Official Series Description


Lab Data Summary

Aggregate lab data for the NALCASE soil series. This aggregation is based on all pedons with a current taxon name of NALCASE, 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 NALCASE 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
3598P008697UT017002Nalcase5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.7676392,-111.4250031

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the NALCASE 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 NALCASE 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 NALCASE 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 NALCASE 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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Competing Series

Soil series competing with NALCASE 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 NALCASE 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 NALCASE 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 hills figure.

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 NALCASE, 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 NALCASE 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
Santrick-Nalcase-Rock outcrop complex, 1 to 15 percent slopes492281814723522v32zaz70720111:24000
Rock outcrop-Mathis-Nalcase complex, 10 to 50 percent slopes4653638940572v3q8az70720111:24000
Rock outcrop-Mathis-Nalcase complex, 10 to 50 percent slopes422061748176942v3q8az71120081:24000
Santrick-Nalcase-Rock outcrop complex, 1 to 15 percent slopes481931648177352v32zaz71120081:24000
Mespun-Nalcase-Bispen complex, 0 to 10 percent slopes2112639313869562rqrsaz71120081:24000
Mespun-Rock outcrop-Nalcase complex, 1 to 25 percent slopes228837416068002rqs3az71120081:24000
Bispen-Nalcase-Rock outcrop complex, 5 to 60 percent slopes9113028789882ttg8ut6421:63360
Mespun-Nalcase-Santrick complex, 1 to 8 percent slopes4775228789862ttg6ut6421:63360
Rizno-Nalcase complex, 2 to 15 percent slopes80327130302s7k0ut6421:63360
Rock outcrop-Nalcase complex, 2 to 30 percent slopes883358625074392q3s5ut68519901:24000
Rock outcrop-Santrick-Nalcase complex, 2 to 30 percent slopes91544725074472q70hut68519901:24000
Rock outcrop, Navajo Sandstone-Nalcase complex, 2 to 30 percent slopes50073756359752205hut68620041:24000
Rock outcrop, Navajo Sandstone-Mespun-Nalcase complex, 2 to 30 percent slopes50203429659765205xut68620041:24000
Kenzo-Nalcase complex, 2 to 15 percent slopes507313085598352085ut68620041:24000
Santrick-Nalcase-Bispen complex, 2 to 30 percent slopes5012261159757205nut68620041:24000
Rock outcrop-Nalcase complex, 2 to 15 percent slopes115426822478012fg0qut68820091:24000
Rock outcrop-Nalcase complex, 2 to 30 percent slopes472226630302rqy4ut6891:24000

Map of Series Extent

Approximate geographic distribution of the NALCASE 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 .