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HomeMy WebLinkAboutWetland Classification, Identification, Delineation-2013 37II Northern Ave Orono, MN Prepared by Svoboda Ecological Resources for- George Stickney Wetland Classification, Identification, and DelineationReport Project No. 2012-012-03 July 3, 2012 Providing the S1:arper Edge to Natural Resources & Enoiron>'nentad Consulting ECOLOGICAL RESOURCES 25580 Nelsine Drive,Suite 100 Shorewood,NIN 55331 (952)471-1100 (952)471-0007(Fax) 3700 Northern Avenue Hennepin County NDN Wetland Classification, Identification, and Delineation Report Prepared for: George Stickney By: Svoboda Ecological Resources Project Number 2012-020 July 3,2012 The contents and format of this report are considered intellectual property and are subject to copyright restrictions and may not be reproduced without the express permission of Svoboda Ecological Resources. Table of Contents ABSTRACT.................................................................................................................................................1 INTRODUCTION.......................................................................................................................................1 METHODS..................................................................................................................................................1 RESULTS....................................................................................................................................................2 DISCUSSION..............................................................................................................................................3 RECOMMENDATIONS............................................................................................................................4 CERTIFICATION......................................................................................................................................5 DATASOURCES.......................................................................................................................................6 LITERATURE REFERENCED................................................................................................................7 FIGURES: Figure 1: Site Location Overlaid on Topographic Map Figure 2: National Wetlands Inventory Figure 3: Web Soil Survey-Hennepin County Figure 4: DNR-Public Waters Map Figure 5: Approximate Wetland Boundary and Sample Transect Location TECHNICAL DOCUMENTS: Field Data Sheets Photo Log Plant Indicator Status Soil Series Data Wetland Definition ABSTRACT Svoboda Ecological Resources (SER) visited the above referenced property on 6/12/12 to examine the site for the presence of areas meeting wetland criteria. The study parcel is located in Orono MN, Hennepin County (Figure 1). One wetland boundary was delineated at this site. One sample transect was established along the boundary in order to characterize the soil, vegetation, and existing hydrology within the wetland-to-upland transition zone. INTRODUCTION The subject parcel is approximately 4.9 acres and is dominated by southern terrace forest, turf grass, and early successional invasives. The topography of the site slopes towards the central basin on the property. The surrounding land use is suburban consisting mostly of single family homes. The identified wetlands were classified according to the Cowardin et al., the Circular 39 and the Eggers and Reed classification systems and marked with pink"Wetland Delineation"pin flags. The Technical Documents section of this report contains field data sheets, plant indicator status information, soil survey information, and wetland definition information. METHODS The methods used to delineate the subject parcel are as described in the 1987 US Army Corps of Engineers Wetlands Delineation Manual and the 2010 Midwest Regional Supplement Manual. In the 1987 Manual, the methods used were described under the "routine" methods for sites less than 5 acres. This methodology is followed in order to assess whether the three parameters of a wetland are met for areas on the subject parcel. The three parameters required under normal circumstances in order to delineate a wetland are described in the Technical Documents section. The Midwest Regional Supplement Wetland Delineation Manual is also being utilized to increase the accuracy of our wetland boundaries. This addendum to the original 87 Manual was created to address the many regional differences that affect wetlands and the delineation methods used throughout the country. The following explanations are passages from that document. "This Regional Supplement is part of a nationwide effort to address regional wetland characteristics and improve the accuracy and efficiency of wetland- delineation procedures. Regional differences in climate, geology, soils, hydrology plant and animal communities,and other factors are important to the identification and functioning of wetlands. These differences cannot be considered adequately in a single national manual. The development of this supplement follows National Academy of Sciences recommendations to increase the regional sensitivity of wetland-delineation methods (National Research Svoboda Ecological Resources 3700 Northern Avenue Project Number: 2012-020 1 Orono MN Council 1995).The intent of this supplement is to bring the Corps Manual up to date with current knowledge and practice in the region and not to change wetland boundaries." "...This Regional Supplement is designed for use with the current version of the Corps Manual (Environmental Laboratory 1987) and all subsequent versions. Where differences in the two documents occur, this Regional Supplement takes precedence over the Corps Manual for applications in the Midwest Region." National Wetland Inventory (NWI) maps (Figure 2), Web Soil Survey of Hennepin County map (Figure 3), Minnesota Public Waters Inventory maps (Figure 4), and 2010 aerial photographs were reviewed prior to the site visit to identify areas that may be wetlands. 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 characterize wetland types and determine wetland boundaries. Sample transects were established in representative wetland-to-upland transition zones in order to characterize the vegetation, soils, and hydrology of the site. Transects consist of a representative upland sample point and representative wetland sample point. Information obtained at the sample points can be found on the field data sheets located in the Technical Documents section. Hydrophytic status of plants was based on the National Wetland Plant List issued on May 15, 2012 and effective June 1, 2012 and as characterized by the plant status on the Excel Midwest Region data sheet provided by the US Army Corps of Engineers, St. Paul District. Wetland boundaries were marked at the site by pink "Wetland Delineation" pin flags. The wetland boundary is considered to be the topographically highest extent of the wetland basin; areas below the staked boundary met the three required wetland criteria while areas above were lacking in one or more of these criteria. Wetlands were classified in accordance with methods described by Cowardin et al. (1979) and used in the NWI (e.g. PEMB, PSS1C, etc.), completed by the U.S. Fish and Wildlife Service. The Circular 39 and Eggers and Reed classification systems are also given. The indicator status of plants, as described in the Technical Documents section, was determined using the National List of Plant Species That Occur in Wetlands — Region 3 (Sabine 1999). RESULTS The National Wetland Inventory indicates the presence of one wetland within the study area, classified as PEMA(Figure 2). The Web Soil Survey of Hennepin County (Figure 3) identifies four soil map units within the study area. They are as follows: Urban land-Udorthents, Lester loam, Hamel overwash Hamel, and Klossner soils. Klossner soils are considered hydric, Lester loam and Hamel overwash hamel are partially hydric, and Urban land-Udorthents is unknown. Soil series descriptions are provided in the Technical Documents section. Svoboda Ecological Resources 3700 Northern Avenue Project Number: 2012-020 2 Orono MN The Minnesota Department of Natural Resources, State Protected Waters Map (Public Water Inventory) indicates no public waters within the study area(Figure 4). Site Visit SER ecologists examined the subject property for areas meeting jurisdictional wetland criteria during the site visit. One area meeting the jurisdictional criteria of a wetland was flagged, and the boundary determined and delineated. The approximate wetland boundary is outlined in yellow (Figure 5). Wetland is a Type 1 PEMA Seasonally Flooded Basin. The vegetation at sample point 1-1 UP consisted of a canopy of swamp white oak (Quercus bicolor, FACW) with an understory of silver maple(Acer saccharinum, FACW) and common buckthorn(Rhamnus cathatica, FAC). At sample point 1-1 WET the vegetation consisted of a canopy layer of cottonwood (Populus deltoides, FACW) with an understory of box elder (Acer negundo, FAC) and common buckthorn. The transition from wetland to upland is characterized, in part, by this vegetative change. The soils at sample point 1-1 UP consisted of an initial 6 inches of 10yr 3/2 silt loam. From 6-9 inches there was 10yr 3/2 silty clay loam with 3% 7.5yr 5/8 matrix concentrations, from 9-20 inches there is 10yr 3/2 silty clay with 10% 7.5yr 5/8 matrix concentrations. From 20-30 there was 10yr 5/1 silty clay with 5% 7.5yr 5/8 matrix concentrations. The soils at sample point 1-1 WET consisted of an initial 12 inches of 10yr 2/1 mucky loam with 10yr 2/1 silt loam from 12- 24 inches. From 24-30 inches there was 10yr 5/1 silty clay with 2% 5yr 4/6 matrix concentrations. Hydric indicator F1 (Mucky Mineral)was noted. Wetland hydrology was observed at sample point 1-1 UP. Indicators A2 (High Water Table), A3 (Saturation), B4 (Algal Mat or Crust), B9 (Water Stained Leaves) and D5 (FAC-Neutral Test) were all present. The wetland is partially represented in the National Wetland Inventory but is not present in the DNR Public Waters Inventory. Wetland 1 appears to have increased in size, approximately doubled, from the original polygon as mapped by the NWI in the early 1980's. The wetland type remains unchanged. Detailed soils, vegetation, and hydrology data for the delineated jurisdictional wetlands are provided in the data sheets of the Technical Documents section. DISCUSSION SER completed all on-site delineations based on the three required technical criteria as outlined by the 1987 Manual: the presence of hydric soils, a predominance of hydrophytic vegetation, and indicators of wetland hydrology in each basin. The site visit portion of the wetland delineation was completed on 6/12/12. Svoboda Ecological Resources 3700 Northern Avenue Project Number: 2012-020 3 Orono MN SER personnel examined the subject property for areas meeting jurisdictional wetland criteria during the site visit and delineated the edge of two basins as being jurisdictional wetlands (Figure 5). Detailed soils, vegetation and hydrology data is provided in the data sheets of the Technical Documents section. A set of figures is provided in the Figures section. RECOMMENDATIONS Activities that impact or could potentially impact wetlands are regulated at several levels of government. In Minnesota, the two primary jurisdictions are covered at the state and federal levels by the provisions of the following legislative actions. ➢ State jurisdiction by the Wetland Conservation Act of 1991 (WCA) administered by the WCA Local Governmental Unit(LGU). ➢ Federal jurisdiction by the Clean Water Act of 1972 and subsequent amendments. Wetland protection is implemented by the Corps of Engineers(Corps)with permit certification issued by the Environmental Protection Agency. While the wetland boundaries that SER has delineated are not official until approved by a WCA approved local government unit (LGU), SER advises the property owner/developer to refrain from any filling, draining, or excavating, or any impact to the area SER has delineated as wetland. No grading or filling in wetland basins should commence until all necessary permits have been obtained. Violation of wetland regulations may result in substantial civil and criminal penalties. Local ordinances may regulate wetland modifications such as brush and tree removal and burning in addition to grading and filling. Depending on the location 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 regulatory agencies. It is also advisable to have the wetland boundary surveyed by a licensed land surveyor. Since the pin flags used along the boundary can be vandalized or inadvertently knocked over, a GPS survey of the flags will assure the permanence of the boundary. The client should also be aware that according to current BWSR and COE wetland rules and regulations approved wetland boundaries are typically valid for five years from the date of approval. To avoid project delays associated with wetland regulations, it is essential that you acquire necessary permits from all jurisdictional agencies before initiating activities. A WCA Sequencing form, a WCA and Army Corps of Engineers Replacement Plan Application form, and a DNR permit application are among the materials that you may be required to submit if impacts are proposed for the delineated wetlands. By initiating the permit process as soon as possible,potential costly delays to the project may be avoided. Svoboda Ecological Resources 3700 Northern Avenue Project Number: 2012-020 4 Orono MN CERTIFICATION Frank Svoboda completed the above-described delineation on 6/12/12. This delineation was performed according to the procedures described by the US Army Corps of Engineers in the 1987 Wetlands Delineation Manual and the 2007 Midwest Region Supplement Wetland Delineation Manual. The delineation meets the standards and a criterion described in these manuals and conforms to the applicable standards and regulations in force at the time the delineation was completed. Report and graphics were prepared by David Haar(Wetland Ecologist UGIS Specialist)on this day 06/19/12. The delineation report was reviewed by Frank Svoboda,President of Svoboda Ecological Resources. Field work was completed by Blair Bollig and field checked by Frank Svoboda. Client: George Stickney Project Name: 3700 Northern Avenue Project No.: 2012-020 Location: Orono MN �/ '-,� _Zck `' Wetland Ecologist UGIS Specialist President, Svoboda Ecological Resources 06/19/12 Date Svoboda Ecological Resources 3700 Northern Avenue Project Number:2012-020 5 Orono MN DATA SOURCES Minnesota Department of Natural Resources, Public Waters Inventory Basin Delineations, Published 7/31/2008 and retrieved from http://deli.dnr.state.mn.us United States Fish and Wildlife Service National Wetland Inventory Map. Retrieved from http://www.fws.gov/wetlands/Data/Mapper.html on 06/19/12. 2010 Aerial Color Photos. Publicly Distributed by MN Geo WMS Service. Topographic maps obtained via the National Geographic Society's USA Topo service through ESRI. Web Soil Survey for Hennepin County,MN. Retrieved from http://websoilsurvey.nres.usda.gov/app/HomePage.htm Svoboda Ecological Resources 3700 Northern Avenue Project Number:2012-020 6 Orono MN LITERATURE REFERENCED 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. and Donald M. Reed. 1997. Wetland Plants and 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. Gleason,H.A. and A.C. Cronquist. 1991.Manual of Vascular Plants of Northeastern United States and Adjacent Canada.New York Botanical Garden,Bronx. 91Opp. Sabine,B. J. 1999.National List of Plant Species that Occur in Wetlands:Region 3—North Central(Indiana, Illinois, Iowa, Michigan, Minnesota, Missouri, Wisconsin). Resource Management Group, Inc. 77pp. Shaw, S.P., and C.G. Fredine. 1956. Wetlands of the United States. U.S. Fish and Wildlife Service, Circular 39. 67pp. U.S. Army Corps of Engineers. August 2010. Regional Supplement to the Corps of Engineers Wetland Delineation Manual: Midwest Region(Version 2.0). ERDC/EL TR-10-16. Vicksburg, MS: US Army Engineer Research and Development Center. Svoboda Ecological Resources 3700 Northern Avenue Project Number: 2012-020 7 Orono MN FIGURES •C.;- � -• � ` �`a �''o � 993 � ��'� a 7 t� `- � 1 Maxwell Bay �w f. riw j Saga ) 7 O i \"-...+,. �_ - :rid f , �,.938 3• �� �_ C_a �. � I t2 950 i 1 P JfT to ,.' •`�,1's t M 94 ' �• '�• Sohns Point— --_ CR"TAL BAY l 944 !stand Fagerness �...;} Point •. l;ShadYwood 1Fj 7-• pnIIg �' •9 ti' i" ". Point �,. k i .. t - - r. t. r ll_"}�"" \``•`.. - = �``• `, Lafayette Spring Park 9U Y" Black Lake • CE�.'D \ . . a t �• �' `4,w� `!Point "!J i . • y { Goose • Island < �� ._• •i ��� Codri o,nt 0 — ,("•.. Spray _� LA A Island!' KE MINNETONK !I �% Crescent ' *: se.ch8 .t --Shady ! tne ., •� .-� Island — .Howard Point --- — - 932 m Tonka day Tl 17N R23W S17 Site Overview Figure 1 Overlaid on 2010 Aerial Photo 2012-20 ! SVOBODq 3700 Northern Ave `�• Ecological Resources 0 1,250 2,500 5,000 Feet Orono MN w. PEMA lit, , q. ♦ „ "`s g mom R , a ,r u , .JK� ♦ z sl, e e � s a :fr „ b y ..z aF w f�" r TI 17N R23w S17 National Wetland Inventory Figure 2 Overlaid on 2010 Aerial Photo 2012-20 4 S V O B O DA 0 50 100 200 3700 Northern Ave Ecological Resources Feet Orono MN 11, 01 — r ` { 91, a: f . t • n • • • ceB x f • • • mi AD• • ff " r•Vw .' TI 17N R23w S17 Soil Survey Figure 3 Overlaid on 2010 Aerial Photo 2012-20 �11'4 S V O B O DAo 50 100 200 3700 Northern Ave Ecological Resources Feet Orono MN '. a _ <j Q �Y _ a max`- . } d K ilk TI 17N R23w S17 public Waters Inventory Figure 4 Overlaid on 2010 Aerial Photo 2012-20 i';,.SV O B O DR3700 Northern Ave Ecological Resources 0 50 100 200 Feet Orono MN w t r w x s �AI1A7 - , 4 44 UM ti d TI 17N R23w S17 Approximate Wetland Boundary Figure 5 Overlaid on 2010 Aerial Photo 2012-20 iI't-AISVOBODAp 75 150 300 3700 Northern Ave Ecological Resources Feet Orono MN THE TECHNICAL DOCUMENTATION SECTION Field Data Sheets WETLAND DETERMINATION DATA FORM-Midwest Region Project/Site 3700 Northern Ave City/County: Spring Lake/Hennepin Sampling Date: 6/12/12 Applicant/Owner.. Coldwell Banker Bumet Realty State: Minnesota Sampling Point: 1-1 Wet Investigator(s): Frank Svoboda&Blair Bollig Section,Township,Range: Sec 17,T1 17N,R23W Landform(hillslope,terrace,etc.): Depression Local relief(concave,convex,none): Concave Slope(%): 0 Lat: Long: Datum: Soil Map Unit Name Klossner 4WI Classification: PEMA Are climaticthydrologic conditions of the site typical for this time of the year? Y (If no,explain in remarks) Are vegetation soil or hydrology significantly disturbed? Are"normal circumstances" Are vegetation soil or hydrology naturally problematic? present? Yes SUMMARY OF FINDINGS (If needed,explain any answers in remarks.) Hydrophytic vegetation present? Y Hydric soil present? Y Is the sampled area within a wetland? Y Indicators of wetland hydrology present? Y f yes,optional wetland site ID: Remarks:(Explain alternative procedures here or in a separate report.) VEGETATION—Use scientific names of plants. Absolute Dominan Indicator Dominance Test Worksheet Tree Stratum (Plot size: 30 ) %Cover t Species Staus Number of Dominant Species 1 Populus tremuloides 15 Y FAC that are OBL,FACW,or FAC: 5 (A) 2 Fraxinus pennsylvanica 10 Y FACW Total Number of Dominant 3 Species Across all Strata: 5 (B) 4 Percent of Dominant Species 5 that are OBL,FACW,or FAC: 100.00% (A/B) 25 =Total Cover Sapling/Shrub straturr (Plot size: 15 ) Prevalence Index Worksheet 1 Acer negundo 20 Y FAC Total%Cover of: 2 Rhamnus cathartica 15 Y FAC OBL species 5 x 1 = 5 3 FACW species 10 x2= 20 4 FAC species 50 x 3= 150 5 FACU species 0 x4= 0 35 =Total Cover UPL species 0 x 5= 0 Herb stratum (Plot size: 5 ) Column totals 65 (A) 175 (B) 1 Carex lacustris 5 Y OBL Prevalence Index=B/A= 2.69 2 3 Hydrophytic Vegetation Indicators: 4 _Rapid test for hydrophytic vegetation 5 X Dominance test is>50% 6 X Prevalence index is 53.0* 7 Morphogical adaptations*(provide 8 supporting data in Remarks or on a 9 _separate sheet) 10 Problematic hydrophytic vegetation* 5 =Total Cover _(explain) Woody vine stratum (Plot size: 30 ) Indicators of hydric soil and wetland hydrology must be 1 present,unless disturbed or problematic 2 Hydrophytic 0 =Total Cover vegetation present? Y Remarks:(Include photo numbers here or on a separate sheet) US Amy Corps of Engineers Midwest Region SOIL Sampling Point: 1-1 Wet Profile Description: (Describe to the depth needed to document the Indicator or confirm the absence of indicators.) Depth Matrix Redox Features (Inches) Color(moist) % Color(moist) % Type* Loc** Texture Remarks 12 10YR 2/1 100 Muck S.O.M High,Saturated,Sapric 24 10YR 2/1 100 Silt Loam Saturated 30 10YR 5/1 98 5YR 4/6 2 C M Silt Clay *Type:C=Concentration,D=Depletion,RM=Reduced Matrix,MS=Masked Sand Grains. **Location:PL=Pore Lining,M=Matrix Hydric Soil Indicators: Indicators for Problematic Hydric Soils: Histisol(Al) _Sandy Gleyed Matrix(S4) _Coast Prairie Redox(A16)(LRR K,L,R) X Histic Epipedon(A2) _Sandy Redox(S5) _Dark Surface(S7)(LRR K,L) _Black Histic(A3) _Stripped Matrix(S6) _5 cm Mucky Peat or Peat(S3)(LRR K,L,R) _Hydrogen Sulfide(A4) _Loamy Mucky Mineral(F1) _Iron-Manganese Masses(F12)(LRR K,L,R) _Stratified Layers(A5) _Loamy Gleyed Matrix(F2) _Very Shallow Dark Surface(TF12) 2 cm Muck(A10) _Depleted Matrix(F3) _Other(explain in remarks) _Depleted Below Dark Surface(A11) _Redox Dark Surface(F6) _Thick Dark Surface(Al2) _Depleted Dark Surface(F7) *Indicators of hydrophytic vegetation and weltand _Sandy Mucky Mineral(S1) _Redox Depressions(F8) hydrology must be present,unless disturbed or problematic Restrictive Layer(if observed): Type: Hydric soil present? Y Depth(inches): Remarks: HYDROLOGY Wetland Hydrology Indicators: Primary Indicators(minimum of one is reauired:check all that apply) Secondary Indicators minimum of two re uired Surface Water(Al) _Aquatic Fauna(613) _Surface Soil Cracks(136) X High Water Table(A2) _True Aquatic Plants(1314) _Drainage Patterns(1310) T Saturation(A3) _Hydrogen Sulfide Odor(Cl) _Dry-Season Water Table(C2) Water Marks(B1) Oxidized Rhizospheres on Living Roots_Crayfish Burrows(C8) Sediment Deposits(132) _(C3) _Saturation Visible on Aerial Imagery(C9) Drift Deposits(133) _Presence of Reduced Iron(C4) _Stunted or Stressed Plants(D1) X Algal Mat or Crust(134) Recent Iron Reduction in Tilled Soils Geomorphic Position(D2) Iron Deposits(135) (C6) X FAC-Neutral Test(D5) Inundation Visible on Aerial Imagery(137) _Thin Muck Surface(C7) Sparsely Vegetated Concave Surface(68) _Gauge or Well Data(D9) X Water-Stained Leaves(139) _Other(Explain in Remarks) Field Observations: Surface water present? Yes No X Depth(inches): Water table present? Yes X No Depth(inches): 2 Indicators of wetland Saturation present? Yes No Depth(inches): 0 hydrology present? Y (includes capillary fringe) Describe recorded data(stream gauge,monitoring well,aerial photos,previous inspections),if available: Remarks: US Army Corps of Engineers Midwest Region WETLAND DETERMINATION DATA FORM-Midwest Region Project/Site 3700 Northern Ave City/County: Spring Lake/Hennepin Sampling Date: 6/12/2012 Applicant/Owner. Coldwell Banker Bumet Realty State: Minnesota Sampling Point: 1-1 UPI Investigator(s): Frank Svoboda&Blair Bollig Section,Township,Range: Sec 17,T1 17N,R23W Landform(hillslope,terrace,etc.): Terrace Local relief(concave,convex,none): Concave Slope(%): 2 Let: Long: Datum: Soil Map Unit Name Klossner VWI Classification: PEMA Are climatic/hydrologic conditions of the site typical for this time of the year? Y (If no,explain in remarks) Are vegetation Soil or hydrology significantly disturbed? Are"normal circumstances" Are vegetation soil or hydrology naturally problematic? present? Yes SUMMARY OF FINDINGS (If needed,explain any answers in remarks.) Hydrophytic vegetation present? Y Hydric soil present? N Is the sampled area within a wetland? N Indicators of wetland hydrology present? N f yes,optional wetland site ID: Remarks:(Explain alternative procedures here or in a separate report.) VEGETATION--Use scientific names of plants. Absolute Dominan Indicator Dominance Test Worksheet Tree Stratum (Plot size: 30 ) %Cover t Species Staus Number of Dominant Species 1 Quercus bicolor 15 Y FACW that are OBL,FACW,or FAC: 4 (A) 2 Populus tremuloides 5 Y FAC Total Number of Dominant 3 Tilia americana 5 Y FACU Species Across all Strata: 5 (B) 4 Percent of Dominant Species 5 that are OBL,FACW,or FAC: 80.00% (A/B) 25 =Total Cover Sapling/Shrub straturr (Plot size: 15 ) Prevalence Index Worksheet 1 Acer saccharinum 35 Y FACW Total%Cover of: 2 Rhamnus cathartics 25 Y FAC OBL species 0 x 1 = 0 3 Fraxinus pennsylvanica 5 N FACW FACW species 55 x2= 110 4 FAC species 30 x 3= 90 5 FACU species 7 x4= 28 65 =Total Cover UPL species 0 x 5= 0 Herb stratum (Plot size: 5 ) Column totals 92 (A) 228 (B) 1 Parthenocissus quinquefolia 2 FACU Prevalence Index=B/A= 2.48 2 3 Hydrophytic Vegetation Indicators: 4 _Rapid test for hydrophytic vegetation 5 X Dominance test is>50% 6 X Prevalence index is 53.0* 7 Morphogical adaptations*(provide 8 supporting data in Remarks or on a 9 _separate sheet) 10 Problematic hydrophytic vegetation* 2 =Total Cover _(explain) Woody vine stratum (Plot size: 30 ) *Indicators of hydric soil and wetland hydrology must be 1 present,unless disturbed or problematic 2 Hydrophytic 0 =Total Cover vegetation present? Y Remarks:(Include photo numbers here or on a separate sheet) 5%of ground cover was occupied by moss US Amy Corps of Engineers Midwest Region SOIL Sampling Point: 1-1 UPI Profile Description: (Describe to the depth needed to document the indicator or confirm the absence of Indicators.) Depth Matrix Redox Features (Inches) Color(moist) % Color(moist) % Type* Loc'* Texture Remarks 6 10YR 3/2 100 Silt Loam 9 !0 YR 3/2 97 7.5YR 5/8 3 C M Silty Clay Loam 20 10YR 3/2 90 7.5YR 5/8 10 C M Silty Clay 30 10YR 5/1 95 7.5YR 5/8 5 C M Silty Clay *Type:C=Concentration,D=Depletion,RM=Reduced Matrix,MS=Masked Sand Grains. **Location:PL=Pore Lining,M=Matrix Hydric Soil Indicators: Indicators for Problematic Hydric Soils: _H!stisol(Al) _Sandy Gleyed Matrix(S4) _Coast Prairie Redox(A16)(LRR K,L,R) _Histic Epipedon(A2) _Sandy Redox(S5) _Dark Surface(S7)(LRR K,L) _Black Histic(A3) _Stripped Matrix(S6) _5 cm Mucky Peat or Peat(S3)(LRR K,L,R) _Hydrogen Sulfide(A4) _Loamy Mucky Mineral(F1) _Iron-Manganese Masses(F12)(LRR K,L,R) _Stratified Layers(A5) _Loamy Gleyed Matrix(F2) _Very Shallow Dark Surface(TF12) _2 cm Muck(A10) _Depleted Matrix(F3) _Other(explain In remarks) _Depleted Below Dark Surface(A11) _Redox Dark Surface(F6) Thick Dark Surface(Al2) Depleted Dark Surface(F7) *Indicators of hydrophytic vegetation and weltand _Sandy Mucky Mineral(S1) _Redox Depressions(F8) hydrology must be present,unless disturbed or problematic Restrictive Layer(if observed): Type: Hydric soil present? N Depth(inches): Remarks: HYDROLOGY Wetland Hydrology Indicators: Primary Indicators(minimum of one is required:check all that apply) Secondary Indicators minimum of two required Surface Water(Al) _Aquatic Fauna(B13) _Surface Soil Cracks(B6) High Water Table(A2) _True Aquatic Plants(B14) _Drainage Patterns(B10) Saturation(A3) _Hydrogen Sulfide Odor(Cl) _Dry-Season Water Table(C2) Water Marks(B1) Oxidized Rhizospheres on Living Roots_Crayfish Burrows(C8) Sediment Deposits(B2) (C3) _Saturation Visible on Aerial Imagery(C9) Drift Deposits(133) _Presence of Reduced Iron(C4) _Stunted or Stressed Plants(D1) Algal Mat or Crust(64) Recent Iron Reduction in Tilled Soils Geomorphic Position(D2) Iron Deposits(B5) (C6) X FAC-Neutral Test(D5) Inundation Visible on Aerial Imagery(B7) _Thin Muck Surface(C7) Sparsely Vegetated Concave Surface(B8) _Gauge or Well Data(D9) Water-Stained Leaves(139) _Other(Explain in Remarks) Field Observations: Surface water present? Yes No X Depth(inches): Water table present? Yes No X Depth(inches): Indicators of wetland Saturation present? Yes No --37-Depth(inches): hydrology present? N (includes capillary fringe) Describe recorded data(stream gauge,monitoring well,aerial photos,previous Inspections),if available: Remarks: US Army Corps of Engineers Midwest Region THE TECHNICAL DOCUMENTATION SECTION Plant Indicator Status INDICATOR CATEGORIES* Obligate Wetland(OBL)—Occur almost always (estimated probability>99%)under natural conditions in wetlands. Facultative Wetland(FACW)—Usually occur in wetlands (estimated probability 67%-99%), but occasionally found in non-wetlands. Facultative(FAC)—Equally likely to occur in wetlands or non-wetlands (estimated probability 34%-66916). 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. 1988. National list of plant species that occur in wetlands: Minnesota. National Wetlands Inventory, U.S. Fish and Wildlife Service, St. Petersburg,Florida. THE TECHNICAL DOCUMENTATION SECTION Soil Series Descriptions Acquired from Natural Resource Conservation Service Website,Official Soil Series Descriptions KLOSSNER SERIES The Klossner series consists of very deep,very poorly drained soils formed in well decomposed organic material 16 to 50 inches thick overlying loamy deposits on moraines,till plains,lake plains,flood plains, and hillside seep areas.They have moderately slow to moderately rapid permeability in the organic material,and moderate or moderately slow permeability in the loamy material.Slopes range from 0 to 8 percent.Mean annual precipitation is about 28 inches.Mean annual temperature is about 47 degrees F. TAXONOMIC CLASS: Loamy,mixed, euic, mesic Terric Haplosaprists TYPICAL PEDON: Klossner muck-with a 1 percent slope in a cultivated field. (Colors are for moist soil unless otherwise stated.) Oap--O to 10 inches;black(N 2/0)muck,very dark gray(IOYR 3/1)dry; about 20 percent fiber, less than 5 percent rubbed;weak fine subangular blocky structure;very friable;many very fine roots; moderately acid; abrupt smooth boundary. Oa--10 to 26 inches;black(10YR 2/1)muck, dark gray(1 OYR 4/1)dry; about 60 percent fiber, about 6 percent rubbed; weak fine subangular blocky structure;very friable;many very fine roots; moderately acid; gradual smooth boundary. (Combined thickness of O horizon is 16 to 50 inches.) 2A1--26 to 36 inches;black(N 2/0)mucky silty clay loam; weak medium subangular blocky structure; friable; few very fine roots; slightly acid; gradual smooth boundary. 2A2--36 to 48 inches;black(N 2/0) silty clay loam; massive; friable; few dark reddish brown(5YR 3/4)iron oxide concentrations in root channels; about 1 percent gravel; neutral; gradual wavy boundary. (Combined thickness of 2A horizon is 8 to 45 inches thick.) 2Cg1--48 to 65 inches; olive gray(5Y 5/2) clay loam;massive; friable; dark reddish brown(5YR 3/4)Fe oxide concentrations in root channels;many medium prominent yellowish brown(1 OYR 5/6)Fe concentrations; about 1 percent gravel; slightly effervescent; slightly alkaline; gradual wavy bounday. 2Cg2--65 to 80 inches; gray(5Y 5/1)loam;massive; friable;many medium prominent light olive brown(2.5Y 5/4) and yellowish brown(IOYR 5/4)Fe concentrations; about 3 percent gravel; slightly effervescent; slightly alkaline. TYPE LOCATION:Nicollet County,Minnesota; 2600 feet north and 2300 feet east of the southwest comer, sec. 12,T. 110 N.,R. 28 W.;USGS Nicollet quadrangle; lat. 44 degrees 20 minutes 53 seconds N. and long. 94 degrees 8 minutes 28 seconds W., NAD27. RANGE IN CHARACTERISTICS: The thickness of the organic material ranges from 16 to 50 inches. It is derived primarily from herbaceous plants. The organic matter content ranges from 25 to 60 percent in the organic surface and 5 to 20 percent in the 2A horizon. The reaction of the organic material ranges from moderately acid to slightly alkaline. Some organic layers contain free carbonates. The O horizon has hue of l OYR, 5YR, or is neutral,value of 2 or 3 and chroma of 0 to 2. It is dominantly muck(sapric material)however, some pedons have thin layers of hemic material, less than 10 inches thick. Some pedons have highly organic mineral plow layers. The 2A horizon has hue of l OYR, 2.5Y, 5Y or is neutral, value of 2 or 3 and chroma of 0 to 1. It is loam, silt loam, sandy clay loam, silty clay loam, clay loam or mucky modifiers of these textures. It is moderately acid to slightly alkaline. Some pedons contain thin layers of coprogenous earth. The 2Cg horizon has hue of l OYR, 2.5Y, 5Y, 5GY,or is neutral, value of 2 to 7 and chroma of 0 to 2. It is loam, silt loam, silty clay loam, clay loam, sandy clay loam, sandy loam or fine sandy loam, or their gravelly or cobbly analogues. It is slightly acid to moderately alkaline. The upper 12 inches of this horizon averages less than 35 percent clay. Some pedons contain thin strata of fine sand, loamy sand, or silt. Gravel or cobble sized rock fragments range from 0 to 25 percent by volume. Some pedons contain free carbonates. Sandy substratum and ponded phases are recognized. COMPETING SERIES: These are Linwood, Medo, Palms, Philbon and Shalcar series. Linwood soils have well expressed granular structure to depths of more than 12 inches and formed mainly in woody fibers. Medo soils have sandy textures in the lower part of the series control section. Palms soils have organic matter content greater than 75 percent and do not have an A horizon directly below the organic material. Philbon soils have fibric and hemic material in the upper 12 inches. Shalcar soils ave less than 26 degrees difference between mean January and mean July temperatures. GEOGRAPHIC SETTING: Klossner soils are in basins that were formerly lakes or ponds, lake plains,till plains, flood plains,or moraines. They are also on hillside seep areas in moraines and sideslopes of river valleys. Slopes range from 0 to 8 percent. The soils on nearby uplands are generally loamy. The mean annual temperature ranges from 45 to 50 degrees F. The mean annual precipitation ranges from 24 to 32 inches. Frost free days range from 110 to 160. Elevations above sea level range from 800 to 1400 feet. GEOGRAPHICALLY ASSOCIATED SOILS: The main ones are the Canisteo, Harps, Okoboii, Glencoe, Muskego and Houghton soils. Canisteo and Harps soils are on the rims of depressions. Glencoe and Okoboji are at the outer edges of the depressions. Muskego and Houghton soils are in larger depressions. DRAINAGE AND PERMEABILITY: Very poorly drained. Surface runoff is negligible. Permeability is moderately slow to moderately rapid in the organic layers and moderate or moderately slow in the loamy material. USE AND VEGETATION: The greater part of this soil is cultivated to corn, soybeans, small grains and specialty crops such as vegetables or grass sod. Other areas are in vegetation of grasses,reeds, sedges, alder, aspen, or willow. Some of the hillside seep areas are set aside as natural areas and called fens. DISTRIBUTION AND EXTENT: The south central and southeast part of Minnesota and possibly northern Iowa. The series is extensive. MLRA OFFICE RESPONSIBLE: St. Paul,Minnesota SERIES ESTABLISHED:Nicollet County, Minnesota, 1989. REMARKS: Diagnostic horizons and features recognized are: sapric soil materials from the surface to about 26 inches; loamy mineral material from 26 to 50 inches or more; aquic moisture regime. This soil was formerly included in the Palms Series in Minnesota. ADDITIONAL DATA: Refer to MASS-CFC#'s 2697, 3251, 3400 and 3475. THE TECHNICAL DOCUMENTATION SECTION Wetland Definition WETLAND DEFINITION According to the 1987 U.S. Army Corps of Engineers "Wetlands Delineation Manual" (1987 Manual; the document used by all delineators to define wetlands) a wetland is "Those areas that are inundated or saturated by surface or ground water at a frequency and duration sufficient to support, and that under normal circumstances do support, a prevalence of vegetation typically adapted for life in saturated soil conditions." The Minnesota State Wetland Conservation Act Rules, Chapter 8420, further clarifies that"...wetlands must: (1)have a predominance of hydric soils; (2) be inundated or saturated by surface water or groundwater at a frequency and duration sufficient to support a prevalence of hydrophytic vegetation typically adapted for life in saturated soil conditions; and (3) under normal circumstances, support a prevalence of hydrophytic vegetation." The 1987 U.S. Army Corps of Engineers Manual in Part II, item 24. states that, "The interaction of hydrology, vegetation, and soil results in the development of characteristics unique to wetlands. Therefore, the following technical guidelines for wetlands are based on the three parameters, and diagnostic environmental characteristics used in applying the technical guideline are represented by various indicators of these parameters." It is this premise by which SER ecologists has, in their professional judgment, delineated the wetlands on the subject parcel described in this report. Wetland Hydrology The most important wetland criterion is hydrology. The presence and persistence of water influences the vegetation types and changes soil morphology. Hydrology may be observed as standing water(inundation),or may be observed as freestanding water within the soil pit or auger hole (saturation) usually within the upper 12 inches. This is what would be considered primary hydrology indicators. Only one primary indicator is necessary to make the determination that wetland hydrology indeed exists. The 1987 Corps Manual also has a range of hydrologic zones established based on period of inundation or saturation. These zones and the periods of inundation or saturation for each can be observed in Table 1 below. Excerpted from the 1987 Manual,Hydrologic Zones—Nontidal Areas Zone Name Duration Comments Wetland or Not I Permanently Inundated 100% Inundation>6.6 ft.mean Not(Aquatic Habitat Zone,or Deep Water water depth Habitat Semipermanently To Nearly <75- Inundation defined as II Permanently Inundated Or <100% :!96.6 feet mean water Wetland Saturated depth III Regularly Inundated Or >25-75% Wetland Saturated IV Seasonally Inundated Or <12.5- Saturated 25% Wetland Irregularly Inundated or Many areas having these V y >5-12.5% hydrologic characteristics Wetland(if hydrophytic also s e t and hydric Saturated are not wetlands soils also present Intermittently Or Nevero Areas with these VI Inundated Or Saturated <5% hydrologic characteristics Not are not wetlands A-1 The definition of appropriate hydrology according to the 1987 Manual includes two important terms that must be clarified. First, the definition of a growing season is needed. The growing season is defined in the 1987 Manual as: "...the portion of the year when soil temperature (measured 19.7 inches below the surface) is above biological zero (5° C or 41° F)." According to the 1987 Manual this period of time can be approximated by using the"starting and ending dates for the growing season based on a 28° F air temperature threshold at a frequency of 5 years in 10." Based on this definition the growing season ranges approximately 160 days to 180 days in the Minneapolis/St.Paul metropolitan area(160 in the northern suburbs and greater to the south). Therefore, the required inundation or saturation to the surface for 5% of the growing season would be 8 or 9 consecutive days that ground water would need to be at the surface or saturated to the surface. The second term in the appropriate hydrology definition from the above paragraph to be clarified is "in most years". This means in 5 of 10 years hydrology must exist within a "jurisdictional wetland"for the 8 or 9 consecutive days of the growing season. This means that one observation date or even one whole year worth of detailed hydrology data may be deemed insufficient to determine if appropriate hydrology exists at a given location. In the event that precipitation events accumulate to above or below normal during just prior to a site visit or during a more intensive hydrology study,_the data may be confounded by non-normal circumstances and may be considered outside the bounds of "most years". Ideally, both antecedent soil moisture conditions and precipitation would be normal during all delineations. However, this is not a realistic impression of climate. Therefore, primary indicators of hydrology must be reviewed with scrutiny prior to determining if hydrology indeed exists. Wetland hydrology may be observed as standing water (inundation), or may be observed as freestanding water within a soil pit or auger hole (saturation)usually within the upper 12 inches. This is what would be considered primary hydrology indicators. Examination of this indicator requires digging a soil pit to a depth of 16 inches and observing the level at which water stands after sufficient time has been allowed for water to drain into the hole. The required time will vary depending on soil texture. This level represents the depth to the water table; the depth to saturated soils will always be nearer the surface due to the capillary fringe. According to the Hydrology criteria in the 1987 Delineation Manual, for soil saturation to impact vegetation, it must occur within a major portion of the root zone, typically within 12 inches of the surface. Only one primary indicator is necessary to make the determination that wetland hydrology is present. However, since a single observation is not enough evidence, based on the percentage of the growing season this inundation or saturation is required, these data are only valid when reviewed while also considering the abundance of recent precipitation events or the seasonal trend of climate when the site visit was made (this may be done through review of precipitation records where available). In addition to the primary indicators of wetland hydrology, there are secondary indicators (e.g. oxidized root channels, water-stained leaves, local soil survey data, FAC-Neutral test), of which two must be present to consider the sample point as having wetland hydrology. A-2 Hydrophytic Vegetation (Wetland Vegetation) Wetland vegetation is defined in the 1987 Manual as "The sum total of macrophytic plant life growing in water or on a substrate that is at least periodically deficient in oxygen as a result of excessive water content. When hydrophytic vegetation comprises a community where indicators of hydric soils and wetland hydrology also occur, the area has wetland vegetation." In more standard terms, some plants are more adapted to growing within inundated or saturated soil. Based on literature records and professional experience, a panel of experts compiled a list of plant species and assigned each a hydrophytic status (described below and includes five major classes of probability of a plant occurring within a wetland). In terms of delineation there is a gradient of plant species that are adapted to "growing in water or on substrate that is at least periodically deficient of oxygen". Fieldwork associated with wetland delineations includes a procedure (the 50/20 Rule, for determination of dominance), which is also outlined in the 1987 Manual, by which to determine if hydrophytic plant species dominate the vegetation at a given location. This procedure has been used for the wetland delineation at the subject parcel of this report. Hydric Soil Defined in the 1987 Manual as "A soil that is saturated, flooded, or ponded long enough during the growing season to develop anaerobic conditions that favor the growth and regeneration of hydrophytic vegetation. Hydric soils that occur in areas having positive indicators of hydrophytic vegetation and wetland hydrology are wetland soils." For the purposes of delineation of wetlands, soils cannot be viewed without digging pits or extracting soil using an auger. Therefore, transects of soil samples are taken from perceived upland to perceived wetlands along a transitional boundary. There are specific color indicators, textures, and depth requirements in the soil that are reviewed in order to determine whether hydric soils occur at a given point or not. After a transect of soil samples has been taken, upon consideration of vegetation and indicators of appropriate hydrology a working prototype for the given wetland is developed by the delineator. The wetland delineator then uses this working prototype to complete the location of the remainder of the wetland boundary, unless the wetland is large enough or the landscape features (vegetation or topography) change enough to warrant additional transect samples. A-3 Photo Log 3700 Northern Ave Orono MN f� Svo B o DA f; Ecological Resources 1 Providing the Sharper Edge in Natural Resources&Environmental Consulting t Facing 'Y 9tt A11100 r' a mi Pit e � "'�,+�t .. 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