Soil scientists sampling Tomlin soil (Iredell County, NC)
A soil scientist is a person who is qualified to evaluate and interpret soils and soil-related data for the purpose of understanding soil resources as they contribute to not only agricultural production, but as they affect environmental quality and as they are managed for protection of human health and the environment. The university degree should be in Soil Science, or closely related field (i.e., natural resources, environmental science, earth science, etc.) and include sufficient soils-related course work so the Soil Scientist has a measurable level of understanding of the soil environment, including soil morphology and soil forming factors, soil chemistry, soil physics, and soil biology, and the dynamic interaction of these areas.
TOMLIN SERIES
Depth class: Very deep
Agricultural drainage class: Well drained
Saturated hydraulic conductivity class: Moderately high
Landform: Piedmont uplands
Landform position: Broad ridges and side slopes
Parent material: Residuum weathered from diorite, gabbro, diabase, and/or gneiss
Slope: 2 to 25 percent
Taxonomic classification: Fine, kaolinitic, mesic Rhodic Kanhapludults
RANGE IN CHARACTERISTICS:
Depth to top of argillic or kandic horizon: 2 to 20 inches
Depth to base of argillic or kandic horizon: More than 25 inches
Depth to bedrock: Greater than 80 inches
Depth to seasonal high water table: Greater than 72 inches
Rock Fragment Content: 0 to 35 percent in the A and E horizons and 0 to 15 percent in the B and C horizons; mostly gravel and cobbles
Soil Reaction: Very strongly acid to moderately acid throughout, unless limed.
Mica content: 0 to 20 percent, by volume mica flakes in the A, B, and 0 to 50 percent by volume in the BC and C horizon.
For more information about Describing and Sampling soils, visit;
www.nrcs.usda.gov/Internet/FSE_DOCUMENTS/nrcs142p2_052523...
For more information about Soil Taxonomy, visit;
sites.google.com/site/dinpuithai/Home
Soil scientists sampling Tomlin soil (Iredell County, NC)
A soil scientist is a person who is qualified to evaluate and interpret soils and soil-related data for the purpose of understanding soil resources as they contribute to not only agricultural production, but as they affect environmental quality and as they are managed for protection of human health and the environment. The university degree should be in Soil Science, or closely related field (i.e., natural resources, environmental science, earth science, etc.) and include sufficient soils-related course work so the Soil Scientist has a measurable level of understanding of the soil environment, including soil morphology and soil forming factors, soil chemistry, soil physics, and soil biology, and the dynamic interaction of these areas.
TOMLIN SERIES
Depth class: Very deep
Agricultural drainage class: Well drained
Saturated hydraulic conductivity class: Moderately high
Landform: Piedmont uplands
Landform position: Broad ridges and side slopes
Parent material: Residuum weathered from diorite, gabbro, diabase, and/or gneiss
Slope: 2 to 25 percent
Taxonomic classification: Fine, kaolinitic, mesic Rhodic Kanhapludults
RANGE IN CHARACTERISTICS:
Depth to top of argillic or kandic horizon: 2 to 20 inches
Depth to base of argillic or kandic horizon: More than 25 inches
Depth to bedrock: Greater than 80 inches
Depth to seasonal high water table: Greater than 72 inches
Rock Fragment Content: 0 to 35 percent in the A and E horizons and 0 to 15 percent in the B and C horizons; mostly gravel and cobbles
Soil Reaction: Very strongly acid to moderately acid throughout, unless limed.
Mica content: 0 to 20 percent, by volume mica flakes in the A, B, and 0 to 50 percent by volume in the BC and C horizon.
For more information about Describing and Sampling soils, visit;
www.nrcs.usda.gov/Internet/FSE_DOCUMENTS/nrcs142p2_052523...
For more information about Soil Taxonomy, visit;
sites.google.com/site/dinpuithai/Home