Soil Data Explorer - ATTEWAN

Official Series Description

Lab Data Summary

Aggregate lab data for the ATTEWAN soil series. This aggregation is based on all pedons with a current taxon name of ATTEWAN, 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 ATTEWAN were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.

Water Balance

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

Competing Series

Soil series competing with ATTEWAN 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 ATTEWAN 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 ATTEWAN 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 hills 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 ATTEWAN, 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 ATTEWAN 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
Attewan loams, 2 to 4 percent slopes	Tw	13966	342054	cgy0	mt021	1971	1:24000
Attewan loam, 2 to 4 percent slopes	Tt	13440	342051	cgxx	mt021	1971	1:24000
Attewan loam, 0 to 2 percent slopes	Ts	12176	342050	cgxw	mt021	1971	1:24000
Attewan complex, 4 to 15 percent slopes	Bm	10091	341996	cgw4	mt021	1971	1:24000
Attewan loams, 4 to 8 percent slopes	Ty	9759	342055	cgy1	mt021	1971	1:24000
Attewan loams, 0 to 2 percent slopes	Tv	8050	342053	cgxz	mt021	1971	1:24000
Attewan fine sandy loam, 1 to 4 percent slopes	Tr	5466	342049	cgxv	mt021	1971	1:24000
Attewan loam, 4 to 8 percent slopes	Tu	2946	342052	cgxy	mt021	1971	1:24000
Attewan-Tinsley complex, 2 to 8 percent slopes	272C	2988	343890	cjv7	mt041	1994	1:24000
Attewan loam, 0 to 4 percent slopes	27B	1385	343891	cjv8	mt041	1994	1:24000
Attewan loam, 0 to 4 percent slopes	27B	1114	344165	ck43	mt051	1992	1:24000
Attewan-Tinsley complex, 2 to 8 percent slopes	272C	258	344164	ck42	mt051	1992	1:24000
Crago-Musselshell-Attewan complex, 1 to 4 percent slopes	56A	13763	344599	cgkl	mt065	1996	1:24000
Attewan-Niart loams, 0 to 4 percent slopes	57C	3828	344602	ckl6	mt065	1996	1:24000
Eapa-Attewan loams, 0 to 2 percent slopes	152A	3124	344485	cghw	mt065	1996	1:24000
Attewan loam, 1 to 4 percent slopes	57A	2522	344600	cgkm	mt065	1996	1:24000
Crago-Musselshell-Attewan complex, 1 to 4 percent slopes, fan	356A	1567	1713818	1vfzr	mt065	1996	1:24000
Attewan cobbly loam, 0 to 4 percent slopes	57B	46	344601	ckl5	mt065	1996	1:24000
Attewan loam, 0 to 4 percent slopes	6	7675	344729	ckq9	mt069	1989	1:24000
Crago-Musselshell-Attewan complex, 0 to 2 percent slopes	28	2351	344694	ckp5	mt069	1989	1:24000
Evanston-Attewan loams, 0 to 2 percent slopes	37	1140	344704	ckph	mt069	1989	1:24000
Attewan loam, 0 to 4 percent slopes	27B	1921	345113	cl3p	mt101	1992	1:24000
Attewan sandy loam, 0 to 4 percent slopes	272B	239	345112	cl3n	mt101	1992	1:24000
Attewan loam, 0 to 4 percent slopes	3	6015	345545	clkm	mt105	1976	1:24000
Attewan sandy loam, 0 to 4 percent slopes	Ak	7839	146760	4xq6	mt600	1969	1:24000
Attewan sandy loam, 4 to 8 percent slopes	Am	3745	146761	4xq7	mt600	1969	1:24000
Attewan loam, 0 to 4 percent slopes	An	1717	146762	4xq8	mt600	1969	1:24000
Attewan loam, 4 to 8 percent slopes	Ao	1247	146763	4xq9	mt600	1969	1:24000
Attewan-Nippt complex, 0 to 2 percent slopes	193A	1372	148275	4z92	mt604	2001	1:24000
Attawan-Varney complex, 1 to 4 percent slopes	193B	30	2450839	2n89b	mt604	2001	1:24000
Attewan cobbly loam, cool, 2 to 8 percent slopes	12C	9	609114	4xbb	mt604	2001	1:24000
Attewan-Beaverell complex, 0 to 4 percent slopes	4	21666	346457	cmj1	mt608	1976	1:24000
Attewan loam, 0 to 4 percent slopes	3	19282	346415	cmgp	mt608	1976	1:24000
Attewan-Wabek complex, 0 to 4 percent slopes	5	3854	346484	cmjx	mt608	1976	1:24000
Attewan-Nippt complex, 0 to 2 percent slopes	193A	1088	2597676	4z92	mt612	2011	1:24000
Attewan-Varney complex, 1 to 4 percent slopes	193B	803	2420110	2m7b2	mt612	2011	1:24000
Attewan-Tinsley complex, 2 to 8 percent slopes	272C	5588	346657	cmqh	mt615	1992	1:24000
Attewan loam, 0 to 4 percent slopes	27B	3489	346658	cmqj	mt615	1992	1:24000
Attewan clay loam, 0 to 4 percent slopes	33B	1618	155405	56q2	mt622	1997	1:24000
Attewan loam, 0 to 4 percent slopes	57B	3867	1912423	22612	mt624	2021	1:24000
Attewan-Niart complex, 0 to 4 percent slopes	486B	2882	1912425	22614	mt624	2021	1:24000
Crago-Musselshell-Attewan complex, 0 to 2 percent slopes	496A	1789	1903779	21x17	mt624	2021	1:24000
Eapa-Attewan loams, 0 to 2 percent slopes	152A	1428	2513996	cghw	mt624	2021	1:24000
Crago-Attewan cobbly loams, 2 to 8 percent slopes	95C	495	347537	cnmw	mt624	2021	1:24000
Crago-Musselshell-Attewan complex, 1 to 4 percent slopes, fan	356A	23	3176862	1vfzr	mt624	2021	1:24000
Attewan-Nippt complex, 0 to 2 percent slopes	3513A	33	151661	52t9	mt627	1998	1:24000
Attewan loam, 0 to 2 percent slopes	413A	2676	147811	4yt3	mt630	1991	1:24000
Attewan-Nippt complex, 0 to 2 percent slopes	513A	2333	147839	4yv0	mt630	1991	1:24000
Nippt-Attewan-Beaverell complex, 0 to 4 percent slopes	306A	2078	147782	4ys5	mt630	1991	1:24000
Nippt-Attewan complex, 0 to 2 percent slopes	506A	1228	147836	4ytx	mt630	1991	1:24000
Yamacall-Attewan loams, 0 to 2 percent slopes	569A	398	147859	4yvn	mt630	1991	1:24000
Attewan cobbly loam, cool, 2 to 8 percent slopes	12	18824	146392	4xbb	mt636	1983	1:24000
Attewan loam, cool, 2 to 8 percent slopes	11	4464	146381	4x9z	mt636	1983	1:24000
Attewan loam, cool, 0 to 2 percent slopes	10	3953	146370	4x9m	mt636	1983	1:24000
Attewan very stony loam, cool, 2 to 8 percent slopes	13	3647	146403	4xbp	mt636	1983	1:24000
Attewan loam, 0 to 4 percent slopes	448B	1200	150015	5136	mt639	2000	1:24000
Sieben-Attewan gravelly loams, 0 to 4 percent slopes	443B	270	150009	5130	mt639	2000	1:24000
Attewan-Beaverell complex, 0 to 8 percent slopes	110C	10629	347576	cnp4	mt641	1994	1:24000
Attewan loam, 0 to 4 percent slopes	11	2765	348140	cp8b	mt655	1975	1:24000
Attewan loam, seeped, 0 to 4 percent slopes	12	1846	348141	cp8c	mt655	1975	1:24000
Attewan-Beaverell gravelly loams, 0 to 4 percent slopes	13	1366	348142	cp8d	mt655	1975	1:24000
Attewan-Wabek complex, 0 to 8 percent slopes	216C	6205	348444	cpl4	mt657	1990	1:24000
Attewan fine sandy loam, 0 to 4 percent slopes	116B	588	348306	cpfp	mt657	1990	1:24000
Crago-Musselshell-Attewan complex, 1 to 4 percent slopes, fan	356A	15848	1711533	1vfzr	mt666	2008	1:24000
Crago-Musselshell-Attewan complex, 1 to 4 percent slopes	56A	3652	341700	cgkl	mt666	2008	1:24000
Eapa-Attewan loams, 0 to 2 percent slopes	152A	2146	341647	cghw	mt666	2008	1:24000
Eapa-Attewan loams, 0 to 2 percent slopes, fan	352A	1852	1711527	1vfzk	mt666	2008	1:24000
Attewan loam, 1 to 4 percent slopes	57A	458	341701	cgkm	mt666	2008	1:24000
Beaverell, stony-Attewan complex, 0 to 4 percent slopes	321B	4330	156905	588g	mt669		1:24000
Beaverell-Attewan complex, 0 to 4 percent slopes	721A	3224	156949	589w	mt669		1:24000
Beaverell, extremely stony-Attewan-Beaverell, very stony complex, 0 to 8 percent slopes	3402C	2416	156701	581w	mt669		1:24000
Attewan-Vendome, stony complex, 0 to 4 percent slopes	428B	589	156916	588t	mt669		1:24000
Attewan loam, 2 to 6 percent slopes	AwB	5252	355717	cy4r	sd063	1984	1:24000
Nihill variant-Attewan complex, 4 to 40 percent slopes	NaD	3889	355771	cy6h	sd063	1984	1:24000
Nihill-Attewan complex, 4 to 20 percent slopes	NaD	4880	355453	cxw7	sd601	1983	1:24000
Attewan loam, 1 to 6 percent slopes -- Draft	20AB		152480	53nq	wy629		1:24000

Map of Series Extent

Approximate geographic distribution of the ATTEWAN 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).