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Federal guidelines require that scour effects
be investigated for all bridges over moving water. Movable
bridges are particularly sensitive to scour because they typically
have large piers that obstruct flow in the waterways, leading
to localized scour. Also, movable bridges do not tolerate
settlement or movement caused by scour because of the close
operating tolerances of the bridge. PB engineers have observed
swing bridges with piers that rotate before bridge starts
to move because scour has caused a loss of foundation support.
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The New Jersey Department of Transportation
(NJDOT) initiated a statewide scour evaluation program for highway
bridges in 1990 in response to increased national attention to the
potential risk and catastrophic results of bridge scour. The program
consists of a two-stage evaluation process:
- Stage I. Screening and Prioritization
- Stage II. In-Depth Bridge Scour Evaluation.
Our Princeton office has been involved
in this program since its inception. We have also conducted scour
evaluations for several counties in New Jersey, and the Pennsylvania
Turnpike Commission. This work included Stage II evaluations for
three of the County of Cape May's movable bridges on County Route
619 (Ocean Drive), which is a toll road along the coastline connecting
several major shore towns.
The three bridges had been identified as being potentially vulnerable
to scour damage and assigned high priority as a result of Stage
I evaluations. These structures are located over tidal waterways
along New Jersey's southern Barrier Islands, approximately 1.6 km
(1 mile) off the mainland. All three waterways are in very dynamic
hydraulic environments. The bridges are described in the boxes on
the following page.
Evaluation Process
The primary objectives of our Stage II evaluations were to:
- Estimate the potential long-term scour depth
- Calculate the contraction scour and local scour depths for discharge
events associated with Category 1 and Category 2 hurricanes (Saffir/Simpson
system).
After we determined she scour depths,
we made conceptual recommendations for scour counter measures and/or
remedial actions. Descriptions of the steps taken follow.
Soil Parameters. We took available soil boring information
from each bridge's construction plans and obtained four to six soil
bulk samples from each channel bed. We performed median grain size
analysis on these samples to determine the approximate soil parameters
necessary for calculating the potential scour depths.
Hydraulics. There were no current hydraulic or hydrologic
studies available for any of these inlets,
so we used:
- Computer programs Storm Surge Elevation
(SSEL) and DYNLET 2.01 to perform the hydrologic
and hydraulic analysis for our in-depth evaluation
- The Federal Highway Authority's (FHWA)'s
recommended procedures for developing the storm stage hydrographs
- The 1990 Delaware Hurricane Evacuation Study
for the required parameters
- Maximum storm surges of 2.6 m (8.6 feet), NGVD and 3.4 m (11.3
feet), NGVD for Category 1 and Category 2 hurricanes.
Table 1: Ocean Highway (C.R. 619) over Corson Inlet
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Table 2: Ocean Highway (C.R. 619) over Townsend Inlet

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Table 3: Ocean Highway (C.R. 619) over Grassy Sound

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Variables. We obtained channel
cross section information from National Oceanic and Atmospheric
Administration (NOAA) navigation charts and United States Geological
Survey (USGS) quadrangle maps. This information was supplemented
with data from a fathometric survey at each bridge site. This step
was consistent with the scope of scour analyses, which required
a more site-specific hydraulic analysis. The information was then
used for the computer model in order to determine the variables
needed to perform the scour depth calculations.
Scour Depth. The scour depth calculations were performed
in accordance with HEC-18, assuming that each scour component developed
independently. The HEC-18 equations are based on laboratory data
and are conservative, so the resulting estimates were used in conjunction
with engineering judgment to determine the potential depth of scour.
The calculated scour depths are summarized in Tables 1, 2 and 3.
General Approach at Each Structure
Once the hydraulic analysis was performed for each inlet bay system,
we were able to estimate long-term scour and calculate contraction
and local scour. Long-term scour estimates were based on the comparison
between channel soundings taken periodically from 1986 to 1996 and
the channel bed profiles shown on each bridge's original construction
plans. We used Laursen's equation for live bed contraction scour,
as presented in HEC-18, to estimate the depth of contraction scour.
Clearwater scour equations produced very high values for contraction
scour, which were considered unrealistic.
We used Froehlich's equation for live bed scour to estimate the
potential depth of local scour at the abutments and the Colorado
State University (CSU) equation to estimate the depth of local scour
at the piers. [Ed. note: Dave Froehlich's equation for live scour
was discussed in "Abutment Scour Prediction," a presentation
he gave to the Transportation Research Board in Washington D.C.
in 1989. Dave is also the column editor of PB Network's "PB
Technotes," which frequently features articles on scour
and other hydraulic topics.]
Site-Specific Findings
The bridges were considered to be scour critical because the total
estimated scour depth was estimated to extend well below the pile
caps at the abutments and main piers and expose a significant amount
of the piles at some of the pile bents. Underwater inspections suggested
severe scour at some of the piers.
Corson Inlet Bridge. Both the May 1984 underwater inspection
report and the January 1987 in-depth inspection report stated that
the eastern caissons at piers 28 and 30 were undermined at their
bases. The underwater inspection of 1989 noted undermining of both
eastern and western caissons of pier 28 only. In 1994, both the
east and west caissons of piers 28 and 30 were noted to be undermined.

Typical structure's calculated scour depth show graphically. |

Townsends Inlet Bridge |
Townsends Inlet Bridge.
The channel has migrated laterally southwards over the years, as
evidenced by changing conditions reported in inspections over the
years. Repair plans of 1977 had specified that the repair jackets
extend below the channel bed, however:
- The underwater inspection of May 1984 stated
that the repair jacket on the north pile on the eastern side at
bent #4 terminated above the channel bed.
- The in-depth inspection report dated December
1986 documented scour problems that caused a significant loss
of pile embedment and required supplemental supports to be installed
at some of the pile bent piers.
- The underwater inspection of 1989 noted undermining
of repair jackets at both north and south piles on the eastern
side of bent #2.
- In 1994, the south pile of the eastern cluster at bent #4 and
east pile of the eastern cluster at bent #5 were both noted to
have repair jackets at 0.6 m to 1.2 m (2 feet to 4 feet) above
the channel bed.
Grassy Sound Bridge. The
channel has migrated laterally northwards. The in-depth inspection
report dated October 1986, documents scour problems at the northern
end that are probably due to channel migration to the north, causing
a loss of fill within the bin type abutment and undermining a portion
of the abutment walls. The underwater inspection of May 1989 noted
local scour at the western shaft of pier 4. The underwater inspection
of 1994 noted scour holes at piers 1, 3 and 4.
Countermeasure Recommendations
Based upon the physical conditions present at each structure and
the scour calculations performed, we recommended installation of
stone riprap to preserve the structural integrity of the bridges
from scour damage. We recommended that the riprap extend partial
length or full length under all the spans (as appropriate) across
the channel at a width of 12 m (40 feet) and 3 m (10 feet) beyond
the bridge limits on each side. Similar countermeasures were recommended
at the abutments for a length of 8 m (25 feet) and width of 9 m
(30 feet).
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The dumped riprap was estimated
to be 0.5 to 0.9 meters (1.5 to 3 feet) maximum, an approximation
derived from the calculated depth of the contraction scour plus
four times the estimated median stone size (D50) for the computed
peak velocities.
Future Monitoring and Countermeasures
Because riprap at the piers is considered to be only a temporary
countermeasure, routine monitoring will be required. We recommended
that diving inspections be performed during each biennial bridge
inspection and after any major storm or flood, due to the current
scour conditions.
NJDOT is preparing to solicit design firms to perform detailed design
and prepare contract documents for the installation of scour countermeasures
for many of the scour critical structures throughout the state.
Please contact us for additional information about the scour evaluation
program in New Jersey or to discuss other issues regarding movable
bridges.
Three Cape May Bridges for Stage
II In-Depth Scour Evaluations
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Ocean Highway Bridge Over Corson Inlet
Type: 39-span viaduct, single leaf bascule bridge.
Location: Upper Township. Spans Strathmere Bay, Corson Inlet
and the Atlantic Ocean area immediately east of the bridge.
Construction Date: 1948. No major reconstruction.
Length Between Abutments: Approximately 451 m (1,480 feet).
Bascule Span: 20 m (65 feet).
Waterway opening: Consistent with normal flow width.
Alignment to normal flow:
- North abutment-most piers generally well
aligned
- South abutment-a few southern pile bent piers
skewed due to existing shoreline.
Construction:
- Approach span pile bents are precast concrete
driven piles.
- Main piers are supported on steel bearing
piles.
- Abutments are supported on creosote treated
timber piles.
Design plans: (original 1947 construction plans)
- Estimated lengths of all piles, location
of the bottom of pile caps relative to the original channel bed
- Actual lengths of substructure piles was
unknown because plans may not be "as-built" drawings.
Ocean Highway Bridge Over Townsends Inlet
Type: 27-span viaduct, single leaf bascule bridge.
Location: Between Sea Isle City and Avalon Borough. Spans Townsends
Inlet and Atlantic Ocean to the east and intracoastal waterway to
the west.
Construction Date: 1940. Reconstruction includes:
- Supplemental piles at some pile bents in
1962
- Riprap in 1962 and 1972
- Jacketing some of the piles in 1977
- Strengthening steel members in 1990.
Length Between Abutments: Approximately 420 m (1,370 feet).
Bascule Span: 20 m (65 feet).
Waterway opening: Normal flow does not extend under the northern
third.
Alignment to normal flow:
- Eastern (seaward) side-northern and southern shore lines are
skewed with respect to the bridge
- Western (inland) side-shore lines generally
in alignment with the bridge.
Construction: Same as Corson Inlet Bridge.
Design plans:
- Detailed information available on original "as-built"
construction plans of 1939/1940
- Pier driven pile lengths supplied
- Abutment pile lengths not available, assumed
to be similar to another bridge of similar construction built
about the same time.
Ocean Highway Bridge Over Grassy Sound
Type: 21-span viaduct, single leaf bascule bridge.
Location: Middle Township. Spans Grassy Sound Channel to
the west, Hereford Inlet and the Atlantic Ocean to the east.
Construction Date: 1940. Reconstruction includes:
- Riprap in 1962 and 1976
- Jacketing some piles in 1977
- Strengthening steel members in 1990.
Length Between Abutments: Approximately 325 m (1,067 feet).
Bascule Span: 20 m (65 feet).
Waterway opening: Full length of the structure.
Alignment to normal flow: Abutments and piers are well aligned.
Construction: Same as for Corson Inlet Bridge.
Design plans:
- Detailed information available on the original
"as-built" construction plans of 1938/1940
- Pier driven pile lengths supplied
- Abutment pile lengths not available, assumed to be similar
to another bridge of similar construction built about the same
time.
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