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. ' 2477 Shadywood Road �• ExceLsior,h1N 55331 � , . -
, `{952)471-1100 .• (9521471-OQ07(�ax) , . .
� ,
� . SVOBODA EC�LOGICAL RESUURCES � � '
, r . Prouiding the Sttar-per Edge in Natural Resources & Enuironmental eonsulting
�� -
.. . July 12, 2004
Darrell Pluc}cer �
�� 2640 Fox Street . �
Orono,.MN 553 i b
„ RE: SER Project Name: 2640& 2650 Fox Street �
" SER Project No: 2004-080-03
. ' . Project Location: A portion of the SE �1a of Section 4, T 117N, R 2:3�W, City of
` ', Orono, Hennepin Cauncy,Minnesota
_ Project Descripkion: Wetland Classification, Idemification,Delineation and Staking
• ��' Services
. , .
Dear Tvir. Plucker and Mr. Anderson, ' . � �
_ As requested,Svoboda Ecological Resources{SER)personnel visited the above referenced�
' property on 3une ZS and July 2,2004, to examine the site for the presence.of areas meeting -
, wetland criteria. Criteria for d�tern�ining jurisdictional wetlands are as described in the 1987 U.S. '
Army Corps of Engineers Wetlands Delineation Manual(19$7 Mant�al) as required by the
Minn�sota WetIand Conservation Act. - .
The project site consists of two properties of separate ownership existing adjacentto each other •
in an east-west configuration. Appendix D contains copies of both origirial property surveys
produced by Gronberg.and Associates, Inc. The wesiern property is under the ownership of Mr.
�Darrel Flucker of 2540 Fox Street and the property to the east is owr�ed by Mr. Keith Anderson
of 2650 Fox Street (Figure 5). The western property,Tract B, is 146,293 square feet (�.358 acres)
,. in si2e and the eastern property, Tract A, is 201;321 square feet (4.622 acres) in size. A road,
. . Tract E, running in a north-south direction separates the two properties at the southern porEion up �
� to a centrally [ocated area. The road is 93,558 sq.uare feet (2.1•48 acres) in size. At that cenCral
location are two dciveways leading to each single family horr�e thaE exists on each of the � �
properties. Both homes are located in the northern.portions of each parcei.The name of the road
that extends between the two properties is �ox Run and is privately owned and maintained in
one-third inierest by Mr. Plucker, Mr. Anderson and Mr. Kevin Wehrmann of 2b30 Fox Street
whose property is to the immediate south of Mr. Darrell Ptucker. The wetlands on Mr.
Wehrmann's property are not being delineated for this project..When one-[hird of the road area is
� incorporated into the tota! area of each property the western properry becomes i77,479 square
feet (4.074 acres) in size and the e��.titern property becomes 232,507 square feet in size {5.338
, .
2477 Shadywood Road • Excelsior,MN 55331
(952)471-1100 (Office) • (952)471-�00'1(Fas) '
acres) in size. There are severai wooded areas within both properties that lie within the northern � '
- portion of the property and surround each of the homes.The properties contain rclatively flat to I
Slightly rofling topography on the southern portions but tend to increase in elevation as the
property extends 'rn a northerly direction towards the homesteads.The project site is bordered by
, ihe Luce Line trail on the na�thern end and private properties on its eastern, western and southern
sides containing singte-family homes. The property lies within the SE �/a of Section 4,Township
` f 17N, Range 23W, City of Orono, Hennepin County, Minnesota(Figure I). •
METEiODS
National Wetland Inventory (NWn maps,Minnesota Department of Natural Resources (DNR)
Public Waters maps, Soil Survey of Hennepin County, and aerial photographs were reviewed
prior to the site visit to identify areas of concern. Areas illustrating evidence of wetland
conditions were examined in greater detail during the field survey. Vegetation, soils and
_ hydrology were examined (as outlined in the 1987 Manual) and used to charactarize wetland
types and determine wetland boundaries. Sample transects were established in a representative
wetland-to-upIand transition zone,in order to characterize the vegetation, soils, and hydrology of
� , the site.'T�he transects consist of one representative upland sample point and one representative
wetland sample point. The number of transects completed per basin depends on the size of the
basin and/or the number of wetland types associated with each basin. Other samples were taken
: at unmarked locations to provide verification of the wetland edge as needed.Tnformation
.: obtained from the sample points can be found on the field data sheets located in Appendix A.
� The wetland boundary was marked at the site by blaze-orange "wetland boundary" flagging �� �
attached to 4-faot wooden lath. The wetland boundary is considered to be the topographicaIly
highest extent of the wetlarid basin; areas below the staked houndary met the three required
wetland criteria while areas above lacked one or rnore of these criteria. SER utiiized its suh-
meter accurate GPS surveying capabilities to gather the wetland boundary location after staking
Basins 1 and 2. This reduces the possibility of loSing the boundary locatian at the time of the
• staking in the event of an unauthorized removal c�r relocation of the wetland stakes before the
,� boundary review.
Wetland ciassification followed methods described by Cowardin et al. (i979) and used in the
NWI completed by the U.S. Fish and Wildlife Service. The Circular 39 classification (Shaw and
Fredine 1956) is also given. The indicator status of plants was determined using the National List
. of Plant Species That Occur in Wetlands -Minnesota (Reed �988). Explanation of the plant
indicator categories is provided in Appendix B.
� RESULTS AND DISCUSSION
The NWI map (Excelsior Quadrangle) illustrates two wetiand basins on the subject property.The
NWI identified wetlands on the property consist of a Type (PEMCd) wetland on the western
portion of the property (Figure 2}. -
_ The Soil Survey of Hennepin County indicates five individu�! soil types on the subjeCt pro�erty
(Figure 3}. These individual soil types include: Kilkenny loam {KkB and C), Lester clay loam
(LsD2), Hamel loam (Ha), Le Sueur loam (LtB) and Palms peaty muck (Pm}. See Appendix C �
, for a description of the soil series for each of these soi! types. Of these soil types, the Hamel loam
(Ha) and the Palms peaty muck (Prrt) are classified as hydric soils (Hydric Soils of the United
States). The DNR Pub[ic Waters Map of Hennepin County illustrates no public waters on the
- . subject property (Figure 4).
SER personnel examined the subject property foc areas meeting jurisdictionat wetland criteria
� during the site visit and delineated two areas as being jurisdictional wetfand. Detailed vegetation,
soils, and hydrology data for the wetEand are provided in the data sheets of
Appendix A.
� Basin 1 is located in the in the southern portion of the western property (Figure 5). SER
! delineated the boundary of Basin 1 as a palustrine (P-) type wetland ex[�ibiting emergent (-EM-)
vegetation with a seasonally flooded(-C-) moisture regime that is ditched (-d) or a Type 3
. (PEMCd) wetland. Basin 1 is 40,404 square feet(0.928 acres) in size.
The wetland boundary was based on the transition in elevation from wetland to upland.
� Normally a vegetation dominance wauid be used to identify the boundary but a dominance of
. Reed Canary Grass (Phalaris arundinacea, FACW+) exists in the upland as well as the wetland.
SoiIs and hydrology were also used as a way to further justify the placement of the boundary at
various unmazked Iocations azound the basin as well as the marked transects where vegetation,
hydrology, and soils data was coIlected and recorded.
� SER used 23 lath to delineate the wetland boundary of Basin 1. �
Basin 2 is located in the soutl�-central partion of the eastern property(Figure 5). SER delineated
the boundary of Basin 1 as a palustrine(P-) type wetland exhibiting emergent {-EM-) vegetation
,.,, with a seasonally flooded{-C-) moisture regime that is ditched (-d) or a Type 3 (PEMCd)
wetland. Basin 2 is 10,339 sc�uare feet(0.237 acres) in size
The wetland boundary was based on the transition in elevation from wetland to upland.Normally
a vegetation dominance would be used to identify the boundary but a dominance of Reed Canary
Grass (Phalaris arundinacea,FACW+)exists in the upland as well as the wetland. Soils and
hydrology were also used as a way to further justify the placement of the boundary at various
unmarked locations azound the basin as well as the marked transects where vegetation,
hydrology, and soils data was co3lected and recorded.
SER used 171ath to delineate the wetland boundary of B'asin 2.
Photographs 1 through 4 (Photo Log) depicts Basins 1 and 2 at the time of the site visit.
CONCLUSIONS �
SER examined che subject progerty and delineated two wetland basins, which exhibited a
dominance of hydrophytic vegetation, hydric soils and wetland hydrology. Basins 1 and 2 were
classified as Type 3 (PEMCd) wetlands.
- RECOMMENDATIONS
While the wet3and boundary that SER has delineated is not official until approved by a WCA �
� approved local government unit (LGU), SER advises the property owner to refrain from any
filling, draining, or excavating, or any impact to the area SER has delineated as wetland.
Depending on thelocation of the property, buffers around the wetland may also be protected.
Any activities in the proximity of the wetland should be cleared with appropriate WCA
, regulatary agencies. Tt is also ativisable to have the wetland boundary surveyed by a licensed
land surveyor, or located with a sub-meter GPS unit. Since the lath used along the boundary can
be vandalized or inadvertently knocked over, a survey or GPS location of the lath will assure the
perrnanence of the boundary. The client should also be aware that approyed wetland boundaries
are typically valid for onIy three yeazs from the date of approval.
SER appreciates the opportunity to provide our services on your project: Please feel free to
contact me at (952)�71-1100 if you have any comments or questions regarding this report:
Sincerely,
Svoboda Ecological Resources
. c`�.�5� . .
Franklin 3. 5vobod�CWB PW
, , S
Vice-President
� DATASOUR E
C S
` Minnesota Department of Natural Resources Protected Waters Invento
ry Map, Hennepin County.
1985. �
USDA. $oil Survey of Henepin Counry. June197I. 159pp. pius appendices.
United States Fish and Wildlife Service National Wetland Inventory Map—Excelsior
Quadrangles. 194I. (Taken from May 2003 aerial,photographs).
� USGS. Digital ORhophoto Quadrangle—Hennepin County, Section 4, Township 117N, Range
23W. USGS. May, 2003.
�
LITERATURE CITED
Cowardin, L.M., V. Carter, F,C. Golet, and R.T. LaRoe. 1979. Classification of Wetlands and
Deepwater Habitats of the United States. U.S. Fish and Wildlife Service, FWS/OBS-79/31. '
- 103pp.
Eggers, Steve D. at►d Donald M. Reed. 1997. Wetland Plants und Plant Communities of
- Minnesota and Wisconsin. US Army Corps of Engineers, St.'Paul District. 263pp, unclassified.
Environmental Laboratory. 1987. 1987 U.S.Army Corps of Engineers Wetlands Delineation
" Manual. Technical Report Y-87-1, US Army Engineer Waterways Experiment Station,
� Vicksburg, Mississippi.
� National Technical Committee for Hydric Saiis. 1991. Hydric Soils of the United States.
USDA Soil Conservation Service,Washington,D.C., Misc. Publication Number 1491. 1991. �
Reed, P.B. 1988. National�,ist of Plant Species that Occur in Wetlands:Minnesota. National
� . Wetlands Inventory,U.S. Fish and Wilcllife Service, St. Petersburg,FIorida.
� Shaw, S.P., and C.G. Fredine. 1956. Wetlands of the United States. U.S:Fish and Wildlife
Service, Circular 39. 67pp.
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._. App�ndix A .
- Field Data Sheets
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I. 1.
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�. ) S�OBOD►A ECOLOCICAL R��OUn.C��
,J ��' b�G�ticuirl.s� Inve�rtory cYc Dellneutiuit • FIs'herie.r • 6�ii�llife • 1Vutatru! Ca1�►mu�iitics•
� � ' S:ic N�n,e: 2640&2fi50 Fux Street D:u�: � �
� July _. _0(74
Hus�nAArca: $;�til❑ � Sarnple Polttt ID: r
S P l-I ��F-."I'
im�nsngators: B KE3 CommunitY T�YP� �:
"Cvpe 3 (I LMCdl
� Uisturbrd Cund�tian? Ye� n�� � —
Nature o;Disturbancc:
v�,cE�r.��Tro� �
Dominants �_zoain+basal ur ae�i�t covcra�;;� hon-domin��niti
ti ecics Strawm (;tdicatarStatus S ecies
–�-- fitratum Indica�or Staius
Phufuris artu�dinacea �` 5 T FACW+ Safis exikun �{ �'�T Ot3L �
H V S T F_quiseUun urvense �' S T FA�'_
!i V S T l��ipntiens cur�eresic H V S `f
ti V S T ����W
H V S T
� HVST fI VST
I H V S T H V S T
', H VST FI VST
>50%of Dominants FAC or wetcer? �/ Yes___No %SO�o of Dominants FACI�',QBL(FAC-neutwl test) ✓yw Nu N!A
- Notes: No vine or tree species observed at this sample location
SOILS
County Soi!Survey Map Unit: palms peaty muck ✓ Soi1 Seri�;s on Nacio❑ai Etydric Soi!Lisc
?.ru mapped as dcpressioa or wet spot on Soii Survey.
Field Ohservations
- Hydric soi!assumed because plantz are OF3L and FACW anc'.wetland boundary is abrupt
�/ Minzral Soil Organic Suil
F-iorizon/Deoth Matrix Color Texture F;,atures
0-16" IOYR 2/1 t�tucky mineral
16-20" I Ol'R 2/I Sandv cla��loam
Iiydric Soil Present? �/ yu No Uudaterm�nui
Notes:
Primary indicators(P) 3econdary indicators(S�
HYllI20LOGY
Depth of sampling: 2Q )nches Oxidizui 1Lout Channcls ln Upper 12 inches(S)
Inunda[ed,Depth of Water.(I') llrainage Pauems�n Wetlnuds(Y)
�/ F�rce water in borenule,Depth irom Surfacc: ���� �L`atar-stained li;;syc;s(Sj
Warer hiarks,L•Icvation:(P) �/ Local Soil Survey D'ata(S)
Drift Lines or Sedimem llepusits(P) �/ FAC-Noutrul"I�c�t(S)
Hydrology Critecion btet? �/ Y�s No
Othcr Observations:
WETLANI)DE'I'E'iZMINA`I'ION
[s the Samplc Point in Wedand'? Yes �/ No Undete-nnintd D!s:auce 2�o�n U;:lincated Edgc: (j �t. hr�
Noces: Wetland edge based on topographic line.
`,� � .
ii`
� i . svoBor�A EcoLo��ca� r���or��:�c ��
,� ; .
6�t���lancl.s Invcnturi� c� f�eliiicution • Fis•ficri�.5� • Gf�ilcll�e • Nutln-u! Commtrr�itles
�� >i�c Namc: ?b-30 5't 2b�U F��iX Stredt Datc: Ill1 2,200�3
IJ� l3asin�Arca: _ Y
E3asin l SumplePointlD: SY 1-I UY
ln��cstigaWrs: (jKB Commun�ty Typr:
UPI.ANI�
Uistunc�;d Cundiiiun° Yes No �
Naturc uf Uisturbance:
�'EGET_ITION
Dominants t>20°o+basal or aarial coverage) �
?�on-clominantv
� 5 ecies Str�turn Indicator Statu� S raes
—L--- titraturn Indicatur�tatus
Yhuluris'urturdinucep �V S T FACW+ 13 V 5 T
}i VST �
FI V ST
EI VST H VST
}I VST H VST
HVST ff VST
II V S T H V S T
H VST H VS 'I'
i
>50°/of Dominams FAC or wcaer? �/ �'�—h� :50°io of Duminan�s FACW,OpL(FAC-neutra!test) ✓Yes No N!q
No�cs: No vine,shrub or tree species observed at this sample location
SOILS
COUOtV$Otl SLLI'vey jYiap jJnit: j,g$Ueuf lOam Soil 5eries is on Nationat EIydric Soi!List
Area mappc:d as depression ur wec spot on Suil Sun•cy
Field nhservacions
E{ydric soil assumcd bccause pianU arc OBL and FACW and welland boundary is abnipt
�/ Minc:ral Soil Organic Soi!
Horizon/Denth Matrix Color Texture Features
0-15" lOYR 2/i Sandv loam
15-20" lOYR 2/I SaTidv clnv loam
20-27" lOYR 211 Sandv ciav
Hydric Soi!E'rescnt? Ycs �I No Undeterminc:ci
Notcs:
Primary indicators(P) Secondary indicutors(S)
HYDROLOGY
Depth of sunplin�;: �� lnches Oxidia.ed Raot Channels in Upper 12 inciies(S)
Inundated,Depth of Wa[et:(P) Drainage Patterns in tk'edands(P)
�/ Fcee wate:in 6orctiole,Drpth from Surfacc: ���� Water-st�incd Iwvrs(Sj
Waier MarkS,Eleva[ion:(P) Local Soil Survcy Data;Sl
Drift Linc:s or Scdimcnt Deposics(P) �/ F:�C-N�utral"l�est(S}
Fiydrology Criteriun Mct'? Yes �/ No
Ochcr Observations:
� «'�:TLAIVll D�:"CERI��IINA"fION
Is thr Sa�riple Yoint in Wedand'? Yes Nu �/ Undctemiiiied Distance:Ftu�n L)c lircate d Edbc � �t. N/;�.
Nu�cs: Wetland edge based on tapographic line.
M �' J
F !�
� , svaBo�A Eco�,oGICAL R�sa��cr�
� ' Wetlunds Inventon� c� Delineution • Fi.sheries • GYildlije • .'��uttn-ul Communities
�� Sn�Nun;c: 2640� ?6JQ Fux Street Duin: 7ul �2,�00-1
[3asinlArca: --�---
� Basita I S�mpl�P�int tD: SP I-2\VI�T
Investiga�ors: BIiR Communit T e: � ;
Y m "I'vnc 3�t 1_.MCdI
Diswrbcd Condi�ion'? Yns IJo � —
Nuturc uf Dismrbancc: �
v�c�z'ATI(3N
�ominSnts (_2U°.o t bnsal or acrial corcr�g�j
t�c�n-dominant,
`�—'�C1zS S:ratum indicator Status S ��c;ics S[rawtn Indieatur St.�tu,
Phalaris urtu�dinaceu E I V S T FACW+ Acer nee�indo f 3 V S �
Ei V S T � r�C��-
lmratieas cunensis �� V S T �;����
H VST kIVST
k{ VST H V � �.
Fi VST H VST
FlVST FiVST
HVST HV51'
>50%of Dominants FAC or wettcr'? �/ yes_No >50%of Dominants FACW,OBL(FAGneutral test) ✓yes Nu NiA
Noees: No vine nr shrub species observed at this satnple location
�' SOILS
County Soil Survey Map Unit: palms peaty muck ✓ Soil Series is un National Hydric Soit List
Arca mapped as d�prt;ssion or wc[spoc un Soil Survey
Field nhservations
Eiydric soil assumu!because planu are UBL and F.4CV�,�and wetland boundary is abrupt
�/ Mineral Soil Organic Soil
Horizon/Deoth Matrix Color Texture Features
0-10" lOYR 2/1 Sandy mucky mineral
]0-16" lOYR 2/1 Sandv clay loam
16-14" lOYR 2I1 Fine loamy sand
--_`
FI}'I�ItC SOII PTC5:I7[.l �/ Yc;s No Undetermin�l
Notes:
Primtuy iadicators(P} Secondary indica�ors(S)
HYDROI:OGY
Ucpth of santpling: I� lnches Uxidizcxi koot Chanticls in Upper I Z inches(S)
lnundated,Depth of Water:(P) llrainage Yattems in Wetlands(P)
�/ Frc:e water in borehole,I)epth from Surfacc: �2^ Water-staincd leaves(S)
_ Water Marks,Elevanon:(P) ✓ I.ocal Soi!Survc;y Daia l S)
_ Dr,ft Lines or Scdimen[Deposits(Pj � FAC-Neutial"I'est(S)
Hydrology Criterion Met? �/ Yes No '
Othec Observations:
WETLAND I)1:TERNI�NA'I'IO�t
V thn Sample Point in Wetland? Yes �/ No Undctcnnined Dista�ic�irom Delincated Edge: � ft. Nl:�
N���S: Wettand edge b�.sed on topographic line.
�i��,
��,�,� ; �voson� Eco�oG�cAL ��so��c�c�
� ��� ���'etluncl.�� Inverttorv cti Detineation • Fisheries • WitclliJi; • Nutiu�u! C��nu��unities
� Siic Numc: '?6qp�?650 Eox Street U�ie: Julv?, 200d
! Hasinl,�rca: $,1SIn 1 Sample Point ID: � �
SE i-.,UP
Investigators �KB �:umn�un�iy'C}�u.
UPLANU
Disturbcd Condiuon? Ycs ,y� �
Nature o1'Distur6ance:
- VEGETAI'ION I
DominantS (._20°/+basal or acrial covcragn) :'�'on-dornin�ntti
S ecies Strattim Indicatur Status S �cic�
$tr�tum indicator Statu�
Phularisariu�drnacea QV S T FACI��+ Acerneeundu H V S '� f;q�W_
H V S T Jinpntiens caPensis 1�( V S T
fi V S T �a`CW
Circium arvense E{ V S 'I F��.jJ
H VST E{ V ST
' H V S T Fi V S T
H VST i[ vST.
II VST il VST
>50%of Dominants FAC or wetter? �I Yrs__No >Sll°/of Uominants FACW,C)BL{FAGneutra!test) ✓Yes No N;A
Noees: No vine or shrub species observed at this sample location � '
SOILS
County Soil Survey Map Unit: palms peaty muck ✓ Soil Serics is on National Hydric Soit List
Are:���iappcd as d�pression ur wet spot on Soil Survey
Field Observations
_ Hydric soii assumul becawe planLs arc OBL and FACW and wetland boundary is a6re:pc
�/ Minerat Soil Organic 5uil �
Horizonlncnth Matrix Color Texture Feattires
0-15" lOYR 2/1 5andv clav loam
15-18" IOYR 2/1 clay Ioam
llydric Soil Yresenc'? Yes �/ Nu Undotermined
Notes:
Pc?mary indica[ors(P) Secondary indica[ors(S)
HYDROLOGY
Depth of san�p}ing: 1 g Inches Oxidize<I Ruot Channcls in Upper 12 inchcs(S}
Inundatcd,Dc.pth of Wa�er.(Pj llrainagr Yaucrus iii W'ctl�nds(P)
� Frae water in borehole,Depth from Surface: 1 5" Water-s[ained lwvcs{S)
�Vater tvfarks,Elevation:(P) �/ Loca{Soil Survey D'at3(S)
Urift Lincs or Scdimc-�:D��osits(P) �/ FAC-Neutral Tcst(S)
Hydrofogy Cciterion hlet? �/ Ycs No
�)If1Cf(�bSCCVHIlUf15:
V4'ETLANll llE"I'ERMINATION
Is the Sample Point in Wetland? Ycs Vo �/ Undetermined llisteucc frum D�linc�ted Edgu: 5 ft. NiA
No�es: Wetland edge based on topographic line.
� �' i
� ; SVt�►BODA ECOL(�G�CAL RE�OLTRC�� �
Wetluncls Inv�nrory cY� Delineution • !�'i,sherles • Wlltllife • ,ti'uturul Cun:nriuiities �
� tiiic H�mc: 2640&2650 f�ox S[reet Uu��: lulv"'. 20O-1
�� � . , -
�� (iasml,Area: (3.11in 2 Sampl�I omt lI). �f��-1 �rVFT
lnveshgators: �K� CommunityTypc: �
_Cvpe 3 tPEh4Cd}
Disturbad Cundiuon'! Yes h� � —
Nacure ol'Disturbance:
� vEc�:T.a��ro:v
��C)n7ift8qt5 (_?040+basal ot acrial cuvcrage) h�Otl-(j011llfidlll5
5,ecirs Stramm Indicator Status S�ecies
�--- �trntum Indic.uur St�tus
Phalurisariu�dinncen Pi V S T F'ACW+ ff V S T
H VST t[ VS "f
H VST 3i VST
� 1i VST II VST
H VST fi VST
H VST ti V ST
H V S T H V S T
>5(l%of Uominants FAC or we[ter? �/ Yes`No >SUib of Dominana FACW,OHL{EAGncutral twt) ✓Yes No N/A
Noies: No vine,shrub or tree species observed at this s�mple location
SOILS
County Soil Survey A'Iap Unit: Hamel Loam ✓ Soif Serirs is on National Hydric Soil List
Arca mapped as depression or wet spot un Soil Survey
Fielci nbservatinns
FIydric soil assumed because planrs arc Ok3L and FACW and wetland houndary is ahrupt
�/ Mincral Soil Organic Soil
HorizonlDenth Matrix Color "rexture Feati�res
0-i8" lOYR 2/i Sandv mucky mineral
Hydric Soil Present? �,/ Yes No Undetern�inc�
Notes:
Yrimary indicators(Y) Sccundary indicators(5)
HYllROLOGY
Depth of saznpling: 1$ Inclies Oxidizetl Ruot Channels in Upper 12 incti�s(S j
Uwndated,llepth of Water.(Pj i�rainagn Yatterns in Wetlands(P)
�/ Frcc wator in borchole,Depth from Surface: 6" Water-stained lenvq(S)
_ W'ater Marks,Elevation:(P) �/ Lu:a!Suil Survey Data(S)
_ Drift Lines or Sediment Ucposits(P) �/ E�1C-Neutral Tcs�(S)
Fiydrolagy Critcriun bicC? �/ Yes Nu
Other Observa[ions
� WE i'LAND llETEI21YiINAT10N
!s the Sample Point in 4Vetlund7 Yes ✓ No Ucde�umincd Dis�dncc t"rom DelineateS Edee: 6 ft. N/A
Noies: Wetland edge based on topographic line.
���"�,
��I , SVOBODA ECOL(J�ICAL 12ESOURCE�
�,� ' t�'etluncl.s• Inventoiy �S'c Uellneution • /��isheri�s • GYlldlije • Ncttttra! C��ntnt�t�iities
Sit�Nam�: 2640&26�0 Fox S�rcet ��t�: J��•?,2(J04
�� � E3asin\Area — —
( Bas�n 2 Sarople Puin�IU. Sp�-1 UP
Investigators: BKF3 C`umnwnhy1'ype: (fPLANI)
DisWrbed Condition? Yes No �/
Nature oi'Disturbance:
_ v�;cc�r:�Tior�
� nOT171I18f1IS (>20°6+basal or aerial c�veragej f`IOIi-(jOit1j11aiiCS
�' � t�i�� Stratum Indic�tor Siatus S c,�cies Stratum Indicatcar Status
Phniaris aruncliizu�ra ll ' S T j=AC�Y+ li V S 'C
Eib' ST ii VS1'
!{ VST }1 VST'
H VST H VS7'
H VST k�i VS "I'
HVS 'C ti VJ 'C
f3 V ST H VST
>50%of Dominants E�AC or wetter? �/ Ycx_No »U%of Dominants FAC11',013L(FAGneutral test� ✓yes No N�A
Nuc�:.,: No vine,shrub or tree species observed at this sample location
SOILS
COunty Snil Snrvey 11-Iap Unit: Le Sueur loam Suil Snries is on National}{ydric Soil List
Arw map�d;ic depression or wet spot an Suil Survey
Field Ohserva6ons
Flydric soil assumeci hecaus�plan�s are OBL and FACW and wetland 6oundary is abrupt
�/ Minrra!Soil Organic Soil
Narizon/Denth Matrix Color Texture Features
0-18" 10�'R?/1 Sandy clay loam
18-24" lOYR 2/1 Sandv c.lav
Iiydric Soil Present? Ycs �/ No Undctermineti
Notes:
Primary indicators(P) Secondar}�indicators(S} H'�'DROLOGY
Depth ofsampling: ?4 Inches OXI(IIZC(�RUU[C�tl'SRIIGIS 111 UElOCI l2 mchas(5!
Inundated,Depth of Water:(P) Drainagc Ya[�eats in Wellunds tY)
�/ Free water in borohole,Depth[ron;Surtace: �2�� �ti'atcr-staineS lcavra{S)
�,'ater Matks,Elcvatiun:(P) Luc�l Suil Survcy llata(S)
Dnfr Lines or Sediment Drposits{Y) �/ FAC-neutrul Test(D;
Hyclrulogy Criterion Met'? Ycs �/ No
Other Observatiuns:
«'LTLAiVll llETER!Yti?�A"I'lON
ls the Sample Point in Wc;dand'? Yes _ hu �,/ lind�tcnnined Uiscance trurn Detiucated Edgc: �O ft. N,'A
Noc�s: Wetland edge based on topographic line.
' I
i
�
Appendix B
Plant Indicator Categories
; �
, �
,
.�
�
,
INDICATOR CATEGORIES*
Obligate Wetland (OBL)—Occur almost always (estirnated probability >99%) under natura!
conditions in wetlands.
Facultative Wetland (FACW)—Usually occur in wetlands (estimated probability 67%-•99%},
but occasionaEly found in non-wetlands.
Facultative {FAC)—Equally likely ta occur in wetlands or non-wetlands (estimated probabitity �
: 34%- 66%)•
_ �
Facultative Upland (FACU)—Usually occur in non-wetlands (estimated probability 67%- �
99%), but occasionally found in wetlands(estimated probability I%- 33%).
Obligate Upland (UPL)—Occur in wetlands in another region, but occur almost always
(estimated probability >99%) under natural conditions in non-wetlands in the region specified. If
. a species does not occur in wetlands in any region, it is not on the National List.
, ;
� *Reed,P.B. I988. National Gst of plant species that occur in wetlands:Minnesota I3utional Wednnds lnventory,U.S.Fish and Wildlife Service,
St.PeEersburg,Florida
�
. . A endix
. I�p �
, Soil Series Descriptions
; . .
. �
I � .
PALMS SERIES �
The Palms scries consist of very deep,very poorly drained soils formed in herbaceous organic material l6 i
to 5( inches thick and the underlying loamy deposits in closed depressions on moraines, lake plains, till
plains,outwash plains,and hitlside seep areas,and on backswamps of tlood plains. Permeability is
moderateiy slow to moder�tely rapid in the organic material,and moderate or moderately slow in the loamy
material.Slope ranges from 0 to 6 percent.Mean annual precipitation is Ahout 35 inches,and mean annual
tamperature is about 50 degrees F.
TAXON4MIC CLASS: Loamy, mixed, euic, mesic Terric HapIosaprists ;
TYPICAL PEDON: Palms muck, on 1 percent slope under marsh vegetation at an
elevation of G48 feet. (Colors are for moist soii uniess otherwise stated.)
Oa1--0 to 14 inches; black (lOYR 2/1) broken face and i-ubbed muck(sapric materialj;
ahout S percent fiber, less than 5 percent rubbed; moderate medium granular structure;
slightiy sticky; about 20 to 25 percent mineral material; slightly acid (pH 6.5 in water);
abrupt smooth boundary.
Oa2--14 to 28 inches; black (lOYR 2/1)broken face and rubbed muck(sapric r�aterial);
abaut S percent fiber, less than 5 percent rubbed; massive parting to weak coarse
� subanguiar blocky structure; slightly sticky; 10 to 20 percent mineral material; strongly
acid(pH 5.5 in water); clear smooth boundary.
. Oa3--28 to 35 inches; black (N 2.5/0)rubbed muck(sapric material); about 5 percent
fiber, less than 5 percent rubbed; massive; slightly sticky; 10 to 20 percent mineral
material; moderately acid (pH 6.0 in water}; abrapt smooth boundary.(Combined
- thickness of the Oa horizon�is lb to 51 inches.)
Cg-'-35 to 80 inches; gray (lOYR 5/1) elay loam; massive; friable; common medium
� distinct dark yellowish brown (lOYR 4/4) masses of iron oxide accumulation in the
matrix; neutrai (pH 6.8 in water) in upper part; slightly effervescent, moderately alkaline
in lower part.
,.. TYPE LOCATION: Gratiot County, Michigan; north of the flood plain of the Maple �
River and about 200 feet south of the upland; 1,420 feet south and 820 feet west of the � .
northeast corner af sec. 27,T. 9 N., R. 2 W.; U.S.G.S. Pompeli topographic quadrangie;
Iat. 43 degrees 8 minutes 3i.3 seconds N. and long. 84 degrees 31 minutes 34.7 seconds
W.,NAD 27; UTM Zone 16,701165 easting and 477955� northing,NAD 83.
RANGE IN CHARA,CTERISTICS: The depth to the loamy C hori�on ranges from 16
to 51 inches. The organic material is derived primarily from herbaceovs plants,but some
layers contain as much as 15 peccent woody materiai. Reaction of the organic material �
ranges from strongly acid to slightly alkaline. Some organic Iayers contain carbonates.
The.surface tier has hue of lOYR to SYR, or is neutral; value of 2, 2.5, or 3, and chroma
� of 0 to 2. It is dominantly sapric material; �owever, some pedons have hemic material.
\ The subsurface and bottom tiers have hue of lOYR to SYR, or are neutrai; value of 2 to 4,
and chroma of 4 to 3. Thin layers, iess than 10 inches thick, of hemic material are in
� same pedons. Thin fayers, less than 5 inches thick, oti fibric muterial are in some pedons.
Some pedons have.a thin layer of sedimentary peat above the C horizon. Some pedons
have a thin A horizon above the C horizon.
The C or Cg horizon has hue of I OYR to SY, SGY, or is neutral; value of 3 to 7, �nd
chroma of 0 to 4. It is loamy very fine sand, sandy loam, fine sandy toam, loam, sitt loam, ,
silty clay loam, clay loarn, or sandy clay loam,or the gravelly analogues af thase '
textures. The upper 12 inches of this horizon averages_between 10 and 35 percent clay.
Some pedons contain thin strata of fine sand, loamy sand, or silt. Reaction ranges.from
moderately acid to moderately alkaline. Rock fragment content ranges from 0 to 25
percent and fragments range in size frorrt gravel to stones. Some pedons contain
carbonates. Sandy substratum, gravelly substratum, and overwash phases are recognized. �
I
COMPETING SERIES: These aze the Klossner, Linwood, Medo, Natchau� �T��
Philbon, and Shalcar secies. Similar soils aee the Adrian, Carlisle; Cathro, Dawson,
Edwards, Hou�hton, Markev,Tawas, and Willette series. Klossner soils have A horizons
directly below the organic matter. Linwood soils formed mainly in woody fibers. Medo
soils have less than 14 percent clay in the lower 1/3 of the series control section.
Natchaug soils are in areas where the mean annual precipitation is greater than 43 inches.
Philbon soils have fibric and hemic material in the upper 12 inches. Shalcar soils have a
difference between mean anaual summer and mean annuai winter temperatures that is
less'than 26 degrees F. Adrian, Dawson,Markey, and Tawas soils have sandy mineral
layers at depths of 16 to S l inches. Tn addition, the Dawson,Markey, and Tawas soils
` have frigid soil temperatures. Caziisle and Houghton soils formed in organic depasiEs
more than 51 inches thick. Cathro soils have frigid soil temperatures_ Edwards soils are
underlain by marl at depths of 16 to 51 inches. Wiliette soils have mineral layers that
� average more than 35 percent clay at depths of 16 to 51 inches. '
� �
GEOGRAPHIC SETTING: Palms soils formed herbaceous organic material and the
underlying loamy deposits and are in closed depressions on Iake plains, tili plains,
outwash plains, moraines, and hillside seep areas, and on backswamps of flood plains.
Slope graclients range fram 0 to b percent. The soils on nearby uplands are generally �
loamy. Mean annual temperature ranges from.48 to 53 degrees F., mean annual �
preczpitation ranges from about 30 to 43 inches,frost-free period ranges from 120 to 180'
days, and elevation ranges from S80 to 1,530 feet above sea level.
GEOGRAPffiCALLY AS30CIATED SOILS: The Hou hton soiIs are the znost
common associate and are on similar landform positions. Poorly drained or very poorly �
drained loamy mineral soils are at the edges of the bogs and are adjacent to Palms,soils.
DRA,INAGE AND PERMEAgII,,ITy; Very poorly drained.The potential runoff for
surface r�anoff is negligible. Permeability is moderately slow to moderately rapid in the '
. organic material, and moderate or moderateIy s�ow in the loamy material. The depth to �
the top of an apparent seasonal high water table ranges from 1 foot above the�surface to 1
footbelow the surface from Novemher to May in normal years.
�
I
� �
_ �- LESTER SERIES
'Thc Lester s�ries consists of very deep, well drained soils that formed in calcareous loamy glacis!till on tilf
, plains and moraines.These soils have moderate permeability.Their slopes range from S to 70 percent.
Mean annual precipitation is about 28 inches,Mean Annual temperature is about 47 degrees F.
TAXONOMIC CLASS: Fine-loamy, mixed, superactive, mesic Mollic Hapludalfs
TYPICAL PEDON: Lester loam with a convex slope of about 9 percent on a ground
moraine in a culEivated field. (Colors are for moist soil nnless otherwise noted.)
Ap--O to 7 inches; very dark grayish brown (lOYR 3/2} loam, grayish brown (lOYR 5/2)
dry; moderate fine subangular blocky structure; friable; many fine roots; about 3 percenE
_ gravel; slightly acid; abrupt smooeh boundary. (6 to 10 inches thick)
Bt1--7 to 21 inches; brown (lOYR 4/3} clay loam; moderate medium subangnlar blocky
structure; firm; many very fine roots; common very dark grayish brown (lOYR 3/2}clay
films on faces of peds and few very dark gray(1QYR 3/1)organic coats on faces of peds;
abou[2 percent gravel; slightly acid; clear smooth boundary.
;
, Bt2--21 to 38 inches; dark yellowish brown (lOYR 4/4) clay loam; moderate medium
subangular blocky structure; friable;common�ne roo�s; common dazk grayish brown
(lOYR 4/2)clay films on faces of peds and few very dazk brown (lOYR 2/2) organic
coats on faces of peds; abo�t 3 percent gravel; slightly acid; gradual smooth boundary.
(Comhined Bt horizon is 10 to 44 inches.)
BkZ--38 to 50 inches; yellowish brown (1QYR 5/4) loam; weak tnedittm subangular
blocky structure; friable; few fine roots; common very pale brow� (1(}YR 8/2} carbonate
threads; about 2 percent gravel; violently effezvescent; siightly alkaline; clear wavy '
. bou'ndary. .
" Bk2--50 to 60 inches; yellowish brown (l0YR�5/4) loam; weak medium subangular
blocky structure; friable; common fine distinet yellowish brown (IOYR 5/6)relict Fe
concentrations; common very paie brown (1QYR 8/2) carbonate threads; about 2 percent
y�` grayel; violentIy effervescent; slightly alkaline; clear wavy houndary.r
: C--60 to 80 inches; yellowish brown (1aI'R 5/4} loam; ; massive; fnable; common
medium dzstinct yellowish brown (lOYR 5/6) relict Fe concentrations and few fine
- distinct iight hrownish gray (lOYR 6/2}relict Fe depletions; about l.percent gravel;
strongly effervescent; siightly alkaline.
_ TYPE LOCATION: Wright County, Minnesota; about 3 miles west of Otsego, 1460
feet south and 200 feet west of the northeast corner of Sec. 15,T.121 N., R24 W.; USGS
Big,Lake quadrartgle; lat. 45 degrees 17 minutes 29 seconds N.; long. 93 degrees 41
_ minutes 3 seconds W., NAD27
RANGE IN CHARA,CTERISTTCS: Depth to free carbonates ranges from 20 to 54
inches. Rock fragments of mixed lithology comprise 1 to 8 percent of the voluxne of the
control section.
'; The A or Ap horizons have hue of lOYR, value of 2 or 3, and chroma of I or 2. The E
. horizon where present, has value of 3 to 5, and chroma of 1 to 3. The A and E horizons
are loam or clay loam, but sandy loam, fine sandy loam, or sil[ loam is within the range.
They range from moderately acid to neutraf.
The Bt horizon has hue of IOYR or 2.SY, value of 4 or 5, and chroma of 3 or 4. It is clay
loam or loam and has 24 to 35 percent clay and 30 to 45 percent sand. The B/A clay
, ratios range from 1.2 to 1.4. It is strongly acid to slightly acid in the upper part and
moderateky acid to neutral in the [ower part. A Bw horizon is sometimes present below
the Bt.
� The Bk horizon has hue of lOYR or 2.SYR, value of 4 or 5, and chroma of 3 to 6.The Bk
. horizon is loam or clay loatn. It is slightly alkaline or moderately alkaline. Relict
redoximorphic features are present in some pedons. �
� The C horizon has hue of 2.SY oz lOYR, value of 4 to 6, and chroma of 3 to 6. It is loam
or clay loam. It is slightly alkaline or moderately alkaline. Relict redoximorphic featares
are present in some pedons. �
COMPETING SERIES: These are the Angus,Ar�,vle, Baltimore, Bassett, BIoT omin�,
Caleb, Dowa iac, Danbrid�e, Gara, Koronis,Lauramie, Lon lois, L dick, Mohawk,
. Neda, Newcomer, Oneco;Orwood,Racine,Razort, Sehbo,TaoDi,Waucoma, and
Winneshiek soiis in the same family. Angus and Sebbo soil have saturation in the lower
' third of the series eontrol section. Argyle,Baltimore, and Oneco soils have B horizons
, . � with 7.SYR or redder hue. Bassett soils are very strongly acid to moderately acid in the
upper part of the Bt horizon.Blooming and Racine soils have 15 to 35 percent sand in the
' upper part of the particle-size control sectian. Caleb soils have some subhorizons that
�. have more than 45 percent in the lower part of the control section. Dowagiac and Koronis �
, soils have less than 24 percent clay in the lower one third of the particle-size control
section. Dunbridge,Waucoma,Newcomer and Winneshiek soils have soIa terminated by
bedrock at depths abdve 60 inches.Gara soils average less than 2 percent rock fragments
in the control section. Longlois, Lydic, and Neda soils have more than 8 percent rock
€ragments in some subhorizon of the control section. Lauramie soils have rnare than 45
percent sand in some subhorizon in the middle part of the control seetion. Mohawk soils
have a higher content of silt and have dark color�s in the B horizon which apparently aze
inherited from dark shale. Orwood soils have no rock fragments in the particle-size
control section. Razort soils have less than 30 percent sand in the control section.
� GEOGRAPHIC SETTING:These soils have convex siopes on moraines and till plains.
Slope gradients range from 5 to 70 percent.They formed in calcareous, loamy glacial tiIl
of late Wisconsinan Age.Mean annual temperature ranges from 45 degrees Eo 52 degxees
F. Nlean annuat precipitation ranges from 25 to 33 inches. Frost free days range from 125
to 1 b5. EIevations range from 700 to 1 b00 feet.
GEOGRAPHICALLY ASSOCIATED SOILS: These include the Cordova, Dundas,
Glencoe, Hamel, Houghton, Klossner, Le Sueur,Muske�o, and Nessel soils. Poorly
, drained Cordova and somewhat poorly and poorly drained Dundas soils are on flats and
upper drainageways with a high seasonal water table. Very poorly drained Glencoe,
, Houghton, Klossner, and Muskego soils are mostly in depressions. Poorly drained Hamel I
_ ' soils are on foot and toe slopes. Moderately welt drained Le Sueur and Nessel soils are on
slightiy elevated flats and gently convex slopes.
_ DRAINAGE AND PERMEA.SILITY: Well drained. Pecmeability is moderate. Runoff
is medium to high.
� i
USE AND VEGETATION: Mostly cropped to corn and soybeans. Some is in pasture I
and forest. Native vegetation is savanna. �
DISTRIBUTION AND EXTENT: South-central and east-centraf Minnesota and
' northeastern Iowa. Extensive.
� � MLRA OFFICE RESPONSIBLE: St. Paul, Minnesota
SERIES ESTABLISHED: Dakota County,Minnesota, 1945.
REMARKS: Diagnostic horizons and featured recognized in this pedon are: mollic
subgroup -the zone from the surface to 7 inches (Ap horizon); argillic horizon- the zone
from 7 to 38 inches (Bt horizons). Type location moved from Waseca County, Mn. to
Wright County, Mn., 11/96 to better exempIify the series concept within the MLRA.
Slopes of 1 to 5 percent that were previously correlated as Lester may be included with
the Angus series in the future. •
� . :
�
. • �
. ,
. , -
� .
,
_ ' LE SUEUR SERIES
The Le Sueur scrics consists of very deep,somawhac�oorly drained soils that formed in calcareous loamy
, glacial till on moraines.These soils have moderate permeubility.Thcir slopes range From i to 3 percent.
Mean annual prccipitation is about 29 inches.Mean annual air temperature is abou[47 Jegrees F.
TAXONOMIC CLASS: Fine-ioamy, mixed, superactive, mesic Aquic Argiudolls
TYPICAL PEDON: Le Sueur clay loarr} with a 2 percent plane slope on glacial till plain
in a pastured woodlot. (Colors are for moist.soil unless otherwise noted.)
Ag--O to i2 inches; black{lOYR 2/1} clay loam, dark grayish brown (lOYR 4/2) dry;
moderate mediurt�.granular blocky s[ructure parting to moderate fine subanguiar; friable;
about 2 percent gravel; slightly acid; abrupt smooth boundary. (6 to 22 inches theck)
AB--12 to 17 inches; very dark gray (lOYR 3/1) and about 25 percent dark yellowish �
, brown (lOYR 4/4} clay loam, grayish brown (lOYR S/2}dry; moderate fine subangular
blocky structure; friable; about 2 percent gravei; slightly acid; clear smooth boundary. (Q
to 8 inches thick)
� . Bt1--17 to 24 inches; olive brown (2.SY 4/3) clay loam; moderate medium prismatic
structure parting to strong fine subangular blocky; friable; common dark brown {lOYR
3/3) cIay films on faces of peds; about 2 percent gravei; few fine faint dark grayish brown
�,
(2.5Y 4/2)Fe depletions; slightly acid; clear smooth boundary.
Bt2--24 to 37 inches; olive brown{2.5Y 4/3}clay loam; weak medium prismatic
structure parting to moderate�ne subangular blocky; friable; common very dark grayish
brown (2.SY 3/2)clay fiims on faces of peds and in pores; about 4 percent gravel; few
fine faint grayish brown (2.SY S/2)Fe depletions and few fine prozninent dark yellowish
brown (IOYR 4/6)Fe concentrations;neutral; abrupt smooth boundary. (Combined
thickness of the Bt hor'izon is 16 to 4S inches.} �
� Bk--37 to 46 inches; light olive brown (2.5Y 5/4}loam; weak medium suhangular blocky
structure; friable; common light gray pale brown (2.5Y 7/2) soft masses of carboante
'-' thraughout and carbonate threads; about S percent gravel; common medium distinct
•grayish brown (2.SY 5/2)Fe depletions and common medium distinct light olive brown
(2.SY S/6} Fe concentrations; strongly effervescent; slightly alkaiine; ciear smooth �
boundary.
C--46 ta 80 inches; grayish brown (2.SY 5/2) Ioam; weak medium subangular blocky
• structure parting to massive; friable; common light gray pale brown {2.SY 7/2) soft
masses of carbonate throughout and carbonate threads; about 5 percent gravel; many
common medium promine�t dark yellowish brown (lOYR 4/4) and dark yellowish brown
(lOYR 4/6) Fe concentrations; strongly effervescent; slightly alkaIine.
TYPE LOCATION: Waseca County,Minnesota; abouc 9 miles south of Waseca; 2000
- feet south and 1950 feet sou[t� of northwest corner of sec. 26,T. 108 N., R. 22 W.; USGS �
,
Morrisontown quadr�ngle; lat. 4-� degrees 7 minutes S7 seconds N. and long. 93 degrees
_ 26 minutes 45 seconds W., NAD27.
RANGE I1�1 CHARACTERISTICS: Depth to free carbonates ranges From 22 to 55
_ inches. The thickness of the mollic epipedon ranges frorn 10 to l8 inches. Rock fragment
content is l to 8 percent by volume throughout and is of rr�ixed lithology. . �
The A horizon has hue of lOYR, vaIue of 2 or 3, and chroma of I or 2. The A hocizon is
cfay 1oam, loam, silt loam, or siiry ctay Ioam. It has 20 to 3p percent clay. It is moderately
acid to neutrai. An E horizon as much as 3 inches thick is in some pedons.
The AB horizan has characteristics similar to the A and the Bt. �
� � The upper part of the Bt horizon has hue of lOYR or 2.SY, value of 3 to �, and chroma of
- 2 or 3. 'The lower part of the Bt horizon has a f�ue of 2.5Y, value of 4 or 5, and chroma of
2 to 4. The Bt horizon is mostly clay loam or loam. The argillic horizon averages bet4veen
24 and 35 percent ciay and from 15 to 40 percent fine sand or coarser. The Bt horizon is
strongly acid to slightly acid in the upper part and strongly acid to neutral in the lower
part. The hulk�density ranges from 1.3Q to 1.45 gm/cc.
Some pedans have a BC or Bk horizon.
The C horizon has hue of 2.SY or SY, val.ue of 4 to 6, and chroma of 2 to 4. It is loam or
clay loam. It is slightly alkaline or moderately aIkaline.The bulk density ranges from
I.45 to 1.60 gm/cc. �
COMPETING SERiES: These are the Andres, Aurand(T), Aztalan, Crane, Darroch, �
Gilboa, Houstenader(T},La Ho�ie, Marcellon, Mokena,Nachusa, Nenno, Newhaven,
Odell, Protivin,Tiderishi, Vi�ar, and Wilmer series. The Aurand(T) and Tiderishi series
are presently not in the�SD file. The Andres,Aztalan, and Mokena soils have silty clay
, loain lower B and C horizons. Aztalan soiis also have hue of 7.SYR in the B and C
horizons. Crane soi�s have more than 8 percent rock fragments in Ehe lower part of the
argillic horizon. Darrflch soils have C horizons of stratified silty and sandy sediments
� within the series control section. Gilboa soils have silt loam and silty clay loam in the
� ;�. upper part of the series control section. Houstenader soils have 30 to 40 percent gravel in
, the lower third of the series control section.La Hogue soils have less than 20 percent clay
in the lower part of the series control section. Marcellon soils have less than 24 percent
clay in the argillic horizon. Nachusa soils do not have rock fragmants in the upper part of
the series conteol section. Nenno soils have more than 8 percent rock fragments in the
• lower part of the series control section.Nawhaven soils do not have free carbonates in the
series control section. Odell soils have hue of lOYR in the lower B and C horizons and
higher chroma in the upper B horizon. Protivin soils have bulk density greatez than 1.60
gm/ec in the iower part of the series control section. Vigar soils have a mollic epipedon
greater than 24 inches thick, Wilmer soils have more than 40 percent fine sand or caarser
in the argillic horizon.
GEOGRAPHIC SETTING: The Le Sueur sails have slightly concave, plane, or slightly �
� canvex slopes on moraines within the Des Moines lobe and Grantsburg sublohe of the
Late Wisconsin gtaciation. They formed in a calcareous, loamy till. Slopes range from I �
to 3 pereent. Mean annu�l air temperature ranges from 45 to 52 degrees F. Mean annual
_ precipitation ranges from 25 to 32 inches. Frost-free days range from !25 to 165. �
Elevation �bove sea level ranges From 700 to I600 feet,
GEOGRAPHICALLY ASSOCIATED SOILS: The main ones are tl�e Cordova,
Lester, and Hamel soils, These soils formed in materials simifar to the Le Sueur soils and
are members of a hydrosequence with the Le Sueur soiis. The poorly drained Cordova
_ and Hamei soils are cammon associates on adjacent nearly level slopes. The well drained
Lester soils are the most common associate on the undulating to gently undulating slopes.
- The well drained Ha den soils and the pooriy drained Dundas soils are associates in some
, places.
� . DRAINAGE AND PERMEABILITY: Somewhat pooriy drained. Surface runoff is
. 1ow. Permeability is moderate. An apparent water table is at 1.5 to 2.5 feet during
November to June in most years. .
, � USE AND VEGETATION: Mostly under cultivation with corn, soybeans, grain, and
' hay the principal crops. Native.vegetation was deciduous forest, dominantly eim,
basswood, and maple in some areas, and oak with prairie and brush understory in the
timber outliers within the prairie. ' ,
� DISTRIBUTION AND EXTENT: South-central Minnesota and north-central Iowa.
� This soil is extensive. �
MLRA OFFICE RESPONSIBLE: St. Paul,Minnesota
SERIES ESTABLISHED: Le Sueur County,Minnesota, 1944. .
. REMARKS: Diagnostic horizans and features recognized in this pedon are: moilic
epipedon-the zone from the surface to 13 inches (A and AB horizons); argillic horizon-
the zone from 13 to 41 inches(Bt horizons); aquic subgroup-hue of 1 QYR and chroma of
. 2 immediately below mallic epipedon.
� Somewhat poorly drained matches depth to redox (2 chroma at 17 inches) and taxonomic 1
` . class (Aquic subgroup)closer than the previous moderately well drained class. �
- HAMEL SERIES �
The Hnmel series ccrosists oF very deep, poorly drained and somewhat poorly drained soils th�t Formed in
' slope cfllluvium and giacial tiU on moraines.These soils have moderately slow permeability.Their slopes
range from 1 to 4 percent, Mean annual precipitation is about 2$ inches. Mean annual air temperaWre is
abaut 47 degrees F. •
' TAXONOMIC CLASS: Fine-loamy, mixed, superactive, mesic Typic Argiaquolls
TYPICAL PEDON: Hamel loam with a Z percent concave slope on a glacia! moraine in
- a cultivated fietd. (Colors are for moist soil unless otherwise noted.)
' Ap--0 to i0 inches; black (10YR 2/1} loam, very dark beown (lOYR 212) dry; weak very
fine subangutar blocky structure; friable; common very fine roots; about 1 percent gravel;
I neutral; abrupt smooth boundary.
� A--10 to 16 inches; black(I OYR 2/1) loam, very dark gray(1 OYR 3/1) dry; weak vezy
fine subangular blocky structure; friable; common very fine roots; about 4 percent gravei; .
neutral; gradual smooth boundary. (Cornbined thickness of A horizon is 14 to 30 inches.}
� AB--16 to 24 inches; very dark gray(lOYR 3/1} clay loam, dazk grayish brown (lOYR
, 4/2) dry; many fine prominent brown (7.SYR 4/4) Fe concentrations; moderate fine
angt�lar blocky structure; friable; common very fine roots; about 4 percent gravel; neutral;
gradual wavy boundary. {0 to 10 inches ihick.)
Btg1--24 to 40 inches; very dark grayish brown (2.SY 3/2) clay loam, grayish brown
' . (lOYR S/2) dry; many fine prominent brown (7.SYR 4/4)Fe concentrations; moderate
medium prismatic structure; friable; few black(1QYR 2/1)clay films on faces�of peds;
about 5 percent gravel;neutral; graduat wavy boundary. '
� Btg2--40 to 46 inehes; dack grayish bro�vn (2.SY 4/2) clay loam; many coarse prominent '
�brown (7.SYR 4/4)Fe concentrations; moderate medium subangular blocky structure;
- friable; few black(lOYR 2/1)clay films on faces of peds; about 4 percent gravel; neutral;
: clear wavy boundary. (Combined thickness of Btg horizons is 12 to 30 inches.)
Cg1--46 to 55 inches; olive gray{SY 5!2) loam; znany medium prominent yel�owish
brown {lOYR 5/6)Fe concentratians; massive; friable; about 3 percent gravel; slightly '
effervescent; slightly alkaline; graduaI wavy boundary. �
Cg2--55 to 80 inches; olive gray (SY 5/2) loam; many medium prominent yellowish
brown (IOYR 5/6) Fe concentrations; massive; friable; about 4 percent gravel; slightly '
effervescent; slightly alkaline.
� _ TYPE LOCATION:Wright County,Minnesota; about 1.5 miles southwest of Silver
Creek, 12�0 feet south and 2300 feet west of the northeast corner of Sec. 18, T.121 N.,
R.26 W., USGS Annandale quadrangle; iat. 45 degrees 17 minutes 34 seconds N.; long.
94 degrees 00 minutes 13 seconds W.,NAD27
RANGE IN CI-EARACTERISTICS: Depth to free carbonates range from 30 to 65
_ inches. The mollic ep�peclon thickness ranges from 24 to 60 inches. Typically the upper
colluvim contains less than 2 percent gravel by volume and the lower part contains 2 to 6
percent grave! by volume of mixed lithology.
The A horizons have hue of IOYR or is neutral, value of 2 or 3, and chroma of Q to 2. �
Typically it is loam or clay loam, but silt loam or silty clay loam are within the range. It
, has coatings of clean sand and silt particles in the lower part of the A horizon in some
pedons. It is moderately acid to neutraL
The Btg horizon has hue of lOYR,2.SY, or SY, value of 2 to 4, and chroma of 1 or 2. It is
ctay loam, silty clay loam high in sand, or loam. It has between 25 and 35 percent clay
and 15 to 35 percent fine sand and coarser. It has B/A clay ratios of I.2 to I.4. It has few
to many, faint to prominent clay films. It is moderately acid to neutral.
The C horizon has ttue of a 2.SY or SY, value of 4 to 6,chroma of 1 or 2. It is ]oam or
clay loam.It is slightly alkaline or moderately alkaline. The clay content ranges fcom 18
to 32 percent and the total sand content ranges from 25 to 4S percent.
� COMPETING SERIES: These are the Alvada, Barrv, Berville, Brookston,
Buntin�ville, Clackamas, Cordova, Forestcitv, Jameston, Maren�o,Millgrove, Navan,
Nosoni, Rensselaer, and Westiand soils. The Alvada series (Tentative- OH} is not in the
OSD file at this time. The Barry, Berville,Brookston, Cordova, Marengo, Millgrove,
� Navan,Rensselaer, and Westland soils have a mollic epipedon that is less than 24 inches
�
; thick.The Buntingville soils have carbonates at depths of less than 20 inches. The
Clackamas and Nosoni soils lack free carbonates in the series control section.
The Forestcity soils have 45 to 65 percent sand and 10 to 18 percent clay in the
underlying materiai.The Jamestown soils formed in a firm and very firm till associated
with the Iowan Erosional surface. �
GEOGRAPHIC SETTING: Hamel soils nave concave slopes in swales, rims of ciosed
' depressions, foot and toe slopes, and upper drainageways•below sloping to very steep
slopes. Slope gradients are 1 to 4 percent. Hamel soils formed in slope colluvium and
glacial tilI of Late Wisconsinan Aga. Mean annual air temperature is about 45 to 48
'� degrees F. Mean annual precipitation is about 25 to 30 ini;hes. Frost free days range from
125 to 165. Elevation above sea Ievel ranges from 704 to 1600 feet. '
GEOGRAP�-IICALLY ASSOCIATED SOILS: These.are principally the Ha den and
Lester soils.These soils are well drained and are on the higher lying, gently sloping to
very steep slopes.
DRAINAGE AND PERMEABILITY: Poorly drained and somewhat poorly drained.
Surface runoff is low or moderately low. Permeability is:moderately slow. The apparent
seasonal high water tabie is at .S to 1.5 feet for the poorly drained phase and 1.5 to 2.5
� feet for the somewhat poorly drained phase during spring in�normal years.
USE AND VEGETATION: Most of this sozl is cropped to corn, hay, soybeans, and
smaIl grains. However, significant areas are in pasture and forest. Native vegetation is
mixed wet prairie grasses and deciduous forest.
DISTRIBUTION AND EXTENT: Primarily in the southeast one-quarter of Minnesota
in the timbered, hilly, "gray° till region. Moderately extensive.
MLRA OFFICE RESPONSIBLE: St. Paul, Minnesota
' SERIES ESTABLISHED: Hennepin County, Minnesota, 1969.
REMARKS: Diagnostic horizons and features recognized in ihis pedon are: mollic
- epipedon - the zone from the surface tv a depth of 4Q inches (Ag, A, AB and Btg t); .
argillic horizon- the zone from 24 to 46 inches (Btgl,Btg2,). Type location moved from
' Hennepin County, Mn. to Wright Coanty;Mn., I 1/9b to beEter exempEify the series
concept.
� A somewhat poorly drained overwash phase is recognized that has 8 to 20 inches of
. colluvium over the original dark colored surface.
ADDITIONAL DATA: Refer to MAES Central File Code No. 785 for results of some
laboratory analysis of this series. -
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KILKENNY SERIES
Ttie Kilkenny series consists of very deep, moderately well drained soils that formed in a '
- mantle of c[ayey glacial till or flow titl and t�nderlying loamy glacia! till on moraines.
These soils have moderately slow permeability. Their slopes range from 2 to 35 percent.
The mean annual precipitation is about 28 inches. Mean annual air temperature is about
- 48 degrees F.
TA,XONOMIC CL.ASS: Fine, smectitic, mesic�x a uic Vert'
Y q ic Hapludalfs
TXPICAL PEDON: Kilkenny clay loam with a 15 percent linear sidestope on a glacial
moraine in a pastured field. (Colors are for tnoist soil unless otherwise nated.)
Ap--O to 9 inches; very dazk brown (lOYR 2/2) clay loam, dark grayish brown (lOYR
4/2) dry; weak fine granuIar structure; friable; common very fine roots; about 2 percent
gravel; moderately acid{pH 5.6); abrupt smooth boundayr. (6 to 10 inches thick)
Btl--9 to 19 inches; brown (lOYR�/3) silty clay loam; moderately medium subang�lar
blocky structnre parting to moderately fine subangular blocky; firm; common fine and
very fzne roots; few distinct very dark brown (iOYR 2/2) clay films on faces of Qeds;
about 3 percent gravel; strongly acid; gradual wavy boundary.
Bt2--19 to 38 inches; brown (lOYR 4/3) clay loam; moderate mediam prismatic structure
parting to moderate rnedium subang�lar blocky;�rrri; common very fine roots; common
distinct very dazk brown (lOYR 2/2)clay films on faces of peds; about 5 percent gravel;
strongly acid; gradual wavy boundary.
,
` Bt3--38 to S3 inches; brown (lOYR 4/3) ciay loam; weak medium sabangular blocky '
structure parting to weak fine subangular blocky; firm; common distict very dark.brown
(lOYR 2/2)clay flms on faces of peds; about 5 percent gravel; few fine distict brown
{7.SYR 4/4) Fe concentrations;moderately acid; gradual smooth boundary. (Combined
thicicness of tFie Bt horizons is 20 to 40 inches.)
� . � .
• 2BC--53 to 65 inc:hes; light olive brown (2.SY S/4) loam; wealc fine subangular blocicy
structure; few dis�tinct dark brown (lOYR 3/3) clay films on faces of peds; friable; about 8
percent gravel; ahout 2 percent cobbles; few�ne distinct brown (7.SYR 4/4)Fe deletions;
slightly effervescent; slightly alkaline; gradual wavy boundary.
2C--65 to 84 inches;light olive brown {2.SY S/4) loam; massive; friable; few
concentcations of light gray (2.SY 7/2) calcium carbonates in pares; brown {7.5YR 4/4}
soft masses of iron-manganese in nodules; about 8 percent gravel; about 2 percent
cobbles; corrimon medium prominent dark yellowish brown{1 QYR 4/6) Fe
concentrations and common mediunn distinct gray(2.SY 5/1) Fe depletions; strongly .
effervescent; moderately alkaline.
TYPE LOCATION: Lz Sueur County, Minnesota; about 3 miles west and 3 miles south
of Montgornery;�about 30Q feet east and 800 feet north of the southwest corner of Sec.
USE AND VEGETATION: Most of these soils are cropped to corn, grain, hay, �znd
. soybeans. Some areas are used for pasture und some are forested. Native vegetation is
mixed prairie and forest species. .
, DISTRIBLTTION AND EXTENT: South central Minnesota and notth-central Iowa. The
' series is of moderate extent. _
1VILRA 4FFICE RESPONSIBLE: St. Pau(,Minnesota
SERIES ESTABLISHED: Waseca County, Minnesota, 1963.
REMARKS: Diagnostic horizons and features recognized in this pedon are: Ochric
epipedon -the zone from the soil surface to a depth of 9 inches (Ap horizon); Argillic
horizon - the zone from 9 to 53 inches (Btl, Bt2,Bt3 horizons); Oxyaquic subgroup
based on satnration above a depth of 40 inches; Vertic subgroup based on more than 6 cm
of COLE in upper 40 inches. Water table studies and field observations have veri�ed a
perched candition in most years, particularly in periods of extended rainfall.
ADDITIONAL DATA: Soil Interpretation Record number MN0376. 1
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Property Surveys
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UJ/L3/'GUUO ua:4G NAX a5G 47S 3127 ROGER FAZEh'DTN REALTOR E�003/��03
�'��d� IV VV 1 f.VVC7 f'1CLll CIVVIIV�^„RIIV�S IIVt�. /t1J'�'+L/-VUGV
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Faeld ]�ngineerixig, Inc.
Vb'ATER ANAL.'YSIS
7008 ;19d�Lzne Nor�h-Chnrzplin, h'linn�sota 5531 G 1 O I�la?.^ch 2 C O 6
Tcicphon�:7G31.37-OS 2G
r•8D.rD!r at ia�13?73
TesC �: w13220
=im� : 11 :25 �.M
FZcm: Gu:.side tan
Da�_e drawn : S [�1aro_z 2006
To: SL7DY PLUCKER Daze L�sted: S [�Iarch 2o�G
26h0 FOX Si
ORaNO, MN 55391�
RE: 41a�er tc-st at- : 26_-� Fox St; Oror_o, �1J
Field Eng�r_�er_ng person-tel in cor��unct ion wi L2-� TCw� drev� and
�esced tY�e katz� at thz •a�o-se address . T_�e �est resu"��s =or thc
wa�A=- c3=�U;n by t�iarvin J�.` �4denz�i were �s =ol.lows :
I�� _tilaxin�tim limit Resuli
NitrAte Nitrogen-per Electrodc.Ivlethod tess than 1 O.o m�/1 iess than 1 mo/1
Coliform Eiacteria-per�'�r Ivicthod 0 per 100 i111 O per 100 m1
'T_^.is wat.er DOES meet state, FHP_, '�TA, and L:_ S .p .H_S . speci f;catio*Zs for
the teSL'S 1istC?d zbCv� , Twin Cii�y LQat.er Clinic, Ilinnescta Dc�artmen� ot
?-ie�J.tz certificate #027-,053-119 arid Wiscor_sir_ b�partr,ier_t o� AgY�icu��uz-�
certifa.cate �105-10117 , is authori2ed to perrorm thes� t�sts .
Sincerely You�s,
�i/?��7�r-��l�.�r��
rilar.rin ,T. �TnT�nzel
BL-I'nCI3�WD R.ETU1tN WI'tH PAl'ML-NT .
Fieid ]Engineering, Inc_ 10 *aa=ch 2 0 o b
�VATER ANAL�'SIS
760S 119th LaneNorth-Champlin,T.4innesoca 553I6 To: JUDY PLUCK=R
Tclephonc:?63-42;-GS26 26�0 FO�{ ST
FED.ID#�i!14�]3773
�RONp, r!rT �5 3 91
Rw : [�Tatter t�st at : 2640 Fox St ; p�ono, N_N
're s t i�]'a : 11 8 2 Z O
P_moun� pa�d: $7o. CC
This cest was done on ;�work order for you. VYe li:tve nuCbing io do�vith chc rnalizing of
the sale_Our bi11 is for thc tesY-not Chc sale and rnust be paid.
03/10/2006 P'RI 11:09 [Tl/R,l' NO E330] �002