Official Series Description


Lab Data Summary

Aggregate lab data for the STUTTS soil series. This aggregation is based on all pedons with a current taxon name of STUTTS, 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 STUTTS 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
93B05N0184S2004MI131010Stutts6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.3989944,-89.0814667
94B01N0291S2000MI153002Stutts6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.1011124,-86.2116699
94B05N0176S2004MI003001Stutts6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.1602745,-86.6505356

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the STUTTS 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 STUTTS 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 STUTTS 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 STUTTS 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 STUTTS 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 STUTTS 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 STUTTS 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 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 STUTTS, 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 STUTTS 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
Stutts-Kalkaska complex, 6 to 15 percent slopes125D335716712831t33cmi00320071:24000
Stutts-Kalkaska complex, 0 to 6 percent slopes125B306316712821t33bmi00320071:24000
Stutts-Kalkaska complex, 15 to 35 percent slopes125E78216712841t33dmi00320071:24000
Zandi-Stutts complex, 6 to 18 percent slopes8103C74724419012mz00mi01319841:20000
Noseum-Zandi-Stutts complex, 1 to 6 percent slopes8103B1024419002myzzmi01319841:20000
Stutts loamy fine sand, 6 to 18 percent slopes430C166814561351kw73mi05320071:24000
Stutts-Zandi complex, 1 to 6 percent slopes656B84414563241kwf6mi05320071:24000
Stutts loamy fine sand, 18 to 35 percent slopes430D81614561361kw74mi05320071:24000
Stutts loamy fine sand, 1 to 6 percent slopes430B71214561341kw72mi05320071:24000
Stutts-Keweenaw complex, 6 to 18 percent slopes322C65414560621kw4rmi05320071:24000
Stutts-Keweenaw complex, 1 to 6 percent slopes322B59714560611kw4qmi05320071:24000
Annalake-Stutts-Arnheim, frequently flooded, complex, drainageway, 0 to 35 percent slopes694D51014563541kwg5mi05320071:24000
Stutts-Zandi complex, 6 to 18 percent slopes656C29814563251kwf7mi05320071:24000
Stutts-Keweenaw complex, 18 to 35 percent slopes322D20614560631kw4smi05320071:24000
Stutts-Zandi complex, 18 to 35 percent slopes656D11616072091qyfgmi05320071:24000
Stutts loamy fine sand, 35 to 55 percent slopes430E7814561371kw75mi05320071:24000
Zandi-Stutts complex, 6 to 18 percent slopes8103C756024838792pcp4mi06119891:20000
Stutts loamy fine sand, 18 to 60 percent slopes8123E319824846812pdj0mi06119891:20000
Kalkaska-Stutts-Cusino complex, 6 to 18 percent slopes8072C155924848612pdptmi06119891:20000
Kellogg-Stutts-Amnicon complex, 0 to 4 percent slopes8084B139224861652pg1wmi06119891:20000
Kalkaska-Stutts-Cusino complex, 0 to 6 percent slopes8072B114724848602pdpsmi06119891:20000
Kalkaska-Stutts complex, 6 to 18 percent slopes8045C102724848702pdq3mi06119891:20000
Kalkaska-Stutts complex, 1 to 6 percent slopes8045B90024848692pdq2mi06119891:20000
Noseum-Zandi-Stutts complex, 1 to 6 percent slopes8103B64224838782pcp3mi06119891:20000
Kalkaska-Pence-Stutts complex, 6 to 18 percent slopes8073C57924861202pg0fmi06119891:20000
Kalkaska-Pence-Stutts complex, 18 to 35 percent slopes8073D54224861212pg0gmi06119891:20000
Kalkaska-Stutts complex, 18 to 35 percent slopes8045D47524848712pdq4mi06119891:20000
Kalkaska-Stutts-Cusino complex, 18 to 35 percent slopes8072D41424848622pdpvmi06119891:20000
Zandi-Stutts-Loggerhead complex, 6 to 18 percent slopes8076C32624861612pg1rmi06119891:20000
Zandi-Stutts-Loggerhead complex, 0 to 6 percent slopes8076B31624861602pg1qmi06119891:20000
Kalkaska-Pence-Stutts complex, 35 to 50 percent slopes8073E30824861222pg0hmi06119891:20000
Kalkaska-Pence-Stutts complex, 0 to 6 percent slopes8073B18024861192pg0dmi06119891:20000
Stutts-Noseum-Karlin complex, 0 to 6 percent slopes8188B9924848672pdq0mi06119891:20000
Kalkaska-Stutts complex, 6 to 18 percent slopes8045C19624525432nb29mi07119921:20000
Kalkaska-Stutts complex, 1 to 6 percent slopes8045B19224525422nb28mi07119921:20000
Stutts-Noseum-Karlin complex, 0 to 6 percent slopes8188B18124508542n89tmi07119921:20000
Kalkaska-Stutts-Cusino complex, 0 to 6 percent slopes8072B12924753642p2tgmi07119921:20000
Kalkaska-Pence-Stutts complex, 6 to 18 percent slopes8073C10124753682p2tlmi07119921:20000
Stutts-Noseum-Karlin complex, 6 to 18 percent slopes8188C8024508552n89vmi07119921:20000
Kalkaska-Stutts complex, 18 to 35 percent slopes8045D6724525442nb2bmi07119921:20000
Kalkaska-Pence-Stutts complex, 18 to 35 percent slopes8073D5724753692p2tmmi07119921:20000
Kalkaska-Pence-Stutts complex, 0 to 6 percent slopes8073B5324753672p2tkmi07119921:20000
Kalkaska-Stutts-Cusino complex, 6 to 18 percent slopes8072C4224753652p2thmi07119921:20000
Kalkaska-Stutts-Cusino complex, 18 to 35 percent slopes8072D3624508532n89smi07119921:20000
Kalkaska-Pence-Stutts complex, 6 to 18 percent slopes8073C314216748031t6rxmi13120071:24000
Kalkaska-Stutts-Cusino complex, 6 to 18 percent slopes8072C272916748001t6rtmi13120071:24000
Kalkaska-Pence-Stutts complex, 18 to 35 percent slopes8073D240416748041t6rymi13120071:24000
Kalkaska-Stutts-Cusino complex, 0 to 6 percent slopes8072B231716747991t6rsmi13120071:24000
Stutts loamy fine sand, 18 to 60 percent slopes8123E207316748361t6szmi13120071:24000
Kalkaska-Pence-Stutts complex, 35 to 50 percent slopes8073E166216748051t6rzmi13120071:24000
Stutts-Noseum-Karlin complex, 0 to 6 percent slopes8188B138516748581t6tpmi13120071:24000
Zandi-Stutts complex, 6 to 18 percent slopes8103C98016748191t6sfmi13120071:24000
Zandi-Stutts-Loggerhead complex, 0 to 6 percent slopes8076B87516748071t6s1mi13120071:24000
Kalkaska-Pence-Stutts complex, 0 to 6 percent slopes8073B74316748021t6rwmi13120071:24000
Kalkaska-Stutts-Cusino complex, 18 to 35 percent slopes8072D67216748011t6rvmi13120071:24000
Noseum-Zandi-Stutts complex, 1 to 6 percent slopes8103B65816748181t6sdmi13120071:24000
Stutts-Loggerhead complex, 6 to 18 percent slopes8288C58316748891t6vpmi13120071:24000
Kellogg-Stutts-Amnicon complex, 0 to 4 percent slopes8084B51616748121t6s6mi13120071:24000
Kalkaska-Stutts complex, 6 to 18 percent slopes8045C43816745111t6ghmi13120071:24000
Zandi-Stutts-Loggerhead complex, 6 to 18 percent slopes8076C40816748081t6s2mi13120071:24000
Stutts-Keweenaw complex, 1 to 6 percent slopes8322B24416749201t6wpmi13120071:24000
Kalkaska-Stutts complex, 18 to 35 percent slopes8045D20316745121t6gjmi13120071:24000
Kalkaska-Stutts complex, 1 to 6 percent slopes8045B17416745101t6ggmi13120071:24000
Stutts-Loggerhead complex, 18 to 35 percent slopes8288D11416748901t6vqmi13120071:24000
Stutts-Noseum-Karlin complex, 6 to 18 percent slopes8188C7416748591t6tqmi13120071:24000
Stutts-Keweenaw complex, 6 to 18 percent slopes8322C7316749211t6wqmi13120071:24000
Stutts-Keweenaw complex, 18 to 35 percent slopes8322D4616749221t6wrmi13120071:24000
Stutts loamy fine sand, 6 to 18 percent slopes8430C4316749551t6xtmi13120071:24000
Stutts-Kalkaska complex, 0 to 6 percent slopes125B634914570101kx4bmi15320071:24000
Stutts-Kalkaska complex, 6 to 15 percent slopes125D133414570351kx54mi15320071:24000
Stutts-Kalkaska complex, 15 to 35 percent slopes125E53816119221r3bhmi15320071:24000

Map of Series Extent

Approximate geographic distribution of the STUTTS 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 .