Soil Data Explorer - HARLAKE

Official Series Description

Lab Data Summary

Aggregate lab data for the HARLAKE soil series. This aggregation is based on all pedons with a current taxon name of HARLAKE, 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 HARLAKE 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 HARLAKE 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 HARLAKE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-02) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the HARLAKE 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 HARLAKE 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 HARLAKE share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-02) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the HARLAKE 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 HARLAKE 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 2D hillslope position figure.

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 terrace figure.

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

Soil series sharing subgroup-level classification with HARLAKE, 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 HARLAKE 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
Harlake silty clay loam, 0 to 2 percent slopes	157A	24970	342919	chtx	mt011	1992	1:24000
Harlake silty clay, saline, 0 to 2 percent slopes	57A	9400	343148	cj29	mt011	1992	1:24000
Havre-Harlake complex, 0 to 2 percent slopes	256A	6569	343049	chz3	mt011	1992	1:24000
Harlake silty clay loam, warm, saline, 0 to 3 percent slopes	606B	729	343164	cj2t	mt011	1992	1:24000
Harlake clay, warm, 0 to 3 percent slopes	608B	372	343165	cj2v	mt011	1992	1:24000
Havre-Harlake complex, 0 to 2 percent slopes, occasionally flooded	4871A	5248	343500	cjfn	mt017	1995	1:24000
Harlake silty clay, 0 to 2 percent slopes, occasionally flooded	471A	4202	343479	cjdz	mt017	1995	1:24000
Harlake silty clay, 0 to 2 percent slopes, rarely flooded	47A	3978	343485	cjf5	mt017	1995	1:24000
Havre-Harlake complex, 0 to 2 percent slopes, nonflooded	487A	1244	343501	cjfp	mt017	1995	1:24000
Havre, Harlake, and Glendive soils, channeled, 0 to 2 percent slopes	844A	909	343708	cjnc	mt017	1995	1:24000
Harlake silty clay loam, 0 to 2 percent slopes, occasionally flooded	942A	8	343762	cjq3	mt017	1995	1:24000
Harlake silty clay, saline, 0 to 2 percent slopes	57A	3792	342248	ch48	mt025	1991	1:24000
Havre-Harlake complex, 0 to 2 percent slopes	256A	3751	342171	ch1s	mt025	1991	1:24000
Harlake silty clay loam, 0 to 2 percent slopes	157A	1548	342102	cgzk	mt025	1991	1:24000
Harlake silty clay, 0 to 2 percent slopes, rarely flooded	60A	4886	342672	chky	mt033	2002	1:24000
Havre, Harlake, and Glendive soils, channeled	617A	1167	360656	d392	mt033	2002	1:24000
Harlake-Havre complex, 0 to 2 percent slopes, rarely flooded	621A	136	615802	nnsl	mt033	2002	1:24000
Havre-Harlake clay loams, 0 to 2 percent slopes	603A	15035	344010	cjz3	mt041	1994	1:24000
Harlake clay, 0 to 2 percent slopes	90A	3208	344102	ck22	mt041	1994	1:24000
Harlake silty clay, 0 to 1 percent slopes	90A	1450	344278	ck7r	mt051	1992	1:24000
Harlake silty clay, 0 to 2 percent slopes	81	6313	344448	ckf7	mt055	1981	1:24000
Harlake silty clay, 0 to 2 percent slopes, rarely flooded	80	760	344447	ckf6	mt055	1981	1:24000
Havre-Harlake complex, 0 to 2 percent slopes, occasionally flooded	12A	5856	344473	cghl	mt065	1996	1:24000
Harlake-Marvan-Vanda silty clays, 0 to 4 percent slopes	20B	2690	344505	ckh2	mt065	1996	1:24000
Harlake-Havre complex, 0 to 2 percent slopes, occasionally flooded	8A	2560	344643	cglp	mt065	1996	1:24000
Harlake-Havre complex, 0 to 2 percent slopes, rarely flooded	108A	2300	1717986	1vn89	mt065	1996	1:24000
Havre-Harlake complex, calcareous, 0 to 2 percent slopes, rarely flooded	15A	1025	344493	cgj2	mt065	1996	1:24000
Harlake silty clay, 0 to 2 percent slopes, rarely flooded	5A	717	344604	cgkp	mt065	1996	1:24000
Harlake-Havre complex, calcareous, 0 to 2 percent slopes	17A	714	344497	ckgt	mt065	1996	1:24000
Harlake silty clay, 0 to 2 percent slopes, occasionally flooded	6A	18	344619	cklr	mt065	1996	1:24000
Harlem-Havre complex, 0 to 2 percent slopes	45	8523	344713	ckps	mt069	1989	1:24000
Havre-Harlake complex, 0 to 2 percent slopes	70	936	344994	ckzv	mt079	1986	1:24000
Harlake silty clay loam, 0 to 2 percent slopes	90A	428	345300	cl9q	mt101	1992	1:24000
Harlake silty clay, 0 to 1 percent slopes	90A	2173	346976	cn1s	mt615	1992	1:24000
Havre-Harlake complex, 0 to 2 percent slopes, rarely flooded	9A	4956	347547	cnn6	mt624	2021	1:24000
Havre-Harlake complex, 0 to 4 percent slopes	424A	2731	1910245	223rt	mt624	2021	1:24000
Havre-Harlake-Glendive complex, 0 to 2 percent slopes, occasionally flooded	912A	1427	2431502	2mm5k	mt624	2021	1:24000
Havre-Harlake complex, cool, 0 to 2 percent slopes, rarely flooded	423A	1033	1909475	222yz	mt624	2021	1:24000
Kobase-Harlake, rarely flooded-Lostriver, rarely flooded complex, 0 to 4 percent slopes	807B	499	2384474	2l17j	mt624	2021	1:24000
Havre-Harlake complex, 0 to 2 percent slopes, occasionally flooded	12A	13	3176843	cghl	mt624	2021	1:24000
Harlake clay, 0 to 2 percent slopes	90A	34359	347797	cnx8	mt641	1994	1:24000
Harlake-Lostriver clays, 0 to 2 percent slopes	903A	32528	347794	cnx5	mt641	1994	1:24000
Harlake-Marvan association, 0 to 4 percent slopes	1090B	27317	347570	cnny	mt641	1994	1:24000
Havre-Harlake-Glendive complex, 0 to 2 percent slopes	601A	17111	347761	cnw3	mt641	1994	1:24000
Harlake-Havre clay loams, 0 to 2 percent slopes	905A	6020	347796	cnx7	mt641	1994	1:24000
Havre, Harlake, and Glendive soils, channeled, 0 to 2 percent slopes	104	48251	347925	cp1d	mt649	1985	1:24000
Havre-Harlake complex, 0 to 2 percent slopes, occasionally flooded, channeled	12A	43	1712460	1vgyn	mt655	1975	1:24000
Harlake clay loam, 0 to 4 percent slopes, rarely flooded	406	2725	348633	cps7	mt657	1990	1:24000
Havre-Harlake complex, 0 to 2 percent slopes, occasionally flooded	12A	3798	341638	cghl	mt666	2008	1:24000
Harlake-Havre complex, 0 to 2 percent slopes, rarely flooded	108A	1777	1717564	1vn89	mt666	2008	1:24000
Harlake silty clay, 0 to 2 percent slopes, rarely flooded	5A	1169	341703	cgkp	mt666	2008	1:24000
Havre-Harlake complex, calcareous, 0 to 2 percent slopes, rarely flooded	15A	1017	341653	cgj2	mt666	2008	1:24000
Harlake-Havre complex, 0 to 2 percent slopes, occasionally flooded	8A	961	341734	cglp	mt666	2008	1:24000
Havre-Harlake complex	Hh	4465	355752	cy5w	sd063	1984	1:24000
Harlake silty clay, channeled	Hf	1836	355750	cy5t	sd063	1984	1:24000

Map of Series Extent

Approximate geographic distribution of the HARLAKE 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).