Soil Data Explorer - RAZOR

Official Series Description

Lab Data Summary

Aggregate lab data for the RAZOR soil series. This aggregation is based on all pedons with a current taxon name of RAZOR, 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 RAZOR 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
67B	12N8339	S2012CO001003	Razor	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.9760278,-103.8053333
67B	12N7619	S2012CO005002	Razor	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.5956111,-103.7343611
69	90P0037	08CO073026	Razor	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.5959722,-103.4849972
69	89P0619	89CO073007	Razor	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.5961113,-103.4852753

Water Balance

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

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 RAZOR, 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. KS-2012-01-20-19 | Cheyenne County - June 1989

   Typical pattern of soils and parent material in the Colby-Razor association (Soil Survey of Cheyenne County, Kansas; 1989).

2. SD-2012-03-15-14 | Custer and Pennington Counties, Prairie Parts - May 1996

   Pattern of soils and underlying material in the Ottumwa-Razor and the Midway-Razor associations (Soil Survey of Custer and Pennington Counties, Prairie Parts, SD; 1996).

3. SD-2012-03-15-42 | Haakon County - 1998

   Typical pattern of soils and parent material in the Ottumwa-Kirley and Ottumwa-Razor-Midway associations (Soil Survey of Haakon County, SD; 1998).

Map Units

Map units containing RAZOR 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
Razor clay loam, 1 to 6 percent slopes	35	13313	94324	354q	co017	1985	1:24000
Razor-Midway clay loams, 6 to 12 percent slopes	36	6767	94325	354r	co017	1985	1:24000
Stoneham-Razor complex, 2 to 6 percent slopes	44	5784	94334	3551	co017	1985	1:24000
Midway-Razor clay loams, 5 to 15 percent slopes	51	5623	96847	37s3	co063	1996	1:24000
Midway-Razor clay loams, moist, 5 to 15 percent slopes	154	44291	105235	3jhp	co073	2001	1:24000
Razor clay loam, moist, 1 to 5 percent slopes	178	30154	105259	3jjg	co073	2001	1:24000
Razor clay loam, dry, 2 to 5 percent slopes	177	19138	105258	2t529	co073	2001	1:24000
Fort Collins-Razor, moist, complex, 5 to 15 percent slopes	128	9845	105209	3jgv	co073	2001	1:24000
Midway-Razor clay loams, dry, 1 to 18 percent slopes	153	7945	105234	2t52f	co073	2001	1:24000
Fort-Razor complex, 5 to 15 percent slopes	132	1735	105213	3jgz	co073	2001	1:24000
Razor silty clay, dry, 1 to 4 percent slopes	CaD	20228	94720	2t527	co089	1966	1:15840
Razor-Heldt complex, 3 to 9 percent slopes	60	23481	95024	35w9	co121	1982	1:24000
Razor-Midway complex, 9 to 15 percent slopes	61	10156	95025	35wb	co121	1982	1:24000
Razor-Midway complex, 3 to 9 percent slopes	39	2842	95083	35y6	co125	1976	1:24000
Razor clay, 3 to 25 percent slopes	RaE	3823	498752	jqzs	co622	1968	1:20000
Midway-Razor clay loams, dry, 1 to 18 percent slopes	127	22148	2766628	2t52f	co625	1975	1:24000
Schamber-Razor complex, 8 to 50 percent slopes	82	18148	95447	369y	co625	1975	1:24000
Razor-Midway complex	75	10235	95439	369p	co625	1975	1:24000
Razor stony clay loam, 5 to 15 percent slopes	74	3496	95438	369n	co625	1975	1:24000
Terry-Razor complex, 3 to 20 percent slopes	91	3147	95457	36b8	co625	1975	1:24000
Razor clay loam, 3 to 9 percent slopes	73	2799	95437	369m	co625	1975	1:24000
Razor clay loam, dry, 2 to 5 percent slopes	128	841	2766647	2t529	co625	1975	1:24000
Razor silty clay, 0 to 3 percent slopes, eroded	Re2	42877	95531	2t52d	co626	1974	1:24000
Razor clay loam, dry, 2 to 5 percent slopes	Ra	18344	95530	2t529	co626	1974	1:24000
Razor silty clay, 2 to 20 percent slopes	69	2662	496508	jnnd	co627	1980	1:24000
Razor clay loam, 1 to 12 percent slopes	68	433	496507	jnnc	co627	1980	1:24000
Razor silty clay, dry, 1 to 4 percent slopes	CaC	26288	3390088	2t527	co628	2008	1:24000
Midway-Razor-Rock outcrop complex, dry, 1 to 15 percent slopes	MP	24997	105379	2t52h	co628	2008	1:24000
Razor-Heldt-Midway cobbly clay loams, 15 to 30 percent slopes	127	639	497404	jpl9	co641	1980	1:24000
Razor-Heldt clay loams, 9 to 25 percent slopes	126	493	497403	jpl8	co641	1980	1:24000
Razor silty clay loam, 3 to 12 percent slopes	66	2677	496646	jnsv	co679	1976	1:24000
Razor-Midway silty clay loams, 5 to 20 percent slopes	1751	6431	1149575	17l72	ks023	1987	1:24000
Kim-Razor complex, 3 to 6 percent slopes	1646	1510	1149569	17l6w	ks023	1987	1:24000
Razor clay, 1 to 6 percent slopes	1748	511	1150541	17m77	ks109	1962	1:24000
Razor clay, 1 to 6 percent slopes	1748	2426	1150206	17lwf	ks199	1984	1:24000
Midway-Razor clay loams, 4 to 7 percent slopes	Mw	18085	345780	clt6	mt111	1966	1:20000
Razor clay loam, 2 to 7 percent slopes	Ra	7337	345786	cltd	mt111	1966	1:20000
Razor-Cushman complex, 2 to 4 percent slopes	Rc	1239	345787	cltf	mt111	1966	1:20000
Razor-Thedalund clay loams, 4 to 15 percent slopes	Rb	1343	347119	cn6d	mt611	1971	1:24000
Razor clay loam, 2 to 8 percent slopes	Ra	1343	347118	cn6c	mt611	1971	1:24000
Midway-Razor silty clay loams, 3 to 15 percent slopes	MrD	21923	353208	cvjt	sd019	1970	1:24000
Razor silty clay loam, 2 to 6 percent slopes	RcB	8857	353224	cvkb	sd019	1970	1:24000
Razor silty clay loam, 6 to 9 percent slopes	RcC	617	353225	cvkc	sd019	1970	1:24000
Razor silty clay loam, 0 to 2 percent slopes	RcA	474	353223	cvk9	sd019	1970	1:24000
Razor-Midway complex, 6 to 15 percent slopes	RbD	32068	354146	cwj2	sd055	1992	1:24000
Ottumwa-Razor silty clays, 6 to 9 percent slopes	OxC	18422	354136	cwhr	sd055	1992	1:24000
Ottumwa-Razor-Savo complex, 6 to 15 percent slopes	OyC	12385	354137	cwhs	sd055	1992	1:24000
Razor-Shingle complex, 6 to 15 percent slopes	RdD	1156	354147	cwj3	sd055	1992	1:24000
Shingle-Razor complex, 15 to 25 percent slopes	SwE	149	354164	cwjn	sd055	1992	1:24000
Razor silty clay, 6 to 9 percent slopes	RaC	53	354145	cwj1	sd055	1992	1:24000
Razor silty clay, 2 to 6 percent slopes	RaB	3	354144	cwj0	sd055	1992	1:24000
Razor-Midway complex, 6 to 15 percent slopes	RbD	30812	2580962	cyk3	sd606	2011	1:24000
Ottumwa-Razor complex, 6 to 9 percent slopes	OvC	8288	2580949	cyjp	sd606	2011	1:24000
Razor silty clay, 6 to 9 percent slopes	RaC	3940	2580961	cyk2	sd606	2011	1:24000
Razor silty clay, 2 to 6 percent slopes	RaB	3396	2580960	cyk1	sd606	2011	1:24000
Razor-Midway silty clay loams, 6 to 15 percent slopes	RmD	17472	2582663	cy3y	sd611	2011	1:24000
Emigrant-Razor complex, 6 to 9 percent slopes	ErC	6421	2581017	cy2g	sd611	2011	1:24000
Emigrant-Razor complex, 9 to 15 percent slopes	ErD	5295	2581018	cy2h	sd611	2011	1:24000
Emigrant-Razor complex, 1 to 6 percent slopes	ErB	4719	2581016	cy2f	sd611	2011	1:24000
Razor-Hisle complex, 2 to 9 percent slopes	RhC	2708	2582662	cy3x	sd611	2011	1:24000
Winler-Razor clay loams, 2 to 10 percent slopes	206	34022	349293	2y6dc	wy011	1978	1:24000
Razor clay loam, 2 to 10 percent slopes	141	15356	349222	2y6dk	wy011	1978	1:24000
Samsil-Razor complex, 2 to 10 percent slopes	158	2873	349240	cqdt	wy011	1978	1:24000
Samsil-Razor complex, 10 to 30 percent slopes	159	2709	349241	cqdv	wy011	1978	1:24000
Razor-Samsil complex, 3 to 10 percent slopes	142	2682	349223	2y6dl	wy011	1978	1:24000
Renohill-Razor-Samsil, dry complex, 6 to 20 percent slopes	RED	45614	350913	2xtvf	wy619	1971	1:24000
Razor-Gaynor, dry-Samsil, dry complex, 6 to 30 percent slopes	RAD	41194	350910	2xtvj	wy619	1971	1:24000
Renohill-Razor association, undulating	REC	2405	350912	cs4r	wy619	1971	1:24000

Map of Series Extent

Approximate geographic distribution of the RAZOR 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).