Soil Data Explorer - ZAHL

Official Series Description

Lab Data Summary

Aggregate lab data for the ZAHL soil series. This aggregation is based on all pedons with a current taxon name of ZAHL, 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 ZAHL 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
53A	89P0538	89ND023071	Zahl	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	48.9808333,-104.0344444
53A	89P0539	89ND023072	Zahl	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	48.9116667,-104.0369444
53A	89P0540	89ND023073	Zahl	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	48.8538889,-104.0419444
53A	89P0541	89ND023074	Zahl	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	48.8144455,-103.9872208
53A	89P0542	89ND023075	Zahl	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	48.765,-104.015
53A	89P0543	89ND023076	Zahl	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	48.7411111,-104.0083333
53A	89P0544	89ND023077	Zahl	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	48.6936111,-104.0413889
53A	89P0545	89ND023078	Zahl	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	48.6758333,-104.0280556
53B	87P0564	87ND083430	Zahl	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	47.4052773,-100.4266663
53B	00P0600	S1999ND055002	Zahl	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	47.6890373,-100.8628693
n/a	87P0532	87MT085001	Zahl	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	87P0533	87MT085001A	Zahl	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	87P0534	87MT085001B	Zahl	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	87P0535	87MT085001C	Zahl	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ZAHL 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 ZAHL 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 ZAHL 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 ZAHL 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 ZAHL 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 ZAHL 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 ZAHL 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 flats position figure.

Soil series sharing subgroup-level classification with ZAHL, 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. ND-2010-09-27-07 | McKenzie County - 2006

   Typical pattern of soils and underlying material in the Williams-Temvik-Wilton-Zahl association (Soil Survey of McKenzie County, North Dakota; 2006).

2. ND-2010-09-27-11 | Williams County - 2002

   Typical pattern of soils and underlying material in the Williams-Zahl association (Soil Survey of Williams County, North Dakota; 2002).

3. ND-2012-02-07-24 | Dickey County - May 1993

   Typical pattern of soils and parent material in the Williams-Bowbells-Zahl association (Soil Survey of Dickey County, North Dakota; May 1993).

4. ND-2012-02-07-25 | Divide County - 2002

   Typical pattern of soils and underlying material in the Williams-Zahl association (Soil Survey of Divide County, North Dakota; 2002).

5. ND-2012-02-07-26 | Divide County - 2002

   Typical pattern of soils and underlying material in the Wabek-Appam-Lehr association (Soil Survey of Divide County, North Dakota; 2002).

6. ND-2012-02-07-27 | Divide County - 2002

   Typical pattern of soils and underlying material in the Williams-Niobell-Noonan association (Soil Survey of Divide County, North Dakota; 2002).

7. ND-2012-02-07-29 | Divide County - 2002

   Typical pattern of soils and underlying material in the Zahl-Williams association (Soil Survey of Divide County, North Dakota; 2002).

8. ND-2012-02-07-33 | Dunn County - April 1982

   Typical pattern of soils and underlying material in the Williams-Amor-Arnegard association (Soil Survey of Dunn County, North Dakota; April 1982).

9. ND-2012-02-08-16 | Kidder County - March 1988

   Typical pattern of soils and parent material in the Williams-Bowbells association (Soil Survey of Kidder County, North Dakota; March 1988).

10. ND-2012-02-08-24 | McIntosh County - 2001

    Typical pattern of soils and underlying material in the Williams-Zahl association (Soil Survey of McIntosh County, North Dakota; 2001).

11. ND-2012-02-08-27 | McIntosh County - 2001

    Typical pattern of soils and underlying material in the Wabek-Appam-Lehr association (Soil Survey of McIntosh County, North Dakota; 2001).

12. ND-2012-02-08-31 | Mountrail County - June 1991

    Typical pattern of soils and parent material in the Williams-Hamerly-Bowbells association (Soil Survey of Mountrail County, North Dakota; June 1991).

13. ND-2012-02-08-32 | Mountrail County - June 1991

    Typical pattern of soils and parent material in the Zahl-Williams association (Soil Survey of Mountrail County, North Dakota; June 1991).

14. ND-2012-02-08-33 | Mountrail County - June 1991

    Typical pattern of soils and parent material in the Manning-Livona-Lihen association (Soil Survey of Mountrail County, North Dakota; June 1991).

15. ND-2012-02-08-35 | Mountrail County - June 1991

    Typical pattern of soils and parent material in the Williams-Zahl association (Soil Survey of Mountrail County, North Dakota; June 1991).

16. ND-2012-02-08-36 | Mountrail County - June 1991

    Typical pattern of soils and parent material in the Farnuf-Makoti association (Soil Survey of Mountrail County, North Dakota; June 1991).

17. ND-2012-02-08-50 | Sheridan County - November 1994

    Typical pattern of soils and parent material in the Williams-Bowbells-Zahl association (Soil Survey of Sheridan County, North Dakota; November 1994).

18. ND-2012-02-08-59 | Ward County - 1974

    Relationship of soils to topography and parent material (Soil Survey of Ward County, North Dakota; 1974).

19. ND-2012-02-14-01 | Ward County - 1974

    Relationship of soils to topography and parent material (Soil Survey of Ward County, North Dakota; 1974).

20. SD-2010-11-01-14 | Spink County - 2009

    Pattern of soils and underlying materials in the Nahon-Aberdeen-Exline and Max-Arnegard-Zahl associations (Soil Survey of Spink County, South Dakota; 2009).

21. SD-2012-03-15-34 | Faulk County - January 1984

    Pattern of soils and parent material in the Max-Niobell-Noonan association (Soil Survey of Faulk County, SD; 1984).

22. SD-2012-03-15-44 | Hand County - April 1963

    A cross section typical in both the south-central and northwestern parts of Hand County (Soil Survey of Hand County, SD; 1963).

23. SD-2012-03-15-45 | Hand County - April 1963

    A typical cross section of the southwestern part of the county (Soil Survey of Hand County, SD; 1963).

24. SD-2012-03-15-46 | Hand County - April 1963

    A cross section typical of an area next to the Ree Hills or the Wessington Hills (Soil Survey of Hand County, SD; 1963).

Map Units

Map units containing ZAHL 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
Zahill-Zahl clay loams, 15 to 60 percent slopes	72F	36866	344044	2vyt5	mt041	1994	1:24000
Zahill-Zahl clay loams, 15 to 60 percent slopes	72F	4319	344258	2vyt5	mt051	1992	1:24000
Zahill-Zahl clay loams, 15 to 60 percent slopes	721F	15934	345257	2vyt5	mt101	1992	1:24000
Zahill-Zahl complex, 15 to 25 percent slopes	721E	5744	345256	cl89	mt101	1992	1:24000
Zahl loam, 8 to 30 percent slopes	Za	2133	345669	clpm	mt109	1956	1:31680
Williams-Zahl complex, hilly	WS	16841	146965	4xxt	mt600	1969	1:24000
Scobey-Zahl complex, hilly	SO	13815	146919	4xwb	mt600	1969	1:24000
Zahl complex, hilly	ZA	5376	146974	4xy3	mt600	1969	1:24000
Williams-Zahl complex, steep	WT	3764	146966	4xxv	mt600	1969	1:24000
Williams-Zahl complex, undulating	Wr	2900	146972	4xy1	mt600	1969	1:24000
Zahill-Zahl clay loams, 15 to 60 percent slopes	150	30074	346329	2vyt5	mt608	1976	1:24000
Zahill-Zahl clay loams, 15 to 60 percent slopes	72F	24601	346901	2vyt5	mt615	1992	1:24000
Zahl-Max-Parnell complex, 0 to 35 percent slopes	C165F	72437	2564058	2q3b9	nd013	1991	1:24000
Zahl-Williams loams, 9 to 15 percent slopes	C135D	55278	2596889	2q52k	nd013	1991	1:24000
Zahl-Williams-Zahill complex, 6 to 9 percent slopes	C135C	50870	2564088	2w42f	nd013	1991	1:24000
Williams-Zahl loams, 3 to 6 percent slopes	C132B	31486	2564059	2w42d	nd013	1991	1:24000
Williams-Zahl loams, 3 to 6 percent slopes	2031	18240	341103	cfyb	nd013	1991	1:24000
Williams-Zahl complex, 3 to 6 percent slopes	2184	10733	341125	cfz1	nd013	1991	1:24000
Zahl-Williams loams, 6 to 9 percent slopes	2175	8349	341116	cfyr	nd013	1991	1:24000
Williams-Zahl-Parnell complex, 0 to 9 percent slopes	C148C	6436	2564070	2q2jf	nd013	1991	1:24000
Zahl-Max-Arnegard loams, 15 to 60 percent slopes	C155F	4606	2564081	2q3bg	nd013	1991	1:24000
Zahl-Williams-Vallers loams, 0 to 60 percent slopes	2177	4388	341118	cfyt	nd013	1991	1:24000
Zahl-Williams loams, 15 to 60 percent slopes	2176	3577	341117	cfys	nd013	1991	1:24000
Zahl-Williams loams, 9 to 15 percent slopes	2081	2847	341104	cfyc	nd013	1991	1:24000
Williams-Zahl-Lihen complex, 6 to 15 percent slopes	2185	2040	341126	cfz2	nd013	1991	1:24000
Zahl-Max loams, 15 to 25 percent slopes	C153E	1435	2596888	2w42h	nd013	1991	1:24000
Zahl-Max-Bowbells loams, 6 to 35 percent slopes	C156F	1097	2595626	2q3bd	nd013	1991	1:24000
Zahl-Williams-Bowbells loams, 3 to 9 percent slopes	C154C	171	2595619	2q2jb	nd013	1991	1:24000
Williams-Zahl-Parnell complex, 0 to 9 percent slopes	2130	26	341108	cfyh	nd013	1991	1:24000
Williams-Zahl-Zahill complex, 6 to 9 percent slopes	C132C	22	2595620	2w42j	nd013	1991	1:24000
Williams-Zahl-Bowbells complex, 3 to 9 percent slopes, very stony	C161C	5	2595628	2rrq5	nd013	1991	1:24000
Miranda-Zahl loams, 3 to 25 percent slopes	C559E	2	2595629	2q4xb	nd013	1991	1:24000
Williams-Zahl-Zahill complex, 6 to 9 percent slopes	C132C	97722	2564099	2w42j	nd015	1967	1:20000
Zahl-Williams loams, 9 to 15 percent slopes	C135D	57995	2596897	2q52k	nd015	1967	1:20000
Williams-Zahl-Bowbells complex, 3 to 9 percent slopes, very stony	C161C	3768	2564151	2rrq5	nd015	1967	1:20000
Zahl-Max-Bowbells loams, 6 to 35 percent slopes	C156F	2219	2567050	2q3bd	nd015	1967	1:20000
Zahl-Max-Arnegard loams, 15 to 60 percent slopes	C155F	981	2595669	2q3bg	nd015	1967	1:20000
Zahl-Max loams, 15 to 25 percent slopes	C153E	738	2596894	2w42h	nd015	1967	1:20000
Zahl-Williams loams, 9 to 15 percent slopes	E3555D	468	2661675	cdpx	nd015	1967	1:20000
Williams-Zahl loams, 3 to 6 percent slopes	C132B	240	2595632	2w42d	nd015	1967	1:20000
Zahl-Max-Parnell complex, 0 to 35 percent slopes	C165F	79	2595641	2q3b9	nd015	1967	1:20000
Zahl-Max-Arnegard loams, 9 to 25 percent slopes	C155E	73	2596895	2q3bf	nd015	1967	1:20000
Zahl-Max-Bowbells loams, 6 to 35 percent slopes	C156F	25315	2595434	2q3bd	nd021	1989	1:20000
Williams-Zahl-Zahill complex, 6 to 9 percent slopes	C132C	14765	2564199	2w42j	nd021	1989	1:20000
Zahl-Williams-Zahill complex, 6 to 9 percent slopes	C135C	7101	2595690	2w42f	nd021	1989	1:20000
Zahl-Max-Arnegard loams, 15 to 60 percent slopes	C155F	4281	2595680	2q3bg	nd021	1989	1:20000
Williams-Zahl-Parnell complex, 0 to 9 percent slopes	C148C	2598	2595430	2q2jf	nd021	1989	1:20000
Williams-Zahl loams, 3 to 6 percent slopes	C132B	2229	2564200	2w42d	nd021	1989	1:20000
Williams-Zahl-Bowbells complex, 3 to 9 percent slopes, very stony	C161C	1839	2564224	2rrq5	nd021	1989	1:20000
Zahl-Max-Parnell complex, 0 to 35 percent slopes	C165F	508	2595433	2q3b9	nd021	1989	1:20000
Zahl-Williams loams, 9 to 15 percent slopes	C135D	119	2596909	2q52k	nd021	1989	1:20000
Williams-Zahl-Bowbells loams, 3 to 15 percent slopes	C177D	90	2596831	2w42m	nd021	1989	1:20000
Zahl-Max loams, 15 to 25 percent slopes	C176E	26	2596830	2w42h	nd021	1989	1:20000
Williams-Zahl loams, 3 to 15 percent slopes, very stony	C172D	10	2596828	2qyfw	nd021	1989	1:20000
Zahl-Williams loams, 6 to 15 percent slopes	C175D	3	2596829	2w42g	nd021	1989	1:20000
Max-Zahl-Arnegard complex, 9 to 35 percent slopes, very stony	C162F	1	2595686	2q52g	nd021	1989	1:20000
Zahl-Williams-Zahill complex, 6 to 9 percent slopes	C135C	115520	2564282	2w42f	nd023	1992	1:24000
Williams-Zahl loams, 3 to 6 percent slopes	C132B	95017	2564242	2w42d	nd023	1992	1:24000
Zahl-Williams loams, 9 to 15 percent slopes	C135D	79174	2596914	2q52k	nd023	1992	1:24000
Zahl-Max-Parnell complex, 0 to 35 percent slopes	C165F	47757	2564260	2q3b9	nd023	1992	1:24000
Williams-Zahl loams, 3 to 6 percent slopes	2031	45920	341303	cg4s	nd023	1992	1:24000
Williams-Zahl-Parnell complex, 0 to 9 percent slopes	C148C	30869	2564241	2q2jf	nd023	1992	1:24000
Zahl-Williams loams, 6 to 9 percent slopes	2175	19209	341316	cg56	nd023	1992	1:24000
Dooley-Zahl complex, 3 to 6 percent slopes	2278	8987	341332	cg5q	nd023	1992	1:24000
Zahl-Williams loams, 9 to 15 percent slopes	2081	8576	341304	cg4t	nd023	1992	1:24000
Zahl-Max-Bowbells loams, 6 to 35 percent slopes	C156F	4192	2595768	2q3bd	nd023	1992	1:24000
Zahl-Williams-Vallers loams, 0 to 60 percent slopes	2177	1933	341318	cg58	nd023	1992	1:24000
Williams-Zahl-Parnell complex, 0 to 9 percent slopes	2130	1737	341308	cg4y	nd023	1992	1:24000
Zahl-Dooley complex, 6 to 9 percent slopes	2279	1647	341333	cg5r	nd023	1992	1:24000
Dooley-Zahl complex, 3 to 6 percent slopes	C384B	1640	2564266	2q3hj	nd023	1992	1:24000
Dooley-Lihen-Zahl complex, 9 to 15 percent slopes	2280	1312	341334	cg5s	nd023	1992	1:24000
Zahl-Max loams, 15 to 25 percent slopes	C153E	1308	2596913	2w42h	nd023	1992	1:24000
Zahl-Williams-Parnell complex, 0 to 35 percent slopes	2131	1149	341309	cg4z	nd023	1992	1:24000
Miranda-Zahl loams, 3 to 25 percent slopes	1309	984	341284	cg45	nd023	1992	1:24000
Dooley-Lihen-Zahl complex, 9 to 15 percent slopes	C386D	669	2564265	2q3hh	nd023	1992	1:24000
Zahl-Dooley-Zahill complex, 6 to 9 percent slopes	C385C	618	2564240	2q2jd	nd023	1992	1:24000
Zahl-Max-Arnegard loams, 15 to 60 percent slopes	C155F	458	2564261	2q3bg	nd023	1992	1:24000
Zahl-Williams loams, 15 to 60 percent slopes	2176	370	341317	cg57	nd023	1992	1:24000
Miranda-Zahl loams, 3 to 25 percent slopes	C559E	148	2564275	2q4xb	nd023	1992	1:24000
Williams-Zahl-Zahill complex, 6 to 9 percent slopes	C132C	6	2595765	2w42j	nd023	1992	1:24000
Zahl-Max loams, 15 to 25 percent slopes	E3559E	10076	2707234	d340	nd025	1981	1:20000
Zahl-Williams loams, 9 to 15 percent slopes	E3555D	8521	2707233	cdpx	nd025	1981	1:20000
Williams-Zahl loams, 6 to 9 percent slopes	E3541C	4410	2707232	cdpt	nd025	1981	1:20000
Zahl-Williams-Arikara loams, 9 to 45 percent slopes	E3569F	395	2758488	d1xz	nd025	1981	1:20000
Zahl-Cabba-Arikara complex, 9 to 70 percent slopes	E3607F	12	2758489	cvsw	nd025	1981	1:20000
Williams-Zahl-Zahill complex, 6 to 9 percent slopes	C132C	25482	2564291	2w42j	nd029	1979	1:20000
Zahl-Max-Arnegard loams, 9 to 25 percent slopes	C155E	7612	2595779	2q3bf	nd029	1979	1:20000
Zahl-Williams loams, 9 to 15 percent slopes	C135D	6436	2596924	2q52k	nd029	1979	1:20000
Zahl-Max loams, 15 to 25 percent slopes	C153E	441	2596920	2w42h	nd029	1979	1:20000
Zahl-Max loams, dissected, 15 to 45 percent slopes	E3567F	206	2661757	cdq2	nd029	1979	1:20000
Williams-Zahl loams, 6 to 9 percent slopes	E3541C	92	2661756	cdpt	nd029	1979	1:20000
Zahl-Williams-Zahill complex, 6 to 9 percent slopes	C135C	91	2595824	2w42f	nd029	1979	1:20000
Williams-Zahl loams, 3 to 6 percent slopes	C132B	6	2595794	2w42d	nd029	1979	1:20000
Livona-Zahl-Zahill complex, 6 to 9 percent slopes	C368C	2	2596922	2q2kj	nd029	1979	1:20000
Zahl-Max-Bowbells loams, 6 to 35 percent slopes	C156F	1370	2564377	2q3bd	nd031	1990	1:20000
Williams-Zahl-Zahill complex, 6 to 9 percent slopes	C132C	1057	2564372	2w42j	nd031	1990	1:20000
Zahl-Max-Arnegard loams, 15 to 60 percent slopes	C155F	301	2596942	2q3bg	nd031	1990	1:20000
Zahl-Williams loams, 9 to 15 percent slopes	C135D	23	2596943	2q52k	nd031	1990	1:20000
Zahl-Max-Bowbells loams, 6 to 35 percent slopes	C156F	114551	2596655	2q3bd	nd043	1985	1:20000
Zahl-Max-Parnell complex, 0 to 35 percent slopes	C165F	57975	2564400	2q3b9	nd043	1985	1:20000
Williams-Zahl-Zahill complex, 6 to 9 percent slopes	C132C	49217	2564387	2w42j	nd043	1985	1:20000
Zahl-Williams-Zahill complex, 6 to 9 percent slopes	C135C	15745	2596677	2w42f	nd043	1985	1:20000
Livona-Zahl-Zahill complex, 6 to 9 percent slopes	C368C	8391	2596947	2q2kj	nd043	1985	1:20000
Zahl-Williams loams, 9 to 15 percent slopes	C135D	3500	2596950	2q52k	nd043	1985	1:20000
Zahl-Max-Arnegard loams, 9 to 25 percent slopes	C155E	1637	2596948	2q3bf	nd043	1985	1:20000
Flaxton-Zahl complex, 3 to 6 percent slopes	C358B	110	2596664	2q4vy	nd043	1985	1:20000
Zahl-Max loams, 15 to 25 percent slopes	C153E	25	2596946	2w42h	nd043	1985	1:20000
Williams-Zahl-Bowbells complex, 3 to 9 percent slopes, very stony	C161C	13	2596669	2rrq5	nd043	1985	1:20000
Wabek-Williams-Zahl complex, 9 to 15 percent slopes, very stony	C895D	7	2596682	2q839	nd043	1985	1:20000
Wabek-Max-Zahl loams, 9 to 25 percent slopes	C897E	1	2596657	2q3br	nd043	1985	1:20000
Zahl-Williams-Zahill complex, 6 to 9 percent slopes	C135C	9438	2566466	2w42f	nd045	1966	1:20000
Zahl-Williams loams, 9 to 15 percent slopes	C135D	7766	2596957	2q52k	nd045	1966	1:20000
Williams-Zahl loams, 3 to 6 percent slopes	C132B	6038	2595752	2w42d	nd045	1966	1:20000
Williams-Zahl-Zahill complex, 6 to 9 percent slopes	C132C	4200	2566434	2w42j	nd045	1966	1:20000
Williams-Zahl-Bowbells complex, 3 to 9 percent slopes, very stony	C161C	206	2566451	2rrq5	nd045	1966	1:20000
Zahl-Max loams, 15 to 25 percent slopes	C153E	156	2596954	2w42h	nd045	1966	1:20000
Zahl-Max-Bowbells loams, 6 to 35 percent slopes	C156F	149	2595754	2q3bd	nd045	1966	1:20000
Zahl-Williams-Zahill complex, 6 to 9 percent slopes	C135C	100491	2566533	2w42f	nd047	1992	1:20000
Zahl-Williams loams, 9 to 15 percent slopes	C135D	95309	2596969	2q52k	nd047	1992	1:20000
Williams-Zahl loams, 3 to 6 percent slopes	C132B	64822	2566478	2w42d	nd047	1992	1:20000
Zahl-Max-Bowbells loams, 6 to 35 percent slopes	C156F	24774	2566494	2q3bd	nd047	1992	1:20000
Max-Zahl-Arnegard complex, 9 to 35 percent slopes, very stony	C162F	7679	2566506	2q52g	nd047	1992	1:20000
Williams-Zahl-Parnell complex, 0 to 9 percent slopes	C148C	7073	2595497	2q2jf	nd047	1992	1:20000
Zahl-Max-Arnegard loams, 15 to 60 percent slopes	C155F	2325	2596687	2q3bg	nd047	1992	1:20000
Krem-Lihen-Zahl complex, 0 to 9 percent slopes	C379C	1764	2595509	2q76z	nd047	1992	1:20000
Zahl-Max-Parnell complex, 0 to 35 percent slopes	C165F	736	2595501	2q3b9	nd047	1992	1:20000
Zahl-Max loams, 15 to 25 percent slopes	C153E	468	2596965	2w42h	nd047	1992	1:20000
Krem-Lihen-Zahl complex, 9 to 25 percent slopes	C379E	426	2595510	2q770	nd047	1992	1:20000
Zahl-Max loams, dissected, 15 to 45 percent slopes	E3567F	273	2661850	cdq2	nd047	1992	1:20000
Zahl-Williams loams, 9 to 15 percent slopes	E3555D	261	2661849	cdpx	nd047	1992	1:20000
Livona-Zahl-Zahill complex, 6 to 9 percent slopes	C368C	181	2596967	2q2kj	nd047	1992	1:20000
Williams-Zahl-Zahill complex, 6 to 9 percent slopes	C132C	75	2596696	2w42j	nd047	1992	1:20000
Wabek-Max-Zahl loams, 9 to 25 percent slopes	C897E	4	2596702	2q3br	nd047	1992	1:20000
Flaxton-Zahl complex, 3 to 6 percent slopes	C358B	4	2596704	2q4vy	nd047	1992	1:20000
Williams-Zahl-Zahill complex, 6 to 9 percent slopes	C132C	4290	2566545	2w42j	nd049	1987	1:20000
Zahl-Max-Bowbells loams, 6 to 35 percent slopes	C156F	2795	2595513	2q3bd	nd049	1987	1:20000
Williams-Zahl loams, 3 to 6 percent slopes	C132B	1478	2566546	2w42d	nd049	1987	1:20000
Zahl-Max-Arnegard loams, 15 to 60 percent slopes	C155F	332	2567114	2q3bg	nd049	1987	1:20000
Zahl-Max-Parnell complex, 0 to 35 percent slopes	C165F	157	2567115	2q3b9	nd049	1987	1:20000
Zahl-Williams loams, 9 to 15 percent slopes	C135D	64	2661668	2q52k	nd049	1987	1:20000
Zahl-Williams loams, 9 to 15 percent slopes	C135D	63148	2596981	2q52k	nd051	1992	1:24000
Zahl-Williams-Zahill complex, 6 to 9 percent slopes	C135C	61271	2566619	2w42f	nd051	1992	1:24000
Williams-Zahl loams, 3 to 6 percent slopes	C132B	41706	2566566	2w42d	nd051	1992	1:24000
Zahl-Max-Bowbells loams, 6 to 35 percent slopes	C156F	13429	2566585	2q3bd	nd051	1992	1:24000
Williams-Zahl-Zahill complex, 6 to 9 percent slopes	C132C	4743	2596727	2w42j	nd051	1992	1:24000
Max-Zahl-Arnegard complex, 9 to 35 percent slopes, very stony	C162F	3813	2566595	2q52g	nd051	1992	1:24000
Zahl-Max-Arnegard loams, 15 to 60 percent slopes	C155F	2005	2596720	2q3bg	nd051	1992	1:24000
Williams-Zahl-Parnell complex, 0 to 9 percent slopes	C148C	1179	2595517	2q2jf	nd051	1992	1:24000
Zahl-Max loams, 15 to 25 percent slopes	C153E	307	2662602	2w42h	nd051	1992	1:24000
Zahl-Max-Parnell complex, 0 to 35 percent slopes	C165F	198	2596736	2q3b9	nd051	1992	1:24000
Zahl-Williams loams, 9 to 15 percent slopes	E3555D	86	2661987	cdpx	nd051	1992	1:24000
Williams-Zahl loams, 3 to 15 percent slopes, very stony	C172D	68	2596759	2qyfw	nd051	1992	1:24000
Zahl-Max loams, dissected, 15 to 45 percent slopes	E3567F	54	2661988	cdq2	nd051	1992	1:24000
Williams-Zahl-Bowbells loams, 3 to 15 percent slopes	C177D	11	2596760	2w42m	nd051	1992	1:24000
Williams-Zahl-Bowbells complex, 3 to 9 percent slopes, very stony	C161C	3	2596743	2rrq5	nd051	1992	1:24000
Zahl-Cabba-Maschetah complex, 6 to 70 percent slopes	E3609F	88670	2715121	d341	nd053	2003	1:24000
Williams-Zahl loams, 6 to 9 percent slopes	E3541C	60652	2715114	cdpt	nd053	2003	1:24000
Williams-Zahl loams, 3 to 6 percent slopes	E3541B	51105	2715113	d33y	nd053	2003	1:24000
Zahl-Williams loams, 9 to 15 percent slopes	E3555D	38618	2715115	cdpx	nd053	2003	1:24000
Zahl-Cabba-Arikara complex, 9 to 70 percent slopes	E3607F	34262	2715120	cvsw	nd053	2003	1:24000
Zahl-Max loams, dissected, 15 to 45 percent slopes	E3567F	32398	2715117	cdq2	nd053	2003	1:24000
Zahl-Cabba-Williams complex, 9 to 15 percent slopes	E3641D	28282	2699325	d330	nd053	2003	1:24000
Zahl-Williams-Cabba complex, 6 to 9 percent slopes	E3639C	18294	2699324	d32z	nd053	2003	1:24000
Zahl-Beisigl-Tally complex, 9 to 15 percent slopes	E3637D	15853	2715123	d332	nd053	2003	1:24000
Zahl-Max loams, 15 to 25 percent slopes	E3559E	12503	2715116	d340	nd053	2003	1:24000
Dooley-Zahl complex, 6 to 9 percent slopes	E3703C	12447	2699328	d343	nd053	2003	1:24000
Dooley-Zahl complex, 3 to 6 percent slopes	E3703B	9253	2699327	d342	nd053	2003	1:24000
Temvik-Zahl complex, 3 to 6 percent slopes	E3769B	6374	2699332	d345	nd053	2003	1:24000
Zahl-Tally-Williams complex, 6 to 9 percent slopes	E3635C	5522	2715122	d331	nd053	2003	1:24000
Dooley-Zahl complex, 9 to 15 percent slopes	E3703D	4640	2699329	d344	nd053	2003	1:24000
Wabek-Zahl complex, 9 to 35 percent slopes	E3571F	3840	2715119	cdtv	nd053	2003	1:24000
Zahl-Williams-Arikara loams, 9 to 45 percent slopes	E3569F	2311	2715118	d1xz	nd053	2003	1:24000
Zahl-Cabba-Williams complex, 9 to 15 percent slopes	460D	61	351831	ct3d	nd053	2003	1:24000
Zahl-Cabba-Maschetah complex, 3 to 70 percent slopes	45F	29	351828	ct39	nd053	2003	1:24000
Williams-Zahl-Zahill complex, 6 to 9 percent slopes	C132C	117493	2566636	2w42j	nd055	1974	1:20000
Williams-Zahl loams, 3 to 6 percent slopes	C132B	60329	2566637	2w42d	nd055	1974	1:20000
Zahl-Williams loams, 9 to 15 percent slopes	C135D	47404	2596997	2q52k	nd055	1974	1:20000
Zahl-Max-Arnegard loams, 15 to 60 percent slopes	C155F	33486	2567123	2q3bg	nd055	1974	1:20000
Zahl-Max-Bowbells loams, 6 to 35 percent slopes	C156F	26095	2595544	2q3bd	nd055	1974	1:20000
Zahl-Max-Parnell complex, 0 to 35 percent slopes	C165F	16477	2566662	2q3b9	nd055	1974	1:20000
Zahl-Williams-Zahill complex, 6 to 9 percent slopes	C135C	10185	2566719	2w42f	nd055	1974	1:20000
Zahl-Werner complex, 15 to 35 percent slopes	C966F	4883	2566720	2q73f	nd055	1974	1:20000
Wabek-Max-Zahl loams, 9 to 25 percent slopes	C897E	3768	2596869	2q3br	nd055	1974	1:20000
Zahl-Max-Arnegard loams, 9 to 25 percent slopes	C155E	1939	2596993	2q3bf	nd055	1974	1:20000
Lihen-Zahl complex, 9 to 25 percent slopes	C318E	833	2566630	2q0rm	nd055	1974	1:20000
Zahl-Max loams, dissected, 15 to 45 percent slopes	E3567F	754	2662436	cdq2	nd055	1974	1:20000
Williams-Zahl-Bowbells complex, 3 to 9 percent slopes, very stony	C161C	660	2566686	2rrq5	nd055	1974	1:20000
Zahl-Max loams, 15 to 25 percent slopes	C153E	496	2596992	2w42h	nd055	1974	1:20000
Zahl-Williams loams, 9 to 15 percent slopes	E3555D	424	2662435	cdpx	nd055	1974	1:20000
Wabek-Zahl complex, 9 to 35 percent slopes	E3571F	263	2662443	cdtv	nd055	1974	1:20000
Zahl-Williams-Haplustolls complex, 9 to 15 percent slopes	C1018D	183	2775239	2w42w	nd055	1974	1:20000
Williams-Zahl loams, 6 to 9 percent slopes	E3541C	148	2662434	cdpt	nd055	1974	1:20000
Vebar-Flasher-Zahl complex, 6 to 25 percent slopes	C959E	85	2567158	2q836	nd055	1974	1:20000
Wabek-Williams-Zahl complex, 3 to 9 percent slopes, very stony	C895C	62	2567159	2q838	nd055	1974	1:20000
Williams-Zahl-Parnell complex, 0 to 9 percent slopes	C148C	16	2567135	2q2jf	nd055	1974	1:20000
Miranda-Zahl loams, 3 to 25 percent slopes	C559E	13	2567152	2q4xb	nd055	1974	1:20000
Krem-Lihen-Zahl complex, 9 to 25 percent slopes	C379E	1	2567156	2q770	nd055	1974	1:20000
Zahl-Williams loams, 9 to 15 percent slopes	E3555D	19032	2699396	cdpx	nd057	1976	1:20000
Williams-Zahl loams, 6 to 9 percent slopes	E3541C	14385	2699394	cdpt	nd057	1976	1:20000
Zahl-Max loams, 15 to 25 percent slopes	E3559E	5469	2699395	d340	nd057	1976	1:20000
Bowbells-Zahl loams, 3 to 6 percent slopes	E3505B	1895	2699248	2qkx2	nd057	1976	1:20000
Williams-Zahl loams, 6 to 9 percent slopes	E3541C	13128	2699233	cdpt	nd059	1998	1:20000
Zahl-Max loams, dissected, 15 to 45 percent slopes	E3567F	7596	2699234	cdq2	nd059	1998	1:20000
Zahl-Williams loams, 9 to 15 percent slopes	E3555D	412	2759678	cdpx	nd059	1998	1:20000
Zahl-Williams loams, 9 to 15 percent slopes	C135D	201195	2597011	2q52k	nd061	1988	1:24000
Williams-Zahl loams, 3 to 6 percent slopes	C132B	168033	2566734	2w42d	nd061	1988	1:24000
Zahl-Williams-Bowbells loams, 3 to 9 percent slopes	C154C	122052	2566732	2q2jb	nd061	1988	1:24000
Williams-Zahl-Zahill complex, 6 to 9 percent slopes	C132C	99634	2566733	2w42j	nd061	1988	1:24000
Zahl-Max-Parnell complex, 0 to 35 percent slopes	C165F	46190	2566749	2q3b9	nd061	1988	1:24000
Zahl-Max-Arnegard loams, 15 to 60 percent slopes	C155F	28945	2567076	2q3bg	nd061	1988	1:24000
Zahl-Max loams, 15 to 25 percent slopes	C153E	4004	2597006	2w42h	nd061	1988	1:24000
Vebar-Flasher-Zahl complex, 6 to 25 percent slopes	C959E	3344	2566779	2q836	nd061	1988	1:24000
Miranda-Zahl loams, 3 to 25 percent slopes	C559E	2640	2566761	2q4xb	nd061	1988	1:24000
Zahl-Max-Bowbells loams, 6 to 35 percent slopes	C156F	1916	2595561	2q3bd	nd061	1988	1:24000
Zahl-Williams-Zahill complex, 6 to 9 percent slopes	C135C	1707	2567106	2w42f	nd061	1988	1:24000
Vebar-Cohagen-Zahl complex, 9 to 25 percent slopes	E3615E	972	2662537	2r4hr	nd061	1988	1:24000
Zahl-Max loams, 15 to 25 percent slopes	E3559E	961	2662509	d340	nd061	1988	1:24000
Williams-Zahl loams, 6 to 9 percent slopes	E3541C	910	2662502	cdpt	nd061	1988	1:24000
Werner-Amor-Zahl loams, 25 to 60 percent slopes	C908F	675	2597015	2q6lr	nd061	1988	1:24000
Williams-Zahl loams, 3 to 6 percent slopes	E3541B	535	2662508	d33y	nd061	1988	1:24000
Zahl-Max loams, dissected, 15 to 45 percent slopes	E3567F	527	2662503	cdq2	nd061	1988	1:24000
Zahl-Max-Arnegard loams, 9 to 25 percent slopes	C155E	400	2597009	2q3bf	nd061	1988	1:24000
Williams-Zahl-Parnell complex, 0 to 9 percent slopes	C148C	105	2567082	2q2jf	nd061	1988	1:24000
Amor-Zahl-Werner loams, 9 to 25 percent slopes	C906E	59	2567103	2q1nq	nd061	1988	1:24000
Wabek-Williams-Zahl complex, 3 to 9 percent slopes, very stony	C895C	2	2567108	2q838	nd061	1988	1:24000
Zahl-Williams loams, 9 to 15 percent slopes	E3555D	18761	2525963	cdpx	nd065	1971	1:20000
Zahl-Max loams, 15 to 25 percent slopes	E3559E	7118	2525964	d340	nd065	1971	1:20000
Williams-Zahl loams, 6 to 9 percent slopes	E3541C	5	2755697	cdpt	nd065	1971	1:20000
Williams-Zahl-Zahill complex, 6 to 9 percent slopes	C132C	92585	2566782	2w42j	nd083	1990	1:20000
Zahl-Williams loams, 9 to 15 percent slopes	C135D	52529	2597022	2q52k	nd083	1990	1:20000
Zahl-Max-Parnell complex, 0 to 35 percent slopes	C165F	32234	2566794	2q3b9	nd083	1990	1:20000
Zahl-Max-Bowbells loams, 6 to 35 percent slopes	C156F	19662	2566795	2q3bd	nd083	1990	1:20000
Williams-Zahl-Parnell complex, 0 to 9 percent slopes	C148C	19617	2566781	2q2jf	nd083	1990	1:20000
Krem-Lihen-Zahl complex, 0 to 9 percent slopes	C379C	924	2566819	2q76z	nd083	1990	1:20000
Zahl-Max-Arnegard loams, 15 to 60 percent slopes	C155F	896	2597020	2q3bg	nd083	1990	1:20000
Zahl-Max loams, 15 to 25 percent slopes	C153E	636	2597018	2w42h	nd083	1990	1:20000
Krem-Lihen-Zahl complex, 9 to 25 percent slopes	C379E	250	2566820	2q770	nd083	1990	1:20000
Wabek-Williams-Zahl complex, 9 to 15 percent slopes, very stony	C895D	96	2567191	2q839	nd083	1990	1:20000
Williams-Zahl loams, 3 to 6 percent slopes	C132B	46	2567169	2w42d	nd083	1990	1:20000
Wabek-Max-Zahl loams, 9 to 25 percent slopes	C897E	28	2596872	2q3br	nd083	1990	1:20000
Zahl-Williams-Zahill complex, 6 to 9 percent slopes	C135C	27	2567189	2w42f	nd083	1990	1:20000
Williams-Zahl-Bowbells complex, 3 to 9 percent slopes, very stony	C161C	2	2567184	2rrq5	nd083	1990	1:20000
Zahl-Max-Bowbells loams, 6 to 35 percent slopes	C156F	91238	2566846	2q3bd	nd093	1990	1:24000
Williams-Zahl-Zahill complex, 6 to 9 percent slopes	C132C	91072	2566829	2w42j	nd093	1990	1:24000
Zahl-Williams loams, 9 to 15 percent slopes	C135D	83274	2661634	2q52k	nd093	1990	1:24000
Zahl-Williams-Zahill complex, 6 to 9 percent slopes	C135C	21430	2595739	2w42f	nd093	1990	1:24000
Zahl-Max-Parnell complex, 0 to 35 percent slopes	C165F	16668	2566844	2q3b9	nd093	1990	1:24000
Williams-Zahl loams, 3 to 6 percent slopes	C132B	14776	2595733	2w42d	nd093	1990	1:24000
Wabek-Max-Zahl loams, 9 to 25 percent slopes	C897E	13794	2566848	2q3br	nd093	1990	1:24000
Livona-Zahl-Zahill complex, 6 to 9 percent slopes	C368C	2295	2597028	2q2kj	nd093	1990	1:24000

Map of Series Extent

Approximate geographic distribution of the ZAHL 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).