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Research on the Carbon and Water Cycle in Aquatic Ecosystems

A special issue of Water (ISSN 2073-4441). This special issue belongs to the section "Ecohydrology".

Deadline for manuscript submissions: 30 November 2025 | Viewed by 737

Special Issue Editors


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Guest Editor
Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
Interests: carbon cycling; carbon budget; climate change; aquatic ecosystem; ecohydrology; greenhouse gas emission

E-Mail Website
Guest Editor
Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
Interests: inland water carbon cycle; carbon production and emission; greenhouse gases; carbon metabolism; carbon budget; phytoplankton; primary productivity

Special Issue Information

Dear Colleagues,

Cabon (C) and water act as the fundamental driving forces of the earth system. The movement of water drives the biogeochemical cycle of carbon. The land-to-ocean aquatic continuum (LOAC), constituted by rivers, lakes, estuaries, tidal wetlands, and continental shelf waters, is recognized as an important pipeline and reactor for different forms of natural C, such as dissolved organic carbon (DOC), particulate organic carbon (POC), dissolved inorganic carbon (DIC), particulate inorganic carbon (PIC), carbon dioxide (CO2), and methane (CH4). LOAC C cycling involves multiple biological, chemical, geological, and physical processes from different interfaces between land, water, and atmosphere. As we are limited by observational data and assessment methodology, there still exists a large knowledge gap in understanding the biogeochemical processes and associated drivers of LOAC C cycling.

This Special Issue in Water aims to document the most recent advances in understanding aquatic ecosystem C cycling. The scope of this Special Issue includes, but is not limited to, the following:

(1) observation, simulation, and evaluation of the multi-interface and multi-process C cycling (such as C evasion, C burial, C transportation, and C metabolism) in aquatic ecosystems;

(2) the C flux and budget of aquatic ecosystems ranging from regional to global scales;

(3) the coupling mechanism between the hydrologic process and C cycling;

(4) the response of aquatic ecosystem C biogeochemistry to climate change and human activities.

Dr. Kun Sun
Dr. Junjie Jia
Guest Editors

Manuscript Submission Information

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Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Water is an international peer-reviewed open access semimonthly journal published by MDPI.

Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 2600 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI's English editing service prior to publication or during author revisions.

Keywords

  • aquatic ecosystem
  • inland water
  • carbon cycle
  • carbon budget
  • carbon metabolism
  • biogeochemistry
  • ecohydrology
  • greenhouse gas emission

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Published Papers (1 paper)

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Research

20 pages, 3273 KiB  
Article
Source Identification and Release Potential of Soil Phosphorus in the Water-Level Fluctuation Zone of Large Reservoirs: A Case Study of the Three Gorges Reservoir, China
by Chaonan Han, Tianhao Dai, Zebin Tian, Yu Tang, Hao Wu, Yimei Wang and Zhulai Wang
Water 2025, 17(5), 611; https://doi.org/10.3390/w17050611 - 20 Feb 2025
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Abstract
Reservoir water level regulation induces intricate processes of phosphorus (P) migration and release within the water-level fluctuation zone (WLFZ). These dynamic interactions pose significant challenges for effective pollution management strategies. This study focused on two typical tributary WLFZs (narrow gorges type and wide [...] Read more.
Reservoir water level regulation induces intricate processes of phosphorus (P) migration and release within the water-level fluctuation zone (WLFZ). These dynamic interactions pose significant challenges for effective pollution management strategies. This study focused on two typical tributary WLFZs (narrow gorges type and wide river type) in Three Gorges Reservoir (TGR), aiming to quantify P sources and assess their release potentials across two operational periods. Results showed that the deposition of suspended particulate P (SS-P) transported from the upstream was the dominant P source in the two WLFZs during the low water level period (August 2022). During the drainage period, the main P source of the ‘narrow gorges type’ WLFZ was P loss from slope soil above the WLFZ, but the ‘wide river type’ WLFZ had a mix of P sources, including P loss from slope soil, SS-P depositions from the TGR backwater and the tributary upstream. Among the three P sources, the slope soil source exhibited a relatively higher degree of P saturation (DPS) values (0.5–18.8%), indicating a greater potential for P release. Given that P loss from slope soil is the primary P source in the WLFZs during the drainage period, which coincides with the spring plowing season, it is crucial to implement measures to prevent P loss from slope soils to safeguard water quality in the TGR. Full article
(This article belongs to the Special Issue Research on the Carbon and Water Cycle in Aquatic Ecosystems)
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