Official Series Description


Lab Data Summary

Aggregate lab data for the HAMBRIGHT soil series. This aggregation is based on all pedons with a current taxon name of HAMBRIGHT, 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 HAMBRIGHT 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
17UCD561100956-CA-11-009HAMBRIGHT2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.788456,-122.3420334
18UCD660400366-CA-04-003xHAMBRIGHT3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5816574,-121.5516357
18UCD670401667-CA-04-016xHAMBRIGHT3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5525436,-121.5701523

Water Balance

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

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

Soil series sharing subgroup-level classification with HAMBRIGHT, 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 HAMBRIGHT 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
Sobrante-Guenoc-Hambright complex, 15 to 30 percent slopes2197318459622hf8jca03319851:24000
Konocti-Hambright complex, 15 to 30 percent slopes1534075459556hf6dca03319851:24000
Sobrante-Hambright-Guenoc complex, 30 to 50 percent slopes2203212459623hf8kca03319851:24000
Konocti-Hambright complex, 5 to 15 percent slopes1522806459555hf6cca03319851:24000
Sobrante-Guenoc-Hambright complex, 2 to 15 percent slopes2182488459621hf8hca03319851:24000
Neice-Sobrante-Hambright complex, 30 to 75 percent slopes1822052459585hf7bca03319851:24000
Neice-Sobrante-Hambright complex, 15 to 30 percent slopes1811943459584hf79ca03319851:24000
Konocti variant-Konocti-Hambright complex, 15 to 30 percent slopes1561838459559hf6hca03319851:24000
Konocti-Hambright-Rock outcrop complex, 30 to 75 percent slopes1541015459557hf6fca03319851:24000
Konocti variant-Konocti-Hambright complex, 2 to 15 percent slopes155916459558hf6gca03319851:24000
Hambright rock-Outcrop complex, 30 to 75 percent slopes152n2016068901qy35ca03319851:24000
Hambright rock-Outcrop complex, 30 to 75 percent slopes15218200458976hdlpca05519741:24000
Rock outcrop-Hambright complex, 50 to 75 percent slopes1768290459000hdmgca05519741:24000
Hambright-Rock outcrop complex, 2 to 30 percent slopes1513975458975hdlnca05519741:24000
Sobrante-Hambright-Guenoc complex, 30 to 50 percent slopes220l435813837w9vtca05519741:24000
Hambright loam, 15 to 40 percent slopesHaFso210825271wprnca05519741:24000
Hambright-Toomes stony loams, 9 to 30 percent slopesHtEso206816530wdnpca05519741:24000
Sobrante-Guenoc-Hambright complex, 15 to 30 percent slopes219l41813836w9vsca05519741:24000
Hambright loam, 15 to 40 percent slopesHaF8983456088h9ljca09519691:24000
Hambright-Toomes stony loams, 9 to 30 percent slopesHtE1314456089h9lkca09519691:24000
Hambright rock-Outcrop complex, 30 to 75 percent slopes152n438816877wf0wca09519691:24000
Hambright-Rock outcrop complex, 2 to 30 percent slopes151n52816876wf0vca09519691:24000
Hambright-Rock outcrop complex, 2 to 30 percent slopes151n16074321qynnca09719681:20000
Hambright rock-Outcrop complex, 30 to 75 percent slopes152n16074331qynpca09719681:20000
Hambright gravelly clay loam, 30 to 75 percent slopesHaG9794456829hbcfca63819671:24000
Hambright very rocky loam, 15 to 75 percent slopesHaG11104457707hc8rca67419681:24000
Hambright rocky clay loam, 30 to 50 percent slopesHbF565457708hc8sca67419681:24000
Urban land-Hambright, landscaped-Talepop complex, 0 to 50 percent, residential18123624038722lpf8ca69220011:24000
Livermore-Agua Dulce-Hambright families association, 30 to 80 percent slopes1448217465279hm50ca77219811:24000
Lodo-Hambright-Millsholm families association, 30 to 60 percent slopes1635276465281hm52ca77219811:24000

Map of Series Extent

Approximate geographic distribution of the HAMBRIGHT 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 .