The University of Vermont (UVM) Extension’s New Farmer Project recently launched the Vermont Agriculture Land Access Database to help connect farmers seeking land and business opportunities with land and farm owners with available resources.  The database was created to provide a means for new, expanding or relocating farmers to search for land or farms for lease or sale at agricultural or fair market value, partnerships, farm transition arrangements, work exchanges and farm employment opportunities throughout and within 50 miles of Vermont.

Established farmers interested in providing access to land or transitioning their operations can list their information in the database. So can landowners not currently farming who wish to develop tenure arrangements such as lease-to-own, farm management or owner-financed farm sales.

The database may be accessed at Click on “Land Access Database” under “Quick Links.” Farm seekers may search the database or submit information about their specific requirements for land, jobs or business arrangements. Farm and landowners are encouraged to publicize available land and other resources and opportunities.

Depending on how the landowner chooses to list the information, individuals may contact the owner directly or work with UVM Extension land access specialists to learn more. In addition, these Extension consultants are available to help farmers assess their needs and explore various types of farm tenure arrangements. They also serve as a third-party facilitator for negotiations between incoming farmers and landowners. For more information, contact Ben Waterman at or .

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Important Considerations when Looking for Land


New York State’s climate is very diverse.  It is not uncommon that just 10 miles away, you could move from one microclimate to a completely different one. For example, precipitation is double the state average in the Tug Hill Plateau region and the recommended winter hardiness level changes from –5oF to –40 oF in a 100-mile distance as you travel from Wayne County to the Adirondacks.

For information about the climate in a particular area of NYS, check the Northeast Regional Climate Center website: or call 607-255-2106 .

Climatic factors that impact crop growth include: minimum temperatures, hardiness, frost-free dates, growing degree-days, precipitation, air drainage, and wind exposure.

You can learn more about these factors on the Northeast Beginning Farmer website at – look at # 3 in the New Farmer Hub, “Accessing and Evaluating Land”.

Soil Considerations

Soils vary in their properties and influence what crops will grow.  Important soil characteristics include:  texture (the percent of sand, silt or clay particles that make up the soil as depicted in the chart); pH (acidity or alkalinity of the soil); fertility (nutrients available for crop growth); and drainage. Select the best soil possible for high value specialty and agronomic crops; for hay or pasture, soil quality is slightly less critical.

Developing an understanding of the basics of soil physiology and the factors that affect plant fertility is essential for successful agricultural production.

What is soil?

In addition to air, water, and nutrients, soils provide mechanical support to growing plants. There are four major components to soil: minerals, organic matter, water, and air. The approximate composition of a soil for optimum plant growth would have the solid space made up of 45% mineral and 5% organic matter, and the remainder would have roughly 25% water and 25% air. The water and air would be contained within the pore spaces of the soil.

Soil Texture

Soil texture refers to the size of mineral particles, specifically the relative proportion of various size groups in a given soil.  This property helps determine the nutrient-supplying ability of soil solids and the supply of water and air that support plant life.

Soil texture is divided into three parts—sand, silt and clay—based on particle size.  Silt and clay soils impart a fine texture and slow water and air movement. They also have high water holding capacity due to the higher percentage of pore spaces. These are referred to as heavy soils, with clay being the heavier of the two. Clay is also the primary plant nutrient-holding mechanism in the soil.

Soil textural names are how we refer to and identify our soils.  Sandy to gravelly soils are referred to as lighter soils, as water moves through more rapidly than the heavier soils, and they have lower water holding capacities. Sandy soils contain 70% or more sand by weight.  Clay soils have at least 40% clay and may have names like sandy clay or silty clay. Loamy soils possess the desirable qualities of sand and clay without exhibiting the undesirable characteristics of extreme looseness, low water holding capacity and slow water and air movement.  Some examples would be clay loam, sand loam, silt loam, and silty clay loam.

Soil pH

Soil pH is used as a measure of its relative alkalinity or acidity.  Soil test results for pH are based on a pH scale where 7.0 is neutral, above 7.0 is alkaline and below 7.0 is acidic.

Soil pH is critical to health plant growth. It directly affects the availability of the essential nutrients to plants.  It is important to know the optimum pH for the plants to be grown.  Soil pH also affects the adaptability of plants in a given soil. Most agricultural plants prefer a slightly acidic pH of 6.4.  However there are exceptions so be familiar with the pH and nutritional needs of all the crops to be grown.

The addition of any liming (alkalinizing) or acidifying materials should always be based on the results of a reliable soil test.  Over-application of either can lead to crop injury.

Soil Organic Fraction

A good, loamy soil contains about one-half pore space (air and water) and one-half solid material.  Of this one-half solid material, 90% is composed of minerals (bits of rock).  The remaining 10% is the organic fraction.  The influence of this small part of the soil on the soil’s ability to support plant growth is significant.

The soil’s organic fraction is dynamic and is always undergoing a process of change.  The organic fraction consists of living organisms, plan and animal residues, and plan roots. Adequate levels benefit soil in many ways including; improved physical condition, increased water infiltration, improved soil tilth, decreased erosion losses, enhanced nutrient availability, and retention for plants.

Soil Compaction and Depth

Fine textured soils are more easily compacted than lighter soils, especially when they are wet.  Compaction reduces pore spaces that hold air and water.  Plant growth in compacted soils will be significantly reduced.  Operating equipment on wet soils can create problems in a field for an entire season or longer.

Sometimes a soil is referred to as being deep or shallow.  Soil depth can be defined as that depth of soil material favorable for plant root penetration.  Deep, well-drained soils of desirable texture and structure are favorable for plant growth.  Shallow, poorly drained soils are very restrictive to plant growth.

Soil Testing Services

AgroOne Services will test soil for nutrients and pH and indicate amounts of lime and fertilizer needed.  Soil samples can be taken to Dairy One’s sample pick-up points (see website) where you will fill out forms and pay for the testing. Your county extension office may also accept samples; contact them to check.  Results will be mailed in approximately 2 weeks. To contact the lab call 800-344-2697 or check:

Soil Maps

To learn about the soil types on your property, a useful tool available in almost all NY counties is the USDA-NRCS Soil Survey that consists of soil maps and descriptions of soil characteristics and capabilities.  You can find a copy of the Soil Survey at county offices of USDA-NRCS, Soil and Water District, or Cornell Cooperative Extension. Maps can also be viewed online at:

This fact sheet is part of the Guide to Farming in NY by Monika Roth et al, published by the Cornell Small Farms Program and Cornell Cooperative Extension. Fact sheets are updated once annually, so information may have changed since last revision. If you are reading a printed version of a fact sheet, compare revision date with online fact sheet publish dates to make sure you have the latest version.