Official Series Description


Lab Data Summary

Aggregate lab data for the NECONISH soil series. This aggregation is based on all pedons with a current taxon name of NECONISH, 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 NECONISH 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
9202N0710S2001MI131008Neconish6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7963867,-88.9367294
9202N0714S2001MI131013Neconishn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7988853,-88.9372864
94B95P0361S1994WI078420Neconish6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.9458351,-88.5494461

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the NECONISH 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 NECONISH 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 NECONISH 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 NECONISH 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 NECONISH 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 NECONISH 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 NECONISH 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.

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Click the image to view it full size.

Soil series sharing subgroup-level classification with NECONISH, 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 NECONISH 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
Neconish fine sand, 0 to 3 percent slopes986B61194151772zyttmi03319891:15840
Neconish loamy fine sand, outwash plain, 0 to 3 percent slopes984A472833400562zytvmi04319851:20000
Neconish fine sand, 0 to 3 percent slopes986B187033400572zyttmi10919851:20000
Rousseau-Neconish-Finch complex, 0 to 25 percent slopes20E952115431671nsslmi15320071:24000
Neconish-Kinross-Wainola complex, 0 to 6 percent slopes525B856014570461kx5hmi15320071:24000
Rousseau-Neconish-Deford complex, 0 to 25 percent slopes22E773515380361nmg2mi15320071:24000
Neconish-Deford, rarely flooded-Wainola complex, 0 to 6 percent slopes491B249016118201r376mi15320071:24000
Neconish loamy fine sand, 0 to 3 percent slopes639A2114444631kh2lwi00320061:12000
Neconish loamy fine sand, 0 to 3 percent slopes639A1035433710gk9nwi00720051:12000
Neconish loamy fine sand, 0 to 3 percent slopes639A62781408v73qwi03120051:12000
Neconish loamy fine sand, 0 to 3 percent slopes639A139782276v80qwi05120061:12000
Neconish fine sand, 0 to 3 percent slopes986B440033400582zyttwi07519871:20000
Neconish loamy fine sand, outwash plain, 0 to 3 percent slopes984A187033400592zytvwi07519871:20000
Neconish loamy fine sand, outwash plain, 0 to 3 percent slopes984A14133957842zytvwi07819981:12000
Neconish loamy fine sand, outwash plain, 0 to 3 percent slopes984A1813933400622zytvwi08319851:15840
Neconish fine sand, 0 to 3 percent slopes986B111533400612zyttwi08319851:15840
Neconish loamy fine sand, outwash plain, 0 to 3 percent slopes984A410733400642zytvwi11519811:15840

Map of Series Extent

Approximate geographic distribution of the NECONISH 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 .