Official Series Description


Lab Data Summary

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

There are insufficient data to create the lab data summary figure.


Water Balance

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

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 ATTEWAN, 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 ATTEWAN 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
Attewan loams, 2 to 4 percent slopesTw13966342054cgy0mt02119711:24000
Attewan loam, 2 to 4 percent slopesTt13440342051cgxxmt02119711:24000
Attewan loam, 0 to 2 percent slopesTs12176342050cgxwmt02119711:24000
Attewan complex, 4 to 15 percent slopesBm10091341996cgw4mt02119711:24000
Attewan loams, 4 to 8 percent slopesTy9759342055cgy1mt02119711:24000
Attewan loams, 0 to 2 percent slopesTv8050342053cgxzmt02119711:24000
Attewan fine sandy loam, 1 to 4 percent slopesTr5466342049cgxvmt02119711:24000
Attewan loam, 4 to 8 percent slopesTu2946342052cgxymt02119711:24000
Attewan-Tinsley complex, 2 to 8 percent slopes272C2988343890cjv7mt04119941:24000
Attewan loam, 0 to 4 percent slopes27B1385343891cjv8mt04119941:24000
Attewan loam, 0 to 4 percent slopes27B1114344165ck43mt05119921:24000
Attewan-Tinsley complex, 2 to 8 percent slopes272C258344164ck42mt05119921:24000
Crago-Musselshell-Attewan complex, 1 to 4 percent slopes56A13763344599cgklmt06519961:24000
Attewan-Niart loams, 0 to 4 percent slopes57C3828344602ckl6mt06519961:24000
Eapa-Attewan loams, 0 to 2 percent slopes152A3124344485cghwmt06519961:24000
Attewan loam, 1 to 4 percent slopes57A2522344600cgkmmt06519961:24000
Crago-Musselshell-Attewan complex, 1 to 4 percent slopes, fan356A156717138181vfzrmt06519961:24000
Attewan cobbly loam, 0 to 4 percent slopes57B46344601ckl5mt06519961:24000
Attewan loam, 0 to 4 percent slopes67675344729ckq9mt06919891:24000
Crago-Musselshell-Attewan complex, 0 to 2 percent slopes282351344694ckp5mt06919891:24000
Evanston-Attewan loams, 0 to 2 percent slopes371140344704ckphmt06919891:24000
Attewan loam, 0 to 4 percent slopes27B1921345113cl3pmt10119921:24000
Attewan sandy loam, 0 to 4 percent slopes272B239345112cl3nmt10119921:24000
Attewan loam, 0 to 4 percent slopes36015345545clkmmt10519761:24000
Attewan sandy loam, 0 to 4 percent slopesAk78391467604xq6mt60019691:24000
Attewan sandy loam, 4 to 8 percent slopesAm37451467614xq7mt60019691:24000
Attewan loam, 0 to 4 percent slopesAn17171467624xq8mt60019691:24000
Attewan loam, 4 to 8 percent slopesAo12471467634xq9mt60019691:24000
Attewan-Nippt complex, 0 to 2 percent slopes193A13721482754z92mt60420011:24000
Attawan-Varney complex, 1 to 4 percent slopes193B3024508392n89bmt60420011:24000
Attewan cobbly loam, cool, 2 to 8 percent slopes12C96091144xbbmt60420011:24000
Attewan-Beaverell complex, 0 to 4 percent slopes421666346457cmj1mt60819761:24000
Attewan loam, 0 to 4 percent slopes319282346415cmgpmt60819761:24000
Attewan-Wabek complex, 0 to 4 percent slopes53854346484cmjxmt60819761:24000
Attewan-Nippt complex, 0 to 2 percent slopes193A108825976764z92mt61220111:24000
Attewan-Varney complex, 1 to 4 percent slopes193B80324201102m7b2mt61220111:24000
Attewan-Tinsley complex, 2 to 8 percent slopes272C5588346657cmqhmt61519921:24000
Attewan loam, 0 to 4 percent slopes27B3489346658cmqjmt61519921:24000
Attewan clay loam, 0 to 4 percent slopes33B161815540556q2mt62219971:24000
Attewan loam, 0 to 4 percent slopes57B3867191242322612mt62420211:24000
Attewan-Niart complex, 0 to 4 percent slopes486B2882191242522614mt62420211:24000
Crago-Musselshell-Attewan complex, 0 to 2 percent slopes496A1789190377921x17mt62420211:24000
Eapa-Attewan loams, 0 to 2 percent slopes152A14282513996cghwmt62420211:24000
Crago-Attewan cobbly loams, 2 to 8 percent slopes95C495347537cnmwmt62420211:24000
Crago-Musselshell-Attewan complex, 1 to 4 percent slopes, fan356A2331768621vfzrmt62420211:24000
Attewan-Nippt complex, 0 to 2 percent slopes3513A3315166152t9mt62719981:24000
Attewan loam, 0 to 2 percent slopes413A26761478114yt3mt63019911:24000
Attewan-Nippt complex, 0 to 2 percent slopes513A23331478394yv0mt63019911:24000
Nippt-Attewan-Beaverell complex, 0 to 4 percent slopes306A20781477824ys5mt63019911:24000
Nippt-Attewan complex, 0 to 2 percent slopes506A12281478364ytxmt63019911:24000
Yamacall-Attewan loams, 0 to 2 percent slopes569A3981478594yvnmt63019911:24000
Attewan cobbly loam, cool, 2 to 8 percent slopes12188241463924xbbmt63619831:24000
Attewan loam, cool, 2 to 8 percent slopes1144641463814x9zmt63619831:24000
Attewan loam, cool, 0 to 2 percent slopes1039531463704x9mmt63619831:24000
Attewan very stony loam, cool, 2 to 8 percent slopes1336471464034xbpmt63619831:24000
Attewan loam, 0 to 4 percent slopes448B12001500155136mt63920001:24000
Sieben-Attewan gravelly loams, 0 to 4 percent slopes443B2701500095130mt63920001:24000
Attewan-Beaverell complex, 0 to 8 percent slopes110C10629347576cnp4mt64119941:24000
Attewan loam, 0 to 4 percent slopes112765348140cp8bmt65519751:24000
Attewan loam, seeped, 0 to 4 percent slopes121846348141cp8cmt65519751:24000
Attewan-Beaverell gravelly loams, 0 to 4 percent slopes131366348142cp8dmt65519751:24000
Attewan-Wabek complex, 0 to 8 percent slopes216C6205348444cpl4mt65719901:24000
Attewan fine sandy loam, 0 to 4 percent slopes116B588348306cpfpmt65719901:24000
Crago-Musselshell-Attewan complex, 1 to 4 percent slopes, fan356A1584817115331vfzrmt66620081:24000
Crago-Musselshell-Attewan complex, 1 to 4 percent slopes56A3652341700cgklmt66620081:24000
Eapa-Attewan loams, 0 to 2 percent slopes152A2146341647cghwmt66620081:24000
Eapa-Attewan loams, 0 to 2 percent slopes, fan352A185217115271vfzkmt66620081:24000
Attewan loam, 1 to 4 percent slopes57A458341701cgkmmt66620081:24000
Beaverell, stony-Attewan complex, 0 to 4 percent slopes321B4330156905588gmt6691:24000
Beaverell-Attewan complex, 0 to 4 percent slopes721A3224156949589wmt6691:24000
Beaverell, extremely stony-Attewan-Beaverell, very stony complex, 0 to 8 percent slopes3402C2416156701581wmt6691:24000
Attewan-Vendome, stony complex, 0 to 4 percent slopes428B589156916588tmt6691:24000
Attewan loam, 2 to 6 percent slopesAwB5252355717cy4rsd06319841:24000
Nihill variant-Attewan complex, 4 to 40 percent slopesNaD3889355771cy6hsd06319841:24000
Nihill-Attewan complex, 4 to 20 percent slopesNaD4880355453cxw7sd60119831:24000
Attewan loam, 1 to 6 percent slopes -- Draft20AB15248053nqwy6291:24000

Map of Series Extent

Approximate geographic distribution of the ATTEWAN 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 .