Official Series Description


Lab Data Summary

Aggregate lab data for the LUHON soil series. This aggregation is based on all pedons with a current taxon name of LUHON, 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 LUHON 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
34A88P009787WY037005Luhon5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.038887,-109.7483368
34A80P0326S1980WY007005Luhon8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.9075012,-106.206665

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LUHON 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 LUHON 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 LUHON 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 LUHON 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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Competing Series

Soil series competing with LUHON 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 LUHON 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 LUHON 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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There are insufficient data to create the 3D mountains figure.

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

Soil series sharing subgroup-level classification with LUHON, 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. CO-2012-05-09-09 | Rio Grande County Area - February 1980

    Pattern of soils and parent material in Luhon-Garita-Travelers association (Soil Survey of Rio Grande County Area, Colorado; February 1980).

Map Units

Map units containing LUHON 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
Luhon loam, 3 to 9 percent slopes297350498597jqtsco63019751:24000
Luhon loam, 1 to 3 percent slopes286200498596jqtrco63019751:24000
Luhon loam, 1 to 3 percent slopesLuB16097498661jqwvco63119721:24000
Luhon loam, 3 to 6 percent slopesLuC6664498662jqwwco63119721:24000
Luhon loam, 0 to 3 percent slopes4317042498476jqpwco63319811:24000
Luhon loam, 3 to 6 percent slopes449299498477jqpxco63319811:24000
Guben-Luhon association, 0 to 20 percent slopes1461515224536862nc85co66419871:24000
Luhon-Travelers, extremely stony complex, 1 to 9 percent slopesLtC77708507830k1fmnm67019761:24000
Stunner-Travelers, extremely stony-Luhon association, 2 to 8 percent slopesSVC53382507888k1hhnm67019761:24000
Stunner-Luhon association, 1 to 8 percent slopesSUC8019507887k1hgnm67019761:24000
Luhon-Travelers complex, 3 to 7 percent slopesLtC11727702012v5psnm6721:24000
Nicks-Luhon, very stony complex, 8 to 35 percent slopesXSE296225045792q4kmut6291:24000
Luhon loam, moist, 3 to 15 percent slopes833260504481jxylut63619841:24000
Luhon loam, 2 to 5 percent slopes803093504478jxyhut63619841:24000
Luhon very cobbly sandy loam, 2 to 15 percent slopes841871504482jxymut63619841:24000
Luhon loam, gravelly substratum, 1 to 2 percent slopes81325504479jxyjut63619841:24000
Luhon loam, gravelly substratum, 2 to 5 percent slopes82293504480jxykut63619841:24000
Luhon, dry-Hickey, dry-Heath complex, 3 to 25 percent slopesNS74470932540352zw6yut6471:24000
Luhon, gravelly-Evanston complex, 3 to 30 percent slopesNS74935832540362zw6zut6471:24000
Luhon loam, 1 to 5 percent slopes18418799501727jv2rwy60119911:24000
Luhon-Rock River association, 0 to 10 percent slopes -- draft3141651823781142ktmcwy6301:24000
Luhon-Edlin complex, 1 to 7 percent slopes -- draft420853325161922qg2dwy6301:24000
Luhon-Edlin-Rock outcrop complex, 3 to 15 percent slopes -- draft421262425160422qftbwy6301:24000
Luhon-Luhon subirrigated complex, 0 to 3 percent slopes -- draft31514523785352kv1ywy6301:24000
Diamondville-Chaperton-Luhon complex, 1 to 6 percent slopes5415299614755711ljg2wy6351:24000
Luhon-Evanston complex, 3 to 30 percent slopes14919405504001jxg3wy63819901:24000
Brownsto-Luhon-McFadden complex, 3 to 15 percent slopes1117814503951jxdhwy63819901:24000
Brownsto-Luhon complex, 10 to 35 percent slopes1106856503949jxdfwy63819901:24000
Rockinchair-Luhon-Rentsac complex, 6 to 30 percent slopes1714662504031jxh2wy63819901:24000
Luhon channery loam, 2 to 8 percent slopes1473002503999jxg1wy63819901:24000
Luhon loam, 3 to 6 percent slopes1462936503998jxg0wy63819901:24000
Luhon-Hickey-Heath complex, 3 to 25 percent slopes1502224504004jxg6wy63819901:24000
Luhon-Rockinchair loams, 1 to 6 percent slopes1512199504005jxg7wy63819901:24000
Luhon loam, 0 to 3 percent slopes1451477503997jxfzwy63819901:24000
Luhon-Brownsto complex, 4 to 15 percent slopes1481451504000jxg2wy63819901:24000
Luhon-Rockinchair loams, 8 to 20 percent slopes22511884733704smgwwy6471:24000
Luhon-Rock River-Forelle complex, 1 to 10 percent slopes037952215755058y8wy6471:24000
Rockinchair-Luhon fine sandy loams, 3 to 12 percent slopes08440161577055938wy6471:24000
Fiveoh gravelly sandy loam, 1 to 6 percent slopes150367815741758szwy6471:24000
Forelle-Luhon complex, 1 to 10 percent slopes147D2415795259c7wy65620081:24000
Luhon-Rock River-Forelle complex, undulating65169190156621tqvwy67719751:24000
Luhon-Rock River-Forelle complex, undulating16918580503034jwfxwy71319861:24000
Forelle-Luhon loams, 1 to 10 percent slopes1474936503012jwf6wy71319861:24000
Langspring, clayey substratum-Luhon complex, 0 to 20 percent slopes -- draft7141515025724212pgp9wy7371:24000
Luhon-Rock River complex, 0 to 10 percent slopes -- draft7314132825724252pr26wy7371:24000
Luhon loam, 4 to 8 percent slopes -- draft5553532572289jx2hwy7371:24000
Forelle-Luhon complex, 3 to 10 percent slopes -- draft5142792572283jx1pwy7371:24000
Luhon channery loam, 8 to 20 percent slopes -- draft5922125723852pbjzwy7371:24000

Map of Series Extent

Approximate geographic distribution of the LUHON 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 .