The depositional evolution and internal sedimentary architecture of a flood event-dominated experimental alluvial fan
Abstract In this article, based on a flume tank experiment, we attempt to provide some key insights to the depositional process and geomorphological evolution of an experimental alluvial fan dominated by flood events. In the experiment, all boundary conditions were kept constant besides the sediment...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Feng, Wenjie [verfasserIn] Wu, Shenghe [verfasserIn] Liu, Junling [verfasserIn] Zhang, Changmin [verfasserIn] Yin, Yanshu [verfasserIn] Yin, Taiju [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2019 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Arabian journal of geosciences - Berlin : Springer, 2008, 12(2019), 9 vom: 23. Apr. |
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| Übergeordnetes Werk: |
volume:12 ; year:2019 ; number:9 ; day:23 ; month:04 |
| Links: |
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| DOI / URN: |
10.1007/s12517-019-4468-z |
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| Katalog-ID: |
SPR025983164 |
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| 100 | 1 | |a Feng, Wenjie |e verfasserin |4 aut | |
| 245 | 1 | 4 | |a The depositional evolution and internal sedimentary architecture of a flood event-dominated experimental alluvial fan |
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| 520 | |a Abstract In this article, based on a flume tank experiment, we attempt to provide some key insights to the depositional process and geomorphological evolution of an experimental alluvial fan dominated by flood events. In the experiment, all boundary conditions were kept constant besides the sediment and water supply in each flood event. The experimental fan formed after 12 flood events. The elevation at the observation points was measured and the geomorphology evolution during the whole experiment was recorded by time-lapsed digital images. It is showed that the depositional process of the experimental fan could be subdivided into three stages, including the sheet flood-dominated stage, the unconfined channel-dominated stage, and the confined channel-dominated stage. The spontaneous evolution of the experimental fan was indicated to be controlled by the continuously occupation of the accommodation space and resulted in the three-layer sedimentary architecture. With the growth of this experimental fan, the increasing rate of fan area and the vertically aggradational rate decreased. Meanwhile, the roughness of the fan edge changed from rapid fluctuation to gradually decrease. | ||
| 650 | 4 | |a Flood event-dominated alluvial fan |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Autogenic |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Flume experiment |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Depositional evolution |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Sedimentary architecture |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Geomorphology |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Wu, Shenghe |e verfasserin |4 aut | |
| 700 | 1 | |a Liu, Junling |e verfasserin |4 aut | |
| 700 | 1 | |a Zhang, Changmin |e verfasserin |4 aut | |
| 700 | 1 | |a Yin, Yanshu |e verfasserin |4 aut | |
| 700 | 1 | |a Yin, Taiju |e verfasserin |4 aut | |
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10.1007/s12517-019-4468-z doi (DE-627)SPR025983164 (SPR)s12517-019-4468-z-e DE-627 ger DE-627 rakwb eng 550 ASE Feng, Wenjie verfasserin aut The depositional evolution and internal sedimentary architecture of a flood event-dominated experimental alluvial fan 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract In this article, based on a flume tank experiment, we attempt to provide some key insights to the depositional process and geomorphological evolution of an experimental alluvial fan dominated by flood events. In the experiment, all boundary conditions were kept constant besides the sediment and water supply in each flood event. The experimental fan formed after 12 flood events. The elevation at the observation points was measured and the geomorphology evolution during the whole experiment was recorded by time-lapsed digital images. It is showed that the depositional process of the experimental fan could be subdivided into three stages, including the sheet flood-dominated stage, the unconfined channel-dominated stage, and the confined channel-dominated stage. The spontaneous evolution of the experimental fan was indicated to be controlled by the continuously occupation of the accommodation space and resulted in the three-layer sedimentary architecture. With the growth of this experimental fan, the increasing rate of fan area and the vertically aggradational rate decreased. Meanwhile, the roughness of the fan edge changed from rapid fluctuation to gradually decrease. Flood event-dominated alluvial fan (dpeaa)DE-He213 Autogenic (dpeaa)DE-He213 Flume experiment (dpeaa)DE-He213 Depositional evolution (dpeaa)DE-He213 Sedimentary architecture (dpeaa)DE-He213 Geomorphology (dpeaa)DE-He213 Wu, Shenghe verfasserin aut Liu, Junling verfasserin aut Zhang, Changmin verfasserin aut Yin, Yanshu verfasserin aut Yin, Taiju verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 12(2019), 9 vom: 23. Apr. (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:12 year:2019 number:9 day:23 month:04 https://dx.doi.org/10.1007/s12517-019-4468-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 12 2019 9 23 04 |
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10.1007/s12517-019-4468-z doi (DE-627)SPR025983164 (SPR)s12517-019-4468-z-e DE-627 ger DE-627 rakwb eng 550 ASE Feng, Wenjie verfasserin aut The depositional evolution and internal sedimentary architecture of a flood event-dominated experimental alluvial fan 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract In this article, based on a flume tank experiment, we attempt to provide some key insights to the depositional process and geomorphological evolution of an experimental alluvial fan dominated by flood events. In the experiment, all boundary conditions were kept constant besides the sediment and water supply in each flood event. The experimental fan formed after 12 flood events. The elevation at the observation points was measured and the geomorphology evolution during the whole experiment was recorded by time-lapsed digital images. It is showed that the depositional process of the experimental fan could be subdivided into three stages, including the sheet flood-dominated stage, the unconfined channel-dominated stage, and the confined channel-dominated stage. The spontaneous evolution of the experimental fan was indicated to be controlled by the continuously occupation of the accommodation space and resulted in the three-layer sedimentary architecture. With the growth of this experimental fan, the increasing rate of fan area and the vertically aggradational rate decreased. Meanwhile, the roughness of the fan edge changed from rapid fluctuation to gradually decrease. Flood event-dominated alluvial fan (dpeaa)DE-He213 Autogenic (dpeaa)DE-He213 Flume experiment (dpeaa)DE-He213 Depositional evolution (dpeaa)DE-He213 Sedimentary architecture (dpeaa)DE-He213 Geomorphology (dpeaa)DE-He213 Wu, Shenghe verfasserin aut Liu, Junling verfasserin aut Zhang, Changmin verfasserin aut Yin, Yanshu verfasserin aut Yin, Taiju verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 12(2019), 9 vom: 23. Apr. (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:12 year:2019 number:9 day:23 month:04 https://dx.doi.org/10.1007/s12517-019-4468-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 12 2019 9 23 04 |
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10.1007/s12517-019-4468-z doi (DE-627)SPR025983164 (SPR)s12517-019-4468-z-e DE-627 ger DE-627 rakwb eng 550 ASE Feng, Wenjie verfasserin aut The depositional evolution and internal sedimentary architecture of a flood event-dominated experimental alluvial fan 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract In this article, based on a flume tank experiment, we attempt to provide some key insights to the depositional process and geomorphological evolution of an experimental alluvial fan dominated by flood events. In the experiment, all boundary conditions were kept constant besides the sediment and water supply in each flood event. The experimental fan formed after 12 flood events. The elevation at the observation points was measured and the geomorphology evolution during the whole experiment was recorded by time-lapsed digital images. It is showed that the depositional process of the experimental fan could be subdivided into three stages, including the sheet flood-dominated stage, the unconfined channel-dominated stage, and the confined channel-dominated stage. The spontaneous evolution of the experimental fan was indicated to be controlled by the continuously occupation of the accommodation space and resulted in the three-layer sedimentary architecture. With the growth of this experimental fan, the increasing rate of fan area and the vertically aggradational rate decreased. Meanwhile, the roughness of the fan edge changed from rapid fluctuation to gradually decrease. Flood event-dominated alluvial fan (dpeaa)DE-He213 Autogenic (dpeaa)DE-He213 Flume experiment (dpeaa)DE-He213 Depositional evolution (dpeaa)DE-He213 Sedimentary architecture (dpeaa)DE-He213 Geomorphology (dpeaa)DE-He213 Wu, Shenghe verfasserin aut Liu, Junling verfasserin aut Zhang, Changmin verfasserin aut Yin, Yanshu verfasserin aut Yin, Taiju verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 12(2019), 9 vom: 23. Apr. (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:12 year:2019 number:9 day:23 month:04 https://dx.doi.org/10.1007/s12517-019-4468-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 12 2019 9 23 04 |
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10.1007/s12517-019-4468-z doi (DE-627)SPR025983164 (SPR)s12517-019-4468-z-e DE-627 ger DE-627 rakwb eng 550 ASE Feng, Wenjie verfasserin aut The depositional evolution and internal sedimentary architecture of a flood event-dominated experimental alluvial fan 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract In this article, based on a flume tank experiment, we attempt to provide some key insights to the depositional process and geomorphological evolution of an experimental alluvial fan dominated by flood events. In the experiment, all boundary conditions were kept constant besides the sediment and water supply in each flood event. The experimental fan formed after 12 flood events. The elevation at the observation points was measured and the geomorphology evolution during the whole experiment was recorded by time-lapsed digital images. It is showed that the depositional process of the experimental fan could be subdivided into three stages, including the sheet flood-dominated stage, the unconfined channel-dominated stage, and the confined channel-dominated stage. The spontaneous evolution of the experimental fan was indicated to be controlled by the continuously occupation of the accommodation space and resulted in the three-layer sedimentary architecture. With the growth of this experimental fan, the increasing rate of fan area and the vertically aggradational rate decreased. Meanwhile, the roughness of the fan edge changed from rapid fluctuation to gradually decrease. Flood event-dominated alluvial fan (dpeaa)DE-He213 Autogenic (dpeaa)DE-He213 Flume experiment (dpeaa)DE-He213 Depositional evolution (dpeaa)DE-He213 Sedimentary architecture (dpeaa)DE-He213 Geomorphology (dpeaa)DE-He213 Wu, Shenghe verfasserin aut Liu, Junling verfasserin aut Zhang, Changmin verfasserin aut Yin, Yanshu verfasserin aut Yin, Taiju verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 12(2019), 9 vom: 23. Apr. (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:12 year:2019 number:9 day:23 month:04 https://dx.doi.org/10.1007/s12517-019-4468-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 12 2019 9 23 04 |
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10.1007/s12517-019-4468-z doi (DE-627)SPR025983164 (SPR)s12517-019-4468-z-e DE-627 ger DE-627 rakwb eng 550 ASE Feng, Wenjie verfasserin aut The depositional evolution and internal sedimentary architecture of a flood event-dominated experimental alluvial fan 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract In this article, based on a flume tank experiment, we attempt to provide some key insights to the depositional process and geomorphological evolution of an experimental alluvial fan dominated by flood events. In the experiment, all boundary conditions were kept constant besides the sediment and water supply in each flood event. The experimental fan formed after 12 flood events. The elevation at the observation points was measured and the geomorphology evolution during the whole experiment was recorded by time-lapsed digital images. It is showed that the depositional process of the experimental fan could be subdivided into three stages, including the sheet flood-dominated stage, the unconfined channel-dominated stage, and the confined channel-dominated stage. The spontaneous evolution of the experimental fan was indicated to be controlled by the continuously occupation of the accommodation space and resulted in the three-layer sedimentary architecture. With the growth of this experimental fan, the increasing rate of fan area and the vertically aggradational rate decreased. Meanwhile, the roughness of the fan edge changed from rapid fluctuation to gradually decrease. Flood event-dominated alluvial fan (dpeaa)DE-He213 Autogenic (dpeaa)DE-He213 Flume experiment (dpeaa)DE-He213 Depositional evolution (dpeaa)DE-He213 Sedimentary architecture (dpeaa)DE-He213 Geomorphology (dpeaa)DE-He213 Wu, Shenghe verfasserin aut Liu, Junling verfasserin aut Zhang, Changmin verfasserin aut Yin, Yanshu verfasserin aut Yin, Taiju verfasserin aut Enthalten in Arabian journal of geosciences Berlin : Springer, 2008 12(2019), 9 vom: 23. Apr. (DE-627)572421877 (DE-600)2438771-X 1866-7538 nnns volume:12 year:2019 number:9 day:23 month:04 https://dx.doi.org/10.1007/s12517-019-4468-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 12 2019 9 23 04 |
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Enthalten in Arabian journal of geosciences 12(2019), 9 vom: 23. Apr. volume:12 year:2019 number:9 day:23 month:04 |
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Flood event-dominated alluvial fan Autogenic Flume experiment Depositional evolution Sedimentary architecture Geomorphology |
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Arabian journal of geosciences |
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Feng, Wenjie @@aut@@ Wu, Shenghe @@aut@@ Liu, Junling @@aut@@ Zhang, Changmin @@aut@@ Yin, Yanshu @@aut@@ Yin, Taiju @@aut@@ |
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2019-04-23T00:00:00Z |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR025983164</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20220111132221.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201007s2019 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s12517-019-4468-z</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR025983164</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s12517-019-4468-z-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">ASE</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Feng, Wenjie</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="4"><subfield code="a">The depositional evolution and internal sedimentary architecture of a flood event-dominated experimental alluvial fan</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2019</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract In this article, based on a flume tank experiment, we attempt to provide some key insights to the depositional process and geomorphological evolution of an experimental alluvial fan dominated by flood events. In the experiment, all boundary conditions were kept constant besides the sediment and water supply in each flood event. The experimental fan formed after 12 flood events. The elevation at the observation points was measured and the geomorphology evolution during the whole experiment was recorded by time-lapsed digital images. It is showed that the depositional process of the experimental fan could be subdivided into three stages, including the sheet flood-dominated stage, the unconfined channel-dominated stage, and the confined channel-dominated stage. The spontaneous evolution of the experimental fan was indicated to be controlled by the continuously occupation of the accommodation space and resulted in the three-layer sedimentary architecture. With the growth of this experimental fan, the increasing rate of fan area and the vertically aggradational rate decreased. 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Feng, Wenjie |
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Feng, Wenjie ddc 550 misc Flood event-dominated alluvial fan misc Autogenic misc Flume experiment misc Depositional evolution misc Sedimentary architecture misc Geomorphology The depositional evolution and internal sedimentary architecture of a flood event-dominated experimental alluvial fan |
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550 ASE The depositional evolution and internal sedimentary architecture of a flood event-dominated experimental alluvial fan Flood event-dominated alluvial fan (dpeaa)DE-He213 Autogenic (dpeaa)DE-He213 Flume experiment (dpeaa)DE-He213 Depositional evolution (dpeaa)DE-He213 Sedimentary architecture (dpeaa)DE-He213 Geomorphology (dpeaa)DE-He213 |
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ddc 550 misc Flood event-dominated alluvial fan misc Autogenic misc Flume experiment misc Depositional evolution misc Sedimentary architecture misc Geomorphology |
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ddc 550 misc Flood event-dominated alluvial fan misc Autogenic misc Flume experiment misc Depositional evolution misc Sedimentary architecture misc Geomorphology |
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The depositional evolution and internal sedimentary architecture of a flood event-dominated experimental alluvial fan |
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The depositional evolution and internal sedimentary architecture of a flood event-dominated experimental alluvial fan |
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Feng, Wenjie Wu, Shenghe Liu, Junling Zhang, Changmin Yin, Yanshu Yin, Taiju |
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depositional evolution and internal sedimentary architecture of a flood event-dominated experimental alluvial fan |
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The depositional evolution and internal sedimentary architecture of a flood event-dominated experimental alluvial fan |
| abstract |
Abstract In this article, based on a flume tank experiment, we attempt to provide some key insights to the depositional process and geomorphological evolution of an experimental alluvial fan dominated by flood events. In the experiment, all boundary conditions were kept constant besides the sediment and water supply in each flood event. The experimental fan formed after 12 flood events. The elevation at the observation points was measured and the geomorphology evolution during the whole experiment was recorded by time-lapsed digital images. It is showed that the depositional process of the experimental fan could be subdivided into three stages, including the sheet flood-dominated stage, the unconfined channel-dominated stage, and the confined channel-dominated stage. The spontaneous evolution of the experimental fan was indicated to be controlled by the continuously occupation of the accommodation space and resulted in the three-layer sedimentary architecture. With the growth of this experimental fan, the increasing rate of fan area and the vertically aggradational rate decreased. Meanwhile, the roughness of the fan edge changed from rapid fluctuation to gradually decrease. |
| abstractGer |
Abstract In this article, based on a flume tank experiment, we attempt to provide some key insights to the depositional process and geomorphological evolution of an experimental alluvial fan dominated by flood events. In the experiment, all boundary conditions were kept constant besides the sediment and water supply in each flood event. The experimental fan formed after 12 flood events. The elevation at the observation points was measured and the geomorphology evolution during the whole experiment was recorded by time-lapsed digital images. It is showed that the depositional process of the experimental fan could be subdivided into three stages, including the sheet flood-dominated stage, the unconfined channel-dominated stage, and the confined channel-dominated stage. The spontaneous evolution of the experimental fan was indicated to be controlled by the continuously occupation of the accommodation space and resulted in the three-layer sedimentary architecture. With the growth of this experimental fan, the increasing rate of fan area and the vertically aggradational rate decreased. Meanwhile, the roughness of the fan edge changed from rapid fluctuation to gradually decrease. |
| abstract_unstemmed |
Abstract In this article, based on a flume tank experiment, we attempt to provide some key insights to the depositional process and geomorphological evolution of an experimental alluvial fan dominated by flood events. In the experiment, all boundary conditions were kept constant besides the sediment and water supply in each flood event. The experimental fan formed after 12 flood events. The elevation at the observation points was measured and the geomorphology evolution during the whole experiment was recorded by time-lapsed digital images. It is showed that the depositional process of the experimental fan could be subdivided into three stages, including the sheet flood-dominated stage, the unconfined channel-dominated stage, and the confined channel-dominated stage. The spontaneous evolution of the experimental fan was indicated to be controlled by the continuously occupation of the accommodation space and resulted in the three-layer sedimentary architecture. With the growth of this experimental fan, the increasing rate of fan area and the vertically aggradational rate decreased. Meanwhile, the roughness of the fan edge changed from rapid fluctuation to gradually decrease. |
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9 |
| title_short |
The depositional evolution and internal sedimentary architecture of a flood event-dominated experimental alluvial fan |
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https://dx.doi.org/10.1007/s12517-019-4468-z |
| remote_bool |
true |
| author2 |
Wu, Shenghe Liu, Junling Zhang, Changmin Yin, Yanshu Yin, Taiju |
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Wu, Shenghe Liu, Junling Zhang, Changmin Yin, Yanshu Yin, Taiju |
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| doi_str |
10.1007/s12517-019-4468-z |
| up_date |
2024-07-03T18:09:41.206Z |
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| score |
7.397977 |