DOU Ming1,2, CAO Yingshu1, MI Qingbin1, DING Junxiang2, WANG Han1, PAN Deng3
Abstract:
The wetland area between Huayuankou and Jiahetan in the lower reaches of the Yellow River is a vital component of the Yellow River corridor ecosystem. Its formation, evolution, and degradation are closely linked to the unique variations in the river′s water and sediment dynamics.To clarify the evolution characteristics of different types of wetland landscape patterns in this section and their response mechanisms to changes in water and sediment elements such as runoff, sediment transport volume and water level, in this study the section of the Yellow River from Huayuankou to Jiahetan was examined. Utilizing 12 phases of Landsat satellite imagery from 1994 to 2023, a wetland landscape database was constructed. The study employed land use transfer matrices and landscape pattern index methods to quantitatively analyze the spatiotemporal changes in wetland types, patch characteristics, and landscape structure.Subsequently, by integrating the flow, water level, sediment concentration and other data from the Huayuankou station, the response relationship between the landscape pattern characteristics of different types of wetlands and water and sediment elements was highlighted.The results indicated that: ①From 1994 to 2023, the runoff at the Huayuankou Station showed an upward trend, while sediment discharge and water levels exhibited an overall downward trend.②The areas of wetland types such as rivers, ponds, mudflats, and wild grasslands in the study area showed an overall shrinking trend, with an average annual reduction of 5.90 km2. The most significant transformation was the conversion of wetlands into farmland. ③At the landscape level, following the implementation of the water and sediment regulation policy, the overall connectivity of wetland landscapes improved, while landscape richness and evenness increased and tended to stabilize. ④In pond wetlands, mudflat wetlands, and wild grassland wetlands, indices such as the largest patch index, mean patch area, and contagion index showed significant correlations with sediment discharge and water level at the Huayuankou Station, with a particularly stronger correlation with sediment discharge. The findings of this study provided a theoretical basis for wetland ecological protection and restoration in the Yellow River Basin.