Official Series Description


Lab Data Summary

Aggregate lab data for the LAPEER soil series. This aggregation is based on all pedons with a current taxon name of LAPEER, 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 LAPEER 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
95B40A1576S1962WI021004Lapeer6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.4558334,-89.4608307
95B40A1577S1962WI021005Lapeer6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.4355545,-89.4194412
9840A1908S1971MI087001Lapeer7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.9944417,-83.3007639

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LAPEER 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 LAPEER 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 LAPEER 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 LAPEER 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 LAPEER 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 LAPEER 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 LAPEER 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 mountains figure.

There are insufficient data to create the 3D terrace figure.

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Soil series sharing subgroup-level classification with LAPEER, 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 LAPEER 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
Lapeer sandy loam, 2 to 6 percent slopesLaB73418637667y4mi03719741:15840
Lapeer sandy loam, 2 to 6 percent slopes, moderately erodedLnB2218018802469n9mi06719651:15840
Lapeer sandy loam, 6 to 12 percent slopes, moderately erodedLnC2168118802569nbmi06719651:15840
Lapeer sandy loam, 2 to 6 percent slopesLnB152118802369n8mi06719651:15840
Lapeer sandy clay loam, 6 to 12 percent slopes, severely erodedLmC367918801969n4mi06719651:15840
Lapeer sandy clay loam, 12 to 18 percent slopes, severely erodedLmD357618802069n5mi06719651:15840
Lapeer sandy loam, 12 to 18 percent slopes, moderately erodedLnD251218802669ncmi06719651:15840
Lapeer loam, 2 to 6 percent slopesLlB31918801669n1mi06719651:15840
Lapeer sandy loam, 0 to 2 percent slopesLnA28718802269n7mi06719651:15840
Lapeer loam, 2 to 6 percent slopes, moderately erodedLlB223218801769n2mi06719651:15840
Lapeer loam, 6 to 12 percent slopes, moderately erodedLlC218718801869n3mi06719651:15840
Lapeer sandy clay loam, 18 to 40 percent slopes, severely erodedLmF318318802169n6mi06719651:15840
Lapeer sandy loam, 18 to 40 percent slopes, moderately erodedLnF214918802769ndmi06719651:15840
Lapeer loam, 0 to 2 percent slopesLlA8618801569n0mi06719651:15840
Lapeer sandy loam, 2 to 6 percent slopesLaB93981920386ftsmi08719661:15840
Lapeer sandy loam, 6 to 12 percent slopes, moderately erodedLaC229811920416ftwmi08719661:15840
Lapeer sandy loam, 2 to 6 percent slopes, moderately erodedLaB218391920396fttmi08719661:15840
Lapeer sandy loam, 6 to 12 percent slopesLaC14031920406ftvmi08719661:15840
Lapeer sandy loam, 12 to 18 percent slopes, moderately erodedLaD212291920436ftymi08719661:15840
Lapeer sandy loam, 0 to 2 percent slopesLaA11421920376ftrmi08719661:15840
Lapeer sandy loam, 25 to 60 percent slopesLaF4501920476fv2mi08719661:15840
Lapeer sandy loam, 18 to 25 percent slopes, moderately erodedLaE24451920456fv0mi08719661:15840
Lapeer sandy loam, 12 to 18 percent slopes, severely erodedLaD33491920446ftzmi08719661:15840
Lapeer sandy loam, 6 to 12 percent slopes, severely erodedLaC32691920426ftxmi08719661:15840
Lapeer sandy loam, 18 to 25 percent slopes, severely erodedLaE31941920466fv1mi08719661:15840
Lapeer sandy loam, 2 to 6 percent slopesLdB124401142mx4cmi09319681:20000
Lapeer sandy loam, 2 to 6 percent slopesLeB45571876496986mi09919671:20000
Lapeer sandy loam, 6 to 12 percent slopesLeC26831876506987mi09919671:20000
Lapeer sandy loam, 12 to 18 percent slopesLeD6201876516988mi09919671:20000
Lapeer sandy loam, 18 to 25 percent slopesLeE2731876526989mi09919671:20000
Lapeer sandy loam, 2 to 6 percent slopes, moderately erodedLeB2425085276fttmi09919671:20000
Lapeer sandy loam, 18 to 25 percent slopes133E4625086886989mi12519801:15840
Lapeer sandy loam, 2 to 6 percent slopes133B1225086866986mi12519801:15840
Lapeer sandy loam, 6 to 12 percent slopes133C325086876987mi12519801:15840
Lapeer sandy loam, 2 to 6 percent slopesLmB37218781269fgmi15519671:12000
Lapeer sandy loam, 6 to 12 percent slopes, moderately erodedLmC218818781369fhmi15519671:12000
Lapeer fine sandy loam, 2 to 6 percent slopesLaB23672423291g6gkwi02119721:15840
Lapeer fine sandy loam, 6 to 12 percent slopes, erodedLaC215501423292g6glwi02119721:15840
Lapeer fine sandy loam, 12 to 20 percent slopes, erodedLaD27416423293g6gmwi02119721:15840
Lapeer fine sandy loam, 20 to 30 percent slopes, erodedLaE24416423294g6gnwi02119721:15840
Lapeer loamy fine sand, 2 to 6 percent slopesLaB3794423706g6wywi04719741:20000
Lapeer loamy fine sand, 6 to 12 percent slopes, erodedLaC22348423707g6wzwi04719741:20000
Lapeer loamy fine sand, 12 to 25 percent slopes, erodedLaD2695423708g6x0wi04719741:20000
Lapeer fine sandy loam, 0 to 2 percent slopesLb279423709g6x1wi04719741:20000
Lapeer-Pardeeville fine sandy loams, 2 to 6 percent slopesLpB2618426086g9cqwi07719691:20000
Lapeer-Pardeeville fine sandy loams, 6 to 12 percent slopes, erodedLpC22101426087g9crwi07719691:20000
Lapeer-Pardeeville fine sandy loams, 12 to 20 percent slopes, erodedLpD2964426088g9cswi07719691:20000
Lapeer-Pardeeville fine sandy loams, 20 to 30 percent slopes, erodedLpE2528426089g9ctwi07719691:20000

Map of Series Extent

Approximate geographic distribution of the LAPEER 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 .