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监测黄河三角洲受人类活动影响的滩涂动态。

Monitoring tidal flat dynamics affected by human activities along an eroded coast in the Yellow River Delta, China.

机构信息

State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai, 200062, China.

College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, 97331, USA.

出版信息

Environ Monit Assess. 2018 Jun 12;190(7):396. doi: 10.1007/s10661-018-6747-7.

DOI:10.1007/s10661-018-6747-7
PMID:29896719
Abstract

The coast of the northern Yellow River Delta (YRD) has experienced significant erosion since 1976 due to avulsion and consequent lack of sediment supply. Moreover, massive reclamation activity, expansion of the oil industry, and sea-level rise have jointly contributed to the rapid change of tidal flats over recent decades. Therefore, accurate reporting of the coast spatial extent and stability status is urgently required. We presented a method using remotely sensed waterlines to map tidal flats and monitor their spatiotemporal dynamics. The empirical results show that the area of the intertidal zone west of Tiao River Mouth (TRM) appeared to be decreasing. Despite intense hydrodynamic force, the intertidal zone to the east of TRM has expanded due to law prohibiting land reclamation in nature reserve. However, this trend weakened due to the expansion of oil industry after 2007. The movement of the mean high-tide line is the main cause for the increase-decrease patterns of the intertidal zone area. To achieve and maintain land equilibrium in this area, we suggest that a 554-m buffer must be preserved for mean high-tide line retreat. Unfortunately, the shrink crisis of the tidal flats has been extremely severe. Future reclamation and oil projects must be supplemented by studies that evaluate the complexities and dynamics of tidal flats so as to prevent the loss of this unique ecosystem.

摘要

黄河三角洲(YRD)北部沿海自 1976 年以来由于决口和随后缺乏泥沙供应而经历了严重的侵蚀。此外,大规模的开垦活动、石油工业的扩张和海平面上升共同导致了近几十年来潮滩的快速变化。因此,迫切需要准确报告海岸的空间范围和稳定状况。我们提出了一种使用遥感水线来绘制潮滩并监测其时空动态的方法。经验结果表明,条子河口(TRM)以西的潮间带区域似乎在减少。尽管受到强烈的水动力作用,但由于自然保护区禁止开垦土地的法律,TRM 以东的潮间带已经扩大。然而,由于 2007 年后石油工业的扩张,这一趋势有所减弱。平均高潮线的移动是潮间带面积增减模式的主要原因。为了在该地区实现和维持土地平衡,我们建议为平均高潮线后退保留 554 米的缓冲区。不幸的是,潮滩的收缩危机已经极其严重。未来的开垦和石油项目必须辅以评估潮滩复杂性和动态的研究,以防止这一独特生态系统的丧失。

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