Official Series Description


Lab Data Summary

Aggregate lab data for the PIPESTONE soil series. This aggregation is based on all pedons with a current taxon name of PIPESTONE, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to PIPESTONE were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
144A92P0990S1992NH011002Pipestone6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.8516655,-71.5922241
144A92P0994S1992NH011006Pipestone6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.9494438,-71.6999969
144B92P099792NH009003Pipestone5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.3133316,-71.6730576
9695P0529S1995MI019005Pipestone6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.6124992,-85.8647232
97LP76121976IN091012Pipestone3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.7522139,-86.7490306
9740A1966S1975MI021011Pipestone7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.1833458,-86.3980331
9781P0509S1981MI005001PIPESTONE5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.7094536,-85.6949539
9781P0508S1981MI005002PIPESTONE6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.743618,-86.158577
9808N0658F2008MI121005Pipestone6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.1561661,-86.0627518
9808N0660F2008MI121007Pipestone6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.1604996,-86.201889
9808N0661F2008MI121008Pipestone6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.1605263,-86.2030029
9808N0667F2008MI121014Pipestone6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.2387238,-86.1354752
9810N0098S09MI121002Pipestone6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.2926407,-85.9693604
98S80MI-73-7S1980MI073007Pipestone6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.6025,-84.6415833
9807N0723S2007MI139007Pipestone6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.9468613,-86.1830521

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PIPESTONE soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the PIPESTONE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the PIPESTONE series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the PIPESTONE series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .

Click the image to view it full size.

Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with PIPESTONE share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the PIPESTONE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the PIPESTONE series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

There are insufficient data to create the 3D mountains figure.

There are insufficient data to create the 3D terrace figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with PIPESTONE, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database .

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. MI-2012-02-06-06 | Allegan County - March 1987

    Pattern of soils and underlying material in the Oakville association (Soil Survey of Allegan County, Michigan; March 1987).

  2. MI-2012-02-06-50 | Saginaw County - January 1994

    Pattern of soils and parent material in the Pipestone-Granby-Wixom association (Soil Survey of Saginaw County, Michigan; January 1994).

  3. MI-2012-02-06-53 | Tuscola County - September 1986

    Pattern of soils and parent material in the Pipestone-Granby-Chelsea association (Soil Survey of Tuscola County, Michigan; September 1986).

  4. NH-2012-02-14-19 | Rockingham County - October 1994

    Typical pattern of soils and parent material in the Windsor-Hinckley-Canton general soil map unit (Soil Survey of Rockingham County, New Hampshire; October 1994).

Map Units

Map units containing PIPESTONE as a major component. Limited to 250 records.

Map Unit Name Symbol Map Unit Area (ac) Map Unit Key National Map Unit Symbol Soil Survey Area Publication Date Map Scale
Saugatuck-Pipestone complexSa79527268994rfin09119791:15840
Pipestone loamy coarse sand, 0 to 3 percent slopes38A76927654198rpma00119841:25000
Pipestone loamy fine sand, 0 to 3 percent slopes38A689277041998tma60219761:20000
Pipestone loamy sand, 0 to 3 percent slopes38A274780060v5q7ma60319791:20000
Pipestone loamy sand, 0 to 3 percent slopes38A1762790622vjpyma60519771:15840
Pipestone loamy fine sand, 0 to 3 percent slopes38A335791213vkb0ma60619811:15840
Pipestone sand, 0 to 4 percent slopes26A87112124477424mi00519841:15840
Covert-Pipestone sands, 0 to 6 percent slopesCovabB3626894342rfgwmi00519841:15840
Pipestone sand, Erie-Huron Lake Plain, 0 to 3 percent slopesPpA373326734322wb2cmi01119641:20000
Pipestone sand, loamy substratum, 0 to 2 percent slopesPrA249426734342qz4hmi01119641:20000
Pipestone-Grattan associationPx116326734382qz4mmi01119641:20000
Pipestone associationPu42526734362qz4kmi01119641:20000
Pipestone sand, loamy substratum, 2 to 6 percent slopesPrB20326734352qz4jmi01119641:20000
Pipestone-Tobico fine sands, 0 to 3 percent slopesPtA1642507831683tmi01119641:20000
Pipestone fine sand, loamy substratum, 0 to 3 percent slopesPnA4725078296833mi01119641:20000
Pipestone-Roscommon associationPw1526734372qz4lmi01119641:20000
Pipestone sand, Erie-Huron Lake Plain, 0 to 3 percent slopes35A133771865322wb2cmi01719781:20000
Pipestone fine sand, loamy substratum, 0 to 3 percent slopes25A57391865306833mi01719781:20000
Pipestone-Tobico fine sands, 0 to 3 percent slopes66A3434186552683tmi01719781:20000
Pipestone sand, loamy substratum, 0 to 2 percent slopes127A1926735742qz4hmi01719781:20000
Pipestone sand, 0 to 2 percent slopes26A160418616367q8mi02119791:15840
Pipestone sand, Erie-Huron Lake Plain, 0 to 3 percent slopesPsA23326735082wb2cmi03519771:15840
Pipestone sand, Erie-Huron Lake Plain, 0 to 3 percent slopesPiA245123995522wb2cmi04919671:20000
Pipestone loamy sand, loamy substratum, 0 to 6 percent slopesAuB220526736622qz47mi04919671:20000
Pipestone sand, loamy substratum, 0 to 3 percent slopesPhA16423995252ljx1mi04919671:20000
Covert-Urban land-Pipestone complex, 0 to 6 percent slopesCovaaB18190542321yr8mi04919671:20000
Pipestone sand, Erie-Huron Lake Plain, 0 to 3 percent slopesPqA642026734752wb2cmi05119661:15840
Pipestone-Kinross associationPX519326734772qz5gmi05119661:15840
Grayling-Covert-Pipestone associationGW402626734922qz5ymi05119661:15840
Covert-Pipestone-Roscommon associationCZ347426734902qz5wmi05119661:15840
Covert-Pipestone associationCX313626734882qz5tmi05119661:15840
Pipestone-Roscommon associationPZ295526734792qz5jmi05119661:15840
Iosco-Pipestone-Ingalls associationIP190426734932qz5zmi05119661:15840
Pipestone sand, loamy substratum, 0 to 2 percent slopesPuA189726734762qz5fmi05119661:15840
Covert-Pipestone-Kinross associationCY159426734892qz5vmi05119661:15840
Chelsea-Pipestone associationCF90026734862qz5rmi05119661:15840
Pipestone sand, loamy substratum, 0 to 3 percent slopesPrA8582673472686wmi05119661:15840
Pipestone-Kinross loamy substratum associationPY19126734782qz5hmi05119661:15840
Pipestone-Tobico fine sands, 0 to 3 percent slopesPtA772507845683tmi05119661:15840
Pipestone fine sand, loamy substratum, 0 to 3 percent slopesPnA4725078436833mi05119661:15840
Pipestone-Tedrow loamy sands, 0 to 2 percent slopesPpA531318703268m9mi05719751:12000
Pipestone-Tedrow loamy sands, loamy substratum, 0 to 2 percent slopesPrA287318703368mbmi05719751:12000
Pipestone sand, loamy substratum, 0 to 3 percent slopesPoA1302673593686wmi05719751:12000
Pipestone sand, Erie-Huron Lake Plain, 0 to 3 percent slopesPnA5126735922wb2cmi05719751:12000
Pipestone sand, Erie-Huron Lake Plain, 0 to 3 percent slopes36A72081867862wb2cmi06319781:20000
Riverdale-Pipestone complex, 0 to 2 percent slopes56A538718680668d0mi06319781:20000
Pipestone-Tobico-Adrian complex, 0 to 2 percent slopes29A254018678168c6mi06319781:20000
Pipestone sand, Erie-Huron Lake Plain, 0 to 3 percent slopes20A207821866092wb2cmi07319831:15840
Pipestone sand, loamy substratum, 0 to 3 percent slopes111A192673526686wmi07319831:15840
Pipestone sand, 0 to 4 percent slopes87B44918721568t6mi08119841:15840
Pipestone sand, Erie-Huron Lake Plain, 0 to 3 percent slopesPpB90525084192wb2cmi08719661:15840
Pipestone loamy sand, loamy substratum, 0 to 2 percent slopesAuA16226736822qz49mi08719661:15840
Pipestone sand, Erie-Huron Lake Plain, 0 to 3 percent slopesAsB605426737072wb2cmi09919671:20000
Pipestone sand, loamy substratum, 0 to 6 percent slopesAuB510026737082qz43mi09919671:20000
Wasepi-Pipestone complex, 0 to 4 percent slopesWvB113526737102qz6cmi09919671:20000
Pipestone fine sand, 0 to 4 percent slopes59B69981925806gd8mi10519921:15840
Pipestone-Saugatuck sands, 0 to 4 percent slopes56B42531925726gd0mi10519921:15840
Pipestone fine sand, loamy substratum, 0 to 4 percent slopes44B13821925616gcnmi10519921:15840
Pipestone loamy sand, 0 to 3 percent slopes34A405618774069c4mi10719821:15840
Pipestone sand, Erie-Huron Lake Plain, 0 to 3 percent slopesPsB491511866462wb2cmi11119761:15840
Pipestone sand, loamy substratum, 0 to 3 percent slopesPtB17879186647686wmi11119761:15840
Pipestone-Oakville-Urban land complex, 0 to 6 percent slopesPuB4049186648686xmi11119761:15840
Pipestone-Tedrow loamy sands, loamy substratum, 0 to 2 percent slopesPrA79267355668mbmi11119761:15840
Pipestone fine sand, loamy substratum, 0 to 3 percent slopesPnA3525079746833mi11119761:15840
Pipestone-Covert-Saugatuck sands, 0 to 3 percent slopesPpsaaA2968226894382rfgvmi12119661:15840
Covert-Pipestone sands, 0 to 6 percent slopesCovabB2649426894372rfgwmi12119661:15840
Pipestone sand, 0 to 4 percent slopes5B202421865016825mi12319901:15840
Pipestone-Kingsville complex, 0 to 3 percent slopes96A5611186521682tmi12319901:15840
Pipestone-Covert-Saugatuck sands, 0 to 3 percent slopesPpsaaA8326894632rfgvmi12319901:15840
Covert-Pipestone sands, 0 to 6 percent slopesCovabB4626894622rfgwmi12319901:15840
Pipestone sand, Erie-Huron Lake Plain, 0 to 3 percent slopes126B226737062wb2cmi12519801:15840
Pipestone fine sand, 0 to 4 percent slopes51B80051890546bqjmi12719921:15840
Pipestone-Covert-Saugatuck sands, 0 to 3 percent slopesPpsaaA1426894712rfgvmi12719921:15840
Covert-Pipestone sands, 0 to 6 percent slopesCovabB526894702rfgwmi12719921:15840
Covert-Pipestone sands, 0 to 6 percent slopesCovabB1521126894782rfgwmi13919671:15840
Pipestone-Covert-Saugatuck sands, 0 to 3 percent slopesPpsaaA1487226894792rfgvmi13919671:15840
Pipestone sand, Erie-Huron Lake Plain, 0 to 3 percent slopes31A411351866712wb2cmi14519911:15840
Pipestone sand, loamy substratum, 0 to 3 percent slopes26A16150186668687kmi14519911:15840
Pipestone-Tedrow loamy sands, 0 to 2 percent slopes140A309267360568m9mi14519911:15840
Pipestone-Tedrow loamy sands, loamy substratum, 0 to 2 percent slopes141A116267360668mbmi14519911:15840
Pipestone fine sand, loamy substratum, 0 to 3 percent slopes130A6925079846833mi14519911:15840
Pipestone loamy sand, loamy substratum, 0 to 6 percent slopes101B4526736312qz47mi14519911:15840
Pipestone and Saugatuck loamy sands, 0 to 2 percent slopesAeA071126736362qz3jmi15119551:15840
Pipestone and Saugatuck loamy sands, 2 to 6 percent slopes, slightly erodedAeB111426736372qz3kmi15119551:15840
Pipestone loamy sand, loamy substratum, 0 to 2 percent slopesAgA2326736382qz49mi15119551:15840
Pipestone sand, loamy substratum, 0 to 3 percent slopesPsA324231192mbg4mi15519671:12000
Pipestone loamy sand, loamy substratum, 0 to 6 percent slopesAuB326736592qz47mi15519671:12000
Pipestone sand, Erie-Huron Lake Plain, 0 to 3 percent slopes10B224151874662wb2cmi15719841:15840
Pipestone fine sand, loamy substratum, 0 to 4 percent slopes67B2481187516693xmi15719841:15840
Pipestone-Kingsville complex, 0 to 3 percent slopes48A1360218632767wkmi15919841:15840
Dair-Pipestone complex, 0 to 2 percent slopes100A48811933716h6smi61420051:12000
Covert-Pipestone sands, 0 to 6 percent slopes104B4198899731z67lmi61420051:12000
Pipestone sand, 0 to 4 percent slopes59B21371932716h3kmi61420051:12000
Platteriver-Pipestone sands, 0 to 4 percent slopes123B10961935146hcdmi61420051:12000
Pipestone sand, 0 to 5 percent slopes314A90352793129cn2nh01519861:24000
Pipestone loamy sand, 0 to 3 percent slopesPiA49692810029fdlnh60119801:20000
Pipestone loamy sand, 3 to 8 percent slopesPiB1492810039fdmnh60119801:20000
Pipestone fine sandPh19422902159qzsny01919951:24000

Map of Series Extent

Approximate geographic distribution of the PIPESTONE soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry .