塔里木盆地和田河汇流区的平面形态演变

魏豪; 李嘉光; 谭虎成

doi:10.3799/dqkx.2022.413

Volume 48 Issue 1

Jan. 2023

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Wei Hao, Li Jiaguang, Tan Hucheng, 2023. Channel Morphological Evolution in Confluence Area of Hotan River in Tarim Basin. Earth Science, 48(1): 359-374. doi: 10.3799/dqkx.2022.413

Citation:

Wei Hao, Li Jiaguang, Tan Hucheng, 2023. Channel Morphological Evolution in Confluence Area of Hotan River in Tarim Basin. Earth Science, 48(1): 359-374. doi: 10.3799/dqkx.2022.413

Wei Hao, Li Jiaguang, Tan Hucheng, 2023. Channel Morphological Evolution in Confluence Area of Hotan River in Tarim Basin. Earth Science, 48(1): 359-374. doi: 10.3799/dqkx.2022.413

Citation:

Wei Hao, Li Jiaguang, Tan Hucheng, 2023. Channel Morphological Evolution in Confluence Area of Hotan River in Tarim Basin. Earth Science, 48(1): 359-374. doi: 10.3799/dqkx.2022.413

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Channel Morphological Evolution in Confluence Area of Hotan River in Tarim Basin

doi: 10.3799/dqkx.2022.413

Wei Hao^{1, 2
,
,},
Li Jiaguang^{1, 2
,
,},
Tan Hucheng¹

1.
Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, China University of Geosciences, Wuhan 430074, China
2.
Key Laboratory of Theory and Technology of Petroleum Exploration and Development in Hubei Province, Wuhan 430074, China

Received Date: 2022-06-30
Available Online: 2023-02-01
Publish Date: 2023-01-25

Abstract

Abstract

River confluence has a great potential of hydrocarbon reservoirs owing to wide and thick channel-fill deposits by widening and deepening effects. The Mesozoic and Cenozoic hydrocarbon-bearing basins in China are internally drainage basins dominated and fluvial deposits are widely regarded as important hydrocarbon. The (semi-) arid regions cover 41% of the global continental areas, and river systems are widely distributed with substantial ecological resources. However, current research on river confluence is mainly focused on humid regions, and research on the channel morphology of river confluence in drylands and their controls has been rarely reported. In this study, we select the confluence (Kalakashen River and Yulongkashen River) of the Hotan River in Tarim Basin as study area. Firstly, the combination of Digital Elevation Model (DEM) and high-resolution Google Earth images were used to identify the bankfull boundaries of all river channels. Subsequently the evolution of river planform in the confluence area was analyzed using hydrological data and time-series remote sensing images. Results show that the confluence of Hotan River is a fixed and "Y" type confluence, and their junctions have different river types: Kalakashen River is meandering while Yulongkashen River is meandering-braided transitional. Cutoffs occurred along these junctions. The confluence is transformed into braided river, and its bankfull width increases by 58% (505 m wider) compared with that of junctions. Furthermore, we select 23 river confluences in typical semi-arid-arid regions (n= 10) and humid regions (n=13) around the world to investigate the changes in bankfull width from junctions to confluences. Results reveal that the increase (> 50%) in bankfull widths of river confluence in drylands with (non-) sparse vegetation greatly exceeded that (17%) of river confluence in humid areas with riparian vegetation. Slopes (2‰) of these selected dryland rivers (lack of riparian vegetation) are on average one category higher than those (0.6‰) in humid regions. Therefore, lack of riparian vegetation and high slope of river profiles are the main controls for significant widening in river confluences of dryland regions. Our results not only complement the models of river confluence, but also provide a basis for the further research of sedimentary processes and their sedimentary model in dryland river confluence.
- Hotan River,
- channel confluence,
- river type evolution,
- bankfull width,
- sedimentology

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Channel Morphological Evolution in Confluence Area of Hotan River in Tarim Basin

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