Soil Data Explorer - KREMLIN

Official Series Description

Lab Data Summary

Aggregate lab data for the KREMLIN soil series. This aggregation is based on all pedons with a current taxon name of KREMLIN, 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 KREMLIN 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
58A	13N97461	S2013MT017002	Kremlin	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.2308861,-106.0394722

Water Balance

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

Soil series sharing subgroup-level classification with KREMLIN, 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 KREMLIN 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
Kremlin loam, warm, 2 to 8 percent slopes	72C	8500	343224	2wby3	mt011	1992	1:24000
Kremlin loam, 0 to 2 percent slopes	72A	2502	343223	cj4q	mt011	1992	1:24000
Kremlin-Cabbart complex, 2 to 8 percent slopes	172C	1236	342962	chw9	mt011	1992	1:24000
Kremlin loam, warm, 2 to 8 percent slopes	50C	8648	343514	2wby3	mt017	1995	1:24000
Kremlin-Delpoint loams, 2 to 8 percent slopes	501C	6285	343512	cjg1	mt017	1995	1:24000
Chinook-Kremlin complex, 2 to 6 percent slopes	353C	5606	343401	cjbg	mt017	1995	1:24000
Kremlin-Tinsley-Degrand complex, 4 to 15 percent slopes	121D	1488	343305	cj7c	mt017	1995	1:24000
Kremlin-Cabbart complex, 2 to 8 percent slopes	613C	52	343583	cjjb	mt017	1995	1:24000
Kremlin loam, warm, 2 to 8 percent slopes	50C	24957	3040425	2wby3	mt021	1971	1:24000
Kremlin-Eapa loams, 0 to 4 percent slopes	501B	14044	754481	tb33	mt021	1971	1:24000
Kremlin loam, 0 to 2 percent slopes	50A	7886	754478	tb30	mt021	1971	1:24000
Kremlin loam, warm, 2 to 8 percent slopes	72C	23470	342280	2wby3	mt025	1991	1:24000
Kremlin-Cabbart complex, 2 to 8 percent slopes	172C	4671	342128	ch0d	mt025	1991	1:24000
Kremlin loam, 0 to 2 percent slopes	72A	2392	342279	ch58	mt025	1991	1:24000
Kremlin-Delpoint loams, 2 to 8 percent slopes	671C	12168	342682	chl8	mt033	2002	1:24000
Chinook-Kremlin complex, 2 to 6 percent slopes	381C	7333	342642	chjz	mt033	2002	1:24000
Kremlin loam, warm, 2 to 8 percent slopes	67C	6963	3040426	2wby3	mt033	2002	1:24000
Kremlin loam, 0 to 4 percent slopes	672B	17	342812	chqg	mt033	2002	1:24000
Kremlin loam, 0 to 4 percent slopes	98B	20185	344124	ck2s	mt041	1994	1:24000
Kremlin loam, 2 to 8 percent slopes	98C	541	344289	ck83	mt051	1992	1:24000
Kremlin loam, 0 to 4 percent slopes	97	5184	344465	ckfs	mt055	1981	1:24000
Kremlin loam, warm, 2 to 8 percent slopes	98	5015	3040427	2wby3	mt055	1981	1:24000
Kremlin loam, 2 to 8 percent slopes	56	492	344725	2wbyb	mt069	1989	1:24000
Kremlin loam, 0 to 2 percent slopes	55	315	344724	ckq4	mt069	1989	1:24000
Kremlin loam, warm, 2 to 8 percent slopes	77	13442	345013	2wby3	mt079	1986	1:24000
Kremlin loam, 0 to 2 percent slopes	76	7640	345009	cl0b	mt079	1986	1:24000
Chinook-Kremlin complex, 2 to 6 percent slopes	35	3840	344885	ckwb	mt079	1986	1:24000
Kremlin-Busby complex, 0 to 2 percent slopes	78	1374	345014	cl0h	mt079	1986	1:24000
Kremlin-Tinsley-Degrand complex, 4 to 15 percent slopes	79	622	345015	cl0j	mt079	1986	1:24000
Kremlin-Eapa loams, 0 to 4 percent slopes	146	319	1145695	17g5x	mt079	1986	1:24000
Kremlin loam, 0 to 2 percent slopes	50A	1271	1711704	1vg58	mt083	1973	1:24000
Kremlin loam, warm, 2 to 8 percent slopes	50C	1206	1677538	2wby3	mt083	1973	1:24000
Kremlin-Eapa loams, 0 to 4 percent slopes	501B	1158	1711692	1vg4w	mt083	1973	1:24000
Kremlin loam, 0 to 4 percent slopes	98B	2264	345314	clb5	mt101	1992	1:24000
Kremlin loam, 0 to 4 percent slopes	98B	11224	347013	cn2z	mt615	1992	1:24000
Kremlin loam, 2 to 8 percent slopes	098C	1058	347014	2wbyb	mt615	1992	1:24000
Kremlin loam, 4 to 8 percent slopes	98C	889	3040430	cn30	mt615	1992	1:24000
Kremlin loam, 0 to 4 percent slopes, fan	414B	908	1914274	227ys	mt624	2021	1:24000
Kremlin loam, 4 to 8 percent slopes	147C	805	2440718	2mxrv	mt624	2021	1:24000
Kremlin loam, 0 to 4 percent slopes	147B	419	347263	cnc1	mt624	2021	1:24000
Kremlin loam, 4 to 8 percent slopes, fan	414C	284	1914323	2280c	mt624	2021	1:24000
Kremlin loam, 8 to 15 percent slopes	147D	14	3176832	50r2	mt624	2021	1:24000
Kremlin loam, 4 to 8 percent slopes	147C	3290	149669	50r1	mt639	2000	1:24000
Kremlin loam, 0 to 4 percent slopes	147B	2128	149668	50r0	mt639	2000	1:24000
Kremlin loam, 8 to 15 percent slopes	147D	483	149670	50r2	mt639	2000	1:24000
Kremlin loam, warm, 2 to 8 percent slopes	117	8275	347939	2wby3	mt649	1985	1:24000
Kremlin loam, 0 to 2 percent slopes	116	4261	347938	cp1t	mt649	1985	1:24000
Delpoint-Kremlin-Vanda complex, 2 to 15 percent slopes	876C	16595	348815	cpz3	mt657	1990	1:24000
Kremlin clay loam, 0 to 4 percent slopes	322B	13180	348566	cpq2	mt657	1990	1:24000
Kremlin-Delpoint clay loams, 2 to 8 percent slopes	522C	11757	348701	cpvf	mt657	1990	1:24000
Kremlin loam, 0 to 4 percent slopes	22B	9949	348470	cplz	mt657	1990	1:24000
Kremlin clay loam, 4 to 8 percent slopes	322C	9890	348567	cpq3	mt657	1990	1:24000
Delpoint-Kremlin-Cabbart complex, 4 to 15 percent slopes	476D	6775	348677	cptn	mt657	1990	1:24000
Chinook-Kremlin complex, 0 to 4 percent slopes	434B	2640	348650	cpss	mt657	1990	1:24000
Kremlin loam, 0 to 4 percent slopes	147B	13	1538575	1nn0g	mt666	2008	1:24000
Notter-Kremlin-Chinook complex, 2 to 25 percent slopes	824E	2953	156967	58bg	mt669		1:24000
Ethridge-Kremlin-Yamacall complex, 0 to 8 percent slopes	2202C	2894	156489	57v1	mt669		1:24000
Kremlin clay loam, 0 to 4 percent slopes	57B	2893	156825	585w	mt669		1:24000
Kremlin-Rothiemay complex, 0 to 4 percent slopes	4B	2549	156795	584x	mt669		1:24000
Sixbeacon-Kremlin-Cozberg complex, 0 to 25 percent slopes	745E	2192	156954	58b1	mt669		1:24000
Kremlin-Beavwan-Vendome, very stony complex, 2 to 8 percent slopes	429C	1112	156917	588v	mt669		1:24000
Ethridge-Urban land-Kremlin complex, 0 to 4 percent slopes	12B	460	886547	yrj9	mt669		1:24000
Kremlin-Ethridge-Gerda complex, 0 to 6 percent slopes	L3251B	8160	2707069	2qz6r	nd007	1998	1:24000
Rhame-Kremlin-Archin complex, 6 to 15 percent slopes	L2335D	6263	2707047	2qxkf	nd007	1998	1:24000
Kremlin, gravelly substratum-Chanta loams, 2 to 6 percent slopes	L4573B	1901	2707090	2qxk3	nd007	1998	1:24000
Kremlin loam, 0 to 2 percent slopes	L2145A	1704	2707042	2qxj9	nd007	1998	1:24000
Boxwell-Kremlin loams, 9 to 15 percent slopes	L2807D	1673	2707052	2q1xs	nd007	1998	1:24000
Kremlin-Shibah loams, 9 to 50 percent slopes, very bouldery	L4511F	1613	2707084	2q38m	nd007	1998	1:24000
Boxwell-Kremlin loams, 3 to 6 percent slopes	L2803B	1606	2707050	2qxkx	nd007	1998	1:24000
Kremlin, gravelly substratum-Chanta loams, 0 to 2 percent slopes	L4573A	1253	2707089	2qxk2	nd007	1998	1:24000
Rhame-Kremlin-Archin complex, 0 to 6 percent slopes	L2335B	885	2707046	2qz9h	nd007	1998	1:24000
Boxwell-Kremlin loams, 6 to 9 percent slopes	L2807C	164	2707051	2qxky	nd007	1998	1:24000
Kremlin-Belfield-Rhoades complex, 0 to 6 percent slopes	KsA	1710	992850	12b4f	nd011	1969	1:20000
Kremlin loam, 0 to 2 percent slopes	KrA	1155	992848	12b4c	nd011	1969	1:20000
Boxwell-Kremlin loams, 0 to 6 percent slopes	BtB	590	992794	12b2m	nd011	1969	1:20000
Kremlin loam, 2 to 6 percent slopes	KrB	374	992849	12b4d	nd011	1969	1:20000
Kremlin, gravelly substratum-Chanta loams, 0 to 2 percent slopes	L4573A	223	2563508	2qxk2	nd011	1969	1:20000
Kremlin, gravelly substratum-Chanta loams, 2 to 6 percent slopes	L4573B	202	2563509	2qxk3	nd011	1969	1:20000
Kremlin-Belfield, low precipitation-Gerda complex, 0 to 2 percent slopes	L0627A	181	2563459	2q2mn	nd011	1969	1:20000
Kremlin loam, 0 to 2 percent slopes	L2145A	125	2758460	2qxj9	nd011	1969	1:20000
Boxwell-Kremlin loams, 6 to 9 percent slopes	L2807C	99	2563481	2qxky	nd011	1969	1:20000
Boxwell-Kremlin loams, 3 to 6 percent slopes	L2803B	95	2563480	2qxkx	nd011	1969	1:20000
Cabbart-Kremlin-Boxwell loams, 9 to 40 percent slopes, slumped	L2621F	19156	2707123	d361	nd025	1981	1:20000
Boxwell-Kremlin loams, 3 to 6 percent slopes	L2803B	722	2707156	2qxkx	nd025	1981	1:20000
Boxwell-Kremlin loams, 6 to 9 percent slopes	L2807C	391	2707157	2qxky	nd025	1981	1:20000
Kremlin loam, 0 to 2 percent slopes	L2145A	54	2707145	2qxj9	nd025	1981	1:20000
Rhame-Bullock-Kremlin complex, 9 to 35 percent slopes	L2307F	38	2758493	2qxjh	nd025	1981	1:20000
Boxwell-Kremlin loams, 9 to 15 percent slopes	L2807D	8	2758497	2q1xs	nd025	1981	1:20000
Kremlin-Shibah loams, 9 to 50 percent slopes, very bouldery	L4511F	2152	2707349	2q38m	nd033	1985	1:24000
Kremlin, gravelly substratum-Chanta loams, 2 to 6 percent slopes	L4573B	1326	2707354	2qxk3	nd033	1985	1:24000
Kremlin-Ethridge-Gerda complex, 0 to 6 percent slopes	L3251B	1286	2707343	2qz6r	nd033	1985	1:24000
Boxwell-Kremlin loams, 3 to 6 percent slopes	L2803B	1015	2707331	2qxkx	nd033	1985	1:24000
Boxwell-Kremlin loams, 6 to 9 percent slopes	L2807C	575	2707332	2qxky	nd033	1985	1:24000
Kremlin, gravelly substratum-Chanta loams, 0 to 2 percent slopes	L4573A	498	2707353	2qxk2	nd033	1985	1:24000
Boxwell-Kremlin loams, 9 to 15 percent slopes	L2807D	4	2759764	2q1xs	nd033	1985	1:24000
Kremlin loam, 0 to 2 percent slopes	L2145A	2	2759757	2qxj9	nd033	1985	1:24000
Cabbart-Kremlin-Boxwell loams, 9 to 40 percent slopes, slumped	L2621F	8225	2715124	d361	nd053	2003	1:24000
Boxwell-Kremlin loams, 9 to 15 percent slopes	L2807D	5344	2715130	2q1xs	nd053	2003	1:24000
Boxwell-Kremlin loams, 3 to 6 percent slopes	L2803B	3171	2715151	2qxkx	nd053	2003	1:24000
Rhame-Kremlin-Archin complex, 6 to 15 percent slopes	L2335D	2600	2715150	2qxkf	nd053	2003	1:24000
Rhame-Bullock-Kremlin complex, 9 to 35 percent slopes	L2307F	2362	2715147	2qxjh	nd053	2003	1:24000
Kremlin-Ethridge-Gerda complex, 0 to 6 percent slopes	L3251B	1557	2715162	2qz6r	nd053	2003	1:24000
Boxwell-Kremlin loams, 6 to 9 percent slopes	L2807C	615	2715152	2qxky	nd053	2003	1:24000
Kremlin loam, 0 to 2 percent slopes	L2145A	443	2715146	2qxj9	nd053	2003	1:24000
Kremlin, gravelly substratum-Chanta loams, 0 to 2 percent slopes	L4573A	421	2715178	2qxk2	nd053	2003	1:24000
Rhame-Kremlin-Archin complex, 0 to 6 percent slopes	L2335B	50	2715149	2qz9h	nd053	2003	1:24000
Kremlin, gravelly substratum-Chanta loams, 2 to 6 percent slopes	L4573B	2865	2715962	2qxk3	nd087	1974	1:20000
Boxwell-Kremlin loams, 3 to 6 percent slopes	L2803B	612	2715919	2qxkx	nd087	1974	1:20000
Boxwell-Kremlin loams, 6 to 9 percent slopes	L2807C	472	2715920	2qxky	nd087	1974	1:20000
Kremlin, gravelly substratum-Chanta loams, 0 to 2 percent slopes	L4573A	458	2715961	2qxk2	nd087	1974	1:20000
Kremlin-Ethridge-Gerda complex, 0 to 6 percent slopes	L3251B	190	2715944	2qz6r	nd087	1974	1:20000
Rhame-Kremlin-Archin complex, 0 to 6 percent slopes	L2335B	114	2758532	2qz9h	nd087	1974	1:20000
Rhame-Kremlin-Archin complex, 6 to 15 percent slopes	L2335D	79	2758533	2qxkf	nd087	1974	1:20000
Boxwell-Kremlin loams, 9 to 15 percent slopes	L2807D	9	2758535	2q1xs	nd087	1974	1:20000
Kremlin-Belfield, low precipitation-Gerda complex, 0 to 2 percent slopes	L0627A	1	2758528	2q2mn	nd087	1974	1:20000
Kremlin-Archin complex, 0 to 3 percent slopes	KrA	4387	355760	cy64	sd063	1984	1:24000
Kremlin loam, 0 to 3 percent slopes	KoA	2361	355759	cy63	sd063	1984	1:24000
Kremlin-Rothican complex, 4 to 10 percent slopes	2363		3203113	2zbtg	wy629		1:24000
Kremlin-Pinehill complex, 4 to 25 percent slopes	9458		3203108	2zbt9	wy629		1:24000

Map of Series Extent

Approximate geographic distribution of the KREMLIN 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).