Soil Data Explorer - SAWICKI

Official Series Description

Lab Data Summary

Aggregate lab data for the SAWICKI soil series. This aggregation is based on all pedons with a current taxon name of SAWICKI, 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 SAWICKI were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). 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 SAWICKI 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.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the SAWICKI series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-06) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the SAWICKI series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2023-10-09).

Geomorphic description summaries for the SAWICKI 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 (updated 2023-10-04).

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with SAWICKI share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-06) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the SAWICKI series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2023-10-09).

Geomorphic description summaries for the SAWICKI 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 (updated 2023-10-04).

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with SAWICKI, 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 (updated 2023-10-02).

Block Diagrams

No block diagrams are available.

Map Units

Map units containing SAWICKI 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
Sawicki-Martinsdale, extremely stony complex, 8 to 25 percent slopes	466E	9	3039642	1hwp7	mt602	1963	1:20000
Sawicki cobbly loam, 2 to 8 percent slopes, very stony	361C	1633	155424	56qp	mt622	1997	1:24000
Sawicki-Catgulch complex, 35 to 60 percent slopes, very stony	761F	1583	155715	5712	mt622	1997	1:24000
Sawicki cobbly loam, 8 to 15 percent slopes, very stony	361D	1341	155425	56qq	mt622	1997	1:24000
Sawicki cobbly loam, 0 to 4 percent slopes	261B	1188	155357	56nj	mt622	1997	1:24000
Sawicki cobbly loam, 4 to 8 percent slopes	261C	1106	155358	56nk	mt622	1997	1:24000
Sawicki cobbly loam, moist 8 to 25 percent slopes, very stony	661E	839	155644	56ys	mt622	1997	1:24000
Sawicki cobbly loam, 8 to 25 percent slopes, bouldery	461D	619	155511	56th	mt622	1997	1:24000
Sawicki, stony-Catgulch, very stony complex, 15 to 35 percent slopes	761E	483	155714	5711	mt622	1997	1:24000
Blaincreek-Sawicki complex, 4 to 15 percent slopes	750C	1599	2495281	2psp3	mt624	2021	1:24000
Blaincreek-Sawicki complex, 0 to 4 percent slopes	750B	571	2526421	2qlxf	mt624	2021	1:24000
Brickner, extremely stony-Skyview, very stony-Sawicki, stony complex, 15 to 35 percent slopes	704E	378	2487413	2phc4	mt624	2021	1:24000
Blaincreek, very stony-Tolbert, extremely stony-Sawicki, stony complex, 15 to 35 percent slopes	703E	191	2487412	2phc3	mt624	2021	1:24000
Sawicki, very stony-Blaincreek, very stony-Tolbert, bouldery, complex, 15 to 45 percent slopes	1658E	1153	150669	51s9	mt627	1998	1:24000
Sawicki-Clasoil complex, 8 to 35 percent slopes, bouldery, warm	1655E	885	150665	51s5	mt627	1998	1:24000
Sawicki, stony-Blaincreek-Tolbert, very stony, complex, 15 to 45 percent slopes	1654E	780	150664	51s4	mt627	1998	1:24000
Sawicki, very bouldery-Crampton, bouldery-Catgulch, bouldery, complex, 15 to 45 percent slopes	1657E	723	150667	51s7	mt627	1998	1:24000
Blaincreek, very stony-Sawicki, very stony-Tolbert, very bouldery, complex, 35 to 70 percent slopes	1451F	691	150620	51qq	mt627	1998	1:24000
Sawicki-Clasoil complex, 8 to 35 percent slopes, bouldery	1652E	489	150663	51s3	mt627	1998	1:24000
Sawicki-Bielenberg, very stony-Tolbert, very stony, complex, 15 to 45 percent slopes	1656E	421	150666	51s6	mt627	1998	1:24000
Clasoil, very stony-Sawicki, bouldery, complex, 4 to 15 percent slopes	2350D	71	150911	5213	mt627	1998	1:24000
Sawicki, stony-Blaincreek, very stony, complex, 4 to 15 percent slopes	1658D	61	150668	51s8	mt627	1998	1:24000
Brickner, extremely stony-Skyview, very stony-Sawicki, stony complex, 15 to 35 percent slopes	704E	1425	2512446	2phc4	mt632		1:24000
Sawicki, extremely stony-Wickes, very stony-Tolbert, very stony complex, 25 to 60 percent slopes	390F	1234	2392813	2l9xj	mt632		1:24000
Blaincreek, very stony-Tolbert, extremely stony-Sawicki, stony complex, 15 to 35 percent slopes	703E	660	2512445	2phc3	mt632		1:24000
Sawicki, extremely stony-Blaincreek, very stony complex, 15 to 35 percent slopes	140E	459	2392775	2l9w9	mt632		1:24000
Sawicki, extremely bouldery-Tolbert, extremely bouldery-Rock outcrop complex, 15 to 35 percent slopes	265E	240	2486250	2pg4m	mt632		1:24000
Sawicki, very stony-Wickes, extremely bouldery complex, 15 to 35 percent slopes	80E	177	2486309	2pg6j	mt632		1:24000
Sawicki-Martinsdale, extremely stony complex, 8 to 25 percent slopes	466E	111	2632243	1hwp7	mt632		1:24000
Sawicki-Clasoil complex, 8 to 35 percent slopes, bouldery	1652E	148	1703070	1v55r	mt635	2006	1:24000
Sawicki, stony-Catgulch, very stony complex, 15 to 35 percent slopes	198	12	146566	4xhy	mt636	1983	1:24000
Sawicki, extremely stony-Blaincreek, very bouldery complex, 15 to 35 percent slopes	140E	2599	637158	pd0h	mt637	2014	1:24000
Sawicki, extremely stony-Wickes, very stony-Tolbert, very stony complex, 25 to 60 percent slopes	390F	1268	1387647	1hkyt	mt637	2014	1:24000
Sawicki-Martinsdale, extremely stony complex, 8 to 25 percent slopes	466E	1114	1396991	1hwp7	mt637	2014	1:24000
Sawicki, very stony-Wickes, extremely bouldery complex, 15 to 35 percent slopes	80E	700	1487636	1ly08	mt637	2014	1:24000
Sawicki, extremely bouldery-Tolbert, extremely bouldery-Rock outcrop complex, 15 to 35 percent slopes	265E	217	637534	pddm	mt637	2014	1:24000
Sawicki-Perma complex, 2 to 8 percent slopes	329C	910	2438037	2mtzc	mt638	1985	1:24000
Sawicki-Perma-Sheafman complex, 8 to 15 percent slopes	329D	469	2438038	2mtzd	mt638	1985	1:24000
Sawicki, very stony-Perma, stony, complex, 15 to 35 percent slopes	329E	259	2438039	2mtzf	mt638	1985	1:24000
Sawicki, very stony-Perma, stony complex, 2 to 8 percent slopes	359C	89	2438041	2mtzh	mt638	1985	1:24000
Shanley-Sawicki complex, 8 to 15 percent slopes	358D	13	2438040	2mtzg	mt638	1985	1:24000
Sawicki, extremely bouldery-Bowery complex, 4 to 25 percent slopes	421E	202	149985	5127	mt639	2000	1:24000
Sawicki-Bitterroot-Capiron complex, 1 to 60 percent slopes	512F	1750	633716	p8fg	mt645	2013	1:12000
Sawicki, extremely stony-Whitlash, rubbly-Quast, stony complex, 8 to 15 percent slopes	520D	1401	158588	5b0r	mt645	2013	1:12000
Sawicki-Whitlash, stony complex, 15 to 45 percent slopes	541F	1111	633731	p8fy	mt645	2013	1:12000
Sawicki, stony-Whitlash, rubbly-Farnuf complex, 2 to 8 percent slopes	520C	441	633719	p8fk	mt645	2013	1:12000
Sawicki-Whitlash, stony complex, 15 to 45 percent slopes	541F	493	2487192	2ph40	mt647	2007	1:24000
Wickes, stony-Whitlash, rubbly-Farnuf complex, 2 to 8 percent slopes	520C	6	2487186	2ph3t	mt647	2007	1:24000
Sawicki, extremely stony-Whitlash, rubbly-Quast, stony complex, 8 to 15 percent slopes	520D	2	2487187	2ph3v	mt647	2007	1:24000
Vershal, very cobbly - Sawicki, extremely stony - Absarook complex, 8 to 45 percent slopes	5610E	5845	156732	582w	mt669		1:24000
Winspect, extremely bouldery-Meagher, extremely bouldery-Sawicki, extremely bouldery-Bacbuster, stony complex, cool, 15 to 45 percent slopes	5620E	3971	699329	rgq0	mt669		1:24000
Bacbuster-Sawicki-Corbly complex, 15 to 60 percent slopes	5619F	3521	711075	rvxx	mt669		1:24000
Sawicki-Sinnigam, very cobbly loam-Bachus, cobbly loam complex, cool, 15 to 45 percent slopes	5644E	3292	699349	rgqn	mt669		1:24000
Deville-Sawicki-Shambo complex, 15 to 60 percent slopes	5641F	3065	696051	rc98	mt669		1:24000
Sawicki, very bouldery-Bowery-Whitlash, very cobbly complex, 15 to 60 percsent slopes	7602F	1305	699357	rgqx	mt669		1:24000
Sawicki-Tolbert,very stony-Rock outcrop complex, 35 to 70 percent slopes	8609F	948	156773	5846	mt669		1:24000
Sawicki, extremely bouldery-Rock outcrop-Whitlash, stony complex, 35 to 70 percent slopes	6706F	838	156755	583m	mt669		1:24000
Sawicki, extremely bouldery-Bowery complex, 4 to 25 percent slopes	421E	18	620233	ntdj	mt669		1:24000

Map of Series Extent

Approximate geographic distribution of the SAWICKI 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 (updated 2023-10-04).