(1) Hillsborough
County North of State Road 60, and Pasco and Pinellas Counties Salt Water
Intrusion within this area has not been regional in nature, but is of localized
concern in some coastal areas. The District has chosen the North Pinellas,
Southwest Pasco and Northwest Hillsborough Counties region as the priority area
for the establishment of Salt Water Intrusion Minimum Aquifer Levels ("SWIMAL")
to prevent regional seawater intrusion because of the availability of data and
the potential for future intrusion. The SWIMALs for the Upper Floridan aquifer
shall be established as follows:
(a) The
location of the SWIMAL sites serves to monitor the area where early signs of
regional salt water intrusion can best be detected.
(b) The SWIMALs shall be established by
setting levels in coastward transects of wells whose potentiometric levels
define the Long-term average hydraulic gradient of the Upper Floridan aquifer
potentiometric surface.
(c) The
Salt Water Intrusion Minimum Aquifer Levels are as set forth in the following
table. Aquifer levels are deemed to be below the SWIMAL when the Long-term
average elevation is below the SWIMAL.
|
TABLE 8-4 SALT WATER
INTRUSION
|
|
MINIMUM AQUIFER LEVELS
|
|
Well Name
|
Saltwater Intrusion Minimum Aquifer Level (feet
NGVD)
|
|
Sheldon Road Deep (RMP-16D)
|
7.7
|
|
RMP-13D
|
16.4
|
|
RMP-8D1
|
26.8
|
|
Tarpon Rd. Deep
|
9.9
|
|
SWI-18S
|
14.8
|
|
201-M
|
13.7
|
|
EW 2S Deep
|
10.3
|
(2) SWUCA Salt Water Intrusion Minimum
Aquifer Level.
(a) The District has determined
that ground water withdrawals in the SWUCA have contributed to water level
declines that advance saltwater intrusion. The coastal portion of the SWUCA in
southern Hillsborough, Manatee and northern Sarasota counties (the Most
Impacted Area or MIA) is a priority area for the establishment of minimum
aquifer levels because of its proximity to the saltwater interface and the
large effect on interface movement caused by lowering of the potentiometric
surface in this area. The Salt Water Intrusion Minimum Aquifer Level (SWIMAL)
is established to stabilize regional water level declines so that long-term
management efforts can slow the rate of regional saltwater intrusion in the
MIA. This is based on an average value to address the regional nature of the
problem and avoids the potential for localized lowering of a minimum
level.
(b) The SWIMAL over the
surface of the MIA is 13.1 feet (National Geodetic Vertical Datum of 1929 or
NGVD 1929). The SWIMAL is derived using the method set forth in paragraph
(2)(c) below.
(c) The reference
period for which the SWIMAL is calculated is the period 1990 through 1999. Ten
wells from within or adjacent to the MIA (Table 8-5), are used to determine the
minimum level. The annual average elevation for each of the years 1990 through
1999 is established utilizing monthly water level data for each of the wells.
The annual averages over the period are then used to calculate the decadal
average for the period. The 1990-99 average Upper Floridan aquifer
potentiometric surface of the MIA is constructed by calculating the average of
these annual average values weighted spatially using the Thiessen polygon
methodology. The resulting Minimum Level over the surface of the MIA is 13.1
feet (National Geodetic Vertical Datum of 1929).
Table 8-5: Wells utilized to determine the Salt Water
Intrusion Minimum Aquifer Level.
|
Site
|
|
|
|
Number
|
Sequence Number
|
Site Name
|
|
564
|
0
|
KIBLER DEEP
|
|
87
|
|
ROMP 123 Hawthorn/Ocala
HAWTHORN/OCALA
|
|
10914
|
0
|
ROMP 50 TAMPA/OCALA
|
|
10883
|
0
|
ROMP TR 10-2 TAMPA
|
|
287
|
0
|
ROMP TR 7-1 TAMPA
|
|
10926
|
0
|
ROMP TR 7-4
Suwannee/Ocala
SUWANNEE/OCALA
|
|
10920
|
0
|
ROMP TR 8-1 Upper Avon
Park
PARK
|
|
10909
|
1
|
ROMP TR 9-3 Ocala/Avon
Park
|
|
561
|
0
|
SARASOTA 9 DEEP
|
|
456
|
0
|
VERNA T 0-4
|
(d)
Implementation of The SWUCA Salt Water Intrusion Minimum Aquifer Level - The
SWIMAL shall be used to gauge the status of the ground water resource with
respect to saltwater intrusion in the region. Determining the status of the
rate of movement of the saltwater interface shall be based on comparison of the
average Floridan aquifer water level over the MIA with the Floridan aquifer
minimum level over ten-year moving windows of time. The ten-year average water
level for a particular year shall be calculated as the average water level for
that year and the previous nine years. The process of calculating the ten-year
average is the same as described in paragraph (c), above, for calculating the
minimum level.
(e) Compliance - The
objective of the District's management efforts is for the ten-year moving
annual average water level to fluctuate in a range at or above the minimum
level. The minimum level is achieved if the ten-year moving annual average
water level has fluctuated at or above the minimum level for a minimum of five
consecutive years. Once the minimum level is achieved, the minimum level is no
longer met when the ten-year moving annual average water level falls below the
minimum level for more than two consecutive years. Then, the five consecutive
years above the minimum level is again required for
compliance.
(3)
Dover/Plant City Water Use Caution Area Minimum Aquifer Level.
(a) The District has determined that
groundwater withdrawals in the Dover/Plant City area have contributed to water
level declines that are significantly harmful to the water resources of the
area. The Minimum Aquifer Level is established as part of a comprehensive
management program intended to arrest water level declines during frost/freeze
events to minimize the potential for impacts to existing legal uses and
sinkhole occurrence.
(b) The
Minimum Aquifer Level is the 10 ft. potentiometric surface elevation (NGVD
1929) at District Well DV-1 Suwannee, located as shown in Figure 8-4. The
Minimum Aquifer Level is the level below which the greatest impact occurred in
terms of well failures and sinkholes during the 2010 frost/freeze
event.
(c) To address the effects
of local and regional groundwater withdrawals and the variable hydrogeologic
factors within the region, a Minimum Aquifer Level Protection Zone is
established. The Minimum Aquifer Level Protection Zone is the area within the
30 ft. drawdown contour that resulted from the January, 2010 frost/freeze
event, as shown in Figure 8-4.
(d)
Compliance with the Minimum Aquifer Level is evaluated annually using a
groundwater flow model simulation of a frost/freeze event and the effects of
the event on aquifer water levels in the Dover/Plant City Water Use Caution
Area. If the resulting potentiometric level is at or above 10 ft. (NGVD 29) at
District Well DV-1 Suwannee, the Minimum Aquifer Level is met. If the resulting
level is below 10 ft. (NGVD 1929) at District Well DV-1 Suwannee, the Minimum
Aquifer Level is not met.
Figure 8-4. Minimum Aquifer Level District Well DV-1 Suwannee
and Minimum Aquifer Level Protection Zone
Click
here to view image
Notes
Fla. Admin.
Code Ann. R. 40D-8.626
Rulemaking Authority 373.044, 373.113, 373.171 FS. Law
Implemented 373.036, 373.042, 373.0421, 373.709
FS.
New 8-7-00, Amended
1-1-07, 6-16-11, Amended by
Florida
Register Volume 48, Number 021, February 1, 2022 effective
2/17/2022.
New 8-7-00, Amended 1-1-07, 6-16-11,
2-17-22.