Official Series Description


Lab Data Summary

Aggregate lab data for the LAUGHLIN soil series. This aggregation is based on all pedons with a current taxon name of LAUGHLIN, 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 LAUGHLIN 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
4BUCD634901063-CA-49-010xLAUGHLIN3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5984154,-123.1914063
5UCD541200254-CA-12-002xLAUGHLIN3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1137848,-123.7574158
5UCD621202562-CA-12-025xLAUGHLIN4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.9753075,-123.8178329

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LAUGHLIN 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 LAUGHLIN 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 LAUGHLIN 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 LAUGHLIN 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 LAUGHLIN 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 LAUGHLIN 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 LAUGHLIN 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 LAUGHLIN, 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 LAUGHLIN 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
Laughlin loam, 30 to 50 percent slopesLgFsn11816514wdn5ca05519741:24000
Laughlin loam, 50 to 75 percent slopesLgG26195459812hfgnca09719681:20000
Laughlin loam, 30 to 50 percent slopesLgF20838459811hfgmca09719681:20000
Yorkville-Laughlin complex, 30 to 50 percent slopesYvF13118459916hfl0ca09719681:20000
Suther-Laughlin loams, 15 to 50 percent slopesSuF10307459894hfk9ca09719681:20000
Suther-Laughlin loams, 50 to 75 percent slopesSuG7040459895hfkbca09719681:20000
Laughlin-Yorkville complex, 30 to 75 percent slopesLhG5290459814hfgqca09719681:20000
Laughlin loam, 2 to 30 percent slopesLgE5002459810hfglca09719681:20000
Laughlin loam, 50 to 75 percent slopes, erodedLgG21703459813hfgpca09719681:20000
Hugo-Laughlin complex, 30 to 75 percent slopesHoG1379459774hfffca09719681:20000
Laughlin-Sweeney loams, very steep, erodedLbF2730456438h9ytca63719581:15000
Laughlin-Sweeney loams, steep, erodedLbE2702456437h9ysca63719581:15000
Laughlin-Sweeney loams, moderately steep, erodedLbD2261456436h9yrca63719581:15000
Laughlin loam, very steep, erodedLaF295456434h9ypca63719581:15000
Laughlin loam, moderately steep, erodedLaD274456432h9ymca63719581:15000
Laughlin-Sweeney loams, sloping, erodedLbC272456435h9yqca63719581:15000
Laughlin loam, sloping, erodedLaC264456431h9ylca63719581:15000
Laughlin loam, steep, erodedLaE248456433h9ynca63719581:15000
Laughlin gravelly loam, 30 to 50 percent slopes1602145458061hcn5ca67819741:24000

Map of Series Extent

Approximate geographic distribution of the LAUGHLIN 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 .