The Effect of Monsoon Rainfall Patterns on Epilithic Diatom Communities in the Hantangang River, Korea

Most of Korea’s rivers and lakes are subject to physico-chemical disturbances, such as increased water quantity and flow rates, and influx of nitrogen and phosphorus, due to intense rainfall concentrated in the Asian monsoon season. To examine the influence of rainfall on epilithic diatom communitie...

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Main Authors: In-Hwan Cho, Ha-Kyung Kim, Min-Hyuk Lee, Yong-Jae Kim, Hyuk Lee, Baik-Ho Kim
Format: Article
Language:English
Published: MDPI AG 2020-05-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/12/5/1471
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author In-Hwan Cho
Ha-Kyung Kim
Min-Hyuk Lee
Yong-Jae Kim
Hyuk Lee
Baik-Ho Kim
author_facet In-Hwan Cho
Ha-Kyung Kim
Min-Hyuk Lee
Yong-Jae Kim
Hyuk Lee
Baik-Ho Kim
author_sort In-Hwan Cho
collection DOAJ
description Most of Korea’s rivers and lakes are subject to physico-chemical disturbances, such as increased water quantity and flow rates, and influx of nitrogen and phosphorus, due to intense rainfall concentrated in the Asian monsoon season. To examine the influence of rainfall on epilithic diatom communities, we measured the diatom distribution and river water quality at 29 sites along the main-stream and tributaries of the Hantangang River, Korea, in the period of 2012–2015. Water quality parameters in the polluted sites had improved following rainfall, but the response of dominant species varied with water quality; the dominant species <i>Nitzschia fonticola</i> decreased in abundance regardless of sampling sites, and the abundance of <i>Achnanthidium minutissimum</i> in the clean sites and <i>Nitzschia palea</i> in the polluted sites increased after rainfall, respectively. The community dynamic index (CDI) showed that the most obvious shift of epilithic diatom community occurred in the mid-polluted sites in 2013 with the highest rainfall. This suggest that the effect of rainfalls on the epilithic diatom community is dependent on various parameters, such as the magnitude of rainfall, water quality and its biotic compositions of diatom communities, but it also indicates that improving the water quality of rivers is important to promote the resilience of diatom communities to extremes of precipitation. Further investigation is needed to generalize the effects of monsoon rainfall on the epilithic diatom communities, considering rivers with different environmental characteristics.
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spelling doaj.art-0482e0cb9e2b416b8fb52e35ef74471b2023-11-20T01:14:33ZengMDPI AGWater2073-44412020-05-01125147110.3390/w12051471The Effect of Monsoon Rainfall Patterns on Epilithic Diatom Communities in the Hantangang River, KoreaIn-Hwan Cho0Ha-Kyung Kim1Min-Hyuk Lee2Yong-Jae Kim3Hyuk Lee4Baik-Ho Kim5Department of Environmental Science, Hanyang University, Seoul 04763, KoreaDepartment of Environmental Science, Hanyang University, Seoul 04763, KoreaDoohee Institute of Ecological Research, Korea Ecosystem Service Inc., Gyeonggi-do 13814, KoreaDepartment of Life Science, Daejin University, Pochun, Gyunggi 487-711, KoreaNational Institute of Environmental Research, Incheon 22689, KoreaDepartment of Life Science and Research Institute for Natural Sciences, Hanyang University, Seoul 04763, KoreaMost of Korea’s rivers and lakes are subject to physico-chemical disturbances, such as increased water quantity and flow rates, and influx of nitrogen and phosphorus, due to intense rainfall concentrated in the Asian monsoon season. To examine the influence of rainfall on epilithic diatom communities, we measured the diatom distribution and river water quality at 29 sites along the main-stream and tributaries of the Hantangang River, Korea, in the period of 2012–2015. Water quality parameters in the polluted sites had improved following rainfall, but the response of dominant species varied with water quality; the dominant species <i>Nitzschia fonticola</i> decreased in abundance regardless of sampling sites, and the abundance of <i>Achnanthidium minutissimum</i> in the clean sites and <i>Nitzschia palea</i> in the polluted sites increased after rainfall, respectively. The community dynamic index (CDI) showed that the most obvious shift of epilithic diatom community occurred in the mid-polluted sites in 2013 with the highest rainfall. This suggest that the effect of rainfalls on the epilithic diatom community is dependent on various parameters, such as the magnitude of rainfall, water quality and its biotic compositions of diatom communities, but it also indicates that improving the water quality of rivers is important to promote the resilience of diatom communities to extremes of precipitation. Further investigation is needed to generalize the effects of monsoon rainfall on the epilithic diatom communities, considering rivers with different environmental characteristics.https://www.mdpi.com/2073-4441/12/5/1471Asia-monsooncommunity dynamic indexdistance methodprincipal component analysisepilithic diatomrainfall
spellingShingle In-Hwan Cho
Ha-Kyung Kim
Min-Hyuk Lee
Yong-Jae Kim
Hyuk Lee
Baik-Ho Kim
The Effect of Monsoon Rainfall Patterns on Epilithic Diatom Communities in the Hantangang River, Korea
Water
Asia-monsoon
community dynamic index
distance method
principal component analysis
epilithic diatom
rainfall
title The Effect of Monsoon Rainfall Patterns on Epilithic Diatom Communities in the Hantangang River, Korea
title_full The Effect of Monsoon Rainfall Patterns on Epilithic Diatom Communities in the Hantangang River, Korea
title_fullStr The Effect of Monsoon Rainfall Patterns on Epilithic Diatom Communities in the Hantangang River, Korea
title_full_unstemmed The Effect of Monsoon Rainfall Patterns on Epilithic Diatom Communities in the Hantangang River, Korea
title_short The Effect of Monsoon Rainfall Patterns on Epilithic Diatom Communities in the Hantangang River, Korea
title_sort effect of monsoon rainfall patterns on epilithic diatom communities in the hantangang river korea
topic Asia-monsoon
community dynamic index
distance method
principal component analysis
epilithic diatom
rainfall
url https://www.mdpi.com/2073-4441/12/5/1471
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