Official Series Description


Lab Data Summary

Aggregate lab data for the AHRS soil series. This aggregation is based on all pedons with a current taxon name of AHRS, 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 AHRS 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
43A89P07471989ID079003Ahrs6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.5356306,-115.8679972
43A75-ID-409075ID079004Ahrs3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.9115,-116.0139

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the AHRS 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 AHRS 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 AHRS 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 AHRS 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 AHRS 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 AHRS 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 AHRS 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 hills figure.

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

    Typical pattern of soils and underlying material in general soil map unit 1 (Soil Survey of St. Joe Area, Parts of Benewah and Shoshone Counties, Idaho; 2002).

  3. 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).

  4. ID-2011-06-01-16 | St. Joe Area, Parts of Benewah and Shoshone Counties - 2002

    Typical pattern of soils and underlying material in General Soil Map Unit 1 (Soil Survey of St. Joe Area, Parts of Benewah and Shoshone Counties, Idaho; 2002).

  5. 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).

  6. 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 AHRS 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
Honeyjones-Ahrs association, very rocky, 35 to 75 percent slopesHy5j592250206354p6id05720131:24000
Bouldercreek-Ahrs families, complex, weakly weathered metasedimentary belt geology, mountain slopes, south aspects2lg9m9828508732lg9mid60419811:24000
Ahrs family-Rock outcrop-Typic Vitrixerands family, complex, weakly weathered metasedimentary belt geology, mountain slopes, south aspects, dry2lg9p1628508742lg9pid60419811:24000
Rubble land-Ahrs family-Typic Haplocryands family, complex2lg08428508312lg08id60419811:24000
Typic Vitrixerands-Ahrs families, complex, weakly weathered metasedimentary belt geology, stream breaklands, south aspects2lgb6128508772lgb6id60419811:24000
Ahrs, moist-Honeyjones, warm complex 35 to 75 percent slopes78120226630071hnkwid60619761:24000
Honeyjones, warm-Ahrs complex, 35 to 65 percent slopes7727626630031hnkdid60619761:24000
Ahrs-Pinecreek association, 25 to 75 percent slopes2v71h6226629522v71hid60619761:24000
Ahrs gravelly ashy silt loam, 35 to 65 percent slopes7153426629981hng9id60619761:24000
Ahrs family-Rock outcrop-Typic Vitrixerands family, complex, weakly weathered metasedimentary belt geology, mountain slopes, south aspects, dry2lg9p528508892lg9pid60619761:24000
Honeyjones-Ahrs association, very rocky, 35 to 75 percent slopes4211862115345654p6id60819941:24000
Ahrs-Pinecreek association, 25 to 75 percent slopes5316581534642v71hid60819941:24000
Ahrs gravelly ashy silt loam, 35 to 75 percent slopes4989027430441hn4jid60819941:24000
Honeyjones-Ahrs association, 15 to 35 percent slopes41336815345554p5id60819941:24000
Honeyjones-Ahrs association, moderately acid, 35 to 75 percent slopes43260215345754p7id60819941:24000
Honeyjones-Ahrs association, 35 to 75 percent slopes1hn5h56227430401hn5hid60819941:24000
Honeyjones, warm-Ahrs complex, 35 to 65 percent slopes1hnkd26027430691hnkdid60819941:24000
Honeyjones-Ahrs complex, 15 to 35 percent slopes1hn8b15727430571hn8bid60819941:24000
Bouldercreek-Ahrs families, complex, weakly weathered metasedimentary belt geology, mountain slopes, south aspects2lg9m7929367752lg9mid60819941:24000
Ahrs gravelly ashy silt loam, 15 to 35 percent slopes1hnh97627430731hnh9id60819941:24000
Ahrs family-Rock outcrop-Typic Vitrixerands family, complex, weakly weathered metasedimentary belt geology, mountain slopes, south aspects, dry2lg9p5829368092lg9pid60819941:24000
Ahrs, moist-Honeyjones, warm complex 35 to 75 percent slopes1hnkw5427430711hnkwid60819941:24000
Rubble land-Ahrs family-Typic Haplocryands family, complex2lg084829368012lg08id60819941:24000
Huckle-Ahrs complex, 5 to 40 percent slopes2v73q4327430592v73qid60819941:24000
Typic Vitrixerands-Ahrs families, complex, weakly weathered metasedimentary belt geology, stream breaklands, south aspects2lgb61729367902lgb6id60819941:24000
Honeyjones, warm-Ahrs complex, 35 to 65 percent slopes772632413901451hnkdid62020131:24000
Ahrs gravelly ashy silt loam, 35 to 75 percent slopes902267713897461hn4jid62020131:24000
Ahrs-Pinecreek association, 25 to 75 percent slopes903114213897632v71hid62020131:24000
Huckle-Ahrs complex, 5 to 40 percent slopes681109113900312v73qid62020131:24000
Ahrs, moist-Honeyjones, warm complex 35 to 75 percent slopes78153113901601hnkwid62020131:24000
Honeyjones-Ahrs association, 35 to 75 percent slopes90852713897761hn5hid62020131:24000
Honeyjones-Ahrs complex, 15 to 35 percent slopes51048813898641hn8bid62020131:24000
Ahrs gravelly ashy silt loam, 15 to 35 percent slopes71624513900801hnh9id62020131:24000
Bouldercreek-Ahrs families, complex, weakly weathered metasedimentary belt geology, mountain slopes, south aspects47013864323970322lg9mid6701:24000
Ahrs family-Rock outcrop-Typic Vitrixerands family, complex, weakly weathered metasedimentary belt geology, mountain slopes, south aspects, dry4715980723970342lg9pid6701:24000
Typic Vitrixerands-Ahrs families, complex, weakly weathered metasedimentary belt geology, stream breaklands, south aspects4834708523970502lgb6id6701:24000
Humic Udivitrands-Ahrs-Goatrock families, complex, steep breaklands with avalanche chutes, weakly weathered belts, timber-brush-fern glade mosaic, south aspects4161980023968622lg44id6701:24000
Rubble land-Ahrs family-Typic Haplocryands family, complex199410823967422lg08id6701:24000
Honeyjones-Ahrs association, very rocky, 35 to 75 percent slopes54p63179285097854p6id6701:24000
Ahrs-Humic Udivitrands families, complex, weakly weathered metasedimentary belt geology, dissected stream headlands, north aspects475250923970412lg9xid6701:24000
Rubble land-Ahrs family, complex, breaklands and forest complex197151623967382lg04id6701:24000
Ahrs-Pinecreek association, 25 to 75 percent slopes2v71h142128509832v71hid6701:24000
Ahrs-Ahrs, slightly acid substratum-Humic Udivitrands families, complex, weakly weathered metasedimentary belt geology, dissected stream headlands, south aspects476118923970422lg9yid6701:24000
Ahrs gravelly ashy silt loam, 35 to 75 percent slopes1hn4j24729368201hn4jid6701:24000
Honeyjones-Ahrs association, 15 to 35 percent slopes54p5228285097754p5id6701:24000
Bouldercreek-Ahrs families, complex, weakly weathered metasedimentary belt geology, mountain slopes, south aspects2lg9m51228509022lg9mwa65119811:24000
Ahrs family-Rock outcrop-Typic Vitrixerands family, complex, weakly weathered metasedimentary belt geology, mountain slopes, south aspects, dry2lg9p14928509442lg9pwa65119811:24000

Map of Series Extent

Approximate geographic distribution of the AHRS 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 .