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Well I get a ton of questions actually about basic soils and things similar to this fairly decent write up.the link has more info but that more general gardening than Canna specific but check it out its pretty nice as a baseline knowledge to have.Small simple matters can alter a soil drastically and a lotta ppl keep wanting to play science guy but simple is key and less is more when you add multi components so with that in mind enjoy the read.
:Sharing One: "AFN smoke out" :Hookah:
Though some gardeners may be blessed with perfect soil, most of us garden in soil that is less than perfect. If your soil has too much clay in it, is too sandy, too stony or too acidic, don't despair. Turning a poor soil into a plant-friendly soil is not difficult to do, once you understand the components of a healthy soil.
Soil is composed of weathered rock and organic matter, water and air. But the hidden "magic" in a healthy soil is the organisms—small animals, worms, insects and microbes—that flourish when the other soil elements are in balance.
Minerals. Roughly half of the soil in your garden consists of small bits of weathered rock that has gradually been broken down by the forces of wind, rain, freezing and thawing and other chemical and biological processes.
Soil type is generally classified by the size of these inorganic soil particles: sand (large particles), silt (medium-sized particles) or clay (very small particles). The proportion of sand, silt and clay particles determines the texture of your soil and affects drainage and nutrient availability, which in turn influence how well your plants will grow.
Organic Matter. Organic matter is the partially decomposed remains of soil organisms and plant life including lichens and mosses, grasses and leaves, trees, and all other kinds of vegetative matter.
Although it only makes up a small fraction of the soil (normally 5 to 10 percent), organic matter is absolutely essential. It binds together soil particles into porous crumbs or granules which allow air and water to move through the soil. Organic matter also retains moisture (humus holds up to 90 percent of its weight in water), and is able to absorb and store nutrients. Most importantly, organic matter is food for microorganisms and other forms of soil life.
You can increase the amount of organic matter in your soil by adding compost, aged animal manures, green manures (cover crops), mulches or peat moss. Because most soil life and plant roots are located in the top 6 inches of soil, concentrate on this upper layer. To learn more about making your own compost, read All About Composting.
Be cautious about incorporating large amounts of high-carbon material (straw, leaves, wood chips and sawdust). Soil microorganisms will consume a lot of nitrogen in their efforts to digest these materials and they may deprive your plants of nitrogen in the short run.
Soil life. Soil organisms include the bacteria and fungi, protozoa and nematodes, mites, springtails, earthworms and other tiny creatures found in healthy soil. These organisms are essential for plant growth. They help convert organic matter and soil minerals into the vitamins, hormones, disease-suppressing compounds and nutrients that plants need to grow.
Their excretions also help to bind soil particles into the small aggregates that make a soil loose and crumbly. As a gardener, your job is to create the ideal conditions for these soil organisms to do their work. This means providing them with an abundant source of food (the carbohydrates in organic matter), oxygen (present in a well-aerated soil), and water (an adequate but not excessive amount).
Air. A healthy soil is about 25 percent air. Insects microbes, earthworms and soil life require this much air to live. The air in soil is also an important source of the atmospheric nitrogen that is utilized by plants.
Well-aerated soil has plenty of pore space between the soil particles or crumbs. Fine soil particles (clay or silt) have tiny spaces between them - in some cases too small for air to penetrate. Soil composed of large particles, like sand, has large pore spaces and contains plenty of air. But, too much air can cause organic matter to decompose too quickly.
To ensure that there is a balanced supply of air in your soil, add plenty of organic matter, avoid stepping in the growing beds or compacting the soil with heavy equipment and never work the soil when it is very wet.
Water. A healthy soil will also contain about 25 percent water. Water, like air, is held in the pore spaces between soil particles. Large pore spaces allow rain and irrigation water to move down to the root zone and into the subsoil. In sandy soils, the spaces between the soil particles are so large that gravity causes water to drain down and out very quickly. That's why sandy soils dry out so fast.
Small pore spaces permit water to migrate back upwards through the process of capillary action. In waterlogged soils, water has completely filled the pore spaces, forcing out all the air. This suffocates soil organisms as well as plant roots.
Ideally, your soil should have a combination of large and small pore spaces. Again, organic matter is the key, because it encourages the formation of aggregate, or crumbs, or soil. Organic matter also absorbs water and retains it until it is needed by plant roots.
Every soil has a different combination of these five basic components. By balancing them you can dramatically improve your soil's healthy and your garden's productivity. But first, you need to know what kind of soil you have.
Soil Texture and TypeSoil texture can range from very fine particles to coarse and gravelly. You don't have to be a scientist to determine the texture of the soil in your garden. To get a rough idea, simply place some soil in the palm of your hand and wet it slightly, then run the mixture between your fingers. If it feels gritty, your soil is sandy; if it feels smooth, like moist talcum powder, your soil is silty; if it feels harsh when dry, sticky or slippery when wet, or rubbery when moist, it is high in clay.
Every soil has unique physical characteristics, which are determined by how it was formed. The silty soil found in an old floodplain is inherently different from stony mountain soil; the clay soil that lay under a glacier for millions of years is unlike the sandy soil near an ocean. Some of these basic qualities can be improved with proper management—or made worse by abuse.
Identifying your soil type: Soils are generally described according to the predominant type of soil particle present: sand, silt or clay. By conducting a simple soil test, you can easily see what kind of soil you're dealing with. You may want to repeat this test with several different soil samples from your lawn and garden.
1. Fill a quart jar about one-third full with topsoil and add water until the jar is almost full.
2. Screw on the lid and shake the mixture vigorously, until all the clumps of soil have dissolved.
3. Now set the jar on a windowsill and watch as the larger particles begin to sink to the bottom.
4. In a minute or two the sand portion of the soil will have settled to the bottom of the jar (see illustration). Mark the level of sand on the side of the jar.
5. Leave the jar undisturbed for several hours. The finer silt particles will gradually settle onto the sand. You will find the layers are slightly different colors, indicating various types of particles.
6. Leave the jar overnight. The next layer above the silt will be clay. Mark the thickness of that layer. On top of the clay will be a thin layer of organic matter. Some of this organic matter may still be floating in the water. In fact, the jar should be murky and full of floating organic sediments. If not, you probably need to add organic matter to improve the soil's fertility and structure.
Improving Soil StructureEven very poor soil can be dramatically improved, and your efforts will be well rewarded. With their roots in healthy soil, your plants will be more vigorous and more productive.
Sandy Soil. Sand particles are large, irregularly shaped bits of rock. In a sandy soil, large air spaces between the sand particles allow water to drain very quickly. Nutrients tend to drain away with the water, often before plants have a chance to absorb them. For this reason, sandy soils are usually nutrient-poor.
A sandy soil also has so much air in it that microbes consume organic matter very quickly. Because sandy soils usually contain very little clay or organic matter, they don't have much of a crumb structure. The soil particles don't stick together, even when they're wet.
Lack of pore space means that clay soils are generally low in both organic matter and microbial activity. Plant roots are stunted because it is too hard for them to push their way through the soil. Foot traffic and garden equipment can cause compaction problems. Fortunately, most clay soils are rich in minerals which will become available to your plants once you improve the texture of the soil.
:Sharing One: "AFN smoke out" :Hookah:
Though some gardeners may be blessed with perfect soil, most of us garden in soil that is less than perfect. If your soil has too much clay in it, is too sandy, too stony or too acidic, don't despair. Turning a poor soil into a plant-friendly soil is not difficult to do, once you understand the components of a healthy soil.
Soil is composed of weathered rock and organic matter, water and air. But the hidden "magic" in a healthy soil is the organisms—small animals, worms, insects and microbes—that flourish when the other soil elements are in balance.
Minerals. Roughly half of the soil in your garden consists of small bits of weathered rock that has gradually been broken down by the forces of wind, rain, freezing and thawing and other chemical and biological processes.
Soil type is generally classified by the size of these inorganic soil particles: sand (large particles), silt (medium-sized particles) or clay (very small particles). The proportion of sand, silt and clay particles determines the texture of your soil and affects drainage and nutrient availability, which in turn influence how well your plants will grow.
Organic Matter. Organic matter is the partially decomposed remains of soil organisms and plant life including lichens and mosses, grasses and leaves, trees, and all other kinds of vegetative matter.
Although it only makes up a small fraction of the soil (normally 5 to 10 percent), organic matter is absolutely essential. It binds together soil particles into porous crumbs or granules which allow air and water to move through the soil. Organic matter also retains moisture (humus holds up to 90 percent of its weight in water), and is able to absorb and store nutrients. Most importantly, organic matter is food for microorganisms and other forms of soil life.
You can increase the amount of organic matter in your soil by adding compost, aged animal manures, green manures (cover crops), mulches or peat moss. Because most soil life and plant roots are located in the top 6 inches of soil, concentrate on this upper layer. To learn more about making your own compost, read All About Composting.
Be cautious about incorporating large amounts of high-carbon material (straw, leaves, wood chips and sawdust). Soil microorganisms will consume a lot of nitrogen in their efforts to digest these materials and they may deprive your plants of nitrogen in the short run.
Soil life. Soil organisms include the bacteria and fungi, protozoa and nematodes, mites, springtails, earthworms and other tiny creatures found in healthy soil. These organisms are essential for plant growth. They help convert organic matter and soil minerals into the vitamins, hormones, disease-suppressing compounds and nutrients that plants need to grow.
Their excretions also help to bind soil particles into the small aggregates that make a soil loose and crumbly. As a gardener, your job is to create the ideal conditions for these soil organisms to do their work. This means providing them with an abundant source of food (the carbohydrates in organic matter), oxygen (present in a well-aerated soil), and water (an adequate but not excessive amount).
Air. A healthy soil is about 25 percent air. Insects microbes, earthworms and soil life require this much air to live. The air in soil is also an important source of the atmospheric nitrogen that is utilized by plants.
Well-aerated soil has plenty of pore space between the soil particles or crumbs. Fine soil particles (clay or silt) have tiny spaces between them - in some cases too small for air to penetrate. Soil composed of large particles, like sand, has large pore spaces and contains plenty of air. But, too much air can cause organic matter to decompose too quickly.
To ensure that there is a balanced supply of air in your soil, add plenty of organic matter, avoid stepping in the growing beds or compacting the soil with heavy equipment and never work the soil when it is very wet.
Water. A healthy soil will also contain about 25 percent water. Water, like air, is held in the pore spaces between soil particles. Large pore spaces allow rain and irrigation water to move down to the root zone and into the subsoil. In sandy soils, the spaces between the soil particles are so large that gravity causes water to drain down and out very quickly. That's why sandy soils dry out so fast.
Small pore spaces permit water to migrate back upwards through the process of capillary action. In waterlogged soils, water has completely filled the pore spaces, forcing out all the air. This suffocates soil organisms as well as plant roots.
Ideally, your soil should have a combination of large and small pore spaces. Again, organic matter is the key, because it encourages the formation of aggregate, or crumbs, or soil. Organic matter also absorbs water and retains it until it is needed by plant roots.
Every soil has a different combination of these five basic components. By balancing them you can dramatically improve your soil's healthy and your garden's productivity. But first, you need to know what kind of soil you have.
Soil Texture and TypeSoil texture can range from very fine particles to coarse and gravelly. You don't have to be a scientist to determine the texture of the soil in your garden. To get a rough idea, simply place some soil in the palm of your hand and wet it slightly, then run the mixture between your fingers. If it feels gritty, your soil is sandy; if it feels smooth, like moist talcum powder, your soil is silty; if it feels harsh when dry, sticky or slippery when wet, or rubbery when moist, it is high in clay.
Every soil has unique physical characteristics, which are determined by how it was formed. The silty soil found in an old floodplain is inherently different from stony mountain soil; the clay soil that lay under a glacier for millions of years is unlike the sandy soil near an ocean. Some of these basic qualities can be improved with proper management—or made worse by abuse.
Identifying your soil type: Soils are generally described according to the predominant type of soil particle present: sand, silt or clay. By conducting a simple soil test, you can easily see what kind of soil you're dealing with. You may want to repeat this test with several different soil samples from your lawn and garden.
1. Fill a quart jar about one-third full with topsoil and add water until the jar is almost full.
2. Screw on the lid and shake the mixture vigorously, until all the clumps of soil have dissolved.
3. Now set the jar on a windowsill and watch as the larger particles begin to sink to the bottom.
4. In a minute or two the sand portion of the soil will have settled to the bottom of the jar (see illustration). Mark the level of sand on the side of the jar.
5. Leave the jar undisturbed for several hours. The finer silt particles will gradually settle onto the sand. You will find the layers are slightly different colors, indicating various types of particles.
6. Leave the jar overnight. The next layer above the silt will be clay. Mark the thickness of that layer. On top of the clay will be a thin layer of organic matter. Some of this organic matter may still be floating in the water. In fact, the jar should be murky and full of floating organic sediments. If not, you probably need to add organic matter to improve the soil's fertility and structure.
Improving Soil StructureEven very poor soil can be dramatically improved, and your efforts will be well rewarded. With their roots in healthy soil, your plants will be more vigorous and more productive.
Sandy Soil. Sand particles are large, irregularly shaped bits of rock. In a sandy soil, large air spaces between the sand particles allow water to drain very quickly. Nutrients tend to drain away with the water, often before plants have a chance to absorb them. For this reason, sandy soils are usually nutrient-poor.
A sandy soil also has so much air in it that microbes consume organic matter very quickly. Because sandy soils usually contain very little clay or organic matter, they don't have much of a crumb structure. The soil particles don't stick together, even when they're wet.
To improve sandy soil:
Clay Soil. Clay particles are small and flat. They tend to pack together so tightly that there is hardly any pore space at all. When clay soils are wet, they are sticky and practically unworkable. They drain slowly and can stay waterlogged well into the spring. Once they finally dry out, they often become hard and cloddy, and the surface cracks into flat plates.- Work in 3 to 4 inches of organic matter such as well-rotted manure or finished compost.
- Mulch around your plants with leaves, wood chips, bark, hay or straw. Mulch retains moisture and cools the soil.
- Add at least 2 inches of organic matter each year.
- Grow cover crops or green manures.
Lack of pore space means that clay soils are generally low in both organic matter and microbial activity. Plant roots are stunted because it is too hard for them to push their way through the soil. Foot traffic and garden equipment can cause compaction problems. Fortunately, most clay soils are rich in minerals which will become available to your plants once you improve the texture of the soil.
To improve clay soil:
Silty Soil. Silty soils contain small irregularly shaped particles of weathered rock, which means they are usually quite dense and have relatively small pore spaces and poor drainage. They tend to be more fertile than either sandy or clayey soils.- Work 2 to 3 inches of organic matter into the surface of the soil. Then add at least 1 inch more each year after that.
- Add the organic matter in the fall, if possible.
- Use permanent raised beds to improve drainage and keep foot traffic out of the growing area.
- Minimize tilling and spading.
To improve silty soil:
Frequently Asked QuestionsWhat are cover crops and green manures?
Cover crops are used primarily to protect fallow (unused) soil. In the North, gardeners usually plant them at the end of the season so their soil is not bare over the winter. Cold-hardy crops such as vetch and winter rye are best for overwintering. They will begin growth again in spring, and need to be tilled in before you can plant your garden.
Green manures can also be planted on a new garden area the year before you plan to use it. They will choke out weeds and add a wealth of organic matter. Legumes, including field peas, soybeans, and alfalfa, will contribute both nitrogen and organic matter to the soil. Fast-growing grains and buckwheat produce the most organic matter and will smother competing weeds as they grow.
If your soil will be fallow for more than one growing season, you can plant perennial or biennial green manures, such as clover or alfalfa. All cover crops should be tilled-in at least three weeks before the area is to be replanted, so the organic matter will already be partially decomposed at planting time.
What are liquid soil conditioners?
Liquid soil conditioners typically contain a blend of humic acid and catalytic enzymes, which are produced in a controlled environment by the same sort of microorganisms that are at work in your compost pile. When applied to your soil, their effect is similar to the effect you get when you add compost. Clay soils become easier to work and nutrients become more available; sandy soils are able to retain more water and nutrients.
Researchers have now isolated specific organic substances that solve specific soil problems. Soon you will be able to buy organic soil conditioners that have been specially selected for their effectiveness in opening up heavy soils or dislodging salts and other elements that have become tied up in the soil.
What is hardpan?
Hardpan is a dense layer of soil that restricts root growth and the movement of moisture, air and beneficial organisms through the soil. Hardpan is usually created by glacial action, heavy rain, or heavy equipment, and typically lies between 6 and 25 inches below the soil surface.
Farmers often cope with hardpan by using a chisel plow to cut and break up this dense layer of soil. Home gardeners can break up and mix the hardpan layer by "double digging" the soil. This involves removing 10 to 12 inches of topsoil, and then working organic matter into the 12-inch layer of material that lies below. If the hardpan layer is not too deep, you can use a digging fork to puncture it and open up passages for air and water.
What does chelated mean?
Chelation is a process that joins a nutrient, such as iron, to a non-nutrient compound that can be easily absorbed by your plants.
What does 5-8-3 mean?
The numbers refer to the percentage by net weight of total nitrogen (N; always the first number), available phosphorus (P; the second number), and soluble potash (K; the third number). In other words, a 5-8-3 fertilizer contains 5 percent nitrogen, 8 percent available phosphorus, and 3 percent soluble potash.
Labeling laws allow only the immediately available nutrients to be listed. That is why the nutrient analysis for organic fertilizers tends to be low. Most organic fertilizers actually have a higher nutrient content, but these nutrients gradually become available to plants over a period of months or even years.
What are the benefits of seaweed?
Seaweed contains at least sixty micronutrients, including iron, copper, zinc, boron, and manganese. Seaweed also contains a high concentration of natural growth hormones which allow it to grow rapidly in its natural environment. When applied to plants, these growth hormones stimulate root growth, reduce transplant shock, promote more rapid fruit set, increase frost resistance and improve storage life. Research has also revealed that seaweed contains antitoxins that help plants fend off bacteria, viruses and pests.
Powdered seaweed (kelp meal) releases its nutrients gradually into the soil. Liquid seaweed makes these nutrients immediately available. Seaweed is not a complete fertilizer because it doesn't provide adequate nitrogen and phosphorus for most plants. But it is an excellent part of a balanced soil-building program.
http://www.gardeners.com/how-to/building-healthy-soil/5060.html
:Sharing One:
Pros of Super Soil
- Add at least 1 inch of organic matter each year.
- Concentrate on the top few inches of soil to avoid surface crusting.
- Avoid soil compaction by avoiding unnecessary tilling and walking on garden beds.
- Consider constructing raised beds.
Frequently Asked QuestionsWhat are cover crops and green manures?
Cover crops are used primarily to protect fallow (unused) soil. In the North, gardeners usually plant them at the end of the season so their soil is not bare over the winter. Cold-hardy crops such as vetch and winter rye are best for overwintering. They will begin growth again in spring, and need to be tilled in before you can plant your garden.
Green manures can also be planted on a new garden area the year before you plan to use it. They will choke out weeds and add a wealth of organic matter. Legumes, including field peas, soybeans, and alfalfa, will contribute both nitrogen and organic matter to the soil. Fast-growing grains and buckwheat produce the most organic matter and will smother competing weeds as they grow.
If your soil will be fallow for more than one growing season, you can plant perennial or biennial green manures, such as clover or alfalfa. All cover crops should be tilled-in at least three weeks before the area is to be replanted, so the organic matter will already be partially decomposed at planting time.
What are liquid soil conditioners?
Liquid soil conditioners typically contain a blend of humic acid and catalytic enzymes, which are produced in a controlled environment by the same sort of microorganisms that are at work in your compost pile. When applied to your soil, their effect is similar to the effect you get when you add compost. Clay soils become easier to work and nutrients become more available; sandy soils are able to retain more water and nutrients.
Researchers have now isolated specific organic substances that solve specific soil problems. Soon you will be able to buy organic soil conditioners that have been specially selected for their effectiveness in opening up heavy soils or dislodging salts and other elements that have become tied up in the soil.
What is hardpan?
Hardpan is a dense layer of soil that restricts root growth and the movement of moisture, air and beneficial organisms through the soil. Hardpan is usually created by glacial action, heavy rain, or heavy equipment, and typically lies between 6 and 25 inches below the soil surface.
Farmers often cope with hardpan by using a chisel plow to cut and break up this dense layer of soil. Home gardeners can break up and mix the hardpan layer by "double digging" the soil. This involves removing 10 to 12 inches of topsoil, and then working organic matter into the 12-inch layer of material that lies below. If the hardpan layer is not too deep, you can use a digging fork to puncture it and open up passages for air and water.
What does chelated mean?
Chelation is a process that joins a nutrient, such as iron, to a non-nutrient compound that can be easily absorbed by your plants.
What does 5-8-3 mean?
The numbers refer to the percentage by net weight of total nitrogen (N; always the first number), available phosphorus (P; the second number), and soluble potash (K; the third number). In other words, a 5-8-3 fertilizer contains 5 percent nitrogen, 8 percent available phosphorus, and 3 percent soluble potash.
Labeling laws allow only the immediately available nutrients to be listed. That is why the nutrient analysis for organic fertilizers tends to be low. Most organic fertilizers actually have a higher nutrient content, but these nutrients gradually become available to plants over a period of months or even years.
What are the benefits of seaweed?
Seaweed contains at least sixty micronutrients, including iron, copper, zinc, boron, and manganese. Seaweed also contains a high concentration of natural growth hormones which allow it to grow rapidly in its natural environment. When applied to plants, these growth hormones stimulate root growth, reduce transplant shock, promote more rapid fruit set, increase frost resistance and improve storage life. Research has also revealed that seaweed contains antitoxins that help plants fend off bacteria, viruses and pests.
Powdered seaweed (kelp meal) releases its nutrients gradually into the soil. Liquid seaweed makes these nutrients immediately available. Seaweed is not a complete fertilizer because it doesn't provide adequate nitrogen and phosphorus for most plants. But it is an excellent part of a balanced soil-building program.
http://www.gardeners.com/how-to/building-healthy-soil/5060.html
:Sharing One:
Pros of Super Soil
- Better Taste, Smell, Smoothness - Many growers believe that growing cannabis in super soil enhances taste and smell compared to other growing methods, while producing some of the smoothest buds without any hint of "harshness" from chemicals or over-fertilization
- Great for Indoors and Outdoors - Super soil is a versatile growing medium that can be used to grow thriving cannabis plants almost anywhere
- Natural - Super soil can be created using only organic ingredients that have been broken down naturally - this closely mimics the best and richest soil found in nature
- No Need to Flush - Since there's no chemical salts to alter taste and smell of buds, many organic growers feel there's no need to flush before harvest
- Easier to Grow - Once the amended soil is composted, growing cannabis in super soil is easier than pretty much any other type of growing medium; with super soil there's no need to worry about maintaining pH or nutrients! Just water your plants and wait until harvest
Cons of Super Soil
- Expensive & Best Suited to Bigger Grows - Can be expensive to get started since you generally compost a lot of soil at once - it's difficult to scale the organic super soil process down to smaller grows that need less soil at a time
- Need to Plan Ahead - Composting take 30-60 days before your soil is ready to be used by your plants, which means you have to plan ahead before each organic grow
- Mixing Soil Can Be Tiring - The amending and composting process involves some physical work (mixing the soil)
[h=2]More tips to save your soil[/h]In addition to disturbing the soil structure by tilling or turning over the earth, Littlefield and Gershuny have a few other pet peeves when it comes to saving your soil.
- Avoid adding chemicals. “Chemical fertilizers and pesticides can be really hard on microorganisms, which are the key to healthy soil ecosystems,” Littlefield says. Gershuny adds that synthetic nitrogen can cause the same problems, plus the process used to make it is extremely energy-intensive. “There are things like blood meal, fish meal, alfalfa meal and similar products that will add soluble nitrogen if soil is very poor,” she says.
- Don’t tread on me. Minimize stepping where you plan to plant to avoid compacting the soil. Create pathways in your garden to walk on and make planting beds narrow enough that you can reach across them from either side when it comes time to harvest.
- Building blunders. Littlefield says that developers often scrape off topsoil from sites during building, leaving behind “really rotten subsoil.” If you’re building a new home, have your contractor stockpile your topsoil to spread back on your garden later, or rope off your garden plot ahead of time and ban bulldozers from that area. This will keep the soil from getting compacted by heavy machinery as well.
- Hands off when wet. We know you’re eager to get started, but avoid working in your garden when the ground is wet. “It can destroy the soil’s structure and turn it into a brick when it dries,” Littlefield says. How wet is too wet? Littlefield suggests molding a handful of soil into a ball with your fist. Flick it with your fingers — the ball should fall apart. “If not, it’s still too wet,” she says.
Within a week, my potted plants held water about as well as a brick. The soil pulled from the sides of the containers and formed tight, water-shedding balls. Only my hardiest seedlings survived.
Clearly, not all potting soils are created equal.
It’s What’s Inside That Counts
In a way, good potting soil tries to mimic nature. Healthy earth relies on critters, rocks and roots for aeration; but when put in a pot, the same soil quickly becomes a dense mass that water and oxygen can’t permeate.
“Soil alone is heavy and poorly aerated. It tends to become waterlogged and sticky when wet,” writes Eric Sideman, director of technical services for MOFGA, in his soil mix fact sheet.
Good potting soil tries to replicate nature by providing plant nutrients and materials that allow for drainage and aeration--but good potting soil, especially organically-approved, can be hard to come by.
Bruce Hoskins, assistant scientist and soil testing coordinator at the University of Maine, says of potting soil, let the buyer beware. “There’s some pretty questionable stuff that we’ve seen sold as potting soil.”
Lois Stack, ornamental horticulture specialist with University of Maine Cooperative Extension, says that just because something is labeled “potting soil” doesn’t mean it’ll work in a pot. “It’s really hard to define what is in that container,” Stack observes. “The word ‘soil’ has a very broad definition.”
Sideman suggests that an ideal mix should be dense enough to hold seedlings and water, but porous enough to shed excess water. It must be free of weed seeds and plant pathogens.
Peat and humus normally provide sponge-like water retention and drainage in organically-approved mixes, while sand provides plant support and drainage. The heat-expanded minerals perlite and vermiculite commonly provide pore space, improving drainage while minimizing the weight of the soil
Good potting soil must have plant nutrients, but getting enough nutrients into an organically-approved potting soil is not easy. In conventional potting soil, synthetic fertilizer can provide most of the food a plant will need for a while, but organic growers must rely on compost, which often doesn’t provide enough nutrients to last long in a pot. One way to overcome the shortage, Hoskins says, is to add fresh compost when transplanting to a larger container. Watering with manure tea or compost tea can also help.
Two Recipes for Success
Making successful compost-based potting soil is both art and science. While some hard and fast rules apply, soil recipes often differ from grower to grower.
Dennis King of King Hill Farm in Penobscot makes most of the potting soil for his vegetable seedlings rather than buying packaged, organically-approved soil, because, “It’s a whole lot cheaper.” He says good compost is the key to healthy potting soil, and heat is the key to good compost. Compost must get hot enough to kill pathogens and weed seeds, but not hot enough to kill beneficial organisms. One batch of improperly heated compost can impact a farmer for a long time. “One year of seeds, seven years of weeds,” he recites.
King keeps his compost at 140-150 degrees F. for at least two weeks in a self-propelled compost-turner that he shares with a neighbor. He then mixes his potting soil in a cement mixer using a recipe from Sideman: 5 gallons of compost, 5 gallons of peat, 2 ½ gallons of sand, a gallon of perlite, and a cup each of greensand, bone meal and lime.
His mix works better than material he used to buy. Store-bought soil caused problems with damping-off, a disease that weakens stems of young seedlings and usually kills them. “With good compost-based potting soil, I’ve forgotten all about damping-off,” says King.
Claudette Nadeau and her husband, Michael Beaudry, make at least 50% of the potting soil they need to grow seedlings at their Roots-n-Shoots Farm in Montville. The main ingredient for their compost is manure from the farm’s five sheep and four goats. “The manure from our girls is purely organic,” says Nadeau. “They are fed ‘Nature's Best’ organic grain and fed organic hay in the winter, [they get] no antibiotics, and are out to pasture and woods in the spring, summer and fall.”
Like King, Nadeau makes sure her compost reaches over 130 degrees for 10 days, turning the pile three times during that period, to destroy pathogens. Her recipe is 21 quarts compost, 6 quarts perlite, 15 quarts peat moss, and 1/2 cup each of lime, rock phosphate and greensand.
To Buy or To Mix
When deciding whether to make or buy soil, consider labor, time, access to dry storage and the cost of materials and mixing equipment. Stack notes that making your own isn’t always cheaper. Homemade mixes “often are not dependably consistent,” writes Sideman, but finding organically approved potting soil that is effective and affordable can be just as tricky.
Prepackaged potting soil is a relatively new concept. Hoskins says that until 30 years ago, most greenhouse growers simply sifted field soil for potting soil.
The organic soil market is even younger. Hoskins says the first wave of organically-approved soils often had problems. Some relied too heavily on compost and drained poorly; others had insufficient nutrients. Stack adds that until recently, turnover in the compost-soil market was high. “Every time they came and went, a grower would have to get used to a new mix.”
While the market has stabilized, Hoskins says knowledge about organically approved mixes still lags far behind that of conventional soil. “We’re all still learning about organic media.”
It’s All in the Nose
Nadeau uses soil made by the Vermont Compost Company (VCC) for the rest of her soil mix needs. She says its light texture is good for plant roots.
Being one of the more established and consistent organic soils on the market, VCC has attracted a following among Maine farmers.
Karl Hammer, VCC founder and owner, says the key to making good compost is to recognize problems that arise before the composting process is finished. “It comes down to telling yourself the truth.”
As VCC compost ages, it changes daily, so employees constantly adjust conditions to create a good product. Hammer adds that a compost maker’s chief ally is his or her nose. “Each of the compounds that could give you trouble has an odor signature.”
Each day, VCC employees sniff each batch of compost. If they detect a problem, they adjust the mixture or the conditions. Hammer smells finished batches as well, because, he says, compost making is too important not to get right. “The cost of potting soil failure to a grower is…hard to exaggerate.”
In the ‘70s, Hammer lived in the same Vermont town as organic pioneer Eliot Coleman, and the two experimented with soil blocks, a Dutch technique of packing soil so that it stands on its own. They needed a peat-free mix for this technique, so Hammer began to make his own. Neighbors soon came knocking for his mix.
After running his own manure removal business in New York, Hammer founded VCC in 1992 and sold his first soil two years later. His compost typically takes a year to age.
Much of VCC’s compost comes from manure generated by large Vermont dairy farms, which must follow VCC guidelines on bedding and manure management. The company also receives 12 tons of food waste a week from the town of Montpelier, but Hammer says the company’s secret weapon is its own flock of chickens. “Chicken manure is the Holy Grail of compost making.”
Chickens defecate and urinate at the same time and often mix their waste into their bedding immediately. This keeps nitrogen from escaping from the manure and maintains a good pH, creating excellent compost material. Hammer says eggs are an added bonus. [Chicken manure must be used in moderation, however, because of its nitrogen and salt content.]
Ultimately, Hammer believes composting can be boiled down to a science only so far. The rest is accepting and working with nature’s variables—and demand for that work is big. “There’s a hell of a lot of new demand and not a lot of excellent product,” concludes Hammer.
GOOD LINK!!
http://www.verticalveg.org.uk/creating-a-living-soil/
- Expensive & Best Suited to Bigger Grows - Can be expensive to get started since you generally compost a lot of soil at once - it's difficult to scale the organic super soil process down to smaller grows that need less soil at a time