Soil Data Explorer - COCHETOPA

Official Series Description

Lab Data Summary

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

There are insufficient data to create the lab data summary figure.

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the COCHETOPA 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 COCHETOPA 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 COCHETOPA 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 COCHETOPA 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 COCHETOPA 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 COCHETOPA 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 COCHETOPA 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 COCHETOPA, 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 COCHETOPA 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
Cochetopa clay loam, 2 to 6 percent slopes	23	2887	498287	jqhs	co637	1986	1:24000
Cochetopa-Gothic complex, 25 to 45 percent slopes, extremely stony	41	91	3106859	jpd8	co648		1:24000
Cochetopa-Antrobus, extremely stony association, 25 to 50 percent slopes	AG19	74	1415077	1jhhn	co654		1:24000
Cochetopa-Antrobus association, 12 to 25 percent slopes	18	25955	497956	jq53	co655	1984	1:24000
Cochetopa-Antrobus association, 25 to 50 percent slopes	19	13702	497957	jq54	co655	1984	1:24000
Cochetopa-Antrobus association, 6 to 12 percent slopes	17	4315	497955	jq52	co655	1984	1:24000
Cochetopa-Clayburn complex, 12 to 40 percent slopes	125	1085	509473	k34m	co660	1994	1:24000
Cochetopa loam, 5 to 30 percent slopes	CoE	8931	498192	jqdq	co662	1968	1:24000
Cochetopa-Harkness association, 10 to 50 percent slopes	118	1260	2453835	2ncdz	co664	1987	1:24000
Cochetopa stony loam, 10 to 40 percent slopes	25	15020	496601	jnrd	co679	1976	1:24000
Cochetopa-Clayburn complex, 12 to 40 percent slopes	24	11211	496684	jnv2	co682	1986	1:24000
Cochetopa loam, 9 to 50 percent slopes	17	17100	496756	2w4zr	co683	1977	1:24000
Cochetopa-Jerry complex, 25 to 50 percent slopes	19	14700	496758	jnxg	co683	1977	1:24000
Cochetopa-Jerry complex, 12 to 25 percent slopes	18	1200	496757	jnxf	co683	1977	1:24000
Cochetopa-Adel-Hapgood loams, 5 to 25 percent slopes	18	17025	496857	jp0n	co684	1984	1:24000
Anvik, warm-Cochetopa-Passar complex, 3 to 25 percent slopes	9	9926	496936	jp36	co684	1984	1:24000
Cochetopa-Adel-Hapgood loams, 25 to 45 percent slopes	19	8845	496858	jp0p	co684	1984	1:24000
Cowdrey-Cochetopa-Quander loams, 5 to 25 percent slopes	32	7452	496873	jp15	co684	1984	1:24000
Cochetopa-Jerry loams, 12 to 25 percent slopes	28	7174	496868	jp10	co684	1984	1:24000
Cochetopa-Gothic-Quander loams, 5 to 25 percent slopes	25	7017	496865	jp0x	co684	1984	1:24000
Cochetopa-Gothic-Hapgood loams, 5 to 25 percent slopes	23	6420	496863	jp0v	co684	1984	1:24000
Cochetopa-Antrobus complex, 5 to 25 percent slopes	20	5514	496860	jp0r	co684	1984	1:24000
Adel-Cochetopa-Mayoworth loams, 25 to 65 percent slopes	2	4908	496859	jp0q	co684	1984	1:24000
Adel-Cochetopa-Mayoworth loams, 5 to 25 percent slopes	1	4851	496821	jnzh	co684	1984	1:24000
Cochetopa loam, 9 to 50 percent slopes	17	4818	496856	jp0m	co684	1984	1:24000
Hapgood-Clayburn-Cochetopa loams, 20 to 65 percent slopes	55	4172	496898	jp1z	co684	1984	1:24000
Cochetopa-Clayburn-Emerald loams, 5 to 25 percent slopes	21	4092	496861	jp0s	co684	1984	1:24000
Cochetopa-Clayburn-Emerald loams, 25 to 65 percent slopes	22	3206	496862	jp0t	co684	1984	1:24000
Cochetopa-Gothic-Hapgood loams, 25 to 65 percent slopes	24	2375	496864	jp0w	co684	1984	1:24000
Cochetopa-Gothic-Quander loams, 25 to 65 percent slopes	26	2116	496866	jp0y	co684	1984	1:24000
Cochetopa-Gourley-Quander complex, 5 to 25 percent slopes	27	1870	496867	jp0z	co684	1984	1:24000
Hapgood-Dunlatop-Cochetopa loams, 20 to 65 percent slopes	56	509	496899	jp20	co684	1984	1:24000
Cochetopa loam, 9 to 50 percent slopes	23	2364	496972	2w4zr	co685	1979	1:24000
Cochetopa-Jerry loams, 12 to 25 percent slopes	24	1518	496973	jp4d	co685	1979	1:24000
Routt-Cochetopa-Binco complex, 10 to 30 percent slopes, extremely stony	167	15239	497132	jp9j	co686	1992	1:31680
Cochetopa loam, 12 to 25 percent slopes	37	7452	497212	jpd3	co686	1992	1:31680
Cochetopa-Gothic complex, 10 to 25 percent slopes, extremely bouldery	40	6647	497216	jpd7	co686	1992	1:31680
Cochetopa-Gothic complex, 25 to 45 percent slopes, extremely stony	41	6219	497217	jpd8	co686	1992	1:31680
Cochetopa-Jerry complex, 3 to 15 percent slopes, extremely stony	42	4679	497218	jpd9	co686	1992	1:31680
Cochetopa loam, warm, 3 to 12 percent slopes	39	4147	497214	jpd5	co686	1992	1:31680
Cochetopa loam, 25 to 65 percent slopes	38	3403	497213	jpd4	co686	1992	1:31680
Jerry-Cochetopa complex, 5 to 35 percent slopes	108	3214	497067	jp7f	co686	1992	1:31680
Cochetopa-Trout Creek families, complex, 0 to 10 percent slopes	70	18292	708349	rs2z	wy632		1:24000
Cochetopa-Trout Creek families, complex, 10 to 25 percent slopes	71	9411	708355	rs35	wy632		1:24000
Cowdrey-Cochetopa families, complex, 25 to 40 percent slopes	25	6193	707864	rrlb	wy632		1:24000
Trout Creek-Cochetopa families, complex, 25 to 40 percent slopes	69	5550	708350	rs30	wy632		1:24000
Cochetopa-Ute families, complex, 0 to 10 percent slopes	98	3187	708431	rs5m	wy632		1:24000
Cochetopa-Ute families, complex, 10 to 25 percent slopes	99	1054	708435	rs5r	wy632		1:24000
Cochetopa family-Mollic Palecryalfs complex, 0 to 15 percent slopes	201	2000	151952	533p	wy663	2012	1:24000

Map of Series Extent

Approximate geographic distribution of the COCHETOPA 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).