The Suspended Sediment Regime of the Waipaoa River Murray Hicks NIWA, Christchurch NIWA Taihoro...
Transcript of The Suspended Sediment Regime of the Waipaoa River Murray Hicks NIWA, Christchurch NIWA Taihoro...
The Suspended Sediment Regime of the Waipaoa River
Murray Hicks
NIWA, Christchurch
NIWATaihoro Nukurangi
Thanks to ….• Landcare Research
– Noel Trustrum – Ted Pinkney
• Basil Gomez• Gisborne District Council
– Dave Peacock
• Hydro-Technologies – Bruce Walpole– Ingrid Pak– Ross Bannister
NZ total:
211 Mt/y
(~ 1% global yield)
Context
15 Mt/y(~0.1%)
35 Mt/y
Content
• NZ and global context
• Datasets
• SS rating characteristics
• C-Q hysteresis behaviour
• Event yields
• Hyperpycnal discharge potential
• Summary
DatasetsDatasets
Mangatu(1999 ..)
Waihora(1999..)
Te Arai(2001..)
Waipaoaat
Kanakanaia(1997..)
Continuous monitoring
Data-logger
Auto-sampler
Mangatu at Omapere
Turbidity sensor(s) 0-50,000 mg/l (0-5,000 mg/l)
Stage sensorSampler intake
SSC vs Discharge Relationship: Waipaoa at Kanakanaia
10
100
1000
10000
100000
1 10 100 1000 10000
Discharge (m3/s)
SS
C (
mg
/l)
No gaugings 301
Maximum C (mg/l)
36814
Max gauged flow (m3/s)
1826
Maximum recorded flow (m3/s)
Mean annual flood (m3/s)
SS yield (t/km2/yr)
Average d50
(microns)
5286
1346
6750
13
Bias-correctedLOWESS curve
Qmaf QmaxQmean
Annual yields at Kanakanaia
• Mean: 10.7 Mt/yr
• Maximum: 32 Mt (1988, Cyclone Bola)
• Minimum: 2.5 Mt
• Std deviation: 6.7 Mt/yr
1
10
100
1000
10000
100000
100 1000 10000 100000 1000000 10000000
Water discharge (l/s)
SS
C (
mg
/l) 16-Nov-97
1-Jul-98
3-Dec-98
21-Jan-99
5-Jun-99
21-Dec-99
Gaugings 1962-1996
Hysteresis behaviour
Example
storm: 2-12 July 2000
0
200
400
620
Flow
m3/s
2-Jul-2000 1.6 hrs/mm 6-Jul 8-Jul 10-Jul 12-Julsite 19701 Waipaoa at Kanakanaia Br Flow m3/s 10units/mmsite 99996 Final Kanakanaia SSC Calibration July 2002 conc ppm 403units/mm
Waipaoa25000
SSC(mg/l)
0
Q(m3/s)
0
20
40
67
Flow
m3/s
2-Jul-2000 1.6 hrs/mm 6-Jul 8-Jul 10-Jul 12-Julsite 19706 Waihora at No 3 Bridge Flow m3/s 1units/mmsite 99994 Final Waihora SSC from Calibration July 2002 conc ppm 373units/mm
Waihora25000
SSC(mg/l)
0
Q(m3/s)
0
20
40
60
77
flow m
3/s
2-Jul-2000 1.6 hrs/mm 6-Jul 8-Jul 10-Jul 12-Julsite 19712 Mangatu at Omapere Flow flow m3/s 1.149units/mmsite 99993 Final Mangatu SSC from Calibration July 2002 SSC ppm 373units/mm
Mangatu25000
SSC(mg/l)
0
Q(m3/s)
Example
storm: 2-12 July 2000
0
5000
10000
15000
20000
25000
0.0 0.5 1.0 1.5 2.0 2.5 3.0
Q/Qmean
SS
C (
mg
/l)
Kanakanaia
Mangatu
Loop of loops
Event peak SS Concentration
0
10000
20000
30000
0 200 400 600 800Event peak discharge (m3/s)
Ev
en
t p
ea
k S
SC
(m
g/l) R2 = 0.07
10
100
1000
10000
100000
1 10 100 1000 10000
Discharge (m3/s)
SS
C (
mg
/l)
All data
< 3 yrs after Bola
Effect of large events: Cyclone bola
x2
Event-yield magnitude-frequency relationships
0.1
1
10
100
1000
10000
100000
-2 0 2 4 6
Return Period(Extreme value reduced variate )
Yie
ld (
tkm
-2)
Mangatu
Waipaoa
Waihora
Te Arai
1-yr1-mo
Shallow landslip(e.g. Waihora, Te Arai)
Gullied(e.g. Mangatu)
Characteristic erosion terrains
Event-yield magnitude-frequency relationships
0.1
1
10
100
1000
10000
100000
-2 0 2 4 6
Return Period(Extreme value reduced variate )
Yie
ld (
tkm
-2)
Mangatu
Waipaoa
Waihora
Te Arai
Gullied
LandslipMixed
Event effectiveness
0%
20%
40%
60%
80%
100%
0.01 0.1 1 10 100
Return period (yr)
Percent of long term sediment
yield Waipaoa
Mangatu
Te Arai
50%
2 yr1.1 yr
Waipaoa River Basin
Bankfulldischarge atKanakanaia
Cum
ulat
ive
Perc
ent Su
spen
ded
Sedi
men
t Lo
ad
Discharge (m3 s-1)
100
80
60
40
20
00 1000 2000 3000 4000 5000 6000
Hyperpycnal discharge potential
Hyperpycnal discharge threshold concentration
Cr > (o0 - r0) / (1 - 0 / s)
River SS concentration
Ocean waterDensity (clear)
River waterdensity (clear)
Sedimentmineraldensity
Referencewaterdensity
Waipaoa/Poverty Bay Conditions
River temp (oC) 10 16 10 16
River density (gcm-3) 1.00013 0.99965 1.00013 0.99965
Ocean density (gcm-3) 1.025 1.025 1.023 1.023
Location Outer Poverty Bay River plume*
Season Winter Summer Winter Summer
Cr
(mgl-1) 39946 40705 36733 37494
37,000-41,000 mg/l* Stephens et al., 2002
Hyperpycnal threshold exceedences
0.1
1
10
100
1000
10000
100000
0.01 0.1 1 10 100
Q/Qmean
SS
C (
mg
/l)~40,000 mg/l
37,000-41,000 mg/l
Hyperpycnal threshold exceedences
1-severalexceedencesin last 40 years??
0
5000
10000
15000
20000
25000
30000
35000
40000
45000
50000
0 20 40 60 80
Q/Qmean
SS
C (
mg
/l)
Waipaoa
RatingNeedcontinuousmonitoring
Summary
• East Cape Region supplies ~ 0.3% sediment flux to global ocean– Waipaoa supplies ~ 15 Mt/yr
• SSC vs Q ratings – top-end curvature– clockwise hysteresis during flood events, over
individual peaks and overall, reflecting sediment supply effects
– event peak SSC poorly correlated with peak discharge– maximum sampled SSC ~ 37,000 mg/l
Summary continued …• Event-yield magnitude-frequency distributions
– Show hillslope erosion-process signatures
– Rarer, larger events more important at delivering long-term sediment yield from landslip terrain, common events more important for gullied terrain
– Waipaoa mainstem shows “mixed” behaviour
• Threshold SSC for hyperpycnal river discharges – ~ 40,000 mg/l
– exceeded 1-several times over last 40 years, but very uncertain
– Recommend maintaining continuous monitoring, ideally at Matawhero, nearer coast