Sunday, 16 February 2025

Composting - How to make it , how to use it and why to bother.

 During this post, we'll uncover the wonders of composting – from the breakdown of once-living matter to the creation of nutrient-rich soil gold. We’ll explore the role of oxygen, the carbon-nitrogen balance, and the fascinating process that turns simple materials into a thriving ecosystem for your plants.

Everything that was once living, everywhere on the planet, is decomposed, i.e. broken down into simpler organic or inorganic matter such as carbon dioxide, water, simple sugars and mineral salts, in order that these constituent elements can be used again by other organisms. Composting is the process of encouraging this decomposition of organic material to create a dark brown, earthy, crumbly material referred to as compost. When added to soil, compost provides essential nutrients plants require, helps to store these nutrients and vastly improves the structure of the soil helping with both its porosity and water retention

To make compost is very simple, we just pile organic matter up in a designated area and eventually it will decompose and viola – compost! This process can take up to a year if not longer, depending on the material in the pile, how much moisture is in the material and how much air (oxygen) there is within the pile. However, by using specific organic materials in your pile with just enough water and oxygen between the layers, it’s possible to accelerate the decomposition process and make a very high quality compost within just three weeks. 

One of the main differences between a pile of organic matter that decomposes slowly (and often smells pretty bad) and a pile of organic matter that decomposes quickly is the presence of oxygen within the pile, and that there is a correct ratio of carbon/nitrogen within the organic matter. 

Oxygen levels 

When oxygen is present, aerobic microbes and invertebrates will be busy decomposing the organic matter. In environments without oxygen, only anaerobic organisms can survive. Aerobic organisms are much more abundant and efficient than anaerobic organisms, with anaerobes decomposing material at a much slower rate. 

The aerobic microbe players in compost production (from left to right) bacteria, actinomycetes, fungi, protozoa and rotifer

Carbon/nitrogen ratio 

Carbon (C) and nitrogen (N) are elements that can be found in organic materials. Microbes use carbon for energy and nitrogen for protein production. For the most efficient processing of organic matter to compost, the microbes require 30 parts carbon to 1 part nitrogen and if the microbes can find this balance they will be very active. In fact, the high activity of these numerous organisms breaking down organic matter will cause the temperature to rise in a compost pile (much the same way as the temperature in crowded nightclub or gig will rise). When the temperature hits a certain point, thermophilic (quite literally means heat loving) bacteria will be triggered and further accelerate the decomposition of the material and increase the temperature further. It’s quite normal for a compost pile to reach 55-60 degrees celsius within a few days. Interestingly, thermophilic bacteria are some of the oldest organisms on the planet and are ubiquitous but dormant in the absence of heat.

The key advantage of the thermophilic bacteria when composting is that the high temperatures they create kill any plant pathogens and pests that may be in the pile, destroy weed seeds and even kill pathogens and parasitic worms that are harmful to humans. All the organisms that cause human diseases are adapted to live around human body temperature, (normal 36.5-37.5°C (97.7–99.5°F)  maximum 44 °C - 46.5 °C  (111.2 °F - 115.7 °F) and higher temperatures will kill them. Compost that stays at 50°C (122°F) for at least 24 hours will be safe to use to grow food. A temperature of 46°C (115°F) will kill pathogens within a week, 62°C (143.6°F) will kill pathogens in one hour.

Pile size, shape and location

The size of the pile should be big enough to retain the heat that is generated during the process. A 1.3m3 pile is probably the minimum it should be and generally speaking, the larger the better. Dome shapes retain temperature most efficiently with less surface area to internal volume, but I find rectangles also work really well. 

I prefer to locate my compost piles where we will need the material and will often build a pile in an area that will be used for planting up later that season or the following season. Once the location is selected, the first stage is to slash all existing vegetation to ground level, broad fork the area and soak it thoroughly with water if it is dry.

For large scale compost making, it’s best to create rows of compost piles on a hard surface for easy mixing with front loading tractors. 

Making hot compost

Hot compost is one of many methods of composting that we regularly use. It involves creating the ideal conditions for the microbes to feed and breed so that they process the material very quickly. For the best performance, the composting microorganisms require the correct proportion of carbon for energy and nitrogen for protein production. They also need moisture and oxygen. This can be provided by piling carbon and nitrogen rich organic materials in alternating layers whilst soaking the dry material with water as we go, making sure to keep the pile light and fluffy to allow good air circulation (oxygen supply).

The ratio of carbon to nitrogen material required to create optimum conditions for the microbes is an exact science, and lots of scientific research can be found on the internet about this. Microorganisms that digest compost need about 30 parts of carbon for every part of nitrogen they consume. That's a balanced diet for them. If there's too much nitrogen, the microorganisms can't use it all, and the excess is lost in the form of smelly ammonia gas. Nitrogen loss due to excess nitrogen in the pile (a low C:N ratio) can be over 60%. At a C:N ratio of 30 or 35 to 1, only one half of one percent of the nitrogen will be lost. That's why we don't want too much nitrogen (fresh manure, for example) in your compost: the nitrogen will be lost to the atmosphere in the form of ammonia gas, and nitrogen is too valuable for plants to allow it to escape into the atmosphere. 

The below lists the C:N ratio of some common compostable materials.

A simpler way to think about how to get the C:N ratio right is to aim for 2 parts brown to 1 part green ingredients in your compost. The materials containing high amounts of carbon are considered ‘browns’, e.g. cardboard, straw, paper and herbaceous perennial stalks from the previous season. The materials containing high amounts of nitrogen are considered ‘greens’, e.g. manure, fresh hay, seaweed, urine and algae. You don’t need to worry too much about this ratio, and I recommend just building a pile as described below and seeing what happens. You will soon learn what ratio of materials work well together. 

How we make our compost 

Green and brown materials we use for our compost piles 

  • Fresh cut grass and herbs - green 

  • Paulownia leaves - green 

  • Comfrey leaves - green 

  • Pond algae - green 

  • Fresh cow manure, sheep manure, horse manure (any manure will do) - green

  • Rabbit droppings - green 

  • Straw - brown

  • Sawdust - brown 

  • Perennial weed stalks cut down from the previous winter and thoroughly dried - brown

  • Soaked, shredded cardboard - brown 

You do not have to use so many different materials and straw, fresh cut grass or weeds and manure of any kind will do. I like to include a lot of variety based on an assumption that the more diverse your materials are the more diverse the microbe population will be and the more efficiently they will decompose the material. 

Hot compost making workflow 

  • Get your materials all together in the area you will build the pile and have a good supply of water available.

  • Begin by soaking the straw and sawdust and any other dry material you may be using.

  • Clear the area from existing vegetation and de-compact the soil, soaking well if dry. The base area should be at least 1.3m2.

  • Start with a layer of damp straw approx. 20cm thick and then add a layer of freshly cut grass or weeds (20cm thick), a fine sprinkling of wet sawdust, a layer of cow manure, sticks, straw, old sheep manure and wet sawdust, and then continue with this layering until you have got the pile the right size.

  • Layer by layer, insert a fork into the pile and pull the material towards the outer edge. This is to create adequate oxygen. 

  • When the pile is approx 1.3-1.5m high it’s ready. The pile should be light and fluffy and a little bit bouncy. 

  • To accelerate the decomposition, provide more oxygen by turning the pile after three or four days and working the material that was on the outside to the inside and add more moisture if needed. Turn again after 2-3 days and then again after another 2-3 days, and then leave to sit for a week.  The pile will be getting smaller all the time and when it is ready it will be around 1/3 - 1/4 of its original size.

  • Put the material through a sieve if you would like a fine tilth potting compost.

You do not need to turn the pile and we’ll often just build a pile in the spring or summer and leave it where it is until the autumn when we are ready to plant out, at which point we spread the material around the area and plant into it. Turning the pile is only useful when in a rush for the compost.


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Advantages and disadvantages of hot composting  

Advantages:

  • Finished compost in a matter of weeks (subject to weather conditions)

  • Higher nutrient content due to less leaching of nutrients

  • Weed tubers, rhizomes and seeds are destroyed in the high temperatures 

  • Plant pathogens are destroyed when the pile reaches 55 °C and above. 

Disadvantages:

  • A big effort required, especially if you are making the pile alone 

  • Large amounts of organic matter are required all at once.

Things to consider when building hot compost piles

  • Finely shredding the carbon rich ingredients such as fallen leaves, hay, straw, paper and cardboard will help considerably. Shredding increases the surface area that the compost microbes have to work on and provides a more even distribution of air and moisture among the material.

  • Build the compost pile where you want the compost to be so when it is ready all you have to do is spread it out.

  • Choose a spell of warm weather if possible and cover the pile if heavy rain is expected. 

  • If you have permanent areas in your garden where you make compost, plant out mineral repositors around the area to make the most of the nutrients that will inevitably leach from the pile.

  • Making compost with a group is a great group activity and we usually include making compost piles during our courses. People really enjoy the hands-on activity, experiencing a process from start to finish, and observing the heat building up the day after. With all of the material and tools on site and a source of water available we will usually build a 1.5 m3 pile within an hour and a half.

Composting without manure 

It’s entirely possible to create hot compost without using manure and probably the best example I have seen of this is with ramial woodchip (a type of woodchip made solely from small to medium-sized fresh branches). I used to work as an arborist and pretty much every day we would fill our vehicles with chipped branches and trimmings from hedges. 

Ramial woodchip - Photo from - www.learningandyearning.com/wood-chips

We’d usually tip the material at farms or municipal sites at the end of the day ready for work the next day but sometimes we’d be late and would have the material on the van overnight. On a cold morning the steam could be seen rising from the pile, the hot air from the decomposing chips mixing with cooler air. On one occasion I went on holiday for a week before tipping off and when I returned I noticed that the pile had shrunk by at least 1/3. When we did tip off there was a beautiful compost already forming within the pile, with most of the material in the centre coated with a soft white substance (probably actinomycetes, a mycelial bacteria).

Ramial woodchip after a week of decomposition 

The low diameter pruning from the trees rich in cambial tissue, along with the trimmings and leaves from the hedges contains the perfect C:N ratio providing the optimal conditions for the microbes.

Compost as habitat 

When you make your own compost, you are in effect breeding trillions upon trillions of tiny lifeforms commonly known as microbes. The microbes feast on the piled up organic matter you provide for them and then the microbes themselves provide meals for a range of other invertebrates such as beetles, centipedes and earthworms that in turn provide food for birds and mammals. At each trophic level, nutrient laden excrement is distributed throughout the material making the end product even more nutrient dense for plants.

A word on humus and compost

These terms are used often, yet the meaning of them and differences between them are generally not very well understood so I hope this will provide some clarity.

Compost - compost is the intentional accumulation and placement of organic matter, the aim being to accelerate the decaying process. The intentional part is important. Dead stuff on the ground is NOT compost, just decaying organic matter. It is the controlled, or semi-controlled conditions that make it compost.

Compost, even if mature, is still breaking down and supplying nutrients. When applied in your garden it has the immediate effect of adding nutrients available to plants and bacterial components that contribute to a healthy soil food web. As the seasons progress and decay continues, it eventually converts to humus.

Humus - humus is supposed to be a stable organic component, the result of the decay of organic matter whether that be natural decay or, as we see above, decay during composting.

Humus being stable cannot be penetrated by microbes and is greatly resistant to further decomposition. Thus stable humus adds few readily available nutrients to the soil, but plays an essential part in forming healthy soil by:

  • Improving soil structure (and texture)

  • Remarkable water retentive properties that help to store water in the soil

  • High cation exchange capacity (CEC), which means it acts as a storehouse for plant nutrients not allowing them to wash away (leach) from the soil with the water passing through the soil. The high CEC of humus is why it is regarded as being fertile.  

There is some debate regarding the existence of humus at all, although the existence of humic substances is generally accepted by most people. I have not looked too closely at the debate, but whether humus exists or not there is no need to worry as it's still super easy to build great soil.

  • Add plenty of organic matter to the soil via chop and drop mulching, manures and composts. 

  • Keep soils inhabited with diverse communities of living plants and mow and prune these plants to encourage root shed that add to the soil organic matter. 

  • Avoid any compaction to the soils you are cultivating - by foot or machine. 

  • Keep soils well hydrated - like a moist sponge is perfect. 

  • Don't use ‘icides’.


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Sunday, 9 February 2025

Unveiling Nature's Messengers: Indicator Plants

 Nature has its own language, and if you know how to read it, you can uncover valuable insights about the soil and environmental conditions of a place. Certain plants serve as reliable indicators, offering clues about soil type, pH levels, fertility, and even the history of a location. From the moisture-loving mosses to the acidic-soil-loving ferns, these silent messengers can reveal secrets hidden beneath the surface. But their language extends beyond soil – plants can also narrate stories about prevailing winds, herbivore presence, pollution levels, and habitat health. During this post we’ll explore the fascinating categories of indicator plants and look at a few of the species in each category.

Let’s start by looking at how plant form can signal environmental factors at work. For example, if there are trees on a site with lopsided crowns as in the photo below, it’s a clear indicator of potentially damaging prevailing winds that are killing the buds exposed to the initial force of wind, hence the tree grows one-sided.

Stone Pine - Pinus pinea on Iztuzu Beac, Dalyan, Turkiye probably the most striking examples of wind induced thigmomorphogenisis I’ve seen.

The small bushy shrubs in the below image are an indicator that herbivorous mammals frequent the area. The bushy form is the result of the herbaceous tips of the plants being grazed by the mammals, with the removal of the apical buds promoting growth of the buds lower down the stem. This type of habitat, i.e. grasses with some low bushy shrubs, is often an indicator of abandoned agricultural land. If left alone it will eventually revert to woodland.

Indicator Plant Categories

Indicator plants can also be categorized based on the types of environmental conditions they indicate. Here's a breakdown of these indication categories:

1. Soil pH Indicators:

  • Acidic Soil Indicator Plants: These plants thrive in soils with low pH levels (acidic conditions), typically below 6. Examples include blueberry (Vaccinium spp.), rhododendron (Rhododendron spp.).

  • Alkaline Soil Indicator Plants: These plants prefer soils with high pH levels (alkaline or basic conditions), often above 7. Examples include lupine (Lupinus spp.), yucca (Yucca spp.).

2. Moisture Indicators:

  • Wetland Indicator Plants: Plants that indicate wet or waterlogged conditions, such as sphagnum moss and sensitive fern (Onoclea sensibilis).

  • Drought-Tolerant Indicator Plants: Plants that thrive in dry conditions, often found in arid regions or well-drained soils, like buckwheat (Eriogonum spp.).

3. Pollution Indicators:

  • Air Quality Indicator Plants: Lichens are sensitive to air pollutants like sulfur dioxide and heavy metals, indicating air quality and pollution levels.

  • Water Pollution Indicator Plants: Aquatic plants like cattails and water hyacinths can indicate water pollution and nutrient contamination.

4. Nutrient and Soil Quality Indicators:

  • Nitrogen-Rich Soil Indicator Plants: Plants that grow well in nutrient-rich soils, like nettle (Urtica dioica). This is a very reliable indicator.

  • Poor Soil Fertility Indicator Plants: Plants that can thrive in nutrient-depleted soils, like Clover (Trifolium spp.).

5. Disturbance Indicators:

  • Disturbed Soil Indicator Plants: Plants that colonize disturbed or compacted soils, such as dandelion (Taraxacum officinale) and mullein (Verbascum spp.).

  • Reclaimed Land Indicator Plants: Species that appear after land disturbances, often indicating the restoration process.

6. Habitat Indicators:

  • Riparian Indicator Plants: Plants that grow in areas near water bodies, indicating wet or riparian habitats, like Alder (Alnus glutinosa).

  • Calcareous Soil Indicator Plants: Plants that indicate limestone-rich or calcareous soils, like wild columbine (Aquilegia canadensis).

7. Succession Indicators:

  • Early Succession Indicator Plants: Species that appear in disturbed or open areas during early stages of ecological succession.

  • Late Succession Indicator Plants: Species that become dominant as ecosystems mature and transition towards climax communities.

8. Habitat-Specific Indicators:

  • Woodland Indicator Plants: Plants that prefer forested environments and indicate well-drained, shaded soils.

  • Grassland Indicator Plants: Plants that thrive in open grasslands, often indicating sunlight exposure.

From Sepp Holzer

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Here is a list of some common species from each category.

Using plants as soil indicators works better in the wild or on neglected land than it does in an established garden because many of the plants that can signal conditions will grow perfectly well on good soils as well as compacted, acidic, alkaline, dry or low/high fertility soils. However, if you find one of the indicator species listed below growing as the dominant species in a given area, it’s more likely they are indicating a certain soil condition. The plants that indicate fertility and acidity are probably the most reliable indicators.

The below table lists some of the most common soil indicator plants along with some notes


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