soil health

Using Coffee Grounds in Your Garden

wooden spoon with coffee grounds on it

We are frequently asked if coffee grounds can be used in a garden. The short answer is yes, coffee grounds can be used in garden soil!

Coffee grounds contain some major nutrients (nitrogen, phosphorus, and potassium) as well as some micronutrients, so put them to work in your garden. Allow them to dry and then spread them around the base of plants.
Apply no more than one-half inch of coffee grounds when putting fresh coffee grounds directly to the ground as mulch. Because coffee grounds are finely textured and easily compacted, thick layers of coffee grounds as mulch can act as a barrier to moisture and air movement in soils.
So if you are using coffee grounds as a “dressing” for specific plants or trees, apply the grounds in a thin layer or work into the top layer of the soil.
Article by Gail Reynolds, Middlesex County Master Gardener Coordinator

Urban Farmer Trainings in Hartford

Urban Farmers and Hartford area Friends!   

Get ready for Urban Farmer Trainings in Hartford!

August 21st and August 28th
At Keney Park Sustainability Project and KNOX Inc
9:00am to 4:00pm
Join the I Got Next Farmers (Lauren Little Edutainment, Samad Garden Initiative, Micro2Life and Derrick Bedward) as they cover topics such as 
  • Community Farming
  • Soil & Plant Health
  • Seed Saving & Plant Genetics
  • Regenerative Soil Amendments
  • Methods of Indoor
  • Soil-less Growing
  • Micro-green Growing
    Register here: by August 14th to claim your spot!!
    Micro-green Growing

    Nutrient Management in Canaan

    dairy cows in East Canaan at Freund's Farm
    Photo: G. Morty Ortega

    Nutrient Management on farms is a balancing act between how much manure needs to be spread and how many nutrients crop fields need. We work with dairy farmers throughout the state to address the challenge of managing nutrient distribution on their fields through research and outreach, innovative technology, and by fostering collaborative partnerships.

    The Canaan Valley Agricultural Cooperative Waste Management Program formed in 1995 when Peter Jacquier of Laurelbrook Farm received a Northeast Sustainable Agriculture Research and Education grant. Jacquier worked with four other farmers to organize the cooperative. The farms improved manure management and disposal practices and adapted new technologies on their farming operations. Extension guides manure digester discussions, and assists with manure management through data collection, soil testing, and ongoing research using drones and other types of innovation.

    Dairy farmers in the cooperative, and other areas of the state, are developing strategies for anaerobic digestion and to deal with phosphorus accumulation in farm soils as a result of the grant.

    Methane digesters reduce odor and make farms more neighbor friendly. Digesters are expensive and need off farm food waste to help make the system profitable.

    Some digester companies include food waste tipping fees in the economic analysis, but not the increases in manure hauling costs to dispose of the added digestate. Farms need accurate hauling cost numbers to include in the economic analysis of the digesters to determine overall profitability of these projects. Extension continues to facilitate discussions with Canaan dairy farmers and others to address these challenges.

    Article by Richard Meinert

    No-till Vegetable Production

    No-till vegetable production: soil health, weed control, and crop yields

    Article by Shuresh Ghimire, Extension Vegetable Specialist, UConn Extension

    Building healthy soils, integrating cover crops, and managing weeds are key elements of vegetable farms. The use of no-till and cover crops provide a wealth of soil benefits thereby improving the productivity of the farming systems. However, due to limited agricultural land, farmers often have increasing pressure to keep greater portions of their land in cash crops. Cover-crop based no-till practices allow farms to gain the benefits of cover crop rotations while still earning a financial return from the land.

    No-tillage cropping systems are known to provide many benefits to soils that can improve crop productivity. Those benefits include better soil aggregate size and strength which means better soil structure, better infiltration, lower bulk density, better water holding capacity, decrease in erosion, and improved water quality. Other benefits include higher cation exchange capacity, which results in higher soil nutrient holding capacity and greater potential mineralizable nitrogen (increased soil nitrogen bank). Additionally, no-till contribute to increased organic matter (carbon) which serves as a food source for soil microbes. Soil microbes are responsible for the decay of organic matter and cycling of both macro-and micro-nutrients back into forms that plants can use.

    Though no-till systems offer a multitude of soil building as well as weed control benefits, implementation is limited, particularly in cooler climates like New England with shorter growing seasons. Correct management of cover crops used in no-till practices is critical because mismanagement can lead to undesired consequences, including serious weed issues rather than effective weed control.

    No-till and cover crop acres were increased significantly in Connecticut from 2012 to 2017. No-till acres was 18,153 acres (487 farms) according to 2017 Census of Agriculture, which was 54% increase from 2012. The cover crops acre was ~22,000 acres in 2017, which was 7.6% greater than 2012 (Soil Health Institute, 2019).

    In this article, I present farmers’ experience and some research evidence that show the use of no-till and cover cropping can provide a wealth of soil benefits thereby improving the farm profitability.

    Bryan O’Hara and Anita Johnson have been growing vegetables for a livelihood since 1990 at Tobacco Road Farm in Lebanon, Connecticut. Over the last twenty plus years of intensive vegetable growing at the farm, they constantly sought ways to improve the health and vitality of crops and soils.

    no till vegetable production“We slowly moved into no-till over the course of many years with experimentation. So, I do like to caution people to make sure it works for you before you put your whole farm into a new system because there are a lot of details.” Bryan says “We switched into no-till because we saw very strong improvement in crop health, less disease pressure, quite stunning results in plant disease and insect resistances, and very reduced need for weed control. We also saw the improvement in soil structure that resulted in much less irrigation needs. All of which resulted into greater profitability because crops were more vigorous, easier to harvest, stored better, and needed less labor.”

    An experiment in Blacksburg, VA, tested the effects of three cultivation techniques (conventional-till, strip-till, and no-till) on ‘Gladiator’ pumpkin production, weed pressure, soil moisture, and soil erosion in 2014 and 2015 (O’Rourke and Petersen, 2016). Overall yields were higher in 2015, averaging 20 tons/acre, compared with 17 tons/acre in 2014. In 2014, pumpkin yields were similar across tillage treatments. In 2015, the average fruit weight of no-till pumpkins was significantly greater than strip-till (13%) and conventional-till (22%) pumpkins. Weed control was variable between years, especially in the strip-till treatment. Soil moisture was consistently highest in the no-till treatment in both years of study. Conventional-till pumpkin plots lost ~9 times more soil than the two conservation tilled treatments during simulated storm events. The 2015 yield advantage of no-till pumpkins seems related to both high soil moisture retention and weed control. Research results suggest that no-till and strip-till pumpkin production systems yield at least as well as conventional-till systems with the advantage of reducing soil erosion during extreme rains.

    Jamie Jones of Jones Family Farm in Shelton, CT practices no-till pumpkin production.

    no till vegetable productionFigure 2 taken in mid-April shows winter rye with an herbicide strip where the pumpkins will be planted in June.  “We will roll the rye with a roller crimper when the rye starts shedding pollen, averaging sometime late in May”.  Jamie says “We planted this winter rye late September or early October in the last fall. It followed a cover crop of sorghum sudangrass that was planted after the strawberry field was turned under in early July”.

    Another research was conducted at University of Massachusetts Amherst to evaluate the nutrient cycling and weed suppressive benefits of forage radish (Raphanus sativus L. longipinnatus) cover crop mixtures to develop an integrated system for no-till sweet corn production (Fine, 2018). Treatments included forage radish (FR); oats (Avena sativa L.) and forage radish (OFR); a mixture of peas (Pisum sativum subsp arvense L.), oats and forage radish (POFR); and no cover crop control (NCC). Fall-planted forage radish cover crops showed successful weed suppression and recycling of fall-captured nutrients. Results indicated that POFR and OFR provided improved N cycling and sweet corn yield compared with FR and NCC. Early season N from decomposing cover crop residue was sufficient to eliminate the need for N fertilizer at sweet corn planting, thereby reducing input costs and risks of environmental pollution.

    Steve Munno, the Farm Manager at Massaro Community Farm in Woodbridge, CT, also uses cover crops and no-till to improve the soil health for organic vegetable production. “The combination of peas, vetch and oats works great in the no-till system”. Steve Munno says “With a single sowing of this cover crop mix in late summer we see significant accumulation of biomass throughout the fall from the peas and oats, an excellent winter cover protecting the soil, vigorous spring growth of vetch which produces more biomass and provides flowers for pollinators, plus nitrogen fixation (peas and vetch) and organic matter build up for the following crop”.

    no till vegetables at massaro community farmLounsbury et al. (2018) tested whether reusable plastic tarps, an increasingly popular tool for small-scale vegetable farmers, could be used to augment organic no-till cover crop termination and weed suppression in New Hampshire. The authors no-till transplanted cabbage into a winter rye (Secale cereale L.)-hairy vetch (Vicia villosa Roth) cover crop mulch that was terminated with either a roller-crimper alone or a roller-crimper plus black or clear tarps. Tarps were applied for durations of 2, 4 and 5 weeks. Across tarp durations, black tarps increased the mean cabbage head weight by 58% compared with the no tarp treatment. This was likely due to a combination of improved weed suppression and nutrient availability. Plastic tarps effectively killed the vetch cover crop, whereas it readily regrew in the crimped but uncovered plots. However, emergence of large and smooth crabgrass (Digitaria spp.) appeared to be enhanced in the clear tarp treatment. Although this experiment was limited to a single site-year in New Hampshire, it showed that use of black tarps can overcome some of the obstacles to implementing cover crop-based no-till vegetable productions in northern climates.

    Bryan also shares his experience using tarps “Black and clear tarps are often superior to tillage events as some weeds can survive the tillage events, but tarps are really effective at giving us weed free surface to begin planting or seeding into”.

    Download a PDF of this article.


    Fine, J.S. 2018. Integrating cover crop mixtures and no-till for sustainable sweet corn production in the Northeast. Masters Theses. 637.

    Lounsbury, N., N. Warren, S. Wolfe, and R. Smith. 2018. Investigating tarps to facilitate organic no-till cabbage production with high-residue cover crops. Renewable Agriculture and Food Systems:1-7. doi:10.1017/S1742170518000509

    O’Hara, B. 2020. No-till intensive vegetable culture: pesticide-free methods for restoring soil and growing nutrient-rich, high-yielding crops. Chelsea Green Publishing, U.S.

    O’Rourke, M.E. and J. Petersen. 2016. Reduced tillage impacts on pumpkin yield, weed pressure, soil moisture, and soil erosion. HortScience 51:1524–1528.

    Soil Health Institute. 2019. Progress report: Adoption of soil health systems based on data from 2017 U.S. Census of Agriculture. Soil Health Institute, Morrisville, NC.

    Have Your Soil Tested for Macro and Micro Nutrients

    person holding a cup of soil
    Photo: Dawn Pettinelli

    Send your soil sample in for testing now. Our standard nutrient analysis includes pH, macro- and micro nutrients, a lead scan and as long as we know what you are growing, the results will contain limestone and fertilizer recommendations. The cost is $12/sample. You are welcome to come to the lab with your ‘one cup of soil’ but most people are content to simply place their sample in a zippered bag and mail it in. For details on submitting a sample, go to UConn Soil and Nutrient Laboratory.

    Have your Soil Tested for Macro & Micro Nutrients

    cup of soil being held in Soil Nutrient analysis lab at UConn

    Send your soil sample in for testing now. Our standard nutrient analysis includes pH, macro- and micro nutrients, a lead scan and as long as we know what you are growing, the results will contain limestone and fertilizer recommendations. The cost is $12/sample. You are welcome to come to the lab with your ‘one cup of soil’ but most people are content to simply place their sample in a zippered bag and mail it in. For details on submitting a sample, go to UConn Soil and Nutrient Laboratory.

    Spotlight – Soil Degradation

    One of the most pressing resource related issues around the world is the continual reduction in the percentage of arable land. Currently, 37% of land worldwide is considered agricultural, only 10% is deemed arable, or plowable, and suitable for crop production (World Bank Group, 2015). The shrinking percentage of suitable farm land is a direct result of soil degradation, which is attributed to tillage practices and the use of agrochemicals in intensive agriculture. Overgrazing of rangelands, natural occurrences such as wildfires, and non-agricultural human activities such as road salt applications also contribute to the degradation of soils, making mediation efforts cumbersome. Although the degradation of soils is a multifaceted process with a range of negative effects, effects tend to be closely tied with one another making the process as a whole degenerative.

    The current intensive agricultural systems in place throughout the world aim to maximize production through increased inputs, such as labor and agrochemicals, while reducing waiting periods between crops. Large-scale annual crop production relies primarily on conventional tillage methods such as the moldboard plow, an implement that cuts a furrow slice of soil (around 8 inches in depth). The furrow slice is lifted, flipped, and dropped back down, inverting the soil profile. Simultaneously, this implement forms a hardpan layer of compacted soil beneath the disturbed portion. Both the inversions and hardpans negatively impact the soil’s structure. A compromised soil structure carries its own concerns and at the same time predicates multiple downstream effects.

    A soil’s structure refers to the arrangement of fine soil articles into groups called aggregates. Many soil activities such as water movement, heat transfer, and aeration are directly impacted by the formation and arrangement of aggregates which results from a range of slow biological, physical and chemical processes. Aggregates are delicate and become destroyed in frequently disturbed soils such as those in annual cropping systems. Destruction of aggregates increases the bulk density of a soil. As bulk density increases water infiltration, water holding capacity, aeration, and root penetration decrease, making it more difficult for crops to access resources essential for growth.

    The regular application of agrochemicals in cropping systems further diminishes the health of soil. Agrochemicals include herbicides, pesticides, fertilizers, and other soil amendments. One of the main concerns with the addition of these chemicals is their interaction with soil organisms. Soil macro- and microorganisms include bacteria, fungi, and earthworms; all contribute to a healthy plant rhizosphere and provide a range of benefits within cropping systems. These organisms are very sensitive to variation in their environment such as changes in pH, salinity, and the carbon:nitrogen ratio. These inputs represent rapid cyclic environmental shifts to which soil organisms cannot acclimate or adapt to. Instead, the diversity of soil organism diversity is diminished.

    Soil organisms play a range of roles in the development and maintenance of a healthy soil profile, which in turn affects the growth and development of crops. Microorganisms such as bacteria fix nitrogen, making the largely inaccessible pool of atmospheric nitrogen available for plant uptake. Fungi, like mycorrhizae, form mutualistic associations with plant roots, extending their network of nutrient and water uptake. Larger organisms such as earthworms help to form soil aggregates by creating macropores and producing worm castings. Many insects also contribute to the formation of soil aggregates as well as help reduce the weed seedbank via predation. Healthy, natural soil systems are engineered by a consortium of organisms and by design are able to provide the needs of plants. However, in some cropping systems, this level of provision is deemed inadequate, prompting the need for agrochemicals and at the same time impacting the functionality of the soil.

    Soil degradation is not limited to artificial systems. There are several factors, both natural and human induced, contributing to the percentage of degraded land around the world, outside of agricultural systems. Wild fires, which occur regularly in arid regions, burn vegetation which help to hold soils in place. Climate change, combined with lack of management in fire-prone areas, has dramatically increased the frequency and intensity of these fires, increasing the potential erosion. Mismanagement and overgrazing of rangelands in dry regions also diminishes soil-stabilizing vegetation, creating the same potential for erosion. In more temperate regions, road salt application during the winter months has become cause for concern as these salts become distributed into the ecosystems affecting both soil structure and soil organisms.

    The effects of soil degradation are not discrete, often tied to each other in a continuum in which some agricultural practices initiate a predictable sequence of events that ultimately leads to diminished soil health. Conventional tillage methods and the use of agrochemicals seem to be the catalytic events for such series of events in annual cropping systems; affecting soil structure, organic matter content, and the health of soil organisms. These in turn compromise the functionality of soils as the medium for crop growth and development. There is wealth of information on alternative practices that aim to reduce the impact of agriculture on soil health. For more information on soil conservation and alternative agricultural practices please visit the UConn Extension website or contact your local extension office.

    Despite the evidence supporting the continual degradation of soils due to agricultural activities, there is little consideration for the viability of suggested remediation practices in regard to the effects on food production, farmers and the agriculture industry as a whole. Reducing tillage and agrochemical input is not a solution for many agricultural systems as some crops simply do not perform well in no till systems, while reduced agrochemical input would greatly compromise crop yields. Considering the importance of agriculture to society at large, farmers, who may be the most hardworking and underpaid individuals in the world, utilize available options to maintain soil health while still maintaining a productive and economically feasible operation.

    From the farmers perspective, this is often represented by tradeoffs. Farmers are not ignorant to the concept of soil degradation or the importance of soil health. In fact, they understand the impact of these much better than anyone else. Operations which use agrochemicals and employ conventional tillage methods still take steps to maintain soil health. Many of these cropping systems utilize conservation practices such as the incorporation of cover crops or selection of organic agrochemical alternatives. Elizabeth Creech of NRCS (Natural Resources Conservation Service) wrote an informative piece entitled “The Dollars and Cents of Soil Health: A Farmer’s Perspective” which depicts many of the challenges farmers face when it comes to maintaining soil health. For more information please follow this link:

    Soil pH – The Master Variable

    The UConn Soil Nutrient Analysis Lab tests for and analyzes multiple soil parameters; but none as critical, and as often overlooked, as pH. Soil pH plays a crucial role in the growth of vegetation planted, as well as ground water quality. Before we start talking about soil pH, I think it is a good idea to try to define what exactly pH is, and how it is determined.

    When most of us think of pH, a pool probably comes to mind. I remember growing up, watching my mother apply different chemicals to our pool, and impatiently wondering why I had to wait to go swimming. She would tell me that she was adjusting the pH of the water to ensure it was safe to swim in. The basic understanding is that pH is tells us how acidic, neutral, or alkaline something is. To get a little more technical, pH is the measurement of the activity of Hydrogen Ions (H+) in an aqueous solution. The equation for determining and quantifying pH is:

    pH = -log10 (aH+)

    (aH+= Hydrogen Ion Activity in Moles/L)

    We express pH on a logarithmic scale of 0-14, where 0-6 is considered “acidic”, 7 is “neutral”, and 8-14 is “basic”.

    soil pH scale
    Image from:

    Mineral soil pH values generally range from 3.0 – 10.0. There are numerous factors that determine soil pH including climate, parent material, weathering, relief, and time. Texture and organic matter content also influence soil pH. Most Connecticut soils are naturally acidic. Nutrient availability is directly influenced by pH with most plants (with some exceptions) thriving at pH values between 6 and 7. A majority of nutrients are available within this range.

    Our lab measures pH using an 1:1 soil-to-DI water ratio. The saturated soil paste is mixed, then is analyzed using a glass electrode and a pH meter. We calibrate our meter using 2 solutions with known pH values, 4 and 7. We use these values because we expect most Connecticut soils to fall within this range. Once the initial pH value is obtained, a buffering agent is added. In our lab we use the Modified Mehlich Buffer. A second pH reading is obtained, and from these two values plus crop information, we are able to make limestone and/or sulfur recommendations.

    The Buffering Capacity of a soil is the resistance it has to change in pH. Soil buffering is controlled by its Cation-Exchange-Capacity, Aluminum content (in acidic soils), organic matter content, and texture. A soil with a lot of organic matter and clay will have a higher buffering capacity than one with little organic matter that is mostly sandy.

    If the soil pH is lower than the target range for a particular plant, limestone would be recommended. Whether you use pelletized, ground or granular limestone, the application rate would be the same. Once the target pH is reached, a maintenance application of 50 lbs/1000 sq ft would be applied every other year to maintain it.

    If the soil pH is higher than desired, sulfur recommendations are made. Typically only powdered sulfur is available locally but granular sulfur could be mail ordered. Aluminum sulfate can be substituted for sulfur and used at a higher rate. Check out this listof preferred pH ranges for many common plants.

    Monitoring your soil pH is essential to ensure that it is falling within the range best suited for the vegetation you are growing. The Standard Nutrient Analysis performed at our lab gives you a pH value, a buffer pH value, a lime/sulfur recommendation, available micro & macro nutrient levels, and a fertilizer recommendation. For more information on pH, you can contact Dawn or myself (Joe) at the UConn Soil Nutrient Analysis Lab ( Test, don’t guess!

    By Joe C.

    Nitrogen – The Fix

    Chlorotic corn. Image provided by T. Morris, 2018

    Nitrogen is an essential nutrient required for the production and growth of all plants, vegetation, and living organisms. It makes up 78% of our atmosphere; however, that only accounts for 2% of the Nitrogen on our planet. The remaining 98% can be found within the Earth’s lithosphere; the crust and outer mantel. The Nitrogen found within the nonliving and living fractions of soil represents an unimaginably low fraction of a percentage of all the Nitrogen on our planet. That tiny percent of all total Nitrogen found in our soils is what we can interact with to help or hinder plant production.

    To be considered an essential nutrient, an element must satisfy certain criteria:

    • Plants cannot complete their life cycles without it.
    • Its role must be specific and defined, with no other element being able to completely substitute for it.
    • It must be directly involved in the nutrition of the plant, meaning that it is a constituent of a metabolic pathway of an essential enzyme.

    In plants, Nitrogen is necessary in the formation of amino acids, nucleic acids (DNA and RNA), proteins, chlorophyll, and coenzymes. Nitrogen gives plants their lush, green color while promoting succulent growth and hastens maturity. When plants do not receive adequate Nitrogen, the leaves and tissues develop chlorosis. However, over-application of Nitrogen can cause even more problems, including delayed maturity, higher disease indigence, lower tolerance to environmental stresses, reduced carbohydrate reserves, and poor root development.

    Read more….