationen_US
thesis.degree.disciplineCoastal and Marine System Scienceen_US
thesis.degree.grantorTexas A & M University--Corpus Christien_US
thesis.degree.levelDoctoralen_US
thesis.degree.nameDoctor of Philosophyen_US

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