基于无人机影像识别冰封水库CH4冒泡分布热点区域
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1:大连理工大学建设工程学院,大连 116024 ;2:长江水利委员会水文局,武汉 430010 ;3:大连理工大学,海岸与海洋工程全国重点实验室,大连 116024 ;4:辽宁省水利水电勘测设计研究院有限责任公司,沈阳 110006 ;5:宁夏回族自治区生态环境监测中心,银川 750002

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10.18307/2025.0652

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国家自然科学基金项目(42077348,42377412)资助


An effective method to identify the distribution of methane ebullition hotspots in ice-covered reservoirs with image data analysis by unmanned aerial vehicle
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1: School of Infrastructure Engineering, Dalian University of Technology, Dalian 116024 , P.R.China ;2: Bureau of Hydrology, Changjiang Water Resources Commission, Wuhan 430010 , P.R.China ;3: State Key Laboratory of Coastal and Offshore Engineering, Dalian University of Technology, Dalian 116024 , P.R.China ;4: Liaoning Water Conservancy and Hydropower Survey and Design Research Institute CO., LTD, Shenyang 110006 , P.R.China ;5: Ningxia Environment Monitoring Center, Yinchuan 750002 , P.R.China

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    摘要:

    冒泡作为湖库等淡水生态系统中温室气体甲烷(CH4)排放的主要方式,具有高度时空异质性。水库库尾浅水区沉积物易产生CH4,并以冒泡的形式释放,但在开放水体中很难捕捉到CH4冒泡的排放热点区域。冰封水库在冰的生长过程中会冻结捕捉由沉积物产生并上浮富含CH4的气泡,在冰面上形成一定规模的“冰封气泡”,这使得基于冰封气泡特征识别CH4冒泡分布热点区域的规模、空间分布成为可能。本研究以我国东北地区大型水库——东风水库为调查对象,基于冬季水库冰面的无人机影像与现场冰封气泡特征调查,结合面向对象的图像分析,构建了冰封气泡影像提取分割方法,利用空间自相关分析探究冰封气泡空间分布模式,识别冰封气泡聚集的热点区域。研究结果表明:(1)东风水库库尾冰封气泡直径范围为1~10 cm,无人机15 m飞行高度空间分辨率为0.4 cm,能够满足识别冰封气泡的质量要求;形态学顶帽变换方法能够有效改善光照不均的图像,显著提高正射影像图片资料的合成质量。(2)利用气泡、冰裂纹在长宽比、亮度、密度等特征值的差异性能够进行冰封气泡的有效提取分类,受调查的3个气泡区分类总体提取精度均为0.8以上,显示了较高的冰封气泡提取效果。(3)3个冰封气泡密集区域总气泡面积占库尾总面积的0.24%,3个区域内部共10个调查样带的气泡面积占比分布范围为2.6%~7.8%。冰封气泡空间分布均呈现显著的聚集模式,被划分为冒泡分布热点区域占库尾总面积的0.9%,说明在整个水库范围内,CH4冒泡热点可能仅存在于有限的区域内。研究成果对揭示湖库甲烷排放热点区域分布特征具有重要指示意义。

    Abstract:

    Ebullition is the primary pathway for methane (CH4) emissions from freshwater ecosystems such as lakes and reservoirs, yet it always exhibits significant spatiotemporal variability. In shallow zones near reservoir inlets, CH4 is often generated in the sediments and released as bubbles. However, capturing the ebullition hotspots in open water bodies remains a challenge. During the ice-covered season, bubbles rich in CH4 are trapped and preserved as “ice-encased bubbles” within the growing ice layer. This natural phenomenon provides an opportunity to identify CH4 ebullition hotspots based on the characteristics and spatial patterns of ice bubbles. This study focuses on the Dongfeng Reservoir, a large reservoir in northeastern China. Using high-resolution unmanned aerial vehicle (UAV) imagery of the winter ice surface and in-situ measurements of ice bubbles, we developed an object-based image analysis method for bubble segmentation and extraction. Spatial autocorrelation analysis was employed to investigate the distribution patterns of ice bubbles and to identify CH4 ebullition hotspot areas. The important findings include: (1) The diameters of ice bubbles in Dongfeng Reservoir ranged from 1 cm to 10 cm. UAV imagery captured at 15 m altitude achieved a spatial resolution of 0.4 cm, sufficient for high-quality bubble identification. A morphological top-hat transformation effectively corrected uneven illumination and enhanced the quality of digital orthophoto mosaics. (2) Differences in shape attributes, brightness, and density allowed for effective classification of bubbles and ice cracks, with the overall classification accuracy exceeding 0.8 across three investigated regions, demonstrating robust extraction performance. (3) The total bubble area in the three dense bubble regions accounted for 0.24% of the reservoir inlet area. Within these regions, the bubble area ratio along ten surveyed transects ranged from 2.6% to 7.8%. Spatial autocorrelation analysis revealed significant clustering of ice-encased bubbles, with CH4 ebullition hotspots occupying only 0.9% of the reservoir inlet area. The results indicate that CH4 ebullition may be concentrated in the limited regions across the reservoir. These findings provide important insights into the spatial distribution characteristics of methane emission hotspots in lakes and reservoirs.

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胡天超,金业,陈小强,金亢,孙源,李志军,许士国.基于无人机影像识别冰封水库CH4冒泡分布热点区域.湖泊科学,2025,37(6):2132-2145. DOI:10.18307/2025.0652

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  • 收稿日期:2024-06-12
  • 最后修改日期:2025-01-12
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  • 在线发布日期: 2025-11-03
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