Soil Data Explorer - AHMEEK

Official Series Description

Lab Data Summary

Aggregate lab data for the AHMEEK soil series. This aggregation is based on all pedons with a current taxon name of AHMEEK, 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 AHMEEK 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
93A	78P0113	77MN137001	Ahmeek	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.8877716,-92.0373993
93A	UMN2563	S1978MN1372563	Ahmeek	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.8948097,-92.3388596
93A	UMN2955	S1979MN137001 (2955)	Ahmeek	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.8236389,-92.4170532
93A	UMN2956	S1979MN137002 (2956)	Ahmeek	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.8262405,-92.4134369
93A	UMN3217	S1979MN137003 (3217)	Ahmeek	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	47.05019,-91.9086304
93A	UMN3205	S1979MN137029 (3205)	Ahmeek	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.9901695,-92.0253296
93A	UMN3216	S1979MN137030 (3216)	Ahmeek	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	47.0351791,-91.9699173
93A	UMN3206	S1979MN137031 (3206)	Ahmeek	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	47.0365982,-91.9567871
93A	UMN3390	S1980MN137002 (3390)	Ahmeek	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	47.0377388,-91.9376831
93A	UMN3391	S1980MN137004 (3391)	Ahmeek	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	47.0591011,-91.87883
93A	UMN3555	S1982MN137003 (3555)	Ahmeek	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	47.5734406,-92.4830704
93A	95P0476	S1995MN137601	AHMEEK	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.9869461,-92.0819473

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the AHMEEK 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 AHMEEK 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 AHMEEK 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 AHMEEK 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 mountains figure.

Competing Series

Soil series competing with AHMEEK 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 AHMEEK 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 AHMEEK 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 mountains figure.

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

Soil series sharing subgroup-level classification with AHMEEK, 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 AHMEEK 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
Ahmeek-Normanna-Canosia complex, 0 to 18 percent slopes	21C	50138	396345	2wcmr	mn017	1973	1:20000
Ahmeek loam, 0 to 2 percent slopes	21	12732	396344	f9f9	mn017	1973	1:20000
Ahmeek-Omega complex, 2 to 12 percent slopes	975C	9659	396382	f9gj	mn017	1973	1:20000
Ahmeek-Canosia complex, 0 to 45 percent slopes	21E	3880	396346	2v6f4	mn017	1973	1:20000
Ahmeek-Omega complex, 12 to 25 percent slopes	975E	1634	396383	f9gk	mn017	1973	1:20000
Ahmeek-Omega complex, 0 to 2 percent slopes	975	867	396381	f9gh	mn017	1973	1:20000
Ahmeek-Normanna-Mesaba, stony complex, 4 to 18 percent slopes, very rocky	A1-41D	9656	2774504	2rmzf	mn031	2013	1:24000
Ahmeek-Mesaba, stony-Giese, rubbly complex, 0 to 18 percent slopes, very rocky	A2-41D	3218	2774601	2rn04	mn031	2013	1:24000
Ahmeek-Mesaba, stony complex, 18 to 35 percent slopes, very rocky	A1-41F	1963	2774598	2rmzg	mn031	2013	1:24000
Ahmeek-Normanna-Canosia complex, 0 to 18 percent slopes	A3-31D	1737	2774524	2wcmr	mn031	2013	1:24000
Aldenlake-Ahmeek complex, 8 to 18 percent slopes	F2-41D	1071	2774646	2rn2b	mn031	2013	1:24000
Ahmeek-Rock outcrop-Udifluvents, frequently flooded complex, 1 to 70 percent slopes	E1-14F	765	2774506	2rn0y	mn031	2013	1:24000
Ahmeek-Udifluvents, frequently flooded-Rock outcrop complex, 1 to 18 percent slopes	E1-9D	152	2774479	2rn1d	mn031	2013	1:24000
Ahmeek-Normanna-Cathro, depressional complex 0 to 25 percent slopes, pitted	A3-42D	73	2943740	2rmzv	mn031	2013	1:24000
Ahmeek-Canosia complex, 0 to 45 percent slopes	A3-32F	40	2774623	2v6f4	mn031	2013	1:24000
Ahmeek-Rock outcrop-Fluvaquents, frequently flooded complex 0 to 50 percent slopes	E1-10F	38	2774607	2rn0x	mn031	2013	1:24000
Ahmeek-Normanna-Mesaba, stony complex, 4 to 18 percent slopes, very rocky	A1-41D	20122	2742117	2rmzf	mn075	2013	1:24000
Ahmeek-Normanna-Canosia complex, 0 to 18 percent slopes	A3-31D	17500	2742126	2yz88	mn075	2013	1:24000
Aldenlake-Ahmeek complex, 8 to 18 percent slopes	F2-41D	16842	2742225	2yz82	mn075	2013	1:24000
Ahmeek-Normanna-Cathro, depressional complex 0 to 25 percent slopes, pitted	A3-42D	7661	2742129	2rmzv	mn075	2013	1:24000
Ahmeek-Aldenlake complex, 18 to 45 percent slopes	F2-42F	4986	2742226	2rn2c	mn075	2013	1:24000
Ahmeek-Mesaba, stony complex, 18 to 35 percent slopes, very rocky	A1-41F	3723	2742118	2rmzg	mn075	2013	1:24000
Ahmeek-Mesaba, stony-Giese, rubbly complex, 0 to 18 percent slopes, very rocky	A2-41D	3365	2742138	2rn04	mn075	2013	1:24000
Ahmeek-Canosia complex, 0 to 45 percent slopes	A3-32F	1581	2742127	2v6f4	mn075	2013	1:24000
Ahmeek-Udifluvents, frequently flooded-Rock outcrop complex, 1 to 18 percent slopes	E1-9D	869	2742182	2rn1d	mn075	2013	1:24000
Ahmeek-Rock outcrop-Udifluvents, frequently flooded complex, 1 to 70 percent slopes	E1-14F	863	2742179	2rn0y	mn075	2013	1:24000
Ahmeek-Rock outcrop-Fluvaquents, frequently flooded complex 0 to 50 percent slopes	E1-10F	811	2742176	2rn0x	mn075	2013	1:24000
Ahmeek-Canosia complex, 0 to 25 percent slopes, very rocky	A3-50D	516	2742131	2rmzw	mn075	2013	1:24000
Ahmeek-Normanna-Canosia complex, 0 to 18 percent slopes	F138D	27215	449575	2wcmr	mn615	2007	1:24000
Ahmeek-Normanna-Cathro, depressional, complex, pitted, 0 to 25 percent slopes	F141D	8986	449578	h2tj	mn615	2007	1:24000
Ahmeek-Canosia-Rock outcrop complex, 0 to 25 percent slopes	F147D	7483	764971	tp0h	mn615	2007	1:24000
Ahmeek-Canosia complex, 0 to 45 percent slopes	F139F	4216	449576	2v6f4	mn615	2007	1:24000
Aldenlake-Ahmeek complex, 8 to 18 percent slopes	F144D	2585	449581	h2tm	mn615	2007	1:24000
Rock outcrop-Ahmeek, bedrock substratum-Barto complex, 4 to 18 percent slopes	F156D	2135	1145761	17g81	mn615	2007	1:24000
Ahmeek-Rock outcrop-Fluvaquents, frequently flooded, complex, 0 to 50 percent slopes	F148F	1404	764970	tp0g	mn615	2007	1:24000
Urban land-Ahmeek-Normanna complex, 3 to 18 percent slopes	F159D	1183	1424899	1jtqh	mn615	2007	1:24000
Ahmeek-Aldenlake complex, 18 to 45 percent slopes	F145F	824	449582	h2tn	mn615	2007	1:24000
Ahmeek-Normanna-Canosia complex, 0 to 18 percent slopes	F138D	6508	1715852	2wcmr	mn619	2009	1:24000
Aldenlake-Ahmeek complex, 8 to 18 percent slopes	F144D	4926	1715858	1vlh8	mn619	2009	1:24000
Ahmeek-Canosia complex, 0 to 45 percent slopes	F139F	2369	1715853	2v6f4	mn619	2009	1:24000
Ahmeek-Aldenlake complex, 18 to 45 percent slopes	F145F	2154	1715859	1vlh9	mn619	2009	1:24000
Ahmeek-Normanna-Cathro, depressional, complex, pitted, 0 to 25 percent slopes	F141D	1983	1715855	1vlh5	mn619	2009	1:24000
Ahmeek-Rock outcrop-Fluvaquents, frequently flooded, complex, 0 to 50 percent slopes	F148F	27	1715862	1vlhd	mn619	2009	1:24000

Map of Series Extent

Approximate geographic distribution of the AHMEEK 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).