Soil Testing in Concord, New Hampshire

Soil Testing in Concord, New Hampshire

Complete Guide to New Hampshire Soil Types: 2025 Agricultural and Land Management Resource

New Hampshire's "Granite State" geology and glacial history have created diverse soil conditions from acidic mountain spodosols to fertile river valley alluviums, requiring specialized management approaches for successful agriculture and land stewardship in northern New England.

Complete Guide to New Hampshire Soil Types: 2025 Agricultural and Land Management Resource

New Hampshire features eight distinct soil types dominated by acidic Spodosols and glacial till soils, with limited prime farmland (125,000 acres) requiring careful pH management and soil amendments for successful agricultural production in the challenging granite-based landscape.

New Hampshire, known for its picturesque landscapes and rugged terrain, is home to a diverse range of soil types. These soils play a critical role in the state's agriculture, forestry, and overall ecosystem. Understanding the soil types in New Hampshire is essential for anyone engaged in farming, gardening, or land management within the state. This article provides an in-depth look at the different soil types found in New Hampshire, their characteristics, distribution, and suitability for various uses.

NRCS Soil Survey and Classification Framework

The USDA Natural Resources Conservation Service conducts comprehensive soil surveys throughout New Hampshire as part of the National Cooperative Soil Survey. Through detailed soil mapping and data collection, NRCS provides critical information about soil characteristics, properties, limitations, and potentials for land use planning and conservation efforts.

NRCS soil surveys contain information in the form of detailed soil maps, data tables, and text narratives that can be used in land-planning programs, with predictions of soil behavior for selected land uses and highlights of limitations and hazards inherent in the soil.

Primary Soil Orders of New Hampshire

Spodosols: Dominant Forest Floor Specialists

Spodosols are the most widespread soil type in New Hampshire, particularly in areas with significant cover of pine and spruce forests. These soils are characterized by a distinct subsoil layer rich in organic matter, iron, and aluminum, which is typically dark in color and forms under coniferous forest conditions.

pH levels in Spodosols range from 4.0 to 5.5, making them highly acidic. The sandy to loamy texture provides high drainage capacity, which can lead to nutrient leaching. These soils are typically low in nutrients, particularly in the upper layers, though organic matter accumulation in the subsoil can provide moderate nutrient reserves.

For agricultural use, Spodosols require significant management including liming and fertilization to improve productivity. They are naturally better suited for forestry and specialized horticultural crops like cranberries that tolerate acidic conditions.

Inceptisols: Young Developing Soils

Inceptisols are younger soils found throughout New Hampshire, particularly in the southern and central regions. These soils are less developed than Spodosols and are often found in areas with moderate to steep slopes, representing early stages of soil formation.

pH levels in Inceptisols range from 5.0 to 6.5, depending on parent material and local conditions. Texture varies from sandy to clayey with moderate to high drainage capacity. These soils generally have higher nutrient content compared to Spodosols, containing more organic matter and exhibiting greater natural fertility.

Inceptisols are more suitable for agriculture, particularly for growing vegetables, fruits, and pasture crops. They support mixed hardwood forests and are commonly used for both forestry and agricultural applications.

Alfisols: Premium Fertile Soils

Alfisols represent some of the most fertile soils found in New Hampshire, though they are less common than other soil types. These soils are typically found in the southern part of the state and are often associated with deciduous forest ecosystems.

pH levels in Alfisols range between 5.5 and 7.0, making them less acidic and more conducive to agricultural use. The typically loamy texture provides a balanced mixture of sand, silt, and clay with moderate to high water-holding capacity.

Alfisols are rich in essential nutrients like calcium, magnesium, and potassium, with higher organic matter content compared to other New Hampshire soils. Their natural fertility makes them excellent for diverse agricultural activities including grain cultivation, vegetables, fruits, and pasture crops.

Histosols: Organic-Rich Wetland Soils

Histosols are organic-rich soils found in wetland areas such as bogs, marshes, and swamps. In New Hampshire, these soils are more localized, occurring in low-lying areas throughout the state where water accumulation promotes organic matter preservation.

pH levels in Histosols range from 4.0 to 7.0, depending on the decomposition state of organic matter and local hydrology. These soils are composed primarily of decomposed plant material, making them very rich in organic matter with characteristic spongy, waterlogged texture.

While Histosols are high in organic matter and can be very fertile, their waterlogged nature limits conventional agricultural use. They are often preserved for ecological value as wetlands supporting diverse plant and animal species, though some are drained for specialized crops like cranberries.

Specialized New Hampshire Soil Types

Glacial Till Soils: Ice Age Legacy

Much of New Hampshire's landscape reflects glacial activity during the last Ice Age, resulting in widespread glacial till soils throughout the state. These soils consist of clay, sand, gravel, and boulders deposited by retreating glaciers, creating the characteristic rocky terrain of the region.

pH levels in glacial till soils typically range from 5.0 to 6.5, varying based on till composition. Texture varies widely from sandy to clayey, often containing significant amounts of gravel and stones that complicate cultivation.

These soils are generally low in nutrients and organic matter due to glacial action stripping topsoil. Their stony nature and poor fertility make them challenging for agriculture, better suited for pasture, forestry, and hardy crops that tolerate rocky conditions.

Alluvial Soils: River Valley Productivity

Alluvial soils occur in New Hampshire's river valleys, particularly along the Connecticut River and its tributaries. These soils form through sediment deposition carried by rivers and represent some of the most fertile agricultural land in the state.

pH levels in alluvial soils typically range from 6.0 to 7.0, providing neutral to slightly acidic conditions favorable for crop production. The loamy texture offers good balance of sand, silt, and clay with excellent water-holding capacity.

Rich in nutrients, particularly in surface layers where organic matter accumulates, alluvial soils support intensive agriculture including vegetables, grains, fruits, pasture, and hay production.

Granite-Derived Soils: Bedrock Foundation

As the "Granite State," New Hampshire's geology is dominated by granite bedrock, resulting in widespread granite-derived soils throughout the state, particularly in mountainous regions. This parent material significantly influences soil chemistry and fertility.

pH levels in granite-derived soils are typically acidic, ranging from 4.5 to 6.0. Texture is usually sandy or loamy with coarse characteristics and low water-holding capacity. These soils are generally low in nutrients and organic matter since granite provides limited fertility.

Agricultural use is challenging due to acidity, low fertility, and coarse texture. These soils are naturally better suited for forestry, particularly pine and spruce cultivation adapted to acidic, low-nutrient conditions.

Soil Testing and Management Resources

University of New Hampshire Extension Services

UNH Cooperative Extension provides comprehensive soil analysis and fertilizer recommendations to farmers, homeowners, and researchers. The soil testing service, dating back to 2005, processes more than 3,000 samples annually with recommendations based on latest research and specific to crops being grown.

New Hampshire soils are naturally very acidic (pH 4.5-5.5), while most plants prefer pH range of 6.0-6.5. Exceptions include acid-loving plants such as blueberries, azaleas, rhododendrons, mountain laurel, and holly, which prefer pH 4.5-5.5. Lime is most commonly used to raise soil pH levels.

Standard soil testing includes pH analysis, organic matter content, extractable nutrients (calcium, magnesium, potassium, phosphorus), and lead screening for home gardens. Turnaround time is approximately three weeks with recommendations for lime and fertilizers based upon intended crops.

Soil Sampling Best Practices

Proper soil sampling involves taking samples from 6-8 spots in each area to be tested, avoiding areas with obvious differences in soil type, drainage, or plant growth. Mix samples together to create representative samples from each area, taking samples at 6-inch depth for gardens, 6-8 inches for trees and shrubs, and 3-4 inches for lawns.

Agricultural Challenges and Prime Farmland

Limited Prime Farmland Resources

New Hampshire has significantly less prime farmland compared to neighboring states. USDA-NRCS data shows New Hampshire has only 125,000 acres of prime farmland soils compared to Vermont's 382,000 acres. This disparity reflects New Hampshire's challenging soil conditions, mountainous terrain, and granite-based geology.

Prime farmland soils are characterized by moderate pH, fine-textured particles, infrequent flooding during growing season, depth to bedrock of 40 inches or more, gentle slopes, and minimal surface stones. New Hampshire's acidic, rocky, and often shallow soils limit prime agricultural land availability.

Soil Management Strategies

Successful agriculture in New Hampshire requires strategic soil management approaches. Liming is often necessary to raise pH to suitable levels for crop growth. Organic matter additions through compost, manure, or cover crops improve soil structure, nutrient retention, and biological activity.

For acidic soils, targeted fertilization addresses nutrient deficiencies common in leached, low-pH conditions. Proper drainage management prevents waterlogging in areas with glacial till or high clay content, while erosion control protects topsoil on sloped terrain.

Conservation and Sustainability

NRCS Conservation Programs

Through USDA Service Centers across the state, NRCS provides technical and financial assistance to agricultural producers and forest landowners. Conservation programs help address resource concerns including soil health, water quality, erosion control, and habitat enhancement.

New Hampshire is nearly 85% forested, and NRCS regularly works with forest landowners to address resource concerns on their lands through conservation practices that protect soil resources while maintaining forest productivity.

Sustainable Land Management

Understanding New Hampshire's soil diversity enables sustainable land use decisions that work with natural soil characteristics rather than against them. Matching crops and management practices to soil capabilities ensures long-term productivity while protecting environmental resources.

Conservation practices such as cover cropping, reduced tillage, nutrient management, and erosion control help maintain soil health and fertility in New Hampshire's challenging soil environment.

Conclusion

New Hampshire's diverse landscape is reflected in its wide range of soil types, each with unique characteristics and challenges. Understanding these soils is crucial for anyone involved in agriculture, forestry, or land management in the state. From acidic Spodosols and glacial till soils to fertile alluvial and Alfisol soils, each soil type offers different opportunities and limitations for land use.

By understanding and managing these soils effectively through proper testing, amendment, and conservation practices, New Hampshire's landowners can ensure sustainable and productive use of their land for generations to come. The state's soil testing resources, conservation programs, and technical assistance provide essential support for successful soil management in this challenging but rewarding landscape.

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Understanding Soil Health

Assessing soil health involves looking at physical, chemical, and biological components.

Soil health is a fundamental concept that underpins the success of agriculture, gardening, and land management practices. It refers to the overall well-being and vitality of the soil ecosystem, encompassing physical, chemical, and biological aspects. Understanding soil health is crucial for maintaining sustainable and productive landscapes while also contributing to environmental conservation.

  1. Physical
    The physical properties of soil play a critical role in its health. These properties include soil texture, structure, compaction, and water-holding capacity. Soil texture refers to the proportions of sand, silt, and clay particles in the soil. A balanced texture allows for adequate water drainage and retention, preventing waterlogging and drought stress. Soil structure influences root penetration, aeration, and nutrient movement. Healthy soil structure promotes a friable and well-drained medium for plant growth.
  2. Chemical
    Soil chemistry directly affects nutrient availability and plant growth. Key chemical factors include soil pH, nutrient content, and the presence of contaminants. Soil pH measures the soil's acidity or alkalinity and profoundly influences nutrient uptake by plants. Nutrient content, including macronutrients like nitrogen, phosphorus, and potassium, must be in balance to support healthy plant growth. Monitoring and maintaining proper nutrient levels through fertilization are essential for maximizing crop yields and preventing nutrient deficiencies.
  3. Biological
    The biological component of soil health pertains to the diverse array of microorganisms, insects, and other organisms that inhabit the soil ecosystem. These organisms play crucial roles in nutrient cycling, organic matter decomposition, and disease suppression. Soil microorganisms break down organic matter, releasing nutrients that are subsequently made available to plants. A rich and diverse soil microbiome contributes to enhanced nutrient availability and plant resilience against diseases.

Our Soil Tests

We provide a range of soil tests from basic chemistry, to texture/infiltration rate, all the way to biology.

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Basic Soil Health Test

The Basic Soil Health Test is an excellent starting point for understanding your soil's condition. It offers a comprehensive analysis encompassing pH levels, nutrient content, CEC (Cation Exchange Capacity), salts, and organic matter. This budget-friendly test is ideal for identifying potential soil health issues and establishing a solid foundation for further management.

Full Chemistry Test

Our Full Chemistry Test provides a detailed assessment of your soil's quality, guiding you towards healthy and sustainable soil management practices. Through an extensive analysis, we examine macro and micronutrient levels, pH, CEC, organic matter, and salinity. This comprehensive understanding empowers us to create tailored recommendations for soil amendments and treatments, optimized for the specific plants you intend to cultivate. By optimizing your soil's chemistry, you can expect to foster more robust and vibrant plant growth.

Complete Soil Health Test

Uncover a deeper understanding of your soil's health with the Complete Soil Health Test. This comprehensive analysis goes beyond the basics, measuring nutritional factors and examining soil texture. It covers macro and micronutrients, organic matter, pH, CEC, as well as sand, silt, and clay percentages. Additionally, we assess carbon sequestration levels, providing you with a holistic view of your soil's composition. The personalized recommendations derived from this test empower you to make precise adjustments to enhance your soil's health and productivity.

MWELO Soil Management Report

For those navigating California's MWELO guidelines, our MWELO Soil Management Report is an indispensable resource. This report not only ensures compliance but also promotes sustainable and thriving landscapes. It includes comprehensive data such as soil texture, infiltration rate, pH, total soluble salts, sodium content, and organic matter percentage. With amendment recommendations, optionally tailored to specific plant types, and annual maintenance tips, you'll be equipped to create landscapes that are both aesthetically pleasing and environmentally responsible.

Heavy Metals

The Heavy Metals analysis is a vital tool in assessing potential soil contamination. Given the uncertain history of properties, this analysis identifies the presence of heavy metals that might have accumulated due to past activities or nearby industrial sources. With results available in approximately nine business days, you'll gain insights to ensure the safety and health of your soil.

Soil Food Web

Explore the intricate world beneath the surface with our Soil Food Web analysis. By estimating population sizes of essential trophic groups—bacteria, fungi, protozoa, and nematodes—we unveil the microbiological health of your soil. Additionally, we identify specific organisms within these groups, providing insights into the soil's successional level and overall condition. This analysis is applicable to soil, compost, and compost tea samples, offering a holistic perspective on your soil's biological vitality.

Pesticide Screening

The Pesticide Screening can detect hundreds on common pesticides that may have been applied or drifted from nearby sources.

Herbicide Screening

The Herbicide Screening plays an important role in ensuring the safety of your soil and plants. By detecting the presence of herbicide residues, this test can indicated whether a soil has had history of herbicide applications.

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Regenerative Soil Management Practices

Working with nature to improve soil means implementing practices like cover cropping, mulching, and composting.

Cover Cropping

Cover cropping involves planting specific crops during non-growing seasons to cover and protect the soil. These crops enhance soil structure, prevent erosion, suppress weeds, and provide organic matter when incorporated into the soil. Leguminous cover crops also contribute nitrogen fixation, enriching soil fertility naturally. Cover cropping is a sustainable method that improves soil health and biodiversity.

Mulching

Mulching entails covering the soil surface with organic materials like straw, leaves, or wood chips. Mulch conserves soil moisture, moderates temperature fluctuations, suppresses weeds, and prevents soil erosion. As the mulch breaks down, it contributes organic matter, enriching the soil's structure and fertility. Mulching is an effective and easy way to maintain soil health.

Composting

Composting transforms organic waste into nutrient-rich compost. Incorporating compost into the soil enhances its structure, moisture retention, and fertility. Compost also introduces beneficial microorganisms that aid in nutrient cycling and disease suppression. Composting not only reduces waste but also revitalizes soil, making it an essential component of sustainable gardening.

Water Conservation Techniques

Implementing water-efficient practices such as drip irrigation, rainwater harvesting, and utilizing drought-resistant plants minimizes water use and reduces soil erosion. Conserving water in landscapes maintains soil moisture, supports plant growth, and sustains overall soil health. Water conservation techniques are vital for responsible gardening in arid and water-scarce regions.

If you have any questions feel free to get in touch with the Alluvial Soil Lab team at (831) 216-1367 or at info@alluvialsoillab.com

This page was written with the help of AI. The content provided on this website, including blog posts, articles, and instructional materials, is for informational and educational purposes only. Alluvial Soil Lab makes no warranties or guarantees regarding the accuracy, completeness, or applicability of any information presented. Recommendations and procedures described herein may not be appropriate for all situations or soil conditions. Readers are solely responsible for any actions they take based on this content.

References to third-party laboratories, addresses, services, or products are provided for convenience and do not constitute endorsement or affiliation. We strongly encourage users to independently verify all contact information, lab addresses, and service availability before relying on them.

Alluvial Soil Lab is not liable for any outcomes, damages, or losses resulting from the use of this content or any third-party services mentioned. Always consult with a qualified professional or certified lab before making decisions that may affect soil health, property, environmental compliance, or agricultural productivity.

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