IDENTIFIERS

Current Taxon Name (Soil Name): Blackhammer

OSD

Series Extent

User Site ID: S2005WI011001

User Pedon ID: S2005WI011001

Vegetation Plot ID: S2005WI011001

Lab Information:

Certified Lab Pedon Description - no

Lab Source ID - SSL

Lab Pedon # - 11N0306

NCSS Pedon Lab Data NASIS Record ID - 72885

User Project ID: 10-ONA_*

Project Name: MLRA 105 - Rountree Formation Depth class by Landscape modeling project

Print Date: 2/16/2025

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: 44.4022942

Std. Longitude: -91.5628967

Datum: WGS84

GPS - Positional Error: 6.00

Township: 22N

Range: 10W

Section: 11

PLSS Details: NW1/4

Country: US—United States

State: Wisconsin

County: WI011—Buffalo

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: WI011—Buffalo County, Wisconsin

7.5 Minute USGS Quad: 44091-D5—Lookout, Wisconsin

PEDON

Describers Name: Donna Ferren Guy

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

Current Taxon Kind: series

Pedon Type: classifies to current taxon name, brief description

Pedon Purpose: laboratory sampling site

Pedon Record Orgin: PedonPC 4.2

Correlated Information:

Soil Name - Blackhammer

PSC - 25 to 75 cm.

Classificaton Date - 2/16/2021

Classifier - Donna Ferren Guy

Soil Taxonomic Edition - eleventh edition

Moisture Subclass - typic

Sampled As Information:

Soil Name - Dubuque

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

Taxon Kind - series

PSC - 25 to 75 cm.

Classificaton Date - 11/15/2004

Classifier - Donna Ferren Guy

Moisture SUBClass - typic

Dynamic Soil Properties:

Pedoderm Loose Cover Indicator - no

Pedon Vegetation and Crop Cover Information:

Agronomic Feature - close grown annual crop, or crop-fallow

Current Crop - alfalfa

Hydric: no

Certification Status: not certified

QC Status: not reviewed

QA Status: not reviewed

SITE

Parent Material: Peoria silty loess over pedisediment

Slope Complexity: simple

Slope Shape Across: concave

Slope Shape Down: concave

Drainage Class: well

Flooding: none flooding

Ponding: none ponding

Bedrock: dolomite (dolostone)

Geology: Oneota formation of the Prairie Du Chien group.

Surface Fragments:

Benchmark Soil?: no

RaCA Information:

Plot/Site Set Up By - Tim Meyer

Plot or Site Recorder - Donna Ferren Guy

VEGETATION

Vegplot Text Note(s): A scan of the original data (i.e. field sheet(s), edits, manuscripts, notes, and other associated data) is available in the RO10 Field Documentation Archive maintained by Adolfo Diaz, RO10 GIS Specialist. This web map can be accessed using the following link: http://arcg.is/1iDqnO Google Chrome is recomended to explore the map. At its full extent, the web map will display the 9 states that make up Region 10 along with a summary of the number of pedons per state. Since there are too many points to display at the full extent you will have to zoom in to an approximate scale of an average county. Once zoomed in you will notice that the pedons will appear both in the legend (Table of content area) and in the map. Once displayed, you can click on any point to open the identification window and get basic information such as: Series Name, location description, Lat-Long and other information. The original document has also been embedded as an attachment and can be previewed by clicking on the pdf file within the identification window. This database represents a snapshot and will be updated once a month. This database can also be directly streamed into an ArcGIS/ArcPro session to be overlaid with your project layers. However, to do so you must have an ArcGIS Online for Organizational account. If you are interested in this please let Adolfo Diaz know and he can work with you to set it up. As a recap, here are the main objectives of this project: 1. Inventory and digitally archive - As soil survey crews finalized surveys and made their way to different offices, many of the original soil survey documentation was left behind or simply discarded as being irrelevant material. The inventory process was an opportunity to collect and organize this legacy documentation. For preservation and accessibility purposes these files were also scanned. 2. Develop a GIS database In order to view the spatial distribution of our inventory and perform spatial queries, pedons with a valid location were digitized. As part of this process, each pedon was assigned a unique siteID using the current NASIS naming convention. 3. Enter into NASIS as needed Having pedons in a GIS gives the user the advantage of spatially assessing field documentation availability and determine whether a pedon should be entered into NASIS for project purposes. If you have any questions contact: Adolfo Diaz, RO10 GIS Specialist, Madison, WI Shaunna Repking, MLRA Soil Scientist, Onalaska, WI

SITE OBSERVATION

Observation Date: 11/15/2004 (actual site observation date)

Data Collector: Donna Ferren Guy

Surface Water Kind: none observed

Hydrology Status: unaltered

Surface Cover Properties:

Site Obs. Cover Kind 1 - crop cover

Site Obs. Cover Kind 2 - hayland

Pedoderm Loose Cover Indicator - no

Biol. Crust Type Dominant - none evident

Biol. Crust Type Secondary - none evident

Drained? - no

Bedded Soil? - no

Forest Plantation? - no

Vegetation Plot Plants
Plant Symbol	Scientific Name	National Vernacular Name	Plant Type Group	Canopy Cover %	Vegetation Stata Level
MEDIC	Medicago	alfalfa	forb	100	overstory

Pedon Diagnostic Features
Feature Kind	Feature Depth L-H	Feature Thickness L-RV-H
	cm
ochric epipedon argillic horizon lithologic discontinuity agric horizon	— — — 25—203	—- —- —- —-

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
16	—	—	—	—		899	—	155	8	22	-5	12	22	2	558	—	470124	ALMA DAM 4, WI US	NOAA/COOP

Ap—0 to 25 centimeters (0.0 to 9.8 inches); dark grayish brown (10YR 4/2) broken face, brown (10YR 5/3) broken face, dry; silt loam; moderate fine subangular blocky structure; friable; 1 percent by volume nonflat angular very strongly coherent cemented 5-20-76 millimeter dolomite (dolostone) fragments observed by visual inspection method; slightly acid, pH 6.5, hellige-truog. Lab sample # 11N01352; moist when described; observed in pit, large or quarry

Bt1—25 to 41 centimeters (9.8 to 16.1 inches); dark yellowish brown (10YR 4/4) broken face silt loam; moderate medium subangular blocky structure; friable; fragments; slightly acid, pH 6.5, hellige-truog. Lab sample # 11N01353; moist when described; observed in pit, large or quarry

Bt2—41 to 76 centimeters (16.1 to 29.9 inches); dark yellowish brown (10YR 4/4) broken face silt loam; moderate medium subangular blocky structure; friable; fragments; neutral, pH 7.0, hellige-truog. Lab sample # 11N01354; moist when described; observed in pit, large or quarry

2Bt3—76 to 109 centimeters (29.9 to 42.9 inches); strong brown (7.5YR 4/6) broken face gravelly clay loam; moderate medium subangular blocky structure; firm; 2 percent by volume nonflat angular very strongly coherent cemented 76-163-250 millimeter dolomite (dolostone) fragments observed by visual inspection method and 15 percent by volume nonflat angular very strongly coherent cemented 5-20-76 millimeter dolomite (dolostone) fragments observed by visual inspection method; strongly acid, pH 5.5, hellige-truog. Lab sample # 11N01355; moist when described; observed in pit, large or quarry

2Bt4—109 to 163 centimeters (42.9 to 64.2 inches); olive (5Y 5/6) broken face cobbly sandy loam; weak coarse subangular blocky structure; 6 percent by volume nonflat angular very strongly coherent cemented 5-20-76 millimeter dolomite (dolostone) fragments observed by visual inspection method and 12 percent by volume nonflat angular very strongly coherent cemented 76-163-250 millimeter dolomite (dolostone) fragments observed by visual inspection method; strongly acid, pH 5.5, hellige-truog. Lab sample # 11N01356; moist when described; observed in pit, large or quarry

2Bt5—163 to 203 centimeters (64.2 to 79.9 inches); yellowish red (5YR 4/6) broken face very gravelly clay loam; structureless massive; 10 percent by volume nonflat angular very strongly coherent cemented 5-20-76 millimeter dolomite (dolostone) fragments observed by visual inspection method and 40 percent by volume nonflat angular very strongly coherent cemented 76-163-250 millimeter dolomite (dolostone) fragments observed by visual inspection method; very strongly acid, pH 4.5, hellige-truog. Lab sample # 11N01357; moist when described; observed in pit, large or quarry