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A study on the occurrence of black water in reservoirs in Eucalyptus Plantation region
Tianbao reservoir in southern China (surrounded by Eucalyptus plantation) serves as a source of drinking water for the inhabitants. However, the reservoir water experiences black water (BW) of which the cause remains unclear. In this study, field observation and simulated laboratory experiment were...
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Published in: | Environmental science and pollution research international 2020-10, Vol.27 (28), p.34927-34940 |
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creator | Luo, Fan Li, Yiping Norgbey, Eyram Li, Ronghui Ya, Zhu Nwankwegu, Amechi S. Lie, Huang Sarpong, Linda |
description | Tianbao reservoir in southern China (surrounded by
Eucalyptus
plantation) serves as a source of drinking water for the inhabitants. However, the reservoir water experiences black water (BW) of which the cause remains unclear. In this study, field observation and simulated laboratory experiment were conducted to understand the cause of the BW. The diffusive gradient in thin-film (DGT) device monitored the spatial changes in concentration of iron (Fe
2+
), manganese (Mn
2+
), sulfide (S
2−
), and dissolved organic carbon (DOC) at the SWI. The planar optode (PO) showed that hypoxia contributed immensely to the high positive fluxes Fe
2+
, Mn
2+
, and S
2−
measured, which co-precipitated to form black materials (FeS and MnS) at the SWI. The co-precipitation between Fe–S and Mn–S was supported by their significant positive correlation (Fe–S:
r
> 0.05,
p
< 0.05, Mn–S:
r
> 0.2,
p
< 0.05). Significant reduction (
p
< 0.05) in tannins concentration from November (strong thermal stratification) to December (weak thermal stratification) indicated that Fe
2+
and tannins reacted during the mixing of reservoir water in December due to weak stratification. The simulated experiment confirmed that fresh
Eucalyptus
leaves produces a significant (
p
< 0.05) amount of tannins during hypoxia and reacts with Fe
2+
to produce black water. A high positive correlation (
r
> 0.8) between Fe
2+
and DOC demonstrated that Fe
2+
and DOC combined and contributed to the reservoir water blackening. The study provides a better understanding on the impact of
Eucalyptus
plantation on water quality and provide guidance for scientific planting of Eucalyptus plantation in reservoir basins in southern China to ensure safe drinking water. |
doi_str_mv | 10.1007/s11356-020-09613-3 |
format | article |
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Eucalyptus
plantation) serves as a source of drinking water for the inhabitants. However, the reservoir water experiences black water (BW) of which the cause remains unclear. In this study, field observation and simulated laboratory experiment were conducted to understand the cause of the BW. The diffusive gradient in thin-film (DGT) device monitored the spatial changes in concentration of iron (Fe
2+
), manganese (Mn
2+
), sulfide (S
2−
), and dissolved organic carbon (DOC) at the SWI. The planar optode (PO) showed that hypoxia contributed immensely to the high positive fluxes Fe
2+
, Mn
2+
, and S
2−
measured, which co-precipitated to form black materials (FeS and MnS) at the SWI. The co-precipitation between Fe–S and Mn–S was supported by their significant positive correlation (Fe–S:
r
> 0.05,
p
< 0.05, Mn–S:
r
> 0.2,
p
< 0.05). Significant reduction (
p
< 0.05) in tannins concentration from November (strong thermal stratification) to December (weak thermal stratification) indicated that Fe
2+
and tannins reacted during the mixing of reservoir water in December due to weak stratification. The simulated experiment confirmed that fresh
Eucalyptus
leaves produces a significant (
p
< 0.05) amount of tannins during hypoxia and reacts with Fe
2+
to produce black water. A high positive correlation (
r
> 0.8) between Fe
2+
and DOC demonstrated that Fe
2+
and DOC combined and contributed to the reservoir water blackening. The study provides a better understanding on the impact of
Eucalyptus
plantation on water quality and provide guidance for scientific planting of Eucalyptus plantation in reservoir basins in southern China to ensure safe drinking water.</description><identifier>ISSN: 0944-1344</identifier><identifier>EISSN: 1614-7499</identifier><identifier>DOI: 10.1007/s11356-020-09613-3</identifier><identifier>PMID: 32577983</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Aquatic Pollution ; Atmospheric Protection/Air Quality Control/Air Pollution ; Blackening ; Blackwater ; China ; Computer simulation ; Concentration gradient ; Dissolved organic carbon ; Drinking water ; Earth and Environmental Science ; Ecotoxicology ; Environment ; Environmental Chemistry ; Environmental Health ; Environmental Monitoring ; Environmental science ; Eucalyptus ; Fluxes ; Hypoxia ; Iron ; Iron - analysis ; Iron sulfides ; Manganese ; Plantations ; Research Article ; Reservoirs ; Tannins ; Thermal stratification ; Thin films ; Waste Water Technology ; Water ; Water Management ; Water Pollutants, Chemical - analysis ; Water Pollution Control ; Water quality</subject><ispartof>Environmental science and pollution research international, 2020-10, Vol.27 (28), p.34927-34940</ispartof><rights>Springer-Verlag GmbH Germany, part of Springer Nature 2020</rights><rights>Springer-Verlag GmbH Germany, part of Springer Nature 2020.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c412t-7a2646cc90a0d6f2c722c2bd680d3dc85e77280e045a8d2e7457bf061ad3b26d3</citedby><cites>FETCH-LOGICAL-c412t-7a2646cc90a0d6f2c722c2bd680d3dc85e77280e045a8d2e7457bf061ad3b26d3</cites><orcidid>0000-0002-1020-2533</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/2436977803/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$H</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/2436977803?pq-origsite=primo$$EHTML$$P50$$Gproquest$$H</linktohtml><link.rule.ids>314,780,784,11688,27924,27925,36060,44363,74895</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/32577983$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Luo, Fan</creatorcontrib><creatorcontrib>Li, Yiping</creatorcontrib><creatorcontrib>Norgbey, Eyram</creatorcontrib><creatorcontrib>Li, Ronghui</creatorcontrib><creatorcontrib>Ya, Zhu</creatorcontrib><creatorcontrib>Nwankwegu, Amechi S.</creatorcontrib><creatorcontrib>Lie, Huang</creatorcontrib><creatorcontrib>Sarpong, Linda</creatorcontrib><title>A study on the occurrence of black water in reservoirs in Eucalyptus Plantation region</title><title>Environmental science and pollution research international</title><addtitle>Environ Sci Pollut Res</addtitle><addtitle>Environ Sci Pollut Res Int</addtitle><description>Tianbao reservoir in southern China (surrounded by
Eucalyptus
plantation) serves as a source of drinking water for the inhabitants. However, the reservoir water experiences black water (BW) of which the cause remains unclear. In this study, field observation and simulated laboratory experiment were conducted to understand the cause of the BW. The diffusive gradient in thin-film (DGT) device monitored the spatial changes in concentration of iron (Fe
2+
), manganese (Mn
2+
), sulfide (S
2−
), and dissolved organic carbon (DOC) at the SWI. The planar optode (PO) showed that hypoxia contributed immensely to the high positive fluxes Fe
2+
, Mn
2+
, and S
2−
measured, which co-precipitated to form black materials (FeS and MnS) at the SWI. The co-precipitation between Fe–S and Mn–S was supported by their significant positive correlation (Fe–S:
r
> 0.05,
p
< 0.05, Mn–S:
r
> 0.2,
p
< 0.05). Significant reduction (
p
< 0.05) in tannins concentration from November (strong thermal stratification) to December (weak thermal stratification) indicated that Fe
2+
and tannins reacted during the mixing of reservoir water in December due to weak stratification. The simulated experiment confirmed that fresh
Eucalyptus
leaves produces a significant (
p
< 0.05) amount of tannins during hypoxia and reacts with Fe
2+
to produce black water. A high positive correlation (
r
> 0.8) between Fe
2+
and DOC demonstrated that Fe
2+
and DOC combined and contributed to the reservoir water blackening. The study provides a better understanding on the impact of
Eucalyptus
plantation on water quality and provide guidance for scientific planting of Eucalyptus plantation in reservoir basins in southern China to ensure safe drinking water.</description><subject>Aquatic Pollution</subject><subject>Atmospheric Protection/Air Quality Control/Air Pollution</subject><subject>Blackening</subject><subject>Blackwater</subject><subject>China</subject><subject>Computer simulation</subject><subject>Concentration gradient</subject><subject>Dissolved organic carbon</subject><subject>Drinking water</subject><subject>Earth and Environmental Science</subject><subject>Ecotoxicology</subject><subject>Environment</subject><subject>Environmental Chemistry</subject><subject>Environmental Health</subject><subject>Environmental Monitoring</subject><subject>Environmental science</subject><subject>Eucalyptus</subject><subject>Fluxes</subject><subject>Hypoxia</subject><subject>Iron</subject><subject>Iron - analysis</subject><subject>Iron sulfides</subject><subject>Manganese</subject><subject>Plantations</subject><subject>Research Article</subject><subject>Reservoirs</subject><subject>Tannins</subject><subject>Thermal stratification</subject><subject>Thin films</subject><subject>Waste Water Technology</subject><subject>Water</subject><subject>Water Management</subject><subject>Water Pollutants, Chemical - analysis</subject><subject>Water Pollution Control</subject><subject>Water quality</subject><issn>0944-1344</issn><issn>1614-7499</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><sourceid>M0C</sourceid><recordid>eNp9kMtOwzAQRS0EoqXwAyyQJdYGv2Iny6oqD6kSLICt5dhOSWmTYjug_j0OKbBjNTOaM3ekA8A5wVcEY3kdCGGZQJhihAtBGGIHYEwE4UjyojgEY1xwjgjjfAROQljhRBZUHoMRo5mURc7G4GUKQ-zsDrYNjK8OtsZ03rvGpLaC5VqbN_ipo_OwbqB3wfmPtvahn-ad0evdNnYBPq51E3Ws255ZpnIKjiq9Du5sXyfg-Wb-NLtDi4fb-9l0gQwnNCKpqeDCmAJrbEVFjaTU0NKKHFtmTZ45KWmOHeaZzi11kmeyrLAg2rKSCssm4HLI3fr2vXMhqlXb-Sa9VJQzUUiZY5YoOlDGtyF4V6mtrzfa7xTBqlepBpUqCVLfKlV_dLGP7sqNs78nP-4SwAYgpFWzdP7v9z-xX5vhfqE</recordid><startdate>20201001</startdate><enddate>20201001</enddate><creator>Luo, Fan</creator><creator>Li, Yiping</creator><creator>Norgbey, Eyram</creator><creator>Li, Ronghui</creator><creator>Ya, Zhu</creator><creator>Nwankwegu, Amechi S.</creator><creator>Lie, Huang</creator><creator>Sarpong, Linda</creator><general>Springer Berlin 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study on the occurrence of black water in reservoirs in Eucalyptus Plantation region</title><author>Luo, Fan ; Li, Yiping ; Norgbey, Eyram ; Li, Ronghui ; Ya, Zhu ; Nwankwegu, Amechi S. ; Lie, Huang ; Sarpong, Linda</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c412t-7a2646cc90a0d6f2c722c2bd680d3dc85e77280e045a8d2e7457bf061ad3b26d3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Aquatic Pollution</topic><topic>Atmospheric Protection/Air Quality Control/Air Pollution</topic><topic>Blackening</topic><topic>Blackwater</topic><topic>China</topic><topic>Computer simulation</topic><topic>Concentration gradient</topic><topic>Dissolved organic carbon</topic><topic>Drinking water</topic><topic>Earth and Environmental Science</topic><topic>Ecotoxicology</topic><topic>Environment</topic><topic>Environmental Chemistry</topic><topic>Environmental Health</topic><topic>Environmental Monitoring</topic><topic>Environmental science</topic><topic>Eucalyptus</topic><topic>Fluxes</topic><topic>Hypoxia</topic><topic>Iron</topic><topic>Iron - analysis</topic><topic>Iron sulfides</topic><topic>Manganese</topic><topic>Plantations</topic><topic>Research Article</topic><topic>Reservoirs</topic><topic>Tannins</topic><topic>Thermal stratification</topic><topic>Thin films</topic><topic>Waste Water Technology</topic><topic>Water</topic><topic>Water Management</topic><topic>Water Pollutants, Chemical - analysis</topic><topic>Water Pollution Control</topic><topic>Water quality</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Luo, Fan</creatorcontrib><creatorcontrib>Li, Yiping</creatorcontrib><creatorcontrib>Norgbey, Eyram</creatorcontrib><creatorcontrib>Li, Ronghui</creatorcontrib><creatorcontrib>Ya, Zhu</creatorcontrib><creatorcontrib>Nwankwegu, Amechi S.</creatorcontrib><creatorcontrib>Lie, 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region</atitle><jtitle>Environmental science and pollution research international</jtitle><stitle>Environ Sci Pollut Res</stitle><addtitle>Environ Sci Pollut Res Int</addtitle><date>2020-10-01</date><risdate>2020</risdate><volume>27</volume><issue>28</issue><spage>34927</spage><epage>34940</epage><pages>34927-34940</pages><issn>0944-1344</issn><eissn>1614-7499</eissn><abstract>Tianbao reservoir in southern China (surrounded by
Eucalyptus
plantation) serves as a source of drinking water for the inhabitants. However, the reservoir water experiences black water (BW) of which the cause remains unclear. In this study, field observation and simulated laboratory experiment were conducted to understand the cause of the BW. The diffusive gradient in thin-film (DGT) device monitored the spatial changes in concentration of iron (Fe
2+
), manganese (Mn
2+
), sulfide (S
2−
), and dissolved organic carbon (DOC) at the SWI. The planar optode (PO) showed that hypoxia contributed immensely to the high positive fluxes Fe
2+
, Mn
2+
, and S
2−
measured, which co-precipitated to form black materials (FeS and MnS) at the SWI. The co-precipitation between Fe–S and Mn–S was supported by their significant positive correlation (Fe–S:
r
> 0.05,
p
< 0.05, Mn–S:
r
> 0.2,
p
< 0.05). Significant reduction (
p
< 0.05) in tannins concentration from November (strong thermal stratification) to December (weak thermal stratification) indicated that Fe
2+
and tannins reacted during the mixing of reservoir water in December due to weak stratification. The simulated experiment confirmed that fresh
Eucalyptus
leaves produces a significant (
p
< 0.05) amount of tannins during hypoxia and reacts with Fe
2+
to produce black water. A high positive correlation (
r
> 0.8) between Fe
2+
and DOC demonstrated that Fe
2+
and DOC combined and contributed to the reservoir water blackening. The study provides a better understanding on the impact of
Eucalyptus
plantation on water quality and provide guidance for scientific planting of Eucalyptus plantation in reservoir basins in southern China to ensure safe drinking water.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><pmid>32577983</pmid><doi>10.1007/s11356-020-09613-3</doi><tpages>14</tpages><orcidid>https://orcid.org/0000-0002-1020-2533</orcidid></addata></record> |
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ispartof | Environmental science and pollution research international, 2020-10, Vol.27 (28), p.34927-34940 |
issn | 0944-1344 1614-7499 |
language | eng |
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source | ABI/INFORM Global; Springer Nature |
subjects | Aquatic Pollution Atmospheric Protection/Air Quality Control/Air Pollution Blackening Blackwater China Computer simulation Concentration gradient Dissolved organic carbon Drinking water Earth and Environmental Science Ecotoxicology Environment Environmental Chemistry Environmental Health Environmental Monitoring Environmental science Eucalyptus Fluxes Hypoxia Iron Iron - analysis Iron sulfides Manganese Plantations Research Article Reservoirs Tannins Thermal stratification Thin films Waste Water Technology Water Water Management Water Pollutants, Chemical - analysis Water Pollution Control Water quality |
title | A study on the occurrence of black water in reservoirs in Eucalyptus Plantation region |
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