STATUS REPORT FOR THE SUBMERGED REEF BALL TM ARTIFICIAL REEF BEACH STABILIZATION PROJECT FOR THE GRAND CAYMAN MARRIOTT HOTEL

Similar documents
STATUS REPORT FOR THE SUBMERGED REEF BALL TM ARTIFICIAL REEF SUBMERGED BREAKWATER BEACH STABILIZATION PROJECT FOR THE GRAND CAYMAN MARRIOTT HOTEL

SITE INVESTIGATIONS OF THE BEACH EROSION PROBLEM AT MAHO BEACH, ST. MAARTEN

SHORELINE STABILIZATION RECOMMENDATIONS FOR PLAYA DEL SECRETO MAYA RIVIERA, Q.R., MEXICO

COMPARISON OF FIXED & VARIABLE RATES (25 YEARS) CHARTERED BANK ADMINISTERED INTEREST RATES - PRIME BUSINESS*

COMPARISON OF FIXED & VARIABLE RATES (25 YEARS) CHARTERED BANK ADMINISTERED INTEREST RATES - PRIME BUSINESS*

COASTAL DAMAGE INSPECTION SOUTHWEST VITI LEVU, FIJI AFTER CYCLONE SINA

AT&T Global Network Client for Windows Product Support Matrix January 29, 2015

The Coast of Crystal Cove Orange County, California

Tropical Storm Debby. Post-Debby Beach/Dune Damage Assessment Report Sarasota Florida. By Weiqi Lin P.E., Ph.D. Coastal Resources/Community Services

Using LIDAR to monitor beach changes: Goochs Beach, Kennebunk, Maine

Coastal Erosion Risk Mitigation Strategies applied in a Small Island Developing State: The Barbados Model

Tropical Storm Debby

Enhanced Vessel Traffic Management System Booking Slots Available and Vessels Booked per Day From 12-JAN-2016 To 30-JUN-2017

Evaluating the Condition of Seawalls/Bulkheads

Analysis One Code Desc. Transaction Amount. Fiscal Period

Case 2:08-cv ABC-E Document 1-4 Filed 04/15/2008 Page 1 of 138. Exhibit 8

St Lucia. Wise practices for coping with. i b bea n Se a

Martin County Coastal GIS Program St Lucie Inlet Planning Tool

ebb current, the velocity alternately increasing and decreasing without coming to

RESTORATION AND ENHANCEMENT OF SOUTHERN CALIFORNIA LAGOONS

HURRICANE WORKFORCE ANALYSIS HURRICANES ANDREW AND OPAL

BEACH NOURISHMENT COMBINED WITH SIC VERTICAL DRAIN IN MALAYSIA.

Ways We Use Integers. Negative Numbers in Bar Graphs

Ashley Institute of Training Schedule of VET Tuition Fees 2015

Storm tide is the water level rise during a storm due to the combination of storm surge and the astronomical tide.

2011 Annual Inspection Report

Storm tide is the water level rise during a storm due to the combination of storm surge and the astronomical tide.

Sea Water Heat Pump Project

Infographics in the Classroom: Using Data Visualization to Engage in Scientific Practices

An Assessment of Prices of Natural Gas Futures Contracts As A Predictor of Realized Spot Prices at the Henry Hub

How Did These Ocean Features and Continental Margins Form?

Ariana Sutton-Grier, Holly Bamford & Kateryna Wowk University of Maryland and National Oceanic and Atmospheric Administration

FINAL REPORT FOR 2012 ON THE CONDITION OF THE MUNICIPAL BEACHES IN THE CITY OF BRIGANTINE BEACH, ATLANTIC COUNTY, NEW JERSEY

Southern AER Atmospheric Education Resource

Climate Change. Lauma M. Jurkevics - DWR, Southern Region Senior Environmental Scientist

Hazards of the Jamaican Coastline ERODING BEACHES: A RESPONSE TO RISING SEA LEVEL?

COST AND MAINTENANCE OF LIVING SHORELINES

Quadrant 1 Sea Breeze: Routing Considerations Table of Contents

Financial Operating Procedure: Budget Monitoring

asbpa Preserving our coastal economy and ecology since 1926

An Initial Assessment of the Impacts of Sea Level Rise to the California Coast

The impact of coral bleaching 2010

Coffee year 2014/15 ends with prices at 20-month low

Using INZight for Time series analysis. A step-by-step guide.

Offshore Windfarm Egmond aan Zee 4 years of Operation

Scott Market Report. Weather Affects Winter Sales

Future of our coasts: Potential for natural and hybrid infrastructure to enhance ecosystem and community resilience Ariana Sutton-Grier

ANATOMY OF A MUDSLIDE AND DAMAGE CAUSED BY HURRICANE IVAN

Coffee prices fall but Brazilian production estimated lower

CENTERPOINT ENERGY TEXARKANA SERVICE AREA GAS SUPPLY RATE (GSR) JULY Small Commercial Service (SCS-1) GSR

Illinois Coastal Management Program 2011

2011 Operations, Maintenance, Monitoring and Rehabilitation Plan

Box Plots. Objectives To create, read, and interpret box plots; and to find the interquartile range of a data set. Family Letters

NEAR-SHORE CIRCULATION IN THE CALIFORNIA CURRENT

GLOSSARY OF TERMINOLOGY

SECTION 10.0 MANAGEMENT UNIT 5: HORNSEA

oct 03 / 2013 nov 12 / oct 05 / oct 07 / oct 21 / oct 24 / nov 07 / 2013 nov 14 / 2013.

SARASOTA COUNTY LIDO KEY HURRICANE & STORM DAMAGE REDUCTION PROJECT

TECTONICS ASSESSMENT

Final Project Report

EFFECTS OF ARUNDO DONAX ON RIVER HYDRAULICS, SEDIMENT TRANSPORT, AND GEOMORPHOLOGY, SANTA MARGARITA RIVER, CALIFORNIA

Natural Gas Futures Trading Markets

RESUME for Christopher G. Creed, P.E.

Year

Natural Gas Wholesale Prices at PG&E Citygate as of November 7, 2006

OPERATIONS SERVICE UPDATE

Texas Prairie Wetlands Project (TPWP) Performance Monitoring

Employers Compliance with the Health Insurance Act Annual Report 2015

A Case Study Documenting the Dubai Coastal Zone Monitoring Programme An International Example.

TOPIC: CLOUD CLASSIFICATION

Wind Resource Assessment for BETHEL, ALASKA Date last modified: 2/21/2006 Compiled by: Mia Devine

Natural Gas: Winter Abundance! and Some Confusion

Important Dates Calendar FALL

Hurricanes and Storm Surge

Sandia National Laboratories New Mexico Wind Resource Assessment Lee Ranch

P/T 2B: 2 nd Half of Term (8 weeks) Start: 25-AUG-2014 End: 19-OCT-2014 Start: 20-OCT-2014 End: 14-DEC-2014

P/T 2B: 2 nd Half of Term (8 weeks) Start: 26-AUG-2013 End: 20-OCT-2013 Start: 21-OCT-2013 End: 15-DEC-2013

When Is an Elephant Not an Elephant? When It's a Seal, Of Course! By Mikki Sadil

COPPER GOLD PLATINUM SILVER PALLADIUM

Renewable Energy. Solar Power. Courseware Sample F0

P/T 2B: 2 nd Half of Term (8 weeks) Start: 24-AUG-2015 End: 18-OCT-2015 Start: 19-OCT-2015 End: 13-DEC-2015

Strategic Beach Management Plan Southeast Atlantic Coast Region

Breakaway Walls

REPORTS & PRESENTATIONS AGENDA ITEM #III-3 CORTEZ BRIDGE PROJECT DEVELOPMENT AND ENVIRONMENT (PD&E) STUDY

Geotechnical Investigation Reports and Foundation Recommendations - Scope for Improvement - Examples

Departures to the south from Runways 16L and 16R.

Resource Management Accomplishments FY 2014

For St. Kitts, this would be an investment of approximately US$100 million

A Few Facts about Antarctica

How To Check For Scour At A Bridge

In the Caribbean, August and September are peak months during the hurricane season that lasts from June 1 through November 30.

December 2015 Lutgert College Of Business FGCU Blvd. South Fort Myers, FL Phone

Beach Management Funding Assistance Program

Market Monitor Number 3 November 2012

By Chris Gorman, PE M.ASCE PROBLEM:

Spread Betting and Trading Naked Options

Managing Cattle Price Risk with Futures and Options Contracts

Computing & Telecommunications Services Monthly Report March 2015

Consumer ID Theft Total Costs

1. Introduction. 2. User Instructions. 2.1 Set-up

Transcription:

STATUS REPORT FOR THE SUBMERGED REEF BALL TM ARTIFICIAL REEF BEACH STABILIZATION PROJECT FOR THE GRAND CAYMAN MARRIOTT HOTEL performed by Lee E. Harris, Ph.D., P.E. Consulting Coastal Engineer Assoc. Professor of Ocean Engineering Florida Institute of Technology Melbourne, Florida 3291 USA July 22 This report presents an update on the submerged Reef Ball TM artificial reef breakwater that was installed to assist with beach and shoreline stabilization during the summer and fall of 22. Initial field inspections were first performed in February 22 to investigate the beach erosion problem at the Marriott Hotel on Seven Mile Beach on Grand Cayman Island, and to determine alternatives that can be considered to restore and stabilize the beach at this site. An array of alternatives were considered, and a submerged breakwater constructed of 2 Reef Ball TM artificial reef units was chosen. Design and permitting of the project was performed during the winter and spring of 22, with fabrication of the units and deployment offshore completed Beach Erosion Problem The Marriott Hotel lies at the southern end of Seven Mile Beach. The beaches in this area have been very narrow in recent years, having last been stripped of sand during Hurricane Michelle in November 21 and again during storm events in 22. The beaches to the north generally become wider as you go north from the Marriott Hotel to the central Seven Mile Beach area, while to the south there is only a short stretch of sand beach that is followed by a rocky shoreline as you approach the Treasure Island Resort. There are some rock groins that were constructed in this area, and the shoreline here curves around to the east. This rocky shoreline to the south and reorientation of the shoreline effectively blocks any potential transport of sand from the south to the Marriott s beaches. Therefore the Marriott s beach area is particularly susceptible to erosion from waves coming from the southwest, due to the lack of sand along the coast to the south. Waves from the southwest, especially during storm events, transport sand to the north. Waves from the northwest tend to transport sand to the south along the Seven Mile Beach area which nourishes the beaches at the south end (including the Marriott), but this occurs at a much slower rate, and an increase in southwest waves over the past few years has prevented the beach from accreting out to the beach width that the Marriott had prior to 1996. Due to the erosion of the beaches along the southern reach of the Seven Mile Beach area, natural sand accretion and return of the beach width to that in the mid 199 s could take several years, if at all, and any future southwest wave events will further erode the beaches in this area, and slow this natural recovery. Lee E. Harris, Ph.D., P.E. Page 1 of 11

The Grand Cayman Marriott Resort has experienced beach erosion. The existing beach width varies seasonally and with storm events, and although it does begin to recover by sand transport into the area from the north, the beach continues to be eroded away by waves coming from the southwest each fall. The staff at the Marriott measures the beach width from the seawall at the north, center and south end of the property every day, with this information providing a good record of beach changes, and should be continued to be collected. These data are shown in the graphs below for the variation in the average beach width in front of the Marriott over time: 8 Grand Cayman Marriott Beach Resort 1998 7 Avg. Beach Widths (ft) 6 5 4 3 2 1 -Jan 31-Jan 2-Mar 2-Apr 3-May 3-Jun 4-Jul 4-Aug 4-Sep 5-Oct 5-Nov 6-Dec 8 Grand Cayman Marriott Beach Resort 1999 7 Avg. Beach Widths (ft) 6 5 4 3 2 1 -Jan 31-Jan 2-Mar 2-Apr 3-May 3-Jun 4-Jul 4-Aug 4-Sep 5-Oct 5-Nov 6-Dec Lee E. Harris, Ph.D., P.E. Page 2 of 11

Grand Cayman Marriott Beach Resort 2 8 7 Avg. Beach Width (ft) 6 5 4 3 2 1 -Jan 31-Jan 2-Mar 2-Apr 3-May 3-Jun 4-Jul 4-Aug 4-Sep 5-Oct 5-Nov 6-Dec 8 Grand Cayman Marriott Resort 21 7 Avg. Beach Width (ft) 6 5 4 3 2 1 -Jan 31-Jan 2-Mar 2-Apr 3-May 3-Jun 4-Jul 4-Aug 4-Sep 5-Oct 5-Nov 6-Dec Lee E. Harris, Ph.D., P.E. Page 3 of 11

Grand Cayman Marriott Resort 22 8 7 Avg. Beach Width (ft) 6 5 4 3 2 1 -Jan 31-Jan 2-Mar 2-Apr 3-May 3-Jun 4-Jul 4-Aug 4-Sep 5-Oct 5-Nov 6-Dec Grand Cayman Marriott Resort 23 8 7 Avg. Beach Width (ft) 6 5 4 3 2 1 -Jan 31-Jan 2-Mar 2-Apr 3-May 3-Jun 4-Jul 4-Aug 4-Sep 5-Oct 5-Nov 6-Dec Note that these graphs show that there are seasonal changes in the beach width, but prior to the installation of the Reef Ball breakwater at the end of 22, the beach width was decreasing each year. In 22 the maximum beach width was only 45 feet and the minimum width was zero, and the zero beach width occurred over a much greater time period than in prior years. Following the installation of the Reef Ball breakwater (completed at the end of 22) the data to date for 23 show that the beach width reached a width in excess of 6 feet, with the minimum width of 25 Lee E. Harris, Ph.D., P.E. Page 4 of 11

feet. The fall tropical storm and hurricane season has the narrowest beach widths, which may reduce the existing beach width further. Artificial Reef Submerged Breakwater Project Design To stabilize and enhance the beach at the Grand Cayman Marriott Resort, an artificial reef submerged breakwater was recommended and installed to reduce the wave action reaching the beach. A submerged breakwater reduces the wave action that reaches the beach, thereby assisting to stabilize the shoreline. Unlike traditional breakwaters that project above the water surface and stop all wave action, submerged breakwaters allow the smaller waves to pass over the structure so that sand transport along the coast is maintained during normal conditions. During large wave events, the larger waves are forced to break on the submerged breakwater, thereby reducing the wave energy reaching the beach from large waves, and reducing the associated beach erosion. The disadvantage of submerged breakwaters is that they become less effective as their depth of submergence increases, so that they are less effective at reducing wave action during elevated water levels due to storm surge. The use of artificial reef units for a submerged breakwater also provides underwater habitat, enhancing the environment. The submerged Reef Ball artificial reef breakwater has assisted in stabilizing the shoreline by reducing the wave action that impacts and erodes the beach, especially when the waves strike and reflect from the vertical seawall. The existing reef offshore of the hotel is only sufficiently wide and high enough to assist with wave attenuation in one spot, which is where the gap between the two breakwaters was designed. The recommended and installed design shown in Figure 6 uses 5 rows of Reef Ball TM artificial reef units to provide a 3-foot wide submerged breakwater. The 3.7 to 4.5 feet high artificial breakwater units were installed in low tide water depths of 4 to 5.5 feet, so that the top of the units are slightly below the lowest normal water level (.3 to 1.8 feet)..5.5.5 5-row ReefBall Artificial Reef Submerged Breakwater.5 Survey date: 9 Feb 22.5... sand beach -9-9.5 existing reef -5.5.5..5.5 rocky bottom.5.5 seawall -9-5.5.5.5. Marriott Resort, Grand Cayman Lee E. Harris, Ph.D., P.E. Page 5 of 11

As presented in Table 1, various sizes and weights of Reef Ball TM artificial reef units are available. To obtain the highest heights and individual unit weights possible, the largest Reef Ball TM units (Ultra Balls and Reef Balls) fabricated with the maximum volume of concrete for the molds were used, resulting in each individual Reef Ball TM unit weighing approximately 4, pounds (2 tons). Microsilica and other additives were used in the concrete to increase the strength and workability plus decrease the ph of the concrete to that of marine environment. Table 1. Reef Ball TM Sizes, Weights, Volume & Number of Holes Style Width Height Weight Concrete Volume No. of Holes Ultra Ball 6 feet (1.83m) 4.5 feet (1.37m) 4 lbs (1814722 kg) 1 yard.76m 3 294 Reef Ball 6 feet (1.83m) 4 feet (1.22m) 3 lbs (136722 kg).75 yard.57m 3 294 Pallet Ball 4 feet (1.22m) 3 feet (.91m) 152 lbs (68-998 kg).33 yard.25m 3 174 Bay Ball 3 feet (.91m) 2 feet (.61m) 3755 lbs (174 kg).1 yard.8m 3 16 The sea bottom where the submerged breakwater is installed consists primarily of barren rock with some patches of sand, so that scour and settlement of the artificial reef units are not a problem. For increased stability of the structure, sleeves for fiberglass rebar were pre-cast into the Reef Ball TM units, with No. 5 fiberglass rebar driven or drilled into the bottom to provide additional resistance to sliding of the units. If desired, the central cavities of the Reef Ball TM units can be filled approximately one-third full with small rocks to provide additional weight and habitat. Field Investigations Inspections of the Reef Ball submerged breakwater constructed offshore the Marriott Resort on Grand Cayman, Cayman Islands were performed on February 6, 23 and on May 268, 23. This included inspections, surveys, and photographs of the beach areas at the property, and the beach areas to the south and north along Grand Cayman s western Seven Mile Beach shoreline. The photographs below show the condition of the beach in February 23, which increased in width from zero to over sixty feet wide following the installation of the Reef Ball breakwater. Over 2 Reef Ball units were installed in the design template, with top elevations near but below the normal low tide elevation as was designed and permitted. Lee E. Harris, Ph.D., P.E. Page 6 of 11

View North: View South: The photographs below taken in February 23 show the offshore Reef Ball breakwater: Northern breakwater: Southern breakwater at extreme low tide. The underwater photographs below show the condition of the Reef Ball units. After only 3 months, there is considerable marine growth on the Reef Ball units and several species of fish in and around the artificial reef units. Note that some of the Reef Ball units had to be fabricated shorter than the standard size, due to the shallower water depths at the south end of the breakwater. Lee E. Harris, Ph.D., P.E. Page 7 of 11

Additional Reef Balls A survey of the water depths in the vicinity of the south end of the breakwater was performed to investigate the proposed addition of 32 more Reef Ball units at the south end to increase wave protection from the SW. Special permission was required from the property owners to the south, as this extension will be located offshore of the north end of their property. The proposed extension is shown in the aerial photograph below, which would increase protection for the Marriott from waves from the southwest. Lee E. Harris, Ph.D., P.E. Page 8 of 11

December 22 Aerial Photograph showing Reef Ball breakwater: Proposed additional Reef Ball units: Other Alternatives As discussed in previous reports, there are several alternatives that can be used to stabilize and restore the beach. The most direct approach is to add sand to the beach, and this method has been employed in the past, but the sand is easily eroded away by southwest waves. Structures such as groins or a nearshore sill can be employed to assist in holding the sand in place, but these structural elements can affect the adjacent beaches, and impede the natural transport of sand along the beach. The recommended and most environmentally friendly option is an offshore submerged breakwater to reduce the wave action reaching the beach. The use of artificial reef units to form a submerged breakwater provides marine habitat, as well as allowing some of the wave action to pass through and over the breakwater so that the natural flow of sand along the beach can Lee E. Harris, Ph.D., P.E. Page 9 of 11

continue. This is the present system at the Marriott, which has been assisting with wave attenuation and shoreline stabilization since its completion at the end of 22. Recent Beach Profile Data Surveys were performed in February 23 which document the beach condition after 3 months, and are compared with the beach condition immediately following the completion of the Reef Ball breakwater in November 22, as shown in the Figures below for the 3 profile lines at the south end of the Marriott. These graphs below show the additional sand that accreted seaward of the Marriott seawall following the installation of the Reef Ball breakwater. The beach width increased from zero to 4 to 55 feet in width from November 22 to February 23, whereas the widest beach width in all of 22 was 45 feet. Recent wave action has reduced the beach widths to 25 feet at the Marriott (but even less at adjacent beaches in the area), and the current tropical storm and hurricane season may further erode the beach. However, the completed Reef Ball breakwater (and extension if added) is designed to minimize the beach erosion and assist with the stabilization of the beach at the Marriott. 6 5 4 Nov-2 Feb-3 3 2 1 Elevation (feet) -5 Profile Line A 5 1 15 2 25 Distance (feet) Profile Line A Across South End of Reef Ball Breakwater Lee E. Harris, Ph.D., P.E. Page 1 of 11

6 5 4 Nov-2 Feb-3 3 2 1 Elevation (feet) -5 Profile Line B 5 1 15 2 25 Distance (feet) Profile Line B 3 feet North of Southern End of Reef Ball Breakwater 6 5 4 Nov-2 Feb-3 3 2 1 Elevation (feet) -5 Profile Line D 5 1 15 2 25 Distance (feet) Profile Line D 13 feet North of Southern End of Reef Ball Breakwater Lee E. Harris, Ph.D., P.E. Page 11 of 11