Soil Data Explorer - KYLE

Official Series Description

Lab Data Summary

Aggregate lab data for the KYLE soil series. This aggregation is based on all pedons with a current taxon name of KYLE, 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 KYLE 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
60A	86P0596	86NE165017	Kyle	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.9166679,-103.9102783
60A	90P0888	90NE165001	Kyle	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.9791679,-103.5749969
60A	90P0889	90NE165002M	Kyle	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.9788895,-103.5744476
60A	90P0890	90NE165003M	Kyle	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.9791679,-103.5752792
63A	80P0250	79SD071001	Kyle	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.9477768,-101.8655548
67A	40A3121	S1964WY015002	Kyle	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.9880562,-104.351944

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KYLE 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 KYLE 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 KYLE 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 KYLE 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 KYLE 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 KYLE 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 KYLE 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 mountains figure.

Soil series sharing subgroup-level classification with KYLE, 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. SD-2012-03-15-12 | Custer and Pennington Counties, Prairie Parts - May 1996

   Pattern of soils and underlying material in the Bankard-Haverson-Lohmiller and the Samsil-Pierre associations (Soil Survey of Custer and Pennington Counties, Prairie Parts, SD; 1996).

2. SD-2012-03-15-31 | Fall River County - April 1982

   Pattern of soils in the Pierre-Samsil association (Soil Survey of Fall River County, SD; 1982).

3. SD-2012-03-15-53 | Jackson County, Northern Part - July 1987

   Pattern of soils and underlying material in the Samsil-Pierre and Haverson associations (Soil Survey of Jackson County, Northern Part, SD; 1987).

4. SD-2012-03-15-72 | Meade County, Northern Part - January 1986

   Pattern of soils and parent material in the Samsil association (Soil Survey of Meade County, Northern Part, SD; 1986).

5. SD-2012-03-15-94 | Shannon County - April 1971

   Representative pattern of soils in association 6 (Soil Survey of Shannon County, SD; 1971).

6. SD-2012-03-16-04 | Ziebach County - March 1990

   Pattern of soils and parent material in the Samsil-Pierre association (Soil Survey of Ziebach County, SD; 1990).

Map Units

Map units containing KYLE 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
Kyle silty clay, 4 to 7 percent slopes	Kn	8150	345751	cls8	mt111	1966	1:20000
Kyle silty clay, 1 to 4 percent slopes	Km	5416	345750	cls7	mt111	1966	1:20000
Kyle silty clay, 0 to 1 percent slopes	Kl	2472	345749	cls6	mt111	1966	1:20000
Kyle silty clay, 0 to 2 percent slopes	Ks	22471	346030	cm28	mt607	1970	1:24000
Kyle silty clay, 4 to 8 percent slopes	Ku	5272	346032	cm2b	mt607	1970	1:24000
Kyle gravelly silty clay, 8 to 15 percent slopes	KV	4867	346018	cm1w	mt607	1970	1:24000
Kyle clay, saline	Kw	4558	346033	cm2c	mt607	1970	1:24000
Pierre-Kyle clays, gently undulating	Pk	3662	2428546	2mj36	mt607	1970	1:24000
Kyle silty clay, 2 to 4 percent slopes	Kt	2565	346031	cm29	mt607	1970	1:24000
Kyle clay, 0 to 2 percent slopes	Kc	3095	347076	cn50	mt611	1971	1:24000
Kyle clay, 4 to 8 percent slopes	Ke	2906	347078	cn52	mt611	1971	1:24000
Kyle clay, 2 to 4 percent slopes	Kd	2229	347077	cn51	mt611	1971	1:24000
Kyle clay, 8 to 15 percent slopes	Kf	1582	347079	cn53	mt611	1971	1:24000
Kyle clay, 8 to 15 percent slopes	Kn	6090	347886	cp04	mt643	1967	1:20000
Kyle clay, 4 to 8 percent slopes	Km	1775	347885	cp03	mt643	1967	1:20000
Kyle clay, 2 to 4 percent slopes	Kl	272	347884	cp02	mt643	1967	1:20000
Kyle silty clay, 2 to 6 percent slopes	5359	39002	358122	2tnmc	ne045	1973	1:20000
Kyle-Hisle complex, 0 to 2 percent slopes	5360	7226	358123	d0nc	ne045	1973	1:20000
Kyle silty clay, 0 to 2 percent slopes	5358	5987	358121	2tnmb	ne045	1973	1:20000
Kyle silty clay, 2 to 6 percent slopes	5359	7419	357930	2tnmc	ne165	1993	1:20000
Kyle silty clay, 0 to 2 percent slopes	5358	2882	357929	2tnmb	ne165	1993	1:20000
Kyle clay, 2 to 6 percent slopes	KlB	29517	2768039	2rd41	sd019	1970	1:24000
Kyle clay, terrace	Kt	17745	353189	cvj6	sd019	1970	1:24000
Kyle-Pierre clays, 0 to 6 percent slopes	KuB	17132	353190	30wnb	sd019	1970	1:24000
Kyle clay, 0 to 2 percent slopes	KlA	11553	2768038	2rd40	sd019	1970	1:24000
Kyle clay, 6 to 9 percent slopes	KlC	616	2768040	2rd42	sd019	1970	1:24000
Kyle clay, moist, 2 to 6 percent slopes	P186B	383	2668875	2qt3h	sd019	1970	1:24000
Kyle clay, moist, 6 to 9 percent slopes	P186C	174	2668876	2qt3j	sd019	1970	1:24000
Kyle clay, 2 to 6 percent slopes	KyB	26481	2768046	2rd41	sd047	1980	1:24000
Kyle clay, 0 to 2 percent slopes	KyA	23067	2768045	2rd40	sd047	1980	1:24000
Kyle clay, 3 to 6 percent slopes	KyB	3259	354106	cwgs	sd055	1992	1:24000
Kyle clay, 0 to 3 percent slopes	KyA	1677	354105	cwgr	sd055	1992	1:24000
Kyle clay, 2 to 6 percent slopes	KyB	819	2768048	2rd41	sd063	1984	1:24000
Kyle clay, 2 to 6 percent slopes	614B	2007	2768051	2rd41	sd081	2007	1:24000
Kyle clay, 0 to 2 percent slopes	614A	633	2768050	2rd40	sd081	2007	1:24000
Kyle clay, moist, 2 to 6 percent slopes	P186B	118	2733294	2qt3h	sd081	2007	1:24000
Kyle clay	Ky	4148	353384	cvqh	sd095	1971	1:20000
Kyle clay, 2 to 6 percent slopes	KyB	24960	355852	cy93	sd137	1985	1:24000
Swanboy-Kyle clays, 2 to 15 percent slopes	SxC	2711	355896	cybj	sd137	1985	1:24000
Kyle clay, 2 to 6 percent slopes	KbB	50062	2768058	2rd41	sd600	1974	1:24000
Kyle clay, 0 to 2 percent slopes	KbA	19307	2768057	2rd40	sd600	1974	1:24000
Kyle soils, 2 to 6 percent slopes, mounded	KcB	5531	354322	cwpr	sd600	1974	1:24000
Kyle clay, moist, 2 to 6 percent slopes	P186B	431	2733425	2qt3h	sd600	1974	1:24000
Kyle clay, 2 to 6 percent slopes	KyB	10970	2768062	2rd41	sd601	1983	1:24000
Kyle clay, 0 to 2 percent slopes	KyA	3119	2768061	2rd40	sd601	1983	1:24000
Kyle clay, 2 to 6 percent slopes	KyB	25462	2768068	2rd41	sd606	2011	1:24000
Kyle clay, 0 to 2 percent slopes	KyA	18735	2768067	2rd40	sd606	2011	1:24000
Kyle clay, 6 to 9 percent slopes	KyC	7505	2768069	2rd42	sd606	2011	1:24000
Kyle clay, 0 to 1 percent slopes	KtA	2170	2580917	cyhn	sd606	2011	1:24000
Kyle clay, 2 to 6 percent slopes	N464B	106	2582894	2kqth	sd606	2011	1:24000
Kyle clay, 3 to 6 percent slopes	KyB	5136	2582633	cy2z	sd611	2011	1:24000
Kyle clay, 0 to 3 percent slopes	KyA	4381	2582632	cy2y	sd611	2011	1:24000
Kyle clay, 6 to 9 percent slopes	KyC	1396	2582634	cy30	sd611	2011	1:24000
Kyle clay, 6 to 9 percent slopes	N464C	236	2375342	2kqqy	sd612	2011	1:20000
Kyle clay, 2 to 6 percent slopes	N464B	179	2375421	2kqth	sd612	2011	1:20000
Kyle silty clay, 0 to 2 percent slopes	KzA	3788	2582714	2tnmb	sd613	2011	1:24000
Kyle clay, 6 to 9 percent slopes	N464C	12	2582805	2kqqy	sd613	2011	1:24000
Kyle-Shingle-Bidman association	36	23787	152081	537v	wy043	1976	1:24000

Map of Series Extent

Approximate geographic distribution of the KYLE 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).