An in-depth analysis of the sediment processes is required to determine if the detached breakwaters are enhancing the natural spawning habitats for the American Horseshoe Crabs along Money Island. Since the American Horseshoe Crab prefers to spawn along beaches with certain elevation and grain-size composition characteristics, it is important to compare the sediment deposition pre and post-project implementation of the detached breakwaters to evaluate if their preferred criteria are achieved due to the installations of the five detached breakwaters. For this project, various sediment components were evaluated utilizing Geographic Information Systems (G.I.S) techniques and programs (ArcGIS pro) to conduct this sediment evaluation. In total, eleven different G.I.S maps were produced to evaluate different aspects of sediment transport (longshore, cross-shore, shoreline change, etc.) over the course of 20 years at Money Island. These maps were generated to deliver a physical display of the sediment change within the project delineation and provide accurate data and integers to utilize for sediment volume change calculations due to NJDEP's Blue Acres Project. The methodology utilized for each G.I.S map is found below, and the corresponding map can be found with it. An analysis of the map is explained in this website's Results (Sediment) section!
Special note: All data utilized for this sediment analysis was obtained through Stockton University's Coastal Research Center, Stockton University Marine Field Station, or New Jersey Geographic Information Network (NJGIN) open source data pool. All maps and G.I.S products are listed below in order of project completion.
Generated in the Google Earth Pro application
Derived from the information presented in the Money Island Project's original plan documentation written by Rich Weggel in February 2021.
The conceptual model was created to display a general assumption of longshore sediment transport (littoral drift) along Money Island due to the installations of the five detached breakwaters.
Boxes were created to display five littoral cells to which future analysis can be completed in the sediment volume change calculations (seen below).
The model displays areas of anticipated erosion (red coloration) and areas of accumulation (green coloration), while arrows indicate direction of movement
Generally, sediment transport is anticipated to come from the Southern portion of the beach (Nantuxent point), and head in a North direction towards the Nantuxent Creek. With significant erosion happening on the Southern point of the beach, and significant accumulation occurring landward of the breakwaters and the adjacent littoral cells to the breakwaters.
Note: this is just a conceptual model, not a final product of the sediment analysis.
The first portion of the Money Island sediment analysis consisted of shoreline change maps to display where the "0" foot elevation had begun. Three separate shoreline change maps were produced to show the gradual change since 2007. These maps depict what the shoreline looked like when occupied by residential plots, after NJDEP's removal of anthropogenic construction and debris, and after implementing the detached breakwaters and beach nourishment project.
Shoreline Change since 2007:
Data was derived from NJGIN (Coastline (2007) of New Jersey & Coastline (2012) of New Jersey) and from Dr. Shah Alam Khan: Assistant Professor of Coastal Zone Management, Stockton University (Shoreline 2022).
Downloaded all the shapefiles and imported them into an ArcGIS Pro project
Change the symbology to represent a gradient color scheme (blue) that shows the changes over time. Each line was given its own shade of blue (lighter colors represent the youngest coastline)
Added a Definition Query to the Coastline (2007) of New Jersey and the Coastline (2012) of New Jersey files to display only the coastline along Money Island based on the FID of each line.
Shoreline Change since 2017:
Data derived from Dr. Shah Alam Khan: Assistant Professor of Coastal Zone Management, Stockton University (Shoreline 2017, Shoreline 2019, & Shoreline 2022)
Downloaded all the shapefiles from a shared Google Drive and imported them into an ArcGIS Pro project.
Adjusted the symbology of the three shapefiles to match the symbology utilized in the Shoreline Change since 2007 project. A gradient blue color scheme was chosen where all lines were given a different shade of blue (lighter lines represent younger shorelines).
Shoreline Change (Sept. 2022- March 2023):
Data derived from the Stockton University Coastal Research Center Digital Elevation Maps
Imported Digitial Elevation Maps (Raster dataset) from September 2022 and March 2023 into an ArcGIS Pro project.
Utilized the Contour (3D Analyst Tool) in the geoprocessing toolbox to create a feature class of contours from the raster surfaces provided by the D.E.Ms.
Once contour feature classes were generated (Contours_Sept2022 & Contours_March2023), a definition query was created for each feature class to which contour equals "0".
"0" indicates 0-foot elevation or the shoreline during data acquisition via triangulation with a Total-Station tripod and Global Position Systems (GPS) collection with an RTK GPS unit.
Changed the symbology of both feature classes to display thicker lines with colors that vary from each other (Teal and Gold). Teal is March 2023, while Gold is September 2022.
Then, I re-added the two generated contour feature classes into the same ArcGIS Pro project (four total contour files in one project).
Added a definition query to the two newly imported contour feature classes where contour equals 1 or -1.
Adjusted the symbology of each contour feature class to match the symbology of the "0-ft" file mentioned.
The "1" and "-1" contours were adjusted to a dashed line of smaller thickness.
"1" and "-1" were added to display a 1-foot overlap in elevation for the Money Island coastline.
A Money Island breakwater shapefile was also added (provided by Dr. Shah Alam Khan) to show the project area.
Shoreline Change (2007-2022)
Shoreline Change (2017-2022)
Shoreline Change Sept. 2022 - March 2023).
The second portion of the sediment analysis was conducted due to the results of the shoreline change maps mentioned above. With unexpected results in the shoreline change map (Sept. 2022- March 2023), further evaluation was presented in a contour change map displaying elevations below sea level to see if accumulation occurred between the breakwaters and the shoreline.
Data for this project was derived from the Stockton University Coastal Research Center D.E.M maps for September 2022 and March 2023.
Utilizing the Contour_Sept2022 and Contour_March2023 feature classes generated in the shoreline change project, a new definition query was generated where contours equal -1 through -5.
Negative five was chosen since that is roughly the depth where detached breakwaters were constructed.
The symbology of the feature classes was also adjusted to match the shoreline change maps, where September 2022 was indicated in gold and March 2023 was displayed in teal.
The Money Island breakwaters shapefile was also added to show impacted areas from the coastal structures.
To avoid confusion about overlapping contour lines, an ArcGIS Pro layout was generated where each contour shapefile was added as its own individual map frame to show a side-by-side comparison.
Digital elevation models (D.E.Ms) were generated for the Money Island project to display changes in elevation from September 2022 through March 2023. D.E.Ms are a way to represent the earth's bare ground (elevation) in a 2-D format without the interference of natural features such as vegetation, structures, etc. For Money Island in particular, the D.E.Ms utilized for the sediment analysis consisted of a series of points collected by the Stockton University Coastal Research Center via triangulation from a Total-Station tripod and RTK GPS point collection from professional swimmers. All points collected were either along the beachfront or seaward of the beachfront.
ArcGIS Pro project details:
Created a new ArcGIS Pro project, separated from the shoreline change and contour work titled "MI_Elevation_Change."
Imported the two D.E.M. models created by the Stockton University Coastal Research Center.
Adjusted the symbology of both raster datasets to show a "stretch" color ramp pattern from blue to red.
Blue displays lower elevations, while red is higher elevations.
Once the symbology was altered for each raster dataset, the stretch color ramp "advanced labeling" was adjusted to match each other. Eleven "intervals" were chosen between -17.95 foot NAVD88 and 8.18 foot NAVD88.
Each D.E.M was created into its own ArcGIS Pro Layout, adding the shorelines generated from the shoreline change project ("0-ft" elevation lines).
To display where the shoreline is in reference to the D.E.M products.
D.E.M (September 2022)
D.E.M (March 2023)
Sediment Volume Change maps were derived from the two D.E.Ms the Stockton University Coastal Research Center provided.
The goal was to show the changes in elevations throughout project delineation in one map without viewing two separate D.E.M models.
Two sediment volume change maps were created to show areas of net sediment accumulation and net sediment erosion between September 2022 and March 2023 and the amount of sediment gained or lost in cubic feet throughout the Money Island Project area.
Net Gain/Net Loss Analysis:
Utilizing the two D.E.Ms already created from projects mentioned above, the Cut Fill (3D Analyst Tool) geoprocessing tool was used to create a new raster dataset that will display changes in value between inputted feature classes.
September's D.E.M was selected as the "Input before raster surface," while March's D.E.M was selected as the "Input after raster surface."
Once the new feature class was created (CutFill_Test), a field was added to the attribute table called "Volume_Inverse"
The field was then calculated so that the Volume_Inverse field would equal "Volume * -1" to get the inverse of the Cut_Fill Volume.
This is because the Cut Fill tool has an opposite reaction, were positive volumes are net losses, while negative volumes are net gains in sediment.
A second field was then added to the attribute table titled "Changed"
This field was then calculated so that all positive "Volume_Inverse" integers would be classified as "Gain" while the negative "Volume_Inverse" integers would be "Loss"
Once the new raster dataset was generated, the symbology was adjusted to be a "unique values" color scheme with two "values" based on the newly created "Change" filed attribute
A Green and Red color scheme was also added for the map to highlight areas of Net Gain in green and Net Loss in red.
Cubic Feet Changes:
In the same ArcGIS Pro project, a new raster dataset was generated utilizing the Minus (3D Analyst Tool) geoprocessing tool, which subtracts the value of a second input raster from the value of an original input raster
For the Money Island D.E.Ms, the "input raster or constant value 1" was selected as the D.E.M from March 2023, while the "input raster or constant value 2" was selected as the D.E.M from September 2022.
As in, the Minus Tool is subtracting the following equation: Volume_March2023 - Volume_September2022= Change in Volume.
With the new D.E.M created from the Minus Geoprocessing Tool, the symbology was changed to a "Classify" color ramp (Red to Green) based on 10 "classes" in cubic feet.
Red indicates loss volumes in cubic feet, while green indicates gained volumes in cubic feet.
The classes identified between 0.2 and -0.2 represent No Change in volume (No Loss or Gain).
This map now shows individual volume changes rather than losses and gains.
The Money Island breakwaters shapefile & shoreline of 2023 were also added.
Sediment Volume Change (Net Gain/Loss)
Sediment Volume Change (Amount in Cubic Feet)
The following digital elevation maps were completed using a combination of data provided by the Stockton University Coastal Research Center and the Stockton University Marine Field Station. Methods for data collection included RTK GPS rover, Total-Station triangulation with prisms, Mulitbeam sonar scanning with a R2 Sonic Echosounder, and lidar scanning with a Dynascan 250 MDL. The collected data was then processed utilizing a series of applications including: Leica Geoffice, Leica Infinity, Qinsy, Qimera, and ArcGIS Pro. The data for September's D.E.M was collected in November 2022, while the D.E.M for June 2023 was generated using data collected in March and June 2023.
A patch test was run to calibrate the results of the lidar and Multibeam data for corrections in pitch, roll, and heading (yaw) to gather exact positioning.
These mobile scanning techniques come equipped with an Inertial Measurement Unit (IMU), which can account for the movement of the vessel/vehicle during data collection to determine exact locations of the returned "pings" or soundings.
For the Patch Test, a total of 8 lines were run in a parking lot (Dynascan 250 was mounted to a vessel on a trailer prior to deployment in the Delaware Bay).
Once the data was collected and calibration were accounted for utilizing the Patch Tests, the data was then cleaned to remove any unwanted "pings" or points collected.
Specifically, a blanking filter was used to remove points collected for the boat gunnel and any sunspots/height identifiable noise.
The "slice editor" tool in Qimera was primarily utilized to remove unwanted point collected from the lidar and Multibeam data.
Prior to formulating a map in ArcGIS Pro, both the mulitbeam and lidar points were exported as XYZ text files.
Once rhe XYZ text files were imported into an ArcGIS Pro project, any gaps within the files were filled in using RTK GPS points collected via handheld rovers collected by the Stockton University Coastal Research Center.
The "Create TIN" geoprocessing tool as then utilized to create an editable TIN surface from the XYZ and RTK GPS files.
Once the TIN was created, minor cleaning was completed using the "edit TIN" features
A Blue-Red stretch symobology was then added to the created TIN to display lower elevations in blue and higher elevations in red (reference to NAVD88).
D.E.M (September 2022)
D.E.M (March 2023)
The final portion of the Money Island G.I.S Sediment Analysis was conducting a sediment volume change (calculations) for the Money Island Coastline based on the conceptual model generated from the Rich Weggel engineering report in February 2021. The sediment volume change calculation project aimed to create littoral cells in different sections of the shoreline to see changes in each cell and to observe if the changes match the conceptual model's prediction. This volume calculation map was generated utilizing the output raster "Surface Volume Change" from the Minus Geoprocessing Tool mentioned above.
Data Analysis Portion:
To highlight the littoral cells identified in the conceptual model, five separate feature class "polygons" were created based on the output raster from the Minus Geoprocessing Tool.
Once the five polygons or littoral cells were generated, the Extract by Mask Geoprocessing Tool was used to extract the raster's contents corresponding to areas defined by a mask.
The Extract by Mask Tool was conducted for all five polygons.
The newly created five individual raster datasets correspond directly with the littoral cells' size and shape.
The Surface Volume (3D Analyst Tool) Geoprocessing Tool was then used to calculate the area and volumes of the five littoral cells above or below a plane
The "input surface" was selected as each of the five littoral cells
The "output text file" is a CSV file named after the corresponding cell
The Surface Volume Tool was run twice for each littoral cell:
Once "Above the Plane" and once "Below the Plane"
For this analysis, the "Plane" is set to "0"; therefore, the Surface Volume Tool is calculating the amount of sediment above and below "0" based on the sediment volume change from September 2022 through March 2023.
Or, the tool calculates the amount of sediment gains and losses for each cell and exports them as a CSV file, which can later be saved as an Excel file.
Inside the newly formed Microsoft Excel files, a simple calculation was run to determine the actual volume change in each littoral cell
Volume Change (Cubic Feet) = Above the Plane Volume - Below the Plane Volume
Cubic Feet was then converted to Cubic Yard by the following equation: Cubic Feet/27 = Cubic Yards
Back in the ArcGIS Pro project: the five littoral cells/polygons were adjusted to match the outcome of the volume change calculations from the Excel files
Each polygon's attribute table (Littoral Cell 1 through Littoral Cell 5) had three fields added, including:
Name (Text)
Change_Cubic_ft (Double & Numeric)
Change_Cubic_yard (Double & Numeric)
The corresponding data from the Excel files were then transferred to the ArcGIS Pro project for each littoral cell.
Map Making Portion:
To show the littoral cells, plus a little overlap region, in one shapefile, a new feature class polygon was created and titled "Littoral_Zone" and matched the outline of the Minus Tool output raster & the Littoral Cell Polygons.
The Extract by Mask Geoprocessing Tool was run to extract the contents of the "Surface Volume Change" output raster to match the mask of the "Littoral_Zone" polygon.
The "Surface Volume Change" output raster had the symbology changed already, so no alterations were made. The same "classify" color ramp was utilized with the same amount of "classes" and values associated with those classes.
This new raster in the shape of the "Littoral_Zone" polygon was then adjusted to have a 30.0% Transparency.
The symbology of each littoral cell was changed to be unique colors from each other to distinguish the areas of each cell. (Black, Pink, Purple, Teal, & Yellow were chosen).
Each cell did not have a fill "color" but had an "outline color"
Each Cell was also "labeled" to where the "Expression = $feature.Change_Cubic_yard"
The cubic yard values were present with a "halo" to make them stand out from the raster dataset presented behind the cells.
To further examine the data presented in the project layout, the Money Island breakwaters shapefile, 2023 shoreline, and arrows indicating the direction of sediment transport were added.
Text boxes indicating where Littoral Cell 1 began, and Littoral Cell 5 ended were also added in case of confusion.