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Erosion and sedimentation during the September 2015 flooding of the Kinu River, central Japan.


ABSTRACT: Erosional and sedimentary features associated with flooding have been documented in both modern and past cases. However, only a few studies have demonstrated the relationship between these features and the corresponding hydraulic conditions that produced them, making it difficult to evaluate the magnitude of paleo-flooding. This study describes the characteristics associated with inundation depth and flow direction, as well as the erosional and sedimentary features resulting from the disastrous flooding of the Kinu River, central Japan, in September 2015. Water levels rose rapidly due to heavy rainfall that eventually overtopped, and subsequently breached, a levee in Joso City, causing destructive flooding on the surrounding floodplain. Distinctive erosional features are found next to the breached levee, while depositional features, such as a sandy crevasse-splay deposit are found further away from the breach. The deposit can be divided into three units based on sedimentary facies. The vertical and lateral changes of these sedimentary facies may be the result of temporal and spatial changes associated with flow during the single flooding event. These observations and quantitative data provide information that can be used to reveal the paleohydrology of flood deposits in the stratigraphic record, leading to improved mitigation of future flooding disasters.

SUBMITTER: Dan Matsumoto 

PROVIDER: S-EPMC5039755 | biostudies-literature | 2016 Sep

REPOSITORIES: biostudies-literature

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Erosion and sedimentation during the September 2015 flooding of the Kinu River, central Japan.

Dan Matsumoto   Sawai Yuki Y   Yamada Masaki M   Namegaya Yuichi Y   Shinozaki Tetsuya T   Takeda Daisuke D   Fujino Shigehiro S   Tanigawa Koichiro K   Nakamura Atsunori A   Pilarczyk Jessica E JE  

Scientific reports 20160928


Erosional and sedimentary features associated with flooding have been documented in both modern and past cases. However, only a few studies have demonstrated the relationship between these features and the corresponding hydraulic conditions that produced them, making it difficult to evaluate the magnitude of paleo-flooding. This study describes the characteristics associated with inundation depth and flow direction, as well as the erosional and sedimentary features resulting from the disastrous  ...[more]

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