Official Series Description


Lab Data Summary

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

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
105X49-315-2S1982IA097005Perks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.1269757,-90.8603521
105X49-315-1S1988IA097036Perks1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.1095451,-90.795814
n/aX49-000-11S1988IA097936Perks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PERKS 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 PERKS 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 PERKS 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 PERKS 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 mountains figure.

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Competing Series

Soil series competing with PERKS 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 PERKS 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 PERKS 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 .

Click the image to view it full size.

Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with PERKS, 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. IA-2011-06-01-11 | Louisa County - 1980

    Pattern of soils and parent material in the Titus-Ambraw-Colo association (Soil Survey of Louisa County, Iowa; 1980).

  2. IA-2011-06-01-26 | Muscatine County - 1989

    Typical pattern of soils and parent material in the Ambraw-Aquolls-Colo association (Soil Survey of Muscatine County, Iowa; 1989).

Map Units

Map units containing PERKS 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
Sigglekov-Perks, channeled-Shandep, ponded, complex, 0 to 2 percent slopes, frequently flooded158622464132872y8r7ia01320011:12000
Sigglekov-Perks, channeled-Shandep, ponded, complex, 0 to 2 percent slopes, frequently flooded1586632722202632y8r7ia01720081:12000
Perks-Spillville complex, 0 to 2 percent slopes, channeled, frequently flooded13153691190222930qvtia03120081:12000
Perks variant, sand, 0 to 2 percent slopes1139440404644fl21ia05119881:15840
Klum-Perks-Nodaway complex, 1 to 3 percent slopes3153540406850fnc6ia08719821:15840
Klum-Perks-Nodaway complex, channeled, 1 to 3 percent slopes13151015406805fn9ria08719821:15840
Chaseburg-Perks complex, 0 to 2 percent slopes1282643407448fnzhia09719881:15840
Nodaway-Klum-Perks complex, 0 to 3 percent slopes315462407794fpbnia10119921:15840
Perks loamy sand, 1 to 3 percent slopes139150407736fp8sia10119921:15840
Perks-Spillville complex, 0 to 2 percent slopes, channeled, frequently flooded1315469140793930qvtia10319791:15840
Amana-Lawson-Perks complex, 0 to 2 percent slopes24221705407983fpjria10319791:15840
Perks sandy loam, 0 to 2 percent slopes, occasionally flooded53919840802730qvria10319791:15840
Perks-Chaseburg complex, 0 to 2 percent slopes, frequently flooded315761540813830qvsia10519881:15840
Perks sandy loam, 0 to 2 percent slopes, occasionally flooded53941640818130qvria10519881:15840
Coland-Perks-Lawson complex, frequently flooded, 0 to 2 percent slopes15398650408723fq9mia11519841:15840
Perks loamy sand, 0 to 3 percent slopes, occasionally flooded139239340871830qvvia11519841:15840
Perks sandy loam, 0 to 2 percent slopes, occasionally flooded539152340878930qvria11519841:15840
Perks sandy loam, rarely flooded, 0 to 3 percent slopes3539628408766fqc0ia11519841:15840
Perks sandy loam, 0 to 2 percent slopes, occasionally flooded539339941000530qvria13919861:15840
Perks loamy sand, 0 to 3 percent slopes, occasionally flooded139116140992130qvvia13919861:15840
Ambraw-Perks-Lawson complex, frequently flooded, 0 to 2 percent slopes15396335410882fsk8ia16319891:15840
Nodaway-Perks complex, channeled, 0 to 5 percent slopes1730B835410914fsl9ia16319891:15840
Perks sandy loam, 0 to 2 percent slopes, occasionally flooded53965141102030qvria16319891:15840
Perks loamy sand, 0 to 3 percent slopes, occasionally flooded13936441088030qvvia16319891:15840
Nodaway-Klum-Perks complex, 0 to 3 percent slopes, occasionally flooded3151885413063fvtmia17719941:12000
Perks loamy sand, 0 to 2 percent slopes, rarely flooded3139438413054fvtbia17719941:12000
Nodaway-Klum-Perks complex, 0 to 3 percent slopes, rarely flooded3315380413067fvtria17719941:12000
Perks loamy sand, 2 to 5 percent slopes, rarely flooded139B361413016fvs3ia17719941:12000
Perks loamy sand, 0 to 2 percent slopes, occasionally flooded13952413015fvs2ia17719941:12000
Landes-Perks-Nodaway complex, 1 to 3 percent slopes, frequently flooded315252030046882xjd8ia17919781:15840
Nodaway-Perks complex, 0 to 2 percent slopes, frequently flooded715400141208830qvwia18319831:15840
Perks sandy loam, 0 to 2 percent slopes, occasionally flooded5398541206430qvria18319831:15840
Perks loamy sand, 0 to 2 percent slopes, occasionally flooded660982836888766yttwmo04519921:24000

Map of Series Extent

Approximate geographic distribution of the PERKS 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 .