Official Series Description


Lab Data Summary

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

Soil series sharing subgroup-level classification with LAMPHIER, 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 LAMPHIER 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
Lamphier loam, 4 to 20 percent slopes169440498379jqlrco63519791:24000
Lamphier loam, 4 to 20 percent slopes542M28509877k3knco63620111:24000
Lamphier loam, 5 to 45 percent slopesLaF1855509749k3fjco66119681:31680
Lamphier-Hapgood families complex, 5 to 20 percent slopes2537805510589k49mco67619831:24000
Hapgood-Lamphier families complex, 20 to 50 percent slopes2131955510585k49hco67619831:24000
Hoosan-Lamphier-Leaps families complex, 3 to 30 percent slopes2222917510586k49jco67619831:24000
Lamphier loam, 15 to 50 percent slopes4221800496784jny9co68319771:24000
Lamphier-Tampico, cool-Kamack loams, 5 to 60 percent slopes6561393496909jp2bco68419841:24000
Rhone-Northwater-Lamphier loams, 3 to 50 percent slopes1005277496823jnzkco68419841:24000
Lamphier-Tampico-Kamack loams, 5 to 60 percent slopes5012125497002jp5bco68519791:24000
Rhone-Northwater-Lamphier loams, 3 to 50 percent slopes779316497031jp68co68519791:24000
Lamphier-Jerry complex, 25 to 65 percent slopes11711844497077jp7rco68619921:31680
Lamphier fine sandy loam, 25 to 65 percent slopes1158680497075jp7pco68619921:31680
Lamphier-Jerry complex, 3 to 25 percent slopes1162647497076jp7qco68619921:31680
Lamphier fine sandy loam, 3 to 25 percent slopes1142525497074jp7nco68619921:31680
Hierro, extremely stony-Lamphier, stony-Nopemountain families, complex, 15 to 65 percent slopes6321G21031692602v117mt60019691:24000
Hierro, stony-Lamphier, stony-Elkwalow families, complex, 4 to 30 percent slopes6321E15331692592v116mt60019691:24000
Hierro, extremely stony-Lamphier, stony-Nopemountain families, complex, 15 to 65 percent slopes6321G555928324482v117mt6321:24000
Lamphier, stony-Pishkun, rubbly-Charpeak, very stony families, complex, 40 to 70 percent slopes6339G230728324452v113mt6321:24000
Hierro, stony-Lamphier, stony-Elkwalow families, complex, 4 to 30 percent slopes6321E182528324492v116mt6321:24000
Lamphier, stony-Needleton, very stony-Yellowmule, very stony families, complex, 15 to 60 percent slopes, landslides6201F124229804302wqqcmt6321:24000
Lamphier, stony-Needleton, very stony-Yellowmule, very stony families, complex, 15 to 60 percent slopes, landslides6201F34730941492wqqcmt65719901:24000

Map of Series Extent

Approximate geographic distribution of the LAMPHIER 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 .