Official Series Description


Lab Data Summary

Aggregate lab data for the BAMTUSH soil series. This aggregation is based on all pedons with a current taxon name of BAMTUSH, 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 BAMTUSH 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
584P009183CA105002Bamtush6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6083336,-123.019165
584P008583CA105010Bamtush7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6630554,-122.8094406

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BAMTUSH 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 BAMTUSH 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 BAMTUSH 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 BAMTUSH 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 terrace figure.

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with BAMTUSH 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 BAMTUSH 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 BAMTUSH 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.

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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 BAMTUSH, 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 BAMTUSH 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
Neuns-Bamtush-Goulding association, 30 to 50 percent slopes61015573461657hhd5ca01119991:24000
Bamtush-Marpa complex, 30 to 50 percent slopes6511755461659hhd7ca01119991:24000
Bamtush-Marpa complex, 15 to 30 percent slopes650587461658hhd6ca01119991:24000
Neuns-Bamtush-Speaker complex, 30 to 50 percent slopes557560461647hhcvca01119991:24000
Neuns-Bamtush-Deadwood association, 30 to 50 percent slopes18311273459586hf7cca03319851:24000
Bamtush-Speaker-Sanhedrin gravelly loams, 30 to 50 percent slopes1105940459513hf50ca03319851:24000
Neuns-Deadwood-Bamtush association, 50 to 75 percent slopes1844213459587hf7dca03319851:24000
Bamtush-Speaker-Sanhedrin gravelly loams, 50 to 75 percent slopes1113623459514hf51ca03319851:24000
Bamtush-Neuns gravelly loams, 15 to 30 percent slopes1091165459512hf4zca03319851:24000
MARPA-HOOSIMBIM-BAMTUSH COMPLEX, 50 TO 75 PERCENT SLOPES17112591466072hmzlca60619901:24000
BAMTUSH-BROWNBEAR COMPLEX, 50 TO 75 PERCENT SLOPES1044061465999hmx7ca60619901:24000
HOOSIMBIM-BAMTUSH-MARPA COMPLEX, 30 TO 50 PERCENT SLOPES1573832466060hmz6ca60619901:24000
BROWNBEAR-BAMTUSH COMPLEX, 30 TO 50 PERCENT SLOPES1123073466009hmxkca60619901:24000
BAMTUSH-BROWNBEAR-WEAVERVILLE COMPLEX, 30 TO 75 PERCENT SLOPES1052997466000hmx8ca60619901:24000
BAMTUSH-WEAVERVILLE-BROWNBEAR COMPLEX, 15 TO 50 PERCENT SLOPES1072684466004hmxdca60619901:24000
WEITCHPEC VARIANT-BAMTUSH VARIANT COMPLEX, 50 TO 75 PERCENT SLOPES2121708466116hn10ca60619901:24000
ETSEL-BAMTUSH COMPLEX, 50 TO 75 PERCENT SLOPES1431205466045hmyqca60619901:24000
BAMTUSH-BROWNBEAR COMPLEX, 15 TO 30 PERCENT SLOPES103599465998hmx6ca60619901:24000
WEITCHPEC VARIANT-BAMTUSH VARIANT COMPLEX, 9 TO 50 PERCENT SLOPES211582466114hn0yca60619901:24000
BAMTUSH-WEAVERVILLE COMPLEX, 15 TO 30 PERCENT SLOPES106220466002hmxbca60619901:24000
Marpa-Hoosimbim-Bamtush complex, 50 to 75 percent slopes171tw1989186880720qn3ca70719831:24000
Bamtush-Brownbear complex, 15 to 30 percent slopes103tw908186872120qkbca70719831:24000
Hoosimbim-Bamtush-Marpa complex, 30 to 50 percent slopes157tw338186878620qmfca70719831:24000
Bamtush-Brownbear-Weaverville complex, 30 to 75 percent slopes105tw210186872520qkgca70719831:24000
Bamtush-Brownbear complex, 50 to 75 percent slopes104tw149186872320qkdca70719831:24000
Brownbear-Bamtush complex, 30 to 50 percent slopes112tw9186873220qkpca70719831:24000
Etsel-Bamtush complex, 50 to 75 percent slopes143tw5186876320qlpca70719831:24000
Bamtush-Speaker-Sanhedrin gravelly loams, 30 to 50 percent slopes110la18727478662q3r6ca70920101:24000
Bamtush-Speaker-Sanhedrin gravelly loams, 50 to 75 percent slopes111la5227478672q3r7ca70920101:24000

Map of Series Extent

Approximate geographic distribution of the BAMTUSH 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 .