Official Series Description


Lab Data Summary

Aggregate lab data for the BATAN soil series. This aggregation is based on all pedons with a current taxon name of BATAN, 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 BATAN were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BATAN 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 BATAN 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 BATAN 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 BATAN 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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Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

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Click the image to view it full size.

Competing Series

Soil series competing with BATAN 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 BATAN 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 BATAN 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.

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Soil series sharing subgroup-level classification with BATAN, 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. NV-2012-05-09-13 | Lander County, South Part - November 1991

    General soil map units representative of those on a bolson that is an internally drained intermontane basin (Soil Survey of Lander County, Nevada, South Part; November 1991).

Map Units

Map units containing BATAN 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
Batan-Ocala-Ocala, rarely flooded, association169652126338702rgndnv61219681:24000
Ocala-Batan-Devilsgait association4315100475035hy9qnv76519861:24000
Devilsgait-Batan-Devilsgait, drained association4812185475043hy9znv76519861:24000
Xipe-Batan-Devilsgait association3411330475005hy8rnv76519861:24000
Geysen-Crooked Creek-Batan association7311215475099hycsnv76519861:24000
Geysen-Welch-Batan association7301045475098hycrnv76519861:24000
Caphor-Batan-Unsel association32529280479213j2nhnv76819851:63360
Batan-Bubus-Ocala association1687765479067j2hsnv76819851:63360
Needle Peak-Batan-Yobe association1807205479079j2j5nv76819851:63360
Batan-Kelk association1624485479065j2hqnv76819851:63360
Gund-Batan association44321654792752whllnv76819851:63360
Batan association1601800479062j2hmnv76819851:63360
Batan-Ocala association1691525479071j2hxnv76819851:63360
Batan silt loam1611470479064j2hpnv76819851:63360
Batan-Wendane-Valmy association81310091475315hylrnv76919861:24000
Batan silt loam, moderately saline-sodic814881475316hylsnv76919861:24000
Batan silt loam16115700479484j2y7nv77519851:24000
Batan-Wendane-Sonoma association1666460479488j2ycnv77519851:24000
Wendane-Batan-Broyles association11446000479417j2w2nv77519851:24000
Batan-Bubus-Ocala association1685100479494j2yknv77519851:24000
Bubus-Batan-Reese association2484630479548j309nv77519851:24000
Cren-Raglan-Batan association3044420479609j328nv77519851:24000
Batan silt loam, occasionally flooded1622750479485j2y8nv77519851:24000
Batan-Ocala-Ocala, rarely flooded, association1692150479497j2ynnv77519851:24000
Batan-Wendane-Valmy association1671675479490j2yfnv77519851:24000
Batan silt loam, slightly saline1631635479486j2y9nv77519851:24000
Gund-Batan association44313154796802whllnv77519851:24000
Batan fine sandy loam1601185479481j2y4nv77519851:24000
Batan-Ocala association88161710479903j3crnv77619831:63360
Batan silt loam*8832500479904j3csnv77619831:63360
Batan-Goldrun-Bubus complex, 0 to 30 percent slopes81811231475938hz7vnv77719931:24000
Batan-Goldrun association81010172475931hz7mnv77719931:24000
Batan-Prideen-Wendane complex8158729475936hz7snv77719931:24000
Batan complex8117869475932hz7nnv77719931:24000
Needle Peak-Batan-Goldrun association3635069475701hz06nv77719931:24000
Batan silt loam, 0 to 2 percent slopes 1/813984475934hz7qnv77719931:24000

Map of Series Extent

Approximate geographic distribution of the BATAN 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 .