Official Series Description


Lab Data Summary

Aggregate lab data for the BATA soil series. This aggregation is based on all pedons with a current taxon name of BATA, 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 BATA 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
43B75C0004S1974MT063009Bata6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.2840538,-113.5848312

Water Balance

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

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 BATA, 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 BATA 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
Holloway-Evaro-Bata families, complex, steep ridges and mountain slopes51ND32593300507750hxmt60319891:24000
Bata gravelly ashy silt loam, 8 to 30 percent slopes86E187300505457q6mt60319891:24000
Bata gravelly ashy silt loam, 2 to 8 percent slopes86C13300505357q4mt60319891:24000
Hollandlake-Bata complex, 4 to 30 percent slopes541029955014wcpmt60319891:24000
Waldbillig-Bata-Upsata families, complex, glacial moraines347Sa5870814934550dlmt60520071:24000
Upsata-Bata-Petty families, complex, glacial moraines348Sa324941485894zm6mt60520071:24000
Garlet-Holloway-Bata families, complex, moderately steep mountain slopes537Sa2562814936150f3mt60520071:24000
Waldbillig-Bata-Lowder, frequently flooded families, complex, cirque basins257Sa2312614934850dpmt60520071:24000
Upsata-Bata-Lowder, frequently flooded families, complex, cirque basins258Sa2013914935350dvmt60520071:24000
Bata-Petty-Worock families, complex, alluvial fans683Sa1786314936250f4mt60520071:24000
Bata-Holloway-Garlet families, complex, gentle mountain slopes527Sa13227149093504gmt60520071:24000
Petty-Como-Bata families, complex, gentle mountain slopes528Sa1273114935650dymt60520071:24000
Rubycreek-Bata-Lowder, frequently flooded families, complex, trough bottoms237Ua109271491165056mt60520071:24000
Bata-Rubycreek-Lowder, frequently flooded families, complex, alluvial-colluvial deposits basins613Ua3507640647phn1mt60520071:24000
Bata-Littlesalmon-Lowder, frequently flooded families, complex, landslide deposits708Ua3123637476pdbrmt60520071:24000
Garlet-Bata families-Rock outcrop complex, steep glaciated mountain slopes and ridges15UD2308185959320f1wmt60520071:24000
Waldbillig-Bata-Upsata families, complex, glacial moraines347Sa268415312201ndc6mt61020051:24000
Upsata-Bata-Petty families, complex, glacial moraines348Sa47015312101ndbwmt61020051:24000
Bata-Petty-Worock families, complex, alluvial fans683Sa38915312131ndbzmt61020051:24000
Bata-Holloway-Garlet families, complex, gentle mountain slopes527Sa37815312251ndccmt61020051:24000
Garlet-Holloway-Bata families, complex, moderately steep mountain slopes537Sa36315903311qcw0mt61020051:24000
Petty-Como-Bata families, complex, gentle mountain slopes528Sa24515312141ndc0mt61020051:24000
Rubycreek-Bata-Lowder families, complex, trough bottoms237Ua8415312221ndc8mt61020051:24000
Garlet-Holloway-Bata families, complex, moderately steep mountain slopes537Sa1755259777850f3mt61220111:24000
Bata-Holloway-Garlet families, complex, gentle mountain slopes527Sa13972597755504gmt61220111:24000
Waldbillig-Bata-Upsata families, complex, glacial moraines347Sa407259777550dlmt61220111:24000
Bata gravelly ashy loam, 15 to 35 percent slopes66E448154981568dmt61620031:24000
Bata gravelly ashy silt loam, 15 to 50 percent slopes92F85614524871krffmt61820081:24000
Bata gravelly loam, 15 to 35 percent slopes66E3601445464vdsmt62119971:24000
Bata gravelly loam, 8 to 15 percent slopes66D661445454vdrmt62119971:24000
Bata gravelly silt loam, 30 to 60 percent slopes47271451744w21mt62919911:20000
Bata gravelly silt loam, 8 to 30 percent slopes31561451324w0pmt62919911:20000
Ovando-Littlesalmon-Bata families complex, steep glaciated mountain slopes and ridges15GDE9917035131v5n1mt63119881:24000
Holloway-Evaro-Bata families, complex, steep ridges and mountain slopes51ND33085714944850hxmt63520061:24000
Ovando-Littlesalmon-Bata families, complex, steep glaciated mountain slopes and ridges15GDE2765614937750fmmt63520061:24000
Waldbillig-Bata families-Rock outcrop complex, moderately steep trough bottoms37UD22129914943550hhmt63520061:24000
Garlet family-Rock outcrop-Bata family, complex, steep glaciated mountain slopes and ridges15UD3545114938550fwmt63520061:24000
Ovando-Bata families-Rock outcrop complex, moderately steep young moraines21UE2474814940450ghmt63520061:24000
Garlet-Bata families-Rock outcrop complex, steep glaciated mountain slopes and ridges15UD2361714938450fvmt63520061:24000
Cowood family-Rock outcrop-Bata family, complex, moderately steep trough bottoms37UD3311414943650hjmt63520061:24000
Bata-Lowder-Elve families, complex, moderately steep young moraines21UF2215114940550gjmt63520061:24000
Garlet-Bata-Elvick families, complex, nivational mountain slopes and ridges15UDB209814938650fxmt63520061:24000
Cowood family-Rock outcrop-Bata family, complex, moderately steep trough bottoms2575717034371v5klmt63619831:24000
Hollandlake-Bata complex, 4 to 30 percent slopes54198151454734wcpmt63819851:24000
Bata-Waldbillig gravelly silt loams, 4 to 30 percent slopes13144771454204w9zmt63819851:24000
Hollandlake-Bata complex, 30 to 60 percent slopes5559941454744wcqmt63819851:24000
Bata gravelly silt loam, cool, 2 to 8 percent slopes129431454094w9mmt63819851:24000
Ovando-Littlesalmon-Bata families, complex, steep glaciated mountain slopes and ridges43N608816830911thd8mt64720071:24000
Ovando-Bata families-Rock outcrop complex, moderately steep young moraines21UE21216782621tbchmt64720071:24000
Bata gravelly ashy silt loam, 8 to 30 percent slopes86E117015637057q6mt65119971:24000
Bata gravelly ashy silt loam, 2 to 8 percent slopes86C111015636857q4mt65119971:24000
Bata-Cabell-Hasshollow complex, 0 to 30 percent slopes0858NO85531202481q6x9or60720181:24000
Tyeecreek-Bata complex, 0 to 15 percent slopes0895AO31031202331nxy7or60720181:24000
Cabell-Bata-Bandarrow complex, 0 to 15 percent slopes0859AO7931203511qyg9or60720181:24000
Bata-Cabell-Hasshollow complex, 0 to 30 percent slopes0858NO161024850901q6x9or63120181:24000
Cabell-Bata-Bandarrow complex, 0 to 15 percent slopes0859AO57024957311qyg9or63120181:24000
Tyeecreek-Bata complex, 0 to 15 percent slopes0895AO9924850911nxy7or63120181:24000

Map of Series Extent

Approximate geographic distribution of the BATA 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 .