Soil Data Explorer - KYLER

Official Series Description

Lab Data Summary

Aggregate lab data for the KYLER soil series. This aggregation is based on all pedons with a current taxon name of KYLER, 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 KYLER were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). 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
28A	05N0665	S2005NV017004	Kyler	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.9049606,-114.687233

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KYLER 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 KYLER 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 KYLER 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 KYLER 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 KYLER 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 KYLER 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 KYLER 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 KYLER, 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 KYLER 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
Theriot-Kyler-Rock outcrop association	250ec	61	2390465	2l7gs	ca763	1984	1:24000
Kyler-Eaglepass-Rock outcrop association, warm	KER	613	645069	2s224	nv611	1967	1:24000
Penelas-Kyler association	PE	1407	495625	jmqx	nv622	1972	1:24000
Kyler-Rock outcrop complex, 8 to 50 percent slopes	KT	707	495584	2v431	nv622	1972	1:24000
Kyler-Amtoft, very shallow-Rock outcrop association	3036	1537	2406204	2tzg7	nv709	2012	1:24000
Ubehebe-Penalas-Kyler assosciation	1526	390	2406201	2lrvd	nv709	2012	1:24000
Kyler-Eaglepass-Rock outcrop association	1092	19	2406195	2tzg0	nv709	2012	1:24000
Kyler-Rock outcrop complex, 8 to 50 percent slopes	3674	3174	2480721	2v431	nv713	2014	1:24000
Kyler-Eaglepass-Rock outcrop association	1090	1797	2480495	2p84z	nv713	2014	1:24000
Kyler-Eaglepass-Rock outcrop association, warm	1091	79	2480496	2s224	nv713	2014	1:24000
Kyler-Logring-Rock outcrop association, warm	1571	22301	478123	2s22n	nv754	1992	1:24000
Kyler-Eaglepass-Rock outcrop association, warm	1570	17652	478122	2s224	nv754	1992	1:24000
Kyler, very stony-Rock outcrop-Kyler association	3673	393	1904680	21xz9	nv754	1992	1:24000
Amtoft-Kyler association	1540	27185	478657	j22k	nv766	1994	1:24000
Kyler-Rock outcrop association	1541	18197	478658	j22l	nv766	1994	1:24000
Kyler-Amtoft-Jericho association	1542	10037	478659	j22m	nv766	1994	1:24000
Armespan-Kyler-Heist association	1581	6309	478664	j22s	nv766	1994	1:24000
Lomoine-Kyler-Budihol association	1821	15474	476812	j051	nv774	1985	1:24000
Stewval-Kyler association	4155	12279	476944	2v42v	nv774	1985	1:24000
Kyler very gravelly fine sandy loam, 15 to 50 percent slopes	1844	12247	476818	2s23k	nv774	1985	1:24000
Logring-Kyler association, steep	7000	8759	477013	j0cj	nv774	1985	1:24000
Kyler-Rock outcrop complex, 8 to 50 percent slopes	1842	6298	476816	2v431	nv774	1985	1:24000
Theriot, moist-Kyler-Rock outcrop association	2032	4440	476854	2v433	nv774	1985	1:24000
Kyler-Gabbvally association	1840	4149	476815	j054	nv774	1985	1:24000
Lomoine-Kyler-Petspring association	1822	4035	476813	j052	nv774	1985	1:24000
Kyler-Logring-Rock outcrop association	1843	3048	476817	2s23z	nv774	1985	1:24000
Rodad-Theriot-Kyler association	2100	1692	476864	2v41k	nv774	1985	1:24000
Logring-Eaglepass-Kyler complex, 15 to 75 percent slopes	7002	1560	477015	j0cl	nv774	1985	1:24000
Logring-Kyler association	7001	1516	477014	j0ck	nv774	1985	1:24000
Radol-Kyler-Logring association	3676	7275	2632636	2rfwq	nv778	2013	1:24000
Kyler-Rock outcrop complex, 8 to 50 percent slopes	3580	5480	2215713	2v431	nv778	2013	1:24000
Logring-Rock outcrop-Kyler association	3670	1980	2215718	2dcms	nv778	2013	1:24000
Kyler-Amtoft-Rock outcrop association	3030	1966	2215672	2dcl9	nv778	2013	1:24000
Kyler-Eaglepass-Rock outcrop association	1092	1074	2215609	2dcj8	nv778	2013	1:24000
Amtoft-Kyler association	1360	725	2215637	2dck5	nv778	2013	1:24000
Logring-Kyler-Eaglepass association	3672	507	2512898	2whnn	nv778	2013	1:24000
Kyler-Amtoft, very shallow-Rock outcrop association	3036	91	2215676	2dclf	nv778	2013	1:24000
Kyler-Amtoft association	3033	75	2215673	2dclb	nv778	2013	1:24000
Kyler-Amtoft, thin surface-Rock outcrop association	3036	19677	479996	j3gr	nv779	2004	1:24000
Amtoft-Kyler association	1360	13566	479974	j3g1	nv779	2004	1:24000
Kyler-Amtoft association	3033	13400	479993	j3gn	nv779	2004	1:24000
Kyler-Amtoft-Rock outcrop association	3030	12889	479990	j3gk	nv779	2004	1:24000
Kyler association	3039	6051	479999	j3gv	nv779	2004	1:24000
Kyler-Amtoft-Eaglepass association	1307	3107	479955	j3ff	nv779	2004	1:24000
Kyler-Eaglepass-Rock outcrop association	1092	3058	780492	v655	nv779	2004	1:24000
Tarnach-Kyler-Jericho association	3253	2949	480042	j3j7	nv779	2004	1:24000
Rock outcrop-Kyler-Buzztail association	3035	1714	479995	j3gq	nv779	2004	1:24000
Kyler-Eaglepass-Rock outcrop association, warm	650	8850	480564	2s224	nv780	1990	1:24000
Kyler-Rock outcrop complex, 8 to 50 percent slopes	3580	1759	2634059	2v431	nv780	1990	1:24000
Berzatic-Kyler-Rock outcrop association	1262	11923	480723	j476	nv781	1994	1:24000
Kyler very gravelly fine sandy loam, 15 to 50 percent slopes	1580	3504	480790	2s23k	nv781	1994	1:24000
Logring-Kyler association	1670	779	480799	j49n	nv781	1994	1:24000
Logring-Kyler-Eaglepass association	3672	36295	481024	2whnn	nv783	1991	1:24000
Kyler-Rock outcrop complex, 8 to 50 percent slopes	3580	31062	481001	2v431	nv783	1991	1:24000
Kyler-Eaglepass-Rock outcrop association, warm	3570	17678	480998	2s224	nv783	1991	1:24000
Logring-Rock outcrop-Kyler association	3670	16382	481022	j4jv	nv783	1991	1:24000
Penelas-Kyler-Rock outcrop association	3730	14236	481032	j4k5	nv783	1991	1:24000
Eaglepass-Kyler-Rock outcrop complex, 15 to 75 percent slopes	3572	12619	481000	j4j4	nv783	1991	1:24000
Radol-Kyler-Logring association	3676	146	2817274	2tzjv	nv783	1991	1:24000
Kyler-Eaglepass-Rock outcrop association, warm	1091	63331	481121	2s224	nv784	2006	1:24000
Kyler-Rock outcrop complex, 8 to 50 percent slopes	3580	46749	811934	2v431	nv784	2006	1:24000
Kyler-Eaglepass-Rock outcrop association	1090	27151	481120	j4n0	nv784	2006	1:24000
Kyler, very stony-Rock outcrop-Kyler association	3673	11496	1454691	1ktqj	nv784	2006	1:24000
Logring-Kyler-Eaglepass association	3670	10677	481208	2whnn	nv784	2006	1:24000
Amtoft-Kyler association, warm	1370	4175	1454688	1ktqf	nv784	2006	1:24000
Kyler-Logring-Rock outcrop association, warm	1093	3640	481123	2s22n	nv784	2006	1:24000
Ubehebe-Penelas-Kyler association	1525	2486	980461	11x7s	nv784	2006	1:24000
Kyler-Amtoft-Eaglepass association	1307	2233	1395622	1hv82	nv784	2006	1:24000
Amtoft-Kyler association	1362	1259	1395623	1hv83	nv784	2006	1:24000
Kyler-Lodar association	1096	353	1144502	17dyf	nv784	2006	1:24000
Kyler-Amtoft, thin surface-Rock outcrop association	3036	214	1395628	1hv88	nv784	2006	1:24000
Rodad-Theriot-Kyler association	1125	9683	484912	2v41k	nv796	1984	1:63360
Weepah-Kyler-Rock outcrop association	490	8924	485069	j8rd	nv796	1984	1:63360
Logring-Kyler-Ubehebe association	640	4254	485104	j8sj	nv796	1984	1:63360
Theriot-Kyler-Rock outcrop association	250	4230	484968	2v432	nv796	1984	1:63360
Theriot-Kyler-Leo association	252	1244	484970	j8n6	nv796	1984	1:63360
Stewval-Kyler association	650	800	477673	2v42v	nv799	1991	1:24000

Map of Series Extent

Approximate geographic distribution of the KYLER 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).