Official Series Description


Lab Data Summary

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

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
128VPI0310V1985-VA023-310Groseclosen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4536306,-79.919025
128VPI0313V1985-VA023-313Groseclosen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4747972,-79.8492639
128VPI0316V1985-VA023-316Groseclosen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.5057583,-79.7798556
128VPI0336V1985-VA173-336Groseclosen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9418722,-81.51565
128VPI0338V1985-VA173-338Groseclosen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8145694,-81.6394611
128VPI0340V1985-VA173-340Groseclosen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7927028,-81.6420806
128VPI0347V1985-VA173-347Groseclosen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8968278,-81.736875
128VPI0348V1985-VA191-348Groseclosen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7209528,-82.0688444
128VPI0353V1985-VA191-353Groseclosen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.676725,-82.1495306
128VPI0354V1985-VA191-354Groseclosen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.6410222,-82.0404861
128VPI0355V1985-VA191-355Groseclosen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7517417,-81.8110667
128VPI0357V1985-VA191-357Groseclosen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.6666222,-81.9657139
128VPI0359V1985-VA191-359Groseclosen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7153667,-81.9690361
128VPI0362V1985-VA197-362Groseclosen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9408944,-81.2586528
128VPI0364V1985-VA197-364Groseclosen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9298278,-81.1699056
128VPI0365V1985-VA197-365Groseclosen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.903225,-81.1914944
147VPI0325V1985-VA163-325Groseclosen/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8065417,-79.3734639
n/a00P1392S2000VA169001Groseclose6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

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Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the GROSECLOSE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

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Select annual climate data summaries for the GROSECLOSE series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the GROSECLOSE 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 .

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Competing Series

Soil series competing with GROSECLOSE share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

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Select annual climate data summaries for the GROSECLOSE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the GROSECLOSE 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 .

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

Soil series sharing subgroup-level classification with GROSECLOSE, 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 .

Block Diagrams

No block diagrams are available.

Map Units

Map units containing GROSECLOSE 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
Groseclose silty clay loam, 12 to 20 percent slopesGsD716526457knthtn01920001:24000
Groseclose silty clay loam, 20 to 35 percent slopesGsE519526458kntjtn01920001:24000
Groseclose silty clay loam, eroded rolling phaseGl1447525134kmfttn05919541:15840
Groseclose cherty silt loam, eroded rolling phaseGc1369525127kmfltn05919541:15840
Groseclose cherty silt loam, eroded hilly phaseGb799525126kmfktn05919541:15840
Groseclose silty clay loam, eroded hilly phaseGk605525133kmfstn05919541:15840
Groseclose cherty silt loam, rolling phaseGf503525130kmfptn05919541:15840
Groseclose cherty silt loam, hilly phaseGe321525129kmfntn05919541:15840
Groseclose cherty silt loam, eroded steep phaseGd235525128kmfmtn05919541:15840
Groseclose silt loam, rolling phaseGg126525131kmfqtn05919541:15840
Groseclose silty clay, severely eroded hilly phaseGh113525132kmfrtn05919541:15840
Groseclose silt loam, rolling, 5 to 12 percent slope74C2094525334kmn8tn06320071:24000
Groseclose silt loam, hilly, 12 to 25 percent slope74D1551525335kmn9tn06320071:24000
Groseclose silt loam, steep, 25 to 40 percent slope74E326525336kmnbtn06320071:24000
Groseclose gravelly silt loam, 12 to 25 percent slopes, erodedGrD2149616896581tq73tn17919551:15840
Groseclose gravelly silty clay loam, 5 to 12 percent slopes, erodedGrC293316896591tq74tn17919551:15840
Groseclose gravelly silt loam, 25 to 50 percent slopes, erodedGrE234416896571tq72tn17919551:15840
Groseclose silt loam, 12 to 25 percent slopes, erodedGcD21257563602lxgqtn60620011:24000
Groseclose silt loam, 5 to 12 percent slopes, erodedGcC2688563601lxgptn60620011:24000
Groseclose silt loam, 25 to 60 percent slopes, erodedGcE2200563603lxgrtn60620011:24000
Groseclose silt loam, 15 to 30 percent slopes28D5702519072kf48va02319901:20000
Groseclose-Litz complex, 15 to 30 percent slopes30D5378519077kf4fva02319901:20000
Groseclose silt loam, 7 to 15 percent slopes28C4479519071kf47va02319901:20000
Chiswell-Groseclose complex, 30 to 60 percent slopes11E3698519036kf33va02319901:20000
Chiswell-Groseclose complex, 15 to 30 percent slopes11D2087519035kf32va02319901:20000
Groseclose-Litz complex, 7 to 15 percent slopes30C1892519076kf4dva02319901:20000
Groseclose-Litz complex, 30 to 45 percent slopes30E1671519078kf4gva02319901:20000
Chiswell-Groseclose complex, 7 to 15 percent slopes11C1224519034kf31va02319901:20000
Groseclose silty clay loam, 15 to 30 percent slopes, severely eroded29D735519074kf4bva02319901:20000
Groseclose silty clay loam, 7 to 15 percent slopes, severely eroded29C418519073kf49va02319901:20000
Groseclose silt loam, 2 to 7 percent slopes28B290519070kf46va02319901:20000
Berks-Groseclose complex, 7 to 15 percent slopes2C8023517105kc2tva12119801:15840
Groseclose and Poplimento soils, 7 to 15 percent slopes16C7327517083kc23va12119801:15840
Groseclose and Poplimento soils, 15 to 25 percent slopes16D5828517084kc24va12119801:15840
Groseclose and Poplimento soils, 25 to 60 percent slopes16E5785517085kc25va12119801:15840
Groseclose and Poplimento soils, 2 to 7 percent slopes16B4883517082kc22va12119801:15840
Berks-Groseclose complex, 2 to 7 percent slopes2B1649517104kc2sva12119801:15840
Groseclose-Urban land complex, 2 to 7 percent slopes18B1486517087kc27va12119801:15840
Groseclose-Urban land complex, 7 to 15 percent slopes18C1404517088kc28va12119801:15840
Groseclose and Poplimento gravelly soils, 7 to 15 percent slopes17C1197517086kc26va12119801:15840
Groseclose-Urban land complex, 15 to 25 percent slopes18D661517089kc29va12119801:15840
Rayne-Berks-Groseclose complex, 30 to 60 percent slopes28F14588521277khfdva15519811:15840
Groseclose and Poplimento silt loams, 7 to 15 percent slopes13C8781521243khd9va15519811:15840
Groseclose and Poplimento silt loams, 15 to 30 percent slopes13D6332521244khdbva15519811:15840
Groseclose and Poplimento silt loams, 2 to 7 percent slopes13B4284521242khd8va15519811:15840
Groseclose-Urban land complex, 7 to 15 percent slopes12C1527521241khd7va15519811:15840
Groseclose-Urban land complex, 2 to 7 percent slopes12B897521240khd6va15519811:15840
Groseclose-Litz complex, 25 to 35 percent slopes25E948520257kgchva16119901:24000
Groseclose-Litz complex, 2 to 15 percent slopes25C728520255kgcfva16119901:24000
Groseclose-Litz complex, 15 to 25 percent slopes25D676520256kgcgva16119901:24000
Groseclose silt loam, 7 to 15 percent slopes24C675520251kgc9va16119901:24000
Groseclose silt loam, 15 to 25 percent slopes24D364520253kgccva16119901:24000
Groseclose silt loam, 25 to 35 percent slopes24E231520254kgcdva16119901:24000
Groseclose silt loam, 15 to 25 percent slopes27D455025148002qdb8va16320101:24000
Groseclose silt loam, 8 to 15 percent slopes27C390725147992qdb7va16320101:24000
Litz-Chiswell-Groseclose complex, 35 to 55 percent slopes33F255125148082qdbqva16320101:24000
Groseclose-Needmore complex, 25 to 35 percent slopes28E205825148012qdb9va16320101:24000
Litz-Chiswell-Groseclose complex, 15 to 35 percent slopes33E201925148072qdbpva16320101:24000
Groseclose-Needmore-Urban land complex, 0 to 15 percent slopes29C124825148022qdbbva16320101:24000
Litz-Chiswell-Groseclose complex, 8 to 15 percent slopes33C65325148062qdbnva16320101:24000
Groseclose silt loam, 3 to 8 percent slopes27B62625147982qdb6va16320101:24000
Berks-Groseclose complex, 15 to 35 percent slopes3D268016718251t3nvva16720061:24000
Berks-Groseclose complex, 8 to 15 percent slopes3C58716718241t3ntva16720061:24000
Groseclose-Carbo silty clay loams, 15 to 25 percent slopes, severely eroded23D3026778062v3msva16920031:24000
Berks-Groseclose complex, 15 to 35 percent slopes4D1066778012v3l5va16920031:24000
Groseclose-Carbo silty clay loams, karst, 8 to 15 percent slopes, severely eroded24C791778063v3mtva16920031:24000
Chiswell-Litz-Groseclose complex, 25 to 65 percent slopes10E10120518602kdn3va17319951:24000
Chiswell-Litz-Groseclose complex, 15 to 25 percent slopes10D3955518601kdn2va17319951:24000
Chiswell-Litz-Groseclose complex, 7 to 15 percent slopes10C1716518600kdn1va17319951:24000
Groseclose silt loam, 15 to 25 percent slopes26D223522004kj5vva18519961:24000
Groseclose silt loam, 25 to 35 percent slopes26E127522005kj5wva18519961:24000
Groseclose silt loam, 7 to 15 percent slopes26C80522003kj5tva18519961:24000
Groseclose silt loam, 2 to 7 percent slopes26B67522002kj5sva18519961:24000
Litz-Groseclose complex, 25 to 75 percent slopes28E2652519341kfdyva19119981:15840
Litz-Groseclose complex, 15 to 25 percent slopes28D760519340kfdxva19119981:15840
Litz-Groseclose complex, 7 to 15 percent slopes28C246519339kfdwva19119981:15840
Chiswell-Groseclose-Litz complex, 30 to 60 percent slopes4E22681518990kf1mva19719881:15840
Chiswell-Groseclose-Litz complex, 15 to 30 percent slopes4D12601518989kf1lva19719881:15840
Chiswell-Groseclose-Litz complex, 7 to 15 percent slopes4C9258518988kf1kva19719881:15840
Groseclose silt loam, 15 to 35 percent slopes95D20725568722r7dgva6061:24000
Groseclose silt loam, 3 to 15 percent slopes95C2025568732r7dfva6061:24000
Groseclose-Litz complex, 15 to 30 percent slopes14E8731740512z3dqva8501:24000
Groseclose silt loam, 15 to 30 percent slopes13E3031740502z3dpva8501:24000
Chiswell-Groseclose complex, 15 to 30 percent slopes2E1831740342z3d4va8501:24000
Groseclose-Litz complex, 7 to 15 percent slopes14C1331740522z3drva8501:24000
Chiswell-Groseclose complex, 7 to 15 percent slopes2C431740352z3d5va8501:24000

Map of Series Extent

Approximate geographic distribution of the GROSECLOSE 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 .