Range Production (Unfavorable Year)

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Gervais Terry
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name 1A Fluvaquents-Udifluvents complex, 0 to 3 45, frequently flooded 2A Geneseo silty clay loam, 0 to 3 3A Hemlock silty clay loam, 0 to 3 4A Naples Creek silty clay loam, 0 to 3 5A Wayland soils

1 name 1A Fluvaquents-Udifluvents complex, 0 to 3 45, frequently flooded 2A Geneseo silty clay loam, 0 to 3 3A Hemlock silty clay loam, 0 to 3 4A Naples Creek silty clay loam, 0 to 3 5A Wayland soils complex, 0 to 3, 60 frequently flooded 12D Rockrift channery silt loam, 15 to F Rock outcrop-arnot complex, 35 to 80, extremely stony 14D Cadosia channery silt loam, 15 to A Guyanoga channery silt loam, fan, 0 to 3 15B Guyanoga channery silt loam, fan, 3 to 8 16A Almond channery silt loam, 0 to B Almond channery silt loam, 3 to C Almond channery silt loam, 8 to A Homer fine sandy loam, 0 to 3 19A Fine-loamy, mixed, active, mesic, Typic Argiaquolls, 80 0 to 3 20A Atherton and Fine-loamy, mixed, active, mesic, Typic Argiaquolls, 0 to 3 24A Howard gravelly loam, 0 to B Howard gravelly loam, 3 to C Howard gravelly loam, 8 to D Howard soils, 15 to A Chenango gravelly loam, 0 to 3 25B Chenango gravelly loam, 3 to 8 25C Chenango gravelly loam, 8 to 15 25D Chenango gravelly loam, 15 to 25 25E Chenango gravelly loam, 25 to 35 26B Chenango channery loam, fan, 3 to B Castile gravelly silt loam, 3 to A Collamer silt loam, 0 to B Collamer silt loam, 3 to C Collamer silt loam, 8 to D Collamer silt loam, 15 to 25 32A Dunkirk fine sandy loam, 0 to 3 32B Dunkirk fine sandy loam, 3 to 8 33A Dunkirk silt loam, 0 to 3 33B Dunkirk silt loam, 3 to 8 33C Dunkirk silt loam, 8 to 15 33D Dunkirk silt loam, 15 to 25 33E Dunkirk silt loam, 25 to 35 34A Lakemont silty clay loam, 0 to A Odessa silt loam, 0 to 3 35B Odessa silty clay loam, 3 to 8 Page 1 of 6

2 name 36A Schoharie silty clay loam, 0 to 3 36B Schoharie silty clay loam, 3 to 8 36C Schoharie silty clay loam, 8 to 15 36D Schoharie silty clay loam, 15 to 25 36E Schoharie silty clay loam, 25 to 45 37A Schoharie silt loam, 0 to 3 37B Schoharie silt loam, 3 to 8 38A Niagara silt loam, 0 to B Niagara silt loam, 3 to A Rhinebeck silty clay loam, 0 to 3 41A Aeric Epiaquepts, 0 to A Canandaigua silt loam, 0 to 3 44A Canandaigua mucky silt loam, 0 to 3 45A Fonda mucky silt loam, 0 to A Galen fine sandy loam, 0 to 3 46B Galen fine sandy loam, 3 to 8 48A Arkport fine sandy loam, 0 to B Arkport fine sandy loam, 3 to C Arkport fine sandy loam, 8 to D Arkport fine sandy loam, 15 to 25 49B Arkport loamy fine sand, 3 to D Arkport loamy fine sand, 15 to E Arkport loamy fine sand, 25 to 35 49F Arkport loamy fine sand, 35 to 55 50B Dunkirk-Arkport complex, 3 to C Dunkirk-Arkport complex, 8 to D Dunkirk-Arkport complex, 15 to A Lamson fine sandy loam, 0 to 3 54A Lamson mucky fine sandy loam, 0 to 3 56A Elnora loamy fine sand, 0 to 3 58B Colonie loamy fine sand, 3 to C Colonie loamy fine sand, 8 to B Mardin channery silt loam, 3 to C Mardin channery silt loam, 8 to D Mardin channery silt loam, 15 to E Mardin channery silt loam, 25 to B Langford channery silt loam, 3 to 8 63C Langford channery silt loam, 8 to 15 pecent 63D Langford channery silt loam, 15 to 25 64B Langford-Erie channery silt loams, 3 to A Lyons silt loam, 0 to 3 68A Volusia channery silt loam, 0 to B Volusia channery silt loam, 3 to 8 68C Volusia channery silt loam, 8 to 15 Page 2 of 6

3 name 68D Volusia channery silt loam, 15 to A Erie channery silt loam, 0 to B Erie channery silt loam, 3 to C Erie channery silt loam, 8 to A Darien silt loam, 0 to B Darien silt loam, 3 to C Darien silt loam, 8 to A Darien-Ilion silt loams, 0 to B Darien-Ilion silt loams, 3 to B Gretor silt loam, 3 to C Gretor silt loam, 8 to D Gretor channery silt loam, 15 to 25 76B Orpark silt loam, 3 to C Orpark silt loam, 8 to D Orpark channery silt loam, 15 to 25 77A Chippewa silt loam, 0 to 3 77B Chippewa silt loam, 3 to 8 82B Manlius channery silt loam, 3 to C Manlius channery silt loam, 8 to D Manlius channery silt loam, 15 to A Palms muck, 0 to A Carlisle muck, 0 to A Edwards muck, 0 to A Martisco muck, 0 to A Saprists, 0 to 3, inundated A Honeoye loam, 0 to B Honeoye loam, 3 to C Honeoye loam, 8 to D Honeoye loam, 15 to E Honeoye loam, 25 to A Honeoye loam, 0 to 3, lower clay 98 surface 104B Honeoye loam, 3 to 8, lower clay 98 surface 104C Honeoye loam, 8 to 15, lower clay 98 surface 106B Danley-Lansing complex, 3 to B Conesus-Lansing loams, 3 to C Lansing silt loam, 8 to D Lansing silt loam, 15 to E Lansing silt loam, 25 to B Ontario fine sandy loam, 3 to 8 112C Ontario fine sandy loam, 8 to D Ontario fine sandy loam, 15 to E Ontario fine sandy loam, 25 to B Ontario gravelly loam, 3 to C Ontario gravelly loam, 8 to Page 3 of 6

4 name 114D Ontario gravelly loam, 15 to B Ontario loam, 3 to 8 116C Ontario loam, 8 to D Ontario loam, 15 to F Ontario, Honeoye and Lansing soils, 35 to E Palmyra and Howard soils, 25 to A Palmyra cobbly loam, 0 to B Palmyra cobbly loam, 3 to A Palmyra fine sandy loam, 0 to 3 124B Palmyra fine sandy loam, 3 to 8 126A Palmyra gravelly loam, 0 to B Palmyra gravelly loam, 3 to C Palmyra gravelly loam, 8 to D Palmyra gravelly loam, 15 to A Palmyra gravelly sandy loam, 0 to 3 128B Palmyra gravelly sandy loam, 3 to 8 128C Palmyra gravelly sandy loam, 8 to A Farmington loam, 0 to 3 130B Farmington loam, 3 to 8 132A Galoo loam, 0 to 3, rocky B Galoo loam, 3 to 8, rocky A Camillus silt loam, 0 to B Camillus silt loam, 3 to C Willdin-Norchip complex, 3 to B Valois gravelly loam, 3 to C Valois gravelly loam, 8 to D Valois gravelly loam, 15 to E Valois gravelly loam, 25 to B Valois gravelly loam, cool, 3 to C Valois gravelly loam, cool, 8 to D Valois gravelly loam, cool, 15 to E Valois gravelly loam, cool, 25 to B Willdin channery silt loam, 3 to C Willdin channery silt loam, 8 to D Willdin channery silt loam, 15 to A Ontusia channery silt loam, 0 to B Ontusia channery silt loam, 3 to C Ontusia channery silt loam, 8 to D Ontusia channery silt loam, 15 to C Lordstown-Manlius-Towerville complex, 8 to D Lordstown-Manlius-Towerville complex, 15 to 25, very stony 171E Lordstown-Manlius-Towerville complex, 25 to 35, extremely stony Page 4 of 6

5 name 171F Lordstown-Manlius-Towerville complex, 35 to 80, extremely stony 177A Norchip silt loam, 0 to 3 177B Norchip silt loam, 3 to 8 181B Mongaup-Ischua complex, 3 to C Mongaup-Ischua complex, 8 to D Mongaup-Ischua complex, 15 to 25, 45 very stony 181E Mongaup-Ischua complex, 25 to 35, 45 extremely stony 182B Mongaup channery loam, 3 to C Mongaup channery loam, 8 to A Lima loam, 0 to B Lima loam, 3 to 8 201C Lima loam, 8 to A Lima loam, 0 to 3, lower clay surface 204B Lima loam, 3 to 8, lower clay surface A Phelps gravelly silt loam, 0 to B Phelps gravelly silt loam, 3 to A Nuhi silt loam, 0 to B Aurora-Angola silt loams, 3 to C Aurora-Angola silt loams, 8 to D Aurora-Angola silt loams, 15 to B Aurora silt loam, 3 to C Aurora silt loam, 8 to D Aurora silt loam, 15 to B Cazenovia silt loam, 3 to C Cazenovia silt loam, 8 to D Cazenovia silt loam, 15 to B Cayuga silt loam, 3 to C Cayuga silt loam, 8 to D Cayuga silt loam, 15 to A Kendaia loam, 0 to 3 304B Kendaia loam, 3 to 8 342A Angola silt loam, 0 to 3 356A Ovid silt loam, 0 to B Ovid silt loam, 3 to B Ovid silty clay loam, 3 to C Ovid silty clay loam, 8 to A Udorthents, loamy, 0 to D Udorthents, refuse substratum. 0 to 25 PG Pits, gravel and sand 75 PQ Pits, quarry 80 W Water 100 Page 5 of 6

6 Options Attribute Name: Total range production is the amount of vegetation that can be expected to grow annually in a well managed area that is supporting the potential natural plant community. It includes all vegetation, whether or not it is palatable to grazing animals. It includes the current year's growth of leaves, twigs, and fruits of woody plants. It does not include the increase in stem diameter of trees and shrubs. It is expressed in pounds per acre of air-dry vegetation. In an unfavorable year, growing conditions are well below average, generally because of low available soil moisture. Yields are adjusted to a common of air-dry moisture content. In areas that have similar climate and topography, differences in the kind and amount of vegetation produced on rangeland are closely related to the kind of soil. Effective management is based on the relationship between the soils and vegetation and water. Aggregation is the process by which a set of component attribute values is reduced to a single value to represent the map unit as a whole. A map unit is typically composed of one or more "components". A component is either some type of soil or some nonsoil entity, e.g., rock outcrop. The components in the map unit name represent the major soils within a map unit delineation. Minor components make up the balance of the map unit. Great differences in soil properties can occur between map unit components and within short distances. Minor components may be very different from the major components. Such differences could significantly affect use and management of the map unit. Minor components may or may not be documented in the database. The results of aggregation do not reflect the presence or absence of limitations of the components which are not listed in the database. An on-site investigation is required to identify the location of individual map unit components. For each of a map unit's components, a corresponding composition is recorded. A composition of 60 indicates that the corresponding component typically makes up approximately 60% of the map unit. Percent composition is a critical factor in some, but not all, aggregation methods. For the attribute being aggregated, the first step of the aggregation process is to derive one attribute value for each of a map unit's components. From this set of component attributes, the next step of the aggregation process derives a single value that represents the map unit as a whole. Once a single value for each map unit is derived, a thematic map for soil map units can be generated. Aggregation must be done because, on any soil map, map units are delineated but components are not. The aggregation method "Dominant Component" returns the attribute value associated with the component with the highest composition in the map unit. If more than one component shares the highest composition, the corresponding "tie-break" rule determines which value should be returned. The "tie-break" rule indicates whether the lower or higher attribute value should be returned in the case of a composition tie. The result returned by this aggregation method may or may not represent the dominant condition throughout the map unit. The tie-break rule indicates which value should be selected from a set of multiple candidate values, or which value should be selected in the event of a composition tie. This option indicates that a null value for a component should be converted to zero before aggregation occurs. This will be done only if a map unit has at least one component where this value is not null. Page 6 of 6

Depth to a Selected Soil Restrictive Layer

Depth to a Selected Soil Restrictive Layer 1A 2A 3A 4A 5A 12D 13F 14D 15A 15B 16A 16B 16C 18A 19A 20A 24A 24B 24C 24D 25A 25B 25C 25D 25E 26B 27B 31A 31B 31C 31D 32A 32B 33A 33B 33C 33D 33E 34A 35A 35B Fluvaquents-Udifluvents complex, 0 to 3, frequently