Official Series Description


Lab Data Summary

Aggregate lab data for the CAMBETH soil series. This aggregation is based on all pedons with a current taxon name of CAMBETH, 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 CAMBETH 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 CAMBETH 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 CAMBETH 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 CAMBETH 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 CAMBETH 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 mountains figure.

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Competing Series

Soil series competing with CAMBETH 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 CAMBETH 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 CAMBETH 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 CAMBETH, 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 CAMBETH 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
Cabbart-Cambeth silt loams, 8 to 15 percent slopes260D209883430552w2cmmt01119921:24000
Bonfri-Cambeth complex, 2 to 8 percent slopes191C74653430012yk0xmt01119921:24000
Cambeth-Cabbart silt loams, 2 to 8 percent slopes260C60363430542w2clmt01119921:24000
Cambeth-Cabbart-Yawdim complex, 15 to 25 percent slopes260E24713430562vdklmt01119921:24000
Yamacall-Cambeth complex, 2 to 8 percent slopes193C1898343006chxqmt01119921:24000
Cambeth-Yamacall complex, 8 to 15 percent slopes160D942342927chv5mt01119921:24000
Cambeth-Cabbart-Yawdim complex, 15 to 25 percent slopes297E2557743433812vdklmt01719951:24000
Cambeth, noncalcareous-Megonot complex, 8 to 15 percent slopes297D647963433802w7p4mt01719951:24000
Cambeth-Cabbart-Rock outcrop complex, 8 to 45 percent slopes296F570483433782yk1hmt01719951:24000
Lonna-Cambeth-Cabbart silt loams, 4 to 12 percent slopes577D482673435522tvlsmt01719951:24000
Lonna-Cambeth-Cabbart silt loams, 12 to 25 percent slopes574E442663435482tvlxmt01719951:24000
Lonna-Cambeth silt loams, 2 to 8 percent slopes575C375533435492td94mt01719951:24000
Cambeth, noncalcareous-Megonot complex, 2 to 8 percent slopes297C290533433792w7p3mt01719951:24000
Lonna, Cambeth, and Yamacall soils, gullied, 8 to 15 percent slopes573D10502343547cjh5mt01719951:24000
Cambeth, noncalcareous-Lilsheep-Lonna complex, 15 to 45 percent slopes228F9363343345cj8nmt01719951:24000
Cambeth, calcaerous-Cabbart-Kirby complex, 8 to 45 percent slopes293E50223433762zg5lmt01719951:24000
Floweree-Cambeth, noncalcareous-Lilsheep complex, 4 to 15 percent slopes222D4234343336cj8cmt01719951:24000
Cambeth-Cabbart silt loams, 4 to 15 percent slopes917D17433437492w7p7mt01719951:24000
Cambeth-Cabbart complex, 8 to 25 percent slopes, dissected918E6563437512w7p8mt01719951:24000
Cambeth, calcareous-Cabbart-Yawdim complex, 4 to 25 percent slopes964E5743438102zg5nmt01719951:24000
Cabbart-Cambeth silt loams, 8 to 15 percent slopes605D1913435662w2cmmt01719951:24000
Cambeth, calcareous-Cabbart-Lonna silt loams, 15 to 35 percent slopes963E733438082zg5mmt01719951:24000
Cambeth-Cabbart silt loams, 2 to 8 percent slopes607C273435682w2clmt01719951:24000
Lonna-Cambeth silt loams, 2 to 8 percent slopes201C2207887544732td94mt02119711:24000
Lonna-Cambeth-Cabbart silt loams, 4 to 12 percent slopes202D1196137544742tvlsmt02119711:24000
Lonna-Cambeth-Cabbart silt loams, 12 to 25 percent slopes203E59467544752tvlxmt02119711:24000
Cabbart-Cambeth silt loams, 8 to 15 percent slopes260D567963421752w2cmmt02519911:24000
Cambeth-Cabbart silt loams, 2 to 8 percent slopes260C223133421742w2clmt02519911:24000
Lonna-Cambeth silt loams, 2 to 8 percent slopes193C130513421462td94mt02519911:24000
Bonfri-Cambeth complex, 2 to 8 percent slopes191C94673421442yk0xmt02519911:24000
Lonna-Cambeth-Cabbart silt loams, 4 to 12 percent slopes193D61153421472tvlsmt02519911:24000
Cambeth silt loam, 2 to 8 percent slopes60C2449342257ch4kmt02519911:24000
Cambeth-Lonna silt loams, 8 to 15 percent slopes160D2328342105cgznmt02519911:24000
Cambeth-Cabbart-Yawdim complex, 15 to 25 percent slopes260E16913421762vdklmt02519911:24000
Lonna-Cambeth-Cabbart silt loams, 12 to 25 percent slopes393E11793422212tvlxmt02519911:24000
Lonna-Cambeth silt loams, 2 to 8 percent slopes701C1490493426842td94mt03320021:24000
Cambeth-Cabbart-Yawdim complex, 15 to 25 percent slopes374E126726342637chjtmt03320021:24000
Cambeth, noncalcareous-Megonot complex, 2 to 8 percent slopes373C1193783426352w7p3mt03320021:24000
Lonna-Cambeth-Cabbart silt loams, 4 to 12 percent slopes702D1121643426852tvlsmt03320021:24000
Cambeth-Rock outcrop, soft-Yawdim association, 25 to 70 percent slopes1020F78390342613chj1mt03320021:24000
Cambeth, noncalcareous-Megonot complex, 8 to 15 percent slopes373D732363426362w7p4mt03320021:24000
Badland-Cambeth association, 15 to 70 percent slopes1007F61561342610chhymt03320021:24000
Cambeth-Cabbart-Rock outcrop complex, 8 to 45 percent slopes371F583873426332yk1hmt03320021:24000
Cambeth-Twilight-Cabbart complex, 4 to 15 percent slopes375D511973426382zg5pmt03320021:24000
Lonna-Cambeth-Cabbart silt loams, 12 to 25 percent slopes372E427823426342tvlxmt03320021:24000
Floweree-Cambeth silt loams, 2 to 8 percent slopes521C30304342659chkjmt03320021:24000
Cambeth-Cabbart silt loams, 2 to 8 percent slopes376C13283342639chjwmt03320021:24000
Lonna-Cabbart-Cambeth association, 4 to 15 percent slopes1022D10676342614chj2mt03320021:24000
Cambeth-Cabbart-Yawdim complex, 4 to 25 percent slopes376E66013426072zg5qmt03320021:24000
Cambeth, calcaerous-Cabbart-Kirby complex, 8 to 45 percent slopes377E23463426412zg5lmt03320021:24000
Cambeth-Cabbart silt loams, 4 to 15 percent slopes376D21963427622w7p7mt03320021:24000
Lonna, Cambeth, and Yamacall soils, 8 to 15 percent slopes, gullied704D2047342687chlfmt03320021:24000
Cambeth-Cabbart-Kirby complex, 4 to 15 percent slopes377D2028342640chjxmt03320021:24000
Cambeth silt loam, cool, 2 to 8 percent slopes378C421342780chpfmt03320021:24000
Cambeth-Cabbart complex, 8 to 25 percent slopes, dissected379E3573428182w7p8mt03320021:24000
Cambeth-Cabbart silt loams, 8 to 15 percent slopes379D113342738chn2mt03320021:24000
Cambeth silt loam, 2 to 8 percent slopes354C111339941cdqvmt03320021:24000
Cambeth-Twilight-Cabbart complex, 4 to 15 percent slopes43380583444062zg5pmt05519811:24000
Cambeth silt loam, 2 to 8 percent slopes4126934344404ckctmt05519811:24000
Floweree-Cambeth silt loams, 2 to 8 percent slopes6725227344432ckdqmt05519811:24000
Cambeth-Cabbart silt loams, 8 to 15 percent slopes4217312344405ckcvmt05519811:24000
Lonna-Cambeth silt loams, 2 to 8 percent slopes183549711457042td94mt05519811:24000
Lonna-Cambeth-Cabbart silt loams, 4 to 12 percent slopes17816723615452tvlsmt05519811:24000
Lonna-Cambeth-Cabbart silt loams, 4 to 12 percent slopes901232783450462tvlsmt07919861:24000
Lonna-Cambeth-Cabbart silt loams, 12 to 25 percent slopes911101123450472tvlxmt07919861:24000
Lonna-Cambeth silt loams, 2 to 8 percent slopes89669523450422td94mt07919861:24000
Cambeth, calcareous-Cabbart-Yawdim complex, 4 to 25 percent slopes27242563448472zg5nmt07919861:24000
Cambeth, calcareous-Cabbart-Lonna silt loams, 15 to 35 percent slopes26201193448462zg5mmt07919861:24000
Cambeth, calcaerous-Cabbart-Kirby complex, 8 to 45 percent slopes25155953448452zg5lmt07919861:24000
Cabbart-Cambeth-Rock outcrop, soft complex, 8 to 70 percent slopes1491340224511872n8nkmt07919861:24000
Cambeth-Tricart-Floweree complex, 8 to 45 percent slopes151885924511912n8npmt07919861:24000
Floweree-Cambeth silt loams, 0 to 4 percent slopes585527344967ckyzmt07919861:24000
Cambeth-Twilight-Cabbart complex, 4 to 15 percent slopes150528424511882zg5pmt07919861:24000
Alona-Cambeth, calcareous-Gerdrum complex, 2 to 8 percent slopes62326344971ckz3mt07919861:24000
Cambeth, calcareous-Bigsheep, bedrock substratum, complex, 8 to 45 percent slopes242130344844ckv0mt07919861:24000
Sixbeacon-Cambeth-Lilsheep complex, 2 to 8 percent slopes157154224512012n8p0mt07919861:24000
Yawdim-Cambeth, calcareous, complex, 2 to 8 percent slopes1391070344820ckt7mt07919861:24000
Lonna-Cambeth silt loams, 2 to 8 percent slopes201C7347016775472td94mt08319731:24000
Lonna-Cambeth-Cabbart silt loams, 4 to 12 percent slopes202D6236416775462tvlsmt08319731:24000
Lonna-Cambeth silt loams, 2 to 8 percent slopes201C156616072682td94mt10919561:31680
Lonna-Cambeth-Cabbart silt loams, 4 to 12 percent slopes202D90816072672tvlsmt10919561:31680
Cabbart-Cambeth complex, 4 to 35 percent slopes148E42514967150r3mt63920001:24000
Cambeth-Cabbart silt loams, 4 to 15 percent slopes58638593480902w7p7mt64919851:24000
Lonna-Cambeth silt loams, 2 to 8 percent slopes133588503479572td94mt64919851:24000
Cambeth-Cabbart complex, 8 to 25 percent slopes, dissected59494603480912w7p8mt64919851:24000
Cambeth silt loam, 2 to 8 percent slopes5630092348088cp6nmt64919851:24000
Cambeth-Niler complex, 4 to 15 percent slopes606013348093cp6tmt64919851:24000
Cambeth silt loam, 8 to 15 percent slopes575784348089cp6pmt64919851:24000
Cambeth, calcaerous-Cabbart-Kirby complex, 8 to 45 percent slopes2189203613722zg5lmt64919851:24000
Cabbart-Cambeth complex, 4 to 35 percent slopes148E46361417d42mmt65519751:24000
Cabbart-Cambeth silt loams, 9 to 15 percent slopesL2741D127584382qxkwnd00719981:24000
Cabbart-Cambeth silt loams, 9 to 15 percent slopesL2741D916127073302qxkwnd03319851:24000
Cambeth-Cabbart silt loams, 6 to 9 percent slopesL2709C585827073282q2mvnd03319851:24000
Cabbart-Cambeth silt loams, 9 to 15 percent slopesL2741D1303127159182qxkwnd08719741:20000
Cambeth-Cabbart silt loams, 6 to 9 percent slopesL2709C233427159162q2mvnd08719741:20000
Rangecreek, extremely stony surface-Kayso family-Cambeth family, complex, 4 to 35 percent slopes440432223662zjtqwy7371:24000

Map of Series Extent

Approximate geographic distribution of the CAMBETH 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 .