Abstract

Geosmin is a major concern in the management of water sources worldwide. Thus, we predicted concentration categories of geosmin at three different depths of lakes (i.e., surface, middle, and bottom), and analyzed relationships between geosmin concentration and factors such as phytoplankton abundance and environmental variables. Data were collected monthly from three major lakes (Uiam, Cheongpyeong, and Paldang lakes) in Korea from May 2014 to December 2015. Before predicting geosmin concentration, we categorized it into four groups based on the boxplot method, and multivariate adaptive regression splines, classification and regression trees, and random forest (RF) were applied to identify the most appropriate modelling to predict geosmin concentration. Overall, using environmental variables was more accurate than using phytoplankton abundance to predict the four categories of geosmin concentration based on AUC and accuracy in all three models as well as each layer. The RF model had the highest predictive power among the three SDMs. When predicting geosmin in the three water layers, the relative importance of environmental variables and phytoplankton abundance in the sensitivity analysis was different for each layer. Water temperature and abundance of Cyanophyceae were the most important factors for predicting geosmin concentration categories in the surface layer, whereas total abundance of phytoplankton exhibited relatively higher importance in the bottom layer.

Highlights

  • Cyanobacterial blooms as a result of abnormal growth of algae signify problems such as nutrient over-enrichment, modified hydrology, and poor management of water bodies [1]

  • Species richness and abundance of phytoplankton communities were highest at all depths between August and October, and especially in the surface layer during most of the sampling period

  • The changes of species richness and abundance of phytoplankton communities in Uiam Lake was a significant positive correlation among three layers except for the species richness in the middle and bottom layer (r > 0.50, p < 0.05), whereas Cheongpyeong Lake significantly correlates with species richness only between the surface and bottom layers (r = 0.70, p < 0.05)

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Summary

Introduction

Cyanobacterial blooms as a result of abnormal growth of algae signify problems such as nutrient over-enrichment, modified hydrology, and poor management of water bodies [1]. These cyanobacterial blooms cause changes in various biological habitats of water bodies through deterioration of water quality. Algal and cyanobacterial blooms degrade water quality in drinking water supply reservoirs by producing toxic and unpleasant taste-and-odor causing secondary metabolites, which cause public health concerns and lead to increased treatment costs for water utility companies [2].

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