[1] 陳瑞遠 (2016),「不同水砂比及渠道坡度對沖積扇型態之影響」,
碩士論文,國立中央大學土木工程研究所,中壢。
[2] 吳侑謙 (2015),「顆粒特性及水流條件對顆粒體運動及淤積型態之
實驗研究」,碩士論文,國立中央大學土木工程研究所,中壢。
[3] 曾文毅 (2014),「不同輸砂濃度及基準水面條件下之沖積扇形態分
析」,碩士論文,國立中央大學土木工程研究所,中壢。
[4] 許乃文 (2013),「直渠道顆粒流之顆粒密度分離效應」,碩士論文,國立中央大學能源工程研究所,中壢。
[5] 吳俊銓 (2012),「山洪濁流形成沖積扇之實驗研究」,碩士論文,國立中央大學土木工程研究所,中壢。
[6] 張瑞津 (1997),「臺灣沖積扇之分布、形態及地形意義」,地質17 卷,1-2 期,69-93.
[7] Bahrami,S. (2012), “Tectonic controls on the morphometry of alluvial
fans around Danehkhoshk anticline,Zagros, Iran”, Geomorphology
180–181 (2013) 217–230.
[8] Canellil,L., Ferrero,A.M., Migliazza,M., and Segalini,A. (2012),
“Debris flow risk mitigation by the means of rigid and flexible barriers
– experimental tests and impact analysis”, Nat. Hazards Earth Syst. Sci.,
12, 1693–1699.
[9] Chant,L., Pease,P. ,Tchakerian,V. (1999), “Modelling alluvial fan
morphology”, Earth Surf. Process. Landforms24, 641-652.
[10] de Hass, T. , Berg ,W.V.G. , Braat, L. , Kleinhans,M.G. , “Autogenic
avulsion, channelization and backfilling dynamics of debris-flow
fans” ,Journal of International Association of Sedimentologists,
2016,1596-1619.
[11] Giles,T.P. (2010), “Investigating the use of alluvial fan volume to
represent fan size in morphometric studies”, Geomorphology 121, 317–
328.
[12] Guerit,L., M´etivier,F., Devauchelle,O., Lajeunesse,E., and
Barrier,L.(2014), “Laboratory alluvial fans in one dimension”, Physical
Review E 90, 022203.
[13] Miller,L.K. , Reitz,M.D., and Jerolmack,D.J. (2014), “Generalized
sorting profile of alluvial fans”, Generalized sorting profile of alluvial
fans, Geophys. Res. Lett., 41, 7191–7199, doi:10.1002/2014GL060991.
[14] Nicholas,A.P., Clarke,L. and Quine,T.A. (2009), “A numerical
modelling and experimental study of flow width dynamics on alluvial
fans” , Earth Surf. Process. Landforms 34, 1985–1993.
[15] Schraml,K., Thomschitz,B., McArdell,B.W., Graf,C., and
Kaitna,R.(2015), “Modeling debris-flow runout patterns on two alpine
fans with different dynamic simulation models”, Nat. Hazards Earth
Syst. Sci., 15, 1483–1492.
[16] Welsh,A., Davies,T. (2010), “Identification of alluvial fans susceptible
to debris-flow hazards”,Landslides ,8:183–194 ,DOI10.1007/s10346-010-0238-4.
[17] Wilford,D.J. , Sakals,M.E. , Innes,J.L. , Sidle,R.C. and
Bergerud,W.A.(2004), “Recognition of debris flow, debris flood and
flood hazard through watershed morphometrics” , Landslides ,1:61–66
DOI 10.1007/s10346-003-0002-0.
[18] Wells,S.G. and Harvey,A.M. (1987), “Sedimentologic and geomorphic
variations in storm-generated alluvial fans, Howgill Fells, northwest
England”,Geological Society of America Bulletin, v. 98, p. 182-198.
[19] Wasklewicz,T. and Scheinert,T. (2016) , “Development and
maintenance of a telescoping debris flow fan in response to
human-induced fan surface channelization, Chalk Creek Valley Natural
Debris Flow Laboratory, Colorado, USA” , Geomorphology 252, 51–65.