Soil Data Explorer - JOPLIN

Official Series Description

Lab Data Summary

Aggregate lab data for the JOPLIN soil series. This aggregation is based on all pedons with a current taxon name of JOPLIN, 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 JOPLIN 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
52	92P0841	92MT041006	Joplin	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	48.4933319,-109.7994461
52	40A3345	S1962MT101001	Joplin	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	48.7396278,-111.593956

Water Balance

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

Competing Series

Soil series competing with JOPLIN 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 JOPLIN 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 JOPLIN 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).

Soil series sharing subgroup-level classification with JOPLIN, 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

No block diagrams are available.

Map Units

Map units containing JOPLIN 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
Telstad-Joplin loams, 4 to 8 percent slopes	731C	1022	1596508	1ql98	mt021	1971	1:24000
Hillon-Joplin loams, 4 to 15 percent slopes	931D	382	339748	2t078	mt033	2002	1:24000
Joplin-Hillon loams, 2 to 8 percent slopes	63C	76	339746	2t07b	mt033	2002	1:24000
Telstad-Joplin loams, 2 to 8 percent slopes	93C	49	339747	2v55f	mt033	2002	1:24000
Telstad-Joplin loams, 0 to 4 percent slopes	503B	434238	343969	2v55g	mt041	1994	1:24000
Joplin-Hillon loams, 2 to 8 percent slopes	421C	133630	343952	2t07b	mt041	1994	1:24000
Hillon-Joplin loams, 4 to 15 percent slopes	224D	22250	343878	2t078	mt041	1994	1:24000
Hillon-Joplin loams, 8 to 25 percent slopes	22E	12492	343880	2t079	mt041	1994	1:24000
Telstad-Joplin loams, 2 to 8 percent slopes	503C	8706	343970	2v55f	mt041	1994	1:24000
Joplin-Hillon loams, 2 to 8 percent slopes	421C	126083	344204	2t07b	mt051	1992	1:24000
Telstad-Joplin loams, 0 to 4 percent slopes	503B	113248	344217	2v55g	mt051	1992	1:24000
Hillon-Joplin loams, 8 to 25 percent slopes	224E	25018	344156	2t079	mt051	1992	1:24000
Joplin-Hillon loams, 0 to 4 percent slopes	224B	16944	344155	2vyr9	mt051	1992	1:24000
Telstad-Joplin loams, 2 to 8 percent slopes	503C	7267	344218	2v55f	mt051	1992	1:24000
Marvan-Joplin, complex, 0 to 4 percent slopes	304B	1364	344171	ck49	mt051	1992	1:24000
Joplin-Hillon loams, 2 to 8 percent slopes	134	16774	344332	2t07b	mt055	1981	1:24000
Hillon-Joplin loams, 4 to 15 percent slopes	92	7788	344460	2t078	mt055	1981	1:24000
Telstad-Joplin loams, 2 to 8 percent slopes	133	4923	344331	2v55f	mt055	1981	1:24000
Joplin-Hillon loams, 0 to 4 percent slopes	427B	99711	345172	2vyr9	mt101	1992	1:24000
Telstad-Joplin loams, 0 to 4 percent slopes	504B	98878	345206	2v55g	mt101	1992	1:24000
Joplin-Hillon loams, 2 to 8 percent slopes	421C	91357	345164	2t07b	mt101	1992	1:24000
Hillon-Joplin loams, 4 to 15 percent slopes	421D	23908	345165	2t078	mt101	1992	1:24000
Telstad-Joplin loams, 2 to 8 percent slopes	504C	14850	345207	2v55f	mt101	1992	1:24000
Hillon-Joplin loams, 8 to 25 percent slopes	224E	11507	345102	2t079	mt101	1992	1:24000
Joplin-Hillon gravelly loams, 3 to 8 percent slopes	424C	3901	345168	cl5g	mt101	1992	1:24000
Telstad-Joplin loams, 2 to 8 percent slopes	65	69886	345584	2v55f	mt105	1976	1:24000
Hillon-Joplin loams, 4 to 15 percent slopes	30	10478	345546	2t078	mt105	1976	1:24000
Telstad-Joplin loams, 4 to 8 percent slopes	731C	166	1607271	1qyhg	mt109	1956	1:31680
Joplin-Hillon loams, 8 to 15 percent slopes	491D	82	1607264	1qyh7	mt109	1956	1:31680
Joplin-Hillon loams, 4 to 8 percent slopes	491C	9	1607265	1qyh8	mt109	1956	1:31680
Hillon-Joplin loams, 4 to 15 percent slopes	Sm	6818	146935	2t078	mt600	1969	1:24000
Telstad-Joplin loams, 0 to 4 percent slopes	120	50064	346269	2v55g	mt608	1976	1:24000
Telstad-Joplin loams, 2 to 8 percent slopes	121	40282	346270	2v55f	mt608	1976	1:24000
Telstad-Joplin loams, 0 to 4 percent slopes	503B	186476	346803	2v55g	mt615	1992	1:24000
Telstad-Joplin loams, 2 to 8 percent slopes	503C	67175	346804	2v55f	mt615	1992	1:24000
Joplin-Hillon loams, 2 to 8 percent slopes	421C	30789	346767	2t07b	mt615	1992	1:24000
Hillon-Joplin loams, 8 to 25 percent slopes	224E	25904	346638	2t079	mt615	1992	1:24000
Telstad-Joplin loams, 2 to 8 percent slopes	503C	61096	347737	2v55f	mt641	1994	1:24000
Hillon-Joplin loams, 8 to 25 percent slopes	220E	35137	347634	2t079	mt641	1994	1:24000
Joplin-Hillon loams, 2 to 8 percent slopes	421C	25098	347708	2t07b	mt641	1994	1:24000
Hillon-Joplin loams, 4 to 15 percent slopes	224D	11933	347640	2t078	mt641	1994	1:24000
Telstad-Joplin association, 0 to 15 percent slopes	1503D	9391	347605	cnq2	mt641	1994	1:24000
Joplin-Hillon gravelly loams, 2 to 8 percent slopes	426C	7783	347715	cntm	mt641	1994	1:24000
Telstad-Joplin loams, 0 to 4 percent slopes	165B	23277	348381	2v55g	mt657	1990	1:24000
Telstad-Joplin loams, 2 to 8 percent slopes	162C	9839	348376	2v55f	mt657	1990	1:24000
Chinook-Joplin complex, 2 to 8 percent slopes	334C	2041	348577	cpqf	mt657	1990	1:24000
Joplin-Hillon loams, 2 to 8 percent slopes	51	15806	348257	2t07b	mt661	1982	1:24000
Hillon-Joplin loams, 4 to 15 percent slopes	30	2386	348234	2t078	mt661	1982	1:24000
Telstad-Joplin loams, 2 to 8 percent slopes	50	2058	348256	2v55f	mt661	1982	1:24000
Geohrock-like-Pachel-Joplin complex, 8 to 35 percent slopes	9403		3136887	2yppq	wy629		1:24000

Map of Series Extent

Approximate geographic distribution of the JOPLIN 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).