Soil Data Explorer - MAYBERRY

Official Series Description

Lab Data Summary

Aggregate lab data for the MAYBERRY soil series. This aggregation is based on all pedons with a current taxon name of MAYBERRY, 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 MAYBERRY 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
106	40A2225	1958NE133005	Mayberry	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.0297203,-96.2005539
106	40A2138	1958NE133006	Mayberry	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.1136093,-96.1427765
106	81P0448	1981NE097003	MAYBERRY	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.2897224,-96.1533356
106	90P0413	89KS013021	Mayberry	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.8841667,-95.769722
106	90P0633	90KS013005	Mayberry	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.8847237,-95.7694473
106	90P0675	90NE155017	Mayberry	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.1722221,-96.7633362

Water Balance

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

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

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

Competing Series

Soil series competing with MAYBERRY 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 MAYBERRY 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 MAYBERRY 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 3D mountains figure.

Soil series sharing subgroup-level classification with MAYBERRY, 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. KS-2012-01-26-28 | Washington County - August 1993

   Typical pattern of soils and parent material in the Crete-Mayberry-Morrill association (Soil Survey of Washington County, Kansas; 1993).

Map Units

Map units containing MAYBERRY 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
Mayberry silty clay loam, 5 to 14 percent slopes, moderately eroded	692D2	226	409879	frhx	ia137	1987	1:15840
Mayberry clay loam, 9 to 14 percent slopes, moderately eroded	692D2	2148	410221	frvy	ia145	1975	1:20000
Mayberry clay loam, 9 to 14 percent slopes	692D	815	410220	frvx	ia145	1975	1:20000
Mayberry clay loam, 5 to 9 percent slopes, moderately eroded	692C2	491	410219	frvw	ia145	1975	1:20000
Mayberry clay loam, 3 to 7 percent slopes	7415	1869	1152173	30wyq	ks013	1994	1:24000
Mayberry clay loam, 3 to 7 percent slopes	7415	333	1457081	30wyq	ks117	1977	1:24000
Mayberry clay loam, 3 to 7 percent slopes, eroded	7416	1213	1472334	1lf2n	ks161	1970	1:24000
Mayberry clay loam, 3 to 7 percent slopes	7415	1159	1472333	30wyq	ks161	1970	1:24000
Mayberry clay loam, 3 to 7 percent slopes	7415	21227	1454894	30wyq	ks201	1988	1:24000
Mayberry silty clay loam, 6 to 11 percent slopes, eroded	7668	2465	1691479	1ts3v	ne025	1981	1:20000
Mayberry silty clay loam, 3 to 6 percent slopes, eroded	7666	13674	1691818	1tsgs	ne095	1970	1:20000
Mayberry silty clay loam, 6 to 11 percent slopes	7667	1730	1691819	1tsgt	ne095	1970	1:20000
Mayberry clay loam, 3 to 11 percent slopes	7669	4066	1691582	1ts75	ne097	1984	1:20000
Mayberry silty clay loam, 3 to 6 percent slopes, eroded	7666	9760	1691367	1ts07	ne109	1977	1:20000
Mayberry silty clay loam, 6 to 11 percent slopes, eroded	7668	2215	1691368	1ts08	ne109	1977	1:20000
Mayberry clay loam, 3 to 11 percent slopes	7669	56	2219257	2dh9y	ne109	1977	1:20000
Pawnee and Mayberry clay loams, 3 to 11 percent slopes, eroded	7495	5	2219382	2v8yl	ne127	1983	1:20000
Mayberry clay loam, 3 to 11 percent slopes	7669	4624	1691539	1ts5s	ne131	1979	1:20000
Mayberry silty clay loam, 6 to 11 percent slopes, eroded	7668	160	2219332	2dhdc	ne131	1979	1:20000
Mayberry loam, 3 to 11 percent slopes	7414	2673	1691622	1ts8g	ne133	1969	1:15840
Mayberry clay loam, 3 to 11 percent slopes	7669	128	2219407	2dhgs	ne133	1969	1:15840
Pawnee and Mayberry clay loams, 3 to 11 percent slopes, eroded	7495	6227	1691062	2v8yl	ne147	1967	1:20000
Pawnee and Mayberry clay loams, 6 to 11 percent slopes, eroded	7496	1546	1691063	2v8ym	ne147	1967	1:20000
Mayberry silty clay loam, 3 to 6 percent slopes	7665	343	1691167	1trss	ne151	1985	1:20000

Map of Series Extent

Approximate geographic distribution of the MAYBERRY 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).