Soil Data Explorer - MCCONNEL

Official Series Description

Lab Data Summary

Aggregate lab data for the MCCONNEL soil series. This aggregation is based on all pedons with a current taxon name of MCCONNEL, 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 MCCONNEL 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
24	86P0762	86NV013300	McConnel	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.6282272,-117.8070831

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MCCONNEL 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 MCCONNEL series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-06) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the MCCONNEL 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 2023-10-09).

Geomorphic description summaries for the MCCONNEL 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 2023-10-04).

There are insufficient data to create the 3D mountains figure.

Competing Series

Soil series competing with MCCONNEL share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-06) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the MCCONNEL 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 2023-10-09).

Geomorphic description summaries for the MCCONNEL 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 2023-10-04).

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D mountains figure.

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

Soil series sharing subgroup-level classification with MCCONNEL, 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 2023-10-02).

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

1. OR-2010-09-29-05 | Harney County Area - 2006

   Soil and landscape relationship in Pueblo Valley (Soil Survey of Harney County Area, Oregon; 2006).

2. OR-2010-09-29-09 | Lake County, Southern Part - 1999

   Soil-landscape relationships in Warren Valley. Icene and Mesman soils on basin floor, McConnel soils on terraces, Pait soils on fans, Riddleranch soils on escarpments, and Hager soils on tablelands (Soil Survey of Lake County, Oregon, Southern Part; 1999).

3. OR-2012-05-10-18 | Lake County, Southern Part - 1999

   Soil-landscape relationships in Warner Valley. Icene and Mesman soils on basin floor, McConnel soils on terraces, Pait soils on fans, Riddleranch soils on escarpments, and Hager soils on tablelands (Soil Survey of Lake County Oregon, Southern Part; 1999).

4. OR-2012-05-10-28 | Harney County Area - 2006

   Soil and landscape relationship in Pueblo Valley (Soil Survey of Harney County Area, Oregon; 2006).

Map Units

Map units containing MCCONNEL 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
Cewat-McConnel-Toulon association, 2 to 15 percent slopes	149	7053	487402	jc5n	ca608	2000	1:24000
McConnel-Mottsville complex, 2 to 9 percent slopes	283	2481	487594	jccv	ca608	2000	1:24000
McConnel gravelly fine sandy loam	Mf	4529	476112	hzfg	nv612	1968	1:24000
McConnel-Blackhawk complex	Mh	2915	476113	hzfh	nv612	1968	1:24000
McConnel-Ocala complex	Mo	424	476114	hzfj	nv612	1968	1:24000
McConnel very stony sandy loam, 2 to 8 percent slopes	1120	100	474486	hxr0	nv759	1995	1:24000
McConnel very stony sandy loam, 2 to 8 percent slopes	580	16381	474766	hy11	nv760	1994	1:24000
McConnel very gravelly fine sandy loam, 0 to 2 percent slopes 1/	581	2521	474767	hy12	nv760	1994	1:24000
McConnel-Rasille-Wholan association	633	42315	479287	j2qw	nv768	1985	1:63360
McConnel-Orovada-Misad association	632	7285	479286	j2qv	nv768	1985	1:63360
McConnel-Wholan association	638	4220	479291	j2r0	nv768	1985	1:63360
McConnel-Rasille association	635	3620	479288	j2qx	nv768	1985	1:63360
Orovada-McConnel association	704	2965	479301	j2rb	nv768	1985	1:63360
Tulase-Bubus-McConnel association	1092	2900	479034	2v43m	nv768	1985	1:63360
McConnel-Defler-Rasille association	636	2325	479289	j2qy	nv768	1985	1:63360
McConnel-Orovada association	637	2045	479290	j2qz	nv768	1985	1:63360
McConnel loam, 0 to 2 percent slopes	330	2143	475265	hyk4	nv769	1986	1:24000
McConnel gravelly fine sandy loam, 4 to 8 percent slopes	331	1428	475266	hyk5	nv769	1986	1:24000
Beoska-Oxcorel-McConnel association	177	5405	479504	j2yw	nv775	1985	1:24000
McConnel-Tulase association	631	4220	479696	j352	nv775	1985	1:24000
Tulase-Bubus-McConnel association	1092	1785	479409	2v43m	nv775	1985	1:24000
Tulase-Bubus-McConnel association	1203	12757	479769	2v43m	nv776	1983	1:63360
Enko-Davey-McConnel association	822	7233	479894	j3cg	nv776	1983	1:63360
Chiara-Dacker-McConnel association	185	22292	475615	hyxf	nv777	1993	1:24000
Hunnton-Flue-McConnel association	1172	17110	475429	hyqf	nv777	1993	1:24000
Snapp-McConnel-Adelaide association	756	16844	475914	hz72	nv777	1993	1:24000
McConnel-Pumper-Whirlo complex, 2 to 8 percent slopes	338	15675	475691	hyzw	nv777	1993	1:24000
Connel-McConnel complex, rarely flooded, 0 to 2 percent slopes 1 /	255	13912	475652	hyym	nv777	1993	1:24000
McConnel gravelly fine sandy loam, 2 to 8 percent slopes	331	13722	475685	hyzp	nv777	1993	1:24000
Connel-McConnel complex, 0 to 2 percent slopes 1/	253	8887	475650	hyyk	nv777	1993	1:24000
McConnel very gravelly fine sandy loam, 0 to 2 percent slopes 1/	335	5471	475689	hyzt	nv777	1993	1:24000
Zevadez-McConnel association	963	5170	476003	hz9y	nv777	1993	1:24000
McConnel fine sandy loam, 0 to 2 percent slopes 1/	330	4960	475684	hyzn	nv777	1993	1:24000
McConnel-Shabliss association	333	2846	475687	hyzr	nv777	1993	1:24000
Chiara-McConnel association	184	2349	475614	hyxd	nv777	1993	1:24000
Pyrat-McConnel association	1494	9136	480280	j3rx	nv780	1990	1:24000
Yody-Blimo-McConnel association	570	4763	480530	j40z	nv780	1990	1:24000
McConnel cobbly sandy loam, 3 to 8 percent slopes	192	25435	490570	jggv	or628	1997	1:24000
Calderwood-McConnel complex, 0 to 20 percent slopes	53	6000	490887	jgt2	or628	1997	1:24000
Calderwood-McConnel complex, 0 to 20 percent slopes	238	20200	1689748	1tqb0	or635	2006	1:24000
Enko-McConnel complex, 0 to 5 percent slopes	294	13696	1689803	1tqcs	or635	2006	1:24000
McConnel-Poorjug complex, 1 to 15 percent slopes	439	7917	1689943	1tqj9	or635	2006	1:24000
McConnel gravelly sandy loam, sodic substratum, 0 to 5 percent slopes	435	4336	1689939	1tqj5	or635	2006	1:24000
McConnel very gravelly sandy loam, 0 to 2 percent slopes	436	3550	1689940	1tqj6	or635	2006	1:24000
Mesman-McConnel-Kewake complex, 2 to 8 percent slopes	447	2260	1689951	1tqjk	or635	2006	1:24000
Locolake-McConnel complex, 3 to 10 percent slopes	419	2149	1689924	1tqhp	or635	2006	1:24000
McConnel very gravelly sandy loam, 2 to 15 percent slopes	437	1875	1689941	1tqj7	or635	2006	1:24000
McConnel-Turpin complex, 2 to 15 percent slopes	440	1351	1689944	1tqjb	or635	2006	1:24000
McConnel-Davey complex, 15 to 45 percent slopes	438	1060	1689942	1tqj8	or635	2006	1:24000
McConnel cobbly sandy loam, 3 to 8 percent slopes	434	486	1689938	1tqj4	or635	2006	1:24000
McConnel very gravelly sandy loam, 2 to 15 percent slopes	153C	11210	488968	jdt5	or636	1991	1:24000
McConnel very gravelly sandy loam, 0 to 2 percent slopes	153A	6140	488967	jdt4	or636	1991	1:24000
McConnel gravelly sandy loam, sodic substratum, 0 to 5 percent slopes	156B	1312	488972	jdt9	or636	1991	1:24000
McConnel-Icene complex, 0 to 15 percent slopes	157C	1121	488973	jdtb	or636	1991	1:24000
McConnel very gravelly sandy loam, cold, 2 to 15 percent slopes	155C	614	488971	jdt8	or636	1991	1:24000
McConnel extremely stony loam, 5 to 15 percent slopes	154C	519	488969	jdt6	or636	1991	1:24000
McConnel association, 30 to 50 percent slopes	158F	448	488974	jdtc	or636	1991	1:24000
McConnel cobbly sandy loam, 3 to 8 percent slopes	450B	93	1720982	1vrtk	or636	1991	1:24000
McConnel cobbly sandy loam, 3 to 8 percent slopes	OR0192	906	2494086	2pr0n	or644	2021	1:24000

Map of Series Extent

Approximate geographic distribution of the MCCONNEL 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 2023-10-04).