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An in-depth two-part short course designed for wetland professionals to understand basic processes and advanced problems in hydric soils, including field experience and technical standards.
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01
Gather necessary materials, including course registration form and payment details.
02
Visit the official website or designated registration portal for the Hydric Soils Short Course.
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Complete the registration form by entering personal and contact information.
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Select the course dates you wish to attend and any additional options required.
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Make payment through the provided options, ensuring to keep a receipt for confirmation.
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Who needs Hydric Soils Short Course?

01
Environmental professionals looking to enhance their understanding of hydric soils.
02
Agronomists and land managers involved in wetland delineation and assessment.
03
Students in environmental science or related fields seeking practical knowledge.
04
Regulatory agency staff who need to identify and manage wetland resources.
05
Researchers studying soil science and its implications in hydrology and ecology.
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Infiltration of rain into the topsoil usually starts immediately after the rain hits the ground and lasts until shortly after the rain stops. Percolation through the soil may take minutes or days, depending on soil type, and how wet the ground was to begin with.
The USDA - NRCS recognizes four (4) of the hydric soil indicators that are evidence of a water table at or above the soil surface for more than several weeks during the growing season. The hydric soil indicators are muck, mucky texture, gley colors and sulfidic odor.
Hydric Soil Categories : The map unit class ratings based on the hydric components present are: Hydric, Predominantly Hydric, Partially Hydric, Predominantly Nonhydric, and Nonhydric. The report also shows the total representative percentage of each map unit that the hydric components comprise.
Wetland soil characteristics form when soil is continuously saturated for periods of one or two weeks or more during the growing season. The parent material influences how the soil retains water, and the hydric (wet) soil characteristics that form.
Natural, undisturbed wetlands are usually characterized by organic soils developed over thousands of years and subtle relationships of hydrology, soils, nutrients, vegetation, and animal life.
The soil can absorb large amounts of water during rainfall, rather than letting it accumulate elsewhere and cause flooding. If you get your drinking water from a well or spring, wetland soil helps you by filtering pollutants like sediment and chemicals out of groundwater.

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The Hydric Soils Short Course is a training program designed to educate participants about the identification and classification of hydric soils, which are soils that are saturated with water for sufficient periods to develop anaerobic conditions.
Individuals involved in wetland delineation, environmental assessments, and land use planning, especially those seeking certification or accreditation in wetland science, are typically required to complete the Hydric Soils Short Course.
Participants can fill out the Hydric Soils Short Course by registering through the appropriate educational institution or organization, attending the course sessions, and completing any required assignments or evaluations to demonstrate their understanding of the material.
The purpose of the Hydric Soils Short Course is to provide essential knowledge and skills for properly identifying hydric soils, ensuring compliance with environmental regulations, and supporting sustainable land management practices.
Participants are typically required to report their attendance, completion of course materials, and any assessments or evaluations that demonstrate their understanding of hydric soils and relevant classification methods.
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