hydroacoustic sediment surrogates and methods —test results for a small urban river—
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Hydroacoustic Sediment Surrogates and Methods —test results for a small urban river—. Mark N Landers, [email protected] Federal Interagency Sedimentation Project Chief January 10, 2012 USGS, Reston, VA, and WEB-EX. water.usgs.gov/fisp. - PowerPoint PPT PresentationTRANSCRIPT
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Hydroacoustic Hydroacoustic Sediment Surrogates Sediment Surrogates
and Methodsand Methods—test results for a —test results for a small urban river—small urban river—
Mark N Landers, [email protected] Interagency Sedimentation Project Chief
January 10, 2012USGS, Reston, VA, and WEB-EX
water.usgs.gov/fisp
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Yellow River at Gees Mill Road near Metro Atlanta, Yellow River at Gees Mill Road near Metro Atlanta, GA, 02207335GA, 02207335
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Yellow River at Gees Mill Road near Metro Atlanta, Yellow River at Gees Mill Road near Metro Atlanta, GA, 02207335GA, 02207335
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Yellow River at Gees Mill Road near Metro Atlanta, Yellow River at Gees Mill Road near Metro Atlanta, GA, 02207335GA, 02207335
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Yellow River at Gees Mill Road near Metro Atlanta, Yellow River at Gees Mill Road near Metro Atlanta, GAGA
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Yellow River at Gees Mill Road near Metro Atlanta, Yellow River at Gees Mill Road near Metro Atlanta, GA, 02207335GA, 02207335
Acoustic Doppler Current Profilers (A) 1.2MHz (B) 1.5MHz (C) 3.0MHz
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Acoustic Doppler Current Profiler Acoustic Doppler Current Profiler ConfigurationConfiguration
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Urick’s Method:SSC = 10(A+B ( RL + 2TL))
2TL=20log10(ψr) + 2r(αs+ αw)
αw = 8.686 f 2 (55.9−2.37T+0.0477T 2−0.000348T 3) 10−15
Measured Backscatter
Computed WaterAttenuation
Acoustic Surrogates of SSCAcoustic Surrogates of SSC
Urick’s Method:
Acoustic Surrogates of SSCAcoustic Surrogates of SSC
SSC = 10(A+B ( RL + 2TL))
2TL=20log10(ψr) + 2r(αs+ αw)Measured Backscatter
Computed WaterAttenuation
2.3)/5.2()/35.1(11)(
nn rrrrr
Near Field for 3.0 MHz SW (27mm dia) is 1.16m; for 1.5MHz SL (50mm dia) is 1.98m; for 1.2MH RDI ChanMaster (70mm dia) is 3.11. Correction at 1m for each is about 4%, 20%, and 70%, respectively.
Hybrid Urick-Sheng-Hay Method:
Acoustic Attenuation by Sediment:Acoustic Attenuation by Sediment:
34.4)24.03.11(5)(
)1( 4422
34
222
akakak
ss
kSSCVS
aas
11
49
2
a
495.0
Backcatter Amplitude Profiles: Measured & Normalized
Acoustic Attenuation by Sediment:Acoustic Attenuation by Sediment:
)2)(log20(21
10 ws rrRLdrd
Slope = 2TL
Slope = 2r(αw + αs)
Slope = 2r(αs )
Relative Backscatter
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Urick’s Method:
Acoustic Surrogates of SSCAcoustic Surrogates of SSC
SSC = 10(A+B ( RL + 2TL))
2TL=20log10(ψr) + 2r(αs+ αw)Measured Backscatter
Computed WaterAttenuationMeasured Sediment Attenuation
Acoustic Surrogates of SSCAcoustic Surrogates of SSC
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Acoustic Surrogates of SSCAcoustic Surrogates of SSC
Conclusions re: Acoustic Conclusions re: Acoustic Backscatter and Attenuation as Backscatter and Attenuation as Surrogates of Suspended Sediment Surrogates of Suspended Sediment ConcentrationConcentration
The methods proposed by Topping et al. (2007) to empirically The methods proposed by Topping et al. (2007) to empirically measure acoustic attenuation from profiling ADCP measurements measure acoustic attenuation from profiling ADCP measurements do apply for a stream in the southeastern USA. do apply for a stream in the southeastern USA.
Using both relative acoustic backscatter (Using both relative acoustic backscatter (RBRB) and acoustic ) and acoustic attenuation as explanatory variables results in a significantly attenuation as explanatory variables results in a significantly improved model of improved model of SSCSSCxsxs, compared with traditional sonar , compared with traditional sonar equations using only equations using only RBRB. .
Fluvial suspended sediment concentration can be determined by Fluvial suspended sediment concentration can be determined by high-resolution acoustic measurements with much greater high-resolution acoustic measurements with much greater accuracy than using traditional SSC ~ streamflow discharge accuracy than using traditional SSC ~ streamflow discharge ratings. Rratings. R22 improved from 0.57 to (0.79 to 0.80); and model improved from 0.57 to (0.79 to 0.80); and model residual standard error improved from 73% to (34% to 40%).residual standard error improved from 73% to (34% to 40%).
Sediment Size from Acoustic Sediment Size from Acoustic AttenuationAttenuation
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Sediment Size from Acoustic Sediment Size from Acoustic AttenuationAttenuation
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Sediment Size from Acoustic Sediment Size from Acoustic AttenuationAttenuation
Representative particle sizes cannot be determined Representative particle sizes cannot be determined from these data by optimizing the theoretical from these data by optimizing the theoretical acoustic attenuation equation using measured acoustic attenuation equation using measured acoustic attenuation for single acoustic frequencies acoustic attenuation for single acoustic frequencies nor for ratios of multiple acoustic frequencies. nor for ratios of multiple acoustic frequencies.
Suspended sediment PSD is significantly correlated Suspended sediment PSD is significantly correlated with ratios of measured acoustic attenuation at with ratios of measured acoustic attenuation at different frequencies.different frequencies.
Conclusions re: Acoustic Attenuation Conclusions re: Acoustic Attenuation Surrogates of Sediment SizeSurrogates of Sediment Size
This study has identified the following needs for further research:This study has identified the following needs for further research: Evaluate measured and theoretical acoustic attenuation for Evaluate measured and theoretical acoustic attenuation for
characterization of suspended sediment size. The data needed for this characterization of suspended sediment size. The data needed for this research includes concurrent measurements of SSC, full PSD, and multi-research includes concurrent measurements of SSC, full PSD, and multi-frequency profiles of acoustic backscatter and attenuation on different frequency profiles of acoustic backscatter and attenuation on different streams having diverse sediment characteristics.streams having diverse sediment characteristics.
Test, validate, and develop generalized methods for use of acoustic Test, validate, and develop generalized methods for use of acoustic backscatter and attenuation for estimation of suspended backscatter and attenuation for estimation of suspended sediment concentration and load.sediment concentration and load.
Recommendations for Further Recommendations for Further ResearchResearch
Sediment Size from Acoustic Sediment Size from Acoustic AttenuationAttenuation