報告人 : 黃璿宇 俞佳成 報告日期 : 101/11/23
DESCRIPTION
Impact of rainstorm-triggered landslides on high turbidity in a mountain reservoir Lin, G. W., Chen, H., Petley, D. N., Horng, M. J., Wu, S. J., Chuang, B., 2010. Impact of rainstorm-triggered landslides on high turbidity in a mountain reservoir. Engineering Geology. 報告人 : 黃璿宇 俞佳成 - PowerPoint PPT PresentationTRANSCRIPT
Impact of rainstorm-triggered Impact of rainstorm-triggered landslides on high turbidity in a landslides on high turbidity in a
mountain reservoirmountain reservoir
Lin, G. W., Chen, H., Petley, D. N., Horng, M. J., Wu, S. J., Chuang, B., 2010. Impact of rainstorm-triggered landslides on high turbidity in a mountain reservoir.
Engineering Geology.
報告人 : 黃璿宇 俞佳成報告日期 :101/11/23
Outline
1
Introduction
• Landslide is the key influence on sediment delivery in upland river catchments, which controls both amount and characteristics of sediment released. (Al-Sheriadeh et al., 2000; Korup et al., 2004; Johnson et al., 2008)
• Landslide is also increasingly considered as a primary factor dominating the turbidity of rivers and reservoirs. (Jordan, 2006; Sobieszczyk et al., 2007)
2
Introduction
• Several studies indicate that much of the sediment produced in upper basins often does not immediately migrate downstream but is instead deposited in the riverbed, resulting in channel aggradation. (Kasai et al., 2004; Koi et al., 2008)
3
Study area – GeographicalGeographical
http://www.wranb.gov.tw/ct.asp?xItem=2605&ctNode=815&mp=5
Shihmen Reservoir------------------------------------------------------------------------------------------------------------------------------------------- ------------
Finishes the month July 1964Position 24.81°N, 121.24°Eeffective storage capacity 309×106 m3 average annual precipitation 2556 mmslope gradient 83% 30° to 50°Flow direction southeast to northwest
Fig 1. Geographical. 6
Study area - GeologicalGeological
Fig 3. Distribution of the rock formations in the Shihmen Reservoir catchment.
PERIOD
EPOCH Formation
Tertiary
Miocene Aoti Formation (At)
Oligocene
Tatungshan Formation (Tt)
Gangou Formation (Gg)
Szeleng Sandstone Formation (Ss)
Table 1. Formation
7
Typhoon TrackTyphoon Track
Fig 4. The location of Shihmen Reservoir catchment within Taiwan and the tracks of typhoons.
Table 2-1. Statistics of each typhoon event.Typhoon Nelson Herb Nari Aere MatsaYear 1985 1996 2001 2004 2005
Date8/21-
247/29-8/1
9/13-198/23-
268/3-5
Duration of measurements (hour)
96 120 168 96 72
Accumulated rainfall (mm)
456 700 872 996 830
Maximum daily rainfall (mm)
264 536 368 559 448
Average water discharge (m3s-1)
547 707 710 1398 694
8
Table 2-2. Statistics of each typhoon event.Typhoo
nAverage water
discharge (m3s-1)Peak water
discharge (m3s-1) Reservoir sediment discharge (106m3)
Nelson 547 4906 3.7Herb 707 6363 8.7Nari 710 4123 0.4Aere 1398 8594 27.8
Matsa 694 5322 10
Typhoon eventsTyphoon events
9
Typhoon eventsTyphoon events
19871990
19921994
1996
Fig 5. Sediment deposition (tonne), Annual precipitation (mm) and accumulated rainfall during typhoon (mm) during 1963~2005.
10
Typhoon eventsTyphoon events
Fig 6. Sediment deposition (tonne), Annual precipitation (mm) and accumulated rainfall during typhoon (mm) during 1963~2005.
S
ed
imen
t d
ep
osi
tion
(to
nn
e)
11
Study method
• To study the relationship between water turbidity and the landslide debris of the Shihmen Reservoir.
• To reconstruct the process and impact of forming high turbidity water in the reservoir area.
12
Study method
Statistics of Typhoon
Suspended Sediment Discharge
Turbidity
The relationship between turbidity and landslides.
13
Term descriptions
14
Table 2-3. Statistics of each typhoon event.Typhoon Nelson Herb Nari Aere MatsaLandslide area (km2) 9.83 13.95 21.32 6.71 7.02Landslide ratio (%) 1.3 1.8 2.8 0.9 0.9New generation ratio (%)
86.5 88.8 78.5 49.7
Reactivated ratio (%)
19.2 17.1 6.8 52.6
Landslide volume (106m3)
9.83 13.95 21.32 6.71 7.02
15
Suspended sediment discharge
Turbidity
Nephelometer
DH-48 depth integrating suspended sediment sampler
16
Table 2-4. Statistics of each typhoon event.Typhoon Nelson Herb Nari Aere MatsaAccumulated rainfall (mm)
456 700 872 996 830
Maximum daily rainfall (mm)
264 536 368 559 448
Peak water discharge(m3s-1)
4906 6363 4123 8594 5322
Total sediment discharge (106 tonne)
1.67 1.93 1.41 2.95 1.49
Results analysisResults analysis
17
Results analysis
Fig 7. Higher water discharge could drive more landslide debris. Vertical bars indicate the standard error.
Table 2-5. Statistics of each typhoon event.Typhoon Nelson Herb MatsaPeak water discharge(m3s-1)
4906 6363 5322
Landslide volume (106m3)
9.83 13.95 7.02
Total sediment discharge (106 tonne)
1.67 1.93 1.49
18
Results analysis
Fig 8. Sediment concentration had a positive relation with the water turbidity. Dashed lines indicate the 95% confidence limits.
19
Discussion
Fig 9. The diagram displays the hyperpycnal flow in the Shihmen Reservoir. 20
Conclusion• High landslide ratios do not correspond to high
sediment discharge because sediment discharge is still dominated by water discharge and landslide debris possibly still stay on slopes.
• Factors causing high turbidity in the reservoir water were (1) landslides and surface weathering in the upstream catchment; (2) the high density hyperpycnal flow between upstream channel and the reservoir bottom.
21
Thanks for your attention.