Official Series Description


Lab Data Summary

Aggregate lab data for the CHAMA soil series. This aggregation is based on all pedons with a current taxon name of CHAMA, 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 CHAMA 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
5475ND0250111975ND025011Chama5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.3416667,-102.4380556
5483ND03316383ND033163Chama5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7686111,-103.8075
5498P0162S1997ND033001CHAMA7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7820816,-103.9840851
5498P0163S1997ND033002CHAMA7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7958069,-103.940361
5498P0164S1997ND033003CHAMA8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.763916,-103.9062195
5498P0165S1997ND033004CHAMA7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7758064,-103.9541931
58C83ND03316283ND033162Chama5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7175,-103.8613889
n/a98P0411S1998ND033001CHAMA8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

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

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

Soil series sharing subgroup-level classification with CHAMA, 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. ND-2012-02-07-40 | Golden Valley County - July 1989

    Typical pattern of soils and parent material in the Chama-Golva-Cabba association (Soil Survey of Golden Valley County, North Dakota; July 1989).

Map Units

Map units containing CHAMA 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
Cabba-Chama-Sen silt loams, 9 to 15 percent slopes53D25742493012ct44mt08319731:24000
Chama-Cabba-Sen silt loams, 6 to 9 percent slopesE2737C103332567191vztxmt08319731:24000
Bainville-Chama silt loams, 15 to 30 percent slopesBe483033040356clmpmt10919561:31680
Chama silt loam, 4 to 7 percent slopesCa40400345613clmtmt10919561:31680
Chama-Bainville silt loams, 10 to 14 percent slopesCe21665345617clmymt10919561:31680
Chama-Cabba-Sen silt loams, 6 to 9 percent slopesE2737C83643456161vztxmt10919561:31680
Chama stony silt loam, 4 to 9 percent slopesCb488345614clmvmt10919561:31680
Chama stony silt loam, 10 to 30 percent slopesCc470345615clmwmt10919561:31680
Chama clay loam, 4 to 8 percent slopesCd4981473164y94mt60219631:20000
Chama-Midway clay loams, 8 to 15 percent slopesCg4171473184y96mt60219631:20000
Chama-Midway clay loams, 4 to 8 percent slopesCf1211473174y95mt60219631:20000
Chama-Sen-Cabba silt loams, 3 to 6 percent slopesE2913B1196125257521vzv3nd00119831:20000
Chama-Cabba-Sen silt loams, 6 to 9 percent slopesE2737C960825257491vztxnd00119831:20000
Cabba-Chama-Shambo loams, 9 to 50 percent slopesE2617F766425257471vztsnd00119831:20000
Cabba-Chama-Sen silt loams, 9 to 15 percent slopesE2741D253425257501vztynd00119831:20000
Cabba-Chama-Havrelon, occasionally flooded complex, 2 to 70 percent slopesE4190F2027556632r4j4nd00119831:20000
Cabba-Chama-Sen silt loams, 9 to 15 percent slopesE2741D488717151861vztynd00719981:24000
Chama-Sen-Cabba silt loams, 3 to 6 percent slopesE2913B447117151891vzv3nd00719981:24000
Chama-Cabba-Sen silt loams, 6 to 9 percent slopesE2737C340717151851vztxnd00719981:24000
Cabba-Chama-Shambo loams, 9 to 50 percent slopesE2617F275726990601vztsnd00719981:24000
Cabba-Chama-Shambo loams, 9 to 50 percent slopesE2617F1031125635381vztsnd01119691:20000
Chama-Sen-Cabba silt loams, 3 to 6 percent slopesE2913B804325635421vzv3nd01119691:20000
Chama-Cabba-Sen silt loams, 6 to 9 percent slopesE2737C303625635401vztxnd01119691:20000
Cabba-Chama silt loams, 3 to 9 percent slopesE2707C213925635372r4j2nd01119691:20000
Chama-Sen silt loams, 0 to 3 percent slopesE2903A165625635412r8l2nd01119691:20000
Cabba-Rock outcrop-Chama complex, 15 to 70 percent slopesE2775F12182563539cdnlnd01119691:20000
Cabba-Chama-Sen silt loams, 9 to 15 percent slopesE2741D7327584551vztynd01119691:20000
Cabba-Chama-Havrelon, occasionally flooded complex, 2 to 70 percent slopesE4190F5027584582r4j4nd01119691:20000
Chama, Morton, and Cabba silty clay loams, 6 to 15 percent slopesCnC2099280812b32nd01119691:20000
Chama and Morton silty clay loams, 3 to 6 percent slopesCmB899280712b31nd01119691:20000
Werner-Chama-Sen silt loams, 9 to 15 percent slopesE2747D1050026617272r6ttnd01519671:20000
Sen-Chama silt loams, 6 to 9 percent slopesE2987C765226617422r8l9nd01519671:20000
Sen-Chama silt loams, 3 to 6 percent slopesE2987B48742661671cdn4nd01519671:20000
Cabba-Chama-Shambo loams, 9 to 50 percent slopesE2617F7103625256351vztsnd02519811:20000
Chama-Cabba-Sen silt loams, 6 to 9 percent slopesE2737C2388917146471vztxnd02519811:20000
Sen-Chama silt loams, 3 to 6 percent slopesE2987B129462707212cdn4nd02519811:20000
Sen-Chama silt loams, 6 to 9 percent slopesE2987C1011427072132r8l9nd02519811:20000
Cabba-Chama-Havrelon, occasionally flooded complex, 2 to 70 percent slopesE4190F32027072482r4j4nd02519811:20000
Werner-Chama-Sen silt loams, 9 to 15 percent slopesE2747D28227584822r6ttnd02519811:20000
Chama-Sen-Cabba silt loams, 3 to 6 percent slopesE2913B9817146511vzv3nd02519811:20000
Cabba-Chama-Sen silt loams, 9 to 15 percent slopesE2741D3417146481vztynd02519811:20000
Chama-Sen-Cabba silt loams, 3 to 6 percent slopesE2913B4815327072981vzv3nd03319851:24000
Chama-Cabba-Sen silt loams, 6 to 9 percent slopesE2737C4031827072941vztxnd03319851:24000
Cabba-Chama silt loams, 9 to 15 percent slopesE2709D1713427072932r4j3nd03319851:24000
Cabba-Chama silt loams, 3 to 9 percent slopesE2707C699727072922r4j2nd03319851:24000
Chama-Sen silt loams, 0 to 3 percent slopesE2903A326027072972r8l2nd03319851:24000
Cabba-Chama-Sen silt loams, 9 to 15 percent slopesE2741D99427597421vztynd03319851:24000
Cabba-Chama-Havrelon, occasionally flooded complex, 2 to 70 percent slopesE4190F31727597522r4j4nd03319851:24000
Cabba-Rock outcrop-Chama complex, 15 to 70 percent slopesE2775F2992707295cdnlnd03319851:24000
Cabba-Chama-Shambo loams, 9 to 50 percent slopesE2617F13827597391vztsnd03319851:24000
Cabba-Chama-Shambo loams, 9 to 50 percent slopesE2617F4269625256361vztsnd03719851:20000
Chama-Cabba-Sen silt loams, 6 to 9 percent slopesE2737C1317017154971vztxnd03719851:20000
Chama-Sen-Cabba silt loams, 3 to 6 percent slopesE2913B1035427596481vzv3nd03719851:20000
Cabba-Chama-Sen silt loams, 9 to 15 percent slopesE2741D762317154981vztynd03719851:20000
Cabba-Chama-Havrelon, occasionally flooded complex, 2 to 70 percent slopesE4190F2425258442r4j4nd03719851:20000
Chama-Sen-Cabba silt loams, 3 to 6 percent slopesE2913B2665117186051vzv3nd04119861:20000
Chama-Cabba-Sen silt loams, 6 to 9 percent slopesE2737C2085117186001vztxnd04119861:20000
Cabba-Chama-Shambo loams, 9 to 50 percent slopesE2617F603025258071vztsnd04119861:20000
Chama-Sen silt loams, 0 to 3 percent slopesE2903A107925258102r8l2nd04119861:20000
Cabba-Chama-Havrelon, occasionally flooded complex, 2 to 70 percent slopesE4190F7425258182r4j4nd04119861:20000
Cabba-Chama-Sen silt loams, 9 to 15 percent slopesE2741D2117186011vztynd04119861:20000
Cabba-Chama-Sen silt loams, 9 to 15 percent slopesE2741D3513527150811vztynd05320031:24000
Cabba-Chama-Havrelon, occasionally flooded complex, 2 to 70 percent slopesE4190F2787926993512r4j4nd05320031:24000
Cabba-Chama-Shambo loams, 9 to 50 percent slopesE2617F2625527150771vztsnd05320031:24000
Chama-Cabba-Sen silt loams, 6 to 9 percent slopesE2737C1668327150801vztxnd05320031:24000
Chama-Sen-Cabba silt loams, 3 to 6 percent slopesE2913B519927150841vzv3nd05320031:24000
Sen-Chama silt loams, 6 to 9 percent slopesE2987C78926624942r8l9nd05519741:20000
Werner-Chama-Sen silt loams, 9 to 15 percent slopesE2747D1891526993892r6ttnd05719761:20000
Sen-Chama silt loams, 3 to 6 percent slopesE2987B32822699316cdn4nd05719761:20000
Sen-Chama silt loams, 6 to 9 percent slopesE2987C248226993172r8l9nd05719761:20000
Cabba-Chama-Shambo loams, 9 to 50 percent slopesE2617F15427557271vztsnd05719761:20000
Cabba-Chama-Sen silt loams, 9 to 15 percent slopesE2741D1727585451vztynd05719761:20000
Cabba-Chama-Shambo loams, 9 to 50 percent slopesE2617F7615626991551vztsnd05919981:20000
Chama-Cabba-Sen silt loams, 6 to 9 percent slopesE2737C4346017183561vztxnd05919981:20000
Cabba-Chama-Sen silt loams, 9 to 15 percent slopesE2741D2804117183571vztynd05919981:20000
Sen-Chama silt loams, 3 to 6 percent slopesE2987B91952699211cdn4nd05919981:20000
Chama-Sen-Cabba silt loams, 3 to 6 percent slopesE2913B481326991571vzv3nd05919981:20000
Cabba-Rock outcrop-Chama complex, 15 to 70 percent slopesE2775F16702699156cdnlnd05919981:20000
Werner-Chama-Sen silt loams, 9 to 15 percent slopesE2747D16227596742r6ttnd05919981:20000
Werner-Chama-Sen silt loams, 9 to 15 percent slopesE2747D1728825259482r6ttnd06519711:20000
Sen-Chama silt loams, 3 to 6 percent slopesE2987B3332755713cdn4nd06519711:20000
Cabba-Chama-Sen silt loams, 9 to 15 percent slopesE2741D22427557081vztynd06519711:20000
Sen-Chama silt loams, 6 to 9 percent slopesE2987C16732566582r8l9nd06519711:20000
Chama-Cabba-Sen silt loams, 6 to 9 percent slopesE2737C1227556981vztxnd06519711:20000
Cabba-Rock outcrop-Chama complex, 15 to 70 percent slopesE2775F72755709cdnlnd06519711:20000
Cabba-Chama-Shambo loams, 9 to 50 percent slopesE2617F1724425256371vztsnd08519921:24000
Chama-Cabba-Sen silt loams, 6 to 9 percent slopesE2737C2384617167881vztxnd08719741:20000
Cabba-Chama silt loams, 9 to 15 percent slopesE2709D1600127074262r4j3nd08719741:20000
Chama-Sen-Cabba silt loams, 3 to 6 percent slopesE2913B1221127158301vzv3nd08719741:20000
Chama-Cabba silt loams, 3 to 6 percent slopesE2933B67062715837cdmgnd08719741:20000
Cabba-Chama-Sen silt loams, 9 to 15 percent slopesE2741D409717167891vztynd08719741:20000
Cabba-Chama-Shambo loams, 9 to 50 percent slopesE2617F254627074221vztsnd08719741:20000
Chama-Sen silt loams, 0 to 3 percent slopesE2903A156027074292r8l2nd08719741:20000
Cabba-Chama silt loams, 3 to 9 percent slopesE2707C115827074252r4j2nd08719741:20000
Cabba-Rock outcrop-Chama complex, 15 to 70 percent slopesE2775F42758519cdnlnd08719741:20000
Cabba-Chama-Shambo loams, 9 to 50 percent slopesE2617F2353025256341vztsnd08919651:20000
Cabba-Chama-Sen silt loams, 9 to 15 percent slopesE2741D1010317135341vztynd08919651:20000
Chama-Cabba-Sen silt loams, 6 to 9 percent slopesE2737C880117135331vztxnd08919651:20000
Chama-Sen-Cabba silt loams, 3 to 6 percent slopesE2913B527417135391vzv3nd08919651:20000
Cabba-Chama-Havrelon, occasionally flooded complex, 2 to 70 percent slopesE4190F420527160182r4j4nd08919651:20000

Map of Series Extent

Approximate geographic distribution of the CHAMA 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 .