Official Series Description


Lab Data Summary

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

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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 KRUSE, 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 KRUSE 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
Carlinton-Carrico-Kruse complex, 8 to 35 percent slopesCk37581644802pmz2id05720131:24000
Kruse-Teakean complex, 20 to 45 percent slopesKr2j42772501975v2vwid05720131:24000
Carrico-Carrico, dry-Kruse complex, 5 to 35 percent slopesCr42259644804pmz4id05720131:24000
Kruse-Brodeer complex, 15 to 45 percent slopesKr3153116892711tptmid05720131:24000
Kruse ashy silt loam, 35 to 65 percent slopesKr61234682651qxc0id05720131:24000
Kruse-Noil complex, 10 to 40 percent slopesKr1j9322501974v2vvid05720131:24000
Kruse-Aldermand-Noil complex, 40 to 65 percent slopeKr5893644755pmxkid05720131:24000
Kruse, dry-Kruse complex, 30 to 60 percent slopesKc2686677871qrctid05720131:24000
Carlinton-Kruse complex, 5 to 20 percent slopesCn3j5302501175v24did05720131:24000
Kruse silt loam, 30 to 65 percent slopes262363152981545wid60419811:24000
Kruse variant silt loam, 5 to 20 percent slopes27809152982545xid60419811:24000
Kruse-Ulricher association, 35 to 65 percent slopes1346962794242nn2id60619761:24000
Kruse ashy silt loam, 20 to 35 percent slopes1336049794232nn1id60619761:24000
Kruse ashy silt loam, 5 to 20 percent slopes1324423794222nn0id60619761:24000
Kruse ashy silt loam, 0 to 5 percent slopes131985794212nmzid60619761:24000
Kruse-Teakean complex, 5 to 35 percent slopes2y6v896030990102y6v8id60619761:24000
Keeler-Kruse complex, 15 to 30 percent slopes541331830990112wcrid60619761:24000
Kruse ashy silt loam, 15 to 30 percent slopes52125830990122wc5id60619761:24000
Keeler-Kruse complex, 30 to 60 percent slopes5414443099059nvf7id60619761:24000
Kruse ashy silt loam, 30 to 55 percent slopes5213926629162wcwid60619761:24000
Kruse fine gravelly silt loam, 35 to 65 percent slopes5771215347254pqid60819941:24000
Johnson-Kruse complex, 5 to 40 percent slopes546061796672nwxid61119941:24000
Kruse loam, 20 to 35 percent slopes6927796832nxfid61119941:24000
Kruse-Noil complex, 10 to 40 percent slopes1574799777320v2vvid61220031:24000
Kruse-Aldermand complex, 40 to 65 percent slopes1554117777325v2w0id61220031:24000
Carlinton-Kruse complex, 5 to 20 percent slopes482516776624v24did61220031:24000
Kruse ashy loam, 35 to 65 percent slopes1531570777326v2w1id61220031:24000
Kruse-Teakean complex, 20 to 45 percent slopes1581522777321v2vwid61220031:24000
Kruse-McCrosket complex, 35 to 65 percent slopes1561038777322v2vxid61220031:24000
Kruse-Aldermand complex, 20 to 40 percent slopes154492777324v2vzid61220031:24000
Kruse ashy loam, 20 to 35 percent slopes152175777323v2vyid61220031:24000
Kruse fine gravelly silt loam, 35 to 65 percent slopes54pq85285098654pqid6701:24000
Kruse ashy silt loam, 15 to 30 percent slopes52124967858752wc5wa06320121:24000
Keeler-Kruse complex, 15 to 30 percent slopes54133313858932wcrwa06320121:24000
Kruse ashy silt loam, 30 to 55 percent slopes52133045858972wcwwa06320121:24000
Keeler-Kruse complex, 30 to 60 percent slopes54142058621216nvf7wa06320121:24000
Kruse ashy silt loam, 8 to 15 percent slopes52111953858982wcxwa06320121:24000
Keeler-Kruse complex, 15 to 30 percent slopes541317426513372wcrwa06519781:24000

Map of Series Extent

Approximate geographic distribution of the KRUSE 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 .