Soil Data Explorer - COPENHAVER

Official Series Description

Lab Data Summary

Aggregate lab data for the COPENHAVER soil series. This aggregation is based on all pedons with a current taxon name of COPENHAVER, 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 COPENHAVER 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
43B	99P0428	99MT077001	Copenhaver	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.3511391,-112.4970016

Water Balance

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

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with COPENHAVER 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 COPENHAVER 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 COPENHAVER 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 COPENHAVER, 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 COPENHAVER 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
Copenhaver-Ratiopeak, very stony-Rock outcrop complex, 4 to 25 percent slopes	224E	221	2403807	20d8s	mt605	2007	1:24000
Taylorspring, rubbly-Copenhaver, extremely stony-Libeg, rubbly complex, 8 to 45 percent slopes	900F	99	2403813	2lpcc	mt605	2007	1:24000
Libeg-Copenhaver families-Rubble land complex, steep ridges and mountain slopes	51VH2	52	1859608	20f2c	mt605	2007	1:24000
Copenhaver, extremely stony-Taylorspring, very stony-Rock outcrop complex, 15 to 50 percent slopes	82F	2151	1901745	21txm	mt612	2011	1:24000
Taylorspring, rubbly-Copenhaver, extremely stony-Libeg, rubbly complex, 8 to 45 percent slopes	900F	1549	1685997	1tlf0	mt612	2011	1:24000
Copenhaver-Ratiopeak, very stony-Rock outcrop complex, 4 to 25 percent slopes	224E	491	1858846	20d8s	mt612	2011	1:24000
Copenhaver, extremely stony-Taylorspring, very stony-Rock outcrop complex, 15 to 50 percent slopes	82F	189	2520811	21txm	mt614	2012	1:24000
Libeg-Copenhaver-Rock outcrop complex, 35 to 60 percent slopes	954F	607	609574	ng9p	mt616	2003	1:24000
Libeg-Copenhaver-Rock outcrop complex, 35 to 60 percent slopes, moderately impacted	1954F	513	155279	56l0	mt616	2003	1:24000
Libeg-Copenhaver-Rock outcrop complex, 15 to 35 percent slopes	954E	474	155173	56gl	mt616	2003	1:24000
Redchief-Copenhaver gravelly loams, 15 to 35 percent slopes, moderately impacted	753E	355	155043	56bd	mt616	2003	1:24000
Libeg-Monad-Copenhaver complex, 15 to 35 percent slopes	854E	319	155111	56dl	mt616	2003	1:24000
Libeg-Copenhaver-Rock outcrop complex, 15 to 35 percent slopes, moderately impacted	1954E	117	155278	56kz	mt616	2003	1:24000
Libeg-Monad-Copenhaver complex, 35 to 60 percent slopes	854F	111	155112	56dm	mt616	2003	1:24000
Libeg-Monad-Copenhaver complex, 35 to 60 percent slopes, moderately impacted	1854F	90	155267	56km	mt616	2003	1:24000
Redfern-Copenhaver-Rock outcrop complex, 15 to 45 percent slopes	5025E	84	154863	564l	mt616	2003	1:24000
Libeg-Monad-Copenhaver complex, 15 to 35 percent slopes, moderately impacted	1854E	71	155276	56kx	mt616	2003	1:24000
Copenhaver, stony-Libeg, very stony-Rock outcrop complex, 15 to 60 percent slopes, moderately impacted	1025F	41	155285	56l6	mt616	2003	1:24000
Copenhaver, stony-Libeg, very stony-Rock outcrop complex, 15 to 60 percent slopes	5025F	40	154864	564m	mt616	2003	1:24000
Libeg-Copenhaver-Rock outcrop complex, 35 to 60 percent slopes	130F	611	144197	4v1j	mt621	1997	1:24000
Libeg-Copenhaver-Rock outcrop complex, 15 to 35 percent slopes	130E	529	144196	4v1h	mt621	1997	1:24000
Libeg-Copenhaver-Rock outcrop complex, 8 to 15 percent slopes	130D	342	144195	4v1g	mt621	1997	1:24000
Copenhaver-Libeg complex, 15 to 35 percent slopes	745E	35	144559	4vf6	mt621	1997	1:24000
Copenhaver-Libeg complex, 35 to 60 percent slopes	745F	29	144560	4vf7	mt621	1997	1:24000
Copenhaver-Libeg complex, 8 to 15 percent slopes	745D	16	144558	4vf5	mt621	1997	1:24000
Bangtail-Copenhaver complex, 8 to 25 percent slopes	679E	7030	155655	56z4	mt622	1997	1:24000
Bangtail-Copenhaver-Adel complex, 15 to 35 percent slopes	879E	6288	155760	572j	mt622	1997	1:24000
Bangtail-Copenhaver complex, 35 to 60 percent slopes	679F	3138	155656	56z5	mt622	1997	1:24000
Timberlin-Copenhaver complex, 35 to 60 percent slopes	694F	2924	155665	56zg	mt622	1997	1:24000
Copenhaver-Rock outcrop complex, 8 to 35 percent slopes	178E	1584	155307	56lx	mt622	1997	1:24000
Libeg, stony-Copenhaver complex, 15 to 45 percent slopes	480E	935	155522	56tv	mt622	1997	1:24000
Adel-Copenhaver complex, 4 to 15 percent slopes	814D	597	155738	571t	mt622	1997	1:24000
Copenhaver flaggy loam, 35 to 60 percent slopes	178F	581	155308	56ly	mt622	1997	1:24000
Libeg, very stony-Copenhaver, extremely stony-Adel complex, 15 to 45 percent slopes	580E	543	155604	56xh	mt622	1997	1:24000
Rocko, stony-Copenhaver, extremely stony complex, 35 to 60 percent slopes	894F	484	155763	572m	mt622	1997	1:24000
Adel-Copenhaver complex, 15 to 35 percent slopes	814E	409	155739	571v	mt622	1997	1:24000
Cheadle-Copenhaver-Sebud complex, 15 to 35 percent slopes	170E	297	2523223	nrxh	mt624	2021	1:24000
Skaggs-Copenhaver, stony families, complex, 4 to 15 percent slopes	1263D	1954	2393203	2lbb3	mt632		1:24000
Cheadle-Copenhaver-Sebud complex, 15 to 35 percent slopes	170E	1270	2911084	nrxh	mt632		1:24000
Libeg-Copenhaver families, complex, low relief mountain slopes and ridges	75VH2	6795	149546	50m2	mt635	2006	1:24000
Libeg-Copenhaver families-Rubble land complex, steep ridges and mountain slopes	51VH2	5078	149465	50jg	mt635	2006	1:24000
Libeg-Sebud-Copenhaver families, complex, high relief mountain slopes and ridges	71VH3	3445	149510	50kx	mt635	2006	1:24000
Libeg-Opitz-Copenhaver families, complex, steep glaciated mountain slopes and ridges	15GH3	340	149381	50fr	mt635	2006	1:24000
Libeg-Monad-Copenhaver complex, 15 to 35 percent slopes	854E	76	1703236	1v5c3	mt635	2006	1:24000
Bangtail-Copenhaver complex, 35 to 60 percent slopes	168	21	146561	4xhs	mt636	1983	1:24000
Cheadle-Copenhaver-Sebud complex, 15 to 35 percent slopes	170E	18596	618806	nrxh	mt637	2014	1:24000
Bangtail-Copenhaver-Adel complex, 15 to 35 percent slopes	879E	1722	2493522	572j	mt637	2014	1:24000
Bangtail-Copenhaver complex, 35 to 60 percent slopes	679F	1509	1858533	20cyp	mt637	2014	1:24000
Bangtail-Copenhaver complex, 8 to 25 percent slopes	679E	727	1858536	20cys	mt637	2014	1:24000
Copenhaver-Libeg complex, 15 to 60 percent slopes	7601F	615	2486036	2pfxq	mt637	2014	1:24000
Copenhaver-Dalys-Bridger complex, 8 to 45 percent slopes	5646E	221	2486035	2pfxp	mt637	2014	1:24000
Copenhaver-Rock outcrop complex, 8 to 35 percent slopes	178E	10	2377795	2kt92	mt637	2014	1:24000
Libeg-Monad-Copenhaver complex, 8 to 15 percent slopes	854D	4027	145930	4wvf	mt644	1995	1:24000
Libeg-Monad-Copenhaver complex, 15 to 35 percent slopes	854E	2529	145931	4wvg	mt644	1995	1:24000
Redchief-Copenhaver gravelly loams, 15 to 35 percent slopes	845E	544	145919	4wv2	mt644	1995	1:24000
Libeg-Monad-Copenhaver complex, 35 to 60 percent slopes	854F	455	145932	4wvh	mt644	1995	1:24000
Redchief-Copenhaver gravelly loams, 8 to 15 percent slopes	845D	169	145918	4wv1	mt644	1995	1:24000
Copenhaver-Mollet-Tophat complex, 4 to 60% slopes	5508E	7938	156473	57tj	mt669		1:24000
Libeg, extremely stony-Copenhaver-Rock outcrop complex, 2 to 60 percent slopes	3609F	4355	682549	qx7q	mt669		1:24000
Maciver very bouldery - Copenhaver stony complex , 4 to 35 percent slopes	3526E	4251	697292	rdl9	mt669		1:24000
Copenhaver-Dalys-Bridger complex, 8 to 45 percent slopes	5646E	3236	699347	rgql	mt669		1:24000
Copenhaver-Libeg complex, 15 to 60 percent slopes	7601F	2598	156777	584b	mt669		1:24000
Libeg, stony-Adel-Coppenhaver, stony complex, 15 to 60 percnet slopes, stony	8601F	1957	156764	583x	mt669		1:24000
Worock, stony -Stemple, stony , Copenhaver complex, 35 to 60 percent slopes	8604F	1559	156768	5841	mt669		1:24000
Libeg,stony - Coppenhaver,stony -Adel Complex , 4 to 15 percent slopes	8406E	1193	699356	rgqw	mt669		1:24000
Booneville very stony -Adel -Copenhaver stony complex ,moist, 15 to 60 percent slopes	3616F	1058	697430	rdqr	mt669		1:24000
Timberlin-Copenhaver complex, 35 to 60 percent slopes	694F	263	741555	swn4	mt669		1:24000
Bangtail-Copenhaver complex, 8 to 25 percent slopes	679E	19	741638	swqt	mt669		1:24000
Libeg-Monad-Copenhaver complex, 15 to 35 percent slopes	709E	68	362045	d4qw	mt670	2007	1:24000

Map of Series Extent

Approximate geographic distribution of the COPENHAVER 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).