Official Series Description


Lab Data Summary

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

Competing Series

Soil series competing with SIMEROI 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 SIMEROI 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 SIMEROI 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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 SIMEROI, 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 SIMEROI 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
Simeroi-Paint complex, 2 to 8 percent slopes104-B105932388382n40id7031:24000
Simeroi gravelly loam, 6 to 15 percent slopes190-CL44431736162sfzid7031:24000
Whitecloud-Simeroi complex, 2 to 8 percent slopes22929562831222shcid75219991:24000
Simeroi gravelly loam, 2 to 6 percent slopes18911482830772sfxid75219991:24000
Simeroi gravelly loam, 6 to 15 percent slopes1906429830792sfzid75219991:24000
Simeroi complex, 2 to 8 percent slopes1916238830802sg0id75219991:24000
Simeroi-Paint-Sanfelipe complex, 5 to 20 percent slopes1925756830812sg1id75219991:24000
Simeroi-Whitecloud complex, 2 to 8 percent slopes1933533830822sg2id75219991:24000
Simeroi very gravelly silt loam, 30 to 60 percent slopes2622549829772sbpid75219991:24000
ARTRW8/ARAR8 Simeroi, 4 to 20 percent slopes112719922322142dxsxid75219991:24000
Simeroi gravelly silt loam, 5 to 15 percent slopesSED928894341qs70id75219991:24000
Simeroi very gravelly silt loam, 30 to 60 percent slopes11262054315038951h8id75819981:24000
Simeroi-Zeale complex, 4 to 20 percent slopes1125342815038851h7id75819981:24000
Simeroi gravelly silt loam, cool, 2 to 25 percent slopesSC141528093201qs6yid75819981:24000
Simeroi gravelly silt loam, 5 to 15 percent slopesSED59028093211qs70id75819981:24000
Simeroi-Rubble land association, 5 to 65 percent slopesHSD13628093622mtwbid75819981:24000
Whitecloud-Simeroi complex, 2 to 8 percent slopes22985202363525xrkid75819981:24000
Simeroi-Buist complex, 5 to 30 percent slopesHBD8528093532mpx5id75819981:24000
Simeroi gravelly silt loam, 4 to 20 percent slopes11276715039051h9id75819981:24000
Simeroi gravelly silt loam, dry, 10 to 30 percent slopes2483428093141qs68id75819981:24000
Simeroi gravelly silt loam, 1 to 5 percent slopesSEC1159616022031qs6zid76120181:24000
Peaspear-Shagel, extremely bouldery-Simeroi complex, 4 to 40 percent slopesMVE976024341422mpxqid76120181:24000
Simeroi gravelly silt loam, dry, 10 to 30 percent slopes248612216021811qs68id76120181:24000
Simeroi gravelly silt loam, cool, 2 to 25 percent slopesSC506116022021qs6yid76120181:24000
Simeroi-Zeale complex, 4 to 20 percent slopes1125318728430472szmbid76120181:24000
Simeroi-Sparmo complex, 4 to 12 percent slopesSP2294416022061qs72id76120181:24000
Peaspear-Deecree-Simeroi complex, 5 to 30 percent slopesCHD211124340422mpthid76120181:24000
Simeroi-Westindian complex, 1 to 20 percent slopesHWD188324341302mpxbid76120181:24000
Simeroi very gravelly silt loam, 30 to 60 percent slopes1126164928430302szlqid76120181:24000
Simeroi-Buist complex, 5 to 30 percent slopesHBD155324341252mpx5id76120181:24000
Simeroi gravelly silt loam, 5 to 15 percent slopesSED142416022041qs70id76120181:24000
Simeroi, dry-Simeroi complex, 5 to 30 percent slopes249105716021821qs69id76120181:24000
Simeroi-Rubble land association, 5 to 65 percent slopesHSD92724379432mtwbid76120181:24000
Simeroi, very stony-Simeroi-Rock outcrop complex, 2 to 50 percent slopes1271469224330392mns4id76120181:24000
Simeroi-Whitecloud complex, 2 to 8 percent slopes19354929841692sg2id76120181:24000
Peaspear-Fulwider-Simeroi complex, 1 to 30 percent slopes1271937224330512mnsjid76120181:24000
Simeroi-Sparmo complex, 4 to 8 percent slopes10616723789282n42id76319981:24000
Simeroi-Paint complex, 2 to 8 percent slopes10414144789262n40id76319981:24000
Simeroi-Bealand association, 30 to 70 percent slopes10812573789302n44id76319981:24000
Simeroi-Slide-McCaleb complex, 1 to 6 percent slopes10710998789292n43id76319981:24000
Simeroi complex, 5 to 30 percent slopes1059005789272n41id76319981:24000
Ike-Simeroi-Rock outcrop complex, 25 to 60 percent slopes423925790232n74id76319981:24000
Simeroi gravelly silt loam, 5 to 12 percent slopes1003809789222n3wid76319981:24000
Simeroi gravelly silt loam, 2 to 5 percent slopes993233791222nbbid76319981:24000
Simeroi gravelly silt loam, dry, 10 to 30 percent slopes1033010789252n3zid76319981:24000
Simeroi gravelly silt loam, cool, 2 to 25 percent slopes1021258789242n3yid76319981:24000
Simeroi gravelly silt loam, 8 to 12 percent slopes1011130789232n3xid76319981:24000
Simeroi gravelly silt loam, 1 to 5 percent slopesSEC93528894311qs6zid76319981:24000
Simeroi gravelly silt loam, cool, 2 to 25 percent slopesSC86228894301qs6yid76319981:24000
Sanfelipe-Simeroi complex, 1 to 4 percent slopes98817791212nb9id76319981:24000
Simeroi-Rubble land association, 5 to 65 percent slopesHSD39428894502mtwbid76519751:24000
Simeroi-Sparmo complex, 4 to 12 percent slopesSP218128894561qs72id76519751:24000
Simeroi-Sparmo complex, 4 to 8 percent slopes106-B623632389422n42id7721:24000
Simeroi gravelly silt loam, 1 to 5 percent slopesSEC145432389491qs6zid7721:24000
Simeroi gravelly silt loam, cool, 2 to 25 percent slopes102-B144832389412n3yid7721:24000

Map of Series Extent

Approximate geographic distribution of the SIMEROI 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 .