Ditches as key players in carbon emissions in managed Phragmites-dominated wetland

IF 5.9 1区 地球科学 Q1 ENGINEERING, CIVIL
Hao Xue , Hu Ding , Xiaokun Han , Yunchao Lang , Tiejun Wang , Pan Li , Manrong Qiao , Dandan Liu , Zhanhang Liu , Congqiang Liu
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Abstract

Phragmites wetlands absorb carbon dioxide (CO2) and store organic matter, acting as a greenhouse gas sink, but also emit methane (CH4) from sediment, contributing to greenhouse gas emissions. Managed Phragmites wetlands for reserve purpose, with extensive drainage ditch networks, can be significant emission hotspots for greenhouse gases (GHGs), potentially countering terrestrial carbon sequestration efforts. However, there’s a lack of detailed data on GHG emissions and control from these ditches, and their role in ecosystem carbon budgets. To fill this gap, we conducted comprehensive monitoring of CH4 and CO2 emissions from ditches, rivers and ponds in Qilihai Wetland, a managed Phragmites-dominated Wetland Reserve in Tianjin, China. Our study identified ditches as significant emission hotspots for both CO2 and CH4, emitting CO2 at 2.33 ± 0.71 μmol m−2 h−1, approximately 4.9 and 5.3 times higher than rivers and ponds, respectively. CH4 emissions average 15.53 ± 9.77 μmol m−2 h−1, surpassing those from rivers and ponds by about 2.9 and 2.1 times, respectively. Methane ebullition was identified as a crucial contributor to emitted CH4 from ditches, accounting for a fraction exceeding 70 %. Emissions of CO2 and CH4 in all waters were closely linked to DOC concentration and water temperature (Tw). Both gases increased with higher DOC levels, but while CH4 rose with Tw, CO2 declined. Additionally, CH4 emission was negatively correlated with dissolved oxygen (DO) and the TN/TP (total phosphorus/total nitrogen) ratio. In ditches, it also negatively associated with chlorophyll-a (Chl-a) and positively linked with TP, different from other waters. Despite covering just 19 % of the water area, ditch emissions accounted for 53 % of the entire aquatic CO2 equivalent emissions. The CO2 and CH4 emissions from ditches accounted for 55 % and 37 % of the entire aquatic CO2 equivalent emissions for CO2 and CH4, respectively. Together, they offset 12 % of the net CO2 fixation by vegetation, with ditch CH4 emissions comprising 6 % of the total wetland CH4 emission. This study highlights the substantial role of ditches in carbon emissions within managed Phragmites-dominated wetlands and their responses to environmental changes, providing valuable insights for future wetland management for conservation purposes.
沟渠是管理下的葭萌湿地碳排放的主要参与者
葭萌湿地可吸收二氧化碳 (CO2) 并储存有机物质,是温室气体的吸收汇,但也会从沉积物中排放甲烷 (CH4),造成温室气体排放。以保护区为目的管理的葭萌湿地拥有广泛的排水沟网络,可以成为温室气体(GHGs)的重要排放热点,有可能抵消陆地固碳的努力。然而,关于这些沟渠的温室气体排放和控制,以及它们在生态系统碳预算中的作用,却缺乏详细的数据。为了填补这一空白,我们对中国天津七里海湿地的沟渠、河流和池塘的甲烷和二氧化碳排放进行了全面监测。我们的研究发现,沟渠是二氧化碳和甲烷的重要排放热点,其二氧化碳排放量为 2.33 ± 0.71 μmol m-2 h-1,分别约为河流和池塘的 4.9 倍和 5.3 倍。CH4 排放量平均为 15.53 ± 9.77 μmol m-2 h-1,分别比河流和池塘高出约 2.9 倍和 2.1 倍。甲烷逸出被认为是沟渠排放甲烷的主要原因,所占比例超过 70%。所有水域的二氧化碳和甲烷排放量都与 DOC 浓度和水温密切相关(Tw)。DOC 含量越高,这两种气体的排放量就越高,但随着 Tw 的升高,CH4 的排放量也随之升高,而 CO2 的排放量则有所下降。此外,CH4 排放量与溶解氧 (DO) 和 TN/TP(总磷/总氮)比率呈负相关。在沟渠中,它还与叶绿素 a(Chl-a)呈负相关,与总磷呈正相关,这一点与其他水域不同。尽管沟渠仅占水域面积的 19%,但其排放量却占整个水生二氧化碳当量排放量的 53%。沟渠的二氧化碳和甲烷排放量分别占整个水生二氧化碳和甲烷排放量的 55% 和 37%。两者合计抵消了植被二氧化碳净固定量的 12%,沟渠的甲烷排放量占湿地甲烷总排放量的 6%。这项研究强调了沟渠在以苇草为主的湿地管理范围内的碳排放中的重要作用及其对环境变化的响应,为今后以保护为目的的湿地管理提供了宝贵的见解。
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来源期刊
Journal of Hydrology
Journal of Hydrology 地学-地球科学综合
CiteScore
11.00
自引率
12.50%
发文量
1309
审稿时长
7.5 months
期刊介绍: The Journal of Hydrology publishes original research papers and comprehensive reviews in all the subfields of the hydrological sciences including water based management and policy issues that impact on economics and society. These comprise, but are not limited to the physical, chemical, biogeochemical, stochastic and systems aspects of surface and groundwater hydrology, hydrometeorology and hydrogeology. Relevant topics incorporating the insights and methodologies of disciplines such as climatology, water resource systems, hydraulics, agrohydrology, geomorphology, soil science, instrumentation and remote sensing, civil and environmental engineering are included. Social science perspectives on hydrological problems such as resource and ecological economics, environmental sociology, psychology and behavioural science, management and policy analysis are also invited. Multi-and interdisciplinary analyses of hydrological problems are within scope. The science published in the Journal of Hydrology is relevant to catchment scales rather than exclusively to a local scale or site.
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