Official Series Description


Lab Data Summary

Aggregate lab data for the MURRILL soil series. This aggregation is based on all pedons with a current taxon name of MURRILL, 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 MURRILL were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
12789PA0270881989PA027088Murrill5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7127778,-78.9394444
128WVU0023S01WV063001Murrill5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6124444,-80.2657778
128WVU0024S01WV063002Murrill5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6129167,-80.2658333
130A91P032090PA055024Murrill5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7966652,-77.5066681
14704N080904PA027007Murrill4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7197227,-77.9330521
14759PA0350191959PA035019Murrill5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.99,-77.4258333
14771PA0270291971PA027029Murrill5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.9166667,-77.6769444
14771PA0270301971PA027030Murrill5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8738889,-77.6436111
14771PA0610281971PA061028Murrill5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.4897222,-77.8688889
14772PA0270421972PA027042Murrill5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7169444,-77.9272222
14777PA0270451977PA027045Murrill4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7161111,-77.9275
14791P031590PA055019Murrill5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.8847237,-77.9266663
14791P031690PA055020Murrill5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7844429,-77.5400009
14791P031790PA055021Murrill5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.8533325,-77.9277802
14791P031890PA055022Murrill5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.8741684,-77.9319458
14791P031990PA055023Murrill5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.8722229,-77.9227753
14799P050599PA027095Murrill7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7166672,-77.9333344
n/a90P028289PA055016Murrill6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a98P031597VA167022MURRILL1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a98P031797VA167024MURRILL1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a98P031697VA167033MURRILL1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MURRILL 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.

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Sibling Summary

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

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

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Geomorphic description summaries for the MURRILL 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 .

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

Competing Series

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

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

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Geomorphic description summaries for the MURRILL 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 .

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Click the image to view it full size.

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

Soil series sharing subgroup-level classification with MURRILL, 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. MD-2010-09-07-01 | Frederick County - 2002

    Relationship of soils, topography, and underlying material in the Bagtown-Stumptown-Edgemont general soil map unit (Soil Survey of Frederick County, Maryland; 2002).

  2. MD-2010-09-07-09 | Washington County - 2003

    Relationship of soils to topography and underlying material in the Murrill-Dryrun general soil map unit (Soil Survey of Washington County, Maryland; 2003).

  3. MD-2012-02-03-16 | Frederick County - 2002

    Relationship of soils, topography, and underlying material in the Bagtown-Stumptown-Edgemont general soil map unit (Soil Survey of Frederick County, Maryland; 2002).

  4. MD-2012-02-03-28 | Washington County - 2003

    Relationship of soils to topography and underlying material in the Murrill-Dryrun general soil map unit (Soil Survey of Washington County, Maryland; 2003).

  5. PA-2010-09-30-11 | Franklin County -

    Relationship of soils to topography and underlying material in the Murrill general soil map unit (Soil Survey of Franklin County, Pennsylvania).

  6. PA-2010-09-30-13 | Fulton County - 2004

    Relationship of soils to topography and the underlying material in the Hagerstown general soil map unit (Soil Survey of Fulton County, Pennsylvania; 2004).

  7. PA-2012-03-12-13 | Bedford County - 1998

    Typical pattern of soils and underlying material in the Hagerstown-Clarksburg-Opequon general soil map unit (Soil Survey of Bedford County, PA; 1998).

  8. PA-2012-03-12-17 | Blair County - October 1981

    Typical pattern of soils and underlying material in the Laidig-Hazleton-Buchanan association (Soil Survey of Blair County, PA; 1981).

  9. PA-2012-03-12-20 | Blair County - October 1981

    Typical pattern of soils and underlying material in the Hublersburg-Murrill-Opequon association (Soil Survey of Blair County, PA; 1981).

  10. PA-2012-03-12-21 | Blair County - October 1981

    Typical pattern of soils and underlying material in the Morrison association (Soil Survey of Blair County, PA; 1981).

  11. PA-2012-03-13-20 | Cumberland and Perry Counties - April 1986

    Typical pattern of soils and underlying material in the Murrill-Laidig-Buchanan association (Soil Survey of Cumberland and Perry Counties, PA; 1986).

  12. PA-2012-03-13-28 | Franklin County - August 1975

    Relationship of underlying material and topography in association 3 (Soil Survey of Franklin County, PA; 1975).

  13. PA-2012-03-13-32 | Fulton County - 2004

    Relationship of soils to topography and the underlying material in the Hagerstown general soil map unit (Soil Survey of Fulton County, PA; 2004).

  14. PA-2012-03-13-33 | Fulton County - 2004

    Diagram showing pattern of soils and their parent material on a mountain slope and in an adjacent valley in eastern Fulton County (Soil Survey of Fulton County, PA; 2004).

  15. PA-2012-03-13-41 | Juniata and Mifflin Counties - April 1981

    Typical pattern of soils and underlying material of the Hagerstown-Opequon-Murrill association (Soil Survey of Juniata and Mifflin Counties, PA; 1981).

Map Units

Map units containing MURRILL 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
Murrill gravelly loam, 15 to 25 percent slopesMuD66324012162llnlmd00120091:12000
Murrill gravelly loam, 8 to 15 percent slopesMuC47724012152llnkmd00120091:12000
Murrill gravelly loam, 3 to 8 percent slopesMuB6824012142llnjmd00120091:12000
Murrill gravelly loam, 25 to 45 percent slopesMuE6724012172llnmmd00120091:12000
Murrill gravelly loam, 3 to 8 percent slopesMrB734535040kyrcmd02120011:12000
Murrill-Dryrun-Urban land complex, 0 to 8 percent slopesMtB529564041lxxwmd02120011:12000
Murrill gravelly loam, 3 to 8 percent slopesMsB6656534557ky7smd04319981:12000
Murrill gravelly loam, 8 to 15 percent slopesMsC2185534560ky7wmd04319981:12000
Murrill-Urban land complex, 0 to 8 percent slopesMuB679534565ky81md04319981:12000
Murrill silt loam, 3 to 8 percent slopesMoB490534542ky79md04319981:12000
Murrill gravelly loam, 15 to 25 percent slopesMsD291534562ky7ymd04319981:12000
Murrill-Urban land complex, 8 to 25 percent slopesMuD64534567ky83md04319981:12000
Murrill silt loam, 8 to 15 percent slopesMoC61534545ky7dmd04319981:12000
Murrill channery loam, 3 to 8 percent slopesMuB3983541840l5tqpa00919891:24000
Murrill channery loam, 8 to 15 percent slopesMuC3945541841l5trpa00919891:24000
Morrison-Murrill complex, 8 to 15 percent slopes, very stonyMtC3832541838l5tnpa00919891:24000
Morrison-Murrill complex, 15 to 25 percent slopes, very stonyMtD1734541839l5tppa00919891:24000
Morrison-Murrill complex, 3 to 8 percent slopes, very stonyMtB1257541837l5tmpa00919891:24000
Murrill channery loam, 15 to 25 percent slopesMuD970541842l5tspa00919891:24000
Murrill gravelly loam, 3 to 8 percent slopesMuB6292543053l72vpa01119971:24000
Murrill gravelly loam, 8 to 15 percent slopesMuC1351543054l72wpa01119971:24000
Murrill gravelly loam, 0 to 3 percent slopesMuA981543052l72tpa01119971:24000
Murrill gravelly silt loam, 3 to 8 percent slopesMuB3003542395l6dmpa01319781:20000
Murrill gravelly silt loam, 8 to 15 percent slopesMuC2219542396l6dnpa01319781:20000
Murrill extremely stony silt loam, 8 to 25 percent slopesMxD1000542399l6drpa01319781:20000
Murrill extremely stony silt loam, 3 to 8 percent slopesMxB854542398l6dqpa01319781:20000
Murrill gravelly silt loam, 15 to 25 percent slopesMuD455542397l6dppa01319781:20000
Murrill channery silt loam, 3 to 8 percent slopesMuB8707538329l25gpa02719751:20000
Murrill channery silt loam, 8 to 15 percent slopesMuC2174538330l25hpa02719751:20000
Morrison very stony sandy loam, steepMTF1929538312l24xpa02719751:20000
Murrill channery silt loam, 0 to 3 percent slopesMuA1746538328l25fpa02719751:20000
Murrill very stony silt loam, 0 to 8 percent slopesMvB1504538332l25kpa02719751:20000
Murrill very stony silt loam, 8 to 25 percent slopesMvD287538333l25lpa02719751:20000
Murrill channery silt loam, 15 to 25 percent slopesMuD177538331l25jpa02719751:20000
Murrill gravelly loam, 3 to 8 percent slopesMuB30641363pjd4pa02920081:24000
Murrill silt loam, 3 to 8 percent slopesMuB309544078l84xpa03520021:24000
Murrill silt loam, 15 to 25 percent slopesMuD198544083l852pa03520021:24000
Murrill silt loam, 0 to 3 percent slopesMuA147544076l84vpa03520021:24000
Murrill silt loam, 8 to 15 percent slopesMuC41544080l84zpa03520021:24000
Murrill channery loam, 3 to 8 percent slopesMuB10237693782r8y2pa04119801:15840
Murrill channery loam, 8 to 15 percent slopesMuC2356693783r8y3pa04119801:15840
Murrill channery loam, 0 to 3 percent slopesMuA1871693781r8y1pa04119801:15840
Murrill gravelly loam, 3 to 8 percent slopesMrB16416545169l993pa05519991:24000
Murrill gravelly loam, 8 to 15 percent slopesMrC5784545170l994pa05519991:24000
Murrill gravelly loam, 8 to 25 percent slopes, extremely stonyMvD1774545174l998pa05519991:24000
Murrill cobbly sandy loam, 3 to 8 percent slopesMuB1482545171l995pa05519991:24000
Murrill cobbly sandy loam, 8 to 15 percent slopesMuC1219545172l996pa05519991:24000
Murrill gravelly loam, 0 to 3 percent slopesMrA1194545168l992pa05519991:24000
Murrill gravelly loam, 3 to 8 percent slopes, extremely stonyMvB1193545173l997pa05519991:24000
Murrill gravelly loam, 3 to 8 percent slopesMrB2211544915l90xpa05719991:24000
Murrill gravelly loam, 8 to 15 percent slopesMrC1671544916l90ypa05719991:24000
Murrill gravelly loam, 8 to 25 percent slopes, extremely stonyMvD569544919l911pa05719991:24000
Murrill gravelly loam, 3 to 8 percent slopesMuB2421542026l60qpa06119741:20000
Murrill gravelly loam, 8 to 15 percent slopesMuC2380542027l60rpa06119741:20000
Murrill gravelly loam, 15 to 25 percent slopesMuD923542028l60spa06119741:20000
Murrill gravelly loam, 3 to 8 percent slopes1MuB26557335lpykpa07119821:15840
Murrill gravelly loam, 8 to 15 percent slopes1MuC6557336lpylpa07119821:15840
Murrill gravelly silt loam, 3 to 8 percent slopesMuB1074541316l58tpa07519761:20000
Murrill gravelly loam, 3 to 8 percent slopesMuB499543175l76spa07719971:24000
Murrill gravelly loam, 8 to 15 percent slopesMuC352543176l76tpa07719971:24000
Murrill channery loam, 3 to 8 percent slopesMuB859694007r95bpa09919801:15840
Murrill channery loam, 8 to 15 percent slopesMuC345694008r95cpa09919801:15840
Murrill channery loam, 0 to 3 percent slopesMuA215694006r959pa09919801:15840
Murrill gravelly loam, 3 to 8 percent slopesMvB1605542910l6y7pa13319901:24000
Murrill gravelly loam, 8 to 15 percent slopesMvC749542911l6y8pa13319901:24000
Murrill gravelly loam, 3 to 8 percent slopesMuB4371545523l9njpa60519751:20000
Murrill gravelly loam, 8 to 15 percent slopesMuC2212545524l9nkpa60519751:20000
Oriskany-Murrill complex, 15 to 35 percent slopes, very stony45D7615834384x07mva00520031:24000
Oriskany-Murrill complex, 35 to 55 percent slopes, extremely stony45E3046834385x07nva00520031:24000
Murrill cobbly loam, 15 to 35 percent slopes, very stony39D2163834374x079va00520031:24000
Oriskany-Murrill complex, 8 to 15 percent slopes, very stony45C1575834383x07lva00520031:24000
Murrill loam, 8 to 15 percent slopes38C1279834371x076va00520031:24000
Murrill cobbly loam, 8 to 15 percent slopes, very stony39C788834373x078va00520031:24000
Murrill loam, 15 to 25 percent slopes38D449834372x077va00520031:24000
Murrill loam, 3 to 8 percent slopes38B422834370x075va00520031:24000
Oriskany-Murrill complex, 15 to 35 percent slopes, very stony46D897814514581kqc7va01720051:24000
Oriskany-Murrill complex, 35 to 55 percent slopes, extremely stony47E696614514591kqc8va01720051:24000
Murrill cobbly loam, 15 to 35 percent slopes, very stony40D422514514131kq9sva01720051:24000
Murrill loam, 8 to 15 percent slopes39C201914514101kq9pva01720051:24000
Oriskany-Murrill complex, 8 to 15 percent slopes, very stony46C168814514571kqc6va01720051:24000
Murrill loam, 15 to 25 percent slopes39D87914514111kq9qva01720051:24000
Murrill cobbly loam, 8 to 15 percent slopes, very stony40C85014514121kq9rva01720051:24000
Murrill cobbly loam, 35 to 55 percent slopes, very stony40E26014514141kq9tva01720051:24000
Murrill loam, 3 to 8 percent slopes39B13714514091kq9nva01720051:24000
Oriskany-Murrill complex, 15 to 35 percent slopes, very stony42E1761425120892q9j6va09120101:24000
Oriskany-Murrill complex, 8 to 15 percent slopes, very stony42C863225120912q9j8va09120101:24000
Oriskany-Murrill complex, 35 to 55 percent slopes, extremely stony43F616925120902q9j7va09120101:24000
Murrill cobbly loam, 15 to 35 percent slopes, very stony36E331725120782q9hvva09120101:24000
Murrill loam, 8 to 15 percent slopes37C301725120822q9hzva09120101:24000
Murrill cobbly loam, 8 to 15 percent slopes, very stony36C273525120792q9hwva09120101:24000
Murrill loam, 3 to 8 percent slopes37B208325120812q9hyva09120101:24000
Murrill loam, 15 to 25 percent slopes37D103225120802q9hxva09120101:24000
Oriskany-Murrill complex, 15 to 35 percent slopes, extremely stony49E849125148332qdcbva16320101:24000
Oriskany-Murrill complex, 35 to 55 percent slopes, extremely stony49F530825148342qdccva16320101:24000
Oriskany-Murrill complex, 3 to 15 percent slopes, extremely stony49C440325148322qdc9va16320101:24000
Murrill silt loam, 7 to 15 percent slopes34C1516522089kj8lva18519961:24000
Murrill silt loam, 2 to 7 percent slopes34B703522088kj8kva18519961:24000
Murrill silt loam, 15 to 25 percent slopes34D619522090kj8mva18519961:24000
Murrill gravelly loam, 3 to 8 percent slopesMrB456516264kb6pwv00319971:24000
Murrill gravelly loam, 8 to 15 percent slopesMrC238516265kb6qwv00319971:24000
Murrill channery loam, 8 to 15 percent slopesMuC179417166851vmbywv06319621:24000
Murrill channery loam, 15 to 25 percent slopesMuD1363514539k8f1wv06319621:24000
Murrill channery loam, 3 to 8 percent slopesMuB893514537k8dzwv06319621:24000
Murrill channery loam, 25 to 45 percent slopesMuE16617166871vmc0wv06319621:24000
Murrill loam, 15 to 35 percent slopes, extremely stonyMsE1208555700ln7twv06520031:24000
Murrill loam, 3 to 15 percent slopes, extremely stonyMsC596555699ln7swv06520031:24000
Murrill gravelly loam, 8 to 15 percent slopesMrC146555697ln7qwv06520031:24000
Murrill gravelly loam, 15 to 25 percent slopesMrD53555698ln7rwv06520031:24000
Murrill very stony loam, 3 to 15 percent slopesMsC3078555958lnj4wv60819731:20000
Murrill very stony loam, 15 to 25 percent slopesMsD2109555959lnj5wv60819731:20000
Murrill very stony loam, 25 to 35 percent slopesMsE1160555960lnj6wv60819731:20000
Murrill channery loam, clayey subsoil variant, 8 to 15 percent slopesMvC920555962lnj8wv60819731:20000
Murrill channery loam, clayey subsoil variant, 15 to 25 percent slopesMvD771555963lnj9wv60819731:20000
Murrill channery loam, 15 to 25 percent slopesMlD591555957lnj3wv60819731:20000
Murrill channery loam, 8 to 15 percent slopesMlC537555956lnj2wv60819731:20000
Murrill channery loam, clayey subsoil variant, 3 to 8 percent slopesMvB494555961lnj7wv60819731:20000
Murrill channery loam, 3 to 8 percent slopesMlB122555955lnj1wv60819731:20000
Murrill stony loam, 15 to 35 percent slopesMsD10425515948k9whwv62819801:20000
Murrill stony loam, 8 to 15 percent slopesMsC3555515947k9wgwv62819801:20000
Murrill stony loam, 35 to 65 percent slopesMsF1490515949k9wjwv62819801:20000
Murrill variant channery fine sandy loam, 8 to 15 percent slopesMvC1289515950k9wkwv62819801:20000
Murrill cherty silt loam, 8 to 15 percent slopesMlC957515945k9wdwv62819801:20000
Murrill variant channery fine sandy loam, 15 to 25 percent slopesMvD552515951k9wlwv62819801:20000
Murrill cherty silt loam, 15 to 25 percent slopesMlD471515946k9wfwv62819801:20000
Murrill channery loam, 30 to 60 percent slopes, very stonyMsF46892516656261cdwv7131:24000
Murrill channery loam, 15 to 30 percent slopes, very stonyMsD7362516655261ccwv7131:24000
Murrill channery silt loam, 5 to 15 percent slopesMuC5522516597k9z6wv7131:24000
Murrill channery silt loam, 15 to 30 percent slopesMuD5292516598k9z7wv7131:24000
Urban land-Murrill complex, 15 to 25 percent slopesUmD2572516610k9zwwv7131:24000

Map of Series Extent

Approximate geographic distribution of the MURRILL 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 .