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II.7.2 - Calibration

Calibration of both the empirical and mechanistic equations is show below.

Empirical Equation

The calibration is applied to the hyperbolic empirical model given by eq (113) where

Data for fitting these parameters were obtained from rating curves provided by Bolyvong Tanovan of the Army Corps of Engineers North Pacific Division, Portland, OR. The graphs showing observed nitrogen concentrations in supersaturation for spill flows were copies of in-house documents -unreferenced and unpublished. The graphs were identified with the codes NPDEN-WC, DLL/KPA, 8MAR79. The ruling of the rating curves allowed a precision of ±0.5 kcfs, and ±0.1% saturation.

The parameters in Table 36 were obtained by fitting the hyperbolic submodel of eq (113) to the rating curves using a nonlinear "amoeba" routine from Numerical Recipes (Press et al. 1988). Constraints on fitted parameters were: 0 <= a <= 50, 0 <= b <= 0.12, 0 <= h <= 100.

Table 36 Values for empirical nitrogen model
Dam a b h resida
Bonneville 29.92 0.020 6.07 21.
The Dalles 20.21 0.0006 22.32 72.4
John Day 8.43 0.095 0.00 42.63
McNary 16.33 0.000 35.33 2.22
Ice Harbor 17.36 0.117 3.82 44.07
Low. Monumental 25.44 0.000 8.55 4.05
Little Goose 40.78 0.000 37.36 3.52
Lower Granite 24.22 0.000 18.07 6.12
Priest Rapids 22.02 0.038 3.31 49.22
Wanapum 28.03 0.047 10.35 29.17
Rock Island 42.26 0.0003 99.95 48.30
Rocky Reach 23.82 0.020 1.49 19.08
Wells 20.83 0.065 0.20 9.51
Chief Joseph 28.74 0.008 11.68 39.56
aresid = residual sum of squares / number of data points.

Mechanistic Equation

The mechanistic nitrogen saturation submodel (see Mechanistic Equation section II.7.1) was calibrated using flow/spill/gas saturation data from the rating curve data 1984 to 1990 at most projects. (This data set was supplied by Tom Miller of the Walla Walla District of the U.S. Army Corps of Engineers.) The data originated from the Columbia River Operations Hydrological Monitoring System (CROHMS) data base. At each dam the data consisted of: hourly flow and spill, forebay saturation, forebay elevation, tailrace elevation, and temperature, all measured throughout the summer. Using the same gas dissipation mechanism as was used in earlier versions of CRiSP.1, the tailrace gas saturation was back-calculated from the next dam downstream.

For each point in time the three parameters a, b, and c below were estimated using a multiple linear regression of the equation defining K20 in terms of the energy loss rate, the forebay concentration, and the entrainment coefficient. The mechanistic model for GasSpill 2 assumes that these parameters are related as is given by eq (121) where

For each dam K20 is calculated from data using:

(132)

where

where

and

No data were available for Wanapum Dam thus preventing calibration of both Wanapum and Rock Island, the dam immediately upstream. In these cases the initial calibration of Water Resources Engineers Inc. (WRE 1971) was used as the calibration.

The spill program of 1994 presented an opportunity to recalibrate Gasspill parameters using up-to-date data at a variety of spill levels, including some observations at very high levels that had not previously occurred. Daily average gas levels were compared to those estimated using previously calibrated GasSpill parameters, and parameters were adjusted on a dam by dam basis to bring model predictions into closer agreement with observed data. Required changes were quite small, but the improvement of fit was noticeable; current estimates and observed gas levels are shown for several points in the system in Fig. 46. Note that in all four graphs the predicted and observed saturation tracks do not differ significantly (chi-squared goodness-of-fit test, in all cases p>0.05).

Table 37 Parameters for Gas spill model equations
Dam L Basin Floor Elev. gate wd # gates sgr a b c
BON 144.5 -16.0 60 18 1.0 2.469 1.108 -1.103
TDA 170.0 55.0 60 23 0.50 37.00 3.255 -0.394
JDA 185.0 114.0 62 20 1.0 5.200 0.798 -0.050
MCN 270.0 228.0 60 22 1.0 5.700 0.810 -0.050
IHR 178.0 304.0 60 10 1.0 0.524 0.146 0.000
LMN 218.7 392.0 50 8 1.0 -1.900 1.037 0.010
LGS 78.6 466.5 50 8 1.0 4.072 1.247 -0.035
LWG 188.0 580.0 50 8 1.0 -5.150 0.400 0.060
DWR 40.0 954.0 60 2 1.0 3.310 0.460 -0.032
HCY 80.0 1480.0 50 1 1.0 3.310 0.460 -0.032
PRD 75.3 387.0 40 22 1.0 5.000 -0.337 -0.037
WAN 100.0 456.0 50 12 1.0 0.000 0.029 0.051
RIS 100.0 530.0 30 37 0.1 -4.000 -0.137 0.051
RRH 150.0 599.0 50 12 1.0 22.25 -1.14 -0.077
WEL 30.0 670.0 46 11 1.0 28.00 0.804 0.000
CHJ 180.0 743.0 40 19 1.0 -5.05 0.295 -0.070

Table 38 Variables for reservoir geometry, in feet. Dam abbreviations correspond to dams in Table 36.
Dam Maximum Forebay Elevation Full Pool Depth at Head Forebay Depth Elevation Spillway Crest Normal Tailwater Elevation
BON 82.5 68 98.5 24 14.5
TDA 182.3 85 127.3 121 72
JDA 276.5 105 162.5 210 160
MCN 357 75 129.0 291 265
IHR 446 100 142.0 391 340
LMN 548.3 100 156.3 483 440
LGS 646.5 98 180.0 581 540
LWG 746.5 100 166.5 681 638
PRD 488 82.5 101.0 - -
WAN 575 83.5 121.0 - 485
RIS 619 54 189.0 - 570
RRH 710 93 111.0 - 613
WEL 791 72 121.0 - 705

Fig. 46 Comparison of observed and modeled gas supersaturation for 1994 data. Lower Granite Pool Chi-square = 1.88, p>0.05. Ice Harbor Pool Chi-square = 3.38, p>0.05. Priest Rapids Pool Chi-square = 2.01, p>0.05. Bonneville Pool Chi-square = 1.08, p>0.05.

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Columbia River Salmon Passage Model CRiSP.1.5 Theory, Calibration & Validation Manual
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