We are pleased to present

We are pleased to present Zenk Farms 57 ± Acres Lowville Township, Murray County 80 ± Acres Lowville Township, Murray County 150 ± Acres Mason Township, Murray County 150.31 ± Acres Slayton Township, Murray County PARCEL 1 PARCEL 2 PARCEL 3 PARCEL 4 This property to be sold by Sealed Bid Auction Owner: Steve & Susan Zenk Revocable Trust Date & Time: Tuesday, February 6, 2018 @ 1:30 p.m. Location: Country Host, 3020 20th St., Slayton, MN 56172 Note: See Sealed Bid Information page in the back of this brochure for more details. Only registered bidders may attend. Must be registered prior to auction date. Listing Agent: Darrell Hylen, ALC Office: 507-345-LAND (5263) Toll Free: 800-730-LAND (5263) Direct: 507-381-3843 Auctioneer #07-17-01 Darrell.Hylen@WingertRealty.com www.wingertrealty.com

State Highway Map Minneapolis SUBJECT PROPERTY Slayton Mankato

Murray County Minnesota PARCELS 1 & 2 PARCEL 3 PARCEL 4

Lowville, Mason & Slayton Townships Murray County PARCEL 1 PARCEL 2 PARCEL 3 PARCEL 4 SLAYTON

FSA Aerial View-Parcel 1 PARCEL 1 BUILDING SITE NOT INCLUDED IN SALE

Property Information - Parcel 1 DESCRIPTION: TAX PID #: BUILDINGS: 57± Acres.N½ of NE¼ excluding approximately 25 ± ac building site in the NE¼ of NE¼. Legal survey to govern. Section 36, T107N-R42W (not to be used on legal documents) (Lowville Township, Murray County, Minnesota) 14-036-0010 (160 ± ac) None REAL ESTATE TAXES: 2017 Ag Hmstd taxes (160 ± ac) = $3,346 Special Assessments(included above)= $ 20 *This parcel is being split from a larger tract. The County Assessor will recalculate taxes attributed to each parcel after sale. *Beings parcel is being split from a larger tract, it constitutes a tax split. All 2017 taxes will be due and payable the day of closing. FSA INFORMATION: Total acres = 57 ± acres FSA Tillable acres = 56.3 ± acres Corn base acres = 54.7 ± acres Corn PLC Yield = 162 ± bushels 2014-2018 Farm Program Info - Enrolled into Agricultural Risk Coverage (ARC) County *This parcel is being split from a larger tract. FSA will recalculate Tillable acres, base acres, etc. attributed to each parcel after sale. SOIL DESCRIPTION: Poinsett, Waubay, Highpoint, Fulda. See Soils Map. CPI: Crop Productivity Index = 91.8 TOPOGRAPHY: DRAINAGE: Level to rolling See Tile Map. NRCS CLASSIFICATIONS ON TILLABLE ACRES: Exempt from conservation compliance provisions. NHEL - Non-Highly Erodible Land WINGERT REALTY & LAND SERVICES, INC. stipulates that they are representing the seller exclusively in this transaction. The information gathered for this brochure in its entirety is from sources deemed reliable, but cannot be guaranteed by Seller, Wingert Realty & Land Services, Inc., or its staff. Package is subject to prior sale, price change, correction or withdrawal. The buyer must make their own independent investigation of the property. The buyer is purchasing the property as is.

Tile Map - Parcel 1 This tile map is an approximation. No guarantee is made of tile condition, location, size, grade or depth. BUILDING SITE NOT INCLUDED IN SALE

Soils Map - Parcel 1

FSA Aerial View-Parcel 2 BUILDING SITE NOT INCLUDED IN SALE PARCEL 2

Property Information - Parcel 2 DESCRIPTION: TAX PID #: BUILDINGS: 80 ± Acres. S½ of NE¼ Legal survey to govern. Section 36, T107N-R42W (not to be used on legal documents) (Lowville Township, Murray County, Minnesota) 14-036-0010 (160 ± ac) None REAL ESTATE TAXES: 2017 Ag Hmstd taxes (160 ± ac) = $3,346 Special Assessments(included above)= $ 20 *This parcel is being split from a larger tract. The County Assessor will recalculate taxes attributed to each parcel after sale. *Beings parcel is being split from a larger tract, it constitutes a tax split. All 2017 taxes will be due and payable the day of closing. FSA INFORMATION: Total acres = 80 ± acres FSA Tillable acres = 78.56 ± acres Corn base acres = 76 ± acres Corn PLC Yield = 162 ± bushels 2014-2018 Farm Program Info - Enrolled into Agricultural Risk Coverage (ARC) County *This parcel is being split from a larger tract. FSA will recalculate Tillable acres, base acres, etc. attributed to each parcel after sale. SOIL DESCRIPTION: Fulda, Highpoint, Waubay, Bigstone, Pointsett, Marysland. See Soils Map. CPI: Crop Productivity Index = 89.6 TOPOGRAPHY: DRAINAGE: Level to rolling See Tile Map. NRCS CLASSIFICATIONS ON TILLABLE ACRES: Exempt from conservation compliance provisions. NHEL - Non-Highly Erodible Land WINGERT REALTY & LAND SERVICES, INC. stipulates that they are representing the seller exclusively in this transaction. The information gathered for this brochure in its entirety is from sources deemed reliable, but cannot be guaranteed by Seller, Wingert Realty & Land Services, Inc., or its staff. Package is subject to prior sale, price change, correction or withdrawal. The buyer must make their own independent investigation of the property. The buyer is purchasing the property as is.

Tile Map - Parcel 2 This tile map is an approximation. No guarantee is made of tile condition, location, size, grade or depth. BUILDING SITE NOT INCLUDED IN SALE

Soils Map - Parcel 2

FSA Aerial View-Parcel 3 BUILDING SITE NOT INCLUDED IN SALE

Property Information - Parcel 3 DESCRIPTION: TAX PID #: BUILDINGS: 150 ± Acres. SE¼ excluding approximately 10 ± ac building site Legal survey to govern. Section 31, T107N-R41W (not to be used on legal documents) (Mason Township, Murray County, Minnesota) 15-031-0030 (160 ± ac) None REAL ESTATE TAXES: 2017 Ag Hmstd taxes = $3,932 Special Assessments(included above)= $ 43.34 *This parcel is being split from a larger tract. The County Assessor will recalculate taxes attributed to each parcel after sale. *Beings parcel is being split from a larger tract, it constitutes a tax split. All 2017 taxes will be due and payable the day of closing. FSA INFORMATION: Total acres = 150 ± acres FSA Tillable acres = 143.94 ± acres Corn base acres = 141.89 ± acres Corn PLC Yield = 162 ± bushels 2014-2018 Farm Program Info - Enrolled into Agricultural Risk Coverage (ARC) County SOIL DESCRIPTION: Poinsett, Waubay, Vallers, Egeland, Scerdrup, Buse, Barnes, Arvilla, Parnell, Svea, Balaton. See Soils Map. CPI: Crop Productivity Index = 85.9 TOPOGRAPHY: DRAINAGE: Level to rolling Judicial Ditch # 15. 20,000 of tile with sock installed approximately 1978 in the 35 acre basin. Tile Map shown does not show all tile installed. See Tile Map. NRCS CLASSIFICATIONS ON TILLABLE ACRES: Exempt from conservation compliance provisions. NHEL - Non-Highly Erodible Land WINGERT REALTY & LAND SERVICES, ES, INC. stipulates that they are representing the seller exclusively in this transaction. The information gathered for this brochure in its entirety is from sources deemed reliable, but cannot be guaranteed by Seller, Wingert Realty & Land Services, Inc., or its staff. Package is subject to prior sale, price change, correction or withdrawal. The buyer must make their own independent investigation of the property. The buyer is purchasing the property as is.

Judicial Ditch # 15 Map - Parcel 3 This tile map is an approximation. No guarantee is made of tile condition, location, size, grade or depth. 30 Main PARCEL 2 26 15 6 8 6 12 30 14 10

Tile Map - Parcel 3 This tile map is an approximation. No guarantee is made of tile condition, location, size, grade or depth. 20,000 of tile with sock installed approximately 1978 in the 35 acre basin. Tile Map shown does not show all tile installed. BUILDING SITE NOT INCLUDED IN SALE

Soils Map - Parcel 3

FSA Aerial View-Parcel 4 BUILDING SITE NOT INCLUDED IN AUCTION. AVAILABLE VIA PRIVATE TREATY 12 ± ac Building Site available for sale at Private Treaty/ Negotiated sale. Not available at auction. Contact Darrell Hylen for more information, 507-381-3843.

Property Information - Parcel 4 DESCRIPTION: TAX PID #: BUILDINGS: 150.31 ± Acres. NE¼ less 12 ± acre building site, Comm 1702 South of NE corner. Legal survey to govern. Section 6, T106N-R41W (not to be used on legal documents) (Slayton Township, Murray County, Minnesota) 20-006-0011 (150.31 ± ac) None. 12 ± ac Building Site available for sale at Private Treaty/Negotiated sale. Contact Darrell Hylen for more information, 507-381-3843. REAL ESTATE TAXES: 2017 Ag Hmstd taxes = $2,136 Special Assessments(included above)= $ 15.84 FSA INFORMATION: Total acres = 150.31 ± acres FSA Tillable acres = 144.23 ± acres Corn base acres = 142.18 ± acres Corn PLC Yield = 162 ± bushels 2014-2018 Farm Program Info - Enrolled into Agricultural Risk Coverage (ARC) County SOIL DESCRIPTION: Poinsett, Waubay, Highpoint, Vallers, Sverdrup, Sandberg, Arvilla, Lakepark, Roliss, Parnell, Hokans, Svea, Egeland, Darmen, Renshaw, Fordville, Buse, Barnes, Parnell. See Soils Map. CPI: Crop Productivity Index = 84.3 TOPOGRAPHY: DRAINAGE: Level to rolling Judicial Ditch # 15. See Tile Map. NRCS CLASSIFICATIONS ON TILLABLE ACRES: Exempt from conservation compliance provisions. NHEL - Non-Highly Erodible Land WINGERT REALTY & LAND SERVICES, INC. stipulates that they are representing the seller exclusively in this transaction. The information gathered for this brochure in its entirety is from sources deemed reliable, but cannot be guaranteed by Seller, Wingert Realty & Land Services, Inc., or its staff. Package is subject to prior sale, price change, correction or withdrawal. The buyer must make their own independent investigation of the property. The buyer is purchasing the property as is.

Judicial Ditch # 15 Map - Parcel 4 This tile map is an approximation. No guarantee is made of tile condition, location, size, grade or depth. 30 Main 26 15 6 8 6 12 30 PARCEL 4 14 10

Tile Map - Parcel 4 This tile map is an approximation. No guarantee is made of tile condition, location, size, grade or depth. BUILDING SITE NOT INCLUDED IN SALE

Soils Map - Parcel 4

POINSETT SERIES - Soil # J195B The Poinsett series consists of very deep, well drained soils formed in silty glacial till on uplands. Permeability is moderate. Slopes range from 0 to 15 percent. Mean annual precipitation is about 23 inches, and mean annual air temperature is about 43 degrees F. TYPICAL PEDON: Poinsett silty clay loam - on a northeast facing, 3 percent slope in a cultivated field. When described the soil was moist throughout. GEOGRAPHIC SETTING: Poinsett soils are nearly level to gently rolling on uplands having plane to convex slopes with gradients of 0 to 9 percent. Poinsett soils formed in calcareous silty glacial till. Mean annual air temperature ranges from 38 to 48 degrees F, and mean annual precipitation ranges from 17 to 24 inches. Growing season is about 120 to 130 days; average growing season precipitation ranges from 15 to 18 inches; and growing degree days are about 2500 to 2900. Elevation ranges from 1000 to 2150 feet. Soil Descriptions GEOGRAPHIC SETTING: These soils have plane or slightly concave slopes with gradient of 0 to 2 percent on glacial moraines and lake plains. They formed in calcareous clayey glacial lacustrine or local alluvial sediments. Mean annual air temperature ranges from 40 to 44 degrees F. Mean annual precipitation ranges from 20 to 27 inches. Frost-free days range from 120 to 172. Elevation above sea level ranges from 990 to 1950. GEOGRAPHICALLY ASSOCIATED SOILS: Fulda soils are associated with the well drained Nutley soils, the moderately well drained Sinai soils, and the very poorly drained Dovray soils, which are members of a hydrosequence with the Fulda soils. The silty, well drained Poinsett soils and the moderately well drained Waubay soils are in the nearby uplands in some places. DRAINAGE AND PERMEABILITY: Poorly drained. Surface runoff and internal drainage are slow. Permeability is slow. A perched water table occurs in most years at depths of 1 to 3 feet from October to June. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Barnes, Forman, Heimdal, Oldham, Parnell, Sinai and Waubay soils. Barnes soils are fine-loamy and are on adjacent upland slopes. Forman soils have argillic horizons and are on adjacent slopes. Heimdal soils are coarse-loamy and are on similar landscape positions as the Poinsett soils. Waubay soils have mollic epipedons more than 16 inches thick and are in swales and shallow drainageways. Oldham, Parnell, and Sinai soils have fine textured control sections. In addition, the Oldham and Parnell soils are more poorly drained and are in depressions. Sinai soils are on somewhat higher lying ice-walled lake positions in the silty glacial drift landscape. DRAINAGE AND PERMEABILITY: Well drained. Surface runoff is low or medium. Permeability is moderate. WAUBAY SERIES - Soil # J195B, J256A The Waubay series consists of very deep, moderately well drained soils formed in local silty glacialfluvial deposits on flats or footslopes, in slight depressions and in swales. These soils have moderate permeability. Slopes range from 0 to 6 percent. Mean annual precipitation is about 21 inches, and mean annual temperature is about 42 degrees F. TYPICAL PEDON: Waubay silt loam - under cultivation. GEOGRAPHIC SETTING: Waubay soils are level to gently sloping and are in slight depressions and swales, and on flats and footslopes on uplands. Slopes are plane or concave with gradients of 0 to 6 percent. The soils formed in calcareous silty glacialfluvial deposits. Mean annual temperature ranges from 42 to 48 degrees F, and mean annual precipitation ranges from 17 to 26 inches. Growing season is about 120 to 160 days; average growing season precipitation ranges from 15 to 18 inches; and growing degree days are about 2500 to 3000. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Barnes, Buse, Forman, Oldham, Parnell, and Poinsett soils. Barnes, Buse, and Forman soils are fine-loamy. Poinsett soils have mollic colors less than 16 inches thick. Barnes, Buse, Forman, and Poinsett soils are on convex slopes above the Waubay soils. Oldham and Parnell soils have a fine textured control section and are in the deeper swales and depressions. DRAINAGE AND PERMEABILITY: Moderately well drained. Areas in swales receive additional moisture as run-in from adjacent soils. Runoff is low or medium. Permeability is moderate. A temporary water table is at a depth ranging from 3.5 to 5 feet in the spring of most years. FULDA SERIES - Soil # J199A The Fulda series consists of very deep, poorly drained soils that formed in lacustrine or local alluvial sediments on glacial lake plains and moraines. These soils have slow permeability. They have slopes of 0 to 2 percent. Mean annual precipitation is about 24 inches. Mean annual air temperature is about 44 degrees F. TYPICAL PEDON: Fulda silty clay loam with a plane slope on an icewalled lake plain in a cultivated field. BIGSTONE SERIES - Soil # J32A The Bigstone series consists of very deep, very poorly drained soils that formed in calcareous, local alluvial sediments and the underlying calcareous loamy glacial till in depressions on till plains. These soils have moderately slow or moderate permeability. Their slopes range from 0 to 1 percent. Mean annual air temperature is about 44 degrees F. Mean annual precipitation is about 26 inches. TYPICAL PEDON: Bigstone silt loam on a slope of less than 1 percent in a depression on a till plain. GEOGRAPHIC SETTING: The Bigstone soils have plane or concave slopes ranging from 0 to 1 percent in depressions on till plains. They have primarily formed in calcareous local alluvium and the underlying calcareous, glacial till. Mean annual air temperature ranges from 40 to 44 degrees F. Mean annual precipitation ranges from 24 to 27 inches. The frost-free days range from 120 to 172. The elevation above sea level ranges from 990 to 1950 feet. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Esmond, Flom, Fram, Hamerly, Heimdal, Lakepark, Svea, and Vallers. The well drained Esmond and Heimdal soils are on adjacent uplands. The moderately well drained and somewhat poorly drained Fram, Hamerly, and Svea soils are on low convex rises, concave foot slopes, and side slopes. The poorly drained Lakepark and Vallers soils are in drainageways and on flats. DRAINAGE AND PERMEABILITY: Very poorly drained. Runoff is very slow or ponded. Permeability is moderately slow or moderate. The apparent seasonal high water table is at depths of 1 foot above to 1 foot below the surface. A ponded phase is recognized with the water table at 0 to 3 feet above the surface in most years. MARYSLAND SERIES - Soil # J12A The Marysland series consists of very deep, poorly and very poorly drained soils that formed in glacial lacustrine, alluvium or outwash sediments which consists of a 20 to 40 inch loamy mantle over sandy or sandy-skeletal sediments. These soils are on stream terraces, outwash channels, outwash plains, flood plains and lake plains. They have moderate permeability in the upper part and rapid permeability in the underlying material. Slopes range from 0 to 2 percent. Mean annual temperature is about 43 degrees F. Mean annual precipitation is about 22 inches. TYPICAL PEDON: Marysland loam with a plane level slope on a glacial lake plain in a meadow. GEOGRAPHIC SETTING: The Marysland soils have plane, slightly concave, or slightly convex slopes. They formed in glacial lacustrine, alluvium or outwash with a 20 to 40 inch upper loamy mantle over sandy and gravelly sediment in drainageways and flats on glacial stream terraces, outwash channels, outwash plains, outwash plains, flood plains and lake plains. Slopes range from 0 to 2 percent. Mean annual temperature ranges from about 38 to 45 degrees F. Mean annual precipitation ranges from 18 to 24 inches. Frostfree days range from 100 to 150. Elevation above sea level ranges from 800 to 2350 feet.

Soil Descriptions GEOGRAPHICALLY ASSOCIATED SOILS: These are the Renshaw, Fordville, Spottswood, and Divide soils which are members of a hydrosequence with the Marysland soils. The Renshaw and Fordville soils are well drained and are on higher lying or more sloping terrain. The Spottswood and Divide soils are moderately well and somewhat poorly drained. The Spottswood soils have plane or slightly concave slopes and lack a calcic horizon at shallow depths. The Divide soils have plane or slightly convex slopes. DRAINAGE AND PERMEABILITY: Poorly and very poorly drained. Runoff is slow. Permeability is moderate in the upper loamy mantle and rapid in the 2C horizon. Depth to an apparent seasonal high water table is as high as.5 to 1.5 feet at some time from November through July in most years for the poorly drained phase. The very poorly drained phase has an apparent high water table at depths of +1.0 to 1.0 feet during January to December in most years. GEOGRAPHIC SETTING: Egeland soils are on terraces, outwash plains, and uplands. Slope gradients typically are less than 6 percent, but range from 0 to 20 percent. Egeland soils formed in moderately coarse-textured glaciofluvial deposits and sandy materials of fans and beaches of lake plains. Mean annual air temperature ranges from about 36 to 48 degrees F, and mean annual precipitation ranges from 15 to 24 inches. Growing season is 120 to 155 days; average growing season precipitation ranges from 15 to 20 inches; and growing degree days are about 2500 to 3500. GEOGRAPHICALLY ASSOCIATED SOILS: These are the competing Heimdal soils and the Arvilla, Eckman, Embden, Fordville, Forman, Maddock, Peever, Poinsett, Renshaw and Swenoda soils. The Arvilla, Eckman, Heimdal, and Maddock soils are on similar nearby landscapes. Arvilla soils have sand and gravel below depths of 14 and 25 inches. Eckman soils have a coarse-silty particle size control section. Maddock soils have a sandy particle size control section. Embden and Swenoda soils are on foot slopes below the Egeland soils. They have mollic epipedons more than 16 inches thick. Fordville and Renshaw soils are on nearby terraces and outwash plains. They are fine-loamy over sand and gravel. The Forman, Peever, and Poinsett soils are on nearby glacial till plains. Forman and Peever soils have an argillic horizon. Poinsett soils have a fine-silty series control section. VALLERS SERIES - Soil # J11A The Vallers series consists of very deep, poorly drained soils that formed in calcareous fine-loamy till on till plains, moraines and lake plains. These soils have moderately slow permeability. Slopes range from 0 to 3 percent. Mean annual precipitation is about 22 inches, and mean annual air temperature is about 43 degrees F. TYPICAL PEDON: Vallers loam, on a plane slope on a glacial moraine in cropland. GEOGRAPHIC SETTING: The Vallers soils are on level and nearly level slight rises, shallow depressions and drainageways of till plains, moraines and lake plains. They are on slightly concave to slightly convex slopes with gradient of 0 to 3 percent. These soils formed in fine-loamy, calcareous till of Late Wisconsinan Age. In some areas, these soils have a silty lacustrine mantle as much as 24 inches thick. The mean annual air temperature is about 32 to 45 degrees F, and the mean annual precipitation is about 12 to 26 inches. Frost-free period ranges from 90 to 150 days. Elevation ranges from 650 to 2350 feet. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Langhei, Barnes, Forman, Formdale, Svea, Hamerly, Parnell and Quam soils in a hydrosequence with the Vallers soils on till plains and moraines; and the Roliss, Kratka, Strathcona and Hamre soils on lake plains. The somewhat excessively drained Langhei soils; the well drained Barnes, Forman,and Formdale soils; the moderately well drained Svea soils; and the somewhat poorly drained Hamerly soils are on higher lying or more sloping terrain. The very poorly drained Parnell and Quam soils are in depressions. The Roliss soils do not have a calcic horizon. The Kratka and Strathcona soils have 20 to 40 inches of sandy materials in the upper part. The Hamre soils are on lower lying areas and have a histic epipedon. DRAINAGE AND PERMEABILITY: Poorly drained. Runoff is negligible to low. Permeability is moderately slow. An apparent seasonal high water table is at a depth of 0.5 to 1.5 feet at some time during the period of March through July. EGELAND SERIES - Soil # J8A, J8B The Egeland series consists of very deep, well drained soils formed in glaciofluvial deposits. These soils are on terraces, outwash plains, and uplands. They have moderately rapid permeability. Slopes range from 0 to 20 percent. Mean annual air precipitation is about 22 inches, and mean annual temperature is about 44 degrees F. TYPICAL PEDON: Egeland sandy loam - on a northeast-facing convex slope of 3 percent in cultivation. When described, the soil was moist throughout. DRAINAGE AND PERMEABILITY: Well drained. Surface runoff ranges from negligible to low depending on slope. Permeability is moderately rapid. SVERDRUP SERIES - Soil # J7B The Sverdrup series consists of very deep, well drained soils that formed in glacial outwash deposits consisting of a loamy mantle and underlying sandy deposits. These soils have moderately rapid permeability in the upper part and rapid permeability in the lower part. These soils are on outwash plains, terraces, and moraines. They have slopes of 0 to 18 percent. Mean annual temperature is 43 degrees F. Mean annual precipitation is 22 inches. TYPICAL PEDON: Sverdrup sandy loam with a plane slope of 2 percent on a glacial outwash plain in a cultivated field. GEOGRAPHIC SETTING: The Sverdrup soils have plane or convex slopes on glacial moraines, terraces, and outwash plains. The slopes are commonly short, and the range is 0 to 18 percent. These soils formed in calcareous, coarse-loamy and sandy glacial outwash. The mean annual temperature is 40 to 45 degrees F. The mean annual precipitation is 20 to 26 inches. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Clontarf, Malachy, and Arveson soils, which formed in sediments similar to those of Sverdrup soils and are members of a drainage sequence with those soils. Moderately well drained Clontarf and moderately well and somewhat poorly drained Malachy soils have a thicker mollic epipedon and are on lower- lying terrain. Also, Malachy soils are calcareous in all parts. Poorly and very poorly drained Arveson soils are in nearby level areas and depressions and have a calcic horizon beginning within depths of 16 inches. DRAINAGE AND PERMEABILITY: Well drained. Surface runoff is slow or medium. Permeability is moderately rapid in the upper part and rapid permeability in the lower part. BUSE SERIES - Soil # J235C2 Complex, J96C2 Complex, J106B Complex The Buse series consists of very deep, well drained soils that formed in loamy glacial till on moraines. These soils have moderate and moderately slow permeability. They have slopes of 3 to 60 percent. Mean annual precipitation is about 22 inches. Mean annual air temperature is about 42 degrees F. TYPICAL PEDON: Buse loam with a convex slope of 5 percent on a glacial moraine in a cultivated field. GEOGRAPHIC SETTING: The Buse soils have slightly to strongly convex slopes in glacial moraines. Slope gradient ranges from 3 to 60 percent. The Buse soils formed in calcareous till of the Wisconsinan Age. Mean annual air temperature is about 36 to 45 degrees F. Mean annual precipitation is about 16 to 24 inches. Frost free days are 120 to 150 days. Elevation above sea level ranges from 1,000 to 1,600 feet. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Aastad, Aazdahl, Barnes, Flom, Forman, Formdale, Hamerly, Langhei, Sioux, Svea, Vienna, and Waukon soils. Aastad and Svea soils have cambic horizons and

thicker mollic epipedons. Barnes, Flom, Forman, Vienna and Waukon soils have Bw or Bt horizons, thicker sola and lack free calcium carbonate in the upper part of solum. Hamerly soils have calcic horizons and have lower chroma in the upper part of the C horizon. Langhei soils do not have a mollic epipedon. Sioux soils are coarse textured and excessively drained. Soil Descriptions In addition Fordville soils are pachic. DRAINAGE AND PERMEABILITY: Somewhat excessively drained. Runoff is slow to rapid. Permeability is moderately rapid in the upper part and rapid or very rapid in the underlying material. DRAINAGE AND PERMEABILITY: Well drained. Surface runoff is moderately low on the lesser slopes and very high on steep slopes. Permeability is moderate or moderately slow. BARNES SERIES - Soil # J235C2 Complex, J96C2, J106B The Barnes series consists of very deep, well drained, moderately or moderately slowly permeable soils that formed in loamy till. These soils are on till plains and moraines and have slopes ranging from 0 to 25 percent. Mean annual air temperature is about 42 degrees F, and mean annual precipitation is about 17 inches. TYPICAL PEDON: Barnes loam in a cultivated field. GEOGRAPHIC SETTING: Barnes soils are on level to hilly till plains and moraines. Slope gradients typically are 2 to 6 percent, but range from 0 to 25 percent. The soils formed in loamy till. The climate is cool subhumid with a mean annual air temperature of 36 to 48 degrees F, and mean annual precipitation of 15 to 25 inches. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Aastad, Buse, Forman, Hamerly, Langhei, Parnell, Svea and Tonka soils. Aastad and Svea soils are on concave and nearly level positions. They have mollic epipedons more than 16 inches thick. Buse and Langhei soils are on steeper convex slopes. Buse soils do not have a cambic horizon. Langhei soils do not have mollic epipedons. Forman soils are on similar positions to Barnes. They have an argillic horizon. Hamerly, Parnell and Tonka soils are on lower lying foot slopes and flats, and in depressions. They are wetter and have water tables at or near the surface. DRAINAGE AND PERMEABILITY: Well drained. Runoff ranges from negligible to high depending on the slope. Moderately slow or moderate permeability. ARVILLA SERIES - Soil # J235C2 Complex, J42C Complex The Arvilla series consists of very deep, somewhat excessively drained soils formed in moderately coarse textured glacial outwash and the underlying sand and gravel on glacial lake beaches, stream valley terraces and outwash plains. These soils have moderately rapid permeability in the upper part and rapid or very rapid permeability in the underlying material. Slopes range from 0 to 25 percent. Mean annual air temperature is 42 degrees F, and mean annual precipitation is 18 inches. TYPICAL PEDON: Arvilla sandy loam on a level east facing slope in a cultivated field. When described the soil was moist throughout. GEOGRAPHIC SETTING: Arvilla soils are on level to moderately steep outwash plains, beach areas of glacial lakes, and terraces of glacial stream valleys. Slope gradients are commonly 1 to 5 percent, but range from 0 to 25 percent. The soils formed in a thin mantle of sandy loam alluvium underlain by thick beds of loose sand and gravel. The climate is cool, subhumid with a mean annual air temperature ranging from 36 to 48 degrees F, and a mean annual precipitation ranging from 15 to 24 inches. Three-fourths of the rainfall is in the spring and summer. GEOGRAPHICALLY ASSOCIATED SOILS: These are the competing Maddock and Sioux soils and the Divide, Fordville, Osakis, Renshaw and Wyrene soils. Divide and Wyrene soils have a calcic horizon within a depth of 16 inches. Osakis soils have mottling within depths of 40 inches. The Divide, Osakis and Wyrene soils are on lower level and slight concave depressions in the outwash plains. Sioux soils are on the steeper hills and ridges. Fordville and Renshaw soils have more than 18 percent clay in the upper part. SVEA SERIES - Soil # J106B Complex, J101B Complex, J104A The Svea series consists of very deep, well or moderately well drained soils that formed in calcareous glacial till and local alluvium from the till. Permeability is moderate in the solum and moderate or moderately slow in the C horizon. These soils are on concave positions on glacial till plains and have slopes ranging from 0 to 25 percent. Mean annual air temperature is 42 degrees F, and mean annual precipitation is 20 inches. TYPICAL PEDON: Svea loam - on a concave slope of less than 2 percent under cropland. When described, the soil was moist throughout. GEOGRAPHIC SETTING: Svea soils are on level to moderately steep and slightly concave positions on glacial till plains. Slope gradients commonly are less than 3 percent but range from 0 to 25 percent. The soils formed in calcareous glacial till and local alluvium from the till. The climate is cool subhumid. Mean annual air temperature ranges from 36 to 48 degrees F, and mean annual precipitation from 15 to 24 inches. Most of the moisture falls in the spring and summer. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Barnes, Buse, Hamerly, Hamlet, Langhei, Parnell, Quam and Tonka soils. Barnes soils are on convex and plane, well drained nearby areas and Hamlet soils are on nearby similar positions as Svea. They have mollic epipedons less than 16 inches thick. Buse and Langhei soils are on convex crests of steeper hills. They do not have cambic horizons. Hamerly soils are on slightly convex and smooth lower slopes on nearby areas surrounding depressions. They have calcic horizons within depths of 16 inches. Parnell, Quam and Tonka soils are in poor and very poorly drained depressions. They have an aquic moisture regime. In addition, Parnell and Tonka soils are fine and Quam soils are fine-silty. DRAINAGE AND PERMEABILITY: Well or moderately well drained. Svea soils receive some runoff from higher parts of the landscape. Runoff is negligible to high depending on slope. Permeability is moderate in the solum and moderate or moderately slow in the C horizon. A seasonal high water table is at depths of 3 to 5 feet at some time during the period of April through June in the moderately well drained phase. It is at a depth of 4 to more than 6 feet for the same period in the well drained phase. HOKANS SERIES - Soil # J101B Complex The Hokans series consists of very deep, well drained, moderately or moderately slowly permeable soils that formed in loamy glacial till. These soils are on till plains and moraines and have slopes ranging from 1 to 6 percent. Mean annual air temperature is about 44 degrees F, and mean annual precipitation is about 25 inches. TYPICAL PEDON: Hokans loam, in a cultivated field. GEOGRAPHIC SETTING: Hokans soils are on nearly level to gently undulating till plains and moraines. Slope gradients are 1 to 6 percent. The soils formed in loamy glacial till. The mean annual air temperature is 38 to 45 degrees F. and the mean annual precipitation is 22 to 29 inches. Frost-free period ranges from 120 to 160 days. Elevation is 990 to 1950 feet above sea level. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Balaton, Buse, Langhei, Parnell, and Vallers soils. Buse and Langhei soils are on steeper convex slopes. Balaton, Vallers and Parnell soils are on lower lying foot slopes and flats, and in depressions. They are wetter and have soil saturation at a shallower depth. DRAINAGE AND PERMEABILITY: Well drained. These soils have a sea-

Soil Descriptions sonally high water table between 48 and 72 inches in normal years. Moderately slow or moderate permeability. BALATON SERIES - Soil # J57A The Balaton series consists of very deep, moderately well drained soils that formed in calcareous loamy glacial till. Permeability is moderate. These soils are on moraines and till plains. They have slopes ranging from 1 to 6 percent. Mean annual air temperature is about 43 degrees F., and mean annual precipitation is about 22 inches. TYPICAL PEDON: Balaton loam with a convex 2 percent slope on the summit of a low knoll on a glacial moraine in a cultivated field. GEOGRAPHIC SETTING: Balaton soils are on low knolls on moraines and till plains. Slopes are short and convex, commonly having gradients of less than 3 percent but range to 6 percent. The soil is formed in calcareous, loamy glacial till of the Wisconsin Age. Mean annual air temperature ranges from 38 to 45 degrees F, and mean annual precipitation ranges from 19 to 27 inches. The frost free days range from 120 to 170 days. The elevation above sea level ranges from 850 to 1950 feet. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Barnes, Buse, Parnell, Svea, Vallers and Tonka soils which are members of a hydrosequence with the Balaton soils. The well drained Barnes and Buse soils are on higher landscape positions. The moderately well drained Svea soils are in concave swales and flats. The very poorly drained Parnell and poorly drained Tonka soils are in depressions. The poorly drained Vallers soils are on flats and rims of depressions. DRAINAGE AND PERMEABILITY: Moderately well drained. Surface runoff is low. Permeability is moderate. The seasonal high water table is at a depth of 2.5 to 4.0 feet at some time during the period March through June in most years. SANDBERG SERIES - Soil # J42C Complex The Sandberg Series consists of very deep, excessively drained soils that formed in coarse or moderately coarse glacial outwash sediments or glacial beach deposits with or without a thin loamy mantle. These soils are on outwash plains, glacial lake beaches, stream terraces valley trains, and glacial moraines. Permeability is moderately rapid or rapid in the upper part and very rapid in the lower part. Slopes range from 0 to 45 percent. Mean annual air temperature is about 42 degrees F. Mean annual precipitation is about 23 inches. TYPICAL PEDON: Sandberg loamy sand with a 4 percent convex northeast facing slope in a cultivated field. GEOGRAPHIC SETTING: Sandberg soils are on outwash plains, glacial beach ridges, valley trains, stream terraces and glacial moraines. Slopes range from 0 to 45 percent. They formed in sandy and gravelly outwash sediments or glacial beach deposits with or without a thin loamy upper mantle. These sediments are late Wisconsin in age. The mean annual temperature ranges from 37 to 45 degrees F. Mean annual precipitation ranges from 19 to 28 inches. About 80 percent of the precipitation falls during the growing season. The frost-free days range from 90 to 145. The elevation ranges from 800 to 2000 feet above sea level. GEOGRAPHICALLY ASSOCIATED SOILS: These are Arvilla, Clontarf, Dorset, Flaming, Forada, Fordville, Mavie, Osakis, Radium, Sverdrup, and Syrene soils. Forada, Mavie, and Syrene soils are poorly and very poorly drained and in lower lying positions. Clontarf, Flaming, Osakis, and Radium soils are moderately well drained and in nearby deeply set concave swales and on lower lying flats. Arvilla, Dorset, and Sverdrup soils are on slightly lower landscape positions and have thicker loamy mantles. The well drained Fordville soils are in nearby shallow swales and have a thicker loamy mantle. Sandberg soils are occasionally associated with glacial till soils. DRAINAGE AND PERMEABILITY: Excessively drained. Surface runoff is slow to rapid. Permeability is moderately rapid or rapid in the upper part and very rapid in the lower part. LAKEPARK SERIES - Soil # J107A Complex The Lakepark series consists of very deep, poorly drained soils that formed in loamy colluvium from glacial drift and underlying loamy glacial till on till plains and moraines. These soils have moderately slow permeability. Slopes range from 1 to 3 percent. Mean annual air temperature is about 42 degrees F. Mean annual precipitation is about 24 inches. TYPICAL PEDON: Lakepark clay loam with a 1 percent concave slope in a cultivated field. GEOGRAPHIC SETTING: Lakepark soils are on lower footslopes and toeslopes of head and sideslopes on glacial moraines and till plains. Slopes are plane or concave with 1 to 3 percent gradients. These soils formed in loamy colluvium derived from glacial drift and underlying loamy glacial till. Mean annual air temperature ranges from 38 to 45 degrees F, and mean annual precipitation ranges from 22 to 28 inches. Frost free days range from 90 to 140. Elevation above sea level ranges from 900 to 1800 feet. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Langhei, Formdale, Barnes, Aazdahl, Flom and Quam soils. Langhei, Formdale and Barnes soils are well drained and are on steeper slopes. Aazdahl soils are moderately well drained and are higher lying. Flom soils are poorly drained soils and have mollic epipedons less than 24 inches thick. Quam soils are very poorly drained and are in depressions. DRAINAGE AND PERMEABILITY: Poorly drained. Runoff is slow. Permeability is moderately slow. The apparent seasonal high water table is at a depth of.5 to 1.5 feet from November to June in most years. ROLISS SERIES - Soil # J107A Complex The Roliss series consists of very deep, poorly and very poorly drained soils formed in loamy calcareous till on lake plains and moraines. Permeability is moderate or moderately slow. Slopes are 0 to 2 percent. Mean annual air temperature is 41 degrees F. Mean annual precipitation is 22 inches. TYPICAL PEDON: Roliss loam with a plane north facing slope of less than 1 percent on a lake plain in a cultivated field. GEOGRAPHIC SETTING: The Roliss soils are on plane and slightly concave positions primarily on lake plains. They also occur on moraines. Slopes are 0 to 2 percent. They formed in calcareous till on lake plains. The mean annual air temperature ranges from 36 to 45 degrees F. Mean annual precipitation ranges from 19 to 27 inches. Frost-free days range from 88 to 150. Elevation above sea level ranges from 785 to 1950 feet. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Foxhome, Hamerly, Kittson, Mavie, Rockwell and Vallers soils. Foxhome and Kittson soils are moderately well drained and are on higher lying terrain. Hamerly soils are somewhat poorly drained and have a calcic horizon above a depth of 16 inches. Mavie, Rockwell and Vallers soils have similar drainage but have a calcic horizon above depths of 16 inches. DRAINAGE AND PERMEABILITY: Poorly and very poorly drained. Runoff is negligible or low. Permeability is moderate or moderately slow. Depth to an apparent seasonal high water table is 0.5 to 1.5 feet at some time from April to July for the poorly drained phase and plus 1.0 to 0.5 foot from March to July for the very poorly drained phase. PARNELL SERIES - Soil # J107A Complex, J1A The Parnell series consists of very deep, very poorly drained and poorly drained soils that formed in water-sorted sediments from glacial drift in depressions, swales and drainageways on glacial moraines. These soils have slow permeability. Slopes range from 0 to 3 percent. Mean annual precipitation is about 20 inches; and mean annual air temperature is about 41 degrees F. TYPICAL PEDON: Parnell silty clay loam with a nearly level slightly concave slope in a depression in a glacial moraine. GEOGRAPHIC SETTING: Parnell soils are in depressions, swales and

drainageways on ground and end moraines. Slope gradients are 0 to 3 percent. Parnell soils formed mostly in water-sorted sediments from glacial till. Calcareous loam or clay loam glacial till commonly underlies these sediments. Mean annual air temperature is 38 to 45 degrees F. Mean annual precipitation is 16 to 24 inches thick. Frost-free days range from 120 to 160 days. Elevation above sea level ranges from 1000 to 1600 feet. Soil Descriptions underlain by thick beds of sand and gravel. Mean annual temperature ranges from 36 to 48 degrees F, and mean annual precipitation ranges from 15 to 28 inches, most of which falls in spring and summer. Growing season is about 100 to 165 days; average growing season precipitation ranges from 15 to 28 inches; growing degree days are about 2400 to 3000. Elevation above sea level ranges from 650 to 2350 feet. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Aastad, Aazdahl, Badger, Balaton, Barnes, Flom, Forman, Formdale, Hamerly, Poinsett, Svea, Vallers and Waukon soils. These soils formed in loamy glacial till and are on higher lying or more sloping terrain or both. Aastad, Aazdahl, Balaton and Svea soils are moderately well drained; Badger and Hamerly soils are somewhat poorly drained; Barnes, Forman, Formdale, Poinsett and Waukon soils are well drained; and Flom and Vallers soils are poorly drained. DRAINAGE AND PERMEABILITY: Very poorly drained and poorly drained. Surface runoff is very low on the poorly drained phase and ponded on the very poorly drained phase. Permeability is slow. In most years a seasonal high water table is at a depth of 0.5 to 1.5 feet during the period November to June for the poorly drained phase and +1 to.5 during the period January to December for the very poorly drained phase. DARNEN SERIES - Soil # J26B The Darnen series consists of very deep, moderately well drained and well drained soils that formed in loamy colluvial-alluvial sediments from glacial drift on glacial moraines. These soils have slopes of 0 to 6 percent. They have moderate permeability. Mean annual temperature is about 43 degrees F. Mean annual precipitation is about 22 inches. TYPICAL PEDON: Darnen loam on a 3 percent concave footslope at the base of the bluffs of a small river valley; ground moraine; cultivated field. GEOGRAPHIC SETTING: These soils are on nearly level to gently sloping foot slopes or toe slopes on glacial moraines. Slope gradients range from 0 to 6 percent. The soil formed in loamy, colluvial-alluvial sediments derived from loamy glacial till or drift. The mean annual temperature ranges from 40 to 46 degrees F. The mean annual precipitation is 18 to 24 inches. The frost-free days range from 90 to 150 days. Elevation above sea level is 670 to 1400 feet. GEOGRAPHICALLY ASSOCIATED SOILS: These are the well drained Buse, Langhei and Barnes soils. The Barnes, Langhei and Buse soils are upland soils formed in glacial till, and they are on slopes above the Darnen soils. In some places they are associated with moderately well drained Svea, poorly drained Flom and very poorly drained Quam soils. DRAINAGE AND PERMEABILITY: Moderately well and well drained. Permeability is moderate. Surface runoff is medium. Depth to an apparent seasonal water table is 2.5 to 6 feet at some time from November to June in most years. RENSHAW SERIES - Soil # J75B The Renshaw series consists of very deep, somewhat excessively drained soils formed in loamy sediments and the underlying sand and gravel on outwash plains and terraces. Permeability is moderate in the upper part and very rapid in the underlying material. Slopes range from 0 to 25 percent. Mean annual precipitation is about 22 inches and mean annual air temperature is about 43 degrees F. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Divide, Fordville, Sioux, and Spottswood. The Divide soils have a calcic horizon and are in the lower positions in the landscape adjacent to swales and depressions. Fordville and Spottswood soils have a mollic epipedon more than 16 inches thick. Fordville and Spottswood soils are on similar landscapes. Sioux soils have sand and gravel at depths less than 14 inches and are on steeper convex slopes. DRAINAGE AND PERMEABILITY: Somewhat excessively drained. Runoff is negligible to low depending on slope. Permeability is moderate in the upper part and very rapid in the underlying material. FORDVILLE SERIES - Soil # J75B The Fordville series consists of very deep, well drained soils formed in loamy sediments that are moderately deep over sand and gravel on outwash plains, terraces, and flood plains. Permeability is moderate in the solum and very rapid in the underlying sand and gravel. Slopes range from 0 to 9 percent. Mean annual precipitation is about 22 inches, and mean annual temperature is 41 degrees F. TYPICAL PEDON: Fordville loam - on a plane slope of 1 percent in a cultivated field. When described the soil was dry throughout. GEOGRAPHIC SETTING: Fordville soils are on outwash plains, terraces, and flood plains of streams that dissect the glacial till plains. Surfaces are plane to convex. Slope gradients range from 0 to 9 percent. The soil formed in loamy alluvium over stratified sand and gravel. Mean annual temperature ranges from 38 to 48 degrees F, and mean annual precipitation ranges from 16 to 24 inches. The growing season is about 120 to 140 days; the average growing season precipitation ranges from 13 to 17 inches. The growing degree days are about 2500 to 3000. GEOGRAPHICALLY ASSOCIATED SOILS: This is the competing Spottswood series and the Divide, Marysland, Renshaw, and Sioux soils. Spottswood, Divide, and Marysland soils are on lower and wetter parts of the outwash plains and terraces. Renshaw soils have a mollic epipedon less than 16 inches thick, are shallow to gravel, and are on slightly higher positions. Divide and Marysland soils have calcic horizons within depths of 16 inches. Sioux soils have sand and gravel at depths of less than 14 inches and are higher convex positions. DRAINAGE AND PERMEABILITY: Well drained. Surface runoff is medium or low. Permeability is moderate in the solum and very rapid in the underlying sand and gravel. Soils on flood plains are flooded for short periods. TYPICAL PEDON: Renshaw loam - on a plane slope of less than 1 percent in a cultivated field. When described the soil was dry throughout. GEOGRAPHIC SETTING: Renshaw soils are nearly level to moderately steep on outwash plains, glacial stream terraces, flood plains, and terrace escarpments. Slope gradients typically are less than 6 percent but range from 0 to 25 percent. Renshaw soils formed in a thin layer of loamy alluvium

SEALED BID AUCTION INSTRUCTIONS Sealed Bid Location and Time: Country Host, 3020 20th St. Slayton, MN 56172 Tuesday, February 6, 2018 @ 1:30 p.m. Sealed Bid Instructions: 1. Only registered bidders may attend. Must be registered prior to auction date. All potential bidders shall deliver or mail a sealed bid, postmarked by Wednesday, January 31, 2018 to: Wingert Realty & Land Services, Inc., Attn: Darrell Hylen 1160 Victory Drive So., Suite 6, Mankato, MN 56001 If you are unable to get postmarked bid in on time, call our office for other arrangements. 2. All bids must be accompanied by a $5,000 check for earnest money made out to Wingert Realty Trust Account. 3. The written bid shall state the total price for total deeded acres. 4. All persons submitting a written bid will be allowed to raise their bid after all bids have been opened. 5. The premises described herein will be sold in as is, where is condition 6. Seller shall pay the real estate taxes and special assessments due and payable in 2017, and receive 2017 income. 7. Purchaser shall pay the real estate taxes and special assessments due and payable in 2018 and beyond. 8. The successful bidder or bidders will enter into a Purchase Agreement and shall pay as earnest money 10% of the successful bid on the day of auction. 9. A 2% Buyer Premium will be added to the final bid price to arrive at the final contract price. 10. The entire balance of the purchase price, without interest, will be due and payable on Tuesday, March 6, 2018 at which time possession and marketable title shall be conveyed. 11. All checks will be returned to unsuccessful bidder. 12. The Sellers reserve the right to reject any and all bids and to waive any irregularities in the bidding. 13. Announcements made the day of the auction take precedence over written material. For additional information, contact: Wingert Realty & Land Services, Inc. Darrell Hylen, ALC, Auctioneer #07-17-01 (800) 730-LAND (5263), 507-345-LAND (5263) or 507-381-3843 Direct

REGISTRATION / BIDDING FORM Bid Submitting Instructions: Write in your total price for total deeded acres for each parcel you would like to bid on Write in your name, address, telephone number and e-mail address All bids must be accompanied by a $5,000 check (this check covers any and all parcels you wish to bid on) for earnest money made out to Wingert Realty Trust Account. Only registered bidders may attend. Must be registered prior to auction date. All potential buyers shall deliver or mail a sealed bid, postmarked by Wednesday, January 31, 2018 to: Wingert Realty & Land Services, Inc., Attn: Darrell Hylen 1160 Victory Drive So., Suite 6, Mankato, MN 56001 If you are unable to get postmarked bid in on time, call our office for other arrangements. Refer to the Zenk Farms brochure for further details concerning bidding procedures. Also available to print online: www.wingertrealty.com PARCEL 1 PARCEL 2 ACRES TOTAL BID AMOUNT (Nearest $1,000) PARCEL 3 PARCEL 4 PARCEL 1 57 ± PARCEL 2 80 ± PARCEL 3 150 ± PARCEL 4 150.31 ± $ $ $ $ NAME: ADDRESS: CITY / STATE / ZIP: CELL PHONE: ( ) /RESIDENTIAL ( ) E-MAIL ADDRESS: