Soil Data Explorer - WYMORE

Official Series Description

Lab Data Summary

Aggregate lab data for the WYMORE soil series. This aggregation is based on all pedons with a current taxon name of WYMORE, 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 WYMORE 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
106	02N0091	01NE067001	Wymore	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.2608566,-96.6450882
106	06KS005608	06KS005608	Wymore	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.564724,-95.3663864
106	40A2339	1958NE133002	WYMORE	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.0654889,-96.1705639
106	40A2340	1958NE133007	Wymore	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.0856917,-96.1280722
106	80P0433	1980NE127010	Wymore	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.3676389,-96.0475
106	81P0392	1981NE131001	Wymore	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.7383347,-96.4166641
106	81P0393	1981NE131002	WYMORE	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.7383347,-96.4113922
106	94P0096	1993NE067001	Wymore	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.0088882,-96.7766647
106	97P0085	1996NE067002	Wymore	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.5094452,-96.7580566
106	97P0086	1996NE067003	Wymore	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.1247215,-96.8604202
106	40A2337	60NE109001	Wymore	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.6241684,-96.5027771
106	40A2338	61NE109001	Wymore	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.5538417,-96.5433222
106	40A2208	75NE109025	Wymore	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.7075119,-96.5003052
106	40A2212	77NE109002	Wymore	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.6167194,-96.65035
106	92P0204	91NE109001	Wymore	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.8462222,-96.46625
106	99KS013003S	99KS013003S	Wymore	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.8333321,-95.5500031
106	99KS013004S	99KS013004S	Wymore	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.8333321,-95.5500031
106	40A2207	S1973NE109002	WYMORE	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.7169456,-96.7911148
106	00P0939	S2000KS131009	Wymore	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.8375244,-96.1347351
106	00P0940	S2000KS131010	Wymore	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.8966904,-96.221962
106	00P0941	S2000KS131011	Wymore	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.8950233,-96.2244644
106	02N0092	S2001KS131001	Wymore	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.9878769,-95.8891296
106	02N0483	S2001KS131010	Wymore	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.8588486,-96.2000809
106	02N0484	S2001KS131011	Wymore	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.8592949,-96.1946411
106	02N0485	S2001KS131012	Wymore	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.7368202,-96.1142426
106	02N0486	S2001KS131013	Wymore	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.7448769,-96.1040955
76	99KS149002	99KS149002	Wymore	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.431427,-96.5886765

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the WYMORE 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 WYMORE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-02) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the WYMORE 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 WYMORE 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 mountains figure.

Competing Series

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

Select annual climate data summaries for the WYMORE 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 WYMORE 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 mountains figure.

Soil series sharing subgroup-level classification with WYMORE, 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

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

1. KS-2012-01-25-09 | Pottawatomie County - December 1987

   Pattern of soils and parent material in the Clime-Tully-Benfield association (Soil Survey of Pottawatomie County, Kansas; 1987).

2. KS-2012-01-25-12 | Pottawatomie County - December 1987

   Pattern of soils and parent material in the Morrill-Ortello association (Soil Survey of Pottawatomie County, Kansas; 1987).

3. NE-2012-02-08-17 | Gage County - May 1964

   Schematic diagram showing the relationship of major soil series to parent materials in Gage County, Nebraska (Soil Survey of Gage County, Nebraska; May 1964).

4. NE-2012-02-13-66 | Nemaha County - December 1985

   Typical pattern of soils and parent material in the Pawnee-Nodaway-Gymer association (Soil Survey of Nemaha County, Nebraska; December 1985).

5. NE-2012-02-13-89 | Saunders County - January 1965

   Soils in the Sharpsburg-Burchard association (Soil Survey of Saunders County, Nebraska; January 1965).

6. NE-2012-02-13-90 | Saunders County - January 1965

   Soils in the Burchard-Shelby association (Soil Survey of Saunders County, Nebraska; January 1965).

Map Units

Map units containing WYMORE 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
Wymore silty clay loam, 3 to 6 percent slopes	7683	27641	1475377	2scz1	ks005	1998	1:24000
Wymore silty clay loam, 1 to 3 percent slopes	7681	7985	1475376	2qsk8	ks005	1998	1:24000
Wymore silty clay loam, 3 to 6 percent slopes, eroded	7684	305	1475378	2qskg	ks005	1998	1:24000
Wymore silty clay loam, 3 to 6 percent slopes	7683	67630	1152187	2scz1	ks013	1994	1:24000
Wymore silty clay loam, 1 to 3 percent slopes	7681	56921	1152186	2qsk8	ks013	1994	1:24000
Wymore-Baileyville complex, 3 to 6 percent slopes, eroded	7688	625	1152189	2scz3	ks013	1994	1:24000
Wymore silty clay loam, 3 to 6 percent slopes	7683	1575	747194	2scz1	ks043	1977	1:24000
Wymore silty clay loam, 1 to 3 percent slopes	7681	349	1479420	2qsk8	ks043	1977	1:24000
Wymore silty clay loam, 1 to 3 percent slopes	7681	19103	1480374	2qsk8	ks085	1976	1:24000
Wymore silty clay loam, 3 to 6 percent slopes, eroded	7684	13543	1480375	2qskg	ks085	1976	1:24000
Wymore silty clay loam, 3 to 6 percent slopes	7683	476	1481316	2scz1	ks085	1976	1:24000
Wymore silty clay loam, 3 to 6 percent slopes	7683	2470	1481326	2scz1	ks087	1974	1:24000
Wymore silty clay loam, 1 to 3 percent slopes	7681	1117	1480081	2qsk8	ks087	1974	1:24000
Wymore silty clay loam, 1 to 3 percent slopes	7681	172622	1457092	2qsk8	ks117	1977	1:24000
Wymore silty clay loam, 3 to 6 percent slopes, eroded	7684	28704	1457093	2qskg	ks117	1977	1:24000
Wymore-Baileyville complex, 3 to 6 percent slopes, eroded	7688	46	1457098	2scz3	ks117	1977	1:24000
Wymore silty clay loam, 1 to 3 percent slopes	7681	42322	1406034	2qsk8	ks131	1980	1:24000
Wymore-Baileyville complex, 3 to 6 percent slopes, eroded	7688	23090	1406036	2scz3	ks131	1980	1:24000
Wymore silty clay loam, 3 to 6 percent slopes, eroded	7684	2362	1406035	2qskg	ks131	1980	1:24000
Wymore silty clay loam, 1 to 3 percent slopes	7681	32532	1480729	2qsk8	ks149	1984	1:24000
Wymore silty clay loam, 3 to 6 percent slopes	7683	4084	1480730	2scz1	ks149	1984	1:24000
Wymore variant, fine sandy loam, 1 to 3 percent slopes	7687	1093	1480731	2scz2	ks149	1984	1:24000
Wymore silty clay loam, 0 to 1 percent slopes	7680	562	1480728	2sczd	ks149	1984	1:24000
Wymore silty clay loam, 1 to 3 percent slopes, eroded	7682	40621	1472339	2scz0	ks161	1970	1:24000
Wymore silty clay loam, 1 to 3 percent slopes	7681	12692	1472338	2qsk8	ks161	1970	1:24000
Wymore-Kennebec complex, 0 to 17 percent slopes	7690	9289	1472342	2scz4	ks161	1970	1:24000
Wymore silty clay loam, 3 to 6 percent slopes, eroded	7684	3079	1478250	2qskg	ks161	1970	1:24000
Wymore silty clay loam, 0 to 1 percent slopes	7680	2363	1472337	2sczd	ks161	1970	1:24000
Wymore silty clay loam, 3 to 6 percent slopes	7683	1414	1478249	2scz1	ks161	1970	1:24000
Wymore silty clay loam, 1 to 3 percent slopes	7681	496	2422751	2qsk8	ks177	1966	1:24000
Wymore silty clay loam, 3 to 6 percent slopes	7683	24	1473533	2scz1	ks177	1966	1:24000
Wymore silty clay loam, 3 to 6 percent slopes	7683	8495	1472182	2scz1	ks197	1988	1:24000
Wymore silty clay loam, 1 to 3 percent slopes	7681	3043	1454900	2qsk8	ks201	1988	1:24000
Wymore silty clay loam, 3 to 6 percent slopes, eroded	7684	362	1454901	2qskg	ks201	1988	1:24000
Wymore silty clay loam, 3 to 6 percent slopes, eroded	7684	11019	1691509	2qskg	ne025	1981	1:20000
Wymore silty clay loam, 2 to 6 percent slopes	7693	4635	1691508	2scz7	ne025	1981	1:20000
Wymore silty clay loam, 0 to 2 percent slopes	7689	4410	1691507	2qskf	ne025	1981	1:20000
Wymore silty clay loam, 2 to 6 percent slopes	7693	135763	1691124	2scz7	ne067	2000	1:12000
Wymore silty clay loam, 0 to 2 percent slopes	7689	69464	1691123	2qskf	ne067	2000	1:12000
Wymore silty clay loam, terrace, 0 to 2 percent slopes	7102	2205	1691125	2sczc	ne067	2000	1:12000
Wymore silty clay loam, 0 to 2 percent slopes	7689	5057	2219203	2qskf	ne095	1970	1:20000
Wymore silty clay loam, 2 to 6 percent slopes	7693	2766	2219204	2scz7	ne095	1970	1:20000
Wymore silty clay, 3 to 6 percent slopes, eroded	7695	42471	1691602	2scz8	ne097	1984	1:20000
Wymore silty clay loam, 2 to 6 percent slopes	7693	20039	1691601	2scz7	ne097	1984	1:20000
Wymore silty clay loam, 0 to 2 percent slopes	7689	6534	1691600	2qskf	ne097	1984	1:20000
Wymore silty clay loam, 3 to 6 percent slopes, eroded	7684	78905	1691404	2qskg	ne109	1977	1:20000
Wymore silty clay loam, 1 to 3 percent slopes	7681	12040	1691403	2qsk8	ne109	1977	1:20000
Wymore silty clay loam, 2 to 6 percent slopes	7693	7330	2219253	2scz7	ne109	1977	1:20000
Wymore silty clay, 3 to 6 percent slopes, eroded	7695	7015	2219258	2scz8	ne109	1977	1:20000
Wymore silty clay loam, 0 to 1 percent slopes	7680	4193	1691402	2qskh	ne109	1977	1:20000
Wymore silty clay loam, 0 to 2 percent slopes	7689	2731	2219252	2qskf	ne109	1977	1:20000
Wymore silty clay loam, 6 to 11 percent slopes	7697	1330	1691405	2scz9	ne109	1977	1:20000
Urban land-Wymore complex, 0 to 2 percent slopes	9721	611	1691398	1ts17	ne109	1977	1:20000
Wymore silty clay, 3 to 6 percent slopes, eroded	7695	30252	1691706	2scz8	ne127	1983	1:20000
Wymore silty clay loam, 2 to 6 percent slopes	7693	10259	1691705	2scz7	ne127	1983	1:20000
Wymore silty clay loam, 3 to 11 percent slopes, eroded	7692	4547	2219383	2scz6	ne127	1983	1:20000
Wymore silty clay loam, 0 to 2 percent slopes	7689	1493	1691704	2qskf	ne127	1983	1:20000
Wymore silty clay, 3 to 6 percent slopes, eroded	7695	62279	1691566	2scz8	ne131	1979	1:20000
Wymore silty clay loam, 3 to 6 percent slopes, eroded	7684	52090	2219333	2qskg	ne131	1979	1:20000
Wymore silty clay loam, 0 to 2 percent slopes	7689	9490	1691565	2qskf	ne131	1979	1:20000
Wymore silty clay loam, 2 to 6 percent slopes	7693	6252	2219321	2scz7	ne131	1979	1:20000
Wymore silty clay loam, 2 to 6 percent slopes	7693	21429	2219396	2scz7	ne133	1969	1:15840
Wymore silty clay loam, 3 to 6 percent slopes, eroded	7684	17872	1691648	2qskg	ne133	1969	1:15840
Wymore silty clay loam, 3 to 11 percent slopes, eroded	7692	13176	2219409	2scz6	ne133	1969	1:15840
Wymore silty clay loam, 1 to 3 percent slopes	7681	3364	1691646	2qsk8	ne133	1969	1:15840
Wymore silty clay loam, 3 to 6 percent slopes	7683	1800	1691647	2scz1	ne133	1969	1:15840
Wymore silty clay, 3 to 6 percent slopes, eroded	7695	715	2219408	2scz8	ne133	1969	1:15840
Wymore silty clay loam, 0 to 2 percent slopes	7689	160	2219395	2qskf	ne133	1969	1:15840
Wymore silty clay loam, terrace, 0 to 2 percent slopes	7102	4	2219388	2sczc	ne133	1969	1:15840
Wymore silty clay loam, 3 to 11 percent slopes, eroded	7692	50481	1691079	2scz6	ne147	1967	1:20000
Wymore silty clay loam, 1 to 3 percent slopes	7681	7760	1691077	2qsk8	ne147	1967	1:20000
Wymore silty clay loam, 3 to 11 percent slopes	7691	6743	1691078	2scz5	ne147	1967	1:20000
Wymore silty clay loam, 0 to 2 percent slopes	7689	2704	2229044	2qskf	ne147	1967	1:20000
Wymore silty clay loam, 0 to 1 percent slopes	7680	1125	1691076	2qskh	ne147	1967	1:20000
Wymore silty clay loam, 3 to 6 percent slopes, eroded	7684	1187	1691182	2qskg	ne151	1985	1:20000
Wymore silty clay loam, 3 to 6 percent slopes	7683	581	1691181	2scz1	ne151	1985	1:20000
Wymore silty clay loam, 0 to 2 percent slopes	7689	465	2219191	2qskf	ne151	1985	1:20000
Wymore silty clay loam, 2 to 6 percent slopes	7693	386	2219192	2scz7	ne151	1985	1:20000
Wymore silty clay loam, terrace, 0 to 2 percent slopes	7102	20	2219189	2sczc	ne151	1985	1:20000
Wymore silty clay loam, 3 to 6 percent slopes, eroded	7684	767	1691255	2qskg	ne159	1967	1:20000
Wymore silty clay loam, 0 to 1 percent slopes	7680	678	1691253	2qskh	ne159	1967	1:20000
Wymore silty clay loam, 1 to 3 percent slopes	7681	490	1691254	2qsk8	ne159	1967	1:20000
Wymore soils, 6 to 11 percent slopes, eroded	7699	335	1691257	2sczb	ne159	1967	1:20000

Map of Series Extent

Approximate geographic distribution of the WYMORE 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).