Official Series Description


Lab Data Summary

Aggregate lab data for the KUCERA soil series. This aggregation is based on all pedons with a current taxon name of KUCERA, 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 KUCERA 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
1383P086483ID043003Kucera7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0141678,-111.4683304
1313N17659S2012ID019004Kucera6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.53692,-111.826

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KUCERA 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 KUCERA 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 KUCERA 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 KUCERA 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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Competing Series

Soil series competing with KUCERA 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 KUCERA series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the KUCERA 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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

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 KUCERA, 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 KUCERA 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
Kucera-Ririe complex, 0 to 4 percent slope135171369024260252mfgwid65020111:24000
Kucera-Lostine complex, 0 to 4 percent slopes13455940524278382mhccid65020111:24000
Ririe-Lostine-Kucera complex, 4 to 20 percent slopes13522899924260382mfh9id65020111:24000
Kucera-Ririe-Lostine complex, 2 to 10 percent slopes13520694424260352mfh6id65020111:24000
Alpine-Kucera complex, 0 to 4 percent slopes13419165017120011vggvid65020111:24000
Kucera-Altaby complex, 0 to 8 percent slopes13448608186260620j62id65020111:24000
Jedediah-Kucera complex, 4 to 24 percent slopes1354753624314402mm3kid65020111:24000
Kucera-Dranyon-Tetonia complex, 2 to 15 percent slopes1346342924278422mhchid65020111:24000
Kucera silt loam, 12 to 30 percent slopes332285823662rpzid70719761:24000
Kucera silt loam, 30 to 60 percent slopes341120823672rq0id70719761:24000
Kucera silt loam, 25 to 55 percent slopes931278825702rxkid70819871:24000
Heglar-Kucera association, 20 to 45 percent slopes72793825472rwtid70819871:24000
Kucera silt loam, very steep293378826032rymid70919761:24000
Kucera silt loam, steep28772826022rylid70919761:24000
Kucera silt loam, 12 to 30 percent slopesKUE1284827362s2xid71019681:24000
Kucera-Chausse-Rexburg complex, 10 to 45 percent slopes122319316842861tjmtid71220081:24000
Lonjon-Kucera, dry-Sprollow, dry complex, 5 to 25 percent slopes1401229791552vknyid71220081:24000
Rexburg-Kucera complex, 4 to 12 percent slopes17485415434955m0id71220081:24000
Rexburg-Kucera complex, 1 to 4 percent slopes17374615434855lzid71220081:24000
Rexburg-Kucera complex, 12 to 20 percent slopes17532815435555m6id71220081:24000
Lonjon-Kucera-Sprollow complex, 10 to 25 percent slopes13919915432255l4id71220081:24000
Kucera silt loam, 8 to 20 percent slopes12115115430955kqid71220081:24000
Rexburg-Ririe-Kucera complex, 2 to 8 percent slopes1035720485570j98kid71519941:24000
Ririe-Iphil-Kucera complex, 2 to 8 percent slopes1143711485582j98yid71519941:24000
Hillfield-Kucera complex, 4 to 30 percent slopes382198485631j9bjid71519941:24000
Hillfield-Kucera complex, 30 to 50 percent slopes39938485632j9bkid71519941:24000
Kucera silt loam, 4 to 12 percent slopes63129485659j9cfid71519941:24000
Rexburg, very deep-Kucera complex, 1 to 4 percent slopes700I82661592365bpnid7161:24000
Bothwell-Rexburg, very deep-Kucera complex, 1 to 12 percent slopes2019415529896312x3mlid7161:24000
Rexburg, deep-Kucera-Rock outcrop complex, 1 to 4 percent slopes700J26901594195bwkid7161:24000
Rexburg, very deep-Ririe, deep-Kucera complex, 1 to 8 percent slopes700H21711594205bwlid7161:24000
Ririe, very deep-Kucera complex, 2 to 10 percent slopes710H18811594265bwsid7161:24000
Rexburg, very deep-Kucera complex, cool, 1 to 4 percent slopes700II153223706952kkx1id7161:24000
Rexburg, very deep-Iphil, deep-Kucera complex, 1 to 4 percent slopes700G15251594215bwmid7161:24000
Rexburg, very deep-Kucera complex, 4 to 12 percent slopes700L14051592375bppid7161:24000
Rexburg, deep-Rock outcrop-Kucera complex, 4 to 8 percent slopes700K7961594185bwjid7161:24000
Kucera silt loam, 4 to 8 percent slopes455A4711592005bnhid7161:24000
Rexburg, very deep-Kucera complex, 12 to 20 percent slopes700T4131592435bpwid7161:24000
Rexburg, very deep-Kucera complex, cool, 4 to 12 percent slopes700LL31623706962kkx2id7161:24000
Kucera silt loam, 8 to 15 percent slopes455B2821592015bnjid7161:24000
Ririe, very deep-Kucera complex, cool, 4 to 8 percent slopes710HH19724264102mfw9id7161:24000
Kucera silt loam, cool, 12 to 20 percent slopes455CC17722489082fh5fid7161:24000
Rexburg, very deep-Kucera complex, cool, 12 to 20 percent slopes700TT16223707012kkx7id7161:24000
Kucera silt loam, cool, 4 to 12 percent slopes455AA15822487882fh1kid7161:24000
Ririe-Lostine-Kucera complex, 4 to 20 percent slopes135221625152502qf4zid75819981:24000
Kucera-Lostine silt loams, 2 to 4 percent slopes505656837662t54id76219881:24000
Kucera-Sarilda silt loams, 2 to 6 percent slopes545465837702t58id76219881:24000
Kucera, bedrock substratum-Lostine silt loams, 1 to 6 percent slopes554474837712t59id76219881:24000
Rin-Kucera silt loams, 4 to 12 percent slopes953439838142t6pid76219881:24000
Kucera-Lostine silt loams, 4 to 8 percent slopes512594837672t55id76219881:24000
Kucera-Lostine silt loams, 0 to 2 percent slopes492291837642t52id76219881:24000
Kucera-Sarilda very fine sandy loams, 1 to 4 percent slopes531528837692t57id76219881:24000
Sadorus-Kucera complex, 1 to 6 percent slopes106996836752t26id76219881:24000
Jipper-Ririe-Kucera complex, 1 to 8 percent slopes40820837572t4vid76219881:24000
Kucera, bedrock substratum-Sarilda silt loams, 1 to 4 percent slopes56703837722t5bid76219881:24000
Kucera-Lostine very fine sandy loams, 1 to 4 percent slopes48423837632t51id76219881:24000
Kucera-Lostine silt loams, 8 to 12 percent slopes52341837682t56id76219881:24000
Kucera-Ririe complex, 0 to 4 percent slopes1351742625152332qf4fid76619781:24000
Kucera-Ririe-Lostine complex, 2 to 10 percent slopes1352021425152342qf4gid76619781:24000
Bothwell-Rexburg, very deep-Kucera complex, 1 to 12 percent slopes2019110532389892x3mlid77019681:24000
Rexburg-Kucera complex, 4 to 12 percent slopes174292530955m0wy7231:24000
Rexburg-Kucera complex, 12 to 20 percent slopes175292531055m6wy7231:24000

Map of Series Extent

Approximate geographic distribution of the KUCERA 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 .