Official Series Description


Lab Data Summary

Aggregate lab data for the LAWET soil series. This aggregation is based on all pedons with a current taxon name of LAWET, 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 LAWET 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
102C40A2128S1973NE003021Lawet6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.240551,-97.8636932
6600P060199SD007001Lawet6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0858269,-101.5384445

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LAWET 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 LAWET 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 LAWET 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 LAWET 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 LAWET 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 LAWET 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 LAWET 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 hills figure.

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

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with LAWET, 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 LAWET 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
Lawet silt loam, 0 to 2 percent slopes, occasionally flooded633647024269622zp2pne00319751:20000
Lawet soils, wet, occasionally flooded63431750426963gb90ne00319751:20000
Lawet-Saltine complex, occasionally flooded63465122159542dcwdne00319751:20000
Lawet silt loam, rarely flooded63355612427895gc82ne03719801:20000
Lawet silty clay loam, occasionally flooded63414090427896gc83ne03719801:20000
Lawet silt loam, 0 to 2 percent slopes, occasionally flooded633644422169452zp2pne03719801:20000
Lawet silt loam, drained, rarely flooded6338236616997031v1p4ne04719751:20000
Lawet silt loam, saline-alkali, rarely flooded6340223516997041v1p5ne04719751:20000
Lawet loam, ponded, rarely flooded633368816997021v1p3ne04719751:20000
Lawet loam, drained, rarely flooded633111821001183c5mne08919811:20000
Lawet-Lute complex, rarely flooded634510401001193c5nne08919811:20000
Lawet loam, rarely flooded6330219116988971v0v4ne10119901:20000
Lawet silt loam, drained, occasionally flooded63371991816991991v14wne11119711:24000
Lawet silt loam, saline-alkali, occasionally flooded63391220916992001v14xne11119711:24000
Lawet silt loam, occasionally flooded6336863816991981v14vne11119711:24000
Lawet loam, gravelly subsoil variant, occasionally flooded6332192116992021v14zne11119711:24000
Lawet-Saltine complex, occasionally flooded6346147316992011v14yne11119711:24000
Lawet fine sandy loam, drained, occasionally flooded6328123516991971v14tne11119711:24000
Elsmere complex, 0 to 6 percent slopes4549118316991641v13rne11119711:24000
Lawet silt loam, saline-alkali, rarely flooded634059722197892dhw3ne11119711:24000
Lawet loam, rarely flooded63301157427412gbrhne11919811:20000
Lawet variant fine sandy loam, frequently flooded634455017096581vd18ne12119781:20000
Lawet silt loam, 0 to 2 percent slopes, occasionally flooded6336533222171772zp2pne13919701:20000
Lawet loam, occasionally flooded63295014427573gbxpne13919701:20000
Lawet-Saltine complex, occasionally flooded63461921427574gbxqne13919701:20000
Lawet soils, wet, occasionally flooded634313022171782df4wne13919701:20000
Lawet silt loam, 0 to 2 percent slopes, occasionally flooded633618304276522zp2pne14119841:20000
Lawet silty clay loam, rarely flooded63421105426837gb4yne16719801:20000
Lawet loam, 0 to 1 percent slopesT177A22813901391hnk6sd00720041:20000
Lawet loamLc363353819cw5jsd06919921:20000
Lawet loamLw1175356450cyxdsd07319871:20000
Lawet loam, 0 to 2 percent slopesLn2657356675cz4nsd11519971:24000
Lawet-Davison loams, 0 to 2 percent slopesLp1786356677cz4qsd11519971:24000
Lawet loam, wet, 0 to 1 percent slopesLo880356676cz4psd11519971:24000
Lawet loam, 0 to 1 percent slopesT177A12225827981hv44sd61320111:24000

Map of Series Extent

Approximate geographic distribution of the LAWET 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 .