### 抄録

As a two-phase anisotropic mixture, debris flowshows some complex fluid-dynamical characteristics on its motion behavior, which makes it difficult to be modelled or simulated through standard approaches. Consequently, Cellular Automaton (CA) model in the field of parallel computing, which has long been verified as efficiently applying in the simulation of complex natural process, are recently introduced to simulate flow-type phenomena. In this paper, the components of CA model for debris-flow simulation are reviewed, after that a two-dimensional cellular space is generated from the Digital Terrain Model (DTM) with 2.5m high-resolution, and the relationship of lattices in the space is defined as Moore neighborhood type. A new transition function, aiming at flow direction determination, is proposed through the way that implementing the debris-flow inertial influence into the traditional topography-based D8 algorithm, by a multiplying equation or an addition equation. We also present a three-step propagation algorithm to integrate the single flow routines, then use the constant discharge model to assign the flow depth to each routine, in this way the propagation area can be gradually delineated through each increment step. We test the developed model with CH87 Brichboden debris-flow event, and illustrate its application withYohutagawa debris-flow event in Japan, 2010. Results of both cases show that a more accurate propagation perimeter pattern is observed using addition equation in the modified flow direction algorithm, comparing to the traditional D8 algorithm and multiplying equation-based algorithm.

元の言語 | 英語 |
---|---|

ホスト出版物のタイトル | Geomechanics from Micro to Macro - Proceedings of the TC105 ISSMGE International Symposium on Geomechanics from Micro to Macro, IS-Cambridge 2014 |

出版者 | Taylor and Francis - Balkema |

ページ | 983-988 |

ページ数 | 6 |

ISBN（印刷物） | 9781138027077 |

出版物ステータス | 出版済み - 1 1 2015 |

イベント | International Symposium on Geomechanics from Micro to Macro, IS-Cambridge 2014 - Cambridge, 英国 継続期間: 9 1 2014 → 9 3 2014 |

### 出版物シリーズ

名前 | Geomechanics from Micro to Macro - Proceedings of the TC105 ISSMGE International Symposium on Geomechanics from Micro to Macro, IS-Cambridge 2014 |
---|---|

巻 | 2 |

### その他

その他 | International Symposium on Geomechanics from Micro to Macro, IS-Cambridge 2014 |
---|---|

国 | 英国 |

市 | Cambridge |

期間 | 9/1/14 → 9/3/14 |

### Fingerprint

### All Science Journal Classification (ASJC) codes

- Geophysics

### これを引用

*Geomechanics from Micro to Macro - Proceedings of the TC105 ISSMGE International Symposium on Geomechanics from Micro to Macro, IS-Cambridge 2014*(pp. 983-988). (Geomechanics from Micro to Macro - Proceedings of the TC105 ISSMGE International Symposium on Geomechanics from Micro to Macro, IS-Cambridge 2014; 巻数 2). Taylor and Francis - Balkema.

**Development of the cellular automaton model for simulating the propagation extent of debris flow at the alluvial fan : A case study of Yohutagawa, Japan.** / Han, Z.; Chen, Guangqi; Li, Y.; Zhang, H.; Fan, F.; Jing, P.; Wang, W.; Zhou, S.; Xu, L.; Chen, S.

研究成果: 著書/レポートタイプへの貢献 › 会議での発言

*Geomechanics from Micro to Macro - Proceedings of the TC105 ISSMGE International Symposium on Geomechanics from Micro to Macro, IS-Cambridge 2014.*Geomechanics from Micro to Macro - Proceedings of the TC105 ISSMGE International Symposium on Geomechanics from Micro to Macro, IS-Cambridge 2014, 巻. 2, Taylor and Francis - Balkema, pp. 983-988, International Symposium on Geomechanics from Micro to Macro, IS-Cambridge 2014, Cambridge, 英国, 9/1/14.

}

TY - GEN

T1 - Development of the cellular automaton model for simulating the propagation extent of debris flow at the alluvial fan

T2 - A case study of Yohutagawa, Japan

AU - Han, Z.

AU - Chen, Guangqi

AU - Li, Y.

AU - Zhang, H.

AU - Fan, F.

AU - Jing, P.

AU - Wang, W.

AU - Zhou, S.

AU - Xu, L.

AU - Chen, S.

PY - 2015/1/1

Y1 - 2015/1/1

N2 - As a two-phase anisotropic mixture, debris flowshows some complex fluid-dynamical characteristics on its motion behavior, which makes it difficult to be modelled or simulated through standard approaches. Consequently, Cellular Automaton (CA) model in the field of parallel computing, which has long been verified as efficiently applying in the simulation of complex natural process, are recently introduced to simulate flow-type phenomena. In this paper, the components of CA model for debris-flow simulation are reviewed, after that a two-dimensional cellular space is generated from the Digital Terrain Model (DTM) with 2.5m high-resolution, and the relationship of lattices in the space is defined as Moore neighborhood type. A new transition function, aiming at flow direction determination, is proposed through the way that implementing the debris-flow inertial influence into the traditional topography-based D8 algorithm, by a multiplying equation or an addition equation. We also present a three-step propagation algorithm to integrate the single flow routines, then use the constant discharge model to assign the flow depth to each routine, in this way the propagation area can be gradually delineated through each increment step. We test the developed model with CH87 Brichboden debris-flow event, and illustrate its application withYohutagawa debris-flow event in Japan, 2010. Results of both cases show that a more accurate propagation perimeter pattern is observed using addition equation in the modified flow direction algorithm, comparing to the traditional D8 algorithm and multiplying equation-based algorithm.

AB - As a two-phase anisotropic mixture, debris flowshows some complex fluid-dynamical characteristics on its motion behavior, which makes it difficult to be modelled or simulated through standard approaches. Consequently, Cellular Automaton (CA) model in the field of parallel computing, which has long been verified as efficiently applying in the simulation of complex natural process, are recently introduced to simulate flow-type phenomena. In this paper, the components of CA model for debris-flow simulation are reviewed, after that a two-dimensional cellular space is generated from the Digital Terrain Model (DTM) with 2.5m high-resolution, and the relationship of lattices in the space is defined as Moore neighborhood type. A new transition function, aiming at flow direction determination, is proposed through the way that implementing the debris-flow inertial influence into the traditional topography-based D8 algorithm, by a multiplying equation or an addition equation. We also present a three-step propagation algorithm to integrate the single flow routines, then use the constant discharge model to assign the flow depth to each routine, in this way the propagation area can be gradually delineated through each increment step. We test the developed model with CH87 Brichboden debris-flow event, and illustrate its application withYohutagawa debris-flow event in Japan, 2010. Results of both cases show that a more accurate propagation perimeter pattern is observed using addition equation in the modified flow direction algorithm, comparing to the traditional D8 algorithm and multiplying equation-based algorithm.

UR - http://www.scopus.com/inward/record.url?scp=84907362743&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=84907362743&partnerID=8YFLogxK

M3 - Conference contribution

AN - SCOPUS:84907362743

SN - 9781138027077

T3 - Geomechanics from Micro to Macro - Proceedings of the TC105 ISSMGE International Symposium on Geomechanics from Micro to Macro, IS-Cambridge 2014

SP - 983

EP - 988

BT - Geomechanics from Micro to Macro - Proceedings of the TC105 ISSMGE International Symposium on Geomechanics from Micro to Macro, IS-Cambridge 2014

PB - Taylor and Francis - Balkema

ER -