IDENTIFIERS

Current Taxon Name (Soil Name): Urne

OSD

Series Extent

User Site ID: S1994WI023036

User Pedon ID: S1994WI023036

Vegetation Plot ID: S1994WI023036

Lab Information:

Certified Lab Pedon Description - no

Lab Source ID - SSL

Lab Pedon # - 95P0353

NCSS Pedon Lab Data NASIS Record ID - 67371

Print Date: 11/21/2024

LOCATION

Location In Web Soil Survey

AOI is roughly a square mile and pedon is marked in the center.

Location in SoilWeb

Location in Google Maps

Std. Latitude: 43.2194443

Std. Longitude: -90.8311081

Datum: WGS84

GPS - Positional Error: 10.00

Township: 9N

Range: 4W

Section: 34

PLSS Details: 160 feet south and 1760 feet west of the northeast corner

Country: US—United States

State: Wisconsin

County: WI023—Crawford

MLRA: 105—Upper Mississippi River Bedrock Controlled Uplands and Valleys

Regional Office: NC—North Central

MLRA Soil Survey Area: NC-ONA—Onalaska, Wisconsin

Non-MLRA Soil Survey Area: WI023—Crawford County, Wisconsin

7.5 Minute USGS Quad: 43090-B7—Steuben, Wisconsin

PEDON

Describers Name: Dave Omernik, Dennis Anthony, Dan Fredrick

Current Taxonomic Class: Fine-loamy, mixed, superactive, mesic Typic Hapludalfs

Current Taxon Kind: taxadjunct

Pedon Type: classifies to current taxon name, brief description

Pedon Purpose: laboratory sampling site

Pedon Record Orgin: PedonPC 4.2

Pedon #: 36

Correlated Information:

Soil Name - Urne

PSC - 25 to 75 cm.

Classificaton Date - 4/26/2012

Classifier - Dave Omernik

Moisture Subclass - typic

Sampled As Information:

Soil Name - Urne

Taxonomic Class - Fine-loamy, mixed, superactive, mesic Typic Hapludalfs

Taxon Kind - taxadjunct

PSC - 25 to 75 cm.

Classificaton Date - 7/28/1994

Classifier - Dave Omernik

Moisture SUBClass - typic

Dynamic Soil Properties:

Pedoderm Loose Cover Indicator - no

Hydric: no

Certification Status: certified

QC Status: not reviewed

QA Status: not reviewed

SITE

Parent Material: colluvium derived from glauconite

Landscape: upland

Landform: valley side

Geomorphic Component Hills: nose slope

Hill Slope Profile: footslope

Slope Position: lower third

Slope Complexity: simple

Slope Shape Across: convex

Slope Shape Down: convex

Runoff: high

Drainage Class: well

Flooding: none flooding

Ponding: none ponding

Wet Soil Moisture Duration: 0

Bedrock: strongly coherent slight weathered sandstone, unspecified at 163cm with =>200 and a strike of 220 degrees and a dip of 2 to 2 degrees

Geology: Wonewoc formation of the Elk Mound group.

Surface Fragments: 0.01 percent

Benchmark Soil?: no

RaCA Information:

Plot/Site Set Up By - Unknown

Plot or Site Recorder - Unknown

VEGETATION

SITE OBSERVATION

Observation Date: 7/28/1994 (actual site observation date)

Data Collector: Dave Omernik

Surface Cover Properties:

Site Obs. Cover Kind 1 - grass/herbaceous cover

Site Obs. Cover Kind 2 - other grass/herbaceous cover

Pedoderm Loose Cover Indicator - no

Drained? - no

Bedded Soil? - no

Forest Plantation? - no

Site Erosion Accelerated: water erosion

Vegetation Plot Plants
Plant Symbol	Scientific Name	National Vernacular Name	Plant Type Group	Canopy Cover %	Vegetation Stata Level
JUGLA ULMUS RHUS ACHIL	Juglans Ulmus Rhus Achillea	walnut elm sumac yarrow	tree tree shrub/vine forb	— — — —	— — — —

Pedon Restrictions
Kind	Hardness	Restriction Depth L-H	Restriction Thickness L-RV-H
		cm
bedrock, paralithic	—	—	—

Pedon Diagnostic Features
Feature Kind	Feature Depth L-H	Feature Thickness L-RV-H
	cm
lithologic discontinuity paralithic materials ochric epipedon argillic horizon paralithic contact	— — 0—25 25—113 160—162	—- —- —- —- —-

Setting and Climate
Slope	Slope Length USLE	Upslope Length	Elev.	Corr. Elev	Aspect	MAP	REAP	FFD	MAAT	MSAT	MWAT	MAST	MSST	MWST	MFFP	PE Index	Climate Station ID	Climate Station Name	Climate Station Type
%	m				degrees	mm	mm		C						mm
19	44	33	236	—	270	899	—	155	8	22	-5	12	22	2	558	—	00477869	SOLDIERS GROVE, WI US	NOAA

Ap—0 to 25 centimeters (0.0 to 9.8 inches); brown (10YR 4/3) rubbed and dark grayish brown (10YR 4/2) exterior, pale brown (10YR 6/3) rubbed and pale brown (10YR 6/3) exterior, dry; fine sandy loam; 10 percent sand; 30 percent silt; 60 percent clay; moderate very fine granular, and subangular blocky structure; very friable; 4.0 very fine roots throughout and 4.0 fine roots throughout; 5.0 very fine low-continuity vesicular and 5.0 very fine low-continuity tubular pores; subangular limestone, cherty fragments observed by visual inspection method and 25 percent by volume sandstone, unspecified fragments observed by visual inspection method and 75 percent by volume dolomite (dolostone) fragments observed by visual inspection method; moderately acid, pH 5.7, pH meter; abrupt smooth boundary. Lab sample # 95P02757; moist when described; observed in pit, small. 3percent mixing of Ap and Bt by worms, OM content 1.25percent, 1 or 2 tree roots in top 4 horizon

Bt1—25 to 36 centimeters (9.8 to 14.2 inches); dark yellowish brown (10YR 4/4) exterior loam; 15 percent sand; 34 percent silt; 51 percent clay; weak very fine granular structure; very friable; 2.0 very fine roots throughout and 2.0 fine roots throughout; 4.0 very fine low-continuity vesicular and 4.0 very fine low-continuity tubular pores; 10 percent faint light olive brown (2.5Y 5/4), moist, skeletans on all faces of peds and 15 percent faint dark yellowish brown (10YR 3/4), moist, clay films on all faces of peds; subangular limestone, cherty fragments observed by visual inspection method and 25 percent by volume sandstone, unspecified fragments observed by visual inspection method and 75 percent by volume dolomite (dolostone) fragments observed by visual inspection method; slightly acid, pH 6.1, pH meter; clear wavy boundary. Lab sample # 95P02758; moist when described; observed in pit, small. includes sandstone weathered in place; discontinuous - phpvsfiid 1913124; patchy - phpvsfiid 1913123; discontinuous - phpvsfiid 1913124; patchy - phpvsfiid 1913123

Bt2—36 to 58 centimeters (14.2 to 22.8 inches); dark yellowish brown (10YR 4/6) exterior loam; 20 percent sand; 35 percent silt; 45 percent clay; moderate fine subangular blocky structure; friable; 2.0 very fine roots between peds; 3.0 very fine low-continuity vesicular and 3.0 very fine low-continuity tubular pores; 5 percent faint yellowish brown (10YR 5/6), moist, skeletans on all faces of peds and 35 percent faint dark yellowish brown (10YR 4/4), moist, clay films on all faces of peds; subangular limestone, cherty fragments observed by visual inspection method and 25 percent by volume sandstone, unspecified fragments observed by visual inspection method and 75 percent by volume dolomite (dolostone) fragments observed by visual inspection method; slightly acid, pH 6.1, pH meter; clear wavy boundary. Lab sample # 95P02759; moist when described; observed in pit, small. discontinuous - phpvsfiid 1913119; patchy - phpvsfiid 1913120; discontinuous - phpvsfiid 1913119; patchy - phpvsfiid 1913120

Bt3—58 to 74 centimeters (22.8 to 29.1 inches); dark yellowish brown (10YR 4/6) exterior fine sandy loam; 19 percent sand; 28 percent silt; 53 percent clay; moderate fine subangular blocky, and moderate medium subangular blocky structure; friable; 1.0 very fine roots between peds; 3.0 very fine low-continuity vesicular and 3.0 very fine low-continuity tubular pores; 5 percent faint yellowish brown (10YR 5/6), moist, skeletans on all faces of peds and 50 percent distinct brown (7.5YR 4/4), moist, clay films on all faces of peds; 3 percent by volume subrounded sandstone, unspecified fragments observed by visual inspection method and 3 percent by volume subrounded siltstone, unspecified fragments observed by visual inspection method; moderately acid, pH 6.0, pH meter; abrupt smooth boundary. Lab sample # 95P02760; moist when described; observed in pit, small. channers at contact with lower horizon (frost action); patchy - phpvsfiid 1913127; continuous - phpvsfiid 1913128; patchy - phpvsfiid 1913127; continuous - phpvsfiid 1913128

2Bt4—74 to 112 centimeters (29.1 to 44.1 inches); 50 percent olive yellow (2.5Y 6/6) exterior and 40 percent strong brown (7.5YR 5/6) exterior and 10 percent yellowish brown (10YR 5/6) exterior channery very fine sandy loam; 11 percent sand; 18 percent silt; 71 percent clay; weak medium prismatic parts to weak medium subangular blocky, and weak medium prismatic parts to weak coarse subangular blocky structure; very friable; 1.0 very fine roots between peds; 2.0 very fine low-continuity vesicular pores; 10 percent prominent brown (7.5YR 4/3), moist, clay films on all faces of peds and 30 percent distinct strong brown (7.5YR 4/6), moist, clay films on all faces of peds; prominent black (10YR 2/1), moist, manganese coatings on faces of peds; 8 percent by volume subrounded siltstone, unspecified fragments observed by visual inspection method and 10 percent by volume siltstone, unspecified fragments observed by visual inspection method and 28 percent by volume subrounded sandstone, unspecified fragments observed by visual inspection method and 90 percent by volume sandstone, glauconitic fragments observed by visual inspection method; moderately acid, pH 5.7, pH meter; abrupt wavy boundary. Lab sample # 95P02761; moist when described; observed in pit, small. sieve analysis coarse fragmentsnot sent to lab seperated in field, volume 9percent of channers are 2mm to 75mm size, flagstones in lower horizons and siltstones, NSSL lab has 45percent by volume frags, rock frags 90percent glauconitic sandstone (Lone Rock Fm) 10percent siltstone from St. Lawrence fm Lodi member, 2-quart samples due to the large number of coarse fragments; discontinuous - phpvsfiid 1913125; discontinuous - phpvsfiid 1913126; discontinuous - phpvsfiid 1913125; discontinuous - phpvsfiid 1913126

2BC—112 to 160 centimeters (44.1 to 63.0 inches); olive yellow (2.5Y 6/6) exterior channery very fine sandy loam; 6 percent sand; 33 percent silt; 61 percent clay; weak coarse subangular blocky parts to structureless single grain; loose; 1.0 very fine low-continuity vesicular pores; prominent strong brown (7.5YR 5/6), moist, coats between sand grains and distinct brownish yellow (10YR 6/6), moist, coats on rock fragments; 6 percent by volume subrounded siltstone, unspecified fragments observed by visual inspection method and 10 percent by volume sandstone, glauconitic fragments observed by visual inspection method and 21 percent by volume subrounded sandstone, unspecified fragments observed by visual inspection method and 90 percent by volume siltstone, unspecified fragments observed by visual inspection method; strong effervescence, by hcl, 1n; moderately alkaline, pH 8.3, pH meter; abrupt irregular boundary. Lab sample # 95P02762; moist when described; observed in pit, small. has 40percent by volume frags - about the same as my sieve data. I wonder if they might hace used my data. Otherwise there sure is nice correlation between the two data sets, volume at 18percent of channers are 2mm to 75mm, sieve analysis coarse fragments are random, flagstones in lower horizons and siltstones, Boundary is lamellae-like loamy lense. Nore high silt content is lodi siltstone, Rock fragments 10percent glauconitic sandstone and 90percent st. lawrence fm black earth member to account for effervescence, black earth member is calcitic cemented sandstone. Principles of ascendency decendency apply here; continuous - phpvsfiid 1913121; continuous - phpvsfiid 1913122; continuous - phpvsfiid 1913121; continuous - phpvsfiid 1913122

3Cr—160 to 163 centimeters (63.0 to 64.2 inches); very pale brown (10YR 7/3) exterior bedrock; distinct brownish yellow (10YR 6/6), moist, coats on rock fragments; fragments; noneffervescent, by hcl, 1n.; moist when described; observed in pit, small. crack in bedrock 4-11 cm widedown 8cm filled with BC material, upper 2cm is fractured and has silt coats, easily chipped with spade - more difficult with depth - Wonewoc fm; discontinuous - phpvsfiid 1913129; discontinuous - phpvsfiid 1913129