Depth to Wa1er Tabe--San German Area Southwesern Puetto Rico

tbull I 3 16 1

17 59 2 17S9a

~gtbp Solo 1 ii~J001t pnrJtGonA~YZ (85)( nmiddotJ wet

~bull ~

N ~--~~===~------i~=====~Velers0 360 7Xgt 1400 1100~~ A ----~~~===~~---------~~==========~0 IJOO MOO amp000 9000

~ Naturol ReSOIJICeltgt _ Consllrvaton SttVIoe

We1gt Soil Survey 411012012 NaJon3J Coopetallve Soil Survey Pbullge t of4

Depth to Waler Table-san Germeo Area Southwestern Pueno Rico

MAP LEGEND

Atoa ~~f tntrwst fAOij

0 Arlta of lnlolaquoltl (AOI)

Solibull

_I Soli Map UAls

Soil Rating

u 0-25

0 25 - ~

0 5o-loo

D 100- ISO

Ll 150-200

J gt ltiO

Polttkal I)N bull Citiabull

Water Fbullaturea

~ S1reama bull nd Can111

Tr1naport1Uon

Raila -lnt~fil1 liighWlyt- US Routes-

Ma~orRoada

Local Road-

MAP INFORMATION

Mop Sobulllo 126700 ifpnnled on A size (8S bull 11) sheet

The soli suMy~r lhal oomprise y~gturAOI were mapped al t 2DOOO

Please rely on the bar scale on e-ach map sheet ror accurate map measJemenl3

Soo1ce of Map Na1ural Resouroes C~gtnservalion Service Web SoU Survey URL 11Upllweb$oilsurve-Jnrcsusdagov Coortlinale System UTM Zone 19N NA083

Tlli product It generated from the USOA NRCS centned dara as ol ubullbulle vertiltltl daCe(s) lis led below

Soli SUrvey Aro San German Are~ Slt1uUlwestern Puerto Rioo ampJrvey Alaa Oaia VemiltJn 3 Dec a 2008

Dale(s)aeriallmageswere~ 200lt

The orlhophoiO or o1her gtMe mlgtj) on vfllth he soillnes wero c ond dlg~Jzed probably differs rom 1he baclltground imagary Cfiap1ayed on 1hese maps As a re$Ult some minor Miitung or map unit bouncfarfM may be avc~ent

Natural Raso~~ren Neb Soil SuNey lt11012012~ Conservation Servke Natianat Cooperalive Soil Survey Pogo 2 oflt

Depth to Waler Table-san Germeo Area Southwestern Pueno Rico

MAP LEGEND

Atoa ~~f tntrwst fAOij

0 Arlta of lnlolaquoltl (AOI)

Solibull

_I Soli Map UAls

Soil Rating

u 0-25

0 25 - ~

0 5o-loo

D 100- ISO

Ll 150-200

J gt ltiO

Polttkal I)N bull Citiabull

Water Fbullaturea

~ S1reama bull nd Can111

Tr1naport1Uon

Raila -lnt~fil1 liighWlyt- US Routes-

Ma~orRoada

Local Road-

MAP INFORMATION

Mop Sobulllo 126700 ifpnnled on A size (8S bull 11) sheet

The soli suMy~r lhal oomprise y~gturAOI were mapped al t 2DOOO

Please rely on the bar scale on e-ach map sheet ror accurate map measJemenl3

Soo1ce of Map Na1ural Resouroes C~gtnservalion Service Web SoU Survey URL 11Upllweb$oilsurve-Jnrcsusdagov Coortlinale System UTM Zone 19N NA083

Tlli product It generated from the USOA NRCS centned dara as ol ubullbulle vertiltltl daCe(s) lis led below

Soli SUrvey Aro San German Are~ Slt1uUlwestern Puerto Rioo ampJrvey Alaa Oaia VemiltJn 3 Dec a 2008

Dale(s)aeriallmageswere~ 200lt

The orlhophoiO or o1her gtMe mlgtj) on vfllth he soillnes wero c ond dlg~Jzed probably differs rom 1he baclltground imagary Cfiap1ayed on 1hese maps As a re$Ult some minor Miitung or map unit bouncfarfM may be avc~ent

Natural Raso~~ren Neb Soil SuNey lt11012012~ Conservation Servke Natianat Cooperalive Soil Survey Pogo 2 oflt

Depth 1o ~ter Tetlre-Sell G-erman Area Soulllwestem Pueno Rbulloo

Depth to Water Table

Ooplh to Wa1$r lab-Summaoy by Mop Uni_ t- San Gonnan Al$0 Southweotom PuQ~oRico (PR717)

Map unlC nama Napunlt J ~mbltgt~- i

RaUnr (conUmeters) I ACRis ln AOI Percent ofAOI

AgO Aguilite silty clay loam S to 20 gt200 peroeot slopes

1422 3 3

I AkA Aguirre lay o~casionaly ponded gt200 4397 103

AID Allamira gravelly day 2 to 20 gt200 p(rc+n1 slopes

10M 25

CoA Cattagerla clay 0 to 2 perwnt gt200 1964 U slopes

CtA Cortada silly day 0 lo 2 bullZOO percen bull _ r nooded

268 07

CuD C-osta-Pilafaya compfx 5 lD 20 gtlIgtO percent slgtpe$

101 04

I CoF CostamiddotPitahaya comp5ex 20 to 60 gt200

bull per~enl sklpes 4671 11 0

oac Oeampcalabrado cl~y 2 to 12 gt200 percent slopfs

24 01

OsO

DsF

Oescalabrado clay 12 tegt 20 middot~oo percent slopes

Descalabrado clay 20 lo 00 gt200 pampr~nl sl(lpes

320

4 7

0 8

01

EpC El P apaya grally d IJ lobullm 2 lo gt200 bull 12 pt-rcen1 sklt~~a

1$3 0 4

EpO El Papayo gra~ clay loom 12 gtZOO lo 20 peltelll slopeoI

5U

I 141

~ El P apaya gravely d ay loam 20 gt200 to 60 percent slope$

298 07

FoA Fe ~ay 0 to 2 percelll Jlopes 1122 3646 SS

FrA 1

Fral-emidad clay 0 to 2 percent gt200 slopes I

1478 35

I ~ FrB Fraternid~d clay 2 to 5 peroent gt200

slopes 16 0 0

GnA Guanica day 0 lO 1perwot gt200 bull slopes

14569 343

GyC Gu3yacan clay 5 to 12 perOQnt gt200 85 0 1 sropes

ldA La Luna ~ ilty clay loam 0 tltJ 2 gt200 petltent slopes occaS~ floodpoundlt

673 181

Pgll Patg clay 2 10 5 petcenl gt200 slopes

120 03

PsF PiilhBya-limestone outcropmiddot bull ZOO Seboruco comp~x ~ lo 50 percent slopes

32A I

08

IW$ H1tunl Resources Web Soil Surwy 41102012 Conservation Samprvice National Coope1allve Soil Survey Page 3 of4

Oeplh to Wttt f 1able-san German Ale~ Southwestern Pueno Rico

Dopih to Wator Table- Summary by Mop Unit - Slon Gormbulln A-So-atem Puorto Rico (PR187)

Mbullp unN M-P untt name RbullOng ebullnUmatbullrs) Aeres ln AOt Peteonl 01 AOI symbol

P9 P~o Blanco ciBy 0 to 5 percent gtZOO 23~ 06 slopes

igtzC Pozo Blanco clay S to 12 PEIcent gt200 538 13~ slopes

PzD Pozo Blanco tlsy 12 to 20 percent gt200 Z24 0amp lilo~s

SeA San AtlAln day loam 0 to 2 gt200 783 18 percent slopeamp occuionaIJ nooded

SgD S3n GeiTilanQuey complex 5 10 gt200 e1 01 20 percent sl(lpes

SVF San G0fl111ln-Ouey complex 2010 gt200 1491 35 GO pe~cenl slopes I

u UrbanlallCI gt200 169Z middot~ VoA Voyas bull illy clay 0 to 2 penent 10 1111 26

Wpes occas-ionCJ1ty flooded

w Wales

ITotals tor Area o1 ltrn1

gt200 11 8

4l5lt19

0314

1000

Description

Water table refers lo a saturated zone in the soil It occurs during specified months Estimates of the upper Ifmit are based mainly on observations of the water table at selected sites and on evidence of a saturated zone namely grayish colors (redoximorphic features) in the soil Asaturaled zone that lasts for less than amonth is not considered a water table

This attnoute is actually recorded as lhree separate values in the database A low value and a high value indicate the range of Ihis attribute for the soil component A representativebull value indicales the expected value of this attribute for the component For this soil property only the representative value is used

Rating Options

Units ofMeasure centimeters

Aggregation Method Dominant Component

Component Percent Cutoff None Specified

Tie-break Rule Lower

Interpret Nuns as Zero No

Begjnnjng Month January

Ending Month December

N1tural Resouros Web Soil Surbulley 411012012 Conservation Service Natlonas Cooperative Scil SuNey Page4of4

Physical SoU Propertiu-S~n Gennan Area So11thwestem Puerto Rico

Physical Soil Properties

This table shows estimates ofsome physical characteristics and features that affect soil behavior These estimates are given for the layers of each soil in the survey area The estimates are based on field observations and on test data for these and similar soils

Depth to the upper and lower boundaries ofeach layer is indicated

Partide size is the effective diameter of a soil particle as measured by sedimentation sieving or micrometric methods Partide sizes are expressed as classes with specific effective diameter class limits The broad classes are sand silt and day ranging from the larger to the smaller

Sand as a soil separate consists ofmineral soli partides that are 005 millimeter to 2 millimeters In diameter In this table the estimated sand content ofeach soil layer is given asa percentage by weight of the soil material that is less than 2 millimeters in diameter

Silt as a soil separate consists of mineral soil particles that are 0002 to 005 millimeter in diameter In this table the estimated silt content of each soil layer is given as a percentage by weight of the soil materiallhallsless than 2 millimeters in diameter

Clay as a soil separate consists of mineral soil particles that are less than 0002 millimeter in diameter In this table the estimated clay content of each soil layer is given as a percentage by weight of the soil material that is less than 2 millimeters in diameter

The content of sand silt and clay affects the physical behavior ofa soil Particle size is important for engineering and agronomic interpretations for detellllination of soil hydrologic qualities and tor soil dassification

The amount and kind ofclay affect the fertility and physical condition of the soil and the ability of the soil to adsorb cations and to retain moisture They influence shrinkshyswell potential saturated hydraulic conductivity (Ksat) plasticity the ease of soil dispersion ancl other soil properties The amount and kind of day in a soil also affect tillage and earthmoving operations

Moist bulk density is the weight of soil (ovendry) per unit volume Volume Is measured when the soil is at field moisture capacity that is the moisture content at 13- or 110-bar (33kPa or 1 OkPa) moisture tension Weight is detellllined after the soil is dried at 105 degrees C In the table the estimated moist bulk Clensity of each soil horizon is expressed in grams per cubic centimeter ofsoil material that is less than 2 millimeters in diameter Bulk density data are used to compute linear extensibility shrink-swell potential available water capacity total pore space and other soil properties The moist bulk density ofa soil indicates the pore space available for water and roots Depending onsoil texture a bulkdensity ofmore than 14 can restrict water storage and root penetraUon Moist bulk density is Influenced by texture kind of clay content of organic matter and soil structure

Saturated hydraulic conductivily (Ksal) refers to lhe ease with which pores in a saturated solltransmil water The estimates in the table are expressed In terms of micrometers per second They are based on soil characteristics observea in the field particularly structure porosity and texture Saturated hydraulic conductivity (Ksat) is considered In the design of soft drainage systems and septic tank absorption fields

--middot-middot~~~--------------~~~~----------------------~== bullbull~~ Natun11 Resourcos Web Soil Survey 41012012 cil Connrvatlon SeNICamp Nallonal CoopGf3tiY~ Sol Survey Pagi) 1 or 17

Oeplh to Wttt f 1able-san German Ale~ Southwestern Pueno Rico

Dopih to Wator Table- Summary by Mop Unit - Slon Gormbulln A-So-atem Puorto Rico (PR187)

Mbullp unN M-P untt name RbullOng ebullnUmatbullrs) Aeres ln AOt Peteonl 01 AOI symbol

P9 P~o Blanco ciBy 0 to 5 percent gtZOO 23~ 06 slopes

igtzC Pozo Blanco clay S to 12 PEIcent gt200 538 13~ slopes

PzD Pozo Blanco tlsy 12 to 20 percent gt200 Z24 0amp lilo~s

SeA San AtlAln day loam 0 to 2 gt200 783 18 percent slopeamp occuionaIJ nooded

SgD S3n GeiTilanQuey complex 5 10 gt200 e1 01 20 percent sl(lpes

SVF San G0fl111ln-Ouey complex 2010 gt200 1491 35 GO pe~cenl slopes I

u UrbanlallCI gt200 169Z middot~ VoA Voyas bull illy clay 0 to 2 penent 10 1111 26

Wpes occas-ionCJ1ty flooded

w Wales

ITotals tor Area o1 ltrn1

gt200 11 8

4l5lt19

0314

1000

Description

Water table refers lo a saturated zone in the soil It occurs during specified months Estimates of the upper Ifmit are based mainly on observations of the water table at selected sites and on evidence of a saturated zone namely grayish colors (redoximorphic features) in the soil Asaturaled zone that lasts for less than amonth is not considered a water table

This attnoute is actually recorded as lhree separate values in the database A low value and a high value indicate the range of Ihis attribute for the soil component A representativebull value indicales the expected value of this attribute for the component For this soil property only the representative value is used

Rating Options

Units ofMeasure centimeters

Aggregation Method Dominant Component

Component Percent Cutoff None Specified

Tie-break Rule Lower

Interpret Nuns as Zero No

Begjnnjng Month January

Ending Month December

N1tural Resouros Web Soil Surbulley 411012012 Conservation Service Natlonas Cooperative Scil SuNey Page4of4

Physical SoU Propertiu-S~n Gennan Area So11thwestem Puerto Rico

Physical Soil Properties

This table shows estimates ofsome physical characteristics and features that affect soil behavior These estimates are given for the layers of each soil in the survey area The estimates are based on field observations and on test data for these and similar soils

Depth to the upper and lower boundaries ofeach layer is indicated

Partide size is the effective diameter of a soil particle as measured by sedimentation sieving or micrometric methods Partide sizes are expressed as classes with specific effective diameter class limits The broad classes are sand silt and day ranging from the larger to the smaller

Sand as a soil separate consists ofmineral soli partides that are 005 millimeter to 2 millimeters In diameter In this table the estimated sand content ofeach soil layer is given asa percentage by weight of the soil material that is less than 2 millimeters in diameter

Silt as a soil separate consists of mineral soil particles that are 0002 to 005 millimeter in diameter In this table the estimated silt content of each soil layer is given as a percentage by weight of the soil materiallhallsless than 2 millimeters in diameter

Clay as a soil separate consists of mineral soil particles that are less than 0002 millimeter in diameter In this table the estimated clay content of each soil layer is given as a percentage by weight of the soil material that is less than 2 millimeters in diameter

The content of sand silt and clay affects the physical behavior ofa soil Particle size is important for engineering and agronomic interpretations for detellllination of soil hydrologic qualities and tor soil dassification

The amount and kind ofclay affect the fertility and physical condition of the soil and the ability of the soil to adsorb cations and to retain moisture They influence shrinkshyswell potential saturated hydraulic conductivity (Ksat) plasticity the ease of soil dispersion ancl other soil properties The amount and kind of day in a soil also affect tillage and earthmoving operations

Moist bulk density is the weight of soil (ovendry) per unit volume Volume Is measured when the soil is at field moisture capacity that is the moisture content at 13- or 110-bar (33kPa or 1 OkPa) moisture tension Weight is detellllined after the soil is dried at 105 degrees C In the table the estimated moist bulk Clensity of each soil horizon is expressed in grams per cubic centimeter ofsoil material that is less than 2 millimeters in diameter Bulk density data are used to compute linear extensibility shrink-swell potential available water capacity total pore space and other soil properties The moist bulk density ofa soil indicates the pore space available for water and roots Depending onsoil texture a bulkdensity ofmore than 14 can restrict water storage and root penetraUon Moist bulk density is Influenced by texture kind of clay content of organic matter and soil structure

Saturated hydraulic conductivily (Ksal) refers to lhe ease with which pores in a saturated solltransmil water The estimates in the table are expressed In terms of micrometers per second They are based on soil characteristics observea in the field particularly structure porosity and texture Saturated hydraulic conductivity (Ksat) is considered In the design of soft drainage systems and septic tank absorption fields

--middot-middot~~~--------------~~~~----------------------~== bullbull~~ Natun11 Resourcos Web Soil Survey 41012012 cil Connrvatlon SeNICamp Nallonal CoopGf3tiY~ Sol Survey Pagi) 1 or 17

Physical SoU Propertiu-S~n Gennan Area So11thwestem Puerto Rico

Physical Soil Properties

This table shows estimates ofsome physical characteristics and features that affect soil behavior These estimates are given for the layers of each soil in the survey area The estimates are based on field observations and on test data for these and similar soils

Depth to the upper and lower boundaries ofeach layer is indicated

Partide size is the effective diameter of a soil particle as measured by sedimentation sieving or micrometric methods Partide sizes are expressed as classes with specific effective diameter class limits The broad classes are sand silt and day ranging from the larger to the smaller

Sand as a soil separate consists ofmineral soli partides that are 005 millimeter to 2 millimeters In diameter In this table the estimated sand content ofeach soil layer is given asa percentage by weight of the soil material that is less than 2 millimeters in diameter

Silt as a soil separate consists of mineral soil particles that are 0002 to 005 millimeter in diameter In this table the estimated silt content of each soil layer is given as a percentage by weight of the soil materiallhallsless than 2 millimeters in diameter

Clay as a soil separate consists of mineral soil particles that are less than 0002 millimeter in diameter In this table the estimated clay content of each soil layer is given as a percentage by weight of the soil material that is less than 2 millimeters in diameter

The content of sand silt and clay affects the physical behavior ofa soil Particle size is important for engineering and agronomic interpretations for detellllination of soil hydrologic qualities and tor soil dassification

The amount and kind ofclay affect the fertility and physical condition of the soil and the ability of the soil to adsorb cations and to retain moisture They influence shrinkshyswell potential saturated hydraulic conductivity (Ksat) plasticity the ease of soil dispersion ancl other soil properties The amount and kind of day in a soil also affect tillage and earthmoving operations

Moist bulk density is the weight of soil (ovendry) per unit volume Volume Is measured when the soil is at field moisture capacity that is the moisture content at 13- or 110-bar (33kPa or 1 OkPa) moisture tension Weight is detellllined after the soil is dried at 105 degrees C In the table the estimated moist bulk Clensity of each soil horizon is expressed in grams per cubic centimeter ofsoil material that is less than 2 millimeters in diameter Bulk density data are used to compute linear extensibility shrink-swell potential available water capacity total pore space and other soil properties The moist bulk density ofa soil indicates the pore space available for water and roots Depending onsoil texture a bulkdensity ofmore than 14 can restrict water storage and root penetraUon Moist bulk density is Influenced by texture kind of clay content of organic matter and soil structure

Saturated hydraulic conductivily (Ksal) refers to lhe ease with which pores in a saturated solltransmil water The estimates in the table are expressed In terms of micrometers per second They are based on soil characteristics observea in the field particularly structure porosity and texture Saturated hydraulic conductivity (Ksat) is considered In the design of soft drainage systems and septic tank absorption fields

--middot-middot~~~--------------~~~~----------------------~== bullbull~~ Natun11 Resourcos Web Soil Survey 41012012 cil Connrvatlon SeNICamp Nallonal CoopGf3tiY~ Sol Survey Pagi) 1 or 17

Phy$ical Soil Prope-ttiamp$-San Gtmnan Are~ Sou1Jlwe$letn Pu~rto Rico

Avsisblamp water capacity refers to the qua nifty of water that the soil is capable of storing for use by plants The capacity for water storage is given in inches of water per inch ofsoil for eacn soil layer The capacity varies depending on soil properties lhat affect retention of water The most Important properties are the content of organic matter soil tegtltture bulk density and soil structure Available watercapacity is an important factor in the choice ofplants or crops to be grown and in the design and management of irrigation systems Available water capacity Is not an estimate of the quantity of water actually available to plants at any given time

Linear extensibility refers to the change in length ofan unconfined clod as moisture content Is decreased from a moist to a dry state It is an expression of the volume change between the water content of the clod at 113middot or 111 Omiddotbar tension (33kPa or 1OkPa tension) and oven dryness Tne volume change is reported in the table as percent change for the whole soil The amount and type ofclay minerals in the soil Influence volume change

Linear extensibility is used to determine the shrink-swell potential of soils The shrink-swell potential is low if the soil has a linear extensibility ofless than 3 percent moderate lf3 to 6 percent high if6 to 9 percent and very high ifmore than 9 percent If the linear extensibility is more than 3 shrinking and swelling can cause damage to buildings roads and other structures and to plant roots Special design commonly is needed

Organic matter is the plant and animal residue in the soil at various stages of decomposition In this table the estimated oontent of organic matter is expressed as a percentage by weight of the soil material that is less than 2 millimeters in diameter The content of organic ma~er in a soil can be maintained by returning crop residue to the soil

Organic matter has a positive effect on available water capacity water infiltration soU organism activity and tilth It Is a source ofnltrogen and other nutrients for crops and soil organisms

Erosion factors are shown in the table as the K factor (Kw and Kt) and the T factor Erosion factor K indicates the susceptibility ofa soil to sheet and rill erosion by water Factor K is one ofsix factors used in the Universal Soil loss Equation (USLE) and the Revised Universal Soil Loss Equation (RUSLE) to predict the average annual rate of soil loss by sheet and rill erosion in tons per acre per year The estimates are based primarily on percentage of sill sand and organic matter and on soil structure and Ksat Values of K range from 002 to 069 Other factors being equal the higher the value the more susceptible the soil is to sheet and rill erosion by water

Erosion factorKw indicates the erodibility of the whole soil The estimates are modified by the presence of rock fragments

Erosion factor Kf indicates the erodibility of the fine-earth fraction or the material less than 2 millimeters in size

Erosion faclor Tis an esijmale of the maximum average annual rate ofsoil erosion by wind andor water that can occur without affecting ClOP productivity over a sustained period The rate is in tons per acre per year

IMnd erodibility grovps are made up of soils that have similar properties affecting their susceptibility to wind erosion in cuHivated areas The soils assigned to group 1are the most susceptible to wind erosion and those assigned to group 8 are the least susceptible The groups are described in the National Soil Survey Handbook

Natural Rasoutcefl Wb Soil Suy 411012012 Conservation Servlco NaUonal Coopafatlve Soli SufQy Pag~ 2 of 17

Physical Soil Properties-san GeiJJian Area Sootlwestem Puerto Rico

IMnd erodibtlily index isa numerical value indicating the susceptibility ofsoil to wind erosion or the tons peracre peryear that can beexpected to beIositowind erosion There is a close correlation between wind etosion and the texture of the surface layer the size and durability of surface clods rock fragments organic matter and a calcareous reaction Soli moisture and frozen soil layers also influence wind erosion

Reference United States Department ofAgriculture Natural Resources Conservation Service National soil survey handbook title 430VI (httpsoilsusdagov)

Natural Rosourltes Web Soli Survey ConsbullrvaUon ServiGamp N~liona1 Coope~live Soil Survey Pagi) 3 of t7

411012012

Physical Soil Properties-san GeiJJian Area Sootlwestem Puerto Rico

IMnd erodibtlily index isa numerical value indicating the susceptibility ofsoil to wind erosion or the tons peracre peryear that can beexpected to beIositowind erosion There is a close correlation between wind etosion and the texture of the surface layer the size and durability of surface clods rock fragments organic matter and a calcareous reaction Soli moisture and frozen soil layers also influence wind erosion

Reference United States Department ofAgriculture Natural Resources Conservation Service National soil survey handbook title 430VI (httpsoilsusdagov)

Natural Rosourltes Web Soli Survey ConsbullrvaUon ServiGamp N~liona1 Coope~live Soil Survey Pagi) 3 of t7

411012012

Ptysilt31 Sol Properties-s~n Gennen Aree Soulhweiem Puerto Rico

Report-Physical Soil Properties

Physical Soli Ptoperthts- San German Area Southw(tamptam Pu(trto ~leo

Map symbol I Oopth Sand Silt Clay Moltt Saturlted Avallablt Linear Organle Erosfon Wind Wind and soli name bulk hydullc W11ler oxlongtlblllly mattor rators erodlblllly erodibility

denslly ~onducUvtty capac~ty group fndex KwiKfiT

In Pel Pd Pet gtct milaquolt ml~ IllIn Fltf Pct

AgCl-gu~ita

silyd3y klam 5 to 20 pefalnl 1 stopes

Aguiile 0-6 -~~ 1-51- 130-l() 45 l uo-t~ol1oo4o~oo Io12-gt16 3o-oo middot l so-1oo 124 24 13 lbulll S6

~3 ~$- -3$- 2H()40 120-130 i 10()1000 008-015 3000 05-40 17 24 bull I

--_a middotjs_-- middot-is--- 810Somiddot-middotluo-uo 1oo-1ooo __ -~-oe-o~~----~-~~ _ _ o-~middoto__ ~7 -~~L I AIltA-Aguirre ll

day I bull

~~middotbullbullY i I ______ T Agulrrbull ()18 -11- -2$- 6004- 68 o~S-135 001)10 I038-05 191-270 i30-50 24 24 s 4 ss

1HO -11- -2$- 60-6lt- 68 -MS-130 middoto0)10 038-051 s0-270 110-10 24 j 24 -middot---middotmiddot JAtO--Aft3mlta middot

gravelly day 2lo20 p~rcent

sJopes

Altemitt 0-8 j -23- l-27- Z$-5() 55 j 13()140 101()100 012middot020 30-59 20-40 124 124 3 ~~ -----J~s __ 1614 1-22- -33- 20-45-50 1 12~12-~oo 012-020 ~o-6o 1os-2o 111 1241 middot ~ltt-lt~3 l-29middot ~s- 15--33-35 10()10oo ~1()~ J bullo-~o loo-10 128 126 I 1

43-$4 -39middot ~7middot 115--24- 35 1000-10000 010018 190-300 IOD-10 32 32 I

5-4-79 middot shy

L~Umiddot ~riii Natural Rosources Web Soli Survey 411012012

ConurvatJon Samprvlee Netionllf Coop43raUvamp SoJ Surve) Pbullge 4 or 17

Phyamplcat Soa P1opsttles-San Gstman Area SDtJthwampcltm P~~erto RIGo

Physlell Soli Properttes- San Oennan Area SoU1hW$$ttm Puerto Rico

Mop symbo l Dopill Sancf SIH Clay Moist Satumed Avolllblo Linear Organ~ EroSIO Wind Wlbulld and soil name bulk hydrbulluiJc wator eocentenolblllly matte tutors dlblllly orodlblllty

dtnstly eonductlvlty capadty group Index Kw Kl T

In Pet Pet Pet gkc mimlmrSec Pet Pltf bullbull - -- middot

jCoAshy bull I Cs1tJ9ena Iclay OJo2 Ibullpelaquoef11 sklpes l I I __ -middot -~- - -- bull bull

i Cartagena 0-1 middotII- 1 ~3- 30-60- 60 125-100 010middot1 00 013016 90-250 2~0 24 bull24 s 4 86

7-15 - 9- 1~3- 3()5amp- 60 125-160 011H OO 0 1gt-016 9()250 2()40 24 24 bull 15-48 middot1() 121)- 4 ()61- 61 125middot160 01()100 010-013 9 0-250 lG-25 24 i ~middot i

lt _ _ bull bullbull ----- shy~--middot-- -middot ~----middot ----- _ --- --shy48--tJO bull 1 () -211- 5G-e2- e5J 1 2s-1 ~o 01~100 010-013 90-250 00-10 2~ 12 bull

CIA-Cortada dyday loam 0102 pamplatnt slopes I

bulloccasionally flooded IL

I I I

- middot-Cortada 0-11 -15- -55- 1()31) 38 uo-1 1s 101)1000 021middot022 OG-29 40-110 20 20 s 4 middot661 ---- --~ --middotmiddot - - - middot 6 middot15 middot18- -44middot 1()311- 36 110-115 100-1000 018-020 01)29 40~0 2o- 2or - f- 15--23 -18- -47- 3()35- 38 1 15middot130 1001000 02()022 0~29 20-40 20 20 _ - -middot-middot ~-middot 23-34 -SG- -34- 31)3( 36 bull 115-125 10()1000 01$-020 0~29 20-40 17

~

134-45 5() -21gt- 31)3~38 115-125 10()1000 016-oZO 01)29 2 ()40 20 120 I I 45-58 -as- -3() 11gt-15- 35 115--125 100010000 01$-020 01-29 05-20 20 20 I

middot- shy156-33 -45- 1-37- 1()111- 35 ~1lt5 hooo-1oooo 018-020 i00-29 05-20 20 20 _] - - middotmiddot------- 63-60 -5() -21) 20-30-33 115-125 100-1000 018-020 00-29 05middot20 17 111 _] I

shyshy

fi$ Natural Resources Wob Sci SUn-ey 411 012012 Conampervatlon SbullNfcbull NaUooal Coop-slive Sc~ Stmoey fllve 5 of 11

Physlral Soli PropeiJeamp-San German Alea Soulttwettbullrn Puerto Rico

Physlc-el Soli ProPQrttH- San Ge~rmanArea Souttwtntbullm Puerto Rico

Map symbol Depth Sbullnd Sl~ Cloy NobI Satutea Available Linear Organic Eroeton Wind Wind anG bull oil nampme bulk

denstty hydraulic

eondudJvtty ~~Vater

oapaclty tonslblllty mattr f8ctonll

l(ol Kl I T

ongtltllblllly grovp

orodlblllty fndex

- - middot In Pd Pd Pd ~ mlciD lMltIeshy IMn Pd - Pet I C[)Costa-

Pbha)ll IoomPltx5to

20-slopes

bull

-

i i

I

Costa H -19shy----shymiddotmiddotshy middotmiddotshy7middot11 jmiddot12shybull 1middot19 middot12-

19- c

43-amp3 -

middot36shy

middot35shy

-w

--

30-45middot 60 0 90-100

30-54- 85 0115-105

3C)-44 60 104middot114

- -- -

0~0-100 0 05-010 00-29 26-aO

01~100 1005-010 OC)-29 1()-20 l--shy middot-shy

01 ()~00 005-4)~0 00-29 00-(]4

- - - -_ shy- - - -

24

24

24

2amp 1 a

28

23 I

I

0 I middot-shy

+middotmiddot -~

I I Pllahayt 1-shy

C)-2

2-H

1middot111shy

middot25shy

-Z7-

-2olshy

3$54-80

M-51-60

141)150

1AC)-160

011)100

01C)-1il0

00$-010

00$-010

1()30

~ 1MO

20o80

11)20

24

24

2s 1bull 8

28~

0

11middot2

2HO --

--

-shy

-

--

---

shy_ --

I bull L ___

reg Hturil-Reeoure Web soi-Sotvoy ol11)2()12 ConsetvaUOn Service No~ooalCoopeltaM So~StrVef Pbull~e8ol 17

Physical SltJit P1opertles-San Gennan AreI SoiUlwKlem Puerto RIGa

Physleet Son Propertle_ San Cennan Atoa SouthwHkllm Puerto Rico

Map symbol Dep1ll and $Cji name

Sand SIK Cloy Moist bulk

dons lly

Saturated hydraulic

condueUvJty

Avallablamp water

ltopaclly

ITn-ear emnslblllly

OtgPnh mottor

Ef031on facto

~w Kl T

Wlnd ongtd lblllly

group

Wind 010dlblllly

hldU

In -QE~ I

compl 20 -lo 60 percent I Sklpe_amp i

Cosla 0middot1

7-11 f-middot- middotmiddot -middot- --shy

11~1S

19-43 -43-a3

Pa

middot19shy

middot12middot

middot12middot

--

Pa

middot36middot

~5-

-middotshy

PcJ

130-lt5-M 30-54middot 65

30M-60

-I -

gtc I

- 090-100

095-10S

104-114

--

miciD mlsec

010-100

OIIHOO

01~lQoD

--

Win

005-010

005-010

005-010 - _-middotmiddotshy--

Pel-- - -middot

00-29

00middot29

00-29

--

P1

20-amp0

11)20

01)04

--

-

24 28 t-_

24 u

24 a

---shy

a 0

-

i

Pitalaybull 1)2 -19shy -27shy 35-54-60 bullbullo-150 010100 005-010 middot 1o-so zo-ao 24 28 1 a o 2-11

fshy1127

-25shy

--2+shy

-35-51- 60 1AI)150

- -010100

middot-middot -00~10 middotU~3C)

- - 1Jl2 0

-24 28

27-80 - - - - - - middotshy shyosc-

Descelsbrad oday2to12 penent sl~p~s

Oescalabrado 0 -5 -1 a ~7- 35-44- 45 134-1 35 0 10-100

I ---middot--middot

015-020 So-69

1 zs-~o

I

I---- shy24 24 1 4

I I M--shy

5-10 ----shy middot19shy ~7- 35-44middot 45 130-140 010-100 o11)015 61)89 18 0 17 24

I 11)18 - - - - - - - -I gt18 - - -- - - - ---shy

middot- c~~ Nelurbullt ~bullourcbullbull Weigt Soil Silwy 411012012 Conservation Strvko NalionJI Coopefalle Sell Slrltey Page 1 ol 17

Physlcat Soli Properties-Sa~~ Getman Aft~a Southwealern Puerto Rloo

Ph_yelcal Soil PICperties- San German Area Southwestern Puerto Rlco

Map aymbol and soli name

I Cplth

I _

Send

Ptt

Sl~

Ptt I

Ctay

Ptt

Motst bulk

density

glx 1

Satdf11ted hydroullt

conductlYiry

micro Wee

AvaUabte Wl(bullr

capacity

loWgt

Linear lxtaMibUity

Ptt

Organic rnatcer

Ftf

Erosion redon

Kwl Kd T

Wind orltgtdlblnty

group

Wlod orodlbll~

Indea

ooshytlo$colallfad odoy 111o 20 penenl

] I bull I I iM slopes

Oeampealabfbulldo

1

0-6

r-1_o

-1a

_ -~9 J7middot

-37-

~~s-~5 13middot136 010middot101)

i3s-44-4s middot3o-1 bullbull o lo1ii100middot-015-lllO -1010015

6()39

iso-49 2SSO

1amp-40

2 24 1 bull

17 2 I

10-1B

I bull1s

-

middot- _

-

-

-

1--

i-j-I-

--

_ middot-

- - -

I bullbullbullbull

_1 i

____J l)$f=- I I ~

0Ncalabr~d 1

o clay 20 lo I 60 pelcenl slopes 1

Descelebntdo llLfi Ishyls-10

10-18

gt18

Epc-EI Pepayo grolly clay

1

1middot111--1)

1

-

015-020 1-37middot Js-44-45 1134-1361010100 -37- Tis 5 middot3~~~omiddot~1-~oo- middot 010-01~ -

- _ I I middot-- -----middot -~-I I I

-- --

6089 middot2S50

60-39 111-40

-l --shy

I

24 24

17 24

I i

1 bull

bullbull middot I bull ___ __

I I

66

bull bull -middot-middot- shy

1

I

loam21o12 pelttlnl -M I

El papayo o-2 I-bull

-26-

middot 1

o zaJs 4D 134-136 I0()-1000 o1so2o bull

middotsl)-69 z[)o4o zbull 12bull-bullbull bullbull

1020 17 12-

1

i 4

1

4 I

1as

2-14 middotM- -26- 30-5060 130-140 01()100 010015 60-39 4 1~tf5

bulls -

-_

--

--

--

--

_-_ ~ -middotrmiddot j -

-

- _ _ I _

I --- shy

I I

shy

shy

shy

shy

-middot~ Nelamplrbull l R_ourcn MgtIo Soil SUlvoy 41102012 ConsefVallon Sbullrvkbull NlUonal Coojoenlilte Soil SIJrvey Pagbull ao111

Physlcat Soli Properties-Sa~~ Getman Aft~a Southwealern Puerto Rloo

Ph_yelcal Soil PICperties- San German Area Southwestern Puerto Rlco

Map aymbol and soli name

I Cplth

I _

Send

Ptt

Sl~

Ptt I

Ctay

Ptt

Motst bulk

density

glx 1

Satdf11ted hydroullt

conductlYiry

micro Wee

AvaUabte Wl(bullr

capacity

loWgt

Linear lxtaMibUity

Ptt

Organic rnatcer

Ftf

Erosion redon

Kwl Kd T

Wind orltgtdlblnty

group

Wlod orodlbll~

Indea

ooshytlo$colallfad odoy 111o 20 penenl

] I bull I I iM slopes

Oeampealabfbulldo

1

0-6

r-1_o

-1a

_ -~9 J7middot

-37-

~~s-~5 13middot136 010middot101)

i3s-44-4s middot3o-1 bullbull o lo1ii100middot-015-lllO -1010015

6()39

iso-49 2SSO

1amp-40

2 24 1 bull

17 2 I

10-1B

I bull1s

-

middot- _

-

-

-

1--

i-j-I-

--

_ middot-

- - -

I bullbullbullbull

_1 i

____J l)$f=- I I ~

0Ncalabr~d 1

o clay 20 lo I 60 pelcenl slopes 1

Descelebntdo llLfi Ishyls-10

10-18

gt18

Epc-EI Pepayo grolly clay

1

1middot111--1)

1

-

015-020 1-37middot Js-44-45 1134-1361010100 -37- Tis 5 middot3~~~omiddot~1-~oo- middot 010-01~ -

- _ I I middot-- -----middot -~-I I I

-- --

6089 middot2S50

60-39 111-40

-l --shy

I

24 24

17 24

I i

1 bull

bullbull middot I bull ___ __

I I

66

bull bull -middot-middot- shy

1

I

loam21o12 pelttlnl -M I

El papayo o-2 I-bull

-26-

middot 1

o zaJs 4D 134-136 I0()-1000 o1so2o bull

middotsl)-69 z[)o4o zbull 12bull-bullbull bullbull

1020 17 12-

1

i 4

1

4 I

1as

2-14 middotM- -26- 30-5060 130-140 01()100 010015 60-39 4 1~tf5

bulls -

-_

--

--

--

--

_-_ ~ -middotrmiddot j -

-

- _ _ I _

I --- shy

I I

shy

shy

shy

shy

-middot~ Nelamplrbull l R_ourcn MgtIo Soil SUlvoy 41102012 ConsefVallon Sbullrvkbull NlUonal Coojoenlilte Soil SIJrvey Pagbull ao111

Nlap symbol I Dept~ ad bullonnanw

Ep)-euro1 Itt

Pgtpayo

~ ~- tNm J2 tl20

Sand

PrJ

Sill

Pet

I I

Clay

Pet

-oJst bulk

dt nslly

bull ~ I I

Saturstad Avaliabampe hydraullc water

conductivity tapaclly

_ 1 _Win -

Un~r extGnalblltly

bull - _PrJ -

Organic matter

i -_Pet

o

Ef031on Wind taeto ooodlblllly

group Kw l Ktl T I l I

I

Winderodlblllly

lndu

i

pefQelt slopes

I

1

l s papayo 11-2 1-2~ -4G- 2w~ bull o 1~middot1 36 1011-1000- o 1So2o

2middot14 middot25- middot25- 30511- 60 U 0-140 0111-100 010015

middotmiddotbull - middot- 14-18 1- middot _---middotmiddotr--- - r- middot-middot - -r gt16 - - - i- - -

l EpF-ei - middot bull bull bull bull middot - - middot-

middot bullaOss --middot 1206 - 2lt 2lt bull 86 middotmiddot--- I60middot39 10bull20 17 24 middot- shy

- 1- _ _ _ 1

- I 1--- f--~ I

Papayo j groYOIIyday loam 20 lo 80 percent

I slopebull I _

El papayo 0-2 middot2gt- -41) 211-35- 40 1 ~middot1 36 100-1000 015-020

middot 2-1bull J-zs- -u- raquo5o so Do-bull-lto o111-1oo 1o1D-01s - -middot middot middotmiddot--~ - -- - - - - l- 1shy

1 1 _L _1 1

60-89 20-40 13~2~ I1 - 14 _ ~ -------

16o-aa 1o-2o 17 24

I [gt16 I I l I I I F~eaayo

_ ____]I -- middot1middot-middot- 1- middot-middot middot

to 2 percent Elope I

i-~-=- lo-1 1-bulls- 11- bull soo-sa 1raquo1bullo obullo-bull oo o131s _l soe9 3o-6o 24 24 s 4 oo

7middot 17 -15middot middot31middot 45-S-4-58 130middot1lt0 010middot100 middot2~14 190-250 11)50 2 bull bull 2bull -------L

172 -bull2middot

42middotstS T-2i--33-

middot30-

511-55-ss 130-1 40 o10-1oo

bull5-4~ 55 1130-140 01 11-100

1o1oo13 9D-25o

1 01~~-~250 o11o 24 2bull

01middot30 24 24 J - I

I I Phyelul Soli Propert~a-San German Are~ SouthweatGm Puerto RJco

I

Ptysical Soil Properties-San GermM Area Southwestem Puerto Rico

~~-- Natul Re11auroobull lNeb 501 SurveY middot 411012012 _ ConebullrvbullUon Servke National Coopetalive Sotl Survey Pe~e 9 of 17

-----------

--

MapampymboJ Cpth Sand Sl~ Cloy Molllt Saturated Available Unar Otgank EIOIIO Wind Wnd and soli nbullmbull bulk hydraulic wattr ownslblllly mbullttbullr factoB orodlblllty orodlbllly

denllty conductMty eapatlty graup lndaz IIW Kf T

In Pet Pd Pd gtc mktoWVSec lnn Pet Ptl I FrA- IFtatemldid

doyOto l penent slopes I ____j-- ---- -middot middot- I middotmiddotmiddot-middot - bullFraltwridad jD-13 middot23middot middot29- 408middot 80 117middot125 001~10 012018 90160 2~0 2 24 IS 86

1H7 middot18middot middot22middot 4~060 117middot125 001~10 012018 90middot160 10middot20 24 24

17-65 bull g -n middot 40~6-68 UG-125 001~10 012~018 90-180 00-05 2 2 I middotmiddot-- _- ~ -- --middot- -- middot- _-J-middot-middot-- --middot-----middot --middotmiddotmiddot----- - shyFr8-

Fratemtdad Clay 2 to s Ipercent Iamplopeamp bull

Fralemdad 0middot13 middot23middot middot29- bullo-8- so 117middot125 OOH10 012018 90middot160 1200 24 24 5 4 86 bull -middot-- - bull

113-17 1middot18middot ~2middot 4G-60middot 60 117middot125 001~10 012018 90middot160 10middot20 24 2 bull

uas middot 9middot middot 21) 41)66- 68 12o12S 1oo1-010 012bull018 90-180 00~5 24 24

GnA-Gwnka clay 0 lo1 percant slopes I

Gvanica 0-lt bull 3middot middot 15- 85-82middot 85 0 90-1 20 001010 009-015 90middot250 30SS 24 zbull 5 86bull1--middotshy2 bull Smiddot -15- 65-80middot 85 090-120 001010 010015 90middot250 10middot35 24 24 12middot52 middot Z1 middot 6075- 85 0901 20 1OOHI10 007~11 90250 05middot15 2 24

su11 1middot 2- middot21- 6073- 85 OQ0-120 001~10 005-010 90250 0005 2 24

I

PII)$1Gal Soil Pt~e111K-San German Area Soulhwostecl Puamprto Rlco

Physlcll Soli Propernn- Sin Gennan Alfi Scuthwatem Puerto Rico

shy

l N1turalRuourcu wb SciSltMy 411012012 CGhUtv~Uon SeNtu Poge 10ct1 7 - ~ SQISltHvey

--

---

-- -

---

Map $ymbol Ooptl Sand Sl~ Clay Moist Satunuus Avallabiltgt Lrnear orvant~ Eroston Wind Wind and soil name bulk hydlt8UIIe water extbullnslblllty matter taetara etodlbliJty orltgtltllblllty

dbullnslty eonduc1hllty eapacfty group Index Kw Kf T

In Pet Pet ~I gfw micro mlsec I nAn Per Pel I I -- -middot- --

GyCshy i I Guayacan day S IO 12 percent stapes---- -middot i

shyGuay3ltdn 0-8 -211- -27- 20-46-60 110-115 010-100 loll)-01$ ol)-ze 21)-80 10 17 3 4L aamp-- ---middotmiddot

8-12 -26- middot27- 20-47middot60 12$-140 010middot100 i011)-020 00-29 1D-20 10 -15

12-26 -31- -2amp- 120-41-60 12S1AO 010-100 io11)-02o oo-29 10middot20 10 15 middot~ 2$-45 -44- -33- 10middot23middot 50 121)-130 100middot1000 IOOil-01 s 00middot29 00 20 20 ---

-~~-

45-59 -44- -31middot 5-2S 40 121)-170 100middot1000 loos-o1s 00-29 00 32 32 -middotshy59-76 -9- ~1)- s1o- -to l50-171 100-1000 008-015 oo-ze oo

- -- -2~ -o Lshy7$-91 -31)- -32middot 5-86middot 40 121)-130 100-1000 008-015 00-29 00 20 20 i

LdA-la Luna silty day I I

Iftgtam 0 to 2 I Ipe1cent I I ()CC3Sonally ~IOPQS

I i flooded ____T --

-~1022-- jn--40-60-LaJuna o-11--lio- -61)- 27-31)- 40 116-115 jo1o-1ooo r-2oT~o -Is - 4 86 I I11-ZO - 6- -55- 27-39- 40 1110-115 1 o~o-100 -~~Jo-ze 36-40 I20 ~0-~-- ------i

120middot58 bull 7middot middot54- 27-39-40 115middot130 010middot100 021)-022 Oo-29 10bull20 17 17 I I 58-75 -~ -55- 121)-39- 40 115-125 01~100 1 o1s020 00bull29 05middot20 20 j 20 I

Physical Soil Properties-san Gennan Area $()uUwastaro P~H~ntgt Rico

Phyf~1 Sol Properties- Sen Gennan Aroa SouthWHtom Puerto Rteo

Hatural Reaources Web Soli Survey 4102012~~ ConsetvaUon Servke NaUonal Cooperative SoU Sut18) Pbullge 11 of17

Phyiical Soil Propertiet-San Gennan Area Sou(tlweJttm Puerto Rico

P-ytfcal SoU Pmpertfaa-Stn German Ama SouttlwHtem Puerto Rico

Map symbol and sell name

Ooplh Sbullnd SIH Clay Moffi-t bulk don~

Saturotod ~ydraullc

conduettv1ty

Available wat~r

eapaelty

Linear emnfbltlty

Org-anic matter

Eroston bctoll

Kw Ki T

Wind orodlbll~

group

Wind orodl blllly

fnclampx

In Pel I Pet I Pel gkc micngt~c IMII Pct Pet -middot-middot -fllamp--lar9ueri dgty 2 to 5 perrent

-Palguora

I ()7

17-22 22-lS

middot11middot

middot23shy

i

3()

-2ampshy

l-22shy

Sa-59-60

3amp-Ci- 60

15-34middot 60

i

-10CH25 0 1()100

IZD-1Z5 010-100

12()140 1001000

012-CI18

012-018

009-018

middotshyooso 00-30

00-30

-2070

21)30

06-20

I middotshy

24 24 15

24 124 I

24 i24 _I

bull - middotshy

88

i I

I j39-57

I i7bull79

-61 -

middot1 s -21shy

-33shy

15-1amp- 80

50-12middot 60

1lt()1lt5

12Qo140

100middot1000

010middot100

middot 012middot018

012middot018

00-30 00-30

02-20

02-10

24

24

24

2bull 1 -shy

Nihtral Resources Web Soi SoNey Conurvatlon Servtc National CocpeltaNe Soli SoNey Page 12 ol17 = 41012012

Physic~I Soil Propertieamp-5an German Area Southweslem Puerto Rico

Ph~thQI son Pruperthte- Saq GenTNJn Arebull Sovth~tem Puerto Rico

Mop symbol J Dopth Send SIM Cia) fleofat Saturated Avanebkt Llnnr IOrgbullnlc I Erolon Wind I Windandampofl name bulk hydnullc water GXblnslblllty mattt ( l tiGrl orodlblllly erodibility

donoMy Cortdurtlvtty capacity erou~ lndeampKw l Kd

~-=yo- I Pet Pet Pet bull _~middot~~~ ~---~ Pet I Pa I l j

T

Igtb i--- Ma~ I Seboruco compttx40 lo 60 ~eroent slopes lL---------J---1- --1 middot---1

Pltlhaya 0-l imiddot1lmiddot middot 27 lS-54- 80 U0-150 010-100 00$-010 10-30 20-80 24 28 j 1 Ibull 0 __j

l ~ ~-~~---~~5- _ J-~ 1amp5-51-60 1140-1 50 010100 ooso1o 1o30 middot- l l_o 2lt 28) I

111middot27 1- _ - 1- - - - - I I 127-80 1- - - 1- - - i- -- - --- I I

Limestone 1- IOIJtcrap I

eridicsoil ~- Imois11JIQ I1

I s~ lo2 f1s- lss l1sao 4o j 4s-15s 1oo1ooo -looso-2middot l1oJo l2o-u l 11 j2a 13 1M3 ~4---L----1 1oJo 11 2a I 10-30 17 28 - 1

[11-1~_ middot25- S__ ~~~~-~~J middot~~1ooo looH10 ~~~ -~~o__ ~~ -~middot~L middot I 111-26 -25- -5rgt- 15-20middot so 14fgt-15Sjuo-10oo 1oos-o1o 10-Jo - [ 10-2o 17 1-28 ___l ___middot shy

26-31 o- -40- 10-20- 30 14-S-1$5 100-1000 005-010 10-30 110-20 17 128

31I 1~ 1- - - - 1- J _]_ -shy

~10 Neuarl bsour04ta Web sCti SWey (11012012 Connrvatlon Sbullntlc-e Nallonal Coop~Soi SUnoey Page 13 of 17

Physic~I Soil Propertieamp-5an German Area Southweslem Puerto Rico

Ph~thQI son Pruperthte- Saq GenTNJn Arebull Sovth~tem Puerto Rico

Mop symbol J Dopth Send SIM Cia) fleofat Saturated Avanebkt Llnnr IOrgbullnlc I Erolon Wind I Windandampofl name bulk hydnullc water GXblnslblllty mattt ( l tiGrl orodlblllly erodibility

donoMy Cortdurtlvtty capacity erou~ lndeampKw l Kd

~-=yo- I Pet Pet Pet bull _~middot~~~ ~---~ Pet I Pa I l j

T

Igtb i--- Ma~ I Seboruco compttx40 lo 60 ~eroent slopes lL---------J---1- --1 middot---1

Pltlhaya 0-l imiddot1lmiddot middot 27 lS-54- 80 U0-150 010-100 00$-010 10-30 20-80 24 28 j 1 Ibull 0 __j

l ~ ~-~~---~~5- _ J-~ 1amp5-51-60 1140-1 50 010100 ooso1o 1o30 middot- l l_o 2lt 28) I

111middot27 1- _ - 1- - - - - I I 127-80 1- - - 1- - - i- -- - --- I I

Limestone 1- IOIJtcrap I

eridicsoil ~- Imois11JIQ I1

I s~ lo2 f1s- lss l1sao 4o j 4s-15s 1oo1ooo -looso-2middot l1oJo l2o-u l 11 j2a 13 1M3 ~4---L----1 1oJo 11 2a I 10-30 17 28 - 1

[11-1~_ middot25- S__ ~~~~-~~J middot~~1ooo looH10 ~~~ -~~o__ ~~ -~middot~L middot I 111-26 -25- -5rgt- 15-20middot so 14fgt-15Sjuo-10oo 1oos-o1o 10-Jo - [ 10-2o 17 1-28 ___l ___middot shy

26-31 o- -40- 10-20- 30 14-S-1$5 100-1000 005-010 10-30 110-20 17 128

31I 1~ 1- - - - 1- J _]_ -shy

~10 Neuarl bsour04ta Web sCti SWey (11012012 Connrvatlon Sbullntlc-e Nallonal Coop~Soi SUnoey Page 13 of 17

Ph)ISJcal Soli Propertfu-San Garman Alea Soulhwbulllltm Puel1o Rico

Ph~thalSoli Properthta- SliJn Gbullnnan Arabull SollthweWm Puerto Rico

1fapsymbol I Dopth Sand Sill Clay Malst Saturated Avanattht L~nat IOrgahlc I ErotJon Wind Wind end soQ nelne burbull h)drauUc water bullXWn~~biUty mt~nor faccore trbdlblllty bullrodlblllty

density eonduc11vlty eapaelty group ~ndexKw l K~~ T

Pel Prt bull Prt ~gt-laquo 1 micro mlsoc 1 - Pel _ ~ Plamp---Poo

I Blanco cloy 0 lo 5 percenl

bull slOpes

I Pozoblbullnoo 61 zj l-21middot 4()(6-60 111H40 oHHoo bull

101~ 15 00-29 5010~0 - -~ --7 b middotL 86 I

bull

_ __ 7-22

22--30

Jo-eo

middot26shy

middotraquo ~__

-27shy bull bull 30-47- 60 12G-IJO 010100

]middot38shy lzo-32- so 120Ho o10-100

___3middot 15-23-40 120130_l100-1ooo

010020 -shy -

o1G-o2o

ooa-o1s

0029 l oo-29

Joo-u

_

30-70

~~ -0 fos-Jo

10

10

3_0

IS

middot

20

I

I

o

J

J

1bull

PzC-Pozo I 1

Blanco day 5 lo 12 peltcenl slopes

I Pozo blanco lo-7 i-28shy---shy

zmiddotshy - 40-lt6middot60 110140 010-100 010-015 oo-29 so-100 10 17 --t-shy

3 middot 4i middotmiddot-ti_j86 I

1 17-22 1middot211shyI-shy 22-JO -JO

-shy ---osD ]-lt_

-27shy 307shy80

middot38shy 2032middot 60

~-- -~~zbullo

Uo-1lt10 010-100

~~-O~t0100 12o1Joj1oo-1ooo

010-020

010020

ooH15

0029

0029

oo-29

3070

1o-20

os-10

10 15 _[ _

10 15

-- l middot middot --middot ---1---1

PzO-Pozo B(aooo Qay 1210 20 peroeot

i amplopeamp I I I _j_1 1 11 Pozo blanCltgt 07---2-- -middotmiddot 1middot27middot 140-lt6-60 110-1lt0 01o-100 010-015 00-29 _lso-100 10 ]11 13 4L 86

7-22 middot26- middot27- 30-47middot 60 120middot130 OfD-100 010020 I00-29 3070 10 15

- 22-3o -3o- -Ja- J2D-32middot 60 12o-1Ao o1o-1oo o1o-o20-jo029 j1o-2o 10 1s -~-- - -shy

J(Ho ~bull- _]-3) J23-lto UG-130 1~o-12oo ooe-015 Joo-29 Jos-to- 20 l -2~ -- - I

i Naluml Ra11aurwe Web Sogt Suey 411012012 Co1uu ~rvaUon Setvlco Nalionol Cooalive SOll SuiVef Pege H ol17

---

Ptyseal Sltlit Proponles-San G4)tm311 Ar~a SoUhw~tam PlHintgt Rl~

Phyatcal Son Ptopertl$s- San Gerrnan Anu~ Sou1hweatem Pu~n~o Rfco

MEip$yrnbol and tegtfl na~

Dopth Sond Sl~ Cloy Molgtt bolk

dtnslty

Sotvroted hydrauHc

conductlvlty

AYBIIII~III

water capacity

LTneat bulllt~bullnolblllty

Organ1c matter

Erosion factor$

Kw Kf T

Wind erodl~lllty

QfOUp

Wind erodibility

fndu

-middot -shy In Pel I Pltt Pel gklt microm6ec nAn Pel i Pet -middot I SeA-San

Anton day fOSITI 0 to 2

percont slopes ~ oeeasJtgtnaly1 1oodeltl

I

I bull

I I I

1

l

San ~nton j0-3

e-13 -3()

-23shy

-35shy

-40shy

28-35- 45

12amp-37- 45

125-13~ 400-1400

125-135 400-1400

011-020

01()020

30-59

00-29

26-SO

2030

17

17

20

24

5 bull 8amp

13-24

1 24bull31

-19shy

middot2Zmiddot

-43shy

-38shy

22-3S- 45

22-4050

123-135

123-135

400-1400

4001400

012-ltJ20

012-020

30-59

i 30-59

103-20

03-20

17 17

17 _t--shy

17 --------~

- -

shy31-41

41-54

~()

--17shy

-18shy

-23shy

22-22- -5

122-U -5

141-145 400-4200 012-020 100-29

12_135 ro -oo--middot1otlo~ -- 3oss

OHO

03-20

17

11

17

1 I

Sgo-son Gamprmanshy0ey eompktx 5 to 2~ peroelt1t slopes-San g~tman

54-70

0-lt

-51shy

middot35shy

-25shy 22-23- bulls__ __

-30middot i35-35- 50

121-135 400-4200

14()150 010-100

012-020

005-010

00-29

i00-29

03-20 -middot

2()-250

17 17-------shy

24 26 1 6

I

middot0 I______

Ouey

4middot10

10-60

G-13

middot32middot

-22middot

middot3(

-3~

35-38middot 50 1~1-150 016-100 --~ _ ____

- _ -31-3~ so bull14()150 1400-4200

005-010

-005-010

00-29

-0029

~ 16-250

-2()40

24

24

26

I 28 1 8

0

I

13-17 -25shy -45shy ~30-3( 60 1~1-160 1400-4200 005-010bull 0()29 11-30 24 28

17-35

3~0

--

--

-1shy

-

-- = middot middot --shy - ---middotmiddot --shy

-__ ___

_

j~

--

1

~tM Nlt~-tral Resoure~bull Web soJ Survey 4lloi2ol2 - middot fiE Conervatlon Servi(O Nat1tgtnal COOJH)faliW Sol StUVS) Pbullge 15ol17

- - - --- -

Map symbol Opth sbullct $[~ Cloy NoloI Sattl~ted Avollablo Llnear OrganJc Erosion Wind Wind 1utd eon name bulk hydraulic water olttonbullI~Uity mattampr factor3 ongtdlblllly erodibltrty

dtuuotty eondueUvtty oapampltty group fndampx Kw Kl T

In Pel Prl Prl gclt miaDIMltc lnAn Prl Plotf--middotmiddotmiddot -------middotmiddot --- -shySgF--San -Du I I I I

mtnjllox 20

Ilo 60 I - --middot

San german 1)4 -3$- o- middot-r3$-3 r1bull0150 010-100 Q05-010 oo-~9 2()-250 24 25 8 0 -middotshy10 middot32- -ao- Js-3amp- so Iuo-1so 01()-100 00$-010 0 0-29 1~250 24 28I

-r - middot---middot --1middot-- -- 10-aG - - - - shy -- o-13 zz- -36- ll0-3- so 140150 1400~~-00 005-010 oc-zs tzc-40 24 28 1 8 0

13-17 -25- -1$- l)()-l)()- 60 1A01SO 14 oo-4200 005-010 0029 1()30 14 28

17-35

l~bullY - - - - - - i- I

35-80 - - - - - - - shy--ua--uroan Jald I~ I -- uroan land - - - - - I ~

VaA-Vayas oil1y ltlay 0 to i 2 pftrcent slopes accaclonally ftooded

Vayas D-5 -15- -53- 2amp-3~- 60 130-140 0 fD-fOD 014-ll22 M-90 20-40 24 24 5 4 86 5-12 -55- 2s-3~- eomiddot 1ao-1bullbull ti 01 tgt-100 012018 shy middot1 Dshy 31l-00 03-20 24 24- _-----~middot 12-23 bull 8middot ~- 28-311- 60 1311-140 01G-100 012-018 02-10 2430-60 2bull

23-62 bull 8- -64- IID-33middot 60 130-135 01G-100 012middot018 30-60 02-)5 24 24 middot-I -middot 1LWater I

I ( Wiiter 1- - --_ 1- 1- shy- -middot-middot 1- 1 - - I middotshy --

Ph)ltal Soli Pr09erties-seo Gennan Area Soulhwettem Puerto Rico

Physical Soli PropettfH- Sen Getman Arvbull SollltlWHtamprn Puerto Rico

N~ atural tteourcu Web Sal SUrvey 41012012 _ Cont-arvamptlon Srvte Nalional Cooperativamp Sell Sbtvey Page 16 of17

--middot-----~

Ptyslcal Soil Propenle~San Getman Arta Sou1llwaslem Puerta Rica

Data Source Information

Soil Survey Area San German Area Soulhwestem Puerto Rico Survey Area Data Version 3 Dec 6 2008

NltiINI Reaourcebull Vleb Soli Survoy lt111012012~ Conwrvatfon ServJte thtlonat Coopera~ve S11a Survey Paye 17 o(17

Water fi)ati~~$-San Gennan A~a Southlestem Puetto Rico

Water Features

This table gives estimates of various soil water features The estimates a1e used in land use planning that Involves engineering considerations

Hydrologic soilgroups are based on estimates of runoff potential Soils are assigned to one of four groups according to the rate of water infiltration when the soils are not protected tgty vegetation are thoroughly wet and receive precipitatior frcom long-duration storms

The four hydrologic soit g1oups are

Group A Soils having a high infiltration rate tow runoff potertial) when thoroughly wet These consist mainly of deep well drained to e)(cessively drained sands or gravelly sands These soils have a high rate of water transmission

Group B Soils having a moderate Infiltration rate when thoroughly wet These consist chiefly ofmoderately deep or deep moderately well drained orwell drained soils that have moderately line texture to moderately ooarse texture These soils have a moderate rate of water transmission

Group C Soils having a slow infiltration rate when thoroughly wet These consist chiefly of soils having a layer that impedes the downward movement ofwater or soils ofmoderately fine texture or fine texture These soils have a slow rate of water transmission

Group D Soils having a very slow infiltration rate (high runoff potential) when thoroughly wet These consist chiefly ofclays that have a high shrink-swell potential soils that have a high water table soils that have a claypan or clay layer at or near the surface and soils that are shallow over nearty impervious matenal These soils have a very slow rate of water transmission

If a soil is assigned to a dual hydrologic group (NO BID or CD) the first letter is tor drained areas and the second is for undrained areas

Surface runoff refers to the loss ofwater from an area by flow over the land surface Surface runoff classes are based on slope climate and vegetative cover The concept Indicates relative runoff for very specific oonditions Jt is assumed that the surface of the soil is bare and that the re~ntion of surface water resulting from irregulanties in the ground surface is mirlmal The classes are negligible very low low medium high and very high

The months in the table indicate lhe portion of the year in which a water table ponding andor flooding is most likelY to be a concern

Wetltlrtable refers to a saturated zone in the soil The water features table indicates by month depth to the top (upperimi() and base (lower limit) of the saturated zone in most years Estimates of tile upper and lower limits are based mainly on observations of the water table at selected sites and on evidence of a saturated zone namely grayish ccolors or mollfes (redoximorphic features) in the soli A saturated zone that lasts for less than a month Is not considered a water table

Hatunl R~altgturc~s Web Soil Survey 41012012Consorvatlon Ssrvlcs National Coopetallve Sltlil SuMy Pag~ 1 of 8

Waler Features-S~m Gennn Atea Soulhwastem Poetto Rbullco

Ponding is standing water in a dosed depression Unless a drainage system is installed the water is removed only by peroolation transpiration or evaporation The table indicates surtece water depth and the duratiOtl and frequency ofponding Duration is expressed as very briefif tess than 2 days brief if 2 to 7 days long if 7 to 30 days and very long if more than 30 days Frequency is expressed as none rare occasional and frequent None means that pondlng Is not probable rare that il is unliKely but possible under unusual weather conditions (the chance ofponding Is nearly 0 percent to S percent in any year) occasional that it occurs on the average once or less In 2 years (the chance of ponding is 5 to 50 percent in any year) and frequent that it occurs on the average more than once in 2 years (the chance of ponding is more than 50 percent in any year)

Flooding is the temporary inundation ofan area caused by overflowing streams by runoff from adjacent slopes or by tides Water standing for short periods after rainfall or snowmelt is not considered flooding and water standing in swamps and marshes is oonsidered ponding rather than flooding

Duration and frequency are estimated Duration is expressed as extremely btiefif 01 hour to 4 hours very brief if4 hours to 2 days briefif 2 to 7 days long if 7 to 30 days and very long it more than 30 days Frequency Is expressed as none very rare rare occasional frequent and very frequent None means that flooding is not probable very rare that it is very unlikely but possible under extremely unusual weather conditions (the chance of flooding is less than 1 percent In any year) rare that it is unlikely but possible under unusual weather conditions (the chance of flooding is 1 to 5 percent in any year) occasional that it ocours infrequently undel normal weather oondillons (the chance of flooding is 5 to 50 percent in any year) frequent that it Is likely to occur often under nonnat weather conditions (the chance of flooding is more than 50 percent in any year but is tess than 50 percent in all months in any year) and very frequent that it is likely to occur very often under normal weather conditions (the chance of flooding is more than SO percent in all months ofarw year)

The information is based on evidence in the soil profile namely thin strata ofgravel sand sill or clay deposited by floodwater irregular decrease In o~anic matter content with increasing depth and little or no hOrizon development

Also considered are local information about the extent and levels of flooding and the relation ofeach soil on the landscape to historic floods Information on the extent of nooding based on soit data is less specific than that providelt by detailed engineering surveys that delineate flood-prone areas at specific flood frequency levels

tlgtmiddot~ Natural RuoUfit8- middotmiddotmiddot middot ----------w-bullbsousu--~-----------------4110120-12 ~ Conervetlon Ssrvlcs NaOOnaJ Cooperative Sol Survey Pagel of s

Map unit bull ymbol and aon Ydrologlc Surfan Month Warampt table Poncflng Floodinggroup runoH

Upper limit Lower llrnlt SUlfalu Du-QIUOn Fq uency Duradon Fraqueumiddotl~) damppth

Fl bull Fl Fl-- bullbull AQ~ bullilly ctayaom

5 to 20 peteell4 slottes I --- -bull Aguiila c MedliJm bullJan-Oeamp - - - - None --middot - -- AkA-Agultle da)

I bull bull OOCIIiiolla11y ponded bull I -- --l- Ag~~ -- -

0 t~agtlglbte Aug1-l - 00-20 Bllof Oecacloll

ll -middotmiddotmiddotmiddot

l -t -

- None -0 Nogllglbfe September - - 00-20 Brief Ooculona None

~--- middot 0 Nogflglblo October - - 0020 lariet Ouaslo11a None

AI[)-AJtomlra grawlly cloy 1 Ibull 2 to 20 perCnt slopes I I-- shyi Anamira bull 0 M edium Ja~Dec _ - - - Nooe -r---- -- middot- CeACanagflna day o lo 2

percent slopes I I I__ middotmiddotmiddot- -----middotmiddotmiddot Cartageos 0 low IJafi-Oec - - Nonamp middot- - - - CtA---cortampda sitty day loam

0 to 2 percarrt slopepound oocuionally ftooded

Lbullbull ------Corlodo c Negligible IAugubulll - None Bl1el Ooculonal -

- None 811ef Ocaslonal

None S~ef Occasional-

- - --middot [ c Nagllglbfe September - - -lc Negligible October - - -L ---

Wattr Featuamp-Sah Garrna11 ~Southwestern Puerto Rico

shy

Water Features-San Gemlampn Arampa Southwampstam Putno Rico

Report-Water Features

shy

shy

shy

shy

shy

lSO Nbulltural RbullaouteM Nampb sa Swwy ztFi 4lltV2012ColllampanltaUon Servtc lltalonJ Coop1M Soil SUNey Pege3or8

Waler Features-S~m Gennn Atea Soulhwastem Poetto Rbullco

Ponding is standing water in a dosed depression Unless a drainage system is installed the water is removed only by peroolation transpiration or evaporation The table indicates surtece water depth and the duratiOtl and frequency ofponding Duration is expressed as very briefif tess than 2 days brief if 2 to 7 days long if 7 to 30 days and very long if more than 30 days Frequency is expressed as none rare occasional and frequent None means that pondlng Is not probable rare that il is unliKely but possible under unusual weather conditions (the chance ofponding Is nearly 0 percent to S percent in any year) occasional that it occurs on the average once or less In 2 years (the chance of ponding is 5 to 50 percent in any year) and frequent that it occurs on the average more than once in 2 years (the chance of ponding is more than 50 percent in any year)

Flooding is the temporary inundation ofan area caused by overflowing streams by runoff from adjacent slopes or by tides Water standing for short periods after rainfall or snowmelt is not considered flooding and water standing in swamps and marshes is oonsidered ponding rather than flooding

Duration and frequency are estimated Duration is expressed as extremely btiefif 01 hour to 4 hours very brief if4 hours to 2 days briefif 2 to 7 days long if 7 to 30 days and very long it more than 30 days Frequency Is expressed as none very rare rare occasional frequent and very frequent None means that flooding is not probable very rare that it is very unlikely but possible under extremely unusual weather conditions (the chance of flooding is less than 1 percent In any year) rare that it is unlikely but possible under unusual weather conditions (the chance of flooding is 1 to 5 percent in any year) occasional that it ocours infrequently undel normal weather oondillons (the chance of flooding is 5 to 50 percent in any year) frequent that it Is likely to occur often under nonnat weather conditions (the chance of flooding is more than 50 percent in any year but is tess than 50 percent in all months in any year) and very frequent that it is likely to occur very often under normal weather conditions (the chance of flooding is more than SO percent in all months ofarw year)

The information is based on evidence in the soil profile namely thin strata ofgravel sand sill or clay deposited by floodwater irregular decrease In o~anic matter content with increasing depth and little or no hOrizon development

Also considered are local information about the extent and levels of flooding and the relation ofeach soil on the landscape to historic floods Information on the extent of nooding based on soit data is less specific than that providelt by detailed engineering surveys that delineate flood-prone areas at specific flood frequency levels

tlgtmiddot~ Natural RuoUfit8- middotmiddotmiddot middot ----------w-bullbsousu--~-----------------4110120-12 ~ Conervetlon Ssrvlcs NaOOnaJ Cooperative Sol Survey Pagel of s

Map unit bull ymbol and aon Ydrologlc Surfan Month Warampt table Poncflng Floodinggroup runoH

Upper limit Lower llrnlt SUlfalu Du-QIUOn Fq uency Duradon Fraqueumiddotl~) damppth

Fl bull Fl Fl-- bullbull AQ~ bullilly ctayaom

5 to 20 peteell4 slottes I --- -bull Aguiila c MedliJm bullJan-Oeamp - - - - None --middot - -- AkA-Agultle da)

I bull bull OOCIIiiolla11y ponded bull I -- --l- Ag~~ -- -

0 t~agtlglbte Aug1-l - 00-20 Bllof Oecacloll

ll -middotmiddotmiddotmiddot

l -t -

- None -0 Nogllglbfe September - - 00-20 Brief Ooculona None

~--- middot 0 Nogflglblo October - - 0020 lariet Ouaslo11a None

AI[)-AJtomlra grawlly cloy 1 Ibull 2 to 20 perCnt slopes I I-- shyi Anamira bull 0 M edium Ja~Dec _ - - - Nooe -r---- -- middot- CeACanagflna day o lo 2

percent slopes I I I__ middotmiddotmiddot- -----middotmiddotmiddot Cartageos 0 low IJafi-Oec - - Nonamp middot- - - - CtA---cortampda sitty day loam

0 to 2 percarrt slopepound oocuionally ftooded

Lbullbull ------Corlodo c Negligible IAugubulll - None Bl1el Ooculonal -

- None 811ef Ocaslonal

None S~ef Occasional-

- - --middot [ c Nagllglbfe September - - -lc Negligible October - - -L ---

Wattr Featuamp-Sah Garrna11 ~Southwestern Puerto Rico

shy

Water Features-San Gemlampn Arampa Southwampstam Putno Rico

Report-Water Features

shy

shy

shy

shy

shy

lSO Nbulltural RbullaouteM Nampb sa Swwy ztFi 4lltV2012ColllampanltaUon Servtc lltalonJ Coop1M Soil SUNey Pege3or8

Map unit bull ymbol and aon Ydrologlc Surfan Month Warampt table Poncflng Floodinggroup runoH

Upper limit Lower llrnlt SUlfalu Du-QIUOn Fq uency Duradon Fraqueumiddotl~) damppth

Fl bull Fl Fl-- bullbull AQ~ bullilly ctayaom

5 to 20 peteell4 slottes I --- -bull Aguiila c MedliJm bullJan-Oeamp - - - - None --middot - -- AkA-Agultle da)

I bull bull OOCIIiiolla11y ponded bull I -- --l- Ag~~ -- -

0 t~agtlglbte Aug1-l - 00-20 Bllof Oecacloll

ll -middotmiddotmiddotmiddot

l -t -

- None -0 Nogllglbfe September - - 00-20 Brief Ooculona None

~--- middot 0 Nogflglblo October - - 0020 lariet Ouaslo11a None

AI[)-AJtomlra grawlly cloy 1 Ibull 2 to 20 perCnt slopes I I-- shyi Anamira bull 0 M edium Ja~Dec _ - - - Nooe -r---- -- middot- CeACanagflna day o lo 2

percent slopes I I I__ middotmiddotmiddot- -----middotmiddotmiddot Cartageos 0 low IJafi-Oec - - Nonamp middot- - - - CtA---cortampda sitty day loam

0 to 2 percarrt slopepound oocuionally ftooded

Lbullbull ------Corlodo c Negligible IAugubulll - None Bl1el Ooculonal -

- None 811ef Ocaslonal

None S~ef Occasional-

- - --middot [ c Nagllglbfe September - - -lc Negligible October - - -L ---

Wattr Featuamp-Sah Garrna11 ~Southwestern Puerto Rico

shy

Water Features-San Gemlampn Arampa Southwampstam Putno Rico

Report-Water Features

shy

shy

shy

shy

shy

lSO Nbulltural RbullaouteM Nampb sa Swwy ztFi 4lltV2012ColllampanltaUon Servtc lltalonJ Coop1M Soil SUNey Pege3or8

WateJ Features-San German Area Soulhwestem Puerto Rico

Water Featu~San Gemampn Area Southwstom PU$1tO Aleo

MltJp untt oymbol and 11011 IHydrologic name group

Surface runoff

Month WaNrtablamp

Upper limit I Lowor llmfl

Pondlng

Surface DuraUon

Flooding

FreqlW)ncy Ouratfon Frequency depth

CuO-Ccgtsla-Pitahaya oompex S lltl 20 percent

1 I F1

II

- I F -I Ft 1---shy middot-- shy

slo~s

Costa 0

PllaMybull 0

Cu~oslltl-Pilshybull compfsx 20 tcgt 6(1 perta()l

Very high

Vetyhgh

Jal)o0ec

IJaB-0lt

I

- bull-

~- 1-

1

-

1--

i-None

INonbull

s~pes bull

Costa 0 Very high - Nono

Fdahaya D ivelty high j_- Nonltgt

osc-oescalabrado day 2 to 12 ~teent lop(ls

1 ----- shyOegcaahrs~~dn omiddotDs~scalabrado day 12

Medium

- - -

JanmiddotOe~- =----middotmiddot~ 1

- - I

None

1 I I

I

j I

to 20 petcenl slopes

I OQcalabradcgt -cshyDsF-Oescalabrado day 20

to 60 perltent sfopes

Oescallgt~o o

E~ Papayo gravelly I

Meelum

High

- -middot

Jan-~c - j shy----middot- -- - middot--I Jan-Dec - -

-l

-middot--shy-

-I 1shy1

None

Nnne

1

I

1

I

I day Joam 2 lo 12 pecenl

bulllopes

Elpapayo 0

EpD-El Pbullpayo gravelly bull day 10~111 12 to 20 percentI slopes

El pspayo ID

Medium

M~dum

Jan~-middot

Jo~

-

1shy

-

I

t

-

lshy

-

-

INcme

I

None

1

Jshy1

1shy

1shy1

_j

J

I

--liStM Nstu111l Ro-sourceamp W~b Soil Survey 41102012Conurvatfon SeNke National Cooperative Soil SuNey Page 4 of8

Map untt symbol and 11011 nomo

Hydrologic group

Surfce nmoff

Month Water tabla

Upper limit Lcgtwor llmtt Surface ltloplh

Pondlng

Duration Frtqubullncy

fJoo

Ouratton

clna

Freqpency

EpF-El Papoyu graDy day kwTI 10(0 60 peroerl

s~oFbull

Ft Fl Fl

I I

I El papaya 0

FeA~e ctay 0 to 2 percent i I Slope$

Fe oo

HIOll

MtdliJm

J~

Sepcember

-

40-60

-I

gt60

-

-

-

-

None

I None

-

- --Nonbull

0 10 r---- iO Mtdium

Medium

()doter - --November

41gt-60 -

41gt-60 gt60

jgt~0 -

---

None

Ncne --

Hone

Hone FrA-Fralemidad day 0 lo 2

percent slopes I Ft11lemid11lt1 0 Medium Jan-Dec - - - - None -

FrB-Ffilemidad day 2 to 5 pbullrCenl slcpas I I

i Fnlemldad D Medium Jen-Oec middot------middot-- _ middot- -middot -GnA-Guano day 0 to 1 percent sJopes middot I middot----middot----middot--middot middotmiddotmiddot-Guanlca D Nogllgtblo August

-

-

-

-

-

00-15

0 _ Nona 0

Long Frequent -0

None

0 Nogllglble September - - 00middot15 Long FreqYent - Nona----D Negligible October - - 00-15 -middot- Long Frequampnt ---middot------ - - - -middot - None

middotG)IC-Guayecan clay 5 lo 12 peroeot slopes I

bull Guayacan 0 H~h -- Jan-Dec - - - - None -- -middot

Walar Feawres-San amplrman AMa Soutnwutbullrn Puono Rloo

W11tor Feature-Sao German Area SoutrrMetem Pubullrto Rtto

shy

shy

shyshy

shy

~ Natural Rbullsourcea Web Soil Survey 411012012 Conurvatlon SNkbull NlllonalCoopolta~ So~Survoy p-~middot s ol 8

--

- - - - -

--

-

I

Map unit aymbolbullnd soli Hyd~loglc Surface Month Water tabte Pondlng Flooding name grovp runoff

Upper llmlt Lowatllmlt Sutacbull Otnatlon Frt~quency Cur~tlon Frequancy depth

LdA~ lunulllyd ay loom - - middot---middot

I

R Flt Fl

-

0 to 2 ll4f001l oocaoionaly llooded

lo luna D Nogt91lgible luiJusl - - middot- middot --

middot- -- Nono Velty brie Occsoionll -t middotmiddot shy

J

i D

D - Nogllgibla

N91lf11ble

S_mb

Odober

-- - - middot

---

I_ 0

-None

None

v bull blttel

v brief

Oltgttulootal -OccuionaJ

Pg~ParJLIIra clay lll15

I pamp-rcent slopas

Parguera ~- - middot

PbullF-Pkahaya-um tono

I middoto I

MedltJm Jar-Oec - - -I - -middotmiddot

Nonamp

middotshy- -

oulcrop-SeboNto compl(ox 40 bullo 60 percent sklpes 1

Pitahaya D very hogh Jan-Dec - - - - NoM --Umestone outcrop trfdlc Very hiQh JaHlelt Nono middotsoli moiture reglmo

SobONOO 0 ---tVery high Jal-06c - - - - No - shyPzB-Pozo Blanco day 0 iamp -middot - - -shy

I 5 peroent slopes

__ ______I Poto bliloco D Meltllum Jao-Oec - - - - No - middot- -- ~------ middot--i--middot middot--rmiddot-middot- ~

Pzc--Pozo Blanco day 5 to I

12 pottaht slopes - Pozo blanoo D Medium Jen-Oec - - - - Jllooe -middot- -- -shyPz~Pozo Blanco d ay 12 I t() 20 pcteent clcpes I I Pozo blanco 0 High Ja~Oe( - - - - 1 ~~-middot--~-middot

I shy

Water FealubullerSJn German Area Sltlv lhWestem Puerto Rico

WBter Featul9e- ampIn Gorman Anamp Southwe-ttom Puorto Rleo

shy shy

shy

shy

shyshy

shy

shy

shy

Natu RMourcea Web Soi 5ney 411Ct2012 Concttvation Sbullrvlcbull NollonJI~Soll~ Page6ots

~

Map untt symbol and 11011 nomo

Hydrologic group

Surfce nmoff

Month Water tabla

Upper limit Lcgtwor llmtt Surface ltloplh

Pondlng

Duration Frtqubullncy

fJoo

Ouratton

clna

Freqpency

EpF-El Papoyu graDy day kwTI 10(0 60 peroerl

s~oFbull

Ft Fl Fl

I I

I El papaya 0

FeA~e ctay 0 to 2 percent i I Slope$

Fe oo

HIOll

MtdliJm

J~

Sepcember

-

40-60

-I

gt60

-

-

-

-

None

I None

-

- --Nonbull

0 10 r---- iO Mtdium

Medium

()doter - --November

41gt-60 -

41gt-60 gt60

jgt~0 -

---

None

Ncne --

Hone

Hone FrA-Fralemidad day 0 lo 2

percent slopes I Ft11lemid11lt1 0 Medium Jan-Dec - - - - None -

FrB-Ffilemidad day 2 to 5 pbullrCenl slcpas I I

i Fnlemldad D Medium Jen-Oec middot------middot-- _ middot- -middot -GnA-Guano day 0 to 1 percent sJopes middot I middot----middot----middot--middot middotmiddotmiddot-Guanlca D Nogllgtblo August

-

-

-

-

-

00-15

0 _ Nona 0

Long Frequent -0

None

0 Nogllglble September - - 00middot15 Long FreqYent - Nona----D Negligible October - - 00-15 -middot- Long Frequampnt ---middot------ - - - -middot - None

middotG)IC-Guayecan clay 5 lo 12 peroeot slopes I

bull Guayacan 0 H~h -- Jan-Dec - - - - None -- -middot

Walar Feawres-San amplrman AMa Soutnwutbullrn Puono Rloo

W11tor Feature-Sao German Area SoutrrMetem Pubullrto Rtto

shy

shy

shyshy

shy

~ Natural Rbullsourcea Web Soil Survey 411012012 Conurvatlon SNkbull NlllonalCoopolta~ So~Survoy p-~middot s ol 8

--

- - - - -

--

-

I

Map unit aymbolbullnd soli Hyd~loglc Surface Month Water tabte Pondlng Flooding name grovp runoff

Upper llmlt Lowatllmlt Sutacbull Otnatlon Frt~quency Cur~tlon Frequancy depth

LdA~ lunulllyd ay loom - - middot---middot

I

R Flt Fl

-

0 to 2 ll4f001l oocaoionaly llooded

lo luna D Nogt91lgible luiJusl - - middot- middot --

middot- -- Nono Velty brie Occsoionll -t middotmiddot shy

J

i D

D - Nogllgibla

N91lf11ble

S_mb

Odober

-- - - middot

---

I_ 0

-None

None

v bull blttel

v brief

Oltgttulootal -OccuionaJ

Pg~ParJLIIra clay lll15

I pamp-rcent slopas

Parguera ~- - middot

PbullF-Pkahaya-um tono

I middoto I

MedltJm Jar-Oec - - -I - -middotmiddot

Nonamp

middotshy- -

oulcrop-SeboNto compl(ox 40 bullo 60 percent sklpes 1

Pitahaya D very hogh Jan-Dec - - - - NoM --Umestone outcrop trfdlc Very hiQh JaHlelt Nono middotsoli moiture reglmo

SobONOO 0 ---tVery high Jal-06c - - - - No - shyPzB-Pozo Blanco day 0 iamp -middot - - -shy

I 5 peroent slopes

__ ______I Poto bliloco D Meltllum Jao-Oec - - - - No - middot- -- ~------ middot--i--middot middot--rmiddot-middot- ~

Pzc--Pozo Blanco day 5 to I

12 pottaht slopes - Pozo blanoo D Medium Jen-Oec - - - - Jllooe -middot- -- -shyPz~Pozo Blanco d ay 12 I t() 20 pcteent clcpes I I Pozo blanco 0 High Ja~Oe( - - - - 1 ~~-middot--~-middot

I shy

Water FealubullerSJn German Area Sltlv lhWestem Puerto Rico

WBter Featul9e- ampIn Gorman Anamp Southwe-ttom Puorto Rleo

shy shy

shy

shy

shyshy

shy

shy

shy

Natu RMourcea Web Soi 5ney 411Ct2012 Concttvation Sbullrvlcbull NollonJI~Soll~ Page6ots

~

--

- - - - -

--

-

I

Map unit aymbolbullnd soli Hyd~loglc Surface Month Water tabte Pondlng Flooding name grovp runoff

Upper llmlt Lowatllmlt Sutacbull Otnatlon Frt~quency Cur~tlon Frequancy depth

LdA~ lunulllyd ay loom - - middot---middot

I

R Flt Fl

-

0 to 2 ll4f001l oocaoionaly llooded

lo luna D Nogt91lgible luiJusl - - middot- middot --

middot- -- Nono Velty brie Occsoionll -t middotmiddot shy

J

i D

D - Nogllgibla

N91lf11ble

S_mb

Odober

-- - - middot

---

I_ 0

-None

None

v bull blttel

v brief

Oltgttulootal -OccuionaJ

Pg~ParJLIIra clay lll15

I pamp-rcent slopas

Parguera ~- - middot

PbullF-Pkahaya-um tono

I middoto I

MedltJm Jar-Oec - - -I - -middotmiddot

Nonamp

middotshy- -

oulcrop-SeboNto compl(ox 40 bullo 60 percent sklpes 1

Pitahaya D very hogh Jan-Dec - - - - NoM --Umestone outcrop trfdlc Very hiQh JaHlelt Nono middotsoli moiture reglmo

SobONOO 0 ---tVery high Jal-06c - - - - No - shyPzB-Pozo Blanco day 0 iamp -middot - - -shy

I 5 peroent slopes

__ ______I Poto bliloco D Meltllum Jao-Oec - - - - No - middot- -- ~------ middot--i--middot middot--rmiddot-middot- ~

Pzc--Pozo Blanco day 5 to I

12 pottaht slopes - Pozo blanoo D Medium Jen-Oec - - - - Jllooe -middot- -- -shyPz~Pozo Blanco d ay 12 I t() 20 pcteent clcpes I I Pozo blanco 0 High Ja~Oe( - - - - 1 ~~-middot--~-middot

I shy

Water FealubullerSJn German Area Sltlv lhWestem Puerto Rico

WBter Featul9e- ampIn Gorman Anamp Southwe-ttom Puorto Rleo

shy shy

shy

shy

shyshy

shy

shy

shy

Natu RMourcea Web Soi 5ney 411Ct2012 Concttvation Sbullrvlcbull NollonJI~Soll~ Page6ots

~

Mep untlaymboland soll Hydrologic Surface Manttl Watbullr table Pondlng Floodingaroup runoft

Uppet (lmlt towor llmlt S-urface DuNtron Frequency Duration Frequency

sc~~~anMton cloyloam 0 I 1 1 1(1 2 pbullucant slopes I

occaolonally ftoo~ed

bull Sen anton c r- - c

-t INeiible- Augubullr

Negligibfe bullSeplember -middot

Ff

--

Ff

- ---middotmiddot---

dbullpth

Fr

- middot shy

II -middot Nane

Nofle

Brief

Briel

OltlCuional Occulont

r-- middot c Negligible October - 1-- - - - None Briel OltlCuional ----

SgCgt-S iln Gent~~Ouey complegt s to 20 perunt SIDf - --

I Sampn G8Jm31 o Hbh JafgtoOolt - - -

- -- shyN - -

OUey D Veltyhigh J~Dec - - - 1- None -SgFSan Gt mgtIIImiddotDuoy

tOmpln 20 lo 60 percent stops

Stn german D Very hijjh

Ouey 0 jVOry high -

I I r--middot--1JaOoc -jJan-Doo -

- -- -

-_ Nooe

Hone

--

Vo-VIIgtan l and I Urba land _ - -

Ja~Oec -~

- - - Nonamp

-

Wal ef Features-San Gtrm~n Area Soo1hwestt~fl1 Puett(l RICXl

Wattl Faturw San Gtnnbull n Ar9amp Southwebulltem Putrto RJco

shy

shy

shy

shyshyshy

shy

~ Natural Ruolircn Wb Soli Suoy 110120 12 Conurvatton Sorvke NatJDnat Coopefllltive Soil Survey Pbullge 1 ot 8

W81ef F ealureamp-San Gennan Area Soolhwesterll Puelll Rico

Water FtatiUIamp- San German Area Soutrrwsmm Puerto Rteo

Mep untt$Ymboland soli Hydrologlt name gro11p

Surface Moqtt runoff

Water table

Upper limit ll)wtrllmfr Surlaca dopth

Pondlng

D11raOon Froquentr

Flooding

Durauon F~quency

I R Fl R -VoA-Vayu oily day 0 to 2 prcent stcpamps occasionolly llooded

Vayas 0

I p o I 0

_ HOQIIgltllo Janualty HOQUgllgtlbull February -Nlt1jllgi~le Mrnh

Negligible lpnl

03-1 6 1JHO

D3-16 tJHO

OJ16 11J60

03-16 16-60

---

-

_HollO

middot- Ho-e

- None -- middot-

I

None-Ho- Ncne

None

I

I 0 N1jflglble May 03-1 6 16-60 - - INane Nom~ - - -middot D NegGglblo June 03-16 116-60 - - None -rmiddot ~middot~-middot 0 Negligible I July 03middot16 16-60 - None None-- middot middot L - middot 0 Negligible IAugust 03-1 6 16-SO - - None Briel Ooca~onalt---- --D Negliglblo SeptembEr 03middot1 6 16-60 - - None Briel OCCil5ioosJ

middot-middot middot-- shyI

0 Negligible ---middot-middot-10 Nogllglblbull

OctobeJ

Hgtvember

03middot16

03middot16 -- -middotmiddot-middotshy16-60

16-60

--

--

NoiIEI

None

a~ - --Occasklflar

bullbull 4_

INane__ ___ 0 Neglvible December 03middot16 16-60 - - None NoM

W-Waler I middot----middot j waoor - 1- Jan-OGG - - - -middot- middot------ -- None -

shyshyshy

shyshy

shyshy shy

Data Source Information

Soil Sutvey Area San German Area Southwestem Puerto Rico Sutvey Area Data Version 3 Dec 8 2008

-~ _ Natural Raeourcbulls WebSoiSMwy 4I C201Z ConsbullrvaUon Servlcbull National Coopl131ive Sol SUNey Pagea ota

W81ef F ealureamp-San Gennan Area Soolhwesterll Puelll Rico

Water FtatiUIamp- San German Area Soutrrwsmm Puerto Rteo

Mep untt$Ymboland soli Hydrologlt name gro11p

Surface Moqtt runoff

Water table

Upper limit ll)wtrllmfr Surlaca dopth

Pondlng

D11raOon Froquentr

Flooding

Durauon F~quency

I R Fl R -VoA-Vayu oily day 0 to 2 prcent stcpamps occasionolly llooded

Vayas 0

I p o I 0

_ HOQIIgltllo Janualty HOQUgllgtlbull February -Nlt1jllgi~le Mrnh

Negligible lpnl

03-1 6 1JHO

D3-16 tJHO

OJ16 11J60

03-16 16-60

---

-

_HollO

middot- Ho-e

- None -- middot-

I

None-Ho- Ncne

None

I

I 0 N1jflglble May 03-1 6 16-60 - - INane Nom~ - - -middot D NegGglblo June 03-16 116-60 - - None -rmiddot ~middot~-middot 0 Negligible I July 03middot16 16-60 - None None-- middot middot L - middot 0 Negligible IAugust 03-1 6 16-SO - - None Briel Ooca~onalt---- --D Negliglblo SeptembEr 03middot1 6 16-60 - - None Briel OCCil5ioosJ

middot-middot middot-- shyI

0 Negligible ---middot-middot-10 Nogllglblbull

OctobeJ

Hgtvember

03middot16

03middot16 -- -middotmiddot-middotshy16-60

16-60

--

--

NoiIEI

None

a~ - --Occasklflar

bullbull 4_

INane__ ___ 0 Neglvible December 03middot16 16-60 - - None NoM

W-Waler I middot----middot j waoor - 1- Jan-OGG - - - -middot- middot------ -- None -

shyshyshy

shyshy

shyshy shy

Data Source Information

Soil Sutvey Area San German Area Southwestem Puerto Rico Sutvey Area Data Version 3 Dec 8 2008

-~ _ Natural Raeourcbulls WebSoiSMwy 4I C201Z ConsbullrvaUon Servlcbull National Coopl131ive Sol SUNey Pagea ota