Official Series Description


Lab Data Summary

Aggregate lab data for the ALICE soil series. This aggregation is based on all pedons with a current taxon name of ALICE, 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 ALICE 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
67A84P023083NE007022Alice7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.582222,-103.5199966
67A87P063787NE165320Alice5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.0113907,-103.9130554

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ALICE 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 ALICE 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 ALICE 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 ALICE 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 ALICE 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 ALICE 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 ALICE 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 flats position figure.

Soil series sharing subgroup-level classification with ALICE, 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. NE-2012-02-08-04 | Banner County - October 1994

    Typical pattern of soils and parent material in the Tripp-Alice association (Soil Survey of Banner County, Nebraska; October 1994).

  2. NE-2012-02-13-58 | Morrill County - August 1985

    Pattern of soils, topography, and underlying material in the Tripp-Alice-Duroc association (Soil Survey of Morrill County, Nebraska; August 1985).

  3. NE-2012-02-13-60 | Morrill County - August 1985

    A generalized cross section of Morrill County that shows the relationship of parent material, soil associations, and elevation (Soil Survey of Morrill County, Nebraska; August 1985).

Map Units

Map units containing ALICE 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
Nelson-Alice fine sandy loams, rollingNe5546346087cm43mt60719701:24000
Alice fine sandy loam, 4 to 15 percent slopesAr17593458603105qmt60719701:24000
Alice fine sandy loam, 0 to 4 percent slopesAr33833470313105xmt61119711:24000
Alice fine sandy loam, 4 to 15 percent slopesAs16723470323105qmt61119711:24000
Alice fine sandy loam, 3 to 6 percent slopes5902696316924471tt42ne00719881:20000
Alice fine sandy loam, 0 to 3 percent slopes5901585416924461tt41ne00719881:20000
Alice fine sandy loam, 6 to 9 percent slopes, eroded5903265216924481tt43ne00719881:20000
Chappell-Alice-Broadwater complex, 0 to 3 percent slopes13716322293622dttxne03319891:20000
Chappell-Alice-Broadwater complex, 0 to 3 percent slopes13711435716988001v0r0ne04920001:24000
Chappell-Alice-Broadwater complex, 0 to 3 percent slopes1371157922195772dhn8ne10119901:20000
Alice fine sandy loam, 0 to 3 percent slopes5901896016925681tt7zne12319811:20000
Alice-Dix complex, 6 to 20 percent slopes5907794216925731tt84ne12319811:20000
Alice fine sandy loam, 3 to 6 percent slopes5902522716925691tt80ne12319811:20000
Alice fine sandy loam, 6 to 9 percent slopes, eroded5903406716925701tt81ne12319811:20000
Alice loamy fine sand, 0 to 3 percent slopes5904278516925671tt7yne12319811:20000
Alice-Dix complex, 3 to 6 percent slopes590694816925721tt83ne12319811:20000
Alice-Dix complex, 0 to 3 percent slopes590591616925711tt82ne12319811:20000
Alice fine sandy loam, 0 to 3 percent slopes59011379516537081shtfne15719651:20000
Alice fine sandy loam, 3 to 6 percent slopes5902368516537091shtgne15719651:20000
Alice loamy fine sand, 0 to 3 percent slopes5904239316537101shthne15719651:20000
Alice-Dix complex, 3 to 6 percent slopes590666222276932ds32ne15719651:20000
Alice fine sandy loam, 0 to 1 percent slopes590056722276702ds2bne15719651:20000
Alice fine sandy loam, 0 to 1 percent slopes59002852357844d0ccne16519931:20000
Alice fine sandy loam, 0 to 3 percent slopes59012555357845d0cdne16519931:20000
Alice fine sandy loam, 3 to 6 percent slopes59021044357846d0cfne16519931:20000
Alice fine sandy loam, 2 to 6 percent slopesAfB23963531372zj4ksd01919701:24000
Alice fine sandy loam, 6 to 9 percent slopesAfC6403531382zj4lsd01919701:24000
Alice fine sandy loam, 6 to 10 percent slopesP006C3325474372qt0ksd01919701:24000
Alice-Ucross complex, moist, 3 to 10 percent slopesP010C827680872qt11sd01919701:24000
Alice fine sandy loam, 2 to 9 percent slopesAaC2460355082cxh8sd04719801:24000
Alice fine sandy loam, dry, 2 to 9 percent slopesP004C40327331122qt14sd04719801:24000
Alice fine sandy loam, moist, 0 to 6 percent slopesP008B83027332352qt1ysd08120071:24000
Alice-Ucross complex, moist, 3 to 10 percent slopesP010C670827457052qt11wy01119781:24000
Alice-Ucross complex, moist, 10 to 30 percent slopesP010E448027457062qt13wy01119781:24000
Alice fine sandy loam, 6 to 10 percent slopesP006C155125474362qt0kwy01119781:24000
Alice fine sandy loam, 2 to 6 percent slopesP006B152525474352qt0jwy01119781:24000
Alice fine sandy loam, 6 to 10 percent slopes12537349198cqcgwy01119781:24000
Alice-Thedalund complex, 3 to 10 percent slopes1352934920930wnqwy01119781:24000
Alice-Ucross complex, cool, 3 to 10 percent slopesQ0807C41024392032mw5zwy01119781:24000
Alice-Ucross complex, cool, 10 to 30 percent slopesQ0807E15824392042mw60wy01119781:24000
Alice-Thedalund complex, 10 to 30 percent slopes14111349220cqd5wy01119781:24000
Alice fine sandy loam, 2 to 6 percent slopes1122349187cqc3wy01119781:24000
Alice-Phiferson fine sandy loams, 3 to 10 percent slopes1047240349521cqpwwy02719931:24000
Alice-Manter fine sandy loams, 0 to 6 percent slopes1033873349519cqptwy02719931:24000
Alice-Bayard fine sandy loams, 0 to 6 percent slopes103220291044453hp6wy03119981:24000
Treon-Alice-Phiferson complex, 0 to 6 percent slopes24557561045993hv5wy03119981:24000
Alice-Phiferson fine sandy loams, 3 to 10 percent slopes10442301044513hpdwy03119981:24000
Graystone-Alice fine sandy loams, 0 to 6 percent slopes16326121045183hrkwy03119981:24000
Alice-Recluse-Cedak fine sandy loams, 0 to 6 percent slopes10524801044523hpfwy03119981:24000
Phiferson-Alice, bedrock substratum, very fine sandy loams, 0 to 6 percent slopes19622631045523hsnwy03119981:24000
Alice variant fine sandy loam, 2 to 10 percent slopes2928349421cqlnwy04519841:24000
Alice-Phiferson fine sandy loams, 3 to 10 percent slopes105131216696591t1dzwy60920061:24000
Graystone-Alice fine sandy loams, 0 to 6 percent slopes15920016697661t1jfwy60920061:24000
Alice fine sandy loam, 0 to 3 percent slopes339631048193j28wy62119801:24000
Alice fine sandy loam, 3 to 6 percent slopes437781048293j2lwy62119801:24000
Dix-Alice complex, 10 to 40 percent slopes6E93751048963j4rwy71519741:20000
Alice fine sandy loam, 0 to 6 percent slopes2B72341048793j46wy71519741:20000
Alice fine sandy loam, 6 to 10 percent slopes2C39551048803j47wy71519741:20000
Dix-Alice complex, 0 to 10 percent slopes6C9351048953j4qwy71519741:20000
Alice fine sandy loam, 1 to 3 percent slopes8620014153721jht5wy71519741:20000

Map of Series Extent

Approximate geographic distribution of the ALICE 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 .