Official Series Description


Lab Data Summary

Aggregate lab data for the OLMITZ soil series. This aggregation is based on all pedons with a current taxon name of OLMITZ, 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 OLMITZ 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
10605KS10304705KS103047Olmitz3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2299728,-95.0884476
10605KS10314405KS103144Olmitz3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2131386,-95.0167618
10606KS00560306KS005603Olmitz3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5041656,-95.3000031
10607KS00550607KS005506Olmitz3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4548607,-95.3658066
10694P041794KS013003Olmitz7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.668575,-95.778825
10695KS177174s95KS177174sOlmitz1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1142235,-95.8450546
10606N0949S2006KS005001Olmitz5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4236694,-95.2695111
108D40A1442S1956IA001003Olmitz4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3836098,-94.4661102
108D40A1443S1956IA001004Olmitz3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3791656,-94.4558334
115BM87211041987MO211004Olmitz2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the OLMITZ 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 OLMITZ 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 OLMITZ 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 OLMITZ 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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Click the image to view it full size.

Competing Series

Soil series competing with OLMITZ 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 OLMITZ 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 OLMITZ 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 OLMITZ, 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-2010-09-02-15 | Jefferson County - 1999

    Typical pattern of soils and parent material in the Ladoga-Hedrick-Gara association (Soil Survey of Jefferson County, Iowa; 1999).

  2. IA-2010-09-02-19 | Jefferson County - 1999

    Typical pattern of soils and parent material in the Taintor-Mahaska-Otley association (Soil Survey of Jefferson County, Iowa; 1999).

  3. IA-2010-09-02-21 | Keokuk County - 2003

    Typical pattern of soils and parent material in the Otley-Mahaska-Nira association (Soil Survey of Keokuk County, Iowa; 2003).

  4. IA-2010-09-03-04 | Van Buren County - 2004

    Typical pattern of soils and parent material in the Kniffin-Rinda-Gara association (Soil Survey of Van Buren County, Iowa; 2004).

  5. IA-2010-09-09-01 | Adams County - 2008

    Typical pattern of soils and parent material in the Ladoga-Gara soil association (Soil Survey of Adams County, Iowa; 2008).

  6. IA-2010-09-09-03 | Adams County - 2008

    Typical pattern of soils and parent material in the Sharpsburg-Shelby association (Soil Survey of Adams County, Iowa; 2008).

  7. IA-2010-09-09-04 | Adams County - 2008

    Typical pattern of soils and parent material in the Zook-Nodaway association (Soil Survey of Adams County, Iowa; 2008).

  8. IA-2011-05-31-10 | Davis County - 1991

    Typical pattern of soils and parent material in the Armstrong-Gara-Kniffin association (Soil Survey of Davis County, Iowa; 1991).

  9. IA-2011-05-31-55 | Jefferson County - 1999

    Typical pattern of soils and parent material in the Taintor-Mahaska-Otley association (Soil Survey of Jefferson County, Iowa; 1999).

  10. IA-2011-05-31-56 | Jefferson County - 1999

    Typical pattern of soils and parent material in the Ladoga-Hedrick-Gara association (Soil Survey of Jefferson County, Iowa; 1999).

  11. IA-2011-06-01-13 | Lucas County - 1999

    Typical pattern of soils and parent material in the Arispe-Lamoni-Shelby association (Soil Survey of Lucas County, Iowa; 1999).

  12. IA-2011-06-01-14 | Lucas County - 1999

    Typical pattern of soils and parent material in the Gara-Pershing-Armstrong association (Soil Survey of Lucas County, Iowa; 1999).

  13. IA-2011-06-01-16 | Lucas County - 1999

    Relationship of the major soils in Lucas County to parent material and to position on the landscape (Soil Survey of Lucas County, Iowa; 1999).

  14. IA-2011-06-01-20 | Montgomery County - 1989

    Typical pattern of soils and parent material in the Gara-Ladoga association (Soil Survey of Montgomery County, Iowa; 1989).

  15. IA-2011-06-01-40 | Ringgold County - 1992

    Typical pattern of soils and parent material in the Gara-Armstrong-Pershing association (Soil Survey of Ringgold County, Iowa; 1992).

  16. IA-2011-06-01-41 | Ringgold County - 1992

    Typical pattern of soils and parent material in the Arispe-Shelby-Lamoni association (Soil Survey of Ringgold County, Iowa; 1992).

  17. IA-2011-06-01-42 | Ringgold County - 1992

    Relationship of the major soils in Ringgolg County to parent material and to position on the landscape (Soil Survey of Ringgold County, Iowa; 1992).

Map Units

Map units containing OLMITZ 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
Olmitz loam, 2 to 5 percent slopes273B6044021682wxs8ia00119761:15840
Olmitz loam, 5 to 9 percent slopes273C5664021692wxs9ia00119761:15840
Olmitz-Ely-Zook complex, 2 to 5 percent slopes15B444119139962wxscia00320081:12000
Olmitz loam, 5 to 9 percent slopes273C49814048912wxs9ia00320081:12000
Olmitz loam, 2 to 5 percent slopes273B40914048902wxs8ia00320081:12000
Olmitz-Vesser-Colo complex, 2 to 5 percent slopes13B25019402646fhzlia00719701:15840
Olmitz loam, heavy till, 2 to 5 percent slopes273B8594026722tkb8ia00719701:15840
Olmitz loam, 5 to 9 percent slopes273C10324027702wxs9ia00919821:15840
Olmitz loam, 2 to 5 percent slopes273B17518680402wxs8ia02920101:12000
Olmitz-Ely-Zook complex, 2 to 5 percent slopes15B824230092wxscia02920101:12000
Olmitz-Zook-Colo complex, 0 to 5 percent slopes13B22397404103fkhlia03919871:15840
Olmitz loam, heavy till, 2 to 5 percent slopesS273B10564041332tkb8ia03919871:15840
Olmitz loam, heavy till, 5 to 9 percent slopesS273C9684041342tkb6ia03919871:15840
Olmitz loam, 5 to 9 percent slopesY273C42429482342wxs9ia03919871:15840
Olmitz loam, 2 to 5 percent slopesY273B27029482332wxs8ia03919871:15840
Olmitz-Vesser-Zook complex, 0 to 5 percent slopes13B198684046522tkb9ia05119881:15840
Olmitz loam, heavy till, 2 to 5 percent slopes273B4814046752tkb8ia05119881:15840
Olmitz-Zook-Vesser complex, 0 to 5 percent slopes13B23857404762fl5via05319861:15840
Olmitz loam, heavy till, 2 to 5 percent slopes273B14124047902tkb8ia05319861:15840
Olmitz loam, heavy till, 5 to 9 percent slopes273C8864047912tkb6ia05319861:15840
Olmitz variant loam, 5 to 10 percent slopes1273C746405197flmwia05719801:15840
Olmitz variant loam, 2 to 5 percent slopes1273B330405196flmvia05719801:15840
Olmitz-Colo, occasionally flooded, complex, 0 to 5 percent slopes271B125234063542xbm7ia07719681:15840
Olmitz loam, 2 to 5 percent slopes273B27304063712wxs8ia07719681:15840
Olmitz loam, 5 to 9 percent slopes273C23344063722wxs9ia07719681:15840
Olmitz loam, 2 to 5 percent slopes273B1427407645fp5via09919751:15840
Olmitz loam, 5 to 9 percent slopes273C495407646fp5wia09919751:15840
Olmitz-Zook-Vesser complex, 0 to 5 percent slopes13B79574077382yvjkia10119921:15840
Olmitz loam, 2 to 5 percent slopes273B204407774fpb0ia10119921:15840
Olmitz-Zook-Vesser complex, 0 to 5 percent slopes13B182674470312yvjkia10719981:12000
Olmitz loam, 5 to 9 percent slopes273C505447065h06gia10719981:12000
Olmitz loam, 2 to 5 percent slopes273B502408751fqbjia11519841:15840
Olmitz loam, 5 to 9 percent slopes273C466408752fqbkia11519841:15840
Zook-Olmitz-Vesser complex, 0 to 5 percent slopes13B228654088612wjgbia11719911:15840
Olmitz loam, heavy till, 2 to 5 percent slopes273B7324089172tkb8ia11719911:15840
Olmitz loam, heavy till, 5 to 9 percent slopes273C6074089182tkb6ia11719911:15840
Olmitz loam, 5 to 9 percent slopes273C11174092382wxs9ia12119681:15840
Olmitz loam, 2 to 5 percent slopes273B11014092372wxs8ia12119681:15840
Olmitz loam, 2 to 5 percent slopes273B502409300fqx7ia12319711:15840
Olmitz loam, 5 to 9 percent slopes273C237409301fqx8ia12319711:15840
Olmitz loam, heavy till, 5 to 9 percent slopes273C7144127572tkb6ia12519761:15840
Olmitz loam, 2 to 5 percent slopes273B4234127562wxs8ia12519761:15840
Olmitz-Colo-Vesser complex, 2 to 5 percent slopes13B18170409748frcpia13519821:15840
Olmitz loam, heavy till, 5 to 9 percent slopes273C9714097672tkb6ia13519821:15840
Olmitz loam, 2 to 5 percent slopes273B5354098552wxs8ia13719871:15840
Olmitz loam, 5 to 9 percent slopes273C3014098562wxs9ia13719871:15840
Olmitz loam, 2 to 5 percent slopes273B5844102062wxs8ia14519751:20000
Olmitz loam, 5 to 9 percent slopes273C3974102072wxs9ia14519751:20000
Olmitz loam, 2 to 5 percent slopes273B1197410570fs76ia15719781:15840
Olmitz loam, 5 to 9 percent slopes273C516410571fs77ia15719781:15840
Olmitz-Zook-Humeston complex, 0 to 5 percent slopes13B31848410653fs9wia15919871:15840
Olmitz loam, heavy till, 5 to 9 percent slopesS273C17364106862tkb6ia15919871:15840
Olmitz loam, heavy till, 2 to 5 percent slopes273B13834106852tkb8ia15919871:15840
Olmitz loam, 5 to 9 percent slopesY273C42229482442wxs9ia15919871:15840
Olmitz loam, 3 to 9 percent slopes273C501410950fsmgia16319891:15840
Olmitz loam, 2 to 5 percent slopes273B10584116102wxs8ia17319891:15840
Olmitz loam, 5 to 9 percent slopes273C6734116112wxs9ia17319891:15840
Olmitz loam, 2 to 5 percent slopes273B7554117032wxs8ia17519751:15840
Olmitz-Vesser-Zook complex, 0 to 5 percent slopes13B35564130172tkb9ia17719941:12000
Olmitz loam, heavy till, 2 to 5 percent slopes273B2124130472tkb8ia17719941:12000
Olmitz loam, heavy till, 5 to 9 percent slopes273C504130482tkb6ia17719941:12000
Olmitz loam, 5 to 9 percent slopes273C11234119192wxs9ia18119751:15840
Olmitz loam, 2 to 5 percent slopes273B5134119182wxs8ia18119751:15840
Zook-Olmitz-Vesser complex, 0 to 5 percent slopes13B3473224225392wjgbia18519661:15840
Olmitz loam, heavy till, 2 to 5 percent slopes273B237718604752tkb8ia18519661:15840
Olmitz clay loam, 1 to 5 percent slopes745067524202802m7hkks00519981:24000
Olmitz loam, 1 to 5 percent slopes74551302115217517nxyks01319941:24000
Olmitz clay loam, 1 to 5 percent slopes7450282214803551lpfdks08519761:24000
Olmitz loam, 1 to 5 percent slopes74557214803561lpffks08519761:24000
Olmitz clay loam, 1 to 5 percent slopes745029624202812m7hlks08719741:24000
Olmitz clay loam, 1 to 5 percent slopes745048724202822m7hmks10319731:24000
Olmitz loam, 1 to 5 percent slopes7455218114570851kx6rks11719771:24000
Olmitz loam, 1 to 5 percent slopes7455497414060261j62pks13119801:24000
Olmitz loam, 1 to 5 percent slopes74557216522771sgb8ks14919841:24000
Olmitz loam, 1 to 5 percent slopes745553716522751sgb6ks17719661:24000
Olmitz loam, 3 to 9 percent slopes1011255825212932qkzwmo00319861:24000
Olmitz-Ely-Zook complex, 2 to 5 percent slopes3024281526718472wxscmo00519881:24000
Olmitz loam, 2 to 5 percent slopes3016054025314032wxs8mo00519881:24000
Olmitz loam, 3 to 9 percent slopes1011275525212922qkzwmo02119841:24000
Olmitz-Zook-Vesser complex, 2 to 5 percent slopes302413426076692qs1jmo04719821:24000
Olmitz-Zook-Vesser complex, 2 to 5 percent slopes3024120026076972qs1jmo04919811:24000
Olmitz loam, heavy till, 2 to 5 percent slopes30246189825314042tkb8mo07519821:24000
Olmitz loam, heavy till, 2 to 5 percent slopes3024635925314052tkb8mo11519871:24000
Olmitz-Zook-Vesser complex, 2 to 5 percent slopes3024129425445122qs1jmo12919931:24000
Olmitz loam, 2 to 5 percent slopes30160449325314062wxs8mo14719831:24000
Olmitz-Ely-Zook complex, 2 to 5 percent slopes30242253926718482wxscmo14719831:24000
Olmitz loam, heavy till, 2 to 5 percent slopes3024669229832532tkb8mo14719831:24000
Olmitz-Kennebec complex, 2 to 5 percent slopes3024023326718462qs1hmo14719831:24000
Olmitz loam, 3 to 9 percent slopes10112225212912qkzwmo14719831:24000
Olmitz loam, heavy till, 2 to 5 percent slopes30246229825314072tkb8mo21119901:24000
Olmitz loam, heavy till, 5 to 9 percent slopes3024710168883672tkb6mo21119901:24000
Olmitz-Kennebec complex, 2 to 5 percent slopes302401869825445112qs1hmo22719651:24000
Olmitz loam, heavy till, 2 to 5 percent slopes30246378625314022tkb8mo22719651:24000
Olmitz-Kennebec complex, 0 to 5 percent slopes3016257625314082qnsgmo22719651:24000
Olmitz loam, 2 to 5 percent slopes3016055029482532wxs8mo22719651:24000
Olmitz-Ely-Zook complex, 2 to 5 percent slopes302422926076952wxscmo22719651:24000
Olmitz loam, 2 to 6 percent slopes8110278916914381ts2jne15519951:12000

Map of Series Extent

Approximate geographic distribution of the OLMITZ 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 .