| 2 | Recognition of Fluvial Bank Erosion Along the Main Stream of the Yangtze River显示文摘Recognizing the risk of fluvial bank erosion is an important challenge to ensure the early warning and prevention or control of bank collapse in river catchments,including in the Yangtze River.This study introduces a geomorphons-based algorithm to extract river bank erosion information by adjusting the flatness from multibeam echo-sounding data.The algorithm maps ten subaqueous morphological elements,including the slope,footslope,flat,ridge,peak,valley,pit,spur,hollow,and shoulder.Twentyone flatness values were used to build an interpretation strategy for the subaqueous features of riverbank erosion.The results show that the bank scarp,which is the erosion carrier,is covered by slope cells when the flatness is 10°.The scour pits and bank scars are indicated by pit cells near the bank and hollow cells in the bank slope at a flatness of 0°.Fluvial subaqueous dunes are considered an important factor accelerating bank erosion,particularly those near the bank toe;the critical flatness of the dunes was evaluated as 3°.The distribution of subaqueous morphological elements was analyzed and used to map the bank erosion inventory.The analysis results revealed that the near-bank zone,with a relatively large water depth,is prone to form large scour pits and a long bank scarp.Arc collapse tends to occur at the long bank scarp to shorten its length.The varied assignment of flatness values among terrestrial,marine,and fluvial environments is discussed,concluding that diversified flatness values significantly enable fluvial subaqueous morphology recognition.Consequently,this study provides a reference for the flatness-based recognition of fluvial morphological elements and enhances the targeting of subaqueous signs and risks of bank failure with a range of multibeam bathymetric data. | Ge Yan Heqin Cheng Zeyu Jiang Lizhi Teng Ming Tang Tian Shi Yuehua Jiang Guoqiang Yang Quanping Zhou | 2022 | Engineering2022，，12： | 0 |
| 3 | Changes over flood season in turbidity maximum zone in a mountainous macrotidal estuary from 1986 to 2020显示文摘The construction of channel regulation projects,reservoirs,and other human activities have led to significant changes in channel geometry and hydrodynamic conditions in mountainous macrotidal estuaries.However,their impact on the long-term evolution of the turbidity maximum zone(TMZ)in these estuaries is still unclear.Therefore,the Minjiang Estuary(ME)was selected as the study area and using the Gabor filter and surface suspended sediment concentration(SSSC)data retrieved from GF PMS/WFV and Landsat-TM/ETM+/OLI images in the flood season from 1986 to 2020,the flow direction of Chuanshi Waterway,the spatiotemporal evolution characteristics of TMZ in the ME,and the influence of human activities on these were analyzed.The results indicate that during flood tides in the past 35 years,the TMZ was mainly distributed in sections from the Changmen to the Chuanshi and Meihua waterways.The construction of the Shuikou Reservoir caused the SSSC to decrease by 65 mg/L at the Chuanshi Tidal Gauge Station in the ME.The TMZ in the ME waterway channel notably migrated toward the sea due to the waterway regulation project,with the landward and seaward boundaries moving by 2.5 km and 3 km seaward,respectively.The main distribution area moved from Jinpaimen to the section from Chuanshi Waterway to the mouth of the ME.These variation characteristics were basically consistent with the annual average TMZ in the flood season.Through the interactions between nature and human interventions,the flow regime of the ME tended to converge in the flood season.Therefore,human activities have significantly impacted the long-term evolution of the TMZ in the ME. | LIU Ruiqing CHENG Heqin TENG Lizhi FAN Heshan | 2023 | Journal of Geographical Sciences2023，33，5： | 0 |
您所在的机构暂未开通此部分的功能，请联系管理员