2021
DOI: 10.1007/s00128-021-03359-5
|View full text |Cite
|
Sign up to set email alerts
|

Water Quality Analysis and Evaluation of Eutrophication in a Swamp Wetland in the Permafrost Region of the Lesser Khingan Mountains, China

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1

Citation Types

0
3
0

Year Published

2023
2023
2024
2024

Publication Types

Select...
6

Relationship

0
6

Authors

Journals

citations
Cited by 7 publications
(3 citation statements)
references
References 26 publications
0
3
0
Order By: Relevance
“…The classification criteria are as follows [38]: poor trophic state-TLI(∑) < 30; mesotrophic status-30 ≤ TLI(∑) ≤ 50; rich nutrition-TLI(∑) > 50; mild eutrophication-50 < TLI(∑) ≤ 60; medium eutrophication-60 < TLI(∑) ≤ 70; severe eutrophication-TLI(∑) > 70.…”
Section: Evaluation Of the Comprehensive Nutritional Status Of Lake W...mentioning
confidence: 99%
“…The classification criteria are as follows [38]: poor trophic state-TLI(∑) < 30; mesotrophic status-30 ≤ TLI(∑) ≤ 50; rich nutrition-TLI(∑) > 50; mild eutrophication-50 < TLI(∑) ≤ 60; medium eutrophication-60 < TLI(∑) ≤ 70; severe eutrophication-TLI(∑) > 70.…”
Section: Evaluation Of the Comprehensive Nutritional Status Of Lake W...mentioning
confidence: 99%
“…32−38 In permafrost ecosystems, waterlogging following thaw improved the conversion of Fe(III) to soluble Fe(II) and associated organic carbon mobilization into the porewater along a thaw gradient, 39,40 which might have a subsequent negative impact on lakes and river basin regions impacted by permafrostthaw. 41,42 Recent studies observed a strong correlation between C and Fe (III or II) and organic matter in both Yedoma 22 and non-Yedoma permafrost. 40 Due to its high ice content (ice wedges, segregated ice, pore ice) Yedoma permafrost is highly vulnerable to thermokarst and thermoerosional processes, 43 which might lead to posterior organic C release and mineralization.…”
Section: Introductionmentioning
confidence: 99%
“…Beyond oxygen availability, organo-mineral associations play a crucial role in DOM biogeochemistry in various environmental systems due to complexation reactions such as adsorption, coprecipitation, and aggregation. Fe-bearing minerals are recognized as critical moderators of the temporal and spatial abundance of C in soils. In permafrost ecosystems, waterlogging following thaw improved the conversion of Fe­(III) to soluble Fe­(II) and associated organic carbon mobilization into the porewater along a thaw gradient, , which might have a subsequent negative impact on lakes and river basin regions impacted by permafrost-thaw. , Recent studies observed a strong correlation between C and Fe (III or II) and organic matter in both Yedoma and non-Yedoma permafrost . Due to its high ice content (ice wedges, segregated ice, pore ice) Yedoma permafrost is highly vulnerable to thermokarst and thermoerosional processes, which might lead to posterior organic C release and mineralization. ,, …”
Section: Introductionmentioning
confidence: 99%