Abstract

Human activities have led to excessive nutrient enrichment which is greater than lake systems can naturally assimilate. This process is known as eutrophication and it is driving significant algae growth resulting in the more common release of harmful toxins. Utah Lake, located in Utah County, UT is one such water body that even after major reductions in anthropogenic phosphorus influent, continues to experience frequent, harmful algal blooms. The extent to which natural processes, like atmospheric dust deposition and sediment recycling, contribute to the lake's phosphorus budget is still poorly understood.

To address this gap of knowledge, this study quantified phosphorus inputs from dust and analyzed porewater geochemistry from three lake sediment freeze cores. Dust collected with active air samplers showed no significant attenuation along the southwest–northeast transect as previously hypothesized, although phosphorus solubility declined in the same direction possibly indicating the significance of anthropogenic dust contribution. Porewater geochemistry revealed evidence of diverse porewater movement, exhibiting both groundwater-driven advection and diffusive release of phosphorus from the lake sediments. Using Fick’s law, the estimated lake sediment diffusion contributes an average of 790 mT yr⁻¹ (5.7 mg P m⁻² d⁻¹), representing approximately 68% of total phosphorus loading to the lake.

These results highlight dust and lake sediment recycling as complex, understudied nonpoint sources of phosphorus. By clarifying their magnitude and mechanisms, this study advances understanding of nutrient dynamics in Utah Lake and informs for more effective strategies in eutrophication management.

Degree

MS

College and Department

Computational, Mathematical, and Physical Sciences; Geological Sciences

Rights

https://lib.byu.edu/about/copyright/

Date Submitted

2025-12-18

Document Type

Thesis

Keywords

eutrophication, algal, water quality, atmospheric deposition, sediment flux

Language

english

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