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  1. This field guide is one section of a Field Guide for the Soils of Western Canada, which is currently under development by the three authors. Our intent for the field guide is two-‐fold: 1) to simplify the use of the Canadian System of Soil Classification in the field and 2) to allow field testing of a new soil order for Anthroposolic soils ...

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  2. horizons indicate the magnitude of that expression. Master Horizons and Layers O horizons – Organic soil materials (other than Lim-nic materials). Any mineral content is commonly a small percentage by volume and < 80% by weight. A horizons – Mineral soil formed at the surface or be-low an O horizon, that exhibits little or no remnant rock

  3. soilsofcanada.ca › soil-formation › horizonsHorizons - Soils of Canada

    The horizon description system begins by splitting soil horizons into two distinct groups: organic and mineral horizons. Organic horizons are those that contain 17% or more organic carbon; mineral horizons have less than 17% organic carbon. The major symbols used in describing mineral soil layers in Canada are shown in the following tables.

  4. By following the steps outlined in this lecture and applying the master horizon and suffix designations, soil scientists and other professionals can create standardized, informative soil profile descriptions. These descriptions serve as the foundation for many aspects of soil science, including mapping, research, and management decisions.

  5. All these properties are used to define types of soil horizons. Soil scientists use the capital letters O, A, B, C, and E to identify the master horizons, and lowercase letters for distinctions of these horizons. Most soils have three major horizons -- the surface horizon (A), the subsoil (B), and the substratum (C).

  6. The horizon description system begins by splitting soil horizons into two distinct groups: mineral and organic horizons. Organic horizons are those which contain 17% or more organic carbon by weight; mineral horizons have less than 17% organic carbon by weight. The three master mineral horizons are the A, B, and C horizons.

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  8. Also NOTE: due to depth restrictions in 1. Above, organic soils (Histosols) do not have histic epipedons. Also NOTE: a “folistic” horizon is similar to the histic, but is saturated less than 30 days/year 2. An “A” horizon is mollic if the following conditions are met: 1. Structure is not massive or consistence is not hard when dry; 2.

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