Official Series Description


Lab Data Summary

Aggregate lab data for the LAMPSHIRE soil series. This aggregation is based on all pedons with a current taxon name of LAMPSHIRE, 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 LAMPSHIRE 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
4179P026379AZ003001Lampshire6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.6836109,-109.566391
4174C0175S1974AZ019004LAMPSHIRE6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.2155571,-110.6886139

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LAMPSHIRE 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 LAMPSHIRE 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 LAMPSHIRE 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 LAMPSHIRE 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.

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Competing Series

Soil series competing with LAMPSHIRE 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 LAMPSHIRE 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 LAMPSHIRE 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 LAMPSHIRE, 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. AZ-2010-08-30-03 | Pima County, Eastern Part - 2003

    Typical soil and landscape relationship on the east side of the Baboquivari Mountains (Soil Survey of Pima County, Arizona, Eastern Part; 2003).

  2. AZ-2011-05-27-26 | Pima County, Eastern Part - 2003

    Typical soil and landscape relationship on the east side of the Baboquirari Mountains (Soil Survey of Pima County, Arizona, Eastern Part; 2003).

  3. AZ-2011-05-27-30 | Tohono O'odham Nation - 1999

    Generalized relationship of some warm (thermic) soil map units (Soil Survey of Tohono O'oodham Nation, Arizona; 1999).

Map Units

Map units containing LAMPSHIRE 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
Lampshire-Rock outcrop complex, cool, 30 to 70 percent slopes749375715079371mm44az62720051:24000
Romero-Lampshire-Rock outcrop complex, 35 to 70 percent slopes1078102115079701mm56az62720051:24000
Hassell family-Lampshire-Rock outcrop complex, 10 to 30 percent slopes581683415079211mm3maz62720051:24000
Lampshire-Rock outcrop complex, 15 to 60 percent slopes, stony75723415079381mm45az62720051:24000
Lampshire-Rock outcrop complex, 20 to 60 percent slopes73371715079361mm43az62720051:24000
Lampshire-Romero-Rock outcrop complex, 5 to 90 percent slopes6181403329338332tdthaz6571:24000
Rock outcrop-Lampshire complex, 10 to 60 percent slopes832838914513621kq84az66120091:24000
Chiricahua, Deloro, and Lampshire soils, 5 to 60 percent slopes191586423836792l0dwaz66120091:24000
Pantak-Rock outcrop-Lampshire complex, 5 to 60 percent slopes mlra 3873966214513642tznfaz66120091:24000
Rock outcrop-Lampshire complex, chaparral, 5 to 50 percent slopes84786322316792dx7naz66120091:24000
Rock outcrop-Lampshire complex, 20 to 90 percent slopes335900544571tnpaz66319791:24000
Graham-Lampshire-Rock outcrop complex, 5 to 60 percent slopes451250017273271vzf7az66620071:24000
Lampshire-Graham-Rock outcrop association, steepLgF8887314261091jvzjaz66719711:20000
Lampshire-Chiricahua association, steepLcF8680014256881jvjyaz66719711:20000
Chiricahua-Lampshire association, rollingCrD3668214231011jrvhaz66719711:20000
Lampshire very gravelly sandy loam, 25 to 50 percent slopesLaF3292014261081jvzhaz66719711:20000
Lampshire very gravelly sandy loam, 0 to 25 percent slopesLaE277014261071jvzgaz66719711:20000
Lampshire-Romero-Rock outcrop complex, 10 to 65 percent slopes4048925538271t0caz66919931:24000
Cellar-Lampshire-Rock outcrop complex, 15 to 60 percent slopes1223070537442whx8az66919931:24000
Lampshire-Pantak-Rock outcrop complex, 25 to 60 percent slopes3918914538241t08az66919931:24000
Chiricahua-Lampshire complex, 5 to 15 percent slopes1716353537561sy2az66919931:24000
Romero-Lampshire-Rock outcrop complex, 15 to 65 percent slopes692140538761t1yaz66919931:24000
Brunkcow-Chiricahua-Lampshire complex, 15 to 60 percent slopes1937026550401v8haz67120001:24000
Deloro-Leyte-Lampshire complex, 3 to 55 percent slopes4216360550581v92az67120001:24000
Graham-Lampshire complex, 8 to 60 percent slopes7513475550331v88az67120001:24000
Graham-Lampshire-Rock outcrop complex, 5 to 60 percent slopes23645624985592pzntaz6731:24000
Rock outcrop-Lampshire complex, 10 to 60 percent slopes38215624985692pzp4az6731:24000
Pantak-Rock outcrop-Lampshire complex, 5 to 60 percent slopes mlra 385525811592722tznfaz67520091:24000
Rock outcrop-Lampshire complex, 15 to 50 percent slopes7219390592701znyaz67520091:24000
Rock outcrop-Lampshire complex, 5 to 40 percent slopes58568924342202mq07az6871:24000
Romero-Lampshire-Rock outcrop complex, 35 to 70 percent slopes1304161798507vsx9az69720051:24000
Hassell family-Lampshire-Rock outcrop complex, 10 to 30 percent slopes55488798427vstqaz69720051:24000
Lampshire-Rock outcrop complex, 20 to 60 percent slopes7528114738517hyfaz69720051:24000
Cellar-Lampshire-Rock outcrop complex, 15 to 60 percent slopes1031498545382whx8az70319931:24000
Romero-Lampshire-Rock outcrop complex, 15 to 65 percent slopes5217352546451tvraz70319931:24000
Lampshire-Pantak-Rock outcrop complex, 25 to 60 percent slopes4116171546161tttaz70319931:24000
Chiricahua-Lampshire complex, 15 to 45 percent slopes1111660545401trcaz70319931:24000
Lampshire-Pantak complex, 10 to 60 percent slopesLPG584319067412203stx62620121:24000
Rock outcrop-Lampshire complex, 5 to 60 percent slopesRXG93125116322q92ktx62620121:24000
Lampshire-Pantak complex, 10 to 60 percent slopesLPG2988125041692q3m7tx62720121:24000

Map of Series Extent

Approximate geographic distribution of the LAMPSHIRE 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 .