Official Series Description


Lab Data Summary

Aggregate lab data for the OBSERVATION soil series. This aggregation is based on all pedons with a current taxon name of OBSERVATION, 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 OBSERVATION 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 OBSERVATION 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 OBSERVATION 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 OBSERVATION 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 OBSERVATION 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 OBSERVATION 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 OBSERVATION 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 OBSERVATION 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 flats position figure.

Soil series sharing subgroup-level classification with OBSERVATION, 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 OBSERVATION 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
Observation-Searles-Madeline association, 9 to 30 percent slopes30016011487619jcdnca60820001:24000
Observation-Searles-Madeline association, 30 to 50 percent slopes3017572487621jcdqca60820001:24000
Pequop-Observation association, 30 to 50 percent slopes3151086487648jcflca60820001:24000
Pequop-Observation association, 15 to 30 percent slopes314966487646jcfjca60820001:24000
Observation-Searles-Madeline association4934413871511hkftca68520061:24000
Observation-Searles-Madeline association, 9 to 30 percent slopes300su151189884921qx6ca70319831:24000
Merlin-Observation complex, 2 to 20 percent slopes199m1479634261182mqpor6181:24000
Ateron-Observation-Tweener complex, 2 to 15 percent slopesN8101142434261752mtsor6181:24000
Polkbutte-Merlin-Observation complex, 15 to 50 percent north slopes7301072134321902mktor6181:24000
Observation-Bonnieview complex, 2 to 40 percent south slopes5711057034260992mkwor6181:24000
Observation-Ateron-Polkbutte complex, 0 to 35 percent slopes283104623432191tgbror6181:24000
Observation-Bonnieview-Erakatak complex, 10 to 45 percent south slopes27997533432192tgbtor6181:24000
Observation-Merlin-Erakatak complex, 2 to 20 percent slopesQ570945034346602mlwor6181:24000
Observation-Bonnieview-Ateron complex, 0 to 50 percent slopesB451934634346612mrkor6181:24000
Observation-Cadlebutte complex, 0 to 15 percent slopes27757403434812sqfhor6181:24000
Bonnieview-Observation-Anatone complex, 12 to 30 percent south slopes26552303434817132ryor6181:24000
Polkbutte-Merlin-Observation complex, 5 to 40 percent slopesQ730473734320942mlvor6181:24000
Observation-Wickiser-Bonnieview complex, 0 to 50 percent north slopes2541694343752421vh3or6181:24000
Powellbutte-Observation complex, 0 to 15 percent slopesBL144120034350211t1llor6181:24000
Observation-Lambring-Rock outcrop association, 20 to 50 percent slopes244m30034347072mrgor6181:24000
Observation-Teguro complex, 2 to 20 percent slopes243m23334347342mrhor6181:24000
Magill-Observation association, 5 to 40 percent slopes368m12434347052msyor6181:24000
Observation-Rock outcrop complex, 5 to 20 percent slopes241m2934346762mrjor6181:24000
Observation-Erakatak-Merlin complex, 2 to 20 percent slopes242173426397nk6yor6181:24000
Magill-Observation association, 5 to 40 percent slopes4409BO52433852902msyor62620181:24000
Merlin-Observation complex, 2 to 20 percent slopes4403AO28533854282mqpor62620181:24000
Observation-Sylvaille complex, 2 to 15 percent slopes4309AO20233854762m7gmor62620181:24000
Observation-Erakatak-Merlin complex, 2 to 20 percent slopes4340NO1083385424nk6yor62620181:24000
Observation-Sylvaille complex, 2 to 15 percent slopes273C804234262212m7gmor6271:24000
Observation-Erakatak-Merlin complex, 2 to 20 percent slopes24220113426393nk6yor6271:24000
Daxty-Observation complex, 5 to 30 percent slopes278D154634294672m7gxor6271:24000
Observation-Fopiano-Badland complex, 15 to 50 percent slopes275E53634320262m7gvor6271:24000
Polkbutte-Merlin-Observation complex, 5 to 40 percent slopesQ73037434321012mlvor6271:24000
Merlin-Observation complex, 2 to 20 percent slopes19949628490577jgh2or62819971:24000
Observation-Lambring-Rock outcrop association, 20 to 50 percent slopes24417040490641jgk4or62819971:24000
Westbutte-Observation association, 5 to 40 percent slopes36812542490801jgq9or62819971:24000
Observation-Rock outcrop complex, 5 to 20 percent slopes2418648490638jgk1or62819971:24000
Observation-Royst-Merlin complex, 2 to 30 percent slopes2428024490639jgk2or62819971:24000
Ateron-Observation association, 5 to 30 percent slopes207895490581jgh6or62819971:24000
Ticino-Observation complex, 2 to 20 percent slopes3296509490754jgnsor62819971:24000
Merlin-Observation complex, 20 to 40 percent north slopes2006310490582jgh7or62819971:24000
Observation stony loam, 2 to 20 percent slopes2403608490636jgjzor62819971:24000
Vitale-Observation complex, 2 to 20 percent slopes3453481490774jgpfor62819971:24000
Observation-Teguro complex, 2 to 20 percent slopes2433392490640jgk3or62819971:24000
Anatone-Teguro-Observation complex, 2 to 20 percent slopes92225490968jgwpor62819971:24000
Observation-Booth complex, 0 to 15 percent slopes184C6494489011jdvkor63619911:24000
Merlin-Observation complex, 2 to 15 percent slopes9033490527222902sf3sor6451:24000
Bingville-Ateron-Observation, clay pan, complex, 5 to 40 percent south slopes085E845234217042r5c3or6771:24000
Observation-Finsel-Ateron complex, 10 to 30 percent north slopes476C61273421737261m7or6771:24000
Observation-Ateron-Rock outcrop complex, 10 to 30 percent south slopes474D2182342184325xttor6771:24000
Observation-Bonnieview complex, 2 to 40 percent south slopes57176134244362mkwor6771:24000
Merlin-Observation complex, 2 to 20 percent slopes199m49934245232mqpor6771:24000
Ateron-Observation-Tweener complex, 2 to 15 percent slopesN8105234248332mtsor6771:24000

Map of Series Extent

Approximate geographic distribution of the OBSERVATION 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 .