33 D12. Hydrogeology (Posters)
Sunday, 4 November 2018
9:00 AM - 5:30 PM
Halls J-K
A HYDROLOGIC COMPARISON OF THE CEDAR RIVER AND WEST OKOBOJI LAKE IN IOWA
Paper number: 33-16
Program: Technical Sessions
Time: 9:00 AM – 5:30 PM
Authors
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Mohammad IqbalUniversity of Northern Iowa, Cedar Falls, IA
Abstract
The results show that DO levels are similar in both the Cedar River and West Okoboji Lake. The Cedar River had an average of 8.59 mg/L. Similarly, West Okoboji Lake had a DO average of 8.25 mg/L. The average BOD value for the Cedar River was 0.99 mg/L and 0.61 mg/L for West Okoboji. TDS demonstrated a larger difference; the average for the Cedar River was 342 mg/L, while it was 287 mg/L for West Okoboji Lake. Another parameter with a notable difference between both bodies of water is turbidity. The average for the Cedar River was 15.51 mg/L, while West Okoboji Lake recorded an average of 2.93 mg/L. When compared spatially and temporally, West Okoboji Lake demonstrates consistency of the tested parameters. The Cedar River primarily fluctuates temporally within turbidity and TDS. Spatial fluctuations are observed throughout BOD and turbidity. Despite similar DO levels, the Cedar River’s turbulent flow dissolves surficial materials more actively. Based on low BOD, TDS, and turbidity values, West Okoboji Lake is less biochemically active than the Cedar River. The lower BOD values are somewhat of a surprise. Since West Okoboji Lake is a body of water lacking turbulence, microbiological organisms should complete reactions more effectively than in moving rivers. This trend may be related to the effective best management practices (BMP), such as state regulation or community work.
Geological Society of America Abstracts with Programs. Vol. 50, No. 6
doi: 10.1130/abs/2018AM-317275
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