Official Series Description


Lab Data Summary

Aggregate lab data for the HUGUS soil series. This aggregation is based on all pedons with a current taxon name of HUGUS, 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 HUGUS 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
43A02N1053S2002ID009003Hugus7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.0849991,-116.9530563
43A02N1047S2002ID057005Hugus6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.0283318,-116.5905533

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HUGUS 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 HUGUS 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 HUGUS 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 HUGUS 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 HUGUS 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 HUGUS 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 HUGUS 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 HUGUS, 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. ID-2010-08-31-07 | St. Joe Area, Parts of Benewah and Shoshone Counties - 2002

    Typical pattern of soils and underlying material in general soil map unit 7 (Soil Survey of St. Joe Area, Parts of Benewah and Shoshone Counties, Idaho; 2002).

  2. ID-2010-08-31-09 | St. Joe Area, Parts of Benewah and Shoshone Counties - 2002

    Typical pattern of soils and underlying material in general soil map unit 2 (Soil Survey of St. Joe Area, Parts of Benewah and Shoshone Counties, Idaho; 2002).

  3. ID-2011-06-01-17 | St. Joe Area, Parts of Benewah and Shoshone Counties - 2002

    Typical pattern of soils and underlying material in General Soil Map Unit 2 (Soil Survey of St. Joe Area, Parts of Benewah and Shoshone Counties, Idaho; 2002).

  4. ID-2011-06-01-20 | St. Joe Area, Parts of Benewah and Shoshone Counties - 2002

    Typical pattern of soil and underlying material in General Soil Map Unit 7(Soil Survey of St. Joe Area, Parts of Benewah and Shoshone Counties, Idaho; 2002).

Map Units

Map units containing HUGUS 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
Hugus-Chesley complex, 20 to 60 percent slopesHu63353644898pn25id05720131:24000
Hugus ashy silt loam, dry, 25 to 65 percent slopesHu7927677873qrcwid05720131:24000
Hugus-Chesley-Arson complex, 20 to 55 percent slopesHu876213875141hktjid05720131:24000
Hugus ashy silt loam, 35 to 75 percent slopesHu2j5512501190v268id05720131:24000
Hugus-Dworshak complex, 15 to 35 percent slopesHd1j2452501184v262id05720131:24000
Tigley, moist-Hugus complex, 30 to 65 percent slopes7585926630011hnk0id60619761:24000
Hugus-Honeyjones-Goshawk families, complex, weathered belts, lower sideslopes toeslopes and stream bottoms of drainages in uplands, south aspects2lg9q2928508902lg9qid60619761:24000
Hugus-Honeyjones families, complex, moderately weathered metasedimentary belt geology, mountain ridges and upper slopes, north aspects2lgbc2328508922lgbcid60619761:24000
Hugus-Goshawk-Minaloosa families, complex, weakly to moderately weathered belt geology, dissected rolling uplands, south aspects2lg9v2328508912lg9vid60619761:24000
Hugus-Honeyjones families, complex, moderately weathered metasedimentary belt geology, mountain slopes, north aspects2lg981728508872lg98id60619761:24000
Hugus-Bouldercreek-Humic Udivitrands families, complex, moderately weathered belts, lower sideslopes toeslopes and stream bottoms of incised drainages, north aspects2lg9c1328508882lg9cid60619761:24000
Tigley-Hugus association, 30 to 65 percent slopes883177515350654qtid60819941:24000
Hugus silt loam, 30 to 65 percent slopes461369515346054pbid60819941:24000
Hugus gravelly loam, very strongly acid, 30 to 65 percent slopes, severely eroded45198215345954p9id60819941:24000
Hugus ashy silt loam, high precipitation, 30 to 65 percent slopes47104615346154pcid60819941:24000
Hugus gravelly silt loam, moderately acid, 30 to 65 percent slopes4848215346254pdid60819941:24000
Hugus cobbly silt loam, very strongly acid, 30 to 65 percent slopes4939415346354pfid60819941:24000
Hugus-Honeyjones families, complex, moderately weathered metasedimentary belt geology, mountain slopes, south aspects2lg9d8829368052lg9did60819941:24000
Hugus-Chesley complex, 20 to 60 percent slopesHu6712663018pn25id60819941:24000
Hugus-Bouldercreek-Humic Udivitrands families, complex, moderately weathered belts, lower sideslopes toeslopes and stream bottoms of incised drainages, north aspects2lg9c5729367972lg9cid60819941:24000
Hugus-Honeyjones families, complex, moderately weathered metasedimentary belt geology, mountain slopes, north aspects2lg984029367772lg98id60819941:24000
Hugus-Honeyjones families, complex, moderately weathered metasedimentary belt geology, mountain ridges and upper slopes, north aspects2lgbc3229367742lgbcid60819941:24000
Tigley, moist-Hugus complex, 30 to 65 percent slopes1hnk02327430681hnk0id60819941:24000
Hugus-Honeyjones families, complex, weak to moderately weathered belt rock, dissected mountain slopes, north aspects2lg8r1829367992lg8rid60819941:24000
Typic Vitrixerands-Hugus-Honeyjones families, complex, moderately weathered belt rock, dissected breaklands, south aspects2lgb51129368082lgb5id60819941:24000
Bouldercreek-Hubub-Hugus families, complex, moderately weathered belt rock, dissected lower mountain slopes toeslopes and stream bottoms, south aspects2lg4d829367892lg4did60819941:24000
Hugus-Goshawk-Minaloosa families, complex, weakly to moderately weathered belt geology, dissected rolling uplands, south aspects2lg9v329367932lg9vid60819941:24000
Hugus-Bouldercreek families, complex, weak to moderately weathered belt rock, dissected mountain slopes, south aspects2lg4c129367852lg4cid60819941:24000
Hugus, moist-Hugus complex, 35 to 75 percent slopes1122344776683v269id61220031:24000
Hugus ashy silt loam, 35 to 75 percent slopes1092073776682v268id61220031:24000
Hugus ashy silt loam, 15 to 35 percent slopes108927776681v267id61220031:24000
Hugus ashy silt loam, moist, 15 to 30 percent slopes110637776685v26cid61220031:24000
Hugus-Dworshak complex, 15 to 35 percent slopes113330776676v262id61220031:24000
Hugus ashy silt loam, moist, 30 to 65 percent slopes111184776684v26bid61220031:24000
Tigley, moist-Hugus complex, 30 to 65 percent slopes758173313901331hnk0id62020131:24000
Hugus ashy silt loam, warm, 30 to 65 percent slopes75799513901291hnjwid62020131:24000
Hugus-Honeyjones families, complex, moderately weathered metasedimentary belt geology, mountain slopes, north aspects4625108323970212lg98id6701:24000
Hugus-Bouldercreek-Humic Udivitrands families, complex, moderately weathered belts, lower sideslopes toeslopes and stream bottoms of incised drainages, north aspects4633031623970242lg9cid6701:24000
Hugus-Honeyjones families, complex, moderately weathered metasedimentary belt geology, mountain slopes, south aspects4642241023970252lg9did6701:24000
Hugus-Goshawk-Minaloosa families, complex, weakly to moderately weathered belt geology, dissected rolling uplands, south aspects4731973523970392lg9vid6701:24000
Hugus-Honeyjones families, complex, moderately weathered metasedimentary belt geology, mountain ridges and upper slopes, north aspects4901327623970552lgbcid6701:24000
Garveson-Hugus-Humic Udivitrands families, complex, weathered granitics, lower sideslopes toeslopes and stream bottoms of drainages, rolling uplands, south aspects5171159923970652lgbpid6701:24000
Hugus-Honeyjones-Goshawk families, complex, weathered belts, lower sideslopes toeslopes and stream bottoms of drainages in uplands, south aspects472711423970352lg9qid6701:24000
Hugus-Bouldercreek families, complex, weak to moderately weathered belt rock, dissected mountain slopes, south aspects446472323968692lg4cid6701:24000
McWillar-Hugus-Goshawk families, complex, weakly weathered metasedimentary belt geology, mountain slopes, south aspects, brushy openings474460323970402lg9wid6701:24000
Hugus-Honeyjones families, complex, weak to moderately weathered belt rock, dissected mountain slopes, north aspects449436423970052lg8rid6701:24000
Bouldercreek-Hugus-Humic Udivitrands families, complex, moderately weathered belt rock, dissected breaklands, north aspects481310323970482lgb4id6701:24000
Garveson-Hugus-Humic Udivitrands families, complex, weathered granitics, lower sideslopes toeslopes and stream bottoms of drainages, rolling uplands, north aspects518299423970662lgbqid6701:24000
Hubub-Bouldercreek-Hugus families, complex, weathered belt geology, dissected rolling uplands, north aspects461237423970192lg96id6701:24000
Rettig-Hugus families, complex, moderately weathered mica schist, lower sideslopes toeslopes and stream bottoms of incised drainages along slopes, north aspects763235323974712lgrsid6701:24000
Bouldercreek-Hubub-Hugus families, complex, moderately weathered belt rock, dissected lower mountain slopes toeslopes and stream bottoms, south aspects447232523968702lg4did6701:24000
Typic Vitrixerands-Hugus-Honeyjones families, complex, moderately weathered belt rock, dissected breaklands, south aspects482213423970492lgb5id6701:24000
Rettig-Hugus families, complex, moderately weathered mica schist geology, mountain slopes, north aspects762198523974702lgrrid6701:24000
Typic Vitrixerands-Township-Hugus families, complex, moderately weathered mica schist geology, dissected breaklands, south aspects782194223974852lgs7id6701:24000
Hubub-Flewsie-Hugus families, complex, belts, lower sideslopes toesloes and stream bottoms of incised drainages in rolling uplands, north aspects456181623970112lg8yid6701:24000
Bouldercreek-Hugus families, complex, stream terraces, toe slopes, and alluvial fans131142823967092lfz6id6701:24000
Rettig-Hugus families, complex, moderately weathered mica schist geology, mountain slopes, south aspects764124923974722lgrtid6701:24000
Bouldercreek-Humic Udivitrands families, complex, weakly weathered schists, lower sideslopes toeslopes and stream bottoms of incised drainages along slopes, south aspects76879823974762lgryid6701:24000
Hugus-Honeyjones families, complex, moderately weathered metasedimentary belt geology, mountain ridges and upper slopes, south aspects49268823970572lgbfid6701:24000
Rettig-Hugus families, complex, moderately weathered mica schist geology, dissected, breaklands, north aspects78160723974842lgs6id6701:24000
Humic Udivitrands-Bouldercreek-Hugus families, complex, weathered, rotational failures19844923967392lg05id6701:24000
Tigley-Hugus association, 30 to 65 percent slopes54qt168285100654qtid6701:24000
Hugus silt loam, 30 to 65 percent slopes54pb139285098154pbid6701:24000
Rettig-Hugus families, complex, moderately weathered mica schist, lower sideslopes toeslopes and stream bottoms of incised drainages along slopes, south aspects76512023974732lgrvid6701:24000
Rettig-Hugus-Grandad families, complex, moderately weathered mica schist geology, mountain ridges and upper sideslopes, north aspects7908723974892lgscid6701:24000
Hugus ashy silt loam, high precipitation, 30 to 65 percent slopes54pc67285098254pcid6701:24000
Hugus gravelly loam, very strongly acid, 30 to 65 percent slopes, severely eroded54p925285098054p9id6701:24000
Garveson-Hugus-Humic Udivitrands families, complex, weathered granitics, lower sideslopes toeslopes and stream bottoms of drainages, rolling uplands, south aspects2lgbp65628509392lgbpwa65119811:24000

Map of Series Extent

Approximate geographic distribution of the HUGUS 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 .