Soil Data Explorer - STENDAL

Official Series Description

Lab Data Summary

Aggregate lab data for the STENDAL soil series. This aggregation is based on all pedons with a current taxon name of STENDAL, 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 STENDAL were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
114A	GN7932	1979IN055032	Stendal	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.1611528,-87.1732861
114A	PK8112	1981IN125012	Stendal	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.5099806,-87.0949694
114A	93P0491	S1988IN119035	Stendal	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.2486115,-87.0138855
114B	JN7922	1979IN071022	Stendal	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.8892528,-86.1293944
120A	07KY-107-001	07KY107001	Stendal	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.3220482,-87.8439331
120A	67KY-107-003	67KY-107-003	Stendal	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.3109528,-87.6749917
120C	LW7818	1978IN093018	Stendal	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.9624889,-86.4946139
120C	BR8108	2017IN013002	Stendal	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.1280528,-86.1684722
120C	WS8014	2017IN175003	Stendal	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.5196694,-85.9576194
n/a	CO-123	1959-OH029-123	Stendal	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	AT-008	1961-OH009-008	Stendal	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	78KY-121-005	78KY-121-005	Stendal	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the STENDAL 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 STENDAL 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 STENDAL 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 STENDAL 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 STENDAL 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 STENDAL 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).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the STENDAL 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 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 STENDAL, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

1. IN-2012-01-19-20 | Gibson County - June 1989

   Pattern of soils and parent material in the Hosmer association (Soil Survey of Gibson County, Indiana; 1989).

2. KY-2012-01-26-19 | Bath County - September 1963

   Typical landscape in a river valley and the relative position of the principal soils (Soil Survey of Bath County, Kentucky; September 1963).

3. KY-2012-01-27-56 | Elliott County - 1965

   Diagram of Muskingum-Ramsey-Wellston soil association, showing relationship of soil series to topography and parent material (Soil Survey of Elliott County, Kentucky; 1965).

4. KY-2012-01-27-58 | Elliott County - 1965

   Diagram of Muskingum-Montevallo-Ramsey association, showing relationship of soil series to topography and parent material (Soil Survey of Elliott County, Kentucky; 1965).

5. KY-2012-01-27-64 | Estill and Lee Counties - August 1974

   Pattern of soils and underlying material in the Shelocta-Latham-Jefferson association (Soil Survey of Estill and Lee Counties, Kentucky; August 1974).

6. KY-2012-01-30-04 | Grayson County - December 1972

   Relationship of soils to topography and underlying material in the Zanesville-Gilpin-Wellston-Weikert association (Soil Survey of Grayson County, Kentucky; December 1972).

7. KY-2012-01-30-06 | Grayson County - December 1972

   Relationship of soils to topography and underlying material in the Sadler-Zanesville-Wellston association (Soil Survey of Grayson County, Kentucky; December 1972).

8. KY-2012-01-31-25 | Knox County and Eastern Part of Whitley County - May 1988

   Pattern of soils, topography, and underlying material in the Shelocta-Latham-DeKalb map unit (Soil Survey of Knox County and Eastern Part of Whitley County, Kentucky; May 1988).

9. KY-2012-01-31-27 | Knox County and Eastern Part of Whitley County - May 1988

   Pattern of soils, topography, and underlying material in the Sehlocta-Latham map unit (Soil Survey of Knox County and Eastern Part of Whitley County, Kentucky; May 1988).

10. KY-2012-01-31-29 | Knox County and Eastern Part of Whitley County - May 1988

    Pattern of soils, topography, and underlying material in the Stendal-Shelocta map unit (Soil Survey of Knox County and Eastern Part of Whitley County, Kentucky; May 1988).

11. KY-2012-01-31-32 | Knox County and Eastern Part of Whitley County - May 1988

    Pattern of soils, topography, and underlying material in the Wernock-Shelocta-Latham map unit (Soil Survey of Knox County and Eastern Part of Whitley County, Kentucky; May 1988).

12. KY-2012-02-01-16 | McCreary-Whitley Area - 1970

    General location of the Atkins, Pope, and Tate soils on flood plains and stream terraces in association 1 (Soil Survey of McCreary-Whitley Area, Kentucky; 1970).

13. KY-2012-02-01-34 | Montgomery County - January 1986

    The pattern of soils and relationship to topography and underlying material in the Tilsit-Morehead-Tyler general soil map unit (Soil Survey of Montgomery County, Kentucky; January 1986).

14. OH-2012-02-16-41 | Scioto County - January 1989

    Typical pattern of soils and parent material in the Shelocta-Steinsburg-Latham association (Soil Survey of Scioto County, Ohio; January 1989).

Map Units

Map units containing STENDAL 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
Philo and Stendal silt loams, 0 to 2 percent slopes	PiA	8160	523370	kklx	al015	1959	1:20000
Atkins and Stendal soils, local alluvium, 0 to 2 percent slopes	AsA	7651	523288	kkj8	al015	1959	1:20000
Philo and Stendal fine sandy loams, 0 to 2 percent slopes	PhA	4881	523369	kklw	al015	1959	1:20000
Philo and Stendal soils, local alluvium, 0 to 2 percent slopes	PkA	2467	523371	kkly	al015	1959	1:20000
Philo and Stendal soils, local alluvium	Pm	6112	328937	c18w	al043	1960	1:20000
Stendal soils, local alluvium	Sn	2945	329520	c1wp	al057	1963	1:15840
Stendal silt loam, 0 to 2 percent slopes, frequently flooded, very brief duration	StdAV	2674	202304	6shy	in005	2002	1:12000
Stendal silt loam, 0 to 2 percent slopes, rarely flooded	StdAQ	789	202305	6shz	in005	2002	1:12000
Stendal silt loam, 0 to 2 percent slopes, frequently flooded, brief duration	St	2520	535601	2wh46	in013	1985	1:15840
Stendal silt loam, frequently flooded, very long duration	Sv	522	535602	kzbh	in013	1985	1:15840
Stendal silt loam, 0 to 2 percent slopes, rarely flooded	StdAQ	1390	201141	6r9f	in019	2001	1:12000
Stendal silt loam, 0 to 2 percent slopes, occasionally flooded, very brief duration	StdAW	1323	201143	6r9h	in019	2001	1:12000
Stendal silt loam, frequently flooded	Sn	11152	159631	5c3d	in021	1980	1:15840
Stendal silt loam, 0 to 2 percent slopes, frequently flooded, brief duration	Sr	9806	162978	2wh46	in027	1969	1:20000
Stendal silt loam, frequently flooded	St	27893	535655	kzd6	in037	1978	1:15840
Stendal silt loam, 0 to 2 percent slopes, rarely flooded	StdAQ	393	185210	2wh47	in043	2000	1:12000
Stendal silt loam, frequently flooded	Sr	11033	160158	5cnd	in051	1986	1:15840
Stendal silt loam, frequently flooded	St	10790	161579	5f47	in055	1984	1:15840
Stendal silt loam, 0 to 2 percent slopes, rarely flooded	StdAQ	9203	620351	2wh47	in071	1985	1:15840
Stendal silt loam, 0 to 2 percent slopes, frequently flooded, brief duration	StdAH	6214	1907353	2wh46	in071	1985	1:15840
Urban land-Stendal complex, 0 to 2 percent slopes, rarely flooded	UgmAQ	100	1907677	2212z	in071	1985	1:15840
Stendal silt loam, 0 to 2 percent slopes, frequently flooded, very brief duration	StdAV	53	2027084	261bt	in071	1985	1:15840
Stendal silt loam, 0 to 2 percent slopes, frequently flooded, brief duration	StdAH	1369	633226	p7xn	in079	2010	1:12000
Stendal silt loam, 0 to 2 percent slopes, rarely flooded	StdAQ	543	1613455	1r4xy	in079	2010	1:12000
Stendal silt loam, clayey substratum, 0 to 2 percent slopes, frequently flooded, brief duration	StwAH	2453	1651547	1sfkq	in093	1982	1:15840
Stendal silt loam, 0 to 2 percent slopes, occasionally flooded, very brief duration	StdAW	610	1708167	2wh45	in101	1984	1:15840
Stendal silt loam, 0 to 2 percent slopes, frequently flooded, brief duration	St	4120	535564	2wh46	in105	1979	1:15840
Stendal silt loam, 0 to 2 percent slopes, frequently flooded, brief duration	StdAH	2	1442997	1kfk9	in117	1980	1:15840
Stendal silt loam, 0 to 2 percent slopes, frequently flooded, brief duration	StdAH	692	165855	5kl5	in119	1997	1:12000
Stendal silt loam, 0 to 2 percent slopes, frequently flooded, brief duration	StdAH	1541	535903	2wh46	in123	1997	1:12000
Stendal silt loam, frequently flooded	So	1748	161937	5fhs	in125	1983	1:15840
Stendal silt loam, 0 to 2 percent slopes, frequently flooded, brief duration	StdAH	4214	165792	5kj4	in143	1995	1:12000
Stendal silt loam, 0 to 2 percent slopes, occasionally flooded, very brief duration	StdAW	3341	165793	5kj5	in143	1995	1:12000
Stendal silt loam, 0 to 2 percent slopes, rarely flooded	StdAQ	921	165794	5kj6	in143	1995	1:12000
Stendal silt loam, 0 to 2 percent slopes, frequently flooded, brief duration	Sn	13689	160049	2wh46	in147	1966	1:15840
Stendal silt loam	Sn	11706	162716	5g9x	in153	1966	1:15840
Stendal silt loam	St	5616	162768	5gcl	in163	1972	1:15840
Stendal silt loam, 0 to 2 percent slopes, frequently flooded, brief duration	Sn	14371	159977	2wh46	in173	1976	1:15840
Stendal silt loam, 0 to 2 percent slopes, frequently flooded, brief duration	Sf	13063	535505	2wh46	in175	1984	1:15840
Stendal silt loam, 0 to 2 percent slopes, occasionally flooded, very brief duration	So	1718	535506	2wh45	in175	1984	1:15840
Stendal silt loam	St	1100	550263	lglf	ky043	1980	1:20000
Stendal silt loam	St	2865	549082	lfcb	ky047	1977	1:20000
Stendal silt loam, occasionally flooded	Sn	433	552537	ljys	ky051	1994	1:24000
Stendal silt loam, 0 to 2 percent slopes, occasionally flooded	St	5890	549689	2wh44	ky085	1967	1:20000
Stendal silt loam, 0 to 2 percent slopes, occasionally flooded	Ss	674	549291	2wh44	ky107	1974	1:12000
Stendal silt loam, frequently flooded	St	307	550544	lgwh	ky173	1983	1:20000
Stendal silt loam, 0 to 2 percent slopes, occasionally flooded	Sn	33960	551276	2wh44	ky183	1983	1:20000
Stendal loam	Sn	33	552457	ljw6	ky199	1969	1:12000
Stendal silt loam	Sm	2672	550424	lgrm	ky605	1975	1:20000
Stendal silt loam, 0 to 2 percent slopes, occasionally flooded	St	2081	549628	2wh44	ky607	1992	1:20000
Stendal silt loam, frequently flooded	St	20076	552235	ljn1	ky627	1984	1:20000
Stendal silt loam	Sn	11875	552301	ljq5	ky628	1973	1:20000
Stendal silt loam, terrace	So	5813	552302	ljq6	ky628	1973	1:20000
Stendal fine sandy loam, sandy variant	Ss	493	552303	ljq7	ky628	1973	1:20000
Stendal silt loam	St	2650	1478826	1lmv2	ky645	1971	1:20000
Stendal silt loam, 0 to 3 percent slopes, occasionally flooded	Stn1AO	2323	2450454	2n7wx	oh053	1988	1:15840
Stendal silt loam, occasionally flooded	St	671	536047	kzsv	oh079	1981	1:15840
Stendal silt loam, 0 to 3 percent slopes, occasionally flooded	Stn1AO	639	2451056	2n8jb	oh079	1981	1:15840
Stendal silt loam, occasionally flooded	St	1126	536185	kzy9	oh087	1989	1:15840
Stendal silt loam, 0 to 3 percent slopes, occasionally flooded	Stn1AO	533	2451117	2n8l9	oh087	1989	1:15840
Stendal silt loam, occasionally flooded	Ss	1726	537728	l1k2	oh131	1984	1:15840
Stendal silt loam, occasionally flooded	St	2195	537316	l13s	oh145	1984	1:15840

Map of Series Extent

Approximate geographic distribution of the STENDAL 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).