Official Series Description


Lab Data Summary

Aggregate lab data for the MELHORN soil series. This aggregation is based on all pedons with a current taxon name of MELHORN, 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 MELHORN 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
43C95P0906S1995OR001009Melhorn6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.9627762,-117.069725

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MELHORN 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 MELHORN 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 MELHORN 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 MELHORN 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 terrace figure.

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

Competing Series

Soil series competing with MELHORN 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 MELHORN series and competing. 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 MELHORN 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 terrace figure.

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

Soil series sharing subgroup-level classification with MELHORN, 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

No block diagrams are available.

Map Units

Map units containing MELHORN 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
Klicker-Melhorn-Fivebeaver complex, 30 to 60 percent slopes5767CO48625939061r1hsor60419881:24000
Melhorn-Getaway-Klicker complex, 15 to 30 percent slopes5768BO32325939071q6yxor60419881:24000
Hunsaker-Klicker-Melhorn complex, 30 to 60 percent slopes5735CO32225938991r1gwor60419881:24000
Melhorn-Klicker-Fivebeaver complex, 15 to 30 percent slopes5766BO17625939051r1hror60419881:24000
McCartycreek-Melhorn-Anatone complex, 30 to 60 percent slopes5807CO13325939131r1pror60419881:24000
Melhorn-Hunsaker-Klicker complex, 15 to 30 percent slopes5734BO7125938981r1gvor60419881:24000
Melhorn-Fivebeaver complex, 0 to 15 percent slopes5765AO6825939041r1hqor60419881:24000
Bolobin-Melhorn-Fivebeaver complex, 30 to 60 percent slopes5990CO539631202321nvhmor60720181:24000
Melhorn-Larabee complex, 15 to 30 percent slopes4954BE266231203301qy20or60720181:24000
Klicker-Melhorn-Humarel complex, 60 to 90 percent slopes5029DO266231203381qy77or60720181:24000
Melhorn-Larabee-Dunstan complex, 15 to 30 percent slopes5017BO121631205231r1bhor60720181:24000
Melhorn-Larabee-Klickson complex, depositional, 30 to 60 percent slopes4947CD110931204951r190or60720181:24000
Klicker-Melhorn-Humarel complex, 30 to 60 percent slopes5029CO104531205291r1bpor60720181:24000
Larabee-Fivebeaver-Melhorn complex, depositional, 30 to 60 percent slopes4937CD55031204901r18qor60720181:24000
Bolobin-Melhorn complex, 0 to 15 percent slopes4946AO45731204931r18xor60720181:24000
Melhorn-Getaway-Klicker complex, 15 to 30 percent slopes5768BO9231202511q6yxor60720181:24000
Bolobin-Melhorn complex, depositional, 15 to 30 percent slopes4946BD5631204941r18yor60720181:24000
Melhorn-Humarel-Klicker complex, landslide, 30 to 60 percent slopes5029CL3731205281r1bnor60720181:24000
Melhorn-Hunsaker-Klicker complex, 15 to 30 percent slopes5734BO3431205351r1gvor60720181:24000
Melhorn-Larabee-Dunstan complex, mass failure, 15 to 30 percent slopes5017BM12312079021svnor60720181:24000
Melhorn-Larabee-Gaib complex, 20 to 50 percent north slopes4018BO2312016821zpbor60720181:24000
Larabee-Melhorn-Rock outcrop complex, 50 to 90 percent north slopes418F534263162dv47or6181:24000
Melhorn-Larabee-Gaib complex, 20 to 50 percent north slopes418E2342615921zpbor6181:24000
Melhorn-Larabee complex, 15 to 30 percent slopes4954BE183931221641qy20or62620181:24000
Bolobin-Melhorn complex, 0 to 15 percent slopes4946AO107331223061r18xor62620181:24000
Larabee-Fivebeaver-Melhorn complex, depositional, 30 to 60 percent slopes4937CD79631223031r18qor62620181:24000
Melhorn-Larabee-Gaib complex, 20 to 50 percent north slopes4018BO587338531821zpbor62620181:24000
Larabee-Melhorn-Rock outcrop complex, 50 to 90 percent north slopes4018DO58733853192dv47or62620181:24000
Melhorn-Larabee-Dunstan complex, 0 to 15 percent slopes5017AO25931223391r1bgor62620181:24000
Melhorn-Larabee-Dunstan complex, 15 to 30 percent slopes5017BO24531223401r1bhor62620181:24000
Bolobin-Melhorn complex, depositional, 15 to 30 percent slopes4946BD18531223071r18yor62620181:24000
Melhorn-Larabee-Klickson complex, depositional, 30 to 60 percent slopes4947CD14531223081r190or62620181:24000
Melhorn-Larabee-Dunstan complex, mass failure, 15 to 30 percent slopes5017BM26312251821svnor62620181:24000
Klicker-Melhorn-Humarel complex, 30 to 60 percent slopes5029CO1231223431r1bpor62620181:24000
Melhorn-Larabee-Gaib complex, 20 to 50 percent north slopes418E6724342515621zpbor6271:24000
Larabee-Melhorn-Rock outcrop complex, 50 to 90 percent north slopes418F290134263102dv47or6271:24000
Melhorn-Larabee complex, 15 to 30 percent slopes4954BE95334252131qy20or6271:24000
Larabee-Melhorn-Gaib complex, 2 to 20 percent slopes418C50534320281vtl3or6271:24000
Melhorn-Larabee-Dunstan complex, 0 to 15 percent slopes5017AO20534318871r1bgor6271:24000
Melhorn-Larabee-Klickson complex, 30 to 60 percent slopes, depositional4947CD15234298112ktzlor6271:24000
Larabee-Fivebeaver-Melhorn complex, depositional, 30 to 60 percent slopes4937CD14634260311r18qor6271:24000
Bolobin-Melhorn complex, 0 to 15 percent slopes4946AO11834318761r18xor6271:24000
Bolobin-Melhorn complex, depositional, 15 to 30 percent slopes4946BD2234319361r18yor6271:24000
Melhorn-Larabee-Dunstan complex, 15 to 30 percent slopes5017BO134318881r1bhor6271:24000
Klicker-Melhorn-Fivebeaver complex, 30 to 60 percent slopes5767CO537224372931r1hsor63120181:24000
McCartycreek-Melhorn-Anatone complex, 30 to 60 percent slopes5807CO399324373311r1pror63120181:24000
Bocker-Klicker-Melhorn complex, 15 to 30 percent slopes5803BO323824373281r1pnor63120181:24000
Melhorn-Klicker-Fivebeaver complex, 15 to 30 percent slopes5766BO309624372921r1hror63120181:24000
Hunsaker-Klicker-Melhorn complex, 30 to 60 percent slopes5735CO186524372691r1gwor63120181:24000
Melhorn-Getaway-Klicker complex, 15 to 30 percent slopes5768BO171524372941q6yxor63120181:24000
Larabee-Melhorn-Anatone complex, 0 to 15 percent slopes5876AO133424373961r2bjor63120181:24000
Melhorn-Getaway-Kamela complex, 30 to 60 percent slopes5769CO106124372951r1p1or63120181:24000
Larabee-Melhorn-Anatone complex, 30 to 60 percent slopes5876CO100824373981r2blor63120181:24000
Larabee-Anatone-Melhorn complex, 15 to 30 percent slopes5876BO88024373971r2bkor63120181:24000
Bocker-Melhorn-Klicker complex, 0 to 15 percent slopes5802AO53524373271r1pmor63120181:24000
Larabee-Melhorn complex, 0 to 15 percent slopes6071AO5102437455nj8wor63120181:24000
Melhorn-Kamela complex, 15 to 30 percent slopes5854BO43324373691r294or63120181:24000
Melhorn-Hunsaker-Klicker complex, 15 to 30 percent slopes5734BO36024372681r1gvor63120181:24000
Melhorn-Fivebeaver complex, 0 to 15 percent slopes5765AO34124372911r1hqor63120181:24000
Larabee-Melhorn complex, 0 to 15 percent slopes177140845502tzfor67019991:24000
Melhorn-Larabee-Gaib complex, 20 to 50 percent north slopes418E133342475121zpbor6771:24000
Bolobin-Melhorn-Fivebeaver complex, 30 to 60 percent slopes5990CO6134249511nvhmor6771:24000
Larabee-Fivebeaver-Melhorn complex, depositional, 30 to 60 percent slopes4937CD2834249781r18qor6771:24000
Melhorn-Larabee complex, 15 to 30 percent slopes4954BE1434249581qy20or6771:24000

Map of Series Extent

Approximate geographic distribution of the MELHORN 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 .