GIS-Based Quantification and 3D Rendering of Water ...

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Impacts to Littoral Zone Habitat: Conowingo Hydroelectric Project,. Susquehanna River, MD/PA. Bryan Strawn, Barry Baker, Marjorie L. Zeff. URS Corporation.
GIS-Based Quantification and 3D Rendering of Water Level Fluctuation Impacts to Littoral Zone Habitat: Conowingo Hydroelectric Project, Susquehanna River, MD/PA

Bryan Strawn, Barry Baker, Marjorie L. Zeff URS Corporation HydroVision 2014

Privileged and Confidential: Prepared at the Request of Counsel in Anticipation of Litigation

27,510 mi2

444 mi

RM 56 RM 32 RM 24 RM 10

MDNR

Holtwood

Muddy Run

York Energy Peach Bottom Chester Water

Baltimore

Conowingo

Project Flow Constraints

Minimum downstream flow requirements range 3,500 - 10,000 cfs, or natural river flow, whichever is less

Weekly Average Water Level Fluctuation in Conowingo Pond (Jan 2004 – Sept 2010) 111

110.2 110

Pond Elevation (ft) (NGVD 1929)

109

108

107

summer

106

105

104

103

102

101.2 101 0

5

10

15

20

25

30

35

40

45

50

Week of the Year 2004

2005

2006

2007

2008

2009

2010

Permitted Minimum Elevation

Permitted Maximum Elevation

55

Water Level Fluctuation Magnitude, Frequency, Duration, Rate of Change, and Timing

Quantify impacts of reservoir fluctuation from Project operations on littoral habitat in the Pond

http://www.waterontheweb.org/under/lakeecology/10_biological_lakezones.html

“The Challenge” 1. Develop 1-foot contour plan of river bottom from El. 101.2110.2 ft NGVD 2. Operational and logistical constraints 3. Impractical to use a single survey method (water-based bathymetry or aerial-based LiDAR) 4. Merge 2 surveys a.

Traditional bathymetry (El. 96-108 ft NGVD)

b.

Helicopter-mounted LiDAR (El. 106-112 ft NGVD)

Habitat Substrate (acres) Elevation

Total Acres Bedrock

Gravel

Sand

Silt

110-110.2

0.50

1.27

0.00

0.02

1.78

109-110

2.64

7.15

0.13

0.15

10.07

108-109

2.68

6.68

0.16

0.48

10.00

107-108

3.21

10.51

0.30

0.56

14.59

106-107

3.99

29.70

2.77

0.77

37.23

105-106

4.97

19.33

37.18

1.68

63.16

104-105

4.05

28.40

60.80

5.04

98.28

103-104

4.19

41.56

25.89

13.05

84.69

102-103

3.12

11.51

16.57

49.90

81.09

101.2-102

2.46

6.68

12.24

31.18

52.56

Total

31.79

162.80

156.05

102.84

453.48

SAV coverage greatest at El. 104-105 - 88 percent

Sand is preferred substrate

Cumulative SAV Coverage (acres) 350

14 Coontail Eurasian watermilfoil

12

300

Canadian waterweed Water stargrass

250

10 Hydrilla

8

200

6

150

4

100

2

50

0

0

110.2

110

109

108

107

106

105

Elevation (ft) (NGVD 1929)

104

103

102

101.2

Hydrilla

Not Hydrilla

Unidentified (Side Scan ID)

Summary and Conclusions Water level fluctuations attributable to Project operations do not adversely impact littoral habitat within the Study Area. This was demonstrated by the findings of the quantification analysis. • Coverage of SAV in acres notably drops above El. 106 ft NGVD in concurrence with the reduced availability of unconsolidated substrate. However, Project water level fluctuations are primarily confined between El. 107 ft and 109 ft NGVD and rarely fall below El. 106 ft NGVD. • Water levels below El. 106 ft NGVD (potential dewatering) typically occur over brief periods that do not overlap with the optimal time of the year for SAV growth (summer). • The limited occurrence of EAV is due to geology and not to water level fluctuations. Pond shoreline at favorable elevations is comprised of steeply sloping shorelines and boulder substrates unsuitable for EAV growth.

Questions? [email protected] Booth 1020