Soil Data Explorer - SAMDAY

Official Series Description

Lab Data Summary

Aggregate lab data for the SAMDAY soil series. This aggregation is based on all pedons with a current taxon name of SAMDAY, 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 SAMDAY 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 SAMDAY 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 SAMDAY series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-10-24), parsed OSD records (updated 2024-10-23) and snapshot of SC database (updated 2024-10-23).

Select annual climate data summaries for the SAMDAY 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 2024-10-23).

Geomorphic description summaries for the SAMDAY 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 2024-10-23).

Competing Series

Soil series competing with SAMDAY share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2024-10-23) and snapshot of the SC database (updated 2024-10-23).

Select annual climate data summaries for the SAMDAY 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 2024-10-23).

Geomorphic description summaries for the SAMDAY 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 2024-10-23).

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 SAMDAY, 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 2024-10-23).

Block Diagrams

No block diagrams are available.

Map Units

Map units containing SAMDAY 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
Shingle-Badland-Samday complex, 10 to 30 percent slopes	189	94930	349691	2vhzw	wy027	1993	1:24000
Samday-Savageton-Bahl association, 3 to 10 percent slopes	185	12470	349683	cqw3	wy027	1993	1:24000
Samday clay, 3 to 10 percent slopes	183	3155	349679	cqvz	wy027	1993	1:24000
Samday-Pierre clays, 3 to 30 percent slopes	184	1108	349681	cqw1	wy027	1993	1:24000
Shingle-Samday-Badland complex, 4 to 50 percent slopes	5433		3356672	2w7j3	wy043	1976	1:24000
Taluce-Shingle-Samday complex, 15 to 50 percent slopes	5450		3356673	2w7k3	wy043	1976	1:24000
Samday-Savageton complex, 6 to 30 percent slopes	96	47212	349505	2tvvz	wy045	1984	1:24000
Orella-Samday-Rock outcrop complex, 3 to 30 percent slopes	69	46097	349475	2tvvl	wy045	1984	1:24000
Shingle-Samday-Rock outcrop complex, hilly	100	45129	349383	cqkf	wy045	1984	1:24000
Samday-Grummit complex, 2 to 30 percent slopes	95	17775	349504	cqpb	wy045	1984	1:24000
Samday-Shingle-Worf complex, 3 to 15 percent slopes	97	2948	349506	cqpd	wy045	1984	1:24000
Shingle-Badland-Samday complex, 10 to 30 percent slopes	146	1656	1423944	2vhzw	wy045	1984	1:24000
Samday-Shingle-Badland complex, 10 to 45 percent slopes	206	16975	349904	2v08y	wy605	1995	1:24000
Samday-Samday, very shallow-Shingle clay loams, 6 to 40 percent slopes	204	7685	349902	2yryx	wy605	1995	1:24000
Samday-Savageton clay loams, 3 to 15 percent slopes	205	7108	349903	cr36	wy605	1995	1:24000
Shingle-Badland-Samday complex, 10 to 30 percent slopes	230	32025	1669785	2vhzw	wy609	2006	1:24000
Savageton-Samday complex, 3 to 15 percent slopes	227	2742	1669731	1t1h9	wy609	2006	1:24000
Shingle-Badland-Samday complex, 30 to 60 percent slopes	231	962	1669733	1t1hc	wy609	2006	1:24000
Samday-Shingle-Worf, loamy complex, 3 to 15 percent slopes	226	585	1669729	1t1h7	wy609	2006	1:24000
Samday very cobbly clay, 20 to 60 percent slopes	224	278	1669730	1t1h8	wy609	2006	1:24000
Samday-Shingle-Worf complex, 3 to 15 percent slopes	225	149	1669810	2wxyt	wy609	2006	1:24000
Taluce-Shingle-Samday complex, 15 to 50 percent slopes	5450		3358287	2w7k3	wy617		1:24000
Shingle-Samday-Badland complex, 4 to 50 percent slopes	5433		3358286	2w7j3	wy617		1:24000
Samday-Shingle-Badland complex, 10 to 45 percent slopes	SDE	78456	350923	2v08y	wy619	1971	1:24000
Samday-Savageton clay loams, 3 to 15 percent slopes	205	32	817247	wfdt	wy619	1971	1:24000
Savageton-Samday clay loams, 3 to 15 percent slopes	687	27	2383658	2wlrr	wy619	1971	1:24000
Cadoma-Renohill-Samday clay loams, 3 to 12 percent slopes	140	40133	502218	2xtvk	wy625	1985	1:24000
Shingle-Samday complex, 3 to 45 percent slopes	274	14265	502410	2yryn	wy625	1985	1:24000
Samday very cobbly clay, 20 to 60 percent slopes	272	9796	502408	jvsq	wy625	1985	1:24000
Savageton-Samday complex, 3 to 15 percent slopes	273	9295	502409	jvsr	wy625	1985	1:24000
Urban land-Savageton-Samday complex, 4 to 25 percent slopes	297	2548	502433	jvtj	wy625	1985	1:24000
Shingle-Badland-Samday complex, 10 to 30 percent slopes	332	588	1426090	2vhzw	wy625	1985	1:24000
Cadrina-like, extremely bouldery-Samday-Shingle complex, 6 to 40 percent slopes	5818		3171013	2zyb1	wy629		1:24000
Windwhistle-Worf-like-Samday complex, 4 to 30 percent slopes	5363		3171000	2z210	wy629		1:24000
Taluce-Shingle-Samday complex, 15 to 50 percent slopes	5450		2911928	2w7k3	wy629		1:24000
Shingle-Samday-Badland complex, 4 to 50 percent slopes	5433		2911895	2w7j3	wy629		1:24000
Worfka-Samday-Shingle complex, moist, 6 to 30 percent slopes	305	30309	361018	2yv6z	wy633	1987	1:24000
Shingle-Samday clay loams, moist, 3 to 55 percent slopes	263	17124	361046	2wlrs	wy633	1987	1:24000
Shingle-Worfka-Samday complex, 6 to 30 percent slopes	304	11648	361019	2yv70	wy633	1987	1:24000
Samday-Gayhart-Hilight clay loams, moist, 2 to 60 percent slopes	244	9763	360586	d36t	wy633	1987	1:24000
Shingle-Samday clay loams, 6 to 60 percent slopes	262	3428	361061	d3q4	wy633	1987	1:24000
Samday-Shingle-Badland complex, 10 to 45 percent slopes	326	1284	361228	2v08y	wy633	1987	1:24000
Samday-Hilight clay loams, 2 to 45 percent slopes	245	1119	360585	d36s	wy633	1987	1:24000
Samday-Shingle-Badland complex, 10 to 45 percent slopes	206	20044	817576	2v08y	wy705	2003	1:24000
Samday-Samday, very shallow-Shingle clay loams, 6 to 40 percent slopes	204	13096	817575	2yryx	wy705	2003	1:24000
Savageton-Samday clay loams, 3 to 15 percent slopes	313	7504	817577	2wlrr	wy705	2003	1:24000
Shingle-Badland-Samday complex, 10 to 30 percent slopes	131	176746	351509	2vhzw	wy709	1983	1:24000
Samday-Shingle-Worf complex, 3 to 15 percent slopes	129	70850	351507	2wxyt	wy709	1983	1:24000
Orella, dry-Rock outcrop-Samday complex, 3 to 30 percent slopes	125	16853	351503	2yv7p	wy709	1983	1:24000
Samday-Shingle-Badland complex, 10 to 45 percent slopes	208	324	361280	2v08y	wy709	1983	1:24000
Samday-Shingle-Worf complex, northeast, 3 to 15 percent slopes	244	10	1427901	1jxvb	wy709	1983	1:24000
Samday-Shingle-Badland complex, 10 to 45 percent slopes	684	165173	813948	2v08y	wy719	2013	1:24000
Savageton-Samday clay loams, 3 to 15 percent slopes	687	22607	1479155	2wlrr	wy719	2013	1:24000
Samday-Samday, very shallow-Shingle clay loams, 6 to 40 percent slopes	683	1410	1399142	2yryx	wy719	2013	1:24000
Shingle-Samday clay loams, moist, 3 to 55 percent slopes	785	86	1868574	2wlrs	wy719	2013	1:24000

Map of Series Extent

Approximate geographic distribution of the SAMDAY 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 2024-10-30).