Determining Discharge-Coefficient Ratings for Coastal Structures in Dade County Florida

Metadata:


Identification_Information:
Citation:
Citation_Information:
Originator: Eric D. Swain
Publication_Date: 199707
Title:
Determining Discharge-Coefficient Ratings for Coastal Structures in Dade County Florida
Publication_Information:
Publication_Place: Tallahassee FL
Publisher: U S Geological Survey
Online_Linkage:
Description:
Abstract:
The flows through the 16 coastal structures in Dade County, Fla., are presently computed by theoretical discharge-coefficient ratings developed from scale modeling and theoretical flow coefficients, whose accuracies for specific sites are unknown. To create more accurate discharge-coefficient ratings for the coastal structures, field measurements were taken with an Acoustic Doppler Current Profiler at each coastal structure under a variety of structure operations. The Acoustic Doppler Current Profiler is capable of measuring low and rapidly varying flows that occur at the coastal structures. The field measurements were used to develop computed discharge-coefficient ratings for the coastal structures under different flow regimes: submerged weir flow, submerged orifice flow, free weir flow, and free orifice flow. Additionally, flow hydrographs, using both the theoretical- and computed-coefficient ratings, were plotted for most of the coastal structures. The difference between the theoretical- and computed-coefficient ratings varied from structure to structure. The theoretical- and computed-coefficient ratings for submerged orifice flow were within 10 percent at structures S-22, S-25B, S-26, S-27, S-28, and S-123; however, marked differences (25 percent or greater) were seen at structures S-20F and S-21. The theoretical- and computed-coefficient ratings for submerged weir flow were within 10 percent at structures G-93, S-20F, and S-29; however, marked differences (25 percent or greater) were seen at structures S-20, S-20G, S-21, S-21A, S-25B, S-27 and S-28. The closest match to the theoretical-coefficient rating was at structure S-26, and the worst match to the theoretical-coefficient rating was at structure S-21. The significant differences between the theoretical- and computed-coefficient ratings could be a result of basing the ratings on 30 or fewer data points.
Purpose:
The objective of this study is to determine discharge ratings for 16 coastal hydraulic control structures in eastern Dade County. Discharge data are needed to quantify water that can be made available for water supply and ecosystem restoration and to calibrate regional hydrologic models.
Time_Period_of_Content:
Time_Period_Information:
Range_of_Dates/Times:
Beginning_Date: 199411
Ending_Date: 199510
Currentness_Reference: publication date
Status:
Progress: Complete
Maintenance_and_Update_Frequency: none scheduled
Spatial_Domain:
Bounding_Coordinates:
West_Bounding_Coordinate: -80.45
East_Bounding_Coordinate: -80.15
North_Bounding_Coordinate: 25.93
South_Bounding_Coordinate: 25.28
Keywords:
Theme:
Theme_Keyword_Thesaurus: none
Theme_Keyword: freshwater discharge
Theme_Keyword: surface water
Theme_Keyword: control structures
Theme_Keyword: accoustic doppler current profiler
Place:
Place_Keyword_Thesaurus: none
Place_Keyword: eastern Dade County
Place_Keyword: South Florida
Place_Keyword: Biscayne Bay
Place_Keyword: South East Coast
Place_Keyword: Florida Keys
Place_Keyword: Central Everglades
Access_Constraints: None. Raw data may need revisions.
Use_Constraints: None.
Point_of_Comments and suggestions? Contact:
Contact_Information:
Contact_Person_Primary:
Contact_Person: Eric D. Swain
Contact_Organization: U.S. Geological Survey
Contact_Position: Project Chief
Contact_Address:
Address_Type: mailing address
Address: 9100 NW 36th Street Suite 107
City: Miami
State_or_Province: FL
Postal_Code: 33178
Contact_Voice_Telephone: 305 526 2895
Contact_Facsimile_Telephone: 305 526 2881
Contact_Electronic_Mail_Address: edswain@usgs.gov
Native_Data_Set_Environment:

Data_Quality_Information:
Logical_Consistency_Report: not applicable
Completeness_Report: not applicable
Lineage:
Process_Step:
Process_Description:
Several factors make taking discharge measurements near coastal hydraulic control structures difficult. Very low velocities (0.2 foot per second) can occur, especially when the canal is significantly wider than the flow passage of the coastal hydraulic control structure. Additionally, the spatial distribution of velocities can be atypical near a coastal hydraulic control structure because the flow through the structure disrupts the normal flow lines in the canal. The Acoustic Doppler Current Profiler (ADCP) is an instrument capable of making accurate measurements under these conditions.

The ADCP has many advantages over the commonly used Price meter. An ADCP measurement can be made in minutes, as opposed to the longer time required by the Price meter. This speed allows for a more accurate collection of data in dynamic conditions, such as those encountered in this study. For example, a discharge measurement could be taken before water levels and average channel velocities have changed substantially. Another advantage of the ADCP over the Price meter is that data are collected on a continuum in the water column and cross section rather than at discrete points.

Generally, ADCP measurements were made simultaneously by the USGS and SFWMD at the coastal hydraulic control structure sites. Access to all the sites was made upstream, and a small boat was adequate in almost every situation. Boats had ADCP's mounted on their bows and faced the flow. Taglines were stretched across the canals for pulling the boat slowly across the water to obtain the measurements. Upstream and downstream stages were noted at the beginning and end of every measurement.

When gate openings were planned for a given day, discharge measurements were made repeatedly at discrete gate openings. Using the ADCP, measurements were made quickly and repeatedly during relatively rapid gate operations. All concurrent water-level, gate opening, and discharge data were collated and analyzed with a spreadsheet program. Flow regimes were identified, and a least squares fit was used to determine the best estimate of the appropriate coefficients.

Process_Comments and suggestions? Contact:
Contact_Information:
Contact_Person_Primary:
Contact_Person: Eric D. Swain
Contact_Organization: U.S. Geological Survey
Contact_Position: Project Chief
Contact_Address:
Address_Type: mailing address
Address: 9100 NW 36th Street Suite 107
City: Miami
State_or_Province: FL
Postal_Code: 33178
Contact_Voice_Telephone: 305 526 2895
Contact_Facsimile_Telephone: 305 526 2881
Contact_Electronic_Mail_Address: edswain@usgs.gov
Hours_of_Service:
Process_Date: not complete

Distribution_Information:
Distributor:
Contact_Information:
Contact_Person_Primary:
Contact_Person: Eric D. Swain
Contact_Organization: U.S. Geological Survey
Contact_Position: Project Chief
Contact_Address:
Address_Type: mailing address
Address: 9100 NW 36th Street Suite 107
City: Miami
State_or_Province: FL
Postal_Code: 33178
Contact_Voice_Telephone: 305 526 2895
Contact_Facsimile_Telephone: 305 526 2881
Contact_Electronic_Mail_Address: edswain@usgs.gov
Hours_of_Service: 8:00 AM - 5:00 PM
Resource_Description:
Distribution_Liability: The data have no implied or explicit guarantees.
Standard_Order_Process:
Digital_Form:
Digital_Transfer_Information:
Format_Name:
Digital_Transfer_Option:
Online_Option:
Computer_Contact_Information:
Network_Address:
Network_Resource_Name:
Fees:

Metadata_Reference_Information:
Metadata_Date: 19980804
Metadata_Comments and suggestions? Contact:
Contact_Information:
Contact_Person_Primary:
Contact_Person: Jo Anne Stapleton
Contact_Organization: U.S. Geological Survey
Contact_Address:
Address_Type: mailing address
Address: 521 National Center
City: Reston
State_or_Province: VA
Postal_Code: 20192
Contact_Voice_Telephone: 703 648 4592
Contact_Facsimile_Telephone: 703 648 4614
Contact_Electronic_Mail_Address: jastapleton@usgs.gov
Metadata_Standard_Name: FGDC Content Standard for Digital Geospatial Metadata
Metadata_Standard_Version:
19940608


Generated by mp on Tue Sep 01 13:36:22 1998