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Home My WebLink AboutMAP UNIT DESCRIPTIONSCustom Soil Reso Report Map Unit Legend GGANNE By St Lude.Cavf . I Map Unit Symbol Map Unit Name I Acres in AOI Percent of AOI 32 Pineda sand, 0 to 2 percent slopes I 0.3 48.3% 37 Riviera sand, frequently ponded, 0 to 1 percent slopes 0.3 51.7% Totals for Area of Interest 0.7 100.0% Map Unit Description The map units delineated on the detailed soil maps in a soil survey represent the soils or miscellaneous areas in the surv4 area. The map unit descriptions, along with the maps, can be used to determine j he composition and properties of a unit. A map unit delineation on a soil map rE major kinds of soil or miscellaneous ar according to the taxonomic classificati( class there are precisely defined limits landscape, however, the soils are natu characteristic variability of all natural pl observed properties may extend beyor Areas of soils of a single taxonomic cic including areas of other taxonomic cla,, up of the soils or miscellaneous areas components that belong to taxonomic )resents an area dominated by one or more as. A map unit is identified and named �� of the dominant soils. Within a taxonomic 1)r the properties of the soils. On the it phenomena, and they have the �nomena. Thus, the range of some I the limits defined for a taxonomic class. s rarely, if ever, can be mapped without ;es. Consequently, every map unit is made )r which it is named and some minor asses other than those of the major soils. Most minor soils have properties similar to those of the dominant soil or soils in the map unit, and thus they do not affect I se and management. These are called noncontrasting, or similar, components. They may or may not be mentioned in a particular map unit description. Other minor components, however, have properties and behavioral characteristics divergent enough to affect use or to require different management. These are called contrasting, or dissimilar, components. They generally are in small areas and could not be mapped separately because of the scale used. Some small areas of strongly contrasting soils or miscellaneous areas are identified by a special symbol on the maps. If included in the database for a given area, the contrasting minor components are identified in the map unit descriptions along with some characteristics of each. A few areas of minor components may not have been observed, and consequently they are not mentioned in the descriptions, especially where the pattern was so complex that it was impractical to make enough observations to identify all the soils and miscellaneous areas on the landscape. The presence of minor components in a map unit in no way diminishes the usefulness or accuracy of the data. The objective of mapping is not to delineate pure taxonomic classes but rather to separate the landscape into landforms or landform segments that have similar use and management requirements. The delineation of such segments on 'the map provides sufficient information for the development of resource plans. If intensive use of small areas is planned, however, 9 Custom Soil Resource Report onsite investigation is needed to define and areas. An identifying symbol precedes the map unit r Each description includes general facts about properties and qualities. Soils that have profiles that are almost alike n differences in texture of the surface layer, all t horizons that are similar in composition, thickr Soils of one series can differ in texture of the salinity, degree of erosion, and other characte basis of such differences, a soil series is divil shown on the detailed soil maps are phases c commonly indicates a feature that affects use; silt loam, 0 to 2 percent slopes, is a phase of11 the soils and miscellaneous ne in the map unit descriptions. e unit and gives important soil ike up a soil series. Except for e soils of a series have major .ss, and arrangement. urface layer, slope, stoniness, ristics that affect their use. On the ed into soil phases. Most of the -areas ,f soil series. The name of a soil phase or management. For example, Alpha :he Alpha series. Some map units are made up of two or more major soils or miscellaneous areas. These map units are complexes, associations, or undifferentiated groups. A complex consists of two or more soils or r pattern or in such small areas that they canr The pattern and proportion of the soils or mi in all areas. Alpha -Beta complex, 0 to 6 per( ;ellaneous areas in such an intricate be shown separately on the maps. ,Ilaneous areas are somewhat similar t slopes, is an example. An association is made up of two or more geographically associated soils or miscellaneous areas that are shown as one unit on the maps. Because of present or anticipated uses of the map units in the survey area, it was not considered practical or necessary to map the soils or mliscellaneous areas separately. The pattern and relative proportion of the soils o'r miscellaneous areas are somewhat similar. Alpha -Beta association, 0 to 2 percent slopes, is an example. An undifferentiated group is made up of h that -could be mapped individually, but are I nterpretations can be made for use and r of the soils or miscellaneous areas in a m be made up of only one of the major soils up of all of them. Alpha and Beta,soils, 01 Some surveys include miscellaneous material and support little or no veget or more soils or miscellaneous areas apped as one unit because similar inagement. The pattern and proportion )ped area are not uniform. An area can r miscellaneous areas, or it can be made 2 percent slopes, is an example. . Such areas have little or no soil Rock outcrop is an example. Custom Soil Resource Report St. Lucie County, Florida 32—Pineda sand, 0 to 2 percent slopes Map Unit Setting National map unit symbol: 2x1 nb Elevation: 0 to 100 feet Mean annual precipitation: 47 to 5 Mean annual air temperature: 70 t Frost -free period: 355 to 365 days Farmland classification: Farmland! inches 77 degrees F of unique importance Map Unit Composition Pineda and similar soils: 85 percent Minor components: 15 percent Estimates are based on observation. Description of Pineda descriptions, and transects of the mapunit. Setting Landform: Drainageways on marine terraces, flats on marine terraces Landform position (three-dimensional): Tread, dip, talf Down -slope shape: Linear ' Across -slope shape: Linear, concave Parent material: Sandy and loamy marine deposits Typical profile A - 0 to 5 inches: sand E - 5 to 99 inches: sand Bw - 99 to 35 inches: sand Btg/E - 35 to 38 inches: sandy loam Big - 38 to 60 inches: sandy, loam Cg - 60 to 80 inches: loamyI , sand Properties and qualities Slope: 0 to 2 percent Depth to restrictive feature: I More than 80 inches Natural drainage class: Poorly drained Runoff class: Very high Capacity of the most limiting layer to transmit water (Ksat): Moderately low to moderately high (0.06 to 0.20 in/hr) Depth to water table: About 0 to 12 inches Frequency of flooding: None Frequency of ponding: None Calcium carbonate, maximum in profile: 4 percent Salinity, maximum in profile: Nonsaline to very slightly saline (0.0 to 2.0 mmhos/cm) Sodium adsorption ratio, maximum in profile: 4.0 Available water storage in. profile: Low (about 4.6 inches) Interpretive groups Land capability classification (irrigated): None specified Land capability classification (nonirrigated): 3w Hydrologic Soil Group: C/D 10 Custom Soil Resource Report Forage suitability group: Sandy olver loamy soils on flats of hydric or mesic lowlands (G155XB241 FL) Other vegetative classification: Slough (R155XY011 FL) Hydric soil rating: Yes Minor Components Malabar Percent of map unit: 6 percent Landform: — error in exists on i— Landform position (three-dimensional): Tread, dip, talf Down -slope shape: Linear, concave Across -slope shape: Linear, concave Ecological site: Slough (R155XY011 FL) Other vegetative classification: (Slough (R155XY011 FL) Hydric soil rating: Yes I Wabasso I Percent of map unit. 5 percent Landform: Flatwoods on marine terraces Landform position (three-dimensional) - Tread, talf Down -slope shape: Linear Across -slope shape: Linear Other vegetative classification:* South Florida Flatwoods (R155XY003FL) Hydric soil rating: No ; Valkaria Percent of map unit: 2 percent Landform: Drainageways on'flatwoods on marine terraces Landform position (three-dimensional): Tread, dip, talf Down -slope shape: Linear Across -slope shape: Linear, concave Other vegetative classification: Slough (R155XY011 FL) Hydric soil rating: Yes Hallandale Percent of map unit. 2 percent Landform: Flatwoods on marine terraces Landform position (three-dimensional): Tread, talf Down -slope shape: Linear I Across -slope shape: Linear Other vegetative classification: South Florida Flatwoods (R155XY003FL) Hydric soil rating: Yes 37—Riviera sand, frequently;ponded, 0 to 1 percent slopes Map Unit Setting National map unit symbol. 2tzwm Elevation: 0 to 70 feet Mean annual precipitation: 46 to 58 inches Mean annual air temperature: 68 to 77 degrees F Custom Soil Resource Report Frost -free period. 350 to 365 days Farmland classification: Farmland of unique importance I Map Unit Composition Riviera and similar soils: 85 perce It Minor components: 15 percent Estimates are based on observations, descriptions, and transects of the mapunit. Description of Riviera Setting Landform: Depressions on marine terraces Landform position (three-dimensional): Tread, dip Down -slope shape: Concave Across -slope shape: Concave Parent material. Sandy and loamy marine deposits Typical profile A - 0 to 0 inches: sand E - 0 to 22 inches: sand Btg/E - 22 to 31 inches: sandy loam Btg1 - 31 to 42 inches: sandy;loam Btg2 - 42 to 80 inches: sandylclay loam Properties and qualities Slope: 0 to 1 percent Depth to restrictive feature: More than 80 inches Natural drainage class: Very poorly drained Runoff class: Negligible Capacity of the most limiting layer to transmit water (Ksat): Moderately low to moderately high (0.06 to'0.20 in/hr) Depth to water table: About 0 inches Frequency of flooding: None Frequency of ponding: Frequent Calcium carbonate, maximum in profile: 4 percent Salinity, maximum in profile.i Nonsaline to very slightly saline (0.0 to 2.0 mmhos/cm) Sodium adsorption ratio, maximum in profile: -4.0 Available water storage in profile: Moderate (about 6.7 inches) Interpretive groups Land capability classification (irrigated): None specified Land capability classification (nonirrigated): 7w Hydrologic Soil Group: C/D Forage suitability group: Sandy over loamy soils on stream terraces, flood plains, or in depressions (G155XB245FL) Other vegetative classification: Freshwater Marshes and Ponds (RI 55XY010FL) Hydric soil rating: Yes Minor Components Chobee Percent of map unit. 5 percent Landform: Depressions on marine terraces Landform position (three dimensional): Tread, dip Down -slope shape: Concave Across -slope shape: Concave 12 Custom Soil Resourc,'e Report Ecological site: Freshwater Mars lies and Ponds (R155XY010FL) Other vegetative classification: Freshwater Marshes and Ponds (R155XY010FL) Hydric soil rating: Yes Wabasso Percent of map unit: 4 percent Landform: Flatwoods on marine terraces Landform position (three-dimensional): Tread, talf Down -slope shape: Linear I Across -slope shape: Linear Other vegetative classification: South Florida Flatwoods (R155XY003FL) Hydric soil rating: No Malabar Percent of map unit: ' 3 percent Landform: Depressions on marine terraces Landform position (three-dimensional): Tread, dip Down -slope shape: Concave, Ilinear Across -slope shape: Concave, linear Ecological site: Slough (R155�Y011 FL) Other vegetative classification: South Florida Flatwoods (R155XY003FL) 'Hydric soil rating: Yes I Hallandale Percent of map unit: 3 percent Landform: Flatwoods on marine terraces Landform position (three-dimensional): Tread, talf Down -slope shape: Linear Across -slope shape: Linear Other vegetative classification: South Florida Flatwoods (R155XY003FL) Hydric soil rating: Yes I13 27' 31' 51" N 27° 31' 50" N 3 0 Custom Soil Resource Report Soil Map 557602 557611 557620 557629 557638 3 o N Map Scale: 1:388 if printed on A landscape (11" x 8.5D sheet $ Metes N 0 5 10 20 30 Feet 0 15 30 60 90 Map projection: Web Mercator Comer coordinates: WGS84 Edge tics: UTM Zone 17N WGS84 6 557647 5576% 557665 557674 557683 3 N t7° 31'51"N ' 27° 31' 50" N Custom Soil Resource Report MAP LEGEND MAP INFORMATION Area of Interest (Aol) g Spoil Area The soil surveys that comprise your AOI were mapped at F7 Area of Interest (AOI) Stony Spot 1:24,000. Soils a Soil Map Unit Polygons Very Stony Spot Warning:Soil Ma not be valid at this scale. p may Wet Spot ,—fte Soil Map Unit Lines Enlargement of maps beyond the scale of mapping can cause 0 Soil Map Unit Points Other misunderstanding of the detail of mapping and accuracy of soil 9 PP 9 Y .-. Special Line Features line placement. The maps do not show the small areas of Special Point Features contrasting soils that could have been shown at a more detailed Uo Blowout Water Features scale. Streams and Canals Borrow Pit Transportation Please rely on the bar scale on each map sheet for map Clay Spot i-1-fr Rails measurements. Q Closed Depression Interstate Highways Source of Map: Natural Resources Conservation Service Gravel Pit US Routes Web Soil Survey URL: Gravelly Spot Coordinate System: Web Mercator (EPSG:3857) Major Roads Landfill Local Roads - - - - -- __ _ __Maps from the Web Soil Survey are based on the Web Mercator A. Lava Flow projection, which preserves direction -and -shape -but -distorts _ Background distance and area. A projection that preserves area, such as the Marsh or swamp ® Aerial Photography Albers equal-area conic projection, should be used if more a Mine or quarry accurate calculations of distance or area are required. ® Miscellaneous Water This product is generated from the USDA-NRCS certified data as 0 Perennial Water of the version date(s) listed below. ,J Rock outcrop Soil Survey Area: St. Lucie County, Florida + Saline Spot Survey Area Data: Version 10, Oct 6, 2017 e Sandy Spot Soil map units are labeled (as space allows) for map scales Severely Eroded Spot 1:50,000 or larger. Sinkhole Date(s) aerial images were photographed: Dec 31, 2009—Mar Slide or Slip 20, 2017 oa sodic Spot The orthophoto or other base map on which the soil lines were . compiled and digitized probably differs from the background imagery displayed on these maps. As a result, some minor shifting of map unit boundaries may be evident. 7 7 W-Kr EGRESS . I 110.W. ..•iT,,. g 8 ti� +I I 1 r SHELF k R00 �— DINING MASTER BEDROOM _ -- 'P I 8' 4•_1�• 4 t2,_8• - "' 2D6E fT. .- - _ (2)2868 Sfi. .. -I iv $H SHELF h RW - o o I � � — BATH 2668 -- 1 LMNG ROOM. _ ~ 4' Q . SHF1F h "'_ 8" DNPYENI OMLARD 4' 2,�. (2)2666 r..r, ROOM . 2 2 CAR GARAGE1. b of i I •. ,.. O.. � .I.:. 4 CUMED PORCH - EGf�55 1i P I Y 9'-B' 9:_8. 2�_4• I 6'_4• g•_8• 9:-6" 6.-e" i ------------ ARFA TABULATION r AREA !UNDER AR: I 1,259 SF GARAGE AREA; 446 5F COVERED ENTRY AREA: 87 5F TOTAL AREA UNDER ROOF: 1,792 SF