Front Cover

Group Title: Conservation area land management (CALM) plans
Title: President's park
Full Citation
Permanent Link: http://ufdc.ufl.edu/UF00090230/00019
 Material Information
Title: President's park
Series Title: Conservation area land management (CALM) plans
Physical Description: Book
Language: English
Creator: Facilities Construction & Planning, University of Florida
Publisher: Facilities Construction & Planning, University of Florida
Place of Publication: Gainesville, Fla.
 Record Information
Bibliographic ID: UF00090230
Volume ID: VID00019
Source Institution: University of Florida
Holding Location: University of Florida
Rights Management: All rights reserved by the source institution and holding location.


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Table of Contents
    Front Cover
        Page 1
        Page 2
        Page 3
        Page 4
        Page 5
        Page 6
        Page 7
        Page 8
Full Text

University of Florida Conservation Area Land Management Plan
President's Park


President's Park is a 4.1-acre hardwood hammock located behind the President's house between
University Avenue and S.W. 2nd Street. The property was classified as Conservation in the Campus
Master Plan 2000 2010. Since the park is considered to be part of the President's residence, it is
not generally open to the public, nor to students and faculty.

Natural Areas Inventory

Water Resources
President's Park is bisected by an unnamed creek, which flows for approximately 430 ft on the
property. This creek is a tributary of Hogtown Creek, the primary drainage feature for most of the
older portions of Gainesville. As with many of the creeks in the Gainesville area, Hogtown Creek is
a seepage stream that receives almost constant flow from the surficial aquifer. Seepage streams are
common in stream to sink watersheds, where streams cut through sands and clays and then empty
into sinkholes that recharge the aquifer. Hogtown Creek drains into Surgarfoot Prairie (Haile Sink), a
wetland sink where eventually most of Gainesville's stormwater recharges the Floridan aquifer.
During rainfall events these creeks are augmented by sheet flow and routed stormwater, which is
when major stream bank erosion and sedimentation occurs.

This unnamed creek receives much of its flow from the residential neighborhoods north of
University Avenue. The creek's banks are fairly eroded around the entry into the Park, due to the
high velocity of the water as it enters the property. This velocity results from the lack of upstream
stormwater retention, which would help treat the water coming off of impervious surfaces and
reduce in-stream sedimentation accumulation. In at least two areas fences that trap trash and
landscape debris cross the creek. Regular maintenance is needed to keep these fences clear and to
not back up water on upstream portions of the Park.

Unnamed Creek

Natural Communities
President's Park is a comprised primarily of a mesic / upland-mixed hardwood forest with a small
area of bottomland forest running through it. Due to the relatively small size of the property,
biodiversity is limited by substantial edge effects. Additionally, the site is impacted by non-native
invasive plant species, resulting in a native under story that is being crowded out. In larger, less
strenuous conditions mesic forests typically support significant wildlife and plant diversity, which
result from the nutrient rich nature of hardwood forests and flowering and fruiting plants.

Plant Species
The tree canopy of the park is made up of southern red oak, hackberry, laurel cherry, water oak,
cabbage palm, winged elm, black cherry, pignut hickory, southern magnolia, sweetgum, Florida
maple, red maple, devil's walking stick, redbud, eastern hophombeam, loblolly pine, live oak, and
swamp chestnut oak.

Invasive Non-Native Plant Species
The creek and surrounding residential neighborhoods have been the source for invasive, non-native
plants, of which University staff have documented the following list on site: Cat-Claw Vine,
Scratchthroat, Air Potato, Elephant Ear, White-flowered, wandering Jew, camphor tree, Chinese
privet, Japanese privet, Glossy privet.

Animal Species
Since the President's Park is surrounded by residential land uses and is relatively small in size,
terrestrial usage by mammals is limited to cats, dogs, raccoons, gray squirrels and armadillos. Other
animals typically found in mesic harwood systems, but which have not been documented on the
property, include: slimy salamander, Cope's gray treefrog, bronze frog, box turtle, eastern glass
lizard, green anole, broadhead skink, ground skink, red-bellied snake, gray rat snake, rough green
snake, coral snake, woodcock, barred owl, pileated woodpecker, shrews, eastern mole, wood rat,
cotton mouse, gray fox, and white-tailed deer.

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Soils Inventory
In general, mesic upland mixed hardwood forests occur on rolling hills that often have limestone or
phosphatic rock near the surface and occasionally as outcrops. Soils are generally sandy-clays or
clayey sands with substantial organic and often calcareous components. The topography and clayey
soils increase surface water runoff, although this is counterbalanced by the moisture retention
properties of clays and by the often thick layer of leaf mulch which helps conserve soil moisture and
create decidedly mesic conditions (FNAI).

The following soil information for on-site soils was gathered from the Soil Survey of Alachua
County (1985).

Arredondo Fine Sand (0-5% slope)
This nearly level to gently sloping, well-drained soil is in both small and large areas of uplands.
Slopes are smooth to complex. Typically, the surface layer is dark grayish brown fine sand about 8
inches thick. The subsurface layer is fine sand to a depth of 49 inches.

Blichton Sand (Urban Land Complex)(0-5% slope)
This gently sloping, poorly drained soil is on gently rolling uplands. Slopes are slightly convex. The
areas are mostly irregular in shape and elongated and range from 10 to 40 acres. Typically, the
surface layer is dark brown sand about 6 inches thick.

Millhopper Sand (Urban Land Complex)(0-5% slope)
This nearly level to gently sloping, moderately well drained soil is in small and large irregularly
shaped areas on uplands and slightly rolling knolls in the broad flatwoods. Typically, the surface
layer is dark grayish brown sand about 9 inches thick. The subsurface layer is sand or fine sand
about 49 inches thick.

Cultural and Passive Recreational Resources
President's Park is not open to the public, thus the typical amenities like trails, benches and picnic
tables are not applicable within the scope of this plan. There are no known archeological or historic
sites within the Park.

Future Improvements

As the name implies, this area is considered to be a Nature Park. However, the Park is part of the
President's residence and is inaccessible to the general public. The primary management activity that
needs to be addressed is dealing with the invasive non-native plants that are overtaking the under and
over story of the property. These invasives are not only a problem on site, but since this site is
upstream in the Hogtown basin, the site serves as a seed source for downstream areas. Habitat
enhancements like bird and bat boxes and wildlife friendly plantings are recommended.

Maps on the following pages:
1. Aerial Photo
2. Water Resources
3. Natural Communities
4. Soils

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